National Library of Energy BETA

Sample records for belts speedometer odometer

  1. Laterally bendable belt conveyor

    DOE Patents [OSTI]

    Peterson, William J. (Coraopolis, PA)

    1985-01-01

    An endless, laterally flexible and bendable belt conveyor particularly adapted for coal mining applications in facilitating the transport of the extracted coal up- or downslope and around corners in a continuous manner is disclosed. The conveying means includes a flat rubber belt reinforced along the middle portion thereof along which the major portion of the belt tension is directed so as to cause rotation of the tubular shaped belt when trammed around lateral turns thus preventing excessive belt bulging distortion between adjacent belt supports which would inhibit belt transport. Pretension induced into the fabric reinforced flat rubber belt by conventional belt take-up means supports the load conveyed when the belt conveyor is making lateral turns. The carrying and return portions of the belt are supported and formed into a tubular shape by a plurality of shapers positioned along its length. Each shaper is supported from above by a monorail and includes clusters of idler rollers which support the belt. Additional cluster rollers in each shaper permit the belt supporting roller clusters to rotate in response to the belt's operating tension imposed upon the cluster rollers by induced lateral belt friction forces. The freely rotating roller clusters thus permit the belt to twist on lateral curves without damage to itself while precluding escape of the conveyed material by effectively enclosing it in the tube-shaped, inner belt transport length.

  2. San Juan Montana Thrust Belt WY Thrust Belt Black Warrior

    U.S. Energy Information Administration (EIA) Indexed Site

    San Juan Montana Thrust Belt WY Thrust Belt Black Warrior Paradox - San Juan NW (2) Uinta- Piceance Paradox - San Juan SE (2) Florida Peninsula Appalachian- NY (1) Appalachian...

  3. Replace V-Belts with Notched or Synchronous Belt Drives

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Synchronous belts require minimal maintenance and retensioning, operate in wet and oily ... new installations; the price premium is minimal due to the avoidance of conventional ...

  4. SLH Timing Belt Powertrain

    SciTech Connect (OSTI)

    Schneider, Abe

    2014-04-09

    The main goal of this proposal was to develop and test a novel powertrain solution for the SLH hydroEngine—, a low-cost, efficient low-head hydropower technology. Nearly two-thirds of U.S. renewable electricity is produced by hydropower (EIA 2010). According to the U.S. Department of Energy; this amount could be increased by 50% with small hydropower plants, often using already-existing dams (Hall 2004). There are more than 80,000 existing dams, and of these, less than 4% generate power (Blankinship 2009). In addition, there are over 800 irrigation districts in the U.S., many with multiple, non-power, low-head drops. These existing, non-power dams and irrigation drops could be retrofitted to produce distributed, baseload, renewable energy with appropriate technology. The problem is that most existing dams are low-head, or less than 30 feet in height (Ragon 2009). Only about 2% of the available low-head hydropower resource in the U.S. has been developed, leaving more than 70 GW of annual mean potential low-head capacity untapped (Hall 2004). Natel Energy, Inc. is developing a low-head hydropower turbine that operates efficiently at heads less than 6 meters and is cost-effective for deployment across multiple low-head structures. Because of the unique racetrack-like path taken by the prime-movers in the SLH, a flexible powertrain is required. Historically, the only viable technological solution was roller chain. Despite the having the ability to easily attach blades, roller chain is characterized by significant drawbacks, including high cost, wear, and vibration from chordal action. Advanced carbon-#12;fiber-reinforced timing belts have been recently developed which, coupled with a novel belt attachment system developed by Natel Energy, result in a large reduction in moving parts, reduced mass and cost, and elimination of chordal action for increased fatigue life. The work done in this project affirmatively addressed each of the following 3 major uncertainties concerning a timing-belt based hydroEngine —powertrain: 1. Can a belt handle the high torques and power loads demanded by the SLH? (Yes.) 2. Can the SLH blades be mounted to belt with a connection that can withstand the loads encountered in operation? (Yes.) 3. Can the belt, with blade attachments, live through the required cyclic loading? (Yes.) The research adds to the general understanding of sustainable small hydropower systems by using innovative system testing to develop and demonstrate performance of a novel powertrain solution, enabling a new type of hydroelectric turbine to be commercially developed. The technical effectiveness of the methods investigated has been shown to be positive through an extensive design and testing process accommodating many constraints and goals, with a major emphasis on high cycle fatigue life. Economic feasibility of the innovations has been demonstrated through many iterations of design for manufacturability and cost reduction. The project is of benefit to the public because it has helped to develop a solution to a major problem -- despite the large available potential for new low-head hydropower, high capital costs and high levelized cost of electricity (LCOE) continue to be major barriers to project development. The hydroEngine— represents a significant innovation, leveraging novel fluid mechanics and mechanical configuration to allow lower-cost turbine manufacture and development of low head hydropower resources.

  5. SunBelt Biofuels | Open Energy Information

    Open Energy Info (EERE)

    SunBelt Biofuels Jump to: navigation, search Logo: SunBelt Biofuels Name: SunBelt Biofuels Place: Soperton, Georgia Zip: 30457 Sector: Biomass Product: Freedom Giant Miscanthus...

  6. Replace V-Belts with Notched or Synchronous Belt Drives | Department of

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Energy V-Belts with Notched or Synchronous Belt Drives Replace V-Belts with Notched or Synchronous Belt Drives Belt drives provide flexibility in the positioning of the motor relative to the load. Pulleys (sheaves) of varying diameters allow the speed of the driven equipment to be increased or decreased relative to the motor speed. A properly designed belt power-transmission system offers high efficiency and low noise, requires no lubrication, and presents low maintenance requirements.

  7. Belt Vision Inspection System | Department of Energy

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Mine personnel can review live or historical images several times a day with minimal effort and take action before belt splices fail. The Belt Vision system helps eliminate costly ...

  8. Synchronous and Cogged Fan Belt Performance Assessment

    SciTech Connect (OSTI)

    Cutler, D.; Dean, J.; Acosta, J.

    2014-02-01

    The GSA Regional GPG Team commissioned the National Renewable Energy Laboratory (NREL) to perform monitoring of cogged V-belts and synchronous belts on both a constant volume and a variable air volume fan at the Byron G. Rodgers Federal Building and U.S. Courthouse in Denver, Colorado. These motor/fan combinations were tested with their original, standard V-belts (appropriately tensioned by an operation and maintenance professional) to obtain a baseline for standard operation. They were then switched to the cogged V-belts, and finally to synchronous belts. The power consumption by the motor was normalized for both fan speed and air density changes. This was necessary to ensure that the power readings were not influenced by a change in rotational fan speed or by the power required to push denser air. Finally, energy savings and operation and maintenance savings were compiled into an economic life-cycle cost analysis of the different belt options.

  9. CD-2: Orogenic Belt | Open Energy Information

    Open Energy Info (EERE)

    basin or orogenic mountain belt. Significant crustal subsidence (up to several kilometers) occurs in sedimentary sequences. This subsidence is due to the weight of the...

  10. Corn Belt Power Cooperative Rebate Program

    Broader source: Energy.gov [DOE]

    Corn Belt Power Cooperative is a generation and transmission electric cooperative that provides power to nine distribution rural electric cooperatives and one municipal electric cooperative. These...

  11. Picture of the Week: Bulging Van Allen Belts

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Bulging Van Allen Belts February 25, 2016 Bulging Van Allen Belts Learn about the Van Allen Belts and how new findings from NASA's Van Allen Probes could impact how we protect technology in space. To watch the video: click below

  12. Study finds surprising variability in shape of Van Allen Belts

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Study finds surprising variability in shape of Van Allen Belts Study finds surprising variability in shape of Van Allen Belts Understanding the shape and size of the belts, which shrink and swell in response to magnetic storms coming from the sun, is crucial for protecting our technology in space. February 23, 2016 1. The traditional idea of the radiation belts includes a larger, more dynamic outer belt and a smaller, more stable inner belt with an empty slot region separating the two. However,

  13. Electric filter with movable belt electrode

    DOE Patents [OSTI]

    Bergman, W.

    1983-09-20

    A method and apparatus for removing airborne contaminants entrained in a gas or airstream includes an electric filter characterized by a movable endless belt electrode, a grounded electrode, and a filter medium sandwiched there between. Inclusion of the movable, endless belt electrode provides the driving force for advancing the filter medium through the filter, and reduces frictional drag on the filter medium, thereby permitting a wide choice of filter medium materials. Additionally, the belt electrode includes a plurality of pleats in order to provide maximum surface area on which to collect airborne contaminants. 4 figs.

  14. Electric filter with movable belt electrode

    DOE Patents [OSTI]

    Bergman, Werner (Pleasanton, CA)

    1983-01-01

    A method and apparatus for removing airborne contaminants entrained in a gas or airstream includes an electric filter characterized by a movable endless belt electrode, a grounded electrode, and a filter medium sandwiched therebetween. Inclusion of the movable, endless belt electrode provides the driving force for advancing the filter medium through the filter, and reduces frictional drag on the filter medium, thereby permitting a wide choice of filter medium materials. Additionally, the belt electrode includes a plurality of pleats in order to provide maximum surface area on which to collect airborne contaminants.

  15. A new picture of the Van Allen Belts

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    A new picture of the Van Allen Belts A new picture of the Van Allen Belts A study conducted by Los Alamos and the New Mexico Consortium reveals that the shape of the Van Allen Belts is actually quite different than previously believed. January 21, 2016 van allen belts During geomagnetic storms, the empty region between the two belts can fill in completely with lower-energy electrons. Traditionally, scientists thought this slot region filled in only during the most extreme geomagnetic storms

  16. Picture of the Week: Bulging Van Allen Belts

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    2 Bulging Van Allen Belts Learn about the Van Allen Belts and how new findings from NASA's Van Allen Probes could impact how we protect technology in space. February 25, 2016 Bulging Van Allen Belts Watch the video on YouTube. Bulging Van Allen Belts Learn about the Van Allen Belts and how new findings from NASA's Van Allen Probes could impact how we protect technology in space

  17. Los Alamos provides HOPE for radiation belt storm probes

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    HOPE for radiation belt storm probes Los Alamos provides HOPE for radiation belt storm probes The HOPE analyzer is one of a suite of instruments that was successfully launched as part of the Radiation Belt Storm Probe mission. August 30, 2012 Artist's rendering showing two spacecraft representing the not-yet-designed Radiation Belt Storm Probes that will study the sun and its effects on Earth. PHOTO CREDIT: Johns Hopkins University Applied Physics Laboratory Artist's rendering showing two

  18. New compounds will help coal operators comply with BELT standards

    SciTech Connect (OSTI)

    2009-04-15

    US coal producers will soon have a new set of conveyor belting standards, which are currently proposed as a rulemaking by the Mine Safety and Health Administration (MSHA), to bring higher levels of resistance to propagation of fire by a secondary source. The new test being put into effect is known as a Belt Evaluation Laboratory Test (BELT). The article, submitted by Fenner Dunlop, discusses the company's testing procedures and the development of conveyors to comply with regulations. 2 photos.

  19. Mysterious electron stash found hidden among Van Allen belts

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Van Allen radiation belts Mysterious electron stash found hidden among Van Allen belts The belts are a pair of donut shaped zones of charged particles that surround Earth and occupy the inner region of our planet's Magnetosphere. March 1, 2013 This NASA rendering depicts Earth's Van Allen radiation belts and the path of the Van Allen Probe spacecraft, which were launched in August 2012. Data from the spacecraft have confirmed a never-before-seen phenomenon-a long-lived zone of high-energy

  20. Solar wind conditions leading to efficient radiation belt electron...

    Office of Scientific and Technical Information (OSTI)

    Solar wind conditions leading to efficient radiation belt electron acceleration: A superposed epoch analysis Citation Details In-Document Search This content will become publicly ...

  1. Magnetic refrigeration apparatus with belt of ferro or paramagnetic material

    DOE Patents [OSTI]

    Barclay, J.A.; Stewart, W.F.; Henke, M.D.; Kalash, K.E.

    1986-04-03

    A magnetic refrigerator operating in the 12 to 77 K range utilizes a belt which carries ferromagnetic or paramagnetic material and which is disposed in a loop which passes through the center of a solenoidal magnet to achieve cooling. The magnetic material carried by the belt, which can be blocks in frames of a linked belt, can be a mixture of substances with different Curie temperatures arranged such that the Curie temperatures progressively increase from one edge of the belt to the other. This magnetic refrigerator can be used to cool and liquefy hydrogen or other fluids.

  2. Magnetic refrigeration apparatus with belt of ferro or paramagnetic material

    DOE Patents [OSTI]

    Barclay, John A.; Stewart, Walter F.; Henke, Michael D.; Kalash, Kenneth E.

    1987-01-01

    A magnetic refrigerator operating in the 12 to 77K range utilizes a belt which carries ferromagnetic or paramagnetic material and which is disposed in a loop which passes through the center of a solenoidal magnet to achieve cooling. The magnetic material carried by the belt, which can be blocks in frames of a linked belt, can be a mixture of substances with different Curie temperatures arranged such that the Curie temperatures progressively increase from one edge of the belt to the other. This magnetic refrigerator can be used to cool and liquefy hydrogen or other fluids.

  3. Solar wind conditions leading to efficient radiation belt electron

    Office of Scientific and Technical Information (OSTI)

    acceleration: A superposed epoch analysis (Journal Article) | SciTech Connect Solar wind conditions leading to efficient radiation belt electron acceleration: A superposed epoch analysis Citation Details In-Document Search This content will become publicly available on September 7, 2016 Title: Solar wind conditions leading to efficient radiation belt electron acceleration: A superposed epoch analysis In this study by determining preferential solar wind conditions leading to efficient

  4. Angle stations in or for endless conveyor belts

    DOE Patents [OSTI]

    Steel, Alan

    1987-04-07

    In an angle station for an endless conveyor belt, there are presented to each incoming run of the belt stationary curved guide members (18, 19) of the shape of a major segment of a right-circular cylinder and having in the part-cylindrical portion (16 or 17) thereof rectangular openings (15) arranged in parallel and helical paths and through which project small freely-rotatable rollers (14), the continuously-changing segments of the curved surfaces of which projecting through said openings (15) are in attitude to change the direction of travel of the belt (13) through 90.degree. during passage of the belt about the part-cylindrical portion (16 or 17) of the guide member (18 or 19). The rectangular openings (15) are arranged with their longer edges lengthwise of the diagonals representing the mean of the helix but with those of a plurality of the rows nearest to each end of the part-cylindrical portion (16 or 17) slightly out of axial symmetry with said diagonals, being slightly inclined in a direction about the intersections (40) of the diagonals of the main portion of the openings, to provide a "toe-in" attitude in relation to the line of run of the endless conveyor belt.

  5. Early Proterozoic transcontinental orogenic belts in the United States

    SciTech Connect (OSTI)

    Van Schmus, W.R. . Dept. of Geology); Bickford, M.E. . Dept. of Geology); Condie, K.C. . Dept. Geoscience)

    1993-02-01

    It has been recognized for many years that Early Proterozoic orogenic rocks in the western US range from 1.8 to 1.6 Ga, with a general distribution such that 1.8 to 1.7 Ga rocks underlie Colorado, northern Arizona, and northern New Mexico and 1.7 to 1.6 Ga rocks underlie southern Arizona and southern New Mexico. Recent U-Pb geochronologic and Sm-Nd isotopic studies by a variety of research groups have refined crustal history in the western region and have extended knowledge eastward into the buried midcontinent basement. As a result, the authors propose that 1.8 Ga to 1.6 Ga crust of the US by divided into two distinct, but overlapping, orogenic belts: a 1.8 to 1.7 Ga Inner Accretionary Belt and a 1.7 to 1.6 Ga Outer Tectonic Belt. The Inner Accretionary Belt (IAB) comprises rock suites with compositions and isotopic signatures compatible with origin as juvenile crustal terranes formed as oceanic or off-shore and related terranes that were accreted to southern Laurentia between 1.8 and 1.6 Ga. The IAB includes the Yavapai Province of Arizona, Early Proterozoic basement of Colorado and southern Wyoming, and the basement of Nebraska. The Mojave Province of California may be part of this belt, although it also includes components derived from older Proterozoic or Archean crust. Extension of the IAB eastward from Nebraska is uncertain at present, although coeval rocks that may be eastern manifestations of this 1.8 to 1.7 Ga orogenesis occur in Wisconsin (1.76 Ga granite-rhyolite suite), Ontario (Killarney granite), Labrador (Makkovic Province) and southern Greenland (Ketilidian orogen). The Outer Tectonic Belt (OTB) comprises rock suites which have compositions, structures, and isotopic signature compatible with origin in continental margin tectonic settings between 1.7 and 1.6 Ga.

  6. Dotiki saves money and time with power tool and belt fasteners

    SciTech Connect (OSTI)

    Bargo, K.

    2009-11-15

    The use of a Hilti power tool to improve belt splice installations to minimise downtime is described. 3 photos.

  7. Effective Conveyor Belt Inspection for Improved Mining Productivity

    SciTech Connect (OSTI)

    Chris Fromme

    2006-06-01

    This document details progress on the project entitled ''Effective Conveyor Belt Inspection for Improved Mining Productivity'' during the period from November 15, 2004 to May 14, 2004. Highlights include fabrication of low-cost prototype hardware, acquisition of infrared thermal data, and initial design of a Smart-Camera based system.

  8. Effective Conveyor Belt Inspection for Improved Mining Productivity

    SciTech Connect (OSTI)

    Chris Fromme

    2006-06-01

    This document details progress on the project entitled ''Effective Conveyor Belt Inspection for Improved Mining Productivity'' during the period from November 15, 2004 to May 14, 2004. Highlights include fabrication of an improved LED lightbar, fabrication of a line-scan sensor head for the Smart-Camera based prototype, and development of prototype vulcanized splice detection algorithms.

  9. Effective Conveyor Belt Inspection for Improved Mining Productivity

    SciTech Connect (OSTI)

    David LaRose

    2006-07-01

    This document details progress on the project ''Effective Conveyor Belt Inspection for Improved Mining Productivity'' during the period from November 15, 2005 to May 14, 2006. Highlights include significant improvements in the accuracy and reliability of computer-vision based vulcanized splice detection, deployment of the vulcanized splice detection algorithms for daily use in two working mines, and successful demonstration of an early prototype of a Smart-Camera based system for on-site mechanical splice detection in coal mine installations.

  10. Effective Conveyer Belt Inspection for Improved Mining Productivity

    SciTech Connect (OSTI)

    David LaRose

    2006-11-14

    This document details progress on the project ''Effective Conveyor Belt Inspection for Improved Mining Productivity'' during the period from May 15, 2006 to November 14, 2006. Progress during this period includes significant advances in development of a Smart Camera based prototype system for on-site mechanical splice detection, and continued deployment of both the mechanical splice detection system and the vulcanized splice detection system in area coal mines.

  11. DREAM3D simulations of inner-belt dynamics

    SciTech Connect (OSTI)

    Cunningham, Gregory Scott

    2015-05-26

    A 1973 paper by Lyons and Thorne explains the two-belt structure for electrons in the inner magnetosphere as a balance between inward radial diffusion and loss to the atmosphere, where the loss to the atmosphere is enabled by pitch-angle scattering from Coulomb and wave-particle interactions. In the 1973 paper, equilibrium solutions to a decoupled set of 1D radial diffusion equations, one for each value of the first invariant of motion, ?, were computed to produce the equilibrium two-belt structure. Each 1D radial diffusion equation incorporated an L-and ?-dependent `lifetime' due to the Coulomb and wave-particle interactions. This decoupling of the problem is appropriate under the assumption that radial diffusion is slow in comparison to pitch-angle scattering. However, for some values of ? and L the lifetime associated with pitch-angle scattering is comparable to the timescale associated with radial diffusion, suggesting that the true equilibrium solutions might reflect `coupled modes' involving pitch-angle scattering and radial diffusion and thus requiring a 3D diffusion model. In the work we show here, we have computed the equilibrium solutions using our 3D diffusion model, DREAM3D, that allows for such coupling. We find that the 3D equilibrium solutions are quite similar to the solutions shown in the 1973 paper when we use the same physical models for radial diffusion and pitch-angle scattering from hiss. However, we show that the equilibrium solutions are quite sensitive to various aspects of the physics model employed in the 1973 paper that can be improved, suggesting that additional work needs to be done to understand the two-belt structure.

  12. First ultraviolet reflectance measurements of several Kuiper Belt objects, Kuiper Belt object satellites, and new ultraviolet measurements of A Centaur

    SciTech Connect (OSTI)

    Stern, S. A.; Schindhelm, E.; Cunningham, N. J.

    2014-05-01

    We observed the 2600-3200 (hereafter, mid-UV) reflectance of two Kuiper Belt Objects (KBOs), two KBO satellites, and a Centaur, using the Hubble Space Telescope (HST) Cosmic Origins Spectrograph (COS). Other than measurements of the Pluto system, these constitute the first UV measurements obtained of KBOs, and KBO satellites, and new HST UV measurements of the Centaur 2060 Chiron. We find significant differences among these objects, constrain the sizes and densities of Haumea's satellites, and report the detection of a possible spectral absorption band in Haumea's spectrum near 3050 . Comparisons of these objects to previously published UV reflectance measurements of Pluto and Charon are also made here.

  13. Ultra-low-frequency wave-driven diffusion of radiation belt relativistic electrons

    SciTech Connect (OSTI)

    Su, Zhenpeng; Zhu, Hui; Xiao, Fuliang; Zong, Q. -G.; Zhou, X. -Z.; Zheng, Huinan; Wang, Yuming; Wang, Shui; Hao, Y. -X.; Gao, Zhonglei; He, Zhaoguo; Baker, D. N.; Spence, H. E.; Reeves, G. D.; Blake, J. B.; Wygant, J. R.

    2015-12-22

    The Van Allen radiation belts are typically two zones of energetic particles encircling the Earth separated by the slot region. How the outer radiation belt electrons are accelerated to relativistic energies remains an unanswered question. Recent studies have presented compelling evidence for the local acceleration by very-low-frequency (VLF) chorus waves. However, there has been a competing theory to the local acceleration, radial diffusion by ultra-low-frequency (ULF) waves, whose importance has not yet been determined definitively. Here we report a unique radiation belt event with intense ULF waves but no detectable VLF chorus waves. So, our results demonstrate that the ULF waves moved the inner edge of the outer radiation belt earthward 0.3 Earth radii and enhanced the relativistic electron fluxes by up to one order of magnitude near the slot region within about 10 h, providing strong evidence for the radial diffusion of radiation belt relativistic electrons.

  14. Ultra-low-frequency wave-driven diffusion of radiation belt relativistic electrons

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Su, Zhenpeng; Zhu, Hui; Xiao, Fuliang; Zong, Q. -G.; Zhou, X. -Z.; Zheng, Huinan; Wang, Yuming; Wang, Shui; Hao, Y. -X.; Gao, Zhonglei; et al

    2015-12-22

    The Van Allen radiation belts are typically two zones of energetic particles encircling the Earth separated by the slot region. How the outer radiation belt electrons are accelerated to relativistic energies remains an unanswered question. Recent studies have presented compelling evidence for the local acceleration by very-low-frequency (VLF) chorus waves. However, there has been a competing theory to the local acceleration, radial diffusion by ultra-low-frequency (ULF) waves, whose importance has not yet been determined definitively. Here we report a unique radiation belt event with intense ULF waves but no detectable VLF chorus waves. So, our results demonstrate that the ULFmore » waves moved the inner edge of the outer radiation belt earthward 0.3 Earth radii and enhanced the relativistic electron fluxes by up to one order of magnitude near the slot region within about 10 h, providing strong evidence for the radial diffusion of radiation belt relativistic electrons.« less

  15. MAIN-BELT COMET P/2012 T1 (PANSTARRS)

    SciTech Connect (OSTI)

    Hsieh, Henry H.; Kaluna, Heather M.; Yang Bin; Haghighipour, Nader; Micheli, Marco; Denneau, Larry; Jedicke, Robert; Kleyna, Jan; Veres, Peter; Wainscoat, Richard J.; Ansdell, Megan; Elliott, Garrett T.; Keane, Jacqueline V.; Meech, Karen J.; Riesen, Timm E.; Sonnett, Sarah; Novakovic, Bojan; Fitzsimmons, Alan; Moskovitz, Nicholas A.; Sheppard, Scott S.; and others

    2013-07-01

    We present initial results from observations and numerical analyses aimed at characterizing the main-belt comet P/2012 T1 (PANSTARRS). Optical monitoring observations were made between 2012 October and 2013 February using the University of Hawaii 2.2 m telescope, the Keck I telescope, the Baade and Clay Magellan telescopes, Faulkes Telescope South, the Perkins Telescope at Lowell Observatory, and the Southern Astrophysical Research Telescope. The object's intrinsic brightness approximately doubles from the time of its discovery in early October until mid-November and then decreases by {approx}60% between late December and early February, similar to photometric behavior exhibited by several other main-belt comets and unlike that exhibited by disrupted asteroid (596) Scheila. We also used Keck to conduct spectroscopic searches for CN emission as well as absorption at 0.7 {mu}m that could indicate the presence of hydrated minerals, finding an upper limit CN production rate of Q{sub CN} < 1.5 Multiplication-Sign 10{sup 23} mol s{sup -1}, from which we infer a water production rate of Q{sub H{sub 2O}}<5 Multiplication-Sign 10{sup 25} mol s{sup -1}, and no evidence of the presence of hydrated minerals. Numerical simulations indicate that P/2012 T1 is largely dynamically stable for >100 Myr and is unlikely to be a recently implanted interloper from the outer solar system, while a search for potential asteroid family associations reveals that it is dynamically linked to the {approx}155 Myr old Lixiaohua asteroid family.

  16. Grenville foreland thrust belt hidden beneath the eastern US midcontinent

    SciTech Connect (OSTI)

    Hauser, E.C. (Cornell Univ., Ithaca, NY (United States))

    1993-01-01

    Grenville foreland thrust structures are observed beneath the eastern US midcontinent on COCORP (Consortium for Continental Reflection Profiling) line OH-1 and a short seismic line in southwest Ohio. These structures represent the first evidence for a significant Grenville foreland thrust belt preserved in eastern North America. On the COCORP lines, the structures include a thrust ramp anticline and an associated asymmetric syncline. The Grenville front tectonic zone appears to truncate these foreland structures, indicating a later, second phase expressed as a deeply penetrating, out-of-sequence thrust zone associated with the main uplift of the Grenville province on the east. A short, shallow seismic line in southwestern Ohio reveals an east-dipping sequence of prominently layered rocks that may lie above a footwall ramp to a deeper Grenville thrust fault. A drill hole into the less reflective top of this dipping sequence encountered unmetamorphosed sedimentary rocks like those increasingly reported from other drill holes in southwestern Ohio and adjacent states. Although possibly part of a late Precambrian (Keweenawan ) rift, these clastic sedimentary rocks may instead preserve evidence of a heretofore unrecognized Grenville foreland basin in eastern North America. Alternatively these Precambrian sedimentary rocks together with an underlying, but yet undrilled, strongly layered sequence may correlate with similarly layered rocks observed on COCORP and industrial seismic lines within the Middle Proterozoic granite-rhyolite province to the west in Indiana and Illinois and indicate that unmetamorphosed sedimentary material is an important constituent of the granite-rhyolite province. 25 refs., 6 figs.

  17. Dynamical implantation of objects in the Kuiper Belt

    SciTech Connect (OSTI)

    Brasil, P. I. O.

    2014-09-01

    Several models have been suggested in the past to describe the dynamical formation of hot Kuiper Belt objects (hereafter Hot Classicals or HCs for short). Here, we discuss a dynamical mechanism that allows orbits to evolve from the primordial planetesimal disk at ? 35 AU to reach the orbital region now occupied by HCs. We performed three different sets of numerical simulations to illustrate this mechanism. Two of these simulations were based on modern theories for the early evolution of the solar system (the Nice and jumping-Jupiter models). The third simulation was performed with the purpose of increasing the resolution at 41-46 AU. The common aspect of these simulations is that Neptune scatters planetesimals from ? 35 AU to >40 AU and then undergoes a long phase of slow residual migration. Our results show that to reach an HC orbit, a scattered planetesimal needs to be captured in a mean motion resonance (MMR) with Neptune where the perihelion distance rises due to the Kozai resonance (which occurs in MMRs even for moderate inclinations). Finally, while Neptune is still migrating, the planetesimal is released from the MMR on a stable HC orbit. We show that the orbital distribution of HCs expected from this process provides a reasonable match to observations. The capture efficiency and the mass deposited into the HC region appears to be sensitive to the maximum eccentricity reached by Neptune during the planetary instability phase. Additional work will be needed to resolve this dependency in detail.

  18. COLOR DEPENDENCE IN THE SIZE DISTRIBUTION OF MAIN BELT ASTEROIDS REVISITED

    SciTech Connect (OSTI)

    August, Tyler M.; Wiegert, Paul A.

    2013-06-15

    The size distribution of the asteroid belt is examined with 16956 main belt asteroids detected in data taken from the Canada-France-Hawaii Telescope Legacy Survey in two filters (g' and r'). The cumulative H (absolute magnitude) distribution is examined in both filters, and both match well to simple power laws down to H = 17, with slopes in rough agreement with those reported the literature. This implies that disruptive collisions between asteroids are gravitationally dominated down to at least this size, and probably sub-kilometer scales. The slopes of these distributions appear shallower in the outer belt than the inner belt, and the g' distributions appear slightly steeper than the r'. The slope shallowing in the outer belt may reflect a real compositional difference: the inner asteroid belt has been suggested to consist mostly of stony and/or metallic S-type asteroids, whereas carbonaceous C-types are thought to be more prevalent further from the Sun. No waves are seen in the size distribution above H = 15. Since waves are expected to be produced at the transition from gravitationally-dominated to internal strength-dominated collisions, their absence here may imply that the transition occurs at sub-kilometer scales, much smaller than the H = 17 (diameter {approx} 1.6 km) cutoff of this study.

  19. Solar wind conditions leading to efficient radiation belt electron acceleration: A superposed epoch analysis

    SciTech Connect (OSTI)

    Li, W.; Thorne, R. M.; Bortnik, J.; Baker, D. N.; Reeves, G. D.; Kanekal, S. G.; Spence, H. E.; Green, J. C.

    2015-09-07

    In this study by determining preferential solar wind conditions leading to efficient radiation belt electron acceleration is crucial for predicting radiation belt electron dynamics. Using Van Allen Probes electron observations (>1 MeV) from 2012 to 2015, we identify a number of efficient and inefficient acceleration events separately to perform a superposed epoch analysis of the corresponding solar wind parameters and geomagnetic indices. By directly comparing efficient and inefficient acceleration events, we clearly show that prolonged southward Bz, high solar wind speed, and low dynamic pressure are critical for electron acceleration to >1 MeV energies in the heart of the outer radiation belt. We also evaluate chorus wave evolution using the superposed epoch analysis for the identified efficient and inefficient acceleration events and find that chorus wave intensity is much stronger and lasts longer during efficient electron acceleration events, supporting the scenario that chorus waves play a key role in MeV electron acceleration.

  20. Source and seed populations for relativistic electrons: Their roles in radiation belt changes

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Jaynes, A. N.; Baker, D. N.; Singer, H. J.; Rodriguez, J. V.; Loto'aniu, T. M.; Ali, A. F.; Elkington, S. R.; Li, X.; Kanekal, S. G.; Claudepierre, S. G.; et al

    2015-09-09

    Strong enhancements of outer Van Allen belt electrons have been shown to have a clear dependence on solar wind speed and on the duration of southward interplanetary magnetic field. However, individual case study analyses also have demonstrated that many geomagnetic storms produce little in the way of outer belt enhancements and, in fact, may produce substantial losses of relativistic electrons. In this study, focused upon a key period in August–September 2014, we use GOES geostationary orbit electron flux data and Van Allen Probes particle and fields data to study the process of radiation belt electron acceleration. One particular interval, 13–22more » September, initiated by a short-lived geomagnetic storm and characterized by a long period of primarily northward interplanetary magnetic field (IMF), showed strong depletion of relativistic electrons (including an unprecedented observation of long-lasting depletion at geostationary orbit) while an immediately preceding, and another immediately subsequent, storm showed strong radiation belt enhancement. We demonstrate with these data that two distinct electron populations resulting from magnetospheric substorm activity are crucial elements in the ultimate acceleration of highly relativistic electrons in the outer belt: the source population (tens of keV) that give rise to VLF wave growth and the seed population (hundreds of keV) that are, in turn, accelerated through VLF wave interactions to much higher energies. ULF waves may also play a role by either inhibiting or enhancing this process through radial diffusion effects. Furthermore, if any components of the inner magnetospheric accelerator happen to be absent, the relativistic radiation belt enhancement fails to materialize.« less

  1. Source and seed populations for relativistic electrons: Their roles in radiation belt changes

    SciTech Connect (OSTI)

    Jaynes, A. N.; Baker, D. N.; Singer, H. J.; Rodriguez, J. V.; Loto'aniu, T. M.; Ali, A. F.; Elkington, S. R.; Li, X.; Kanekal, S. G.; Claudepierre, S. G.; Fennell, J. F.; Li, W.; Thorne, R. M.; Kletzing, C. A.; Spence, H. E.; Reeves, G. D.

    2015-09-09

    Strong enhancements of outer Van Allen belt electrons have been shown to have a clear dependence on solar wind speed and on the duration of southward interplanetary magnetic field. However, individual case study analyses also have demonstrated that many geomagnetic storms produce little in the way of outer belt enhancements and, in fact, may produce substantial losses of relativistic electrons. In this study, focused upon a key period in AugustSeptember 2014, we use GOES geostationary orbit electron flux data and Van Allen Probes particle and fields data to study the process of radiation belt electron acceleration. One particular interval, 1322 September, initiated by a short-lived geomagnetic storm and characterized by a long period of primarily northward interplanetary magnetic field (IMF), showed strong depletion of relativistic electrons (including an unprecedented observation of long-lasting depletion at geostationary orbit) while an immediately preceding, and another immediately subsequent, storm showed strong radiation belt enhancement. We demonstrate with these data that two distinct electron populations resulting from magnetospheric substorm activity are crucial elements in the ultimate acceleration of highly relativistic electrons in the outer belt: the source population (tens of keV) that give rise to VLF wave growth and the seed population (hundreds of keV) that are, in turn, accelerated through VLF wave interactions to much higher energies. ULF waves may also play a role by either inhibiting or enhancing this process through radial diffusion effects. Furthermore, if any components of the inner magnetospheric accelerator happen to be absent, the relativistic radiation belt enhancement fails to materialize.

  2. Method for determining molten metal pool level in twin-belt continuous casting machines

    DOE Patents [OSTI]

    Kaiser, Timothy D. (Colchester, VT); Daniel, Sabah S. (Pittsburgh, PA); Dykes, Charles D. (Milton, VT)

    1989-03-21

    A method for determining level of molten metal in the input of a continuous metal casting machine having at least one endless, flexible, revolving casting belt with a surface which engages the molten metal to be cast and a reverse, cooled surface along which is directed high velocity liquid coolant includes the steps of predetermining the desired range of positions of the molten metal pool and positioning at least seven heat-sensing transducers in bearing contact with the moving reverse belt surface and spaced in upstream-downstream relationship relative to belt travel spanning the desired pool levels. A predetermined temperature threshold is set, somewhat above coolant temperature and the output signals of the transducer sensors are scanned regarding their output signals indicative of temperatures of the moving reverse belt surface. Position of the molten pool is determined using temperature interpolation between any successive pair of upstream-downstream spaced sensors, which follows confirmation that two succeeding downstream sensors are at temperature levels exceeding threshold temperature. The method accordingly provides high resolution for determining pool position, and verifies the determined position by utilizing full-strength signals from two succeeding downstream sensors. In addition, dual sensors are used at each position spanning the desired range of molten metal pool levels to provide redundancy, wherein only the higher temperature of each pair of sensors at a station is utilized.

  3. THE NUCLEUS OF MAIN-BELT COMET 259P/GARRADD

    SciTech Connect (OSTI)

    MacLennan, Eric M.; Hsieh, Henry H. E-mail: emaclenn@utk.edu

    2012-10-10

    We present observations of the main-belt comet 259P/Garradd, previously known as P/2008 R1 (Garradd), obtained in 2011 and 2012 using the Gemini North Telescope on Mauna Kea in Hawaii and the SOAR telescope at Cerro Pachon in Chile, with the goal of computing the object's phase function and nucleus size. We find an absolute magnitude of H{sub R} = 19.71 {+-} 0.05 mag and slope parameter of G{sub R} = -0.08 {+-} 0.05 for the inactive nucleus, corresponding to an effective nucleus radius of r{sub e} = 0.30 {+-} 0.02 km, assuming an R-band albedo of p{sub R} = 0.05. We also revisit observations reported for 259P while it was active in 2008 to quantify the dust mass loss and compare the object with other known main-belt comets.

  4. A SOUTHERN SKY AND GALACTIC PLANE SURVEY FOR BRIGHT KUIPER BELT OBJECTS

    SciTech Connect (OSTI)

    Sheppard, Scott S.; Udalski, Andrzej; Kubiak, Marcin; Pietrzynski, Grzegorz; Poleski, Radoslaw; Soszynski, Igor; Szymanski, Michal K.; Ulaczyk, Krzysztof; Trujillo, Chadwick

    2011-10-15

    About 2500 deg{sup 2} of sky south of declination -25{sup 0} and/or near the Galactic Plane were surveyed for bright outer solar system objects. This survey is one of the first large-scale southern sky and Galactic Plane surveys to detect dwarf planets and other bright Kuiper Belt Objects in the trans-Neptunian region. The survey was able to obtain a limiting R-band magnitude of 21.6. In all, 18 outer solar system objects were detected, including Pluto which was detected near the Galactic center using optimal image subtraction techniques to remove the high stellar density background. Fourteen of the detections were previously unknown trans-Neptunian objects, demonstrating that the southern sky had not been well searched to date for bright outer solar system objects. Assuming moderate albedos, several of the new discoveries from this survey could be in hydrostatic equilibrium and thus could be considered dwarf planets. Combining this survey with previous surveys from the northern hemisphere suggests that the Kuiper Belt is nearly complete to around 21st magnitude in the R band. All the main dynamical classes in the Kuiper Belt are occupied by at least one dwarf-planet-sized object. The 3:2 Neptune resonance, which is the innermost well-populated Neptune resonance, has several large objects while the main outer Neptune resonances such as the 5:3, 7:4, 2:1, and 5:2 do not appear to have any large objects. This indicates that the outer resonances are either significantly depleted in objects relative to the 3:2 resonance or have a significantly different assortment of objects than the 3:2 resonance. For the largest objects (H < 4.5 mag), the scattered disk population appears to have a few times more objects than the main Kuiper Belt (MKB) population, while the Sedna population could be several times more than that of the MKB.

  5. From: Hope Albright To: Congestion Study Comments Subject: Block Grain Belt

    Office of Environmental Management (EM)

    Hope Albright To: Congestion Study Comments Subject: Block Grain Belt Date: Monday, September 22, 2014 11:52:07 AM I am opposed to the establishment of National Interest Energy Transmission Corridors (NIETC's) for the following reasons. First, the easements place an undo burden on landowners on and near the transmission lines. The compensation cannot begin to cover the all of the losses, tangible and intangible that landowners would suffer. Second, I believe that condemning private property for

  6. From: Kathy Mikels To: Congestion Study Comments Subject: STOP CLEAN LINE, BLOCK GRAIN BELT

    Office of Environmental Management (EM)

    Kathy Mikels To: Congestion Study Comments Subject: STOP CLEAN LINE, BLOCK GRAIN BELT Date: Monday, September 22, 2014 1:33:53 PM I am opposed to the establishment of National Interest Energy Transmission Corridors (NIETC's) for the following reasons. First, the easements place an undo burden on landowners on and near the transmission lines. The compensation cannot begin to cover the all of the losses, tangible and intangible that landowners would suffer. Second, I believe that condemning

  7. Solar wind conditions leading to efficient radiation belt electron acceleration: A superposed epoch analysis

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Li, W.; Thorne, R. M.; Bortnik, J.; Baker, D. N.; Reeves, G. D.; Kanekal, S. G.; Spence, H. E.; Green, J. C.

    2015-09-07

    In this study by determining preferential solar wind conditions leading to efficient radiation belt electron acceleration is crucial for predicting radiation belt electron dynamics. Using Van Allen Probes electron observations (>1 MeV) from 2012 to 2015, we identify a number of efficient and inefficient acceleration events separately to perform a superposed epoch analysis of the corresponding solar wind parameters and geomagnetic indices. By directly comparing efficient and inefficient acceleration events, we clearly show that prolonged southward Bz, high solar wind speed, and low dynamic pressure are critical for electron acceleration to >1 MeV energies in the heart of the outermore » radiation belt. We also evaluate chorus wave evolution using the superposed epoch analysis for the identified efficient and inefficient acceleration events and find that chorus wave intensity is much stronger and lasts longer during efficient electron acceleration events, supporting the scenario that chorus waves play a key role in MeV electron acceleration.« less

  8. Near-infrared spectra of high-albedo outer main-belt asteroids

    SciTech Connect (OSTI)

    Kasuga, Toshihiro; Shirahata, Mai; Usui, Fumihiko; Kuroda, Daisuke; Ootsubo, Takafumi; Okamura, Natsuko; Hasegawa, Sunao

    2015-02-01

    Most outer main-belt asteroids have low albedos because of their carbonaceouslike bodies. However, infrared satellite surveys have revealed that some asteroids have high albedos, which may suggest the presence of unusual surface minerals for those primitive objects. We present new near-infrared (1.12.5 ?m) spectra of four outer main-belt asteroids with albedos ? 0.1. The C-complex asteroids (555) Norma and (2542) Calpurnia are featureless and have (50%60%) amorphous Mg pyroxenes that might explain the high albedos. Asteroids (701) Oriola (which is a C-complex asteroid) and (2670) Chuvashia (a D/T-type or M-type asteroid) show possible broad absorption bands (1.52.1 ?m). The feature can be reproduced by either Mg-rich amorphous pyroxene (with 50%60% and 80%95% Mg, respectively) or orthopyroxene (crystalline silicate), which might be responsible for the high albedos. No absorption features of water ice (near 1.5 and 2.0 ?m) are detected in the objects. We discuss the origin of high albedo components in the outer main-belt asteroids and their physical relations to comets.

  9. 2007 TY430: A COLD CLASSICAL KUIPER BELT TYPE BINARY IN THE PLUTINO POPULATION

    SciTech Connect (OSTI)

    Sheppard, Scott S.; Ragozzine, Darin; Trujillo, Chadwick

    2012-03-15

    Kuiper Belt object 2007 TY430 is the first wide, equal-sized, binary known in the 3:2 mean motion resonance with Neptune. The two components have a maximum separation of about 1 arcsec and are on average less than 0.1 mag different in apparent magnitude with identical ultra-red colors (g - i = 1.49 {+-} 0.01 mag). Using nearly monthly observations of 2007 TY430 from 2007 to 2011, the orbit of the mutual components was found to have a period of 961.2 {+-} 4.6 days with a semi-major axis of 21000 {+-} 160 km and eccentricity of 0.1529 {+-} 0.0028. The inclination with respect to the ecliptic is 15.68 {+-} 0.22 deg and extensive observations have allowed the mirror orbit to be eliminated as a possibility. The total mass for the binary system was found to be 7.90 {+-} 0.21 Multiplication-Sign 10{sup 17} kg. Equal-sized, wide binaries and ultra-red colors are common in the low-inclination 'cold' classical part of the Kuiper Belt and likely formed through some sort of three-body interactions within a much denser Kuiper Belt. To date 2007 TY430 is the only ultra-red, equal-sized binary known outside of the classical Kuiper Belt population. Numerical simulations suggest 2007 TY430 is moderately unstable in the outer part of the 3:2 resonance and thus 2007 TY430 is likely an escaped 'cold' classical object that later got trapped in the 3:2 resonance. Similar to the known equal-sized, wide binaries in the cold classical population, the binary 2007 TY430 requires a high albedo and very low density structure to obtain the total mass found for the pair. For a realistic minimum density of 0.5 g cm{sup -3} the albedo of 2007 TY430 would be greater than 0.17. For reasonable densities, the radii of either component should be less than 60 km, and thus the relatively low eccentricity of the binary is interesting since no tides should be operating on the bodies at their large distances from each other. The low prograde inclination of the binary also makes it unlikely that the Kozai mechanism could have altered the orbit, making the 2007 TY430 binary orbit likely one of the few relatively unaltered primordial binary orbits known. Under some binary formation models, the low-inclination prograde orbit of the 2007 TY430 binary indicates formation within a relatively high velocity regime in the Kuiper Belt.

  10. THE COLOR DIFFERENCES OF KUIPER BELT OBJECTS IN RESONANCE WITH NEPTUNE

    SciTech Connect (OSTI)

    Sheppard, Scott S.

    2012-12-01

    The optical colors of 58 objects in mean motion resonance with Neptune were obtained. The various Neptune resonant populations were found to have significantly different surface color distributions. The 5:3 and 7:4 resonances have semimajor axes near the middle of the main Kuiper Belt and both are dominated by ultra-red material (spectral gradient: S {approx}> 25). The 5:3 and 7:4 resonances have statistically the same color distribution as the low-inclination 'cold' classical belt. The inner 4:3 and distant 5:2 resonances have objects with mostly moderately red colors (S {approx} 15), similar to the scattered and detached disk populations. The 2:1 resonance, which is near the outer edge of the main Kuiper Belt, has a large range of colors with similar numbers of moderately red and ultra-red objects at all inclinations. The 2:1 resonance was also found to have a very rare neutral colored object showing that the 2:1 resonance is really a mix of all object types. The inner 3:2 resonance, like the outer 2:1, has a large range of objects from neutral to ultra-red. The Neptune Trojans (1:1 resonance) are only slightly red (S {approx} 9), similar to the Jupiter Trojans. The inner 5:4 resonance only has four objects with measured colors but shows equal numbers of ultra-red and moderately red objects. The 9:5, 12:5, 7:3, 3:1, and 11:3 resonances do not have reliable color distribution statistics since few objects have been observed in these resonances, though it appears noteworthy that all three of the measured 3:1 objects have only moderately red colors, similar to the 4:3 and 5:2 resonances. The different color distributions of objects in mean motion resonance with Neptune are likely a result from the disruption of the primordial Kuiper Belt from the scattering and migration of the giant planets. The few low-inclination objects known in the outer 2:1 and 5:2 resonances are mostly only moderately red. This suggests if the 2:1 and 5:2 have a cold low-inclination component, the objects likely had a significantly different origin than the ultra-red-dominated cold components of the cold classical belt and 5:3 and 7:4 resonances.

  11. New Horizons Science Photos from NASA's Pluto-Kuiper Belt Mission

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    DOE provided the power supply for NASA's New Horizons Mission, a mission to the Pluto and Charon, a double-planet system, and the Kuiper Belt. There are 61 science photos posted on the New Horizons website, along with mission photos, spacecraft images, launch photos, posters and renderings that are both scientific and artistic. Dates range from June of 2006 to February of 2008. The images can be searched by keywords, by date, or by subject topic. They can also be browsed as an entire list. Each image has a detailed description.

  12. The Cordilleran foreland thrust belt in northwestern Montana and northern Idaho from COCORP and industry seismic reflection data

    SciTech Connect (OSTI)

    Yoos, T.R.; Potter, C.J.; Thigpen, J.L.; Brown, L.D. (Cornell Univ., Ithaca, NY (United States))

    1991-06-01

    COCORP and petroleum industry seismic reflection profiles in northwestern Montana reveal the structure of the Cordilleran foreland thrust belt. The Front Ranges consist of thick thrust sheets containing Precambrian Belt Supergroup and Paleozoic miogeoclinal shelf rocks above a thin remnant of Paleozoic rocks and gently westward-dipping North American basement. Interpretation of the seismic data and results from a recent petroleum exploration well suggest that 15-22 km of Precambrian Belt Supergroup sedimentary rocks are present in several thrust plates beneath the eastern Purcell anticlinorium. Previous hypotheses of a large mass of Paleozoic miogeoclinal sedimentary rocks or slices of crystalline basement located beneath the eastern Purcell anticlinorium do not appear to be supported by the data. The easternmost occurrence of allochthonous basement is interpreted to be in the western part of the anticlinorium near the Montana-Idaho border. Comparison of the Cordilleran foreland thrust belt in northwestern Montana and southern Canada suggest that a change in the deep structure of the Purcell anticlinorium occurs along strike. The anticlinorium in southern Canada has been interpreted as a hanging-wall anticline that was thrust over the western edge of thick Proterozoic North American basement, whereas in northwestern Montana the anticlinorium appears to consist of a complex series of thrust sheets above highly attenuated North American basement.

  13. A PHOTOMETRIC SYSTEM FOR DETECTION OF WATER AND METHANE ICES ON KUIPER BELT OBJECTS

    SciTech Connect (OSTI)

    Trujillo, Chadwick A.; Sheppard, Scott S.; Schaller, Emily L. E-mail: sheppard@dtm.ciw.edu

    2011-04-01

    We present a new near-infrared photometric system for detection of water ice and methane ice in the solar system. The system consists of two medium-band filters in the K-band region of the near-infrared, which are sensitive to water ice and methane ice, plus continuum observations in the J band and Y band. The primary purpose of this system is to distinguish between three basic types of Kuiper Belt Objects (KBOs)-those rich in water ice, those rich in methane ice, and those with little absorbance. In this work, we present proof-of-concept observations of 51 KBOs using our filter system, 21 of which have never been observed in the near-infrared spectroscopically. We show that our custom photometric system is consistent with previous spectroscopic observations while reducing telescope observing time by a factor of {approx}3. We use our filters to identify Haumea collisional family members, which are thought to be collisional remnants of a much larger body and are characterized by large fractions of water ice on their surfaces. We add 2009 YE{sub 7} to the Haumea collisional family based on our water ice band observations (J - H{sub 2}O = -1.03 {+-} 0.27) which indicate a high amount of water ice absorption, our calculated proper orbital elements, and the neutral optical colors we measured, V - R = 0.38 {+-} 0.04, which are all consistent with the rest of the Haumea family. We identify several objects dynamically similar to Haumea as being distinct from the Haumea family as they do not have water ice on their surfaces. In addition, we find that only the largest KBOs have methane ice, and Haumea itself has significantly less water ice absorption than the smaller Haumea family members. We find no evidence for other families in the Kuiper Belt.

  14. Non-diffusive resonant acceleration of electrons in the radiation belts

    SciTech Connect (OSTI)

    Artemyev, A. V.; Krasnoselskikh, V. V.; Agapitov, O. V.; Rolland, G.

    2012-12-15

    We describe a mechanism of resonant electron acceleration by oblique high-amplitude whistler waves under conditions typical for the Earth radiation belts. We use statistics of spacecraft observations of whistlers in the Earth radiation belts to obtain the dependence of the angle {theta} between the wave-normal and the background magnetic field on magnetic latitude {lambda}. According to this statistics, the angle {theta} already approaches the resonance cone at {lambda}{approx}15 Degree-Sign and remains close to it up to {lambda}{approx}30 Degree-Sign -40 Degree-Sign on the dayside. The parallel component of the electrostatic field of whistler waves often increases around {lambda}{approx}15 Degree-Sign up to one hundred of mV/m. We show that due to this increase of the electric field, the whistler waves can trap electrons into the potential well via wave particle resonant interaction corresponding to Landau resonance. Trapped electrons then move with the wave to higher latitudes where they escape from the resonance. Strong acceleration is favored by adiabatic invariance along the increasing magnetic field, which continuously transfers the parallel energy gained to perpendicular energy, allowing resonance to be reached and maintained. The concomitant increase of the wave phase velocity allows for even stronger relative acceleration at low energy <50keV. Each trapping-escape event of electrons of {approx}10keV to 100 keV results in an energy gain of up to 100 keV in the inhomogeneous magnetic field of the Earth dipole. For electrons with initial energy below 100 keV, such rapid acceleration should hasten their drop into the loss-cone and their precipitation into the atmosphere. We discuss the role of the considered mechanism in the eventual formation of a trapped distribution of relativistic electrons for initial energies larger than 100 keV and in microbursts precipitations of lower energy particles.

  15. A long-lived relativistic electron storage ring embedded in Earth's Outer Van Allen belt

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Baker, D. N.; Kanekal, S. G.; Hoxie, V. C.; Henderson, M. G.; Li, X.; Spence, H. E.; Elkington, S. R.; Friedel, R. H. W.; Goldstein, J.; Hudson, M. K.; et al

    2013-02-28

    Since their discovery over 50 years ago, the Earth’s Van Allen radiation belts are thought to consist of two distinct zones of trapped, highly energetic charged particles. The outer zone is comprised predominantly of mega-electron volt (MeV) electrons that wax and wane in intensity on time scales ranging from hours to days depending primarily on external forcing by the solar wind. Thus, the spatially separated inner zone is comprised of commingled high-energy electrons and very energetic positive ions (mostly protons), the latter being stable in intensity levels over years to decades. In situ energy-specific and temporally resolved spacecraft observations revealmore » an isolated third ring, or torus, of high-energy (E > 2 MeV) electrons that formed on 2 September 2012 and persisted largely unchanged in the geocentric radial range of 3.0 to ~3.5 Earth radii for over four weeks before being disrupted (and virtually annihilated) by a powerful interplanetary shock wave passage.« less

  16. Gold deposits in the late Archaean Nzega-Igunga greenstone belt, central plateau of tanzania

    SciTech Connect (OSTI)

    Feiss, P.G.; Siyomana, S.

    1985-01-01

    2.2 m oz of gold have been produced, since 1935, from late Archaean (2480-2740 Ma) greenstone belts of the Central Plateau, Tanzania. North and east of Nzega (4/sup 0/12'S, 3/sup 0/11'E), 18% of the exposed basement, mainly Dodoman schists and granites, consists of metavolcanics and metasediments of the Nyanzian and Kavirondian Series. Four styles of mineralization are observed. 1. Stratabound quartz-gold veins with minor sulfides. Host rocks are quartz porphyry, banded iron formation (BIF), magnetite quartzite, and dense, cherty jasperite at the Sekenke and Canuck mines. The Canuck veins are on strike from BIF's in quartz-eye porphyry of the Igusule Hills. 2. Stratabound, disseminated gold in coarse-grained, crowded feldspar porphyry with lithic fragments and minor pyrite. At Bulangamilwa, the porphyry is conformable with Nyanzian-aged submarine (.) greenstone, volcanic sediment, felsic volcanics, and sericite phyllite. The deposits are on strike with BIF of the Wella Hills, which contains massive sulfide with up to 15% Pb+Zn. 3. Disseminated gold in quartz-albite metasomes in Nyanzian greenstones. At Kirondatal, alteration is associated with alaskites and feldspar porphyry dikes traceable several hundred meters into post-Dodoman diorite porphyry. Gold is with pyrite, arsenopyrite, pyrrhotite, minor chalcopyrite, and sphalerite as well as tourmalinite and silica-cemented breccias. 4. Basal Kavirondian placers in metaconglomerates containing cobbles and boulders of Dodoman and Nyanzian rocks several hundred meters up-section from the stratabound, disseminated mineralization at Bulangamilwa.

  17. Twin-belt continuous caster with containment and cooling of the exiting cast product for enabling high-speed casting of molten-center product

    DOE Patents [OSTI]

    Dykes, Charles D. (303 Shore Rd., Milton, VT); Daniel, Sabah S. (303 Shore Rd., Pittsburgh, PA); Wood, J. F. Barry (303 Shore Rd., Burlington, VT 05401)

    1990-02-20

    In continuously casting molten metal into cast product by a twin-belt machine, it is desirable to achieve dramatic increases in speed (linear feet per minute) at which cast product exits the machine, particularly in installations where steel cast product is intended to feed a downstream regular rolling mill (as distinct from a planetary mill) operating in tandem with the twin-belt caster. Such high-speed casting produces product with a relatively thin shell and molten interior, and the shell tends to bulge outwardly due to metallostatic head pressure of the molten center. A number of cooperative features enable high-speed, twin-belt casting: (1) Each casting belt is slidably supported adjacent to the caster exit pulley for bulge control and enhanced cooling of cast product. (2) Lateral skew steering of each belt provides an effective increase in moving mold length plus a continuity of heat transfer not obtained with prior art belt steering apparatus. (3) The exiting slab is contained and supported downstream from the casting machine to prevent bulging of the shell of the cast product, and (4) spray cooling is incorporated in the exit containment apparatus for secondary cooling of cast product.

  18. PHYSICAL PROPERTIES OF MAIN-BELT COMET 176P/LINEAR

    SciTech Connect (OSTI)

    Hsieh, Henry H.; Ishiguro, Masateru; Lacerda, Pedro; Jewitt, David E-mail: p.lacerda@qub.ac.uk E-mail: jewitt@ucla.edu

    2011-07-15

    We present a physical characterization of comet 176P/LINEAR, the third discovered member of the new class of main-belt comets, which exhibit cometary activity but are dynamically indistinguishable from main-belt asteroids. Observations show the object exhibiting a fan-shaped tail for at least one month in late 2005, but then becoming inactive in early 2006. During this active period, we measure broadband colors of B - V = 0.63 {+-} 0.02, V - R = 0.35 {+-} 0.02, and R - I = 0.31 {+-} 0.04. Using data from when the object was observed to be inactive, we derive best-fit IAU phase function parameters of H = 15.10 {+-} 0.05 mag and G = 0.15 {+-} 0.10, and best-fit linear phase function parameters of m(1, 1, 0) = 15.35 {+-} 0.05 mag and {beta} = 0.038 {+-} 0.005 mag deg{sup -1}. From this baseline phase function, we find that 176P exhibits a mean photometric excess of {approx}30% during its active period, implying an approximate total coma dust mass of M{sub d} {approx} (7.2 {+-} 3.6) x 10{sup 4} kg. From inactive data obtained in early 2007, we find a rotation period of P{sub rot} = 22.23 {+-} 0.01 hr and a peak-to-trough photometric range of {Delta}m {approx} 0.7 mag. Phasing our photometric data from 176P's 2005 active period to this rotation period, we find that the nucleus exhibits a significantly smaller photometric range than in 2007 that cannot be accounted for by coma damping effects, and as such, are attributed by us to viewing geometry effects. A detailed analysis of these geometric effects showed that 176P is likely to be a highly elongated object with an axis ratio of 1.8 < b/a < 2.1, an orbital obliquity of {epsilon} {approx} 60{sup 0}, and a solstice position at a true anomaly of {nu}{sub o} = 20{sup 0} {+-} 20{sup 0}. Numerical modeling of 176P's dust emission found that its activity can only be reproduced by asymmetric dust emission, such as a cometary jet. We find plausible fits to our observations using models assuming {approx}10 {mu}m dust particles continuously emitted over the period during which 176P was observed to be active, and a jet direction of 180{sup 0} {approx}< {alpha}{sub jet} {approx}< 120{sup 0} and {delta}{sub jet} {approx} -60{sup 0}. We do not find good fits to our observations using models of impulsive dust emission, i.e., what would be expected if 176P's activity was an ejecta cloud resulting from an impact into non-volatile asteroid regolith. Since for a rotating body, the time-averaged direction of a non-equatorial jet is equivalent to the direction of the nearest rotation pole, we find an equivalent orbital obliquity of 50{sup 0} {approx}< {epsilon} {approx}< 75{sup 0}, consistent with the results of our light curve analysis. Furthermore, the results of both our light curve analysis and dust modeling analysis are consistent with the seasonal heating hypothesis used to explain the modulation of 176P's activity. Additional observations are highly encouraged to further characterize 176P's active behavior as the object approaches perihelion on 2011 July 1.

  19. Will new horizons see dust clumps in the Edgeworth-Kuiper Belt?

    SciTech Connect (OSTI)

    Vitense, Christian; Krivov, Alexander V.; Lhne, Torsten

    2014-06-01

    Debris disks are thought to be sculptured by neighboring planets. The same is true for the Edgeworth-Kuiper debris disk, yet no direct observational evidence for signatures of giant planets in the Kuiper Belt dust distribution has been found so far. Here we model the dust distribution in the outer solar system to reproduce the dust impact rates onto the dust detector on board the New Horizons spacecraft measured so far and to predict the rates during the Neptune orbit traverse. To this end, we take a realistic distribution of trans-Neptunian objects to launch a sufficient number of dust grains of different sizes and follow their orbits by including radiation pressure, Poynting-Robertson and stellar wind drag, as well as the perturbations of four giant planets. In a subsequent statistical analysis, we calculate number densities and lifetimes of the dust grains in order to simulate a collisional cascade. In contrast to the previous work, our model not only considers collisional elimination of particles but also includes production of finer debris. We find that particles captured in the 3:2 resonance with Neptune build clumps that are not removed by collisions, because the depleting effect of collisions is counteracted by production of smaller fragments. Our model successfully reproduces the dust impact rates measured by New Horizons out to ?23 AU and predicts an increase of the impact rate of about a factor of two or three around the Neptune orbit crossing. This result is robust with respect to the variation of the vaguely known number of dust-producing scattered disk objects, collisional outcomes, and the dust properties.

  20. Hubble space telescope investigation of main-belt comet 133P/Elst-Pizarro

    SciTech Connect (OSTI)

    Jewitt, David; Ishiguro, Masateru; Weaver, Harold; Agarwal, Jessica; Mutchler, Max; Larson, Steven

    2014-05-01

    We report new observations of the prototype main-belt comet (active asteroid) 133P/Elst-Pizarro taken at high angular resolution using the Hubble Space Telescope. The object has three main components: (1) a point-like nucleus; (2) a long, narrow antisolar dust tail; and (3) a short, sunward anti-tail. There is no resolved coma. The nucleus has a mean absolute magnitude H{sub V} = 15.70 0.10 and a light curve range ?V = 0.42 mag, the latter corresponding to projected dimensions 3.6 5.4 km (axis ratio 1.5:1) at the previously measured geometric albedo of 0.05 0.02. We explored a range of continuous and impulsive emission models to simultaneously fit the measured surface brightness profile, width, and position angle of the antisolar tail. Preferred fits invoke protracted emission, over a period of 150 days or less, of dust grains following a differential power-law size distribution with index 3.25 ?q ? 3.5 and with a wide range of sizes. Ultra-low surface brightness dust projected in the sunward direction is a remnant from emission activity occurring in previous orbits, and consists of the largest (?cm-sized) particles. Ejection velocities of one-micron-sized particles are comparable to the ?1.8 m s{sup 1} gravitational escape speed of the nucleus, while larger particles are released at speeds less than the gravitational escape velocity. The observations are consistent with, but do not prove, a hybrid hypothesis in which mass loss is driven by gas drag from the sublimation of near-surface water ice, but escape is aided by centripetal acceleration from the rotation of the elongated nucleus. No plausible alternative hypothesis has been identified.

  1. Crustal structure of mountain belts and basins: Industry and academic collaboration at Cornell

    SciTech Connect (OSTI)

    Allmendinger, R.; Barazangi, M.; Brown, L. [Cornell Univ., Ithaca, NY (United States)] [and others

    1995-08-01

    Interdisciplinary investigations of the large-scale structure and evolution of key basins and orogenic belts around the world are the focal point of academic-industry interaction at Cornell. Ongoing and new initiatives with significant industry involvement include: Project INDEPTH (Interdisciplinary Deep Profiling of Tibet and the Himalayas), a multinational effort to delineate deep structure across the type example of active continent-continent collision. 300 km of deep reflection profiling was collected across the Himalaya: and southern Tibet Plateau in 1992 and 1994. CAP (Cornell Andes Project), a long-standing interdisciplinary effort to understand the structure and evolution of the Andes, with a focus on Argentina, Chile and Bolivia. A deep reflection profile is tentatively planned for 1997. Intra-plate Orogeny in the Middle East and North Africa is the focus of multidisciplinary regional syntheses of existing seismic reflection and other databases in Syria (Palmyrides)and Morocco (Atlas), with an emphasis on reactivation and inversion tectonics. Project URSEIS (Urals Reflection Seismic Experiment and Integrated Studies) is a collaboration with EUROPROBE to collect 500 km of vibroseis and dynamite deep reflection profiling across the southern Urals in 1995. Project CRATON, an element in COCORP`s systematic exploration of the continental US, is a nascent multi-disciplinary effort to understand the buried craton of the central US and the basins built upon it. Global Basins Research Network (GBRN) is a diversified observational and computational effort to image and model the movement of pore fluids in detail and on a regional scale for a producing oil structure in the Gulf of Mexico.

  2. Geometry and evolution of the frontal part of the Magallanes foreland thrust and fold belt (Vicuna Area), Tierra del Fuego, southern Chile

    SciTech Connect (OSTI)

    Alvarez-Marron, J.; McClay, K.R. ); Harambour, S.; Rojas, L.; Skarmeta, J. )

    1993-11-01

    The Magallanes foreland thrust and fold belt is a thin-skinned foreland thrust and fold belt of Paleocene to Oligocene age that deforms Upper Jurassic through Tertiary volcanic, volcaniclastic, and siliciclastic strata of the Magallanes basin, southern Andean Cordillera, Chile. This paper is a detailed description and analysis of the geology and structural evolution of the thrust front (Vicuna area of southern Tierra del Fuego). Reflection seismic and well data, together with 1:50,000 scale geological mapping, have been used in the analysis. In the southern part of the Vicuna area, two different thrust systems have been found: an upper imbricate fan that deforms Upper Jurassic and Cretaceous strata, and a younger, lower duplex composed of Cretaceous and probably Upper Jurassic rocks. The imbricate fan is characterized by fault-propagation folding in which listric thrust faults merge downward into a sole thrust that probably is located within the Upper Jurassic stratigraphy. The sole thrust of the upper imbricates forms the roof thrust of the underlying duplex. In the northern part of the Vicuna area, the syntectonic sedimentary wedge of the foredeep consists of Late Cretaceous through Tertiary siliciclastics that have been deformed and uplifted by passive back thrusting at the triangle zone. The structural style in the foreland region shows three main subhorizontal detachment levels located within the sedimentary wedge as a result of the progressive transfer of slip from the thrust belt to the foreland. Minor blind thrusts produce stacked [open quotes]pop up[close quotes] and triangle structures that result in complex geometries in the cores of anticlines. A forward-breaking sequence of thrusting is interpreted. During deformation, the active foredeep wedge migrated at least 10 km northward. Balanced geological cross sections indicate approximately 60% (-30 km) shortening for this part of the Magallanes thrust belt.

  3. A Summary of Coupled, Uncoupled, and Hybrid Tectonic Models for the Yakima Fold Belt--Topical Report

    SciTech Connect (OSTI)

    Chamness, Michele A.; Winsor, Kelsey; Unwin, Stephen D.

    2012-08-01

    This document is one in a series of topical reports compiled by the Pacific Northwest National Laboratory to summarize technical information on selected topics important to the performance of a probabilistic seismic hazard analysis of the Hanford Site. The purpose of this report is to summarize the range of opinions and supporting information expressed by the expert community regarding whether a coupled or uncoupled model, or a combination of both, best represents structures in the Yakima Fold Belt. This issue was assessed to have a high level of contention with up to moderate potential for impact on the hazard estimate. This report defines the alternative conceptual models relevant to this technical issue and the arguments and data that support those models. It provides a brief description of the technical issue and principal uncertainties; a general overview on the nature of the technical issue, along with alternative conceptual models, supporting arguments and information, and uncertainties; and finally, suggests some possible approaches for reducing uncertainties regarding this issue.

  4. A Summary of Information on the Behavior of the Yakima Fold Belt as a Structural Entity -- Topical Report

    SciTech Connect (OSTI)

    Last, George V.; Winsor, Kelsey; Unwin, Stephen D.

    2012-08-01

    This document is one in a series of topical reports compiled by the Pacific Northwest National Laboratory to summarize technical information on selected topics important to the performance of a probabilistic seismic hazard analysis (PSHA) of the Hanford Site. The purpose of this report is to summarize available data and analyses relevant to the Yakima Fold Belt (YFB) that may bear on the question of whether or not the YFB behaves as a single seismotectonic province in which activity along one fold structure is representative of behavior along all other fold structures. This topic has met with a fairly high level of contention in the expert community and has the potential to result in significant impacts on an evaluation of seismic hazard at the Hanford Site. This report defines the relevant alternative conceptual models relevant to this technical issue and the arguments and data that support those models. It provides a brief description of the technical issue and principal uncertainties; a general overview on the nature of the technical issue, along with alternative conceptual models, supporting arguments and information, and uncertainties; and finally, it suggests some possible approaches for reducing uncertainties regarding this issue.

  5. CONSTRAINTS ON THE PHYSICAL PROPERTIES OF MAIN BELT COMET P/2013 R3 FROM ITS BREAKUP EVENT

    SciTech Connect (OSTI)

    Hirabayashi, Masatoshi; Snchez, Diego Paul; Gabriel, Travis; Scheeres, Daniel J.

    2014-07-01

    Jewitt etal. recently reported that main belt comet P/2013 R3 experienced a breakup, probably due to rotational disruption, with its components separating on mutually hyperbolic orbits. We propose a technique for constraining physical properties of the proto-body, especially the initial spin period and cohesive strength, as a function of the body's estimated size and density. The breakup conditions are developed by combining mutual orbit dynamics of the smaller components and the failure condition of the proto-body. Given a proto-body with a bulk density ranging from 1000kgm{sup 3} to 1500kgm{sup 3} (a typical range of the bulk density of C-type asteroids), we obtain possible values of the cohesive strength (40-210Pa) and the initial spin state (0.48-1.9hr). From this result, we conclude that although the proto-body could have been a rubble pile, it was likely spinning beyond its gravitational binding limit and would have needed cohesive strength to hold itself together. Additional observations of P/2013 R3 will enable stronger constraints on this event, and the present technique will be able to give more precise estimates of its internal structure.

  6. ON THE EFFECT OF GIANT PLANETS ON THE SCATTERING OF PARENT BODIES OF IRON METEORITE FROM THE TERRESTRIAL PLANET REGION INTO THE ASTEROID BELT: A CONCEPT STUDY

    SciTech Connect (OSTI)

    Haghighipour, Nader; Scott, Edward R. D.

    2012-04-20

    In their model for the origin of the parent bodies of iron meteorites, Bottke et al. proposed differentiated planetesimals, formed in 1-2 AU during the first 1.5 Myr, as the parent bodies, and suggested that these objects and their fragments were scattered into the asteroid belt as a result of interactions with planetary embryos. Although viable, this model does not include the effect of a giant planet that might have existed or been growing in the outer regions. We present the results of a concept study where we have examined the effect of a planetary body in the orbit of Jupiter on the early scattering of planetesimals from the terrestrial region into the asteroid belt. We integrated the orbits of a large battery of planetesimals in a disk of planetary embryos and studied their evolutions for different values of the mass of the planet. Results indicate that when the mass of the planet is smaller than 10 M{sub Circled-Plus }, its effects on the interactions among planetesimals and planetary embryos are negligible. However, when the planet mass is between 10 and 50 M{sub Circled-Plus }, simulations point to a transitional regime with {approx}50 M{sub Circled-Plus} being the value for which the perturbing effect of the planet can no longer be ignored. Simulations also show that further increase of the mass of the planet strongly reduces the efficiency of the scattering of planetesimals from the terrestrial planet region into the asteroid belt. We present the results of our simulations and discuss their possible implications for the time of giant planet formation.

  7. THE HERSCHEL AND JCMT GOULD BELT SURVEYS: CONSTRAINING DUST PROPERTIES IN THE PERSEUS B1 CLUMP WITH PACS, SPIRE, AND SCUBA-2

    SciTech Connect (OSTI)

    Sadavoy, S. I.; Di Francesco, J.; Johnstone, D.; Fallscheer, C.; Matthews, B.; Currie, M. J.; Jenness, T.; Drabek, E.; Hatchell, J.; Nutter, D.; Andre, Ph.; Hennemann, M.; Hill, T.; Koenyves, V.; Benedettini, M.; Bernard, J.-P.; Duarte-Cabral, A.; Friesen, R.; Greaves, J.; Collaboration: JCMT and Herschel Gould Belt Survey teams; and others

    2013-04-20

    We present Herschel observations from the Herschel Gould Belt Survey and SCUBA-2 science verification observations from the JCMT Gould Belt Survey of the B1 clump in the Perseus molecular cloud. We determined the dust emissivity index using four different techniques to combine the Herschel PACS+SPIRE data at 160-500 {mu}m with the SCUBA-2 data at 450 {mu}m and 850 {mu}m. Of our four techniques, we found that the most robust method was filtering out the large-scale emission in the Herschel bands to match the spatial scales recovered by the SCUBA-2 reduction pipeline. Using this method, we find {beta} Almost-Equal-To 2 toward the filament region and moderately dense material and lower {beta} values ({beta} {approx}> 1.6) toward the dense protostellar cores, possibly due to dust grain growth. We find that {beta} and temperature are more robust with the inclusion of the SCUBA-2 data, improving estimates from Herschel data alone by factors of {approx}2 for {beta} and by {approx}40% for temperature. Furthermore, we find core mass differences of {approx}< 30% compared to Herschel-only estimates with an adopted {beta} = 2, highlighting the necessity of long-wavelength submillimeter data for deriving accurate masses of prestellar and protostellar cores.

  8. ELECTRON IRRADIATION OF KUIPER BELT SURFACE ICES: TERNARY N{sub 2}-CH{sub 4}-CO MIXTURES AS A CASE STUDY

    SciTech Connect (OSTI)

    Kim, Y. S.; Kaiser, R. I.

    2012-10-10

    The space weathering of icy Kuiper Belt Objects was investigated in this case study by exposing methane (CH{sub 4}) and carbon monoxide (CO) doped nitrogen (N{sub 2}) ices at 10 K to ionizing radiation in the form of energetic electrons. Online and in situ Fourier transform infrared spectroscopy was utilized to monitor the radiation-induced chemical processing of these ices. Along with isocyanic acid (HNCO), the products could be mainly derived from those formed in irradiated binary ices of the N{sub 2}-CH{sub 4} and CO-CH{sub 4} systems: nitrogen-bearing products were found in the form of hydrogen cyanide (HCN), hydrogen isocyanide (HNC), diazomethane (CH{sub 2}N{sub 2}), and its radical fragment (HCN{sub 2}); oxygen-bearing products were of acetaldehyde (CH{sub 3}CHO), formyl radical (HCO), and formaldehyde (H{sub 2}CO). As in the pure ices, the methyl radical (CH{sub 3}) and ethane (C{sub 2}H{sub 6}) were also detected, as were carbon dioxide (CO{sub 2}) and the azide radical (N{sub 3}). Based on the temporal evolution of the newly formed products, kinetic reaction schemes were then developed to fit the temporal profiles of the newly formed species, resulting in numerical sets of rate constants. The current study highlights important constraints on the preferential formation of isocyanic acid (HNCO) over hydrogen cyanide (HCN) and hydrogen isocyanide (HNC), thus guiding the astrobiological and chemical evolution of those distant bodies.

  9. Corn Belt Power Coop | Open Energy Information

    Open Energy Info (EERE)

    Generation Yes Activity Transmission Yes Activity Buying Transmission Yes Activity Wholesale Marketing Yes Alt Fuel Vehicle Yes Alt Fuel Vehicle2 Yes This article is a stub. You...

  10. Corn Belt Energy Coop- Commercial Energy Efficiency Rebate Program

    Broader source: Energy.gov [DOE]

    A signed application and installation invoice must be received by Wabash Valley Power within 60 days of the installation completion date. View the program web site listed above and the Power Move...

  11. Geologic Setting of the Central Alaskan Hot Springs Belt: Implications...

    Open Energy Info (EERE)

    of the power production scheme at CHS is given. As another approach to the question of sustainability, thisdissertation explores the ways in which external benefits of...

  12. Modeling of the radiation belt megnetosphere in decisional timeframes

    DOE Patents [OSTI]

    Koller, Josef; Reeves, Geoffrey D; Friedel, Reiner H.W.

    2013-04-23

    Systems and methods for calculating L* in the magnetosphere with essentially the same accuracy as with a physics based model at many times the speed by developing a surrogate trained to be a surrogate for the physics-based model. The trained model can then beneficially process input data falling within the training range of the surrogate model. The surrogate model can be a feedforward neural network and the physics-based model can be the TSK03 model. Operatively, the surrogate model can use parameters on which the physics-based model was based, and/or spatial data for the location where L* is to be calculated. Surrogate models should be provided for each of a plurality of pitch angles. Accordingly, a surrogate model having a closed drift shell can be used from the plurality of models. The feedforward neural network can have a plurality of input-layer units, there being at least one input-layer unit for each physics-based model parameter, a plurality of hidden layer units and at least one output unit for the value of L*.

  13. DOE/EIA-0207/2 Residential Energy Consumption Survey:

    Gasoline and Diesel Fuel Update (EIA)

    to keep a log of their fuel purchases and odometer readings for a two-month period. The panel consists of 500 to 1,000 households reporting each month. Separate tabula tions of...

  14. ETATP13AppA.PDF

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    APPENDIX A VEHICLE BATTERY CHARGING CHECKLIST / LOG 13 Page __ of __ DATE TIME CONNECT / DISCONNECT SOC READING VEHICLE ODOMETER BATTERY TEMP. kWh METER READING COMMENTS INITIALS © 1999 E lectric T ransportation A pplications All Rights Reserved

  15. Method and apparatus for setting precise nozzle/belt and nozzle/edge dam block gaps

    DOE Patents [OSTI]

    Carmichael, Robert J. (Colchester, VT); Dykes, Charles D. (Milton, VT); Woodrow, Ronald (Saltsburgh, PA)

    1989-05-16

    A pair of guide pins are mounted on sideplate extensions of the caster and mating roller pairs are mounted on the nozzle assembly. The nozzle is advanced toward the caster so that the roller pairs engage the guide pins. Both guide pins are remotely adjustable in the vertical direction by hydraulic cylinders acting through eccentrics. This moves the nozzle vertically. The guide pin on the inboard side of the caster is similarly horizontally adjustable. The nozzle roller pair which engage the inboard guide pin are flanged so that the nozzle moves horizontally with the inboard guide pin.

  16. Seismic signatures of the Lodgepole fractured reservoir in Utah-Wyoming overthrust belt

    SciTech Connect (OSTI)

    Parra, J.; Collier, H.; Angstman, B.

    1997-08-01

    In low porosity, low permeability zones, natural fractures are the primary source of permeability which affect both production and injection of fluids. The open fractures do not contribute much to porosity, but they provide an increased drainage network to any porosity. An important approach to characterizing the fracture orientation and fracture permeability of reservoir formations is one based upon the effects of such conditions on the propagation of acoustic and seismic waves in the rock. We present the feasibility of using seismic measurement techniques to map the fracture zones between wells spaced 2400 ft at depths of about 1000 ft. For this purpose we constructed computer models (which include azimuthal anisotropy) using Lodgepole reservoir parameters to predict seismic signatures recorded at the borehole scale, crosswell scale, and 3 D seismic scale. We have integrated well logs with existing 2D surfaces seismic to produce petrophysical and geological cross sections to determine the reservoir parameters and geometry for the computer models. In particular, the model responses are used to evaluate if surface seismic and crosswell seismic measurements can capture the anisotropy due to vertical fractures. Preliminary results suggested that seismic waves transmitted between two wells will propagate in carbonate fracture reservoirs, and the signal can be received above the noise level at the distance of 2400 ft. In addition, the large velocities contrast between the main fracture zone and the underlying unfractured Boundary Ridge Member, suggested that borehole reflection imaging may be appropriate to map and fracture zone thickness variation and fracture distributions in the reservoir.

  17. The W40 region in the gould belt: An embedded cluster and H II region at the junction of filaments

    SciTech Connect (OSTI)

    Mallick, K. K.; Ojha, D. K.; Kumar, M. S. N.; Samal, M. R.; Pirogov, L.

    2013-12-20

    We present a multiwavelength study of the W40 star-forming region using infrared (IR) observations in the UKIRT JHK bands, Spitzer Infrared Array Camera bands, and Herschel PACS bands, 2.12 ?m H{sub 2} narrowband imaging, and radio continuum observations from GMRT (610 and 1280 MHz), in a field of view (FoV) of ?34' 40'. Archival Spitzer observations in conjunction with near-IR observations are used to identify 1162 Class II/III and 40 Class I sources in the FoV. The nearest-neighbor stellar surface density analysis shows that the majority of these young stellar objects (YSOs) constitute the embedded cluster centered on the high-mass source IRS 1A South. Some YSOs, predominantly the younger population, are distributed along and trace the filamentary structures at lower stellar surface density. The cluster radius is measured to be 0.44 pcmatching well with the extent of radio emissionwith a peak density of 650 pc{sup 2}. The JHK data are used to map the extinction in the region, which is subsequently used to compute the cloud mass126 M {sub ?} and 71 M {sub ?} for the central cluster and the northern IRS 5 region, respectively. H{sub 2} narrowband imaging shows significant emission, which prominently resembles fluorescent emission arising at the borders of dense regions. Radio continuum analysis shows that this region has a blister morphology, with the radio peak coinciding with a protostellar source. Free-free emission spectral energy distribution analysis is used to obtain physical parameters of the overall photoionized region and the IRS 5 sub-region. This multiwavelength scenario is suggestive of star formation having resulted from the merging of multiple filaments to form a hub. Star formation seems to have taken place in two successive epochs, with the first epoch traced by the central cluster and the high-mass star(s)followed by a second epoch that is spreading into the filaments as uncovered by the Class I sources and even younger protostellar sources along the filaments. The IRS 5 H II region displays indications of swept-up material that has possibly led to the formation of protostars.

  18. Late Cretaceous extension in the hinterland of the Sevier thrust...

    Open Energy Info (EERE)

    Sevier thrust belt, northwestern Utah and southern Idaho Abstract Cover rocks of the Raft River metamorphic core complex, located in the Sevier belt hinterland, preserve a...

  19. Developments in precision casing joint and radioactive bullet measurements for compaction monitoring

    SciTech Connect (OSTI)

    Allen, D.R.

    1981-01-01

    A method has been developed in Wilmington Field, California, for measuring oil zone compaction and expansion by the deformation in well casing. Possible formation compaction is also directly investigated by locating radioactive bullets previously placed in the formation. Random joint lengths, under field conditions, have been repeatedly measured and remeasured with a standard deviation of .0159 ft. (4.8 mm). An alternate system, developed by R.A. Ruedrich et al utilized multiple collar locators and specially milled casing joints. Both systems can be applied to field situations where random joint lengths are found; however, the odometer system should be more reliable under these conditions. 5 refs.

  20. Linear tractor dry coal extrusion pump

    DOE Patents [OSTI]

    Sprouse, Kenneth M.; Matthews, David R.

    2011-10-18

    A pump for transporting particulate material includes an inlet, an outlet, a passageway, a first and second load beam, a first and second scraper seal, and a first and second drive assembly. The inlet introduces the particulate material into the passageway and the outlet expels the particulate material from the passageway. The passageway is defined by a first belt assembly and a second belt assembly that are opposed to each other. The first and second load beams are positioned within the first belt assembly and the second belt assembly, respectively. The first scraper seal and a second scraper seal are positioned proximate the passageway and the outlet. The first drive assembly is positioned within an interior section of the first belt assembly and drives the first belt assembly and the second drive assembly is positioned within an interior section of the second belt assembly and drives the second belt assembly.

  1. Discovery and characteristics of the rapidly rotating active...

    Office of Scientific and Technical Information (OSTI)

    belt We report a new active asteroid in the main belt of asteroids between Mars and Jupiter. Object (62412) 2000 SY178 exhibited a tail in images collected during our survey for...

  2. Linear tractor dry coal extrusion pump

    DOE Patents [OSTI]

    Sprouse, Kenneth M. (Northridge, CA); Matthews, David R. (Simi Valley, CA)

    2008-06-17

    A pump for transporting particulate material includes an inlet, an outlet, a passageway, a first and second load beam, a first and second scraper seal, and a first and second drive assembly. The inlet introduces the particulate material into the passageway and the outlet expels the particulate material from the passageway. The passageway is defined by a first belt assembly and a second belt assembly that are opposed to each other. The first and second load beams are positioned within the first belt assembly and the second belt assembly, respectively. The first scraper seal and a second scraper seal are positioned proximate the passageway and the outlet. The first drive assembly is positioned within an interior section of the first belt assembly and drives the first belt assembly and the second drive assembly is positioned within an interior section of the second belt assembly and drives the second belt assembly.

  3. DOE-0346

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    ... Body Belt (safety belt): A strap with means both for securing it about the waist and for ... forces over at least the thighs, pelvis, waist, chest and shoulders with means for ...

  4. Effects of Mid-Level Ethanol Blends on Conventional Vehicle Emissions

    SciTech Connect (OSTI)

    Knoll, K.; West, B.; Huff, S.; Thomas, J.; Orban, J.; Cooper, C.

    2010-06-01

    Tests were conducted in 2008 on 16 late-model conventional vehicles (1999-2007) to determine short-term effects of mid-level ethanol blends on performance and emissions. Vehicle odometer readings ranged from 10,000 to 100,000 miles, and all vehicles conformed to federal emissions requirements for their federal certification level. The LA92 drive cycle, also known as the Unified Cycle, was used for testing because it more accurately represents real-world acceleration rates and speeds than the Federal Test Procedure. Test fuels were splash-blends of up to 20 volume percent ethanol with federal certification gasoline. Both regulated and unregulated air-toxic emissions were measured. For the 16-vehicle fleet, increasing ethanol content resulted in reductions in average composite emissions of both nonmethane hydrocarbons and carbon monoxide and increases in average emissions of ethanol and aldehydes.

  5. Los Humeros Geothermal Area | Open Energy Information

    Open Energy Info (EERE)

    (0) 10 References Area Overview Geothermal Area Profile Location: Chignautla, Puebla, Mexico Exploration Region: Transmexican Volcanic Belt GEA Development Phase:...

  6. BLACKLEAF CANYON TWO MEDICINE CREEK POTSHOT PROSPECT GLACIER E

    Gasoline and Diesel Fuel Update (EIA)

    Gas Reserve Class No 2001 gas reserves Basin Outline WY UT ID CO MT WA OR NV CANADA INDEX MAP ID Total Total Total Number Liquid Gas BOE of Reserves Reserves Reserves Fields (Mbbl) (MMcf) (Mbbl) Montana Thrust Belt 1 1 0 1 Basin 2001 Reserve Summary for Montana Thrust Belt Fields CANADA USA Montana Thrust Belt Oil & Gas Fields By 2001 Gas

  7. Heating, Ventilation and Air Conditioning Efficiency

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    ... A major N.C. Manufacturer Tested 2-17 Months (yr 1985) .052KWH (.13 EP) 2700 HoursYear 15 HP COGGED BELT 10.67 STANDARD BELT 3.33 PREMIUM BELT 7.34 BRAND A 4.4% BRAND B ...

  8. Van Allen probes pinpoint driver of speeding electrons

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Van Allen probes pinpoint driver of speeding electrons Van Allen probes pinpoint driver of speeding electrons Los Alamos researchers believe they have solved a lingering mystery about how electrons within Earth's radiation belt can suddenly become energetic enough to kill orbiting satellites. July 25, 2013 Artist's rendering of mechanism within Van Allen radiation belts An artist's rendering of a mechanism within the Van Allen radiation belts that can accelerate electrons to satellite-killing

  9. BLACKLEAF CANYON TWO MEDICINE CREEK POTSHOT PROSPECT GLACIER E

    Gasoline and Diesel Fuel Update (EIA)

    BOE Reserve Class No 2001 Reserves 0.1 - 10 MBOE Basin Outline WY UT ID CO MT WA OR NV CANADA INDEX MAP ID Total Total Total Number Liquid Gas BOE of Reserves Reserves Reserves Fields (Mbbl) (MMcf) (Mbbl) Montana Thrust Belt 1 1 0 1 Basin 2001 Reserve Summary for Montana Thrust Belt Fields CANADA USA Montana Thrust Belt Oil & Gas Fields By 2001 BOE

  10. BLACKLEAF CANYON TWO MEDICINE CREEK POTSHOT PROSPECT GLACIER E

    Gasoline and Diesel Fuel Update (EIA)

    Liquids Reserve Class No 2001 liquids reserves 0.1 - 10 Mbbl Basin Outline WY UT ID CO MT WA OR NV CANADA INDEX MAP ID Total Total Total Number Liquid Gas BOE of Reserves Reserves Reserves Fields (Mbbl) (MMcf) (Mbbl) Montana Thrust Belt 1 1 0 1 Basin 2001 Reserve Summary for Montana Thrust Belt Fields CANADA USA Montana Thrust Belt Oil & Gas Fields By 2001 Liquids

  11. Earth's Magnetosphere

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Mysterious electron stash found hidden among Van Allen belts March 1, 2013 Instruments detect never-before-seen phenomenon in Earth's Magnetosphere LOS ALAMOS, N.M., March 1, 2013-U.S. researchers, including a trio from Los Alamos National Laboratory, have witnessed the mysterious appearance of a relatively long-lived zone of high-energy electrons stored between Earth's Van Allen radiation belts. The surprising findings, discovered by NASA's Van Allen Probes (formerly known as the Radiation Belt

  12. Uranium Leasing Program | Department of Energy

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    » Uranium Leasing Program Uranium Leasing Program Abandoned Mine Reclamation, Uravan Mineral Belt, Colorado Abandoned Mine Reclamation, Uravan Mineral Belt, Colorado LM currently manages the Uranium Leasing Program and continues to administer 31 lease tracts, all located within the Uravan Mineral Belt in southwestern Colorado. Twenty-nine of these lease tracts are actively held under lease and two tracts have been placed in inactive status indefinitely. Administrative duties include ongoing

  13. Building Efficiency Technologies by Tomorrow's Engineers and...

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Heat Exchangers, AL - Advanced Renewable Energy - Emrgy Hydro - Atlanta, GA - Fox Theater - Atlanta, GA - Atlanta BeltLine - Atlanta, GA - Ford - Atlanta, GA - SawHorse - ...

  14. File:EIA-MTB-GAS.pdf | Open Energy Information

    Open Energy Info (EERE)

    applicationpdf) Description Montana Thrust Belt By 2001 Gas Reserve Class Sources Energy Information Administration Authors Samuel H. Limerick; Lucy Luo; Gary Long; David F....

  15. File:EIA-WTB-GAS.pdf | Open Energy Information

    Open Energy Info (EERE)

    applicationpdf) Description Wyoming Thrust Belt By 2001 Gas Reserve Class Sources Energy Information Administration Authors Samuel H. Limerick; Lucy Luo; Gary Long; David F....

  16. DOE Zero Energy Ready Home Case Study: M Street Homes, Houston...

    Energy Savers [EERE]

    powered by a small efficient natural gas generator that produces electricity with photovoltaic and battery backup. The generator's belt also mechanically drives the compressor...

  17. summer school flyer.indd

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    The summer school includes a wide range of topics such as: * Ring current and radiation belts * Magnetosphere-ionosphere coupling * Solar wind dynamics * Spacecraft charging *...

  18. Improved Manufacturing Processes Save Company One Billion Dollars...

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    to the filling machines, which then inject empty bottles with the detergent. Conveyor belts whisk the full bottles to capping machines and then to labelers, cartoners, and the...

  19. Discovery and characteristics of the rapidly rotating active asteroid

    Office of Scientific and Technical Information (OSTI)

    (62412) 2000 SY178 in the main belt (Journal Article) | SciTech Connect Journal Article: Discovery and characteristics of the rapidly rotating active asteroid (62412) 2000 SY178 in the main belt Citation Details In-Document Search Title: Discovery and characteristics of the rapidly rotating active asteroid (62412) 2000 SY178 in the main belt We report a new active asteroid in the main belt of asteroids between Mars and Jupiter. Object (62412) 2000 SY178 exhibited a tail in images collected

  20. TRU TeamWorks - a biweekly e-newsletter for the Waste Isolation...

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    WIPP security officers with Santa Fe Protective Services (SFPS) Inc. will soon add guns to their security belts. Many employees remember the early days at WIPP when security...

  1. Los Azufres Geothermal Plant | Open Energy Information

    Open Energy Info (EERE)

    Volcanic Belt Plant Information Facility Type Single Flash, Binary, Back Pressure Energy Purchaser Comisin Federal de Electricidad Commercial Online Date 1982 Power Plant...

  2. Los Azufres II Geothermal Power Plant | Open Energy Information

    Open Energy Info (EERE)

    Transmexican Volcanic Belt Plant Information Facility Type Single Flash Developer Alstom Energy Purchaser Comisin Federal de Electricidad Commercial Online Date 2003 Power Plant...

  3. Sandia National Laboratories: Latest News

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Array (Nomination) * MESA Project Sandia Green Building Awards Sandia Corporate Lean Six Sigma Awards 2008 * Champion of the Year - Dale L. Hetherington * Black Belt of...

  4. Why Is Nevada in Hot Water? Structural Controls and Tectonic...

    Open Energy Info (EERE)

    Walker Lane, diffusing that motion into the Basin-Range. Abundant geothermal fields cluster in several northeasttrending belts in the northern Great Basin (e.g. Humboldt...

  5. Vibrant Solar Inc | Open Energy Information

    Open Energy Info (EERE)

    installs and commissions PV systems for businesses and home. With hundreds of installations under our belt, our designers and installers are among the best in the business....

  6. A Natural History | U.S. DOE Office of Science (SC)

    Office of Science (SC) Website

    when the U.S. Atomic Energy Commission selected it in 1955 for its new headquarters. ... tree swallows, great blue herons, green herons, belted kingfishers, and eastern kingbirds. ...

  7. ARM - Publications: Science Team Meeting Documents

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Measurement (ARM) Science Team Meeting The Arctic plays a major role in global climate change and has considerable influence on the middle latitude belt. The Arctic affects the...

  8. Method and apparatus for scientific analysis under low temperature vacuum conditions

    DOE Patents [OSTI]

    Winefordner, James D. (Gainesville, FL); Jones, Bradley T. (Gainesville, FL)

    1990-01-01

    A method and apparatus for scientific analysis of a sample under low temperature vacuum conditions uses a vacuum chamber with a conveyor belt disposed therein. One end of the conveyor belt is a cool end in thermal contact with the cold stage of a refrigerator, whereas the other end of the conveyor belt is a warm end spaced from the refrigerator. A septum allows injection of a sample into the vacuum chamber on top of the conveyor belt for spectroscopic or other analysis. The sample freezes on the conveyor belt at the cold end. One or more windows in the vacuum chamber housing allow spectroscopic analysis of the sample. Following the spectroscopic analysis, the conveyor belt may be moved such that the sample moves toward the warm end of the conveyor belt where upon it evaporates, thereby cleaning the conveyor belt. Instead of injecting the sample by way of a septum and use of a syringe and needle, the present device may be used in series with capillary-column gas chromatography or micro-bore high performance liquid chromatography.

  9. Analysis of Casualty Risk per Police-Reported Crash for Model Year 2000 to 2004 Vehicles, using Crash Data from Five States

    SciTech Connect (OSTI)

    Wenzel, Tom

    2011-03-20

    In this report we compare two measures of driver risks: fatality risk per vehicle registration-year, and casualty (fatality plus serious injury) risk per police-reported crash. Our analysis is based on three sets of data from five states (Florida, Illinois, Maryland, Missouri, and Pennsylvania): data on all police-reported crashes involving model year 2000 to 2004 vehicles; 2005 county-level vehicle registration data by vehicle model year and make/model; and odometer readings from vehicle emission inspection and maintenance (I/M) programs conducted in urban areas of four of the five states (Florida does not have an I/M program). The two measures of risk could differ for three reasons: casualty risks are different from fatality risk; risks per vehicle registration-year are different from risks per crash; and risks estimated from national data are different from risks from the five states analyzed here. We also examined the effect of driver behavior, crash location, and general vehicle design on risk, as well as sources of potential bias in using the crash data from five states.

  10. Multi-port valve assembly

    DOE Patents [OSTI]

    Guggenheim, S. Frederic

    1986-01-01

    A multi-port fluid valve apparatus is used to control the flow of fluids through a plurality of valves and includes a web, which preferably is a stainless steel endless belt. The belt has an aperture therethrough and is progressed, under motor drive and control, so that its aperture is moved from one valve mechanism to another. Each of the valve mechanisms comprises a pair of valve blocks which are held in fluid-tight relationship against the belt. Each valve block consists of a block having a bore through which the fluid flows, a first seal surrounding the bore and a second seal surrounding the first seal, with the distance between the first and second seals being greater than the size of the belt aperture. In order to open a valve, the motor progresses the belt aperture to where it is aligned with the two bores of a pair of valve blocks, such alignment permitting a flow of the fluid through the valve. The valve is closed by movement of the belt aperture and its replacement, within the pair of valve blocks, by a solid portion of the belt.

  11. Coal-feeding mechanism for a fluidized bed combustion chamber

    DOE Patents [OSTI]

    Gall, Robert L. (Morgantown, WV)

    1981-01-01

    The present invention is directed to a fuel-feeding mechanism for a fluidized bed combustor. In accordance with the present invention a perforated conveyor belt is utilized in place of the fixed grid normally disposed at the lower end of the fluidized bed combustion zone. The conveyor belt is fed with fuel, e.g. coal, at one end thereof so that the air passing through the perforations dislodges the coal from the belt and feeds the coal into the fluidized zone in a substantially uniform manner.

  12. Personal continuous air monitor

    DOE Patents [OSTI]

    Morgan, Ronald G.; Salazar, Samuel A.

    2000-01-01

    A personal continuous air monitor capable of giving immediate warning of the presence of radioactivity has a filter/detector head to be worn in the breathing zone of a user, containing a filter mounted adjacent to radiation detectors, and a preamplifier. The filter/detector head is connected to a belt pack to be worn at the waist or on the back of a user. The belt pack contains a signal processor, batteries, a multichannel analyzer, a logic circuit, and an alarm. An air pump also is provided in the belt pack for pulling air through the filter/detector head by way of an air tube.

  13. Geothermal Studies Scholarship Recipients | Department of Energy

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Through his research, Brink-Roby attempts to answer questions about the origin of these fluids, where fluid flow occurred within the mountain belt, and how long fluid conduits ...

  14. CX-007857: Categorical Exclusion Determination

    Office of Energy Efficiency and Renewable Energy (EERE)

    Development and Endurance Testing of SLH Timing Belt Powertrain in Hydraulic Laboratory Environment CX(s) Applied: A9, B3.6 Date: 01/26/2012 Location(s): Massachusetts Offices(s): Golden Field Office

  15. PRB Coal Users' Group enjoys growing interest in its concerns

    SciTech Connect (OSTI)

    Rahm, R.

    2008-07-15

    A review is given of some of the topics discussed at the PRB Coal Users' Group annual meeting, including combustion dusts and a new session on conveyor belts. 7 figs.

  16. The Surprising Appearance of Nanotubular Fullerene D5h(1)-C90

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    and physical properties of a distinctly cylindrical fullerene. The armchair-style belts that are found at the waist of D5h(1)-C90 are a unique feature of this particular...

  17. Waveguide gas laser

    SciTech Connect (OSTI)

    Zedong, C.

    1982-05-01

    Waveguide gas lasers are described. Transmission loss of hollow tube light waveguides, coupling loss, the calculation of output power, and the width of the oscillation belt are discussed. The structure of a waveguide CO/sub 2/ laser is described.

  18. Hancock County Wind Farm | Open Energy Information

    Open Energy Info (EERE)

    (44 MW); rest purchased by Corn Belt Cooperative and Cedar Falls Location Hancock County IA Coordinates 43.066524, -93.70481 Show Map Loading map... "minzoom":false,"mappingse...

  19. New Opportunities for Outer Solar System Science using Radioisotope...

    Office of Scientific and Technical Information (OSTI)

    the trans-Neptunian objects (TNO), and distant Kuiper Belt objects (KBO) hold a wealth of information about the primordial conditions that led to the formation of our Solar System. ...

  20. CX-004406: Categorical Exclusion Determination

    Broader source: Energy.gov [DOE]

    ArmorBelt Single Point Gas Lift System for Stripper WellsCX(s) Applied: B3.6Date: 11/08/2010Location(s): Chickasha, OklahomaOffice(s): Fossil Energy, National Energy Technology Laboratory

  1. CX-012236: Categorical Exclusion Determination

    Office of Energy Efficiency and Renewable Energy (EERE)

    TechBelt Energy Innovation Center CX(s) Applied: A9, B5.18 Date: 06/27/2014 Location(s): Ohio Offices(s): Golden Field Office

  2. Bulk materials handling equipment roundup

    SciTech Connect (OSTI)

    Fiscor, S.

    2007-07-15

    The article reports recent product developments in belt conveyors. Flexco Steel Lancing Co. (Flexco) has a range of light, portable maintenance tools and offers training modules on procedures for belt conveyor maintenance on its website www.flexcosafe.com. Siemens recently fitted a 19 km long conveyor belt drive system at a Texan aluminium plant with five 556-kW Simovent Masterdrive VC drives. Voith recently launched the TPKL-T turbo coupling for users who want an alignment-free drive solution. Belt cleaners newly on the market include the RemaClean SGB brush and ASGCO Manufacturing's Razor-Back with Spray bar. Continental Conveyor has introduced a new line of dead-shaft pulleys offering increased bearing protection. 6 photos.

  3. CX-004405: Categorical Exclusion Determination

    Office of Energy Efficiency and Renewable Energy (EERE)

    ArmorBelt Single Point Gas Lift System for Stripper WellsCX(s) Applied: A1, A9, A11Date: 11/08/2010Location(s): Hastings, MinnesotaOffice(s): Fossil Energy, National Energy Technology Laboratory

  4. CX-004404: Categorical Exclusion Determination

    Office of Energy Efficiency and Renewable Energy (EERE)

    ArmorBelt Single Point Gas Lift System for Stripper WellsCX(s) Applied: B3.6Date: 11/08/2010Location(s): Cadillac, MichiganOffice(s): Fossil Energy, National Energy Technology Laboratory

  5. Tax Credits, Rebates & Savings | Department of Energy

    Broader source: Energy.gov (indexed) [DOE]

    customers of Corn Belt Energy can receive rebates for geothermal, air-source, and dual fuel heat pumps, as well as electric and heat pump water heaters. To qualify for a...

  6. Presentation title: This can be up to 2 lines

    Gasoline and Diesel Fuel Update (EIA)

    ... 2009 2010 2011 2012 2013 Year of Annual Energy Outlook Unproved Alaska (1) Unproved L48 ... 2,303 Denver Niobrara 1,444 599 Greater Green River 103 Montana Thrust Belt 602 652 ...

  7. The Surprising Appearance of Nanotubular Fullerene D5h(1)-C90

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    ... The armchair-style belts that are found at the waist of D5h(1)-C90 are a unique feature of this particular fullerene, but are the fundamental building block of carbon nanotubes. ...

  8. WCAP-10574

    Office of Legacy Management (LM)

    ... 0 Radiation surveys 0 Evaluation of body badge data Body badges were normally worn between the waist and shoulders, near the most radiosensitive organs, but never on the belt. ...

  9. Regional Gravity Survey of the Northern Great Salt Lake Desert...

    Open Energy Info (EERE)

    of about -196 mgal over the alluvium-covered graben areas. The gravity high over the Raft River Mountains apparently corresponds with the Raft River Mountains anticline. A belt...

  10. 1

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Allen probes pinpoint driver of speeding electrons July 25, 2013 Research team solves decades-old mystery that threatens satellites LOS ALAMOS, N.M., July 25, 2013 - Researchers believe they have solved a lingering mystery about how electrons within Earth's radiation belt can suddenly become energetic enough to kill orbiting satellites. Thanks to data gathered from an intrepid pair of NASA probes roaming the harsh space environment within the Van Allen radiation belts, scientists have identified

  11. DREAM tool increases space weather predictions

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    DREAM tool increases space weather predictions DREAM tool increases space weather predictions Model addresses radiation hazards of the space environment on space systems. April 13, 2012 Scientists studying Earth's radiation belts have a new modeling tool called Dynamic Radiation Environment Assimilation Model (DREAM). Scientists studying Earth's radiation belts have a new modeling tool called Dynamic Radiation Environment Assimilation Model (DREAM). DREAM is a modeling tool that improves the

  12. Interface for liquid chromatograph-mass spectrometer

    DOE Patents [OSTI]

    Andresen, Brian D. (Pleasanton, CA); Fought, Eric R. (Livermore, CA)

    1989-01-01

    A moving belt interface for real-time, high-performance liquid chromatograph (HPLC)/mass spectrometer (MS) analysis which strips away the HPLC solvent as it emerges from the end of the HPLC column and leaves a residue suitable for mass-spectral analysis. The interface includes a portable, stand-alone apparatus having a plural stage vacuum station, a continuous ribbon or belt, a drive train magnetically coupled to an external drive motor, a calibrated HPLC delivery system, a heated probe tip and means located adjacent the probe tip for direct ionization of the residue on the belt. The interface is also capable of being readily adapted to fit any mass spectrometer.

  13. Reduced vibration motor winding arrangement

    DOE Patents [OSTI]

    Slavik, Charles J. (Rexford, NY); Rhudy, Ralph G. (Scotia, NY); Bushman, Ralph E. (Lathem, NY)

    1997-01-01

    An individual phase winding arrangement having a sixty electrical degree phase belt width for use with a three phase motor armature includes a delta connected phase winding portion and a wye connected phase winding portion. Both the delta and wye connected phase winding portions have a thirty electrical degree phase belt width. The delta and wye connected phase winding portions are each formed from a preselected number of individual coils each formed, in turn, from an unequal number of electrical conductor turns in the approximate ratio of .sqroot.3. The individual coils of the delta and wye connected phase winding portions may either be connected in series or parallel. This arrangement provides an armature winding for a three phase motor which retains the benefits of the widely known and utilized thirty degree phase belt concept, including improved mmf waveform and fundamental distribution factor, with consequent reduced vibrations and improved efficiency.

  14. Reduced vibration motor winding arrangement

    DOE Patents [OSTI]

    Slavik, C.J.; Rhudy, R.G.; Bushman, R.E.

    1997-11-11

    An individual phase winding arrangement having a sixty electrical degree phase belt width for use with a three phase motor armature includes a delta connected phase winding portion and a wye connected phase winding portion. Both the delta and wye connected phase winding portions have a thirty electrical degree phase belt width. The delta and wye connected phase winding portions are each formed from a preselected number of individual coils each formed, in turn, from an unequal number of electrical conductor turns in the approximate ratio of {radical}3. The individual coils of the delta and wye connected phase winding portions may either be connected in series or parallel. This arrangement provides an armature winding for a three phase motor which retains the benefits of the widely known and utilized thirty degree phase belt concept, including improved mmf waveform and fundamental distribution factor, with consequent reduced vibrations and improved efficiency. 4 figs.

  15. Solimoes megashear: Intraplate tectonics in northwestern Brazil

    SciTech Connect (OSTI)

    Caputo, M.V. )

    1991-03-01

    A belt of deformation in the Solimoes basin of northwestern Brazil extends east-northeast from near the Peruvian border for about 1300 km. The belt is characterized by the en echelon arrangement of folds and faults interpreted as the result of right-slip displacements in a transpressive regime. The structures were formed during Late Jurassic time, probably due to collision of South America with allochthonous terranes as the opening of the South Atlantic Ocean began. The Iquitos arch near the western end of the megashear separates the Solimoes basin from Subandean basins. The development of the Iquitos arch is interpreted to be related to orogenic loading along western South America by the Andean mountain belt. In Brazil, folds and faults associated with the Solimoes megashear hold hydrocarbons within Paleozoic strata, and 15 gas and oil fields have so far been discovered.

  16. Interface for liquid chromatograph-mass spectrometer

    DOE Patents [OSTI]

    Andresen, B.D.; Fought, E.R.

    1989-09-19

    A moving belt interface is described for real-time, high-performance liquid chromatograph (HPLC)/mass spectrometer (MS) analysis which strips away the HPLC solvent as it emerges from the end of the HPLC column and leaves a residue suitable for mass-spectral analysis. The interface includes a portable, stand-alone apparatus having a plural stage vacuum station, a continuous ribbon or belt, a drive train magnetically coupled to an external drive motor, a calibrated HPLC delivery system, a heated probe tip and means located adjacent the probe tip for direct ionization of the residue on the belt. The interface is also capable of being readily adapted to fit any mass spectrometer. 8 figs.

  17. 1

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    surprising variability in shape of Van Allen Belts February 23, 2016 Findings could impact how we protect technology in space LOS ALAMOS, N.M., Feb. 23, 2016-The shape of the two electron swarms 600 miles to more than 25,000 miles from the Earth's surface, known as the Van Allen Belts, could be quite different than has been believed for decades, according to a new study of data from NASA's Van Allen Probes that was released Friday in the Journal of Geophysical Research. "The shape of the

  18. Phase IV - Resource Production and Power Plant Construction ...

    Open Energy Info (EERE)

    Expansion 25 MW25,000 kW 25,000,000 W 25,000,000,000 mW 0.025 GW 2.5e-5 TW Chignautla, Puebla, Mexico Los Humeros Geothermal Area Transmexican Volcanic Belt 19 December 2013...

  19. The Wallula fault and tectonic framework of south-central Washington, as interpreted from magnetic and gravity anomalies

    SciTech Connect (OSTI)

    Blakely, Richard J.; Sherrod, Brian; Weaver, Craig; Wells, Ray E.; Rohay, Alan C.

    2014-06-11

    Magnetic and gravity data, collected in south-central Washington near the Yakima Fold and Thrust Belt (YFTB) are used to model upper crustal structure, the extent of the late Columbia River Basalt flow named the Ice Harbor member, the vertical conduits (dikes) that the Ice Harbor erupted from, and whether the dikes are offset or affected by faulting on the Wallula Fault zone.

  20. Development of dense-phase pneumatic transport of coal

    SciTech Connect (OSTI)

    Horisaka, S.; Ikemiya, H.; Kajiwara, T.

    1996-12-31

    Dense phase pneumatic transport system has been developed to reduce entrained particles as is seen in the belt conveyor system. High mass flow rate and dense phase (Loading ratio = 50--100kg-coal/kg-N{sub 2}) transport has been achieved by applying this plug flow system to pneumatic conveying of coal (Average particle diameter = 2.5 mm).

  1. Conveyor with rotary airlock apparatus

    DOE Patents [OSTI]

    Kronbert, J.W.

    1993-01-01

    This invention is comprised of an apparatus for transferring objects from a first region to a second region, the first and second regions having differing atmospheric environments. The apparatus includes a shell having an entrance and an exit, a conveyer belt running through the shell from the entrance to the exit, and a horizontally mounted `revolving door` with at least four vanes revolving about its axis. The inner surface of the shell and the top surface of the conveyer belt act as opposing walls of the `revolving door`. The conveyer belt dips as it passes under but against the revolving vanes so as not to interfere with them but to engage at least two of the vanes and define thereby a moving chamber. Preferably, the conveyer belt has ridges or grooves on its surface that engage the edges of the vanes and act to rotate the vane assembly. Conduits are provided that communicate with the interior of the shell and allow the adjustment of the atmosphere of the moving chamber or recovery of constituents of the atmosphere of the first region from the moving chamber before they escape to the second region.

  2. Low-temperature magnetic refrigerator

    DOE Patents [OSTI]

    Barclay, J.A.

    1983-05-26

    The invention relates to magnetic refrigeration and more particularly to low temperature refrigeration between about 4 and about 20 K, with an apparatus and method utilizing a belt of magnetic material passed in and out of a magnetic field with heat exchangers within and outside the field operably disposed to accomplish refrigeration.

  3. Climate Science: Tropical Expansion by Ocean Swing

    SciTech Connect (OSTI)

    Lu, Jian

    2014-04-01

    The tropical belt has become wider over the past decades, but climate models fall short of capturing the full rate of the expansion. The latest analysis of the climate simulations suggests that a long-term swing of the Pacific Decadal Oscillation is the main missing cause.

  4. CX-005274: Categorical Exclusion Determination

    Broader source: Energy.gov [DOE]

    TechBelt Energy Innovation CenterCX(s) Applied: A1, A9, A11, B3.6Date: 02/18/2011Location(s): Youngstown, OhioOffice(s): Energy Efficiency and Renewable Energy, National Energy Technology Laboratory

  5. Types and causes of haulage-system delays out by the face in US underground coal mines. Final report. [Data from 5 mines

    SciTech Connect (OSTI)

    Douglas, W.J.; Kiefer, J.A.; Kohler, J.L.

    1982-04-01

    This report summarizes the results of a study to characterize and quantify the occurrence and impact of outby haulage delays on production in US underground coal mines. An instrumentation system employing digital data loggers was used to acquire data for over 500 belt shifts in six mines. Observers collected section production data and section delay data to supplement the haulage database. A statistical data reduction system was applied to develop statistics on failure rates and delay lengths. A production impact model was developed and applied to analyze the effect of reducing delays and implementing engineering changes to the haulage systems. Analytical investigations of the relationship between delays and mine characteristics were conducted, and the impact of feeder-breakers and bunkerage, and the addition of longwall units to existing mines was investigated. The study provides a quantitative information base on underground belt haulage delays for use by mining companies and mining researchers.

  6. A Summary of Fault Recurrence and Strain Rates in the Vicinity of the Hanford Site--Topical Report

    SciTech Connect (OSTI)

    Bjornstad, Bruce N.; Winsor, Kelsey; Unwin, Stephen D.

    2012-08-01

    This document is one in a series of topical reports compiled by the Pacific Northwest National Laboratory to summarize technical information on selected topics important to the performance of a probabilistic seismic hazard analysis of the Hanford Site. The purpose of this report is to summarize available data and analyses relevant to fault recurrence and strain rates within the Yakima Fold Belt. Strain rates have met with contention in the expert community and may have a significant potential for impact on the seismic hazard estimate at the Hanford Site. This report identifies the alternative conceptual models relevant to this technical issue and the arguments and data that support those models. It provides a brief description of the technical issue and principal uncertainties; a general overview on the nature of the technical issue, along with alternative conceptual models, supporting arguments and information, and uncertainties; and finally, suggests some prospective approaches to reducing uncertainties about earthquake recurrence rates for the Yakima Fold Belt.

  7. Rotary electrical contact device and method for providing current to and/or from a rotating member

    DOE Patents [OSTI]

    Koplow, Jeffrey P

    2013-11-19

    Examples of rotary electrical connectors include a first pair and a second pair of opposing sheaves coupled together by intersecting first shaft connecting the first pair of opposing sheaves and a second shaft connecting the second pair of opposing sheaves, and at least partially electrically conductive belt disposed about respective perimeters of the first pair and second pair of opposing sheaves and adapted to remain in contact with at least a portion of the respective perimeters of the sheaves during motion of said sheaves. In example devices, one of the plurality of sheaves may remain stationary during operation of the device while the remaining sheaves rotate and/or orbit around a center axis of the stationary sheave, the device being configured to couple current between a stationary power source and a rotating member through the electrically conductive belt.

  8. Screw-fed pump system

    DOE Patents [OSTI]

    Sprouse, Kenneth M

    2014-11-25

    A pump system includes a pump that includes a first belt and a second belt that are spaced apart from each other to provide generally straight sides of a passage there between. There is an inlet at one end of the passage and an outlet at an opposite end of the passage, with a passage length that extends between the inlet and the outlet. The passage defines a gap distance in a width direction between the straight sides at the passage inlet. A hopper includes an interior space that terminates at a mouth at the passage inlet. At least one screw is located within the interior space of the hopper and includes a screw diameter in the width direction that is less than or equal to the gap distance.

  9. Project:Modeling Relativistic Electrons from Nuclear Explosions in the Magnetosphere

    SciTech Connect (OSTI)

    Cowee, Misa; Gary, S. Peter; Winske, Dan; Liu, Kaijun

    2012-07-17

    We present a summary of the FY12 activities for DTRA-funded project 'Modeling Relativistic Electrons from Nuclear Explosions in the Magnetosphere'. We briefly review the outstanding scientific questions and discuss the work done in the last year to try to answer these questions. We then discuss the agenda for this Technical Meeting with the DTRA sponsors. In the last year, we have continued our efforts to understand artificial radiation belts from several different perspectives: (1) Continued development of Electron Source Model (ESM) and comparison to HANE test data; (2) Continued studies of relativistic electron scattering by waves in the natural radiation belts; (3) Began study of self-generated waves from the HANE electrons; and (4) Began modeling for the UCLA laser experiment.

  10. Continuous process electrorefiner

    DOE Patents [OSTI]

    Herceg, Joseph E. (Naperville, IL); Saiveau, James G. (Hickory Hills, IL); Krajtl, Lubomir (Woodridge, IL)

    2006-08-29

    A new device is provided for the electrorefining of uranium in spent metallic nuclear fuels by the separation of unreacted zirconium, noble metal fission products, transuranic elements, and uranium from spent fuel rods. The process comprises an electrorefiner cell. The cell includes a drum-shaped cathode horizontally immersed about half-way into an electrolyte salt bath. A conveyor belt comprising segmented perforated metal plates transports spent fuel into the salt bath. The anode comprises the conveyor belt, the containment vessel, and the spent fuel. Uranium and transuranic elements such as plutonium (Pu) are oxidized at the anode, and, subsequently, the uranium is reduced to uranium metal at the cathode. A mechanical cutter above the surface of the salt bath removes the deposited uranium metal from the cathode.

  11. Automatic detection of bone fragments in poultry using multi-energy x-rays

    DOE Patents [OSTI]

    Gleason, Shaun S. (Knoxville, TN); Paulus, Michael J. (Knoxville, TN); Mullens, James A. (Knoxville, TN)

    2002-04-09

    At least two linear arrays of x-ray detectors are placed below a conveyor belt in a poultry processing plant. Multiple-energy x-ray sources illuminate the poultry and are detected by the detectors. Laser profilometry is used to measure the poultry thickness as the x-ray data is acquired. The detector readout is processed in real time to detect the presence of small highly attenuating fragments in the poultry, i.e., bone, metal, and cartilage.

  12. Sandvik sharpens in-pit crushing focus

    SciTech Connect (OSTI)

    Casteel, K.

    2009-04-15

    Major mining equipment supplier Sandvik Mining and Construction has announced a full-fledged fully mobile crushing plant, the PF300. This is shaping up to be the decade's major addition to the large scale open-cut mining toolkit. The PF300 can be connected to a face conveyor by a loading bridge as well as by belt wagon or transfer conveyor. The article describes design features. 2 figs.

  13. Motor Energy Conservation Measures

    Energy Science and Technology Software Center (OSTI)

    2010-12-31

    This software requires inputs of simple motor inventory information and calculates the energy and cost benefits of various retrofit opportunities. This tool includes energy conservation measures for: High Efficiency Motor retrofit and Cogged V-belts retrofit. This tool calculates energy savings, demand reduction, cost savings, and building life cycle costs including: simple payback, discounted payback, net-present value, and savings to investment ratio. In addition this tool also displays the environmental benefits of a project.

  14. Mesozoic and Cenozoic structural geology of the CP Hills, Nevada Test Site, Nye County, Nevada; and regional implications

    SciTech Connect (OSTI)

    Caskey, S.J.

    1991-08-01

    Detailed mapping and structural analysis of upper Proterozoic and Paleozoic rocks in the CP Hills of the Nevada Test Site, together with analysis of published maps and cross sections and a reconnaissance of regional structural relations indicate that the CP thrust of Barnes and Poole (1968) actually comprises two separate, oppositely verging Mesozoic thrust systems: (1) the west-vergent CP thrust which is well exposed in the CP Hills and at Mine Mountain, and (2) the east-vergent Belted Range thrust located northwest of Yucca Flat. West-vergence of the CP thrust is indicated by large scale west-vergent recumbent folds in both its hangingwall and footwall and by the fact that the CP thrust ramps up section through hangingwall strata toward the northwest. Regional structural relations indicate that the CP thrust forms part of a narrow sigmoidal belt of west-vergent folding and thrusting traceable for over 180 km along strike. The Belted Range thrust represents earlier Mesozoic deformation that was probably related to the Last Chance thrust system in southeastern California, as suggested by earlier workers. A pre-Tertiary reconstruction of the Cordilleran fold and thrust belt in the region between the NTS and the Las Vegas Range bears a close resemblance to other regions of the Cordillera and has important implications for the development of hinterland-vergent deformation as well as for the probable magnitude of Tertiary extension north of Las Vegas Valley. Subsequent to Mesozoic deformation, the CP Hills were disrupted by at least two episodes of Tertiary extensional deformation: (1) an earlier episode represented by pre-middle Miocene low-angle normal faults, and (2) a later, post-11 Ma episode of high-angle normal faulting. Both episodes of extension were related to regional deformation, the latter of which has resulted in the present basin and range topography of the NTS region.

  15. Observations and simulations improve space weather models

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Observations improve space weather models Observations and simulations improve space weather models Researchers used data from the Van Allen Probes to improve a three-dimensional model created by Los Alamos scientists called DREAM3D. June 25, 2014 NASA's Van Allen Probes sample the Earth's magnetosphere. NASA's Van Allen Probes sample the Earth's magnetosphere. The work demonstrated that DREAM3D accurately simulated the behavior of a complex and dynamic event in the radiation belt that was

  16. Integrated rig for the production of boron nitride nanotubes via the pressurized vapor-condenser method

    DOE Patents [OSTI]

    Smith, Michael W; Jordan, Kevin C

    2014-03-25

    An integrated production apparatus for production of boron nitride nanotubes via the pressure vapor-condenser method. The apparatus comprises: a pressurized reaction chamber containing a continuously fed boron containing target having a boron target tip, a source of pressurized nitrogen and a moving belt condenser apparatus; a hutch chamber proximate the pressurized reaction chamber containing a target feed system and a laser beam and optics.

  17. Domed community and several alternatives for Winooski, Vermont: the environmental, organizational, and energy conservation issues

    SciTech Connect (OSTI)

    Wendt, R.L.

    1980-01-01

    The environmental, organizational, and energy conservation issues related to a domed structure enveloping Winooski, Vermont, are discussed. Alternative means of accomplishing energy conservation will be addressed. These include retrofitting of existing structures, replacement with state-of-the-art structures, the use of planting shelter-belts, redevelopment to an earth-sheltered community, and redevelopment to a composite domed neighborhood and earth-sheltered community. The assets and liabilities of each alternative are addressed.

  18. Hanford_FinalReport_20140130

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    209054 - Hanford PSHA Seismicity Analysis - Felix Waldhauser - Final Report - 1/31/14 3:37 PM 1 Final Report Project Name: Hanford Site-Wide Probabilistic Seismic Hazard Analysis (PSHA): High-Resolution Seismicity Analysis of the Yakima Fold and Thrust Belt Region, Washington Contract Number: Battelle - 209054 Prepared by: Dr. Felix Waldhauser 423 W 120 th Street, Apt 88 New York, NY 10027 Tel: 212 678 4804 Email: felixw@ldeo.columbia.edu Prepared for: Pacific Northwest National Laboratory

  19. Firm eyes savings from tires-to-fuel system

    SciTech Connect (OSTI)

    Barber, J.

    1983-01-31

    A $600,000 pyrolysis system to convert tire scraps into methane will eliminate a tire retreading company's landfill and boiler fuel costs and achieve a five-year payback. The process also yields steel belts, fibers, and carbon black byproducts that can be sold for additional revenue. Heat from the hot exhaust gases will be recycled to the combustion chamber. A 10% federal energy tax credit and a 10% investment tax credit lowered the capital costs for $480,000. (DCK)

  20. Harvesting Vehicle Exhaust with Zero Parasitics | Department of Energy

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Harvesting Vehicle Exhaust with Zero Parasitics Harvesting Vehicle Exhaust with Zero Parasitics Thermal cycling pyroelectric generator is designed to harvest engine waste heat and electrify belt-driven components PDF icon p-22_lu.pdf More Documents & Publications Automotive Thermoelectric Generators and HVAC Parasitic Energy Losses 21st Century Truck Partnership - Roadmap and Technical White Papers Appendix of Supporting Information - 21CTP-0003, December 2006

  1. UCRL-JC-116524 PREPRINT The Beaverhead Impact Structure, SW Montana and Idaho:

    Office of Scientific and Technical Information (OSTI)

    6524 PREPRINT The Beaverhead Impact Structure, SW Montana and Idaho: Implications for the Regional Geology of the Western U.S. Peter S. Fiske and Robert B. Hargaves This document was prepared for submittal to The Belt Symposium III Whitefish, Montana August 14-21,1993 March 17.1994 I c e Thisisapreprintof apaperintended forpublicationina journalorproceedings. Since changes may be made before publication, this preprint is made available with the understanding that it will not be cited o r

  2. Optimized Pump Systems Save Coal Preparation Plant Money and Energy |

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Department of Energy Optimized Pump Systems Save Coal Preparation Plant Money and Energy Optimized Pump Systems Save Coal Preparation Plant Money and Energy This case study describes how Peabody Holding Company was able to improve the performance of a coal slurry pumping system at its Randolph Coal Preparation plant. Using a systematic approach, three energy-saving opportunities were identified involving the motor, belt drive, and pump components of the pumping system. The modifications

  3. Electric arc saw apparatus

    DOE Patents [OSTI]

    Deichelbohrer, P.R.

    1983-08-08

    A portable, hand-held electric arc saw apparatus comprising a small frame for supporting an electrically conducting rotary blade which serves as an electrode for generating an electric arc between the blade and a workpiece of opposite polarity. Electrically conducting means are provided on said frame for transmitting current to said blade. A pair of freely movable endless belts in the form of crawler treads are employed to facilitate movement of the apparatus relative to the workpiece.

  4. Observations and simulations improve space weather models

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Observations improve space weather models Observations and simulations improve space weather models Researchers used data from the Van Allen Probes to improve a three-dimensional model created by Los Alamos scientists called DREAM3D. June 25, 2014 NASA's Van Allen Probes sample the Earth's magnetosphere. NASA's Van Allen Probes sample the Earth's magnetosphere. The work demonstrated that DREAM3D accurately simulated the behavior of a complex and dynamic event in the radiation belt that was

  5. LOS ALAMOS, NEW MEXICO, August 30,2012-Los Alamos National Laboratory

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    provides HOPE for radiation belt storm probes August 30, 2012 Spacecraft pair to explore mysterious region where other satellites fear to tread LOS ALAMOS, NEW MEXICO, August 30,2012-Los Alamos National Laboratory expertise in radiation detection and shielding is poised to help a national team of scientists better understand a mysterious region that can create hazardous space weather near our home planet. The Helium Oxygen Proton Electron (HOPE) analyzer is one of a suite of instruments that was

  6. LOS ALAMOS, New Mexico, August 4, 2010-Los Alamos National Laboratory today

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    first Recovery Act cleanup project August 4, 2010 Demolition of former fusion facility completed ahead of schedule LOS ALAMOS, New Mexico, August 4, 2010-Los Alamos National Laboratory today announced it has completed the first of four major environmental cleanup projects funded by the American Recovery and Reinvestment Act. The $13 million project involved demolition of an 18,000-square-foot former nuclear fusion research facility. "It's good to get this one under our belt," said

  7. Research Opportunities

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Opportunities /collaboration/_assets/images/icon-collaboration.jpg Research Opportunities Partnering with respected universities, LANL Centers provide exceptional educational opportunities and support staff recruitment, revitalization, and retention. Center for Nonlinear Studies» Quantum Institute» Energy Security Center» Seaborg Institute» Center for Space and Earth Science» TOP STORIES - highlights of our science, people, technologies close Bulging Van Allen Belts Learn about the Van

  8. How Dynein Binds to Microtubules

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    How Dynein Binds to Microtubules Print Cytoplasmic dynein is a protein complex responsible for the transport of a large variety of cargoes, from specific RNAs and proteins to whole organelles, in a directional fashion along microtubules that serve as cellular conveyor belts. Consistent with this central role, cytoplasmic dynein is associated with a number of disease-related processes, including the transport of viruses, neurodegeneration, and the mitotic checkpoint malfunctions that lead to

  9. How Dynein Binds to Microtubules

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    How Dynein Binds to Microtubules Print Cytoplasmic dynein is a protein complex responsible for the transport of a large variety of cargoes, from specific RNAs and proteins to whole organelles, in a directional fashion along microtubules that serve as cellular conveyor belts. Consistent with this central role, cytoplasmic dynein is associated with a number of disease-related processes, including the transport of viruses, neurodegeneration, and the mitotic checkpoint malfunctions that lead to

  10. How Dynein Binds to Microtubules

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    How Dynein Binds to Microtubules Print Cytoplasmic dynein is a protein complex responsible for the transport of a large variety of cargoes, from specific RNAs and proteins to whole organelles, in a directional fashion along microtubules that serve as cellular conveyor belts. Consistent with this central role, cytoplasmic dynein is associated with a number of disease-related processes, including the transport of viruses, neurodegeneration, and the mitotic checkpoint malfunctions that lead to

  11. How Dynein Binds to Microtubules

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    How Dynein Binds to Microtubules How Dynein Binds to Microtubules Print Wednesday, 29 April 2009 00:00 Cytoplasmic dynein is a protein complex responsible for the transport of a large variety of cargoes, from specific RNAs and proteins to whole organelles, in a directional fashion along microtubules that serve as cellular conveyor belts. Consistent with this central role, cytoplasmic dynein is associated with a number of disease-related processes, including the transport of viruses,

  12. Los Alamos National Lab: National Security Science

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Science in 60 Flu Video of the Week Forecasting epidemics like weather Real-time data from Wikipedia and social media helps to model disease spread watch cube sat awardees Los Alamos in the News Kudos to "cube" satellite scientists Agile space systems delivered for DOE, military more mosquito Los Alamos in the News Why is Zika now a threat? Population growth, rising temperatures, embryonic immune systems says Lab scientist more Van Allen Belts video screenshot Picture of the Week

  13. eGSE America: Electric Aircraft Cargo Conveyor Technical Specification

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    EACC Technical Specifications eGSE America: Electric Aircraft Cargo Conveyor (EACC) Technical Specifications Revision 00 August 2005 Prepared by Electric Transportation Applications eGSE America: EACC Technical Specifications 1.0 SCOPE: This document outlines the design and performance requirements for a battery- powered, self propelled belt conveyor for handling baggage and cargo at aircraft bulk cargo holds. The use of "shall" in this document indicates a mandatory requirement. The

  14. From: Luke Lowenstein To: Congestion Study Comments Subject:

    Office of Environmental Management (EM)

    Luke Lowenstein To: Congestion Study Comments Subject: GrainBelt Express Date: Friday, September 19, 2014 10:48:56 AM I am opposed to the establishment of National Interest Energy Transmission Corridors (NIETC's) for the following reasons. First, the easements place an undo burden on landowners on and near the transmission lines. The compensation cannot begin to cover the all of the losses, tangible and intangible that landowners would suffer. Second, I believe that condemning private property

  15. Near-earth injection of MeV electrons associated with intense dipolarization electric fields: Van Allen Probes observations

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Dai, Lei; Wang, Chi; Duan, Suping; He, Zhaohai; Wygant, John R.; Cattell, Cynthia A.; Tao, Xin; Su, Zhenpeng; Kletzing, Craig; Baker, Daniel N.; et al

    2015-08-10

    Substorms generally inject tens to hundreds of keV electrons, but intense substorm electric fields have been shown to inject MeV electrons as well. An intriguing question is whether such MeV electron injections can populate the outer radiation belt. Here we present observations of a substorm injection of MeV electrons into the inner magnetosphere. In the premidnight sector at L~5.5, Van Allen Probes (Radiation Belt Storm Probes)-A observed a large dipolarization electric field (50 mV/m) over ~40 s and a dispersionless injection of electrons up to ~3 MeV. Pitch angle observations indicated betatron acceleration of MeV electrons at the dipolarization front.more » Corresponding signals of MeV electron injection were observed at LANL-GEO, THEMIS-D, and GOES at geosynchronous altitude. Through a series of dipolarizations, the injections increased the MeV electron phase space density by 1 order of magnitude in less than 3 h in the outer radiation belt (L > 4.8). Our observations provide evidence that deep injections can supply significant MeV electrons.« less

  16. PLANETESIMALS IN DEBRIS DISKS OF SUN-LIKE STARS

    SciTech Connect (OSTI)

    Shannon, Andrew; Wu Yanqin

    2011-09-20

    Observations of dusty debris disks can be used to test theories of planetesimal coagulation. Planetesimals of sizes up to a couple of thousand kilometers are embedded in these disks and their mutual collisions generate the small dust grains that are observed. The dust luminosities, when combined with information on the dust spatial extent and the system age, can be used to infer initial masses in the planetesimal belts. Carrying out such a procedure for a sample of debris disks around Sun-like stars, we reach the following two conclusions. First, if we assume that colliding planetesimals satisfy a primordial size spectrum of the form dn/ds{proportional_to}s{sup -q}, observed disks strongly favor a value of q between 3.5 and 4, while both current theoretical expectations and statistics of Kuiper belt objects favor a somewhat larger value. Second, number densities of planetesimals are two to three orders of magnitude higher in detected disks than in the Kuiper belt, for comparably sized objects. This is a surprise for the coagulation models. It would require a similar increase in the disk surface density over that of the Minimum Mass Solar Nebula, which is unreasonable. Both of our conclusions are driven by the need to explain the presence of bright debris disks at a few gigayears of age.

  17. Near-earth injection of MeV electrons associated with intense dipolarization electric fields: Van Allen Probes observations

    SciTech Connect (OSTI)

    Dai, Lei; Wang, Chi; Duan, Suping; He, Zhaohai; Wygant, John R.; Cattell, Cynthia A.; Tao, Xin; Su, Zhenpeng; Kletzing, Craig; Baker, Daniel N.; Li, Xinlin; Malaspina, David; Blake, J. Bernard; Fennell, Joseph; Claudepierre, Seth; Turner, Drew L.; Reeves, Geoffrey D.; Funsten, Herbert O.; Spence, Harlan E.; Angelopoulos, Vassilis; Fruehauff, Dennis; Chen, Lunjin; Thaller, Scott; Breneman, Aaron; Tang, Xiangwei

    2015-08-10

    Substorms generally inject tens to hundreds of keV electrons, but intense substorm electric fields have been shown to inject MeV electrons as well. An intriguing question is whether such MeV electron injections can populate the outer radiation belt. Here we present observations of a substorm injection of MeV electrons into the inner magnetosphere. In the premidnight sector at L~5.5, Van Allen Probes (Radiation Belt Storm Probes)-A observed a large dipolarization electric field (50 mV/m) over ~40 s and a dispersionless injection of electrons up to ~3 MeV. Pitch angle observations indicated betatron acceleration of MeV electrons at the dipolarization front. Corresponding signals of MeV electron injection were observed at LANL-GEO, THEMIS-D, and GOES at geosynchronous altitude. Through a series of dipolarizations, the injections increased the MeV electron phase space density by 1 order of magnitude in less than 3 h in the outer radiation belt (L > 4.8). Our observations provide evidence that deep injections can supply significant MeV electrons.

  18. Geochemistry and habitat of the oils in Italy

    SciTech Connect (OSTI)

    Mattavelli, L.; Novelli, L. )

    1990-10-01

    All varieties of liquid petroleum, ranging from condensates (> 50{degree}API) to immature sulfur-rich heavy oils (as low as 5{degree} API), have been found in Italy. However, nonbiodegraded heavy oils account for about 70% of the total original oil in place. Geochemical analyses indicate that 11 oil groups are present in the Italian basins and two main types of source rocks have been identified: Triassic carbonates and Tertiary shales. About 95% of the oils were originated from Middle and Upper Triassic carbonates containing type II kerogen (about 1% total organic carbon (TOC) and 500 mg hydrocarbon/g TOC). Only a relatively minor amount of oil was generated by Tertiary shales containing type III kerogen with TOC generally less than 1%. Timing of generation and migration and bulk properties of oils were controlled by geodynamic histories of the three main Italian geologic settings: (1) Apennine and Southern Alp thrust belts, (2) foredeep (depression bordering the thrust belts), and (3) foreland (nondeformed African continental margin). Within the Apennine thrust belts, deep burial during the Neogene resulted in the generation of substantially lighter oils, not only from deeply buried Triassic but sometimes also from Tertiary source rocks. In the late Neogene, foredeep depocenters located in the central Adriatic and southern Sicily, high subsidence (up to 1,000 m/m.y.), a low geothermal gradient (22C/km) and compressional tectonics caused the generation of immature heavy oils generally at depths below 5,000 m and temperatures greater than 100C. Rapid burial and higher geothermal gradients (32C/km), which occurred since the Jurassic, resulted in the generation of light oils from the Late Cretaceous to the Oligocene in the southern sector of Adriatic foreland.

  19. Integrated Assessment of Hadley Centre (HadCM2) Climate-Change Impacts on Agricultural Productivity and Irrigation Water Supply in the Conterminous United States. Part II. Regional Agricultural Production in 2030 and 2095.

    SciTech Connect (OSTI)

    Izaurralde, R Cesar C.; Rosenberg, Norman J.; Brown, Robert A.; Thomson, Allison M.

    2003-06-30

    This study used scenarios of the HadCM2 GCM and the EPIC agroecosystem model to evaluate climate change impacts on crop yields and ecosystem processes. Baseline climate data were obtained from records for 1961-1990. The scenario runs for 2025-2034 and 2090-2099 were extracted from a HadCM2 run. EPIC was run on 204 representative farms under current climate and two 10-y periods centered on 2030 and 2095, each at CO2 concentrations of 365 and 560 ppm. Texas, New Mexico, Colorado, Utah, Arizona, and California are projected to experience significant temperature increases by 2030. Slight cooling is expected by 2030 in Alabama, Florida, Maine, Montana, Idaho, and Utah. Larger areas are projected to experience increased warming by 2095. Uniform precipitation increases are expected by 2030 in the NE. These increases are predicted to expand to the eastern half of the country by 2095. EPIC simulated yield increases for the Great Lakes, Corn Belt and Northeast regions. Simulated yields of irrigated corn yields were predicted to increase in almost all regions. Soybean yields could decrease in the Northern and Southern Plains, the Corn Belt, Delta, Appalachian, and Southeast regions and increase in the Lakes and Northeast regions. Simulated wheat yields exhibited upward yield trends under scenarios of climate change. National corn production in 2030 and 2095 could be affected by changes in three major producing regions. In 2030, corn production could increase in the Corn Belt and Lakes regions but decrease in the Northern Plains leading to an overall decrease in national production. National wheat production is expected to increase during both future periods. A proxy indicator was developed to provide a sense of where in the country, and when water would be available to satisfy change in irrigation demand for corn and alfalfa production as these are influenced by the HadCM2 scenarios and CO2-fertilization.

  20. Bounce- and MLT-averaged diffusion coefficients in a physics-based magnetic field geometry obtained from RAM-SCB for the March 17 2013 storm

    SciTech Connect (OSTI)

    Zhao, Lei; Yu, Yiqun; Delzanno, Gian Luca; Jordanova, Vania K.

    2015-04-01

    Local acceleration via whistler wave and particle interaction plays a significant role in particle dynamics in the radiation belt. In this work we explore gyro-resonant wave-particle interaction and quasi-linear diffusion in different magnetic field configurations related to the March 17 2013 storm. We consider the Earth's magnetic dipole field as a reference and compare the results against non-dipole field configurations corresponding to quiet and stormy conditions. The latter are obtained with the ring current-atmosphere interactions model with a self-consistent magnetic field RAM-SCB, a code that models the Earth's ring current and provides a realistic modeling of the Earth's magnetic field. By applying quasi-linear theory, the bounce- and MLT-averaged electron pitch angle, mixed term, and energy diffusion coefficients are calculated for each magnetic field configuration. For radiation belt (~1 MeV) and ring current (~100 keV) electrons, it is shown that at some MLTs the bounce-averaged diffusion coefficients become rather insensitive to the details of the magnetic field configuration, while at other MLTs storm conditions can expand the range of equatorial pitch angles where gyro-resonant diffusion occurs and significantly enhance the diffusion rates. When MLT average is performed at drift shell L = 4.25 (a good approximation to drift average), the diffusion coefficients become quite independent of the magnetic field configuration for relativistic electrons, while the opposite is true for lower energy electrons. These results suggest that, at least for the March 17 2013 storm and for L ? 4.25, the commonly adopted dipole approximation of the Earth's magnetic field can be safely used for radiation belt electrons, while a realistic modeling of the magnetic field configuration is necessary to describe adequately the diffusion rates of ring current electrons.

  1. Bounce- and MLT-averaged diffusion coefficients in a physics-based magnetic field geometry obtained from RAM-SCB for the March 17 2013 storm

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Zhao, Lei; Yu, Yiqun; Delzanno, Gian Luca; Jordanova, Vania K.

    2015-04-01

    Local acceleration via whistler wave and particle interaction plays a significant role in particle dynamics in the radiation belt. In this work we explore gyro-resonant wave-particle interaction and quasi-linear diffusion in different magnetic field configurations related to the March 17 2013 storm. We consider the Earth's magnetic dipole field as a reference and compare the results against non-dipole field configurations corresponding to quiet and stormy conditions. The latter are obtained with the ring current-atmosphere interactions model with a self-consistent magnetic field RAM-SCB, a code that models the Earth's ring current and provides a realistic modeling of the Earth's magnetic field.more » By applying quasi-linear theory, the bounce- and MLT-averaged electron pitch angle, mixed term, and energy diffusion coefficients are calculated for each magnetic field configuration. For radiation belt (~1 MeV) and ring current (~100 keV) electrons, it is shown that at some MLTs the bounce-averaged diffusion coefficients become rather insensitive to the details of the magnetic field configuration, while at other MLTs storm conditions can expand the range of equatorial pitch angles where gyro-resonant diffusion occurs and significantly enhance the diffusion rates. When MLT average is performed at drift shell L = 4.25 (a good approximation to drift average), the diffusion coefficients become quite independent of the magnetic field configuration for relativistic electrons, while the opposite is true for lower energy electrons. These results suggest that, at least for the March 17 2013 storm and for L ≲ 4.25, the commonly adopted dipole approximation of the Earth's magnetic field can be safely used for radiation belt electrons, while a realistic modeling of the magnetic field configuration is necessary to describe adequately the diffusion rates of ring current electrons.« less

  2. OCRWM Bulletin

    SciTech Connect (OSTI)

    1996-04-01

    This document is the Winter 1996 ORCWM Bulletin which is a report from the U.S. Department of Energy`s Office of Civilian Radioactive Waste Management. Budget considerations and a discussion of waste policy forums are described. Several articles about the on-going site characterization at Yucca Mountain are included as a part of this bulletin.Tunnel excavations, meteorology studies, effects of seismic events, and design of a conveyor belt system are some of the topics covered in this issue.

  3. Centerless-drive solar collector system

    SciTech Connect (OSTI)

    Butler, B. L.

    1985-12-24

    A parabolic-trough solar collector system is disclosed, with each collector driven to track the sun using a ring driven in centerless fashion. The parabolic troughs are made of laminated plywood or molded or formed of plastics or metals. The drive motor moves a flexible belt, i.e., chain or cable, which is routed about the drive ring on each collector. The motion of the cable moves all drive rings together to track the sun. A photodetector senses the position of the sun and provides the signal needed to drive the collectors in the correct direction.

  4. BSM Newsletter March 2016

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    March 2016 At the Bradbury Latest Issue:March 2016 all issues All Issues » submit IN THIS ISSUE Science question of the month - Trinity test Did the Trinity Test behave as expected? Fossil analysis pushes back human split from other primates by two million years From our pages From tool to artifact, without missing a beat A new artifact joins our collection Study finds surprising variability in shape of Van Allen Belts From our pages Innovative imaging systems on the Wendelstein 7-X bring

  5. Stabilized PV system

    DOE Patents [OSTI]

    Dinwoodie, Thomas L. (Piedmont, CA)

    2002-12-17

    A stabilized PV system comprises an array of photovoltaic (PV) assemblies mounted to a support surface. Each PV assembly comprises a PV module and a support assembly securing the PV module to a position overlying the support surface. The array of modules is circumscribed by a continuous, belt-like perimeter assembly. Cross strapping, extending above, below or through the array, or some combination of above, below and through the array, secures a first position along the perimeter assembly to at least a second position along the perimeter assembly thereby stabilizing the array against wind uplift forces. The first and second positions may be on opposite sides on the array.

  6. NREL Helps Clean Cities Displace Billions of Gallons of Petroleum, One Vehicle at a Time (Fact Sheet)

    SciTech Connect (OSTI)

    Not Available

    2010-10-01

    With more than 15 years and nearly 3 billion gallons of displaced petroleum under its belt, the Clean Cities program relies on the support and expertise of the National Renewable Energy Laboratory (NREL). An initiative of the U.S. Department of Energy (DOE), Clean Cities creates public-private partnerships with a common mission: to reduce petroleum consumption in the transportation sector. Since the inception of Clean Cities in 1993, NREL has played a central role in supporting the program, an effort that stems from the laboratory's strategy to put scientific innovation into action in the marketplace.

  7. V/STOL aircraft and method

    DOE Patents [OSTI]

    Owens, P.R.

    1997-11-18

    Aircraft apparatus and method capable of V/STOL (vertical, short takeoff and landing) in addition to conventional flight are disclosed. For V/STOL operation, induced lift is provided by blowing air over the upper surface of each wing through a duct installed near the leading edge. Intake air is supplied to the blowing fan through a duct installed near the trailing edge, thus providing suction as well as blowing. Two fans in series are required. The engine provides power not only to the propeller but also to a transmission which provides power to the pulleys driving the belt-driven fans. 10 figs.

  8. A PUBLICATION FOR ALL MEMBERS OF THE NNSA/NSO FAMILY Contents

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    4 October 2003 Brooks addresses NNSA staff 1 NNSA scientists con- duct 20th subcritical experiment 2 Unicorn subcritical experiment planned 2 Tanks a lot! 3 NTS cafeteria prices to increase 3 NTS history gets new home 3 Watusi team honored with award 4 Bechtel donates $500,000 to new UNLV research facility 5 BN reorganizes 5 Stoller-Navarro is new EM contractor 6 First BN yellow belt qualifies 6 And so it continues 7 To Your Health 7 Beryllium All-Hands 9 New toxic metal lab 10 Task foces to

  9. Coal Transportation Issues (released in AEO2007)

    Reports and Publications (EIA)

    2007-01-01

    Most of the coal delivered to U.S. consumers is transported by railroads, which accounted for 64% of total domestic coal shipments in 2004. Trucks transported approximately 12% of the coal consumed in the United States in 2004, mainly in short hauls from mines in the East to nearby coal-fired electricity and industrial plants. A number of minemouth power plants in the West also use trucks to haul coal from adjacent mining operations. Other significant modes of coal transportation in 2004 included conveyor belt and slurry pipeline (12%) and water transport on inland waterways, the Great Lakes, and tidewater areas (9%).

  10. Cost Benefit Analysis Modeling Tool for Electric vs. ICE Airport Ground Support Equipment Development and Results

    SciTech Connect (OSTI)

    James Francfort; Kevin Morrow; Dimitri Hochard

    2007-02-01

    This report documents efforts to develop a computer tool for modeling the economic payback for comparative airport ground support equipment (GSE) that are propelled by either electric motors or gasoline and diesel engines. The types of GSE modeled are pushback tractors, baggage tractors, and belt loaders. The GSE modeling tool includes an emissions module that estimates the amount of tailpipe emissions saved by replacing internal combustion engine GSE with electric GSE. This report contains modeling assumptions, methodology, a users manual, and modeling results. The model was developed based on the operations of two airlines at four United States airports.

  11. Double layer -- a particle accelerator in the magnetosphere

    SciTech Connect (OSTI)

    Fu, Xiangrong

    2015-07-16

    Slides present the material under the following topics: Introduction (What is a double layer (DL)? Why is it important? Key unsolved problems); Theory -- time-independent solutions of 1D Vlasov--Poisson system; Particle-in-cell simulations (Current-driven DLs); and Electron acceleration by DL (Betatron acceleration). Key problems include the generation mechanism, stability, and electron acceleration. In summary, recent observations by Van Allen Probes show large number of DLs in the outer radiation belt, associated with enhanced flux of relativistic electrons. Simulations show that ion acoustic double layers can be generated by field-aligned currents. Thermal electrons can gain energy via betatron acceleration in a dipole magnetic field.

  12. Electric arc saw apparatus

    DOE Patents [OSTI]

    Deichelbohrer, Paul R [Richland, WA

    1986-01-01

    A portable, hand held electric arc saw has a small frame for supporting an electrically conducting rotary blade which serves as an electrode for generating an electric arc to erode a workpiece. Electric current is supplied to the blade by biased brushes and a slip ring which are mounted in the frame. A pair of freely movable endless belts in the form of crawler treads stretched between two pulleys are used to facilitate movement of the electric arc saw. The pulleys are formed of dielectric material to electrically insulate the crawler treads from the frame.

  13. COLLOQUIUM: Dawn, the Asteroid Redirect Mission, and the Future of Solar

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Electric Propulsion | Princeton Plasma Physics Lab April 9, 2015, 2:00pm to 3:30pm Colloquia MBG Auditorium COLLOQUIUM: Dawn, the Asteroid Redirect Mission, and the Future of Solar Electric Propulsion Dr. John Brophy NASA Jet Propulsion Laboratory Abstract: PDF icon COLL.04.09.14.pdf The ongoing Dawn mission has as its goal the exploration of the two most massive main-belt asteroids, 4 Vesta and 1 Ceres. This mission is enabled by an on-board, solar powered, ion propulsion system that will

  14. COLLOQUIUM: Worlds Seen for the First Time - Ceres and Pluto | Princeton

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Plasma Physics Lab 29, 2015, 4:00pm to 5:30pm Colloquia MBG Auditorium COLLOQUIUM: Worlds Seen for the First Time - Ceres and Pluto Dr. James Green NASA This year, planetary spacecraft will visit two significant bodies in the solar system. These bodies are the dwarf planets Ceres and Pluto. Ceres was first discovered in 1801 and thought to be a planet. It was only realized 50 years later that Ceres was a member of a huge number of objects in what we now know as the asteroid belt. The Dawn

  15. V/STOL aircraft and method

    DOE Patents [OSTI]

    Owens, Phillip R.

    1997-01-01

    Aircraft apparatus and method capable of V/STOL (vertical, short takeoff and landing) in addition to conventional flight. For V/STOL operation, induced lift is provided by blowing air over the upper surface of each wing through a duct installed near the leading edge. Intake air is supplied to the blowing fan through a duct installed near the trailing edge, thus providing suction as well as blowing. Two fans in series are required. The engine provides power not only to the propeller but also to a transmission which provides power to the pulleys driving the belt-driven fans.

  16. CAMS Capabilities

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    CAMS Capabilities HVEC 10 MV Model FN Tandem Of the three accelerators CAMS utilizes the largest is the HVEC 10 MV Model FN Tandem, which was obtained from the University of Washington and installed at LLNL in the mid-80s. During installation the accelerator's belt charging system was replaced with a NEC Pelletron, new Dowlish spiral-inclined beam tubes were installed, as were the gas-handling systems necessary for use of SF6 as the insulating tank gas. The FN accelerator is routinely operated

  17. From: Gary Mareschal To: Congestion Study Comments Subject:

    Office of Environmental Management (EM)

    Gary Mareschal To: Congestion Study Comments Subject: NIETC and Eminent Domain Issues Date: Wednesday, September 24, 2014 11:58:31 AM To whom it may concern, I am opposed to the use of NIETC's and the use of federal eminent domain to condemn private land to establish them. I reside in the state of Missouri and have unfortunatly become involved with the Grain Belt Clean Energy Express Line and the Missouri Public Service Commission, which has not yet ruled on the application before them from

  18. Salmon, Mississippi, Site

    Office of Legacy Management (LM)

    Salmon, Mississippi, Site Location of the Salmon, Mississippi, Site Site Description and History The Salmon, Mississippi, Site, also called the Tatum Dome Test Site, is a 1,470-acre tract of land in Lamar County, Mississippi, 21 miles southwest of Hattiesburg. The nearest town is Purvis, about 10 miles east of the site. The site is in a forested region known as the long-leaf pine belt of the Gulf Coastal Plain. Elevations in the area range from about 240 to 350 feet above sea level. The site

  19. Title

    National Nuclear Security Administration (NNSA)

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  20. Title

    National Nuclear Security Administration (NNSA)

    the Nopah and Resting Springs Ranges to the southwest of Pahrump Valley. -45- v . _s' Belted X / ^~" " Range X / * /I \ Pahute Mesa /* \ / | > / Rainier ! \ / Mesa | \ ' Halfp \ 5 \ Ra " 9e }* ^ y \ o * \ l| \ Yucca *j \ Flo- | Timber j -| f / i Mountain * «u ^ / -f ! / */ i i / ii ! Yucca / 5^ Mountain 1 -c 3 ^j ! sJ ! 1 ^S 050 1 , Frenchman Ftar ] Desert | / | L / i L__. _ _^^_ - ^^^ _ ^^^ " . 1 1 fli_. j i 1 i ! i l nt Lincoln County Clark County *- -- *- - - »-s

  1. Relativistic electron scattering by magnetosonic waves: Effects of discrete wave emission and high wave amplitudes

    SciTech Connect (OSTI)

    Artemyev, A. V.; Mourenas, D.; Krasnoselskikh, V. V.

    2015-06-15

    In this paper, we study relativistic electron scattering by fast magnetosonic waves. We compare results of test particle simulations and the quasi-linear theory for different spectra of waves to investigate how a fine structure of the wave emission can influence electron resonant scattering. We show that for a realistically wide distribution of wave normal angles θ (i.e., when the dispersion δθ≥0.5{sup °}), relativistic electron scattering is similar for a wide wave spectrum and for a spectrum consisting in well-separated ion cyclotron harmonics. Comparisons of test particle simulations with quasi-linear theory show that for δθ>0.5{sup °}, the quasi-linear approximation describes resonant scattering correctly for a large enough plasma frequency. For a very narrow θ distribution (when δθ∼0.05{sup °}), however, the effect of a fine structure in the wave spectrum becomes important. In this case, quasi-linear theory clearly fails in describing accurately electron scattering by fast magnetosonic waves. We also study the effect of high wave amplitudes on relativistic electron scattering. For typical conditions in the earth's radiation belts, the quasi-linear approximation cannot accurately describe electron scattering for waves with averaged amplitudes >300 pT. We discuss various applications of the obtained results for modeling electron dynamics in the radiation belts and in the Earth's magnetotail.

  2. Sedimentology of the Mesaverde Formation at Rifle Gap, Colorado and implications for gas-bearing intervals in the subsurface

    SciTech Connect (OSTI)

    Lorenz, J.C.

    1982-03-01

    The exposures of the Mesaverde Formation at Rifle Gap, Colorado, are of a regressive series of marine to fluvial deposits about 1650 m (5000 ft) thick. Grading up out of the marine Mancos Shale, the blanket shoreline sandstones of the Corcoran, Cozzette, and Rollins Sandstones record substages of the regression as delta lobes were activated and abandoned in northwestern Colorado during Late Cretaceous time. The overlying coals, sandstones, and carbonaceous mudstones were deposited on the paludal lower delta plain behind the shoreline. Meandering fluvial systems prograded over the paludal deposits. These systems deposited point-bar sandstones and overbank mudstones and siltstones in composite meander-belt trends, some of which are now gas-bearing, low-permeability reservoirs. Reorientation of the paleogeography during the Laramide orogeny (contemporaneous with fluvial deposition) probably changed the orientation of the meander belt trends. The uppermost sandstones at Rifle Gap, including the Ohio Creek conglomerate, are interpreted as shoreline deposits of a transgression that has been previously unrecognized in the area. Most of the record of this transgression has been destroyed by pre-Eocene erosion. The outcrops at Rifle Gap provide a basis for interpreting subsurface deposis in the Department of Energy's Western Gas Sands Project Multi-Well Experiment, 12 miles away.

  3. Analysis of heavy oils: Method development and application to Cerro Negro heavy petroleum

    SciTech Connect (OSTI)

    Carbognani, L.; Hazos, M.; Sanchez, V. ); Green, J.A.; Green, J.B.; Grigsby, R.D.; Pearson, C.D.; Reynolds, J.W.; Shay, J.Y.; Sturm, G.P. Jr.; Thomson, J.S.; Vogh, J.W.; Vrana, R.P.; Yu, S.K.T.; Diehl, B.H.; Grizzle, P.L.; Hirsch, D.E; Hornung, K.W.; Tang, S.Y.

    1989-12-01

    On March 6, 1980, the US Department of Energy (DOE) and the Ministry of Energy and Mines of Venezuela (MEMV) entered into a joint agreement which included analysis of heavy crude oils from the Venezuelan Orinoco oil belt.The purpose of this report is to present compositional data and describe new analytical methods obtained from work on the Cerro Negro Orinoco belt crude oil since 1980. Most of the chapters focus on the methods rather than the resulting data on Cerro Negro oil, and results from other oils obtained during the verification of the method are included. In addition, published work on analysis of heavy oils, tar sand bitumens, and like materials is reviewed, and the overall state of the art in analytical methodology for heavy fossil liquids is assessed. The various phases of the work included: distillation and determination of routine'' physical/chemical properties (Chapter 1); preliminary separation of >200{degree}C distillates and the residue into acid, base, neutral, saturated hydrocarbon and neutral-aromatic concentrates (Chapter 2); further separation of acid, base, and neutral concentrates into subtypes (Chapters 3-5); and determination of the distribution of metal-containing compounds in all fractions (Chapter 6).

  4. Reworked eolianites: Bahaman highstand anomalies

    SciTech Connect (OSTI)

    Ball, M.M. (Geological Survey, Denver, CO (USA))

    1990-05-01

    Eolianites, presumably formed during the last sea level lowstand, rise more than 40 m above the present-day highstand. These carbonate dune are being reworked by wave action to form sediment bodies (highstand conglomerates) with settings, geometries, internal structures, compositions, and textures that may be similar to those of lowstand conglomerates. The setting of these reworked eolianites is the windward platform edge. The geometry is a belt parallel to the platform edge, that may thin both platformward and basinward. Internal structure should include some large-scale foresets with chaotic dip directions and some evidence of tilted and overturned beds. Composition consists of marine bioclastic carbonate sand in boulder to sand-size clasts. If remnants of the carbonate dunes are preserved in the geologic record, highstand conglomerates should be recognizable on the basis of their association with these eolianites. The original eolianites are confirmed to a belt on the windward margins of the carbonate platform up to 7 km wide. Their geometry consists of linear sand waves or ridges composed of spillover lobes. Internal structure predominantly includes large-scale foresets dipping toward the platform interior. Composition is indistinguishable from that of associated highstand conglomerates with the possible exception that the latter might contain some high-magnesium calcite or aragonite marine cement. Whole marine fossils are absent in the eolianites. Red-weathered zones are common on dune exposure surface. Solution brecciation and cave deposition further complicate the diagenetic history of the eolianites, their associated highstand conglomerates, and their lowstand conglomeratic facies.

  5. Rivesville multicell fluidized bed boiler

    SciTech Connect (OSTI)

    Not Available

    1981-03-01

    One objective of the experimental MFB at Rivesville, WV, was the evaluation of alternate feed systems for injecting coal and limestone into a fluidized bed. A continuous, uniform feed flow to the fluid bed is essential in order to maintain stable operations. The feed system originally installed on the MFB was a gravity feed system with an air assist to help overcome the back pressure created by the fluid bed. The system contained belt, vibrating, and rotary feeders which have been proven adequate in other material handling applications. This system, while usable, had several operational and feeding problems during the MFB testing. A major portion of these problems occurred because the coal and limestone feed control points - a belt feeder and rotary feeder, respectively - were pressurized in the air assist system. These control points were not designed for pressurized service. An alternate feed system which could accept feed from the two control points, split the feed into six equal parts and eliminate the problems of the pressurized system was sought. An alternate feed system designed and built by the Fuller Company was installed and tested at the Rivesville facility. Fuller feed systems were installed on the north and south side of C cell at the Rivesville facility. The systems were designed to handle 10,000 lb/hr of coal and limestone apiece. The systems were installed in late 1979 and evaluated from December 1979 to December 1980. During this time period, nearly 1000 h of operating time was accumulated on each system.

  6. THE SIZE DISTRIBUTION OF THE NEPTUNE TROJANS AND THE MISSING INTERMEDIATE-SIZED PLANETESIMALS

    SciTech Connect (OSTI)

    Sheppard, Scott S.; Trujillo, Chadwick A.

    2010-11-10

    We present an ultra-deep survey for Neptune Trojans using the Subaru 8.2 m and Magellan 6.5 m telescopes. The survey reached a 50% detection efficiency in the R band at m{sub R} = 25.7 mag and covered 49 deg{sup 2} of sky. m{sub R} = 25.7 mag corresponds to Neptune Trojans that are about 16 km in radius (assuming an albedo of 0.05). A paucity of smaller Neptune Trojans (radii < 45 km) compared with larger ones was found. The brightest Neptune Trojans appear to follow a steep power-law slope (q = 5 {+-} 1) similar to the brightest objects in the other known stable reservoirs such as the Kuiper Belt, Jupiter Trojans, and main belt asteroids. We find a roll-over for the Neptune Trojans that occurs around a radius of r = 45 {+-} 10 km (m{sub R} = 23.5 {+-} 0.3), which is also very similar to the other stable reservoirs. All the observed stable regions in the solar system show evidence for Missing Intermediate-Sized Planetesimals (MISPs). This indicates a primordial and not collisional origin, which suggests that planetesimal formation proceeded directly from small to large objects. The scarcity of intermediate- and smaller-sized Neptune Trojans may limit them as being a strong source for the short period comets.

  7. Revealing asymmetries in the HD 181327 debris disk: A recent massive collision or interstellar medium warping

    SciTech Connect (OSTI)

    Stark, Christopher C.; Kuchner, Marc J.; Schneider, Glenn; Weinberger, Alycia J.; Debes, John H.; Grady, Carol A.; Jang-Condell, Hannah

    2014-07-01

    New multi-roll coronagraphic images of the HD 181327 debris disk obtained using the Space Telescope Imaging Spectrograph on board the Hubble Space Telescope reveal the debris ring in its entirety at high signal-to-noise ratio and unprecedented spatial resolution. We present and apply a new multi-roll image processing routine to identify and further remove quasi-static point-spread function-subtraction residuals and quantify systematic uncertainties. We also use a new iterative image deprojection technique to constrain the true disk geometry and aggressively remove any surface brightness asymmetries that can be explained without invoking dust density enhancements/deficits. The measured empirical scattering phase function for the disk is more forward scattering than previously thought and is not well-fit by a Henyey-Greenstein function. The empirical scattering phase function varies with stellocentric distance, consistent with the expected radiation pressured-induced size segregation exterior to the belt. Within the belt, the empirical scattering phase function contradicts unperturbed debris ring models, suggesting the presence of an unseen planet. The radial profile of the flux density is degenerate with a radially varying scattering phase function; therefore estimates of the ring's true width and edge slope may be highly uncertain. We detect large scale asymmetries in the disk, consistent with either the recent catastrophic disruption of a body with mass >1% the mass of Pluto, or disk warping due to strong interactions with the interstellar medium.

  8. REVISITING JOVIAN-RESONANCE INDUCED CHONDRULE FORMATION

    SciTech Connect (OSTI)

    Nagasawa, M.; Tanaka, K. K.; Tanaka, H.; Nakamoto, T.; Miura, H.; Yamamoto, T.

    2014-10-10

    It is proposed that planetesimals perturbed by Jovian mean-motion resonances are the source of shock waves that form chondrules. It is considered that this shock-induced chondrule formation requires the velocity of the planetesimal relative to the gas disk to be on the order of ? 7 km s{sup 1} at 1AU. In previous studies on planetesimal excitation, the effects of Jovian mean-motion resonance together with the gas drag were investigated, but the velocities obtained were at most 8 km s{sup 1} in the asteroid belt, which is insufficient to account for the ubiquitous existence of chondrules. In this paper, we reexamine the effect of Jovian resonances and take into account the secular resonance in the asteroid belt caused by the gravity of the gas disk. We find that the velocities relative to the gas disk of planetesimals a few hundred kilometers in size exceed 12 km s{sup 1}, and that this is achieved around the 3:1 mean-motion resonance. The heating region is restricted to a relatively narrowband between 1.5AU and 3.5AU. Our results suggest that chondrules were produced effectively in the asteroid region after Jovian formation. We also find that many planetesimals are scattered far beyond Neptune. Our findings can explain the presence of crystalline silicate in comets if the scattered planetesimals include silicate dust processed by shock heating.

  9. Electron scattering and nonlinear trapping by oblique whistler waves: The critical wave intensity for nonlinear effects

    SciTech Connect (OSTI)

    Artemyev, A. V. Vasiliev, A. A.; Mourenas, D.; Krasnoselskikh, V. V.

    2014-10-15

    In this paper, we consider high-energy electron scattering and nonlinear trapping by oblique whistler waves via the Landau resonance. We use recent spacecraft observations in the radiation belts to construct the whistler wave model. The main purpose of the paper is to provide an estimate of the critical wave amplitude for which the nonlinear wave-particle resonant interaction becomes more important than particle scattering. To this aim, we derive an analytical expression describing the particle scattering by large amplitude whistler waves and compare the corresponding effect with the nonlinear particle acceleration due to trapping. The latter is much more rare but the corresponding change of energy is substantially larger than energy jumps due to scattering. We show that for reasonable wave amplitudes ?10100?mV/m of strong whistlers, the nonlinear effects are more important than the linear and nonlinear scattering for electrons with energies ?1050?keV. We test the dependencies of the critical wave amplitude on system parameters (background plasma density, wave frequency, etc.). We discuss the role of obtained results for the theoretical description of the nonlinear wave amplification in radiation belts.

  10. Correlation studies between solar wind parameters and the decimetric radio emission from Jupiter

    SciTech Connect (OSTI)

    Bolton, S.J.; Gulkis, S.; Klein, M.J.; De Pater, I.; Thompson, T.J.

    1989-01-01

    Results of a study comparing long-term time variations (years) in Jupiter's synchrotron radio emission with a variety of solar wind parameters and the 10.7-cm solar flux are reported. Data from 1963 through 1985 were analyzed, and the results suggest that many solar wind parameters are correlated with the intensity of the synchrotron emission produced by the relativistic electrons in the Jovian Van Allen radiation belts. Significant nonzero correlation coefficients appear to be associated with solar wind ion density, ram pressure, thermal pressure, flow velocity, momentum, and ion temperature. The highest correlation coefficients are obtained for solar wind ram pressure (NV/sup 2/) and thermal pressure (NT). The correlation analysis suggests that the delay time between fluctuations in the solar wind and changes in the Jovian synchrotron emission is typically about 2 years. The delay time of the correlation places important constraints on the theoretical models describing the radiation belts. The implication of these results, if the correlations are real, is that the solar wind is influencing the supply and/or loss of electrons to Jupiter's inner magnetosphere. We note that the data for this work spans only about two periods of the solar activity cycle, and because of the long time scales of the observed variations, it is important to confirm these results with additional observations. copyright American Geophysical Union 1989

  11. Quantifying the Effects of Idle-Stop Systems on Fuel Economy in Light-Duty Passenger Vehicles

    SciTech Connect (OSTI)

    Jeff Wishart; Matthew Shirk

    2012-12-01

    Vehicles equipped with idle-stop (IS) systems are capable of engine shut down when the vehicle is stopped and rapid engine re-start for the vehicle launch. This capability reduces fuel consumption and emissions during periods when the engine is not being utilized to provide propulsion or to power accessories. IS systems are a low-cost and fast-growing technology in the industry-wide pursuit of increased vehicle efficiency, possibly becoming standard features in European vehicles in the near future. In contrast, currently there are only three non-hybrid vehicle models for sale in North America with IS systems and these models are distinctly low-volume models. As part of the United States Department of Energys Advanced Vehicle Testing Activity, ECOtality North America has tested the real-world effect of IS systems on fuel consumption in three vehicle models imported from Europe. These vehicles were chosen to represent three types of systems: (1) spark ignition with 12-V belt alternator starter; (2) compression ignition with 12-V belt alternator starter; and (3) direct-injection spark ignition, with 12-V belt alternator starter/combustion restart. The vehicles have undergone both dynamometer and on-road testing; the test results show somewhat conflicting data. The laboratory data and the portion of the on-road data in which driving is conducted on a prescribed route with trained drivers produced significant fuel economy improvement. However, the fleet data do not corroborate improvement, even though the data show significant engine-off time. It is possible that the effects of the varying driving styles and routes in the fleet testing overshadowed the fuel economy improvements. More testing with the same driver over routes that are similar with the IS system-enabled and disabled is recommended. There is anecdotal evidence that current Environmental Protection Agency fuel economy test procedures do not capture the fuel economy gains that IS systems produce in real-world driving. The program test results provide information on the veracity of these claims.

  12. Unraveling the Timing of Fluid Migration and Trap Formation in the Brooks Range Foothills: A Key to Discovering Hydrocarbons

    SciTech Connect (OSTI)

    Catherine L. Hanks

    2008-12-31

    Naturally occurring fractures can play a key role in the evolution and producibility of a hydrocarbon accumulation. Understanding the evolution of fractures in the Brooks Range/Colville basin system of northern Alaska is critical to developing a better working model of the hydrocarbon potential of the region. This study addressed this problem by collecting detailed and regional data on fracture distribution and character, structural geometry, temperature, the timing of deformation along the Brooks Range rangefront and adjacent parts of the Colville basin, and the in situ stress distribution within the Colville basin. This new and existing data then were used to develop a model of how fractures evolved in northern Alaska, both spatially and temporally. The results of the study indicate that fractures formed episodically throughout the evolution of northern Alaska, due to a variety of mechanisms. Four distinct fracture sets were observed. The earliest fractures formed in deep parts of the Colville basin and in the underlying Ellesmerian sequence rocks as these rocks experienced compression associated with the growing Brooks Range fold-and-thrust belt. The orientation of these deep basin fractures was controlled by the maximum in situ horizontal stress in the basin at the time of their formation, which was perpendicular to the active Brooks Range thrust front. This orientation stayed consistently NS-striking for most of the early history of the Brooks Range and Colville basin, but changed to NW-striking with the development of the northeastern Brooks Range during the early Tertiary. Subsequent incorporation of these rocks into the fold-and-thrust belt resulted in overprinting of these deep basin fractures by fractures caused by thrusting and related folding. The youngest fractures developed as rocks were uplifted and exposed. While this general order of fracturing remains consistent across the Brooks Range and adjacent Colville basin, the absolute age at any one location varies. Fracturing started in the southwest deep in the stratigraphic section during the Late Jurassic and Early Cretaceous, moving northeastward and upsection as the Colville basin filled from the west. Active fracturing is occurring today in the northeastern parts of the Colville basin, north of the northeastern Brooks thrust front. Across northern Alaska, the early deep basin fractures were probably synchronous with hydrocarbon generation. Initially, these early fractures would have been good migration pathways, but would have been destroyed where subsequently overridden by the advancing Brooks Range fold-and-thrust belt. However, at these locations younger fracture sets related to folding and thrusting could have enhanced reservoir permeability and/or served as vertical migration pathways to overlying structural traps.

  13. Distribution of Clokey's Eggvetch

    SciTech Connect (OSTI)

    David C. Anderson

    1998-12-01

    The Environment, Safety and Health Division of the U.S. Department of Energy, Nevada Operations Office implements the Ecological Monitoring and Compliance Program on the Nevada Test Site (NTS). This program ensures compliance with applicable environmental laws and regulations, delineates and describes NTS ecosystems, and provides ecological information for predicting and evaluating potential impacts of proposed projects on those ecosystems. Over the last several decades, has taken an active role in providing information on the tatus of plant species proposed for protection under the Endangered Species Act(ESA). One such species is Clokey's eggvetch (Astragalus oophorus var. clokeyanus), which is a candidate species under the listing guidelines of the ESA. Surveys for this species were conducted on the NTS in 1996, 1997, and 1998. Field surveys focused on potential habitat for this species in the southern Belted range and expanded to other areas with similar habitat. Over 30 survey day s were completed; five survey days in 1996, 25 survey days in 1997, and three survey days in 1998. Clokey's eggvetch was located at several sites in the southern Belted Range. It was found through much of the northern section of Kawich Canyon, one site at the head of Gritty Gulch, and a rather extensive location in Lambs Canyon. It was also located further south at Captain Jack Springs in the Eleana Range, in much of Falcon Canyon and around Echo Peak on Pahute Mesa, and was also found in the Timber and Shoshone Mountains. Overall, the locations of Clokey's eggvetch on the NTS appears to form a distinct bridge between populations of the species located further north in the Belted and Kawich Ranges and the population located in the Spring Mountains. Clokey's eggvetch was commonly found along washes and small draws, and typically in sandy loam soils with a covering of light tuffaceous rock. It occurs primarily above 1830 meters (6000 feet) in association with single-leaf pinyon (Pinus monophylla), Utah juniper (Juniperus osteosperma), and big sagebrush (Artemisia tridentata ssp. tridentata). Overall, the populations of Clokey's eggvetch on the NTS appear to be vigorous and do not appear threatened. It is estimated that there are approximately 2300 plants on the NTS. It should be considered as a species of concern because of its localized distribution, but it does not appear to warrant protection under the ESA.

  14. Nonlinear electron acceleration by oblique whistler waves: Landau resonance vs. cyclotron resonance

    SciTech Connect (OSTI)

    Artemyev, A. V.; Agapitov, O. V.; Krasnoselskikh, V. V.; Mourenas, D.

    2013-12-15

    This paper is devoted to the study of the nonlinear interaction of relativistic electrons and high amplitude strongly oblique whistler waves in the Earth's radiation belts. We consider electron trapping into Landau and fundamental cyclotron resonances in a simplified model of dipolar magnetic field. Trapping into the Landau resonance corresponds to a decrease of electron equatorial pitch-angles, while trapping into the first cyclotron resonance increases electron equatorial pitch-angles. For 100 keV electrons, the energy gained due to trapping is similar for both resonances. For electrons with smaller energy, acceleration is more effective when considering the Landau resonance. Moreover, trapping into the Landau resonance is accessible for a wider range of initial pitch-angles and initial energies in comparison with the fundamental resonance. Thus, we can conclude that for intense and strongly oblique waves propagating in the quasi-electrostatic mode, the Landau resonance is generally more important than the fundamental one.

  15. Evaluate fundamental approaches to longwall dust control: Subprogram C, Stageloader dust control

    SciTech Connect (OSTI)

    Kelly, J.; Ruggieri, S.

    1990-05-01

    The contamination of intake air is a significant dust control problem, often overlooked on many longwall faces, that can add to the full shift dust exposure of all face personnel. Several sources can contribute to intake air contamination; however, the stageloader (particularly with a crusher) is the single largest source. The objective of this subprogram was to design and evaluate a stageloader dust control system. This was accomplished through a manufacturer's survey to document existing dust controls and determine design parameters for the new systems, laboratory investigations of potential system components, and three underground evaluations of different prototype ideas. Ultimately a series of simple, practical and mineworthy recommendation evolved for optimized stageloader dust control. These included enclosing the entire stageloader with brattice or conveyor belting and installing three auxiliary spraybars at strategic locations along the enclosed stageloader. A field test of these techniques reduced dust levels by 80 percent in the headgate and by 45 percent along the face. 27 figs., 8 tabs.

  16. Tribological sinks in emerging industries: electronics and robotics

    SciTech Connect (OSTI)

    Russell, J.A.; Hane, G.J.

    1986-08-01

    This report describes a preliminary review of the impact of tribological effects - losses due to friction and wear - in two emerging industries: robotics and electronics. Major sources of tribological wear in the robotics industry include the chains used to drive the robots and the joints in the elbow and wrist. In the electronics industry, the largest source of tribological wear is the particulate wear of vacuum pumps used in corrosive environments. Other significant sources of wear are the conveyor belts, blowers, and fans used for clean rooms, and the slicing, lapping and polishing operations for silicon wafers. The major loss mechanisms are friction and abrasion (abrasion includes 2-body wear, 3-body wear, gouging, grinding, erosion, and cutting wear).

  17. Multi-axis planar slide system

    DOE Patents [OSTI]

    Bieg, Lothar F. (Albuquerque, NM)

    2002-01-01

    An apparatus for positioning an item that provides two-dimensional, independent orthogonal motion of a platform in a X-Y plane. A pair of master and slave disks engages opposite sides of the platform. Rotational drivers are connected to master disks so the disks rotate eccentrically about axes of rotation. Opposing slave disks are connected to master disks on opposite sides of the platform by a timing belt, or are electronically synchronized together using stepper motors, to effect coordinated motion. The coordinated eccentric motion of the pairs of master/slave disks compels smooth linear motion of the platform in the X-Y plane without backlash. The apparatus can be a planar mechanism implemented in a MEMS device.

  18. San Antonio spurs increase in solar energy production

    Broader source: Energy.gov [DOE]

    They might always remember the Alamo, but such tourist attractions aren’t the only thing spurring growth in San Antonio — this Texas city is incorporating solar power into its diversified energy portfolio. In June, CPS Energy — the country’s largest municipally owned energy company (meaning profits contribute to the city’s annual budget) — signed a 20-year Power Purchase Agreement to develop a solar project using SunCatcher power systems. These large, concave bowls look like large satellite dishes. Not only will these systems help power Texas, but also they are designed to take advantage of tried-and-true automotive supply chains in the U.S. Rust Belt, using stamped sheet metal, which could help bring new life to manufacturers there.

  19. Liquid-phase-deposited siloxane-based capping layers for silicon solar cells

    SciTech Connect (OSTI)

    Veith-Wolf, Boris; Wang, Jianhui; Hannu-Kuure, Milja; Chen, Ning; Hadzic, Admir; Williams, Paul; Leivo, Jarkko; Karkkainen, Ari; Schmidt, Jan

    2015-02-02

    We apply non-vacuum processing to deposit dielectric capping layers on top of ultrathin atomic-layer-deposited aluminum oxide (AlO{sub x}) films, used for the rear surface passivation of high-efficiency crystalline silicon solar cells. We examine various siloxane-based liquid-phase-deposited (LPD) materials. Our optimized AlO{sub x}/LPD stacks show an excellent thermal and chemical stability against aluminum metal paste, as demonstrated by measured surface recombination velocities below 10 cm/s on 1.3 Ωcm p-type silicon wafers after firing in a belt-line furnace with screen-printed aluminum paste on top. Implementation of the optimized LPD layers into an industrial-type screen-printing solar cell process results in energy conversion efficiencies of up to 19.8% on p-type Czochralski silicon.

  20. Design of Stirling-driven vapor-compression system

    SciTech Connect (OSTI)

    Kagawa, N.

    1998-07-01

    Stirling engines have many unique advantages including higher thermal efficiencies, preferable exhaust gas characteristics, multi-fuel usage, and low noise and vibration. On the other hand, heat pump systems are very attractive for space heating and cooling and industrial usage because of their potential to save energy. Especially, there are many environmental merits of Stirling-driven vapor-compression (SDVC) systems. This paper introduces a design method for the SDVC based on reliable mathematical methods for Stirling and Rankine cycles with reliable thermophysical information for refrigerants. The model treats a kinematic Stirling engine and a scroll compressor coupled by a belt. Some experimental coefficients are used to formulate the SDVC items. The obtained results show the performance behavior of the SDVC in detail. The measured performance of the actual system agrees with the calculated results. Furthermore, the calculated results indicate attractive SDVC performance using alternative refrigerants.

  1. Process improvement studies on the Battelle Hydrothermal Coal Process. Final report, April 1978-April 1984

    SciTech Connect (OSTI)

    Stambaugh, E.P.; Miller, J.F.; Conkle, H.N.; Mezey, E.J.; Smith, R.K.

    1985-06-01

    The report gives results of a study to improve the economic viability of the Battelle Hydrothermal (HT) Coal Process by reducing the costs associated with liquid/solid separation and leachant regeneration. Laboratory experiments were conducted to evaluate process improvements for (1) separating the spent leachant and residual sodium from the coal product, (2) reducing the moisture content of the coal product, and (3) regenerating the leachant. In addition, coal desulfurization experiments were performed and economic studies were conducted to evaluate the impacts of process improvements on coal desulfurization costs. Using countercurrent washing, the optimum washing circuit was composed of four disc-filter stages, six belt-filter stages to separate spent leachant and sodium from the clean coal, and a centrifuge stage to dewater the coal. Several regenerates were found to be effective in removing greater than about 85% of the total sulfide sulfur from the spent leachant: iron carbonate was the leading candidate.

  2. Correlation and deposystem interpretation for Lower Mississippian sequence in subsurface of West Virginia

    SciTech Connect (OSTI)

    Boswell, R.M.; Jewell, G.A. )

    1988-08-01

    Correlation and depositional environments of the Upper Devonian-Lower Mississippian Price-Rockwell delta complex are well understood for units along the outcrop belt in eastern West Virginia. However, the correlation of these units with the sequence of subsurface driller's sandstones is poorly known. Furthermore, little is known concerning the relationships of the well-developed Lower Mississippian hydrocarbon-bearing strata of southern West Virginia with equivalent units to the north. Regional analysis of over 700 gamma-ray well logs, combined with study of outcrops at Rowlesburg and Caldwell, West Virginia, provides insight into the nature of the Cloyd conglomerate, and the Berea, Weir, Squaw, and Big Injun sandstones and allows the refinement of the stratigraphic succession of the Price Formation in southern West Virginia. New members listed herein are as of yet information, pending publication of description of type sections from the Caldwell outcrop.

  3. The whistler mode refractive index as a function of gyrofrequency

    SciTech Connect (OSTI)

    Albert, J. M.

    2011-08-15

    The refractive index for a constant-frequency whistler mode wave in an electron-proton plasma is considered as a function of position, through the local gyrofrequencies {Omega}{sub e,i}. The full cold plasma dispersion relation is used. The wave frequency can take any value up to the smaller of {Omega}{sub e} and the plasma frequency {omega}{sub pe}, but {omega}{sub pe} is allowed to take any fixed value, as is the wavenormal angle. It is rigorously established that the refractive index is a decreasing function of {Omega}{sub e}. One application of this is to finding locations of Landau and cyclotron resonances, to evaluate the effects of whistler mode waves on radiation belt electrons.

  4. Radioisotope thermoelectric generator reliability and safety

    SciTech Connect (OSTI)

    Campbell, R.; Klein, J.

    1989-01-01

    There are numerous occasions when a planetary mission requires energy in remote areas of the solar system. Anytime power is required much beyond Mars or the Asteroid Belts, solar power is not an option. The radioisotope thermoelectric generator (RTG) was developed for such a mission requirement. It is a relatively small and lightweight power source that can produce power under adverse conditions. Just this type of source has become the backbone of the power system for far outer plant exploration. Voyagers I and II are utilizing RTGs, which will soon power the Galileo spacecraft to Jupiter and the Ulysses spacecraft to study the solar poles. The paper discusses RTG operation including thermoelectric design, converter design, general-purpose heat source; RTG reliability including design, testing, experience, and launch approval; and RTG safety issues and methods of ensuring safety.

  5. Constraints on the Formation Age of Cometary Material from the NASA Stardust Mission

    SciTech Connect (OSTI)

    Matzel, J; Ishii, H; Joswiak, D; Hutcheon, I; Bradley, J; Brownlee, D; Weber, P K; Teslich, N; Matrajt, G; McKeegan, K; MacPherson, G

    2009-11-13

    We measured the {sup 26}Al-{sup 26}Mg isotope systematics of a {approx} 5-micrometer refractory particle, Coki, returned from comet 81P/Wild 2 in order to relate the time scales of formation of cometary inclusions to their meteoritic counterparts. The data show no evidence of radiogenic {sup 26}Mg and define an upper limit to the abundance of {sup 26}Al at the time of particle formation: {sup 26}Al/{sup 27}Al < 1 x 10-5. The absence of {sup 26}Al indicates that Coki formed >1.7 million years after the oldest solids in the solar system, calcium- and aluminum-rich inclusions (CAIs). The data suggest that high-temperature inner solar system material formed, was subsequently transferred to the Kuiper Belt, and was incorporated into comets several million years after CAI formation.

  6. The Taiwanese-American occultation survey project stellar variability. III. Detection of 58 new variable stars

    SciTech Connect (OSTI)

    Ishioka, R.; Wang, S.-Y.; Zhang, Z.-W.; Lehner, M. J.; Cook, K. H.; King, S.-K.; Lee, T.; Marshall, S. L.; Schwamb, M. E.; Wang, J.-H.; Wen, C.-Y.; Alcock, C.; Protopapas, P.; Axelrod, T.; Bianco, F. B.; Byun, Y.-I.; Chen, W. P.; Ngeow, C.-C.; Kim, D.-W.; Rice, J. A.

    2014-04-01

    The Taiwanese-American Occultation Survey project is designed for the detection of stellar occultations by small-size Kuiper Belt Objects, and it has monitored selected fields along the ecliptic plane by using four telescopes with a 3 deg{sup 2} field of view on the sky since 2005. We have analyzed data accumulated during 2005-2012 to detect variable stars. Sixteen fields with observations of more than 100 epochs were examined. We recovered 85 variables among a total of 158 known variable stars in these 16 fields. Most of the unrecovered variables are located in the fields observed less frequently. We also detected 58 variable stars which are not listed in the International Variable Star Index of the American Association of Variable Star Observers. These variable stars are classified as 3 RR Lyrae, 4 Cepheid, 1 ? Scuti, 5 Mira, 15 semi-regular, and 27 eclipsing binaries based on the periodicity and the profile of the light curves.

  7. A map of the universe

    SciTech Connect (OSTI)

    Gott III, J. Richard; Juric, Mario; Schlegel, David; Hoyle, Fiona; Vogeley, Michael; Tegmark, Max; Bahcall, Neta; Brinkmann, Jon

    2003-10-20

    We have produced a new conformal map of the universe illustrating recent discoveries, ranging from Kuiper belt objects in the Solar system, to the galaxies and quasars from the Sloan Digital Sky Survey. This map projection, based on the logarithm map of the complex plane, preserves shapes locally, and yet is able to display the entire range of astronomical scales from the Earth s neighborhood to the cosmic microwave background. The conformal nature of the projection, preserving shapes locally, may be of particular use for analyzing large scale structure. Prominent in the map is a Sloan Great Wall of galaxies 1.37 billion light years long, 80 percent longer than the Great Wall discovered by Geller and Huchra and therefore the largest observed structure in the universe.

  8. Large-area Silicon-Film{trademark} panels and solar cells. Final technical report, July 1995--March 1998

    SciTech Connect (OSTI)

    Rand, J.A.; Bai, Y.; Barnett, A.M.; Culik, J.S.; Ford, D.H.; Hall, R.B.; Kendall, C.L.

    1998-09-01

    This report will detail substantial improvements in each of the task areas. A number of new products were developed, including a 130 kW array built using a new panel design. Improvements in laboratory-scale solar cell processing resulted in a confirmed efficiency of 16.6%. A new Silicon-Film{trademark} production sheet machine was built which increased throughput by 70%. Three solar cell fabrication processes were converted from low throughout batch processes to high throughput, continuous, belt processes. These new processes are capable of processing sheet over 31 cm in width. Finally, a new Silicon-Film{trademark} sheet machine was built that demonstrated a sheet width of 38 cm. This tool enabled AstroPower to demonstrate a wide range of solar cell sizes, many of which have generated considerable market interest.

  9. Eddy-current-damped microelectromechanical switch

    DOE Patents [OSTI]

    Christenson, Todd R.; Polosky, Marc A.

    2009-12-15

    A microelectromechanical (MEM) device is disclosed that includes a shuttle suspended for movement above a substrate. A plurality of permanent magnets in the shuttle of the MEM device interact with a metal plate which forms the substrate or a metal portion thereof to provide an eddy-current damping of the shuttle, thereby making the shuttle responsive to changes in acceleration or velocity of the MEM device. Alternately, the permanent magnets can be located in the substrate, and the metal portion can form the shuttle. An electrical switch closure in the MEM device can occur in response to a predetermined acceleration-time event. The MEM device, which can be fabricated either by micromachining or LIGA, can be used for sensing an acceleration or deceleration event (e.g. in automotive applications such as airbag deployment or seat belt retraction).

  10. Eddy-current-damped microelectromechanical switch

    DOE Patents [OSTI]

    Christenson, Todd R.; Polosky, Marc A.

    2007-10-30

    A microelectromechanical (MEM) device is disclosed that includes a shuttle suspended for movement above a substrate. A plurality of permanent magnets in the shuttle of the MEM device interact with a metal plate which forms the substrate or a metal portion thereof to provide an eddy-current damping of the shuttle, thereby making the shuttle responsive to changes in acceleration or velocity of the MEM device. Alternately, the permanent magnets can be located in the substrate, and the metal portion can form the shuttle. An electrical switch closure in the MEM device can occur in response to a predetermined acceleration-time event. The MEM device, which can be fabricated either by micromachining or LIGA, can be used for sensing an acceleration or deceleration event (e.g. in automotive applications such as airbag deployment or seat belt retraction).

  11. Identification of tribological research and development needs for lubrication of advanced heat engines

    SciTech Connect (OSTI)

    Fehrenbacher, L.L.; Levinson, T.M.

    1985-09-01

    The continuous evolution of higher power density propulsion systems has always fueled the search for materials and lubricants with improved thermal and/or durability characteristics. Tribology of the upper cylinder region is the major technology roadblock in the path of the adiabatic diesel engine which has an energy reduction potential that exceeds that of all other engine development types. This tribology assessment resulted in the following major conclusions: a low friction and a low wear seal between the ring belt and cylinder bore are the most critical tribology functions in the diesel combustion chamber; development of solid lubrication systems will not satisfy the simultaneous low friction and low wear requirements in the upper cylinder area; development of separate upper cylinder liquid lubrication systems offers the most attractive design alternative for meeting the operational goals of future ''minimum cooled'' diesel engines.

  12. Reservoir characterization of the Smackover Formation in southwest Alabama

    SciTech Connect (OSTI)

    Kopaska-Merkel, D.C.; Hall, D.R.; Mann, S.D.; Tew, B.H.

    1993-02-01

    The Upper Jurassic Smackover Formation is found in an arcuate belt in the subsurface from south Texas to panhandle Florida. The Smackover is the most prolific hydrocarbon-producing formation in Alabama and is an important hydrocarbon reservoir from Florida to Texas. In this report Smackover hydrocarbon reservoirs in southwest Alabama are described. Also, the nine enhanced- and improved-recovery projects that have been undertaken in the Smackover of Alabama are evaluated. The report concludes with recommendations about potential future enhanced- and improved-recovery projects in Smackover reservoirs in Alabama and an estimate of the potential volume of liquid hydrocarbons recoverable by enhanced- and improved-recovery methods from the Smackover of Alabama.

  13. Gamma-ray burst data from DMSP satellites

    SciTech Connect (OSTI)

    Terrell, J.; Klebesadel, R.W.; Lee, P. ); Griffee, J.W. )

    1991-01-01

    A number of gamma-ray bursts have been detected by means of gamma-ray detectors aboard three Air Force Defense Meteorological Satellite Program (DMSP) satellites, in polar orbits at 800 km altitude. The gamma-ray data have a 2-second resolving time, and are usually telemetered in 5 energy bins in the range 50--1000 keV. Although it is not possible to detect gamma-ray bursts when the DMSP satellites are passing through the radiation belt or the South Atlantic Anomaly, or when the source is obscured by the Earth, a number of gamma-ray bursts have been detected by two or even three of the satellites. The DMSP data may be of considerable, assistance in evaluating time histories, locations, and spectra of gamma-ray bursts.

  14. Gamma-ray burst data from DMSP satellites

    SciTech Connect (OSTI)

    Terrell, J.; Klebesadel, R.W.; Lee, P.; Griffee, J.W.

    1991-12-31

    A number of gamma-ray bursts have been detected by means of gamma-ray detectors aboard three Air Force Defense Meteorological Satellite Program (DMSP) satellites, in polar orbits at 800 km altitude. The gamma-ray data have a 2-second resolving time, and are usually telemetered in 5 energy bins in the range 50--1000 keV. Although it is not possible to detect gamma-ray bursts when the DMSP satellites are passing through the radiation belt or the South Atlantic Anomaly, or when the source is obscured by the Earth, a number of gamma-ray bursts have been detected by two or even three of the satellites. The DMSP data may be of considerable, assistance in evaluating time histories, locations, and spectra of gamma-ray bursts.

  15. Time varying arctic climate change amplification

    SciTech Connect (OSTI)

    Chylek, Petr [Los Alamos National Laboratory; Dubey, Manvendra K [Los Alamos National Laboratory; Lesins, Glen [DALLHOUSIE U; Wang, Muyin [NOAA/JISAO

    2009-01-01

    During the past 130 years the global mean surface air temperature has risen by about 0.75 K. Due to feedbacks -- including the snow/ice albedo feedback -- the warming in the Arctic is expected to proceed at a faster rate than the global average. Climate model simulations suggest that this Arctic amplification produces warming that is two to three times larger than the global mean. Understanding the Arctic amplification is essential for projections of future Arctic climate including sea ice extent and melting of the Greenland ice sheet. We use the temperature records from the Arctic stations to show that (a) the Arctic amplification is larger at latitudes above 700 N compared to those within 64-70oN belt, and that, surprisingly; (b) the ratio of the Arctic to global rate of temperature change is not constant but varies on the decadal timescale. This time dependence will affect future projections of climate changes in the Arctic.

  16. The radiation protection problems of high altitude and space flight

    SciTech Connect (OSTI)

    Fry, R.J.M.

    1993-04-01

    This paper considers the radiation environment in aircraft at high altitudes and spacecraft in low earth orbit and in deep space and the factors that influence the dose equivalents. Altitude, latitude and solar cycle are the major influences for flights below the radiation belts. In deep space, solar cycle and the occurrence of solar particle events are the factors of influence. The major radiation effects of concern are cancer and infertility in males. In high altitude aircraft the radiation consists mainly of protons and neutrons, with neutrons contributing about half the equivalent dose. The average dose rate at altitudes of transcontinental flights that approach the polar regions are greater by a factor of about 2.5 than on routes at low latitudes. Current estimates of does to air crews suggest they are well within the ICRP (1990) recommended dose limits for radiation workers.

  17. The radiation protection problems of high altitude and space flight

    SciTech Connect (OSTI)

    Fry, R.J.M.

    1993-01-01

    This paper considers the radiation environment in aircraft at high altitudes and spacecraft in low earth orbit and in deep space and the factors that influence the dose equivalents. Altitude, latitude and solar cycle are the major influences for flights below the radiation belts. In deep space, solar cycle and the occurrence of solar particle events are the factors of influence. The major radiation effects of concern are cancer and infertility in males. In high altitude aircraft the radiation consists mainly of protons and neutrons, with neutrons contributing about half the equivalent dose. The average dose rate at altitudes of transcontinental flights that approach the polar regions are greater by a factor of about 2.5 than on routes at low latitudes. Current estimates of does to air crews suggest they are well within the ICRP (1990) recommended dose limits for radiation workers.

  18. Internal wave energy radiated from a turbulent mixed layer

    SciTech Connect (OSTI)

    Munroe, James R.; Sutherland, Bruce R.

    2014-09-15

    We examine mixed-layer deepening and the generation of internal waves in stratified fluid resulting from turbulence that develops in response to an applied surface stress. In laboratory experiments the stress is applied over the breadth of a finite-length tank by a moving roughened conveyor belt. The turbulence in the shear layer is characterized using particle image velocimetry to measure the kinetic energy density. The internal waves are measured using synthetic schlieren to determine their amplitudes, frequencies, and energy density. We also perform fully nonlinear numerical simulations restricted to two dimensions but in a horizontally periodic domain. These clearly demonstrate that internal waves are generated by transient eddies at the integral length scale of turbulence and which translate with the background shear along the base of the mixed layer. In both experiments and simulations we find that the energy density of the generated waves is 1%3% of the turbulent kinetic energy density of the turbulent layer.

  19. Analysis of stream sediment reconnaissance data for mineral resources from the Montrose NTMS Quadrangle, Colorado

    SciTech Connect (OSTI)

    Beyth, M.; Broxton, D.; McInteer, C.; Averett, W.R.; Stablein, N.K.

    1980-06-01

    Multivariate statistical analysis to support the National Uranium Resource Evaluation and to evaluate strategic and other commercially important mineral resources was carried out on Hydrogeochemical and Stream Sediment Reconnaissance data from the Montrose quadrangle, Colorado. The analysis suggests that: (1) the southern Colorado Mineral Belt is an area favorable for uranium mineral occurrences; (2) carnotite-type occurrences are likely in the nose of the Gunnison Uplift; (3) uranium mineral occurrences may be present along the western and northern margins of the West Elk crater; (4) a base-metal mineralized area is associated with the Uncompahgre Uplift; and (5) uranium and base metals are associated in some areas, and both are often controlled by faults trending west-northwest and north.

  20. Modeling radiation loads to detectors in a SNAP mission

    SciTech Connect (OSTI)

    Nikolai V. Mokhov et al.

    2004-05-12

    In order to investigate degradation of optical detectors of the Supernova Acceleration Project (SNAP) space mission due to irradiation, a three-dimensional model of the satellite has been developed. Realistic radiation environment at the satellite orbit, including both galactic and trapped in radiation belts cosmic rays, has been taken into account. The modeling has been performed with the MARS14 Monte Carlo code. In a current design, the main contribution to dose accumulated in the photodetectors is shown to be due to trapped protons. A contribution of primary {alpha}-particles is estimated. Predicted performance degradation for the photo-detector for a 4-year space mission is 40% and can be reduced further by means of shielding optimization.

  1. Sludge treating apparatus

    SciTech Connect (OSTI)

    Fujimoto, T.; Kawasugi, T.

    1983-06-14

    A sludge treating apparatus comprises a centrifugal condensing machine for forcedly condensing a raw sludge produced by a waste water treating apparatus. The raw sludge condensed to approximately 94 to 90% in terms of the percentage of moisture content by means of the centrifugal condensing machine is introduced into an anaerobic digestion tank of a deep well type, where the raw sludge undergoes an anaerobic digestion, and a digested sludge obtained from the anaerobic digestion tank is then dewatered by means of a dewatering apparatus such as a belt press, whereupon the dewatered sludge is applied to a post-treatment apparatus. In execution of the anaerobic digestion process, the reactions corresponding to an acid fermentation stage and acid regression stage may be carried out in advance in separate tanks and the reaction corresponding to an alkaline fermentation stage may be mainly performed in an anaerobic digestion tank.

  2. PRB mines mature

    SciTech Connect (OSTI)

    Buchsbaum, L.

    2007-08-15

    Already seeing the results of reclamation efforts, America's largest surface mines advance as engineers prepare for the future. 30 years after the signing of the Surface Mining Control and Reclamation Act by Jimmy Carter, western strip mines in the USA, especially in the Powder River Basin, are producing more coal than ever. The article describes the construction and installation of a $38.5 million near-pit crusher and overland belt conveyor system at Foundation Coal West's (FCW) Belle Ayr surface mine in Wyoming, one of the earliest PRB mines. It goes on to describe the development by Rio Tinto of an elk conservatory, the Rochelle Hill Conservation Easement, on reclaimed land at Jacobs Ranch, adjacent to the Rochelle Hills. 4 photos.

  3. BWR Vessel and Internals Project Removal and Analysis of Material Samples from Core Shroud and Top Guide at Susquehanna Unit 2

    SciTech Connect (OSTI)

    Howell, D; Haertel, T; Lindberg, J; Oliver, B; Greenwood, L

    2005-04-15

    Fast and thermal fluence were determined by a laboratory analysis of the samples. Fluence in the upper regions of the shroud (between the H1 and H2 welds) was substantially lower than that in the belt line region (near the H4 weld). Fluence in the top guide was significantly higher than fluence on the core shroud. As expected, helium concentrations were highest in regions where fluence was highest. Estimates of the initial boron concentration were similar to measurements made on materials removed from other reactors. A technical justification evaluated the acceptability of the sampling process with respect to structural consequences of material removal and to increased cracking susceptibility due to the as-left condition. It was determined that the sampling process was acceptable on both counts.

  4. Science Plan Biogenic Aerosols – Effects on Clouds and Climate (BAECC)

    SciTech Connect (OSTI)

    Petäjä, T

    2013-12-01

    Atmospheric aerosol particles impact human health in urban environments, while on regional and global scales they can affect climate patterns, the hydrological cycle, and the intensity of radiation that reaches the Earth’s surface. In spite of recent advances in the understanding of aerosol formation processes and the links between aerosol dynamics and biosphere-atmosphere-climate interactions, great challenges remain in the analysis of related processes on a global scale. Boreal forests, situated in a circumpolar belt in the northern latitudes throughout the United States, Canada, Russia and Scandinavia, are among the most active areas of atmospheric aerosol formation among all biomes. The formation of aerosol particles and their growth to the sizes of cloud condensation nuclei in these areas are associated with biogenic volatile organic emissions from vegetation and soil.

  5. THE LOST SIBLINGS OF THE SUN

    SciTech Connect (OSTI)

    Portegies Zwart, Simon F.

    2009-05-01

    The anomalous chemical abundances and the structure of the Edgeworth-Kuiper belt observed in the solar system constrain the initial mass and radius of the star cluster in which the Sun was born to M {approx_equal} 500-3000M {sub sun} and R {approx_equal} 1-3 pc. When the cluster dissolved, the siblings of the Sun dispersed through the galaxy, but they remained on a similar orbit around the Galactic center. Today these stars hide among the field stars, but 10-60 of them are still present within a distance of {approx}100 pc. These siblings of the Sun can be identified by accurate measurements of their chemical abundances, positions, and their velocities. Finding even a few will strongly constrain the parameters of the parental star cluster and the location in the Galaxy where we were born.

  6. Oil and gas occurrences vs. geodynamic evolution in the southern Apennines (Italy)

    SciTech Connect (OSTI)

    Casero, P. ); Roure, F.; Vially, R. ); Sarp, A.R.

    1990-05-01

    The present architecture of the southern Apennines results from the Neogene continental subduction of the Apulia margin (part of North Africa margin). An allochthonous complex is formed by the low-angle, large-scale, east-vergent tectonic stack of Triassic to upper Miocene (Messinian) units. The rocks represent both a shelf carbonate domain (Apennine platform) and a deep marine domain (Lagonegro-Molise basin). They are emplaced as a nappe during uppermost Miocene (Messinian) to lowermost Pliocene. They are transported to the northeast onto the flexed inner part of the Apulia platform (Mesozoic to late Miocene shelf carbonate series). During the middle-upper Pliocene, the inner Apulia carbonate margin (intermediate platform) was thrust against the outer Apulia domain (overthrust belt). Pliocene-Quaternary syntectonic clastic series were deposited in the flexural basin developed to the east of the Apenninic, allochthon outer ramp and also in piggyback basins carried on top of the allochthon. Oil occurrences are confined to the top of the platform carbonates. Discoveries have been made in (1) compressional structures of the overthrust belt (outer margin of the inner Apulian Platform), (2) late-stage compressive folds in the outer slope of the foredeep, and (3) slightly inverted structures of the foreland margin. Gas accumulations at the top of platform limestones occur only in antithetic fault block traps or in slightly inverted structures of the foreland. The most important and frequent biogenic accumulations are in clastic rocks of the foredeep, beneath and to the east of the frontal ramp of the allochthon.

  7. Dust control technology for longwall mining. Technical progress report, No. 36, July 1-31, 1984

    SciTech Connect (OSTI)

    Ruggieri, S.K.

    1984-08-21

    Preliminary analysis of the data from the Emery Wilberg Mine evaluation showed that the intake dust level and ventilation conditions were virtually constant throughout the evaluation. These factors coupled with the consistent cutting sequence of the shearer appear to have resulted in very reliable data. The evaluation examined four major test conditions: open stageloader with baseline sprays (10 gpm); open stageloader with all spraybars operating (20 gpm); covered stageloader with baseline sprays (10 gpm); and covered stageloader with all spraybars operating (20 gpm). Data was recorded during both the cutting and clean-up passes. Very little dust was generated during the clean-up pass. Any dust reductions due to improved conditions were difficult to detect because of low dust levels. During the cutting pass, dust levels were considerably higher and the improvements were quite obvious. With an open stageloader the changes from baseline conditions to that of all spray systems operating produced dust reductions of up to 50 percent within the headgate and a 30 percent improvement at shield number 20. Under baseline operating conditions, the dust levels produced with an open stageloader were compared with the levels produced with the stageloader covered. The results showed a significant improvement in the discharge region of the crusher, with 40 percent improvements at the headgate operator and shield number 20. It appears that covering the stageloader provides the largest reduction in dust levels. The application of additional water to the spraybars produced further improvements. Reductions in belt entry dust levels were directly related to the amount of water applied to the stageloader to belt transfer point spraybar.

  8. Major Oil Plays In Utah And Vicinity

    SciTech Connect (OSTI)

    Thomas Chidsey

    2007-12-31

    Utah oil fields have produced over 1.33 billion barrels (211 million m{sup 3}) of oil and hold 256 million barrels (40.7 million m{sup 3}) of proved reserves. The 13.7 million barrels (2.2 million m3) of production in 2002 was the lowest level in over 40 years and continued the steady decline that began in the mid-1980s. However, in late 2005 oil production increased, due, in part, to the discovery of Covenant field in the central Utah Navajo Sandstone thrust belt ('Hingeline') play, and to increased development drilling in the central Uinta Basin, reversing the decline that began in the mid-1980s. The Utah Geological Survey believes providing play portfolios for the major oil-producing provinces (Paradox Basin, Uinta Basin, and thrust belt) in Utah and adjacent areas in Colorado and Wyoming can continue this new upward production trend. Oil plays are geographic areas with petroleum potential caused by favorable combinations of source rock, migration paths, reservoir rock characteristics, and other factors. The play portfolios include descriptions and maps of the major oil plays by reservoir; production and reservoir data; case-study field evaluations; locations of major oil pipelines; identification and discussion of land-use constraints; descriptions of reservoir outcrop analogs; and summaries of the state-of-the-art drilling, completion, and secondary/tertiary recovery techniques for each play. The most prolific oil reservoir in the Utah/Wyoming thrust belt province is the eolian, Jurassic Nugget Sandstone, having produced over 288 million barrels (46 million m{sup 3}) of oil and 5.1 trillion cubic feet (145 billion m{sup 3}) of gas. Traps form on discrete subsidiary closures along major ramp anticlines where the depositionally heterogeneous Nugget is also extensively fractured. Hydrocarbons in Nugget reservoirs were generated from subthrust Cretaceous source rocks. The seals for the producing horizons are overlying argillaceous and gypsiferous beds in the Jurassic Twin Creek Limestone, or a low-permeability zone at the top of the Nugget. The Nugget Sandstone thrust belt play is divided into three subplays: (1) Absaroka thrust - Mesozoic-cored shallow structures, (2) Absaroka thrust - Mesozoic-cored deep structures, and (3) Absaroka thrust - Paleozoic-cored shallow structures. Both of the Mesozoic-cored structures subplays represent a linear, hanging wall, ramp anticline parallel to the leading edge of the Absaroka thrust. Fields in the shallow Mesozoic subplay produce crude oil and associated gas; fields in the deep subplay produce retrograde condensate. The Paleozoic-cored structures subplay is located immediately west of the Mesozoic-cored structures subplays. It represents a very continuous and linear, hanging wall, ramp anticline where the Nugget is truncated against a thrust splay. Fields in this subplay produce nonassociated gas and condensate. Traps in these subplays consist of long, narrow, doubly plunging anticlines. Prospective drilling targets are delineated using high-quality, two-dimensional and three-dimensional seismic data, forward modeling/visualization tools, and other state-of-the-art techniques. Future Nugget Sandstone exploration could focus on more structurally complex and subtle, thrust-related traps. Nugget structures may be present beneath the leading edge of the Hogsback thrust and North Flank fault of the Uinta uplift. The Jurassic Twin Creek Limestone play in the Utah/Wyoming thrust belt province has produced over 15 million barrels (2.4 million m{sup 3}) of oil and 93 billion cubic feet (2.6 billion m{sup 3}) of gas. Traps form on discrete subsidiary closures along major ramp anticlines where the low-porosity Twin Creek is extensively fractured. Hydrocarbons in Twin Creek reservoirs were generated from subthrust Cretaceous source rocks. The seals for the producing horizons are overlying argillaceous and clastic beds, and non-fractured units within the Twin Creek. The Twin Creek Limestone thrust belt play is divided into two subplays: (1) Absaroka thrust-Mesozoic-cored structures and (2) Absaroka thrust - Paleozoic-cored structures. The Mesozoic-cored structures subplay represents a linear, hanging wall, ramp anticline parallel to the leading edge of the Absaroka thrust. Fields in this subplay produce crude oil and associated gas. The Paleozoic-cored structures subplay is located immediately west of the Mesozoic-cored structures subplay. It represents a very continuous and linear, hanging wall, ramp anticline where the Twin Creek is truncated against a thrust splay. Fields in this subplay produce nonassociated gas and condensate. Traps in both subplays consist of long, narrow, doubly plunging anticlines.

  9. Major Oil Plays in Utah and Vicinity

    SciTech Connect (OSTI)

    Thomas C. Chidsey; Craig D. Morgan; Kevin McClure; Douglas A. Sprinkel; Roger L. Bon; Hellmut H. Doelling

    2003-12-31

    Utah oil fields have produced over 1.2 billion barrels (191 million m{sup 3}). However, the 13.7 million barrels (2.2 million m{sup 3}) of production in 2002 was the lowest level in over 40 years and continued the steady decline that began in the mid-1980s. The Utah Geological Survey believes this trend can be reversed by providing play portfolios for the major oil-producing provinces (Paradox Basin, Uinta Basin, and thrust belt) in Utah and adjacent areas in Colorado and Wyoming. Oil plays are geographic areas with petroleum potential caused by favorable combinations of source rock, migration paths, reservoir rock characteristics, and other factors. The play portfolios will include: descriptions and maps of the major oil plays by reservoir; production and reservoir data; case-study field evaluations; locations of major oil pipelines; identification and discussion of land-use constraints; descriptions of reservoir outcrop analogs; and summaries of the state-of-the-art drilling, completion, and secondary/tertiary techniques for each play. This report covers research activities for the sixth quarter of the project (October 1 through December 31, 2003). This work included describing outcrop analogs for the Jurassic Twin Creek Limestone and Mississippian Leadville Limestone, major oil producers in the thrust belt and Paradox Basin, respectively, and analyzing best practices used in the southern Green River Formation play of the Uinta Basin. Production-scale outcrop analogs provide an excellent view of reservoir petrophysics, facies characteristics, and boundaries contributing to the overall heterogeneity of reservoir rocks. They can be used as a ''template'' for evaluation of data from conventional core, geophysical and petrophysical logs, and seismic surveys. In the Utah/Wyoming thrust belt province, the Jurassic Twin Creek Limestone produces from subsidiary closures along major ramp anticlines where the low-porosity limestone beds are extensively fractured and sealed by overlying argillaceous and non-fractured units. The best outcrop analogs for Twin Creek reservoirs are found at Devils Slide and near the town of Peoa, Utah, where fractures in dense, homogeneous non-porous limestone beds are in contact with the basal siltstone units (containing sealed fractures) of the overlying units. The shallow marine, Mississippian Leadville Limestone is a major oil and gas reservoir in the Paradox Basin of Utah and Colorado. Hydrocarbons are produced from basement-involved, northwest-trending structural traps with closure on both anticlines and faults. Excellent outcrops of Leadville-equivalent rocks are found along the south flank of the Uinta Mountains, Utah. For example, like the Leadville, the Mississippian Madison Limestone contains zones of solution breccia, fractures, and facies variations. When combined with subsurface geological and production data, these outcrop analogs can improve (1) development drilling and production strategies such as horizontal drilling, (2) reservoir-simulation models, (3) reserve calculations, and (4) design and implementation of secondary/tertiary oil recovery programs and other best practices used in the oil fields of Utah and vicinity. In the southern Green River Formation play of the Uinta Basin, optimal drilling, development, and production practices consist of: (1) owning drilling rigs and frac holding tanks; (2) perforating sandstone beds with more than 8 percent neutron porosity and stimulate with separate fracture treatments; (3) placing completed wells on primary production using artificial lift; (4) converting wells relatively soon to secondary waterflooding maintaining reservoir pressure above the bubble point to maximize oil recovery; (5) developing waterflood units using an alternating injector--producer pattern on 40-acre (16-ha) spacing; and (6) recompleting producing wells by perforating all beds that are productive in the waterflood unit. As part of technology transfer activities during this quarter, an abstract describing outcrop reservoir analogs was accepted by the American Assoc

  10. Probing for exoplanets hiding in dusty debris disks: Disk imaging, characterization, and exploration with HST/STIS multi-roll coronagraphy

    SciTech Connect (OSTI)

    Schneider, Glenn; Hinz, Phillip M.; Grady, Carol A.; Hines, Dean C.; Debes, John H.; Perrin, Marshall D.; Moro-Martin, Amaya; Stark, Christopher C.; Kuchner, Marc J.; Woodgate, Bruce E.; Weinberger, Alycia J.; Rodigas, Timothy J.; Wisniewski, John P.; Silverstone, Murray D.; Jang-Condell, Hannah; Henning, Thomas; Serabyn, Eugene; Tamura, Motohide

    2014-10-01

    Spatially resolved scattered-light images of circumstellar debris in exoplanetary systems constrain the physical properties and orbits of the dust particles in these systems. They also inform on co-orbiting (but unseen) planets, the systemic architectures, and forces perturbing the starlight-scattering circumstellar material. Using Hubble Space Telescope (HST)/Space Telescope Imaging Spectrograph (STIS) broadband optical coronagraphy, we have completed the observational phase of a program to study the spatial distribution of dust in a sample of 10 circumstellar debris systems and 1 'mature' protoplanetrary disk, all with HST pedigree, using point-spread-function-subtracted multi-roll coronagraphy. These observations probe stellocentric distances ?5 AU for the nearest systems, and simultaneously resolve disk substructures well beyond corresponding to the giant planet and Kuiper Belt regions within our own solar system. They also disclose diffuse very low-surface-brightness dust at larger stellocentric distances. Herein we present new results inclusive of fainter disks such as HD 92945 (F {sub disk}/F {sub star} = 5 10{sup 5}), confirming, and better revealing, the existence of a narrow inner debris ring within a larger diffuse dust disk. Other disks with ring-like substructures and significant asymmetries and complex morphologies include HD 181327, for which we posit a spray of ejecta from a recent massive collision in an exo-Kuiper Belt; HD 61005, suggested to be interacting with the local interstellar medium; and HD 15115 and HD 32297, also discussed in the context of putative environmental interactions. These disks and HD 15745 suggest that debris system evolution cannot be treated in isolation. For AU Mic's edge-on disk, we find out-of-plane surface brightness asymmetries at ?5 AU that may implicate the existence of one or more planetary perturbers. Time-resolved images of the MP Mus protoplanetary disk provide spatially resolved temporal variability in the disk illumination. These and other new images from our HST/STIS GO/12228 program enable direct inter-comparison of the architectures of these exoplanetary debris systems in the context of our own solar system.

  11. U.S. Department of Energy Office of Legacy Management Legacy Uranium Mine Site Reclamation - Lessons Learned - 12384

    SciTech Connect (OSTI)

    Kilpatrick, Laura E.; Cotter, Ed

    2012-07-01

    The U.S. Department of Energy (DOE) Office of Legacy Management is responsible for administering the DOE Uranium Leasing Program (ULP) and its 31 uranium lease tracts located in the Uravan Mineral Belt of southwestern Colorado (see Figure 1). In addition to administering the ULP for the last six decades, DOE has also undertaken the significant task of reclaiming a large number of abandoned uranium (legacy) mine sites and associated features located throughout the Uravan Mineral Belt. In 1995, DOE initiated a 3-year reconnaissance program to locate and delineate (through extensive on-the-ground mapping) the legacy mine sites and associated features contained within the historically defined boundaries of its uranium lease tracts. During that same time frame, DOE recognized the lack of regulations pertaining to the reclamation of legacy mine sites and contacted the U.S. Bureau of Land Management (BLM) concerning the reclamation of legacy mine sites. In November 1995, The BLM Colorado State Office formally issued the United States Department of the Interior, Colorado Bureau of Land Management, Closure/Reclamation Guidelines, Abandoned Uranium Mine Sites as a supplement to its Solid Minerals Reclamation Handbook (H-3042-1). Over the next five-and-one-half years, DOE reclaimed the 161 legacy mine sites that had been identified on DOE withdrawn lands. By the late 1990's, the various BLM field offices in southwestern Colorado began to recognize DOE's experience and expertise in reclaiming legacy mine sites. During the ensuing 8 years, BLM funded DOE (through a series of task orders) to perform reclamation activities at 182 BLM mine sites. To date, DOE has reclaimed 372 separate and distinct legacy mine sites. During this process, DOE has learned many lessons and is willing to share those lessons with others in the reclamation industry because there are still many legacy mine sites not yet reclaimed. DOE currently administers 31 lease tracts (11,017 ha) that collectively contain over 220 legacy (abandoned) uranium mine sites. This contrasts to the millions of hectares administered by the BLM, the U.S. Forest Service, and other federal, tribal, and state agencies that contain thousands of such sites. DOE believes that the processes it has used provide a practical and cost-effective approach to abandoned uranium mine-site reclamation. Although the Federal Acquisition Regulations preclude DOE from competing with private industry, DOE is available to assist other governmental and tribal agencies in their reclamation efforts. (authors)

  12. Low cost supplemental, wind-heating for rural buildings. Final report, 1 October 1981-31 September 1983

    SciTech Connect (OSTI)

    Not Available

    1983-11-14

    To obtain the supplemental electric heat, a cheap electric generator or alternator is needed to provide the electricity. Used or rebuilt car alternators are plentiful and relatively cheap. A car alternator requires at least a thousand rpm to operate, but the windmill rotor turns much slower. To obtain the necessary rpm's a 26 inch bicycle wheel, as a pulley for a V-belt, was mounted to the bottom of the rotor. The wheel drove a 4 inch pulley mounted to an 8 inch pulley. The 8 inch then drove the alternator by a second V-belt for a net speed step up of 13:1. The dc for the alternator field came from a 12 V bicycle generator and a full wave bridge. When done right, the bicycle generator does not excite the field until there is sufficient wind (and not before, which would stall-out the rotor). A windmill and car alternator system is basically unstable. The system is always overshooting or undershooting that stable rpm which would match wind speed to rotor rpm to alternator rpm, so that wind energy input just matches electrical heat energy output. The first techniques used to gain stability is shown in Figure 3. It essentially used three separate stages of either type I or II to switch in resistive loads in successive stages. For example, at low wind speeds, the alternator voltage would be low and none of the stages would turn on. As wind speed increased the alternator voltage would increase with the result that the first stage would turn on providing heat. The most successful circuit is shown in Figure 4. It had the advantages of: identical stages using commonly and easily attainable parts; in the field it was very easy to determine and adjust the cut-in threshold of each stage; the diodes not only acted as a heating load themselves; but the diodes also provided automatic overspeed braking by ''short circuiting'' the alternator which causes a steep increase in alternator drag.

  13. RELATIVISTIC (E > 0.6, > 2.0, AND > 4.0 MeV) ELECTRON ACCELERATION AT GEOSYNCHRONOUS ORBIT DURING HIGH-INTENSITY, LONG-DURATION, CONTINUOUS AE ACTIVITY (HILDCAA) EVENTS

    SciTech Connect (OSTI)

    Hajra, Rajkumar; Echer, Ezequiel; Gonzalez, Walter D.; Tsurutani, Bruce T.; Santolik, Ondrej

    2015-01-20

    Radiation-belt relativistic (E > 0.6, > 2.0, and > 4.0MeV) electron acceleration is studied for solar cycle 23 (1995-2008). High-intensity, long-duration, continuous AE activity (HILDCAA) events are considered as the basis of the analyses. All of the 35 HILDCAA events under study were found to be characterized by flux enhancements of magnetospheric relativistic electrons of all three energies compared to the pre-event flux levels. For the E > 2.0MeV electron fluxes, enhancement of >50% occurred during 100% of HILDCAAs. Cluster-4 passes were examined for electromagnetic chorus waves in the 5 < L < 10 and 0 < MLT < 12 region when wave data were available. Fully 100% of these HILDCAA cases were associated with enhanced whistler-mode chorus waves. The enhancements of E > 0.6, > 2.0, and > 4.0MeV electrons occurred ?1.0day, ?1.5days, and ?2.5days after the statistical HILDCAA onset, respectively. The statistical acceleration rates for the three energy ranges were ?1.8 10{sup 5}, 2.2 10{sup 3}, and 1.0 10{sup 1} cm{sup 2} s{sup 1} sr{sup 1} d{sup 1}, respectively. The relativistic electron-decay timescales were determined to be ?7.7, 5.5, and 4.0days for the three energy ranges, respectively. The HILDCAAs were divided into short-duration (D ? 3days) and long-duration (D > 3days) events to study the dependence of relativistic electron variation on HILDCAA duration. For long-duration events, the flux enhancements during HILDCAAs with respect to pre-event fluxes were ?290%, 520%, and 82% for E > 0.6, > 2.0, and > 4.0MeV electrons, respectively. The enhancements were ?250%, 400%, and 27% respectively, for short-duration events. The results are discussed with respect to the current understanding of radiation-belt dynamics.

  14. WAS THE SUN BORN IN A MASSIVE CLUSTER?

    SciTech Connect (OSTI)

    Dukes, Donald; Krumholz, Mark R.

    2012-07-20

    A number of authors have argued that the Sun must have been born in a cluster of no more than several thousand stars, on the basis that, in a larger cluster, close encounters between the Sun and other stars would have truncated the outer solar system or excited the outer planets into eccentric orbits. However, this dynamical limit is in tension with meteoritic evidence that the solar system was exposed to a nearby supernova during or shortly after its formation; a several-thousand-star cluster is much too small to produce a massive star whose lifetime is short enough to have provided the enrichment. In this paper, we revisit the dynamical limit in the light of improved observations of the properties of young clusters. We use a series of scattering simulations to measure the velocity-dependent cross-section for disruption of the outer solar system by stellar encounters, and use this cross-section to compute the probability of a disruptive encounter as a function of birth cluster properties. We find that, contrary to prior work, the probability of disruption is small regardless of the cluster mass, and that it actually decreases rather than increases with cluster mass. Our results differ from prior work for three main reasons: (1) unlike in most previous work, we compute a velocity-dependent cross-section and properly integrate over the cluster mass-dependent velocity distribution of incoming stars; (2) we recognize that {approx}90% of clusters have lifetimes of a few crossing times, rather than the 10-100 Myr adopted in many earlier models; and (3) following recent observations, we adopt a mass-independent surface density for embedded clusters, rather than a mass-independent radius as assumed many earlier papers. Our results remove the tension between the dynamical limit and the meteoritic evidence, and suggest that the Sun was born in a massive cluster. A corollary to this result is that close encounters in the Sun's birth cluster are highly unlikely to truncate the Kuiper Belt unless the Sun was born in one of the unusual clusters that survived for tens of Myr. However, we find that encounters could plausibly produce highly eccentric Kuiper Belt objects such as Sedna.

  15. Valley filled sand stones In a kootenai formation on the Crow Indian Reservation South Central Montana: Quarterly technical report, January 1, 1997--March 31, 1997

    SciTech Connect (OSTI)

    Lopex, D.A.

    1997-04-04

    Field investigation of the Kootenai valley-fill sandstones was begun in the first quarter. About one half of the outcrop belt was inventoried for occurrences of channel sandstone before heavy snows came to the area. Five exposures of valley-fill sandstone have been located, of these two are 15 meters (50 feet) or greater in thickness and have excellent porosity and permeability. These will be measured and studied in detail during the next field season (1997). No further field work was possible during the second and third quarters because of snow cover. Subsurface data is being collected, organized, and a digital database is being prepared for the project. Geographix petroleum software will probably be used to manage and manipulate the data. Regional subsurface cross sections are being constructed for correlation purposes. All of the four 30 X 60 geologic quadrangles, the Billings, Bridger, Hardin, and Lodge Grass, have been scanned to produce a digital surface geologic data base for the Crow Reservation. These maps are currently being proofed and edited for accuracy. A four-day oil and gas training seminar for Crow Tribal members was completed and was quite successful. The purpose was to enable tribal members and employees to understand and evaluate potential exploration prospects and offers that may result from the completion of this research project.

  16. Late Cenozoic fault kinematics and basin development, Calabrian arc, Italy

    SciTech Connect (OSTI)

    Knott, S.D.; Turco, E.

    1988-08-01

    Current views for explaining the present structure of the Calabrian arc emphasize bending or buckling of an initially straight zone by rigid indentation. Although bending has played an important role, bending itself cannot explain all structural features now seen in the arc for the following reasons: (1) across-arc extension is inconsistent with buckling, (2) north-south compression predicted by a bending mechanism to occur in the internal part of a curved mountain belt is not present in the Calabrian arc, and (3) lateral shear occurs throughout the arc, not just along the northern and southern boundaries. The model presented here is based on lateral bending of mantle and lower crust (demonstrated by variation in extension in the Tyrrhenian basin) and semibrittle faulting and block rotation in the upper crust. These two styles of deformation are confined to the upper plate of the Calabrian subduction system. This deformation is considered to have been active from the beginning of extension in the Tyrrhenian basin (late Tortonian) and is still active today (based on Holocene seismicity). Block rotations are a consequence of lateral heterogeneous shear during extension. Therefore, some of the observed rotation of paleo-magnetic declinations may have occurred in areas undergoing extension and not just during thrusting. Inversion of sedimentary basins by block rotation is predicted by the model. The model will be a useful aid in interpreting reflection seismic data and exploring and developing offshore and onshore sedimentary basins in southern Italy.

  17. Geological setting and geodynamical evolution of the central Apennines (Italy)

    SciTech Connect (OSTI)

    Cavinato, G.P. ); Cosentino, D.; Funiciello, R.; Parotto, M. ); Salvini, F. ); Tozzi, M. )

    1990-05-01

    In the peninsula of Italy, new and revised data allow recognition of geodynamic, units: (1) a deformed intraorogenic foreland (Apulia) made up of several blocks with differing sense and amounts of rotation since the Late Cretaceous; (2) a thrust belt (Apennines) that developed from the late Miocene to at least the middle Pliocene; (3) a deformed foredeep (Bradanic trough) that is widely overthrusted by the Apennine chain and (4) a hinterland (Tyrrehenian basin) that is now undergoing extension and includes large volcanic centers. Within this framework the authors have recognized large-scale, spectacular thrust faults and several new features including backthrusts and important strike-slip zones that lead to new interpretations of the tectonics of the Central Apennines. The new data, acquired during the last 10 yr of field mapping and structural analysis, indicate a complexity of geometry and kinematics not previously recognized. The tectonics of this region cannot be explained in terms of simple extensions and compressional phases. They have included the new data on those styles as well as the backthrust and strike-slip faults into our new model. The recognition of strike-slip components suggests that it will be more difficult to balance cross sections through the region.

  18. Project Overcoat - An Exploration of Exterior Insulation Strategies for 1-1/2-Story Roof Applications in Cold Climates

    SciTech Connect (OSTI)

    Ojczyk, Cindy; Mosiman, Garrett; Huelman, Pat; Schirber, Tom; Yost, Peter; Murry, Tessa

    2013-04-01

    The development of an alternative method to interior-applied insulation strategies or exterior applied 'band-aids' such as heat tapes and ice belts may help reduce energy needs of millions of 1-1/2 story homes while reducing the risk of ice dam formation. A potential strategy for energy improvement of the roof is borrowed from new construction best practices: Here an 'overcoat' of a continuous air, moisture, and thermal barrier is applied on the outside of the roof structure for improved overall performance. The continuous insulation of this approach facilitates a reduction in thermal bridging which could further reduce energy consumption and bring existing homes closer to meeting the Building America goals for energy reduction. Research favors an exterior approach to deep energy retrofits and ice dam prevention in existing homes. The greatest amount of research focuses on whole house deep energy retrofits leaving a void in roof-only applications. The research is also void of data supporting the hygrothermal performance, durability, constructability, and cost of roof-only exterior overcoat strategies. Yet, contractors interviewed for this report indicate an understanding that exterior approaches are most promising for mitigating ice dams and energy loss and are able to sell these strategies to homeowners.

  19. Dust controls at longwalls with water infusion and foam: Technical progress report

    SciTech Connect (OSTI)

    Pothini, R.; Hamilton, H.

    1987-12-31

    A study of the effects of shearer drum rotation on dust generation, product size, productivity, power consumption, machine reliability, and methane generation was undertaken in the Virginia Pocahonatas No. 1 mine. The study was made to determine the benefits, if any, achieved from the reversal of the head drum rotation from the normal direction (roof to floor) to the reversed direction (floor to roof). The operation of the shearer with reversed drum rotation proved superior. There was a 14% reduction in respirable dust on the up-wind side of the shearer and a 40% reduction on the down-wind side when the machine was operated with reversed rotation. Reversed rotation yielded an improvement of approximately 10% in the amount of coarse (+1/4 inch) material reaching the longwall conveyor belt. Time studies indicated a 13% improvement in productivity using reversed rotation. There was no discernible difference in the rate of power consumption. Reversed rotation data indicated a 22% reduction in methane generation per ton of coal mined during the cutting pass. Reversed drum rotation provided the benefits of a safer work environment (reduced respirable dust and methane generation), increased production (improvement in machine potential and availability), and improved product size. Reversed rotation should be considered a standard for all longwall shearers in the Virginia division and evaluated for use on the remaining longwalls within the company.

  20. Giant landslide deposits in northwest Argentina

    SciTech Connect (OSTI)

    Fauque, L.; Strecker, M.R.; Bloom, A.L.

    1985-01-01

    Giant Quaternary landslide deposits occur along mountain fronts in the structural transition zone between the high-angle reverse-fault-bounded Sierras Pampeanas and the low-angle thrust belt of the Sierras Subandinas. There are two modes of occurrence: (1) chaotic masses without distinct geometry, and (2) masses with distinct lobate geometry similar to glacial moraines. Type (1) deposits occur where the moving rock mass followed a narrow valley and blocked the drainage. Many of these caused subsequent formation of lakes and changed the sedimentation processes on pediments at the mountain fronts. In type (2) deposits, lateral and frontal ridges are up to 10 m higher than the interior parts; in some places pressure ridges within the lobes are well preserved. Type (2) deposits show reverse grading and were deposited on relatively smooth pediments or alluvial fans. The lobate geometry strongly suggests that type (2) deposits are a product of flowage and are debris stream or sturzstrom deposits (sense of Heim, 1932 and Hsu, 1975). All investigated deposits occur in areas of demonstrated Quaternary faulting and are interpreted as the result of tectonic movements, although structural inhomogeneities in the source area may have been a significant factor for some of the landslides. No datable materials have yet been found associated with the deposits.

  1. High-resolution in situ observations of electron precipitation-causing EMIC waves

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Rodger, Craig J.; Hendry, Aaron T.; Clilverd, Mark A.; Kletzing, Craig A.; Brundell, James B.; Reeves, Geoffrey D.

    2015-11-21

    Electromagnetic ion cyclotron (EMIC) waves are thought to be important drivers of energetic electron losses from the outer radiation belt through precipitation into the atmosphere. While the theoretical possibility of pitch angle scattering-driven losses from these waves has been recognized for more than four decades, there have been limited experimental precipitation observations to support this concept. We have combined satellite-based observations of the characteristics of EMIC waves, with satellite and ground-based observations of the EMIC-induced electron precipitation. In a detailed case study, supplemented by an additional four examples, we are able to constrain for the first time the location, size,more » and energy range of EMIC-induced electron precipitation inferred from coincident precipitation data and relate them to the EMIC wave frequency, wave power, and ion band of the wave as measured in situ by the Van Allen Probes. As a result, these observations will better constrain modeling into the importance of EMIC wave-particle interactions.« less

  2. Microchip and wedge ion funnels and planar ion beam analyzers using same

    DOE Patents [OSTI]

    Shvartsburg, Alexandre A; Anderson, Gordon A; Smith, Richard D

    2012-10-30

    Electrodynamic ion funnels confine, guide, or focus ions in gases using the Dehmelt potential of oscillatory electric field. New funnel designs operating at or close to atmospheric gas pressure are described. Effective ion focusing at such pressures is enabled by fields of extreme amplitude and frequency, allowed in microscopic gaps that have much higher electrical breakdown thresholds in any gas than the macroscopic gaps of present funnels. The new microscopic-gap funnels are useful for interfacing atmospheric-pressure ionization sources to mass spectrometry (MS) and ion mobility separation (IMS) stages including differential IMS or FAIMS, as well as IMS and MS stages in various configurations. In particular, "wedge" funnels comprising two planar surfaces positioned at an angle and wedge funnel traps derived therefrom can compress ion beams in one dimension, producing narrow belt-shaped beams and laterally elongated cuboid packets. This beam profile reduces the ion density and thus space-charge effects, mitigating the adverse impact thereof on the resolving power, measurement accuracy, and dynamic range of MS and IMS analyzers, while a greater overlap with coplanar light or particle beams can benefit spectroscopic methods.

  3. Refined rotational period, pole solution, and shape model for (3200) Phaethon

    SciTech Connect (OSTI)

    Ansdell, Megan; Meech, Karen J.; Kaluna, Heather; Hainaut, Olivier; Buie, Marc W.; Bauer, James; Dundon, Luke

    2014-09-20

    (3200) Phaethon exhibits both comet- and asteroid-like properties, suggesting it could be a rare transitional object such as a dormant comet or previously volatile-rich asteroid. This justifies detailed study of (3200) Phaethon's physical properties as a better understanding of asteroid-comet transition objects can provide insight into minor body evolution. We therefore acquired time series photometry of (3200) Phaethon over 15 nights from 1994 to 2013, primarily using the Tektronix 2048 2048 pixel CCD on the University of Hawaii 2.2 m telescope. We utilized light curve inversion to (1) refine (3200) Phaethon's rotational period to P = 3.6032 0.0008 hr; (2) estimate a rotational pole orientation of ? = +85 13 and ? = 20 10; and (3) derive a shape model. We also used our extensive light curve data set to estimate the slope parameter of (3200) Phaethon's phase curve as G ? 0.06, consistent with C-type asteroids. We discuss how this highly oblique pole orientation with a negative ecliptic latitude supports previous evidence for (3200) Phaethon's origin in the inner main asteroid belt as well as the potential for deeply buried volatiles fueling impulsive yet rare cometary outbursts.

  4. Audit unto others{hor_ellipsis}

    SciTech Connect (OSTI)

    Maday, J.H. Jr.

    1992-05-01

    My first encounter with a quality assurance auditor is reminiscent of an old Dodge commercial. You remember? The old sheriff, masked in mirrored sunglasses, paunch hanging over his gun belt, prophesying, ``You`re in a heap o` trouble boy!`` Well, my auditor could have been kin to the sheriff; they had the same posture, attitude, and mirrored sunglasses. Plus, my auditor wore a black leather vest and sported a ``Buffalo Bill`` goatee. While certainly memorable, both gentlemen were far from pleasant. I`m fairly certain that the compliance auditor of old deserved this perceived association with his law enforcement counterpart. Both believed in enforcing the letter of the law, or their interpretations of it. Neither seemed capable of exercising interpretive powers, but instead relied on winning through intimidation, possibly with an eye toward claiming some version of a monthly Quota Award. Is the auditor of today any better perceived? Because this ``first encounter of the worst kind`` made a lasting impression on me, I have dedicated considerable time and effort trying to avoid being perceived as another sheriff when I conduct audits. In my auditing career, I am determined to capitalize on each opportunity to turn negative situations, as experienced by the auditee, into meaningful opportunities for improved performance. I want to treat the auditee the way I want to be treated when I am being audited. (author)

  5. Audit unto others hor ellipsis

    SciTech Connect (OSTI)

    Maday, J.H. Jr.

    1992-05-01

    My first encounter with a quality assurance auditor is reminiscent of an old Dodge commercial. You remember The old sheriff, masked in mirrored sunglasses, paunch hanging over his gun belt, prophesying, You're in a heap o' trouble boy '' Well, my auditor could have been kin to the sheriff; they had the same posture, attitude, and mirrored sunglasses. Plus, my auditor wore a black leather vest and sported a Buffalo Bill'' goatee. While certainly memorable, both gentlemen were far from pleasant. I'm fairly certain that the compliance auditor of old deserved this perceived association with his law enforcement counterpart. Both believed in enforcing the letter of the law, or their interpretations of it. Neither seemed capable of exercising interpretive powers, but instead relied on winning through intimidation, possibly with an eye toward claiming some version of a monthly Quota Award. Is the auditor of today any better perceived Because this first encounter of the worst kind'' made a lasting impression on me, I have dedicated considerable time and effort trying to avoid being perceived as another sheriff when I conduct audits. In my auditing career, I am determined to capitalize on each opportunity to turn negative situations, as experienced by the auditee, into meaningful opportunities for improved performance. I want to treat the auditee the way I want to be treated when I am being audited. (author)

  6. Study on detailed geological modelling for fluvial sandstone reservoir in Daqing oil field

    SciTech Connect (OSTI)

    Zhao Hanqing; Fu Zhiguo; Lu Xiaoguang

    1997-08-01

    Guided by the sedimentation theory and knowledge of modern and ancient fluvial deposition and utilizing the abundant information of sedimentary series, microfacies type and petrophysical parameters from well logging curves of close spaced thousands of wells located in a large area. A new method for establishing detailed sedimentation and permeability distribution models for fluvial reservoirs have been developed successfully. This study aimed at the geometry and internal architecture of sandbodies, in accordance to their hierarchical levels of heterogeneity and building up sedimentation and permeability distribution models of fluvial reservoirs, describing the reservoir heterogeneity on the light of the river sedimentary rules. The results and methods obtained in outcrop and modem sedimentation studies have successfully supported the study. Taking advantage of this method, the major producing layers (PI{sub 1-2}), which have been considered as heterogeneous and thick fluvial reservoirs extending widely in lateral are researched in detail. These layers are subdivided into single sedimentary units vertically and the microfacies are identified horizontally. Furthermore, a complex system is recognized according to their hierarchical levels from large to small, meander belt, single channel sandbody, meander scroll, point bar, and lateral accretion bodies of point bar. The achieved results improved the description of areal distribution of point bar sandbodies, provide an accurate and detailed framework model for establishing high resolution predicting model. By using geostatistic technique, it also plays an important role in searching for enriched zone of residual oil distribution.

  7. Operational advances in ring current modeling using RAM-SCB

    SciTech Connect (OSTI)

    Welling, Daniel T; Jordanova, Vania K; Zaharia, Sorin G; Morley, Steven K

    2010-12-03

    The Ring current Atmosphere interaction Model with Self-Consistently calculated 3D Magnetic field (RAM-SCB) combines a kinetic model of the ring current with a force-balanced model of the magnetospheric magnetic field to create an inner magnetospheric model that is magnetically self consistent. RAM-SCB produces a wealth of outputs that are valuable to space weather applications. For example, the anisotropic particle distribution of the KeV-energy population calculated by the code is key for predicting surface charging on spacecraft. Furthermore, radiation belt codes stand to benefit substantially from RAM-SCB calculated magnetic field values and plasma wave growth rates - both important for determining the evolution of relativistic electron populations. RAM-SCB is undergoing development to bring these benefits to the space weather community. Data-model validation efforts are underway to assess the performance of the system. 'Virtual Satellite' capability has been added to yield satellite-specific particle distribution and magnetic field output. The code's outer boundary is being expanded to 10 Earth Radii to encompass previously neglected geosynchronous orbits and allow the code to be driven completely by either empirical or first-principles based inputs. These advances are culminating towards a new, real-time version of the code, rtRAM-SCB, that can monitor the inner magnetosphere conditions on both a global and spacecraft-specific level. This paper summarizes these new features as well as the benefits they provide the space weather community.

  8. Relation between facies, diagenesis, and reservoir quality of Rotliegende reservoirs in north Germany

    SciTech Connect (OSTI)

    David, F.; Gast, R.; Kraft, T. (BEB Erdgas Erdol GmbH, Hannover (Germany))

    1993-09-01

    In north Germany, the majority of Rotliegende gas fields is confined to an approximately 50 km-wide east-west-orientated belt, which is situated on the gently north-dipping flank of the southern Permian basin. Approximately 400 billion m[sup 3] of natural gas has been found in Rotliegende reservoir sandstones with average porosities of depths ranging from 3500 to 5000 m. Rotliegende deposition was controlled by the Autunian paleo-relief, and arid climate and cyclic transgressions of the desert lake. In general, wadis and large dunefields occur in the hinterland, sebkhas with small isolate dunes and shorelines define the coastal area, and a desert lake occurs to the north. The sandstones deposited in large dunefields contain only minor amounts of illite, anhydrite, and calcite and form good reservoirs. In contrast, the small dunes formed in the sebkha areas were affected by fluctuations of the desert lake groundwaters, causing the infiltration of detrital clay and precipitation of gypsum and calcite. These cements were transformed to illite, anhydrite, and calcite-II during later diagenesis, leading to a significant reduction of the reservoir quality. The best reservoirs occur in the shoreline sandstones because porosity and permeability were preserved by early magnesium-chlorite diagenesis. Since facies controls diagenesis and consequently reservoir quality, mapping of facies also indicates the distribution of reservoir and nonreservoir rocks. This information is used to identify play area and to interpret and calibrate three-dimensional seismic data.

  9. High-resolution in situ observations of electron precipitation-causing EMIC waves

    SciTech Connect (OSTI)

    Rodger, Craig J.; Hendry, Aaron T.; Clilverd, Mark A.; Kletzing, Craig A.; Brundell, James B.; Reeves, Geoffrey D.

    2015-11-21

    Electromagnetic ion cyclotron (EMIC) waves are thought to be important drivers of energetic electron losses from the outer radiation belt through precipitation into the atmosphere. While the theoretical possibility of pitch angle scattering-driven losses from these waves has been recognized for more than four decades, there have been limited experimental precipitation observations to support this concept. We have combined satellite-based observations of the characteristics of EMIC waves, with satellite and ground-based observations of the EMIC-induced electron precipitation. In a detailed case study, supplemented by an additional four examples, we are able to constrain for the first time the location, size, and energy range of EMIC-induced electron precipitation inferred from coincident precipitation data and relate them to the EMIC wave frequency, wave power, and ion band of the wave as measured in situ by the Van Allen Probes. As a result, these observations will better constrain modeling into the importance of EMIC wave-particle interactions.

  10. Sensitivity of a global climate model to the critical Richardson number in the boundary layer parameterization

    SciTech Connect (OSTI)

    Zhang, Ning; Liu, Yangang; Gao, Zhiqiu; Li, Dan

    2015-04-27

    The critical bulk Richardson number (Ricr) is an important parameter in planetary boundary layer (PBL) parameterization schemes used in many climate models. This paper examines the sensitivity of a Global Climate Model, the Beijing Climate Center Atmospheric General Circulation Model, BCC_AGCM to Ricr. The results show that the simulated global average of PBL height increases nearly linearly with Ricr, with a change of about 114 m for a change of 0.5 in Ricr. The surface sensible (latent) heat flux decreases (increases) as Ricr increases. The influence of Ricr on surface air temperature and specific humidity is not significant. The increasing Ricr may affect the location of the Westerly Belt in the Southern Hemisphere. Further diagnosis reveals that changes in Ricr affect stratiform and convective precipitations differently. Increasing Ricr leads to an increase in the stratiform precipitation but a decrease in the convective precipitation. Significant changes of convective precipitation occur over the inter-tropical convergence zone, while changes of stratiform precipitation mostly appear over arid land such as North Africa and Middle East.

  11. STELLAR ELEMENTAL ABUNDANCE PATTERNS: IMPLICATIONS FOR PLANET FORMATION

    SciTech Connect (OSTI)

    Chambers, J. E.

    2010-11-20

    The solar photosphere is depleted in refractory elements compared to most solar twins, with the degree of depletion increasing with an element's condensation temperature. Here, I show that adding 4 Earth masses of Earth-like and carbonaceous-chondrite-like material to the solar convection zone brings the Sun's composition into line with the mean value for the solar twins. The observed solar composition could have arisen if the Sun's convection zone accreted material from the solar nebula that was depleted in refractory elements due to the formation of the terrestrial planets and ejection of rocky protoplanets from the asteroid belt. Most solar analogs are missing 0-10 Earth masses of rocky material compared to the most refractory-rich stars, providing an upper limit to the mass of rocky terrestrial planets that they possess. The missing mass is correlated with stellar metallicity. This suggests that the efficiency of planetesimal formation increases with stellar metallicity. Stars with and without known giant planets show a similar distribution of abundance trends. If refractory depletion is a signature of the presence of terrestrial planets, this suggests that there is not a strong correlation between the presence of terrestrial and giant planets in the same system.

  12. Alum Innovative Exploration Project (Ram Power Inc.)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Miller, Clay

    2010-01-01

    Data generated from the Alum Innovative Exploration Project, one of several promising geothermal properties located in the middle to upper Miocene (~11-5 Ma, or million years BP) Silver Peak-Lone Mountain metamorphic core complex (SPCC) of the Walker Lane structural belt in Esmeralda County, west-central Nevada. The geothermal system at Alum is wholly concealed; its upper reaches discovered in the late 1970s during a regional thermal-gradient drilling campaign. The prospect boasts several shallow thermal-gradient (TG) boreholes with TG >75oC/km (and as high as 440oC/km) over 200-m intervals in the depth range 0-600 m. Possibly boiling water encountered at 239 m depth in one of these boreholes returned chemical- geothermometry values in the range 150-230oC. GeothermEx (2008) has estimated the electrical- generation capacity of the current Alum leasehold at 33 megawatts for 20 years; and the corresponding value for the broader thermal anomaly extending beyond the property at 73 megawatts for the same duration.

  13. Simulated Coal-Gas-Fueled Molten Carbonate Fuel Cell Development Program

    SciTech Connect (OSTI)

    Not Available

    1992-08-01

    This final report summarizes the technical work performed under Department of Energy Contract DE-AC21-91MC27393, Simulated Coal- Gas-Fueled Molten Carbonate Fuel Cell Development Program.'' This work consists of five major tasks and their respective subtasks as listed below. A brief description of each task is also provided. The Stack Design Requirements task focused on requirements and specification for designing, constructing, and testing a nominal 100-kilowatt integrated stack and on requirements for the balance-of-plant equipment to support a 1000-kilowatt integrated stack demonstrator. The Stack Design Preparation task focused on the mechanical design of a 100-kilowatt stack comprised of 8-ft[sup 2] cells incorporating the new cell configuration and component technology improvements developed in the previous DOE MCFC contract. Electrode Casting focused on developing a faster drying solvent for use in the electrode tape casting process. Electrode Heat Treatment was directed at scaling up the laboratory continuous debinding process to a new full-size IFC debinding oven coupled to a continuous belt furnace that will both debind and sinter the electrodes in one continuous process train. Repeat Part Quality Assurance and Testing provided the appropriate effort to ensure consistent, high-quality, reproducible and comparable repeat parts.

  14. Simulated Coal-Gas-Fueled Molten Carbonate Fuel Cell Development Program. Final report

    SciTech Connect (OSTI)

    Not Available

    1992-08-01

    This final report summarizes the technical work performed under Department of Energy Contract DE-AC21-91MC27393, ``Simulated Coal- Gas-Fueled Molten Carbonate Fuel Cell Development Program.`` This work consists of five major tasks and their respective subtasks as listed below. A brief description of each task is also provided. The Stack Design Requirements task focused on requirements and specification for designing, constructing, and testing a nominal 100-kilowatt integrated stack and on requirements for the balance-of-plant equipment to support a 1000-kilowatt integrated stack demonstrator. The Stack Design Preparation task focused on the mechanical design of a 100-kilowatt stack comprised of 8-ft{sup 2} cells incorporating the new cell configuration and component technology improvements developed in the previous DOE MCFC contract. Electrode Casting focused on developing a faster drying solvent for use in the electrode tape casting process. Electrode Heat Treatment was directed at scaling up the laboratory continuous debinding process to a new full-size IFC debinding oven coupled to a continuous belt furnace that will both debind and sinter the electrodes in one continuous process train. Repeat Part Quality Assurance and Testing provided the appropriate effort to ensure consistent, high-quality, reproducible and comparable repeat parts.

  15. Structural elements of the Sulu Sea, Philippines

    SciTech Connect (OSTI)

    Hinz, K.; Block, M.; Kudrass, H.R.; Meyer, H. , Hannover )

    1994-07-01

    The structure and tectonic history of the Sulu Sea are described on the basis of seismic reflection data combined with the findings of onshore and offshore geological studies, and the results of ODP Leg 124 drilling. Closing of a hypothetical Mesozoic proto-South China Sea associated with the formation of oceanic crustal splinters in the late Eocene followed by southward subduction and, in turn, progressive collision of the north Palawan continental terrane with the micro-continental Borneo plate since the middle Miocene, resulted in the formation of the structurally complex Sulu-Borneo collision belt. The latter comprises north Sabah, southern and central Palawan, and the northwest Sulu basin. Fracturing of the Borneo micro-continental plate into the Sulu and Cagayan ridges initiated the opening of the southeast Sulu basin during the late Oligocene through the early Miocene. Collision of the north Palawan continental terrane with Cagayan Ridge in the late early Miocene and oblique collision of these blocks with the central Philippines resulted in the still ongoing closing of the southeast Sulu basin since the middle or late Miocene. Closing of the southeast Sulu basin began with the formation of an oceanic crustal slab.

  16. Frequency sweep rates of rising tone electromagnetic ion cyclotron waves: Comparison between nonlinear theory and Cluster observation

    SciTech Connect (OSTI)

    He, Zhaoguo; Zong, Qiugang Wang, Yongfu; Liu, Siqing; Lin, Ruilin; Shi, Liqin

    2014-12-15

    Resonant pitch angle scattering by electromagnetic ion cyclotron (EMIC) waves has been suggested to account for the rapid loss of ring current ions and radiation belt electrons. For the rising tone EMIC wave (classified as triggered EMIC emission), its frequency sweep rate strongly affects the efficiency of pitch-angle scattering. Based on the Cluster observations, we analyze three typical cases of rising tone EMIC waves. Two cases locate at the nightside (22.3 and 22.6 magnetic local time (MLT)) equatorial region and one case locates at the duskside (18MLT) higher magnetic latitude (??=?9.3) region. For the three cases, the time-dependent wave amplitude, cold electron density, and cold ion density ratio are derived from satellite data; while the ambient magnetic field, thermal proton perpendicular temperature, and the wave spectral can be directly provided by observation. These parameters are input into the nonlinear wave growth model to simulate the time-frequency evolutions of the rising tones. The simulated results show good agreements with the observations of the rising tones, providing further support for the previous finding that the rising tone EMIC wave is excited through the nonlinear wave growth process.

  17. Geothermal regime and thermal history of the Llanos Basin, Columbia

    SciTech Connect (OSTI)

    Bachu, S.; Underschultz, J.R.; Ramon, J.C.; Villegas, M.E.

    1995-01-01

    The Llanos basin is a siliciclastic foreland sub-Andean sedimentary basin located in Columbia between the Cordillera Oriental and the Guyana Precambrian shield. Data on bottom-hole temperature, lithology, porosity, and vitrinite reflectance from all 318 wells drilled in the central and southern parts of the basin were used to analyze its geothermal regime and thermal history. Average geothermal gradients in the Llanos basin decrease generally with depth and westward toward the fold and thrust belt. The geothermal regime is controlled by a moderate, generally westward-decreasing basement heat flow, by depositional and compaction factors, and, in places, by advection by formation waters. Compaction leads to increased thermal conductivity with depth, whereas westward downdip flow in deep sandstone formations may exert a cooling effect in the central-western part of the basin. Vitrinite reflectance variation with depth shows a major discontinuity at the pre-Cretaceous unconformity. Areally, vitrinite reflectance increases southwestward in Paleozoic strata and northwestward in post-Paleozoic strata. These patterns indicate that the thermal history of the basin probably includes three thermal events that led to peaks in oil generation: a Paleozoic event in the southwest, a failed Cretaceous rifting event in the west, and an early Tertiary back-arc event in the west. Rapid cooling since the last thermal event is possibly caused by subhorizontal subduction of cold oceanic lithospheric plate.

  18. Method of processing ``BPS`` glass ceramic and seals made therewith

    DOE Patents [OSTI]

    Reed, S.T.; Stone, R.G.; McCollister, H.L.; Wengert, P.R.

    1998-10-13

    A glass ceramic composition, a glass ceramic-to-metal seal, and more specifically a hermetic glass ceramic-to-metal seal prepared by subjecting a glass composition comprising, by weight percent, SiO{sub 2} (65--80%), LiO{sub 2} (8--16%), Al{sub 2}O{sub 3} (2--8%), K{sub 2}O (1--8%), P{sub 2}O{sub 5} (1--5%), B{sub 2}O{sub 3} (0.5--7%), and ZnO (0--5%) to the following processing steps: (1) heating the glass composition in a belt furnace to a temperature sufficient to melt the glass and crystallize lithium phosphate, (2) holding at a temperature and for a time sufficient to create cristobalite nuclei, (3) cooling at a controlled rate and to a temperature to cause crystallization of lithium silicates and growth of cristobalite, and (4) still further cooling in stages to ambient temperature. This process produces a glass ceramic whose high coefficient of thermal expansion (up to 200{times}10{sup {minus}7} in/in/C) permits the fabrication of glass ceramic-to-metal seals, and particularly hermetic glass ceramic seals to nickel-based and stainless steel alloys and copper. 5 figs.

  19. Assembly and Testing of a Radioisotope Power System for the New Horizons Spacecraft

    SciTech Connect (OSTI)

    Kenneth E. Rosenberg; Stephen G. Johnson

    2006-06-01

    The Idaho National Laboratory (INL) recently fueled and assembled a radioisotope power system (RPS) that was used upon the New Horizons spacecraft which was launched in January 2006. New Horizons is the first mission to the last planet - the initial reconnaissance of Pluto-Charon and the Kuiper Belt, exploring the mysterious worlds at the edge of our solar system. The RPS otherwise known as a "space battery" converts thermal heat into electrical energy. The thermal heat source contains plutonium dioxide in the form of ceramic pellets encapsulated in iridium metal. The space battery was assembled in a new facility at the Idaho National Laboratory site near Idaho Falls, Idaho. The new facility has all the fueling and testing capabilities including the following: the ability to handle all the shipping containers currently certified to ship Pu-238, the ability to fuel a variety of RPS designs, the ability to perform vibrational testing to simulate transportation and launch environments, welding systems, a center of mass determination device, and various other support systems.

  20. Effects of enhanced stratification on equatorward dynamo wave propagation

    SciTech Connect (OSTI)

    Käpylä, Petri J.; Mantere, Maarit J.; Cole, Elizabeth; Warnecke, Jörn; Brandenburg, Axel

    2013-11-20

    We present results from simulations of rotating magnetized turbulent convection in spherical wedge geometry representing parts of the latitudinal and longitudinal extents of a star. Here we consider a set of runs for which the density stratification is varied, keeping the Reynolds and Coriolis numbers at similar values. In the case of weak stratification, we find quasi-steady dynamo solutions for moderate rotation and oscillatory ones with poleward migration of activity belts for more rapid rotation. For stronger stratification, the growth rate tends to become smaller. Furthermore, a transition from quasi-steady to oscillatory dynamos is found as the Coriolis number is increased, but now there is an equatorward migrating branch near the equator. The breakpoint where this happens corresponds to a rotation rate that is about three to seven times the solar value. The phase relation of the magnetic field is such that the toroidal field lags behind the radial field by about π/2, which can be explained by an oscillatory α{sup 2} dynamo caused by the sign change of the α-effect about the equator. We test the domain size dependence of our results for a rapidly rotating run with equatorward migration by varying the longitudinal extent of our wedge. The energy of the axisymmetric mean magnetic field decreases as the domain size increases and we find that an m = 1 mode is excited for a full 2π azimuthal extent, reminiscent of the field configurations deduced from observations of rapidly rotating late-type stars.

  1. Enhanced loss of magnetic-mirror-trapped fast electrons by a shear Alfvén wave

    SciTech Connect (OSTI)

    Wang, Y.; Gekelman, W.; Pribyl, P.; Papadopoulos, K.

    2014-05-15

    Laboratory observations of enhanced loss of magnetic mirror trapped fast electrons irradiated by a shear Alfvén Wave (SAW) are reported. The experiment is performed in the quiescent after-glow plasma in the Large Plasma Device [Gekelman et al., Rev. Sci. Instrum. 62(12), 2875–2883 (1991)]. A trapped energetic electron population (>100 keV) is generated in a magnetic mirror section (mirror ratio ≈ 2, length = 3.5 m) by an X-mode high power microwave pulse, and forms a hot electron ring due to the grad-B and curvature drift. SAWs of arbitrary polarization are launched externally by a Rotating Magnetic Field source (δB/B{sub 0} ≈ 0.1%, λ{sub ∥} ≈ 9 m). Irradiated by a right-handed circularly polarized SAW, the loss of electrons, in both the radial and the axial direction of the mirror field, is significantly enhanced and is modulated at f{sub Alfvén}. The periodical loss continues even after the termination of the SAW. Experimental observations suggest that a spatial distortion of the ring is formed in the SAW field and creates a collective mode of the hot electron population that degrades its confinement and leads to electron loss from the magnetic mirror. The results could have implications on techniques of radiation belt remediation.

  2. Applying the cold plasma dispersion relation to whistler mode chorus waves: EMFISIS wave measurements from the Van Allen Probes

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Hartley, D. P.; Chen, Y.; Kletzing, C. A.; Denton, M. H.; Kurth, W. S.

    2015-02-17

    Most theoretical wave models require the power in the wave magnetic field in order to determine the effect of chorus waves on radiation belt electrons. However, researchers typically use the cold plasma dispersion relation to approximate the magnetic wave power when only electric field data are available. In this study, the validity of using the cold plasma dispersion relation in this context is tested using Electric and Magnetic Field Instrument Suite and Integrated Science (EMFISIS) observations of both the electric and magnetic spectral intensities in the chorus wave band (0.1–0.9 fce). Results from this study indicate that the calculated wavemore » intensity is least accurate during periods of enhanced wave activity. For observed wave intensities >10⁻³ nT², using the cold plasma dispersion relation results in an underestimate of the wave intensity by a factor of 2 or greater 56% of the time over the full chorus wave band, 60% of the time for lower band chorus, and 59% of the time for upper band chorus. Hence, during active periods, empirical chorus wave models that are reliant on the cold plasma dispersion relation will underestimate chorus wave intensities to a significant degree, thus causing questionable calculation of wave-particle resonance effects on MeV electrons.« less

  3. Investigation of EMIC wave scattering as the cause for the BARREL 17 January 2013 relativistic electron precipitation event: A quantitative comparison of simulation with observations

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Li, Zan; Millan, Robyn M.; Hudson, Mary K.; Woodger, Leslie A.; Smith, David M.; Chen, Yue; Friedel, Reiner; Rodriguez, Juan V.; Engebretson, Mark J.; Goldstein, Jerry; et al

    2014-12-23

    Electromagnetic ion cyclotron (EMIC) waves were observed at multiple observatory locations for several hours on 17 January 2013. During the wave activity period, a duskside relativistic electron precipitation (REP) event was observed by one of the Balloon Array for Radiation belt Relativistic Electron Losses (BARREL) balloons and was magnetically mapped close to Geostationary Operational Environmental Satellite (GOES) 13. We simulate the relativistic electron pitch angle diffusion caused by gyroresonant interactions with EMIC waves using wave and particle data measured by multiple instruments on board GOES 13 and the Van Allen Probes. We show that the count rate, the energy distribution,more » and the time variation of the simulated precipitation all agree very well with the balloon observations, suggesting that EMIC wave scattering was likely the cause for the precipitation event. The event reported here is the first balloon REP event with closely conjugate EMIC wave observations, and our study employs the most detailed quantitative analysis on the link of EMIC waves with observed REP to date.« less

  4. Interpretation of solar irradiance monitor measurements through analysis of 3D MHD simulations

    SciTech Connect (OSTI)

    Criscuoli, S.; Uitenbroek, H.

    2014-06-20

    Measurements from the Spectral Irradiance Monitor (SIM) on board the Solar Radiation and Climate Experiment mission indicate that solar spectral irradiance at visible and IR wavelengths varies in counter phase with the solar activity cycle. The sign of these variations is not reproduced by most of the irradiance reconstruction techniques based on variations of surface magnetism employed so far, and it is not yet clear whether SIM calibration procedures need to be improved or if instead new physical mechanisms must be invoked to explain such variations. We employ three-dimensional magnetohydrodynamic simulations of the solar photosphere to investigate the dependence of solar radiance in SIM visible and IR spectral ranges on variations of the filling factor of surface magnetic fields. We find that the contribution of magnetic features to solar radiance is strongly dependent on the location on the disk of the features, which are negative close to disk center and positive toward the limb. If features are homogeneously distributed over a region around the equator (activity belt), then their contribution to irradiance is positive with respect to the contribution of HD snapshots, but decreases with the increase of their magnetic flux for average magnetic flux larger than 50 G in at least two of the visible and IR spectral bands monitored by SIM. Under the assumption that the 50 G snapshots are representative of quiet-Sun regions, we thus find that the Spectral Irradiance can be in counter-phase with the solar magnetic activity cycle.

  5. Nonlinear electric field structures in the inner magnetosphere

    SciTech Connect (OSTI)

    Malaspina, D. M.; Andersson, L.; Ergun, R. E.; Wygant, J. R.; Bonnell, J. W.; Kletzing, C.; Reeves, G. D.; Skoug, R. M.; Larsen, B. A.

    2014-08-28

    Recent observations by the Van Allen Probes spacecraft have demonstrated that a variety of electric field structures and nonlinear waves frequently occur in the inner terrestrial magnetosphere, including phase space holes, kinetic field-line resonances, nonlinear whistler-mode waves, and several types of double layer. However, it is nuclear whether such structures and waves have a significant impact on the dynamics of the inner magnetosphere, including the radiation belts and ring current. To make progress toward quantifying their importance, this study statistically evaluates the correlation of such structures and waves with plasma boundaries. A strong correlation is found. These statistical results, combined with observations of electric field activity at propagating plasma boundaries, are consistent with the identification of these boundaries as the source of free energy responsible for generating the electric field structures and nonlinear waves of interest. Therefore, the ability of these structures and waves to influence plasma in the inner magnetosphere is governed by the spatial extent and dynamics of macroscopic plasma boundaries in that region.

  6. Applying the cold plasma dispersion relation to whistler mode chorus waves: EMFISIS wave measurements from the Van Allen Probes

    SciTech Connect (OSTI)

    Hartley, D. P.; Chen, Y.; Kletzing, C. A.; Denton, M. H.; Kurth, W. S.

    2015-02-17

    Most theoretical wave models require the power in the wave magnetic field in order to determine the effect of chorus waves on radiation belt electrons. However, researchers typically use the cold plasma dispersion relation to approximate the magnetic wave power when only electric field data are available. In this study, the validity of using the cold plasma dispersion relation in this context is tested using Electric and Magnetic Field Instrument Suite and Integrated Science (EMFISIS) observations of both the electric and magnetic spectral intensities in the chorus wave band (0.10.9 fce). Results from this study indicate that the calculated wave intensity is least accurate during periods of enhanced wave activity. For observed wave intensities >10? nT, using the cold plasma dispersion relation results in an underestimate of the wave intensity by a factor of 2 or greater 56% of the time over the full chorus wave band, 60% of the time for lower band chorus, and 59% of the time for upper band chorus. Hence, during active periods, empirical chorus wave models that are reliant on the cold plasma dispersion relation will underestimate chorus wave intensities to a significant degree, thus causing questionable calculation of wave-particle resonance effects on MeV electrons.

  7. A background correction algorithm for Van Allen Probes MagEIS electron flux measurements

    SciTech Connect (OSTI)

    Claudepierre, S. G.; O'Brien, T. P.; Blake, J. B.; Fennell, J. F.; Roeder, J. L.; Clemmons, J. H.; Looper, M. D.; Mazur, J. E.; Mulligan, T. M.; Spence, H. E.; Reeves, G. D.; Friedel, R. H. W.; Henderson, M. G.; Larsen, B. A.

    2015-07-14

    We describe an automated computer algorithm designed to remove background contamination from the Van Allen Probes Magnetic Electron Ion Spectrometer (MagEIS) electron flux measurements. We provide a detailed description of the algorithm with illustrative examples from on-orbit data. We find two primary sources of background contamination in the MagEIS electron data: inner zone protons and bremsstrahlung X-rays generated by energetic electrons interacting with the spacecraft material. Bremsstrahlung X-rays primarily produce contamination in the lower energy MagEIS electron channels (~30500 keV) and in regions of geospace where multi-M eV electrons are present. Inner zone protons produce contamination in all MagEIS energy channels at roughly L < 2.5. The background-corrected MagEIS electron data produce a more accurate measurement of the electron radiation belts, as most earlier measurements suffer from unquantifiable and uncorrectable contamination in this harsh region of the near-Earth space environment. These background-corrected data will also be useful for spacecraft engineering purposes, providing ground truth for the near-Earth electron environment and informing the next generation of spacecraft design models (e.g., AE9).

  8. Electroforming of Bi(1-x)Sb(x) nanowires for high-efficiency micro-thermoelectric cooling devices on a chip.

    SciTech Connect (OSTI)

    Overmyer, Donald L.; Webb, Edmund Blackburn, III; Siegal, Michael P.; Yelton, William Graham

    2006-11-01

    Active cooling of electronic systems for space-based and terrestrial National Security missions has demanded use of Stirling, reverse-Brayton, closed Joule-Thompson, pulse tube and more elaborate refrigeration cycles. Such cryocoolers are large systems that are expensive, demand large powers, often contain moving parts and are difficult to integrate with electronic systems. On-chip, solid-state, active cooling would greatly enhance the capabilities of future systems by reducing the size, cost and inefficiencies compared to existing solutions. We proposed to develop the technology for a thermoelectric cooler capable of reaching 77K by replacing bulk thermoelectric materials with arrays of Bi{sub 1-x}Sb{sub x} nanowires. Furthermore, the Sandia-developed technique we will use to produce the oriented nanowires occurs at room temperature and can be applied directly to a silicon substrate. Key obstacles include (1) optimizing the Bi{sub 1-x}Sb{sub x} alloy composition for thermoelectric properties; (2) increasing wire aspect ratios to 3000:1; and (3) increasing the array density to {ge} 10{sup 9} wires/cm{sup 2}. The primary objective of this LDRD was to fabricate and test the thermoelectric properties of arrays of Bi{sub 1-x}Sb{sub x} nanowires. With this proof-of-concept data under our belts we are positioned to engage National Security systems customers to invest in the integration of on-chip thermoelectric coolers for future missions.

  9. Nonlinear electric field structures in the inner magnetosphere

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Malaspina, D. M.; Andersson, L.; Ergun, R. E.; Wygant, J. R.; Bonnell, J. W.; Kletzing, C.; Reeves, G. D.; Skoug, R. M.; Larsen, B. A.

    2014-08-28

    Recent observations by the Van Allen Probes spacecraft have demonstrated that a variety of electric field structures and nonlinear waves frequently occur in the inner terrestrial magnetosphere, including phase space holes, kinetic field-line resonances, nonlinear whistler-mode waves, and several types of double layer. However, it is nuclear whether such structures and waves have a significant impact on the dynamics of the inner magnetosphere, including the radiation belts and ring current. To make progress toward quantifying their importance, this study statistically evaluates the correlation of such structures and waves with plasma boundaries. A strong correlation is found. These statistical results, combinedmore » with observations of electric field activity at propagating plasma boundaries, are consistent with the identification of these boundaries as the source of free energy responsible for generating the electric field structures and nonlinear waves of interest. Therefore, the ability of these structures and waves to influence plasma in the inner magnetosphere is governed by the spatial extent and dynamics of macroscopic plasma boundaries in that region.« less

  10. SYMPATHETIC FILAMENT ERUPTIONS FROM A BIPOLAR HELMET STREAMER IN THE SUN

    SciTech Connect (OSTI)

    Yang Jiayan; Jiang Yunchun; Zheng Ruisheng; Bi Yi; Hong Junchao; Yang Bo

    2012-01-20

    On 2005 August 5, two solar filaments erupted successively from different confined arcades underlying a common overarching multiple-arcade bipolar helmet streamer. We present detailed observations of these two events and identify them as sympathetic filament eruptions. The first (F1) is a small active-region filament located near the outskirts of the streamer arcade. It underwent a nonradial eruption, initially moving in the interior of the streamer arcade and resulting in an over-and-out coronal mass ejection. The second filament (F2), a larger quiescent one far away from F1, was clearly disturbed during the F1 eruption. It then underwent a very slow eruption and finally disappeared completely and permanently. Because two belt-shaped diffuse dimmings formed along the footprints of the streamer arcade in the first eruption and persisted throughout the complete disappearance of F2, the eruption series are interpreted as sympathetic: the simple expansion of the common streamer arcade forced by the F1 eruption weakened magnetic flux overlying F2 and thus led to its slow eruption, with the dimming formation indicating their physical connection. Our observations suggest that multiple-arcade bipolar helmet-streamer configurations are appropriate to producing sympathetic eruptions. Combined with the recent observations of unipolar-streamer sympathetic events, it appears that a multiple-arcade unipolar or bipolar helmet streamer can serve as a common magnetic configuration for sympathetic eruptions.

  11. The impact of high-frequency sedimentation cycles on stratigraphic interpretation

    SciTech Connect (OSTI)

    Perlmutter, M.A.; Radovich, B.J.; Matthews, M.D.

    1997-01-01

    Global cyclostratigraphy, a methodology that utilizes climate change to evaluate sediment flux, characterizes the impact of sediment cycles on stratigraphy. Climatic succession, sediment yield cycles, and the phase relationship of sediment cycles to eustatic cycles are all determined in the early stages of basin analysis. Sedimentologic information is then used to assist in sequence evaluations. Climatic successions are intrinsically associated with global position (paleogeography) and are not necessarily synchronous with glacioeustatic sea-level cycles. A preliminary evaluation of the effect of climate on sediment supply from modem river systems indicates that sediment yield may vary by well over two orders of magnitude during one climate cycle. Consequently, basins in different climatic belts can have distinctly different volumes and lithologies for systems tracts that have similar base-level changes. The stratigraphic computer program Sedpak was utilized to examine the possible impact of different sedimentation cycles on sequence interpretation and reservoir forecasts. The effect of sedimentation cycles on reservoir distribution in real world sequences is demonstrated with a comparison of the Miocene section of the Surma basin, Bangladesh, and the Plio-Pleistocene section of the Gulf of Mexico. In the Surma basin, reservoirs are most likely to occur in transgressive and highstand systems tracts, while reservoirs in the Gulf of Mexico are more likely in lowstand prograding complexes.

  12. Alum Innovative Exploration Project (Ram Power Inc.)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Miller, Clay

    Data generated from the Alum Innovative Exploration Project, one of several promising geothermal properties located in the middle to upper Miocene (~11-5 Ma, or million years BP) Silver Peak-Lone Mountain metamorphic core complex (SPCC) of the Walker Lane structural belt in Esmeralda County, west-central Nevada. The geothermal system at Alum is wholly concealed; its upper reaches discovered in the late 1970s during a regional thermal-gradient drilling campaign. The prospect boasts several shallow thermal-gradient (TG) boreholes with TG >75oC/km (and as high as 440oC/km) over 200-m intervals in the depth range 0-600 m. Possibly boiling water encountered at 239 m depth in one of these boreholes returned chemical- geothermometry values in the range 150-230oC. GeothermEx (2008) has estimated the electrical- generation capacity of the current Alum leasehold at 33 megawatts for 20 years; and the corresponding value for the broader thermal anomaly extending beyond the property at 73 megawatts for the same duration.

  13. Chapter 18: Variable Frequency Drive Evaluation Protocol

    SciTech Connect (OSTI)

    Romberger, J.

    2014-11-01

    An adjustable-speed drive (ASD) includes all devices that vary the speed of a rotating load, including those that vary the motor speed and linkage devices that allow constant motor speed while varying the load speed. The Variable Frequency Drive Evaluation Protocol presented here addresses evaluation issues for variable-frequency drives (VFDs) installed on commercial and industrial motor-driven centrifugal fans and pumps for which torque varies with speed. Constant torque load applications, such as those for positive displacement pumps, are not covered by this protocol. Other ASD devices, such as magnetic drive, eddy current drives, variable belt sheave drives, or direct current motor variable voltage drives, are also not addressed. The VFD is by far the most common type of ASD hardware. With VFD speed control on a centrifugal fan or pump motor, energy use follows the affinity laws, which state that the motor electricity demand is a cubic relationship to speed under ideal conditions. Therefore, if the motor runs at 75% speed, the motor demand will ideally be reduced to 42% of full load power; however, with other losses it is about 49% of full load power.

  14. High throughput optical scanner

    DOE Patents [OSTI]

    Basiji, David A. (Seattle, WA); van den Engh, Gerrit J. (Seattle, WA)

    2001-01-01

    A scanning apparatus is provided to obtain automated, rapid and sensitive scanning of substrate fluorescence, optical density or phosphorescence. The scanner uses a constant path length optical train, which enables the combination of a moving beam for high speed scanning with phase-sensitive detection for noise reduction, comprising a light source, a scanning mirror to receive light from the light source and sweep it across a steering mirror, a steering mirror to receive light from the scanning mirror and reflect it to the substrate, whereby it is swept across the substrate along a scan arc, and a photodetector to receive emitted or scattered light from the substrate, wherein the optical path length from the light source to the photodetector is substantially constant throughout the sweep across the substrate. The optical train can further include a waveguide or mirror to collect emitted or scattered light from the substrate and direct it to the photodetector. For phase-sensitive detection the light source is intensity modulated and the detector is connected to phase-sensitive detection electronics. A scanner using a substrate translator is also provided. For two dimensional imaging the substrate is translated in one dimension while the scanning mirror scans the beam in a second dimension. For a high throughput scanner, stacks of substrates are loaded onto a conveyor belt from a tray feeder.

  15. Automated remote control of fuel supply section for the coal fired power plant

    SciTech Connect (OSTI)

    Chudin, O.V.; Maidan, B.V.; Tsymbal, A.A.

    1996-05-01

    Approximately 6,000 miles east of Moscow, lays the city of Khabarovsk. This city`s coal-fired Power Plant 3 supplies electricity, heat and hot water to approximately 250,000 customers. Plant 3 has three units with a combined turbine capacity of 540 MW, (3 {times} 180) electrical and 780 (3 {times} 260) Gkal an hour thermal capacity with steam productivity of 2010 (3 {times} 670) tons per hour at 540 C. Coal fired thermal electric power plants rely on the equipment of the fuel supply section. The mechanism of the fuel supply section includes: conveyor belts, hammer crushers, guiding devices, dumping devices, systems for dust neutralizing, iron separators, metal detectors and other devices. As a rule, the fuel path in the power plant has three main directions: from the railroad car unloading terminal to the coal warehouse; from the coal warehouse to the acceptance bunkers of the power units, and the railroad car unloading terminal to the acceptance bunkers of power units. The fuel supply section always has a reserve and is capable of uninterruptible fuel supply during routine maintenance and/or repair work. This flexibility requires a large number of fuel traffic routes, some of which operate simultaneously with the feeding of coal from the warehouse to the acceptance bunkers of the power units, or in cases when rapid filling of the bunkers is needed, two fuel supply routes operate at the same time. The remote control of the fuel handling system at Power Plant 3 is described.

  16. MAGNETIC SHIELDING OF EXOMOONS BEYOND THE CIRCUMPLANETARY HABITABLE EDGE

    SciTech Connect (OSTI)

    Heller, Ren; Zuluaga, Jorge I. E-mail: jzuluaga@fisica.udea.edu.co

    2013-10-20

    With most planets and planetary candidates detected in the stellar habitable zone (HZ) being super-Earths and gas giants rather than Earth-like planets, we naturally wonder if their moons could be habitable. The first detection of such an exomoon has now become feasible, and due to observational biases it will be at least twice as massive as Mars. However, formation models predict that moons can hardly be as massive as Earth. Hence, a giant planet's magnetosphere could be the only possibility for such a moon to be shielded from cosmic and stellar high-energy radiation. Yet, the planetary radiation belt could also have detrimental effects on exomoon habitability. Here we synthesize models for the evolution of the magnetic environment of giant planets with thresholds from the runaway greenhouse (RG) effect to assess the habitability of exomoons. For modest eccentricities, we find that satellites around Neptune-sized planets in the center of the HZ around K dwarf stars will either be in an RG state and not be habitable, or they will be in wide orbits where they will not be affected by the planetary magnetosphere. Saturn-like planets have stronger fields, and Jupiter-like planets could coat close-in habitable moons soon after formation. Moons at distances between about 5 and 20 planetary radii from a giant planet can be habitable from an illumination and tidal heating point of view, but still the planetary magnetosphere would critically influence their habitability.

  17. DETECTION OF WIDESPREAD HYDRATED MATERIALS ON VESTA BY THE VIR IMAGING SPECTROMETER ON BOARD THE DAWN MISSION

    SciTech Connect (OSTI)

    De Sanctis, M. C.; Ammannito, E.; Palomba, E.; Longobardo, A.; Capaccioni, F.; Capria, M. T.; Tosi, F.; Zambon, F.; Carraro, F.; Fonte, S.; Frigeri, A.; Magni, G.; Combe, J.-Ph.; McCord, T. B.; Marchi, S.; Mittlefehldt, D. W.; Pieters, C. M.; Sunshine, J.; Raymond, C. A.; Russell, C. T.; and others

    2012-10-20

    Water plays a key role in the evolution of terrestrial planets, and notably in the occurrence of Earth's oceans. However, the mechanism by which water has been incorporated into these bodies-including Earth-is still extensively debated. Here we report the detection of widespread 2.8 {mu}m OH absorption bands on the surface of the asteroid Vesta by the VIR imaging spectrometer on board Dawn. These observations are surprising as Vesta is fully differentiated with a basaltic surface. The 2.8 {mu}m OH absorption is distributed across Vesta's surface and shows areas enriched and depleted in hydrated materials. The uneven distribution of hydrated mineral phases is unexpected and indicates ancient processes that differ from those believed to be responsible for OH on other airless bodies, like the Moon. The origin of Vestan OH provides new insight into the delivery of hydrous materials in the main belt and may offer new scenarios on the delivery of hydrous minerals in the inner solar system, suggesting processes that may have played a role in the formation of terrestrial planets.

  18. Investigation of EMIC wave scattering as the cause for the BARREL 17 January 2013 relativistic electron precipitation event: A quantitative comparison of simulation with observations

    SciTech Connect (OSTI)

    Li, Zan; Millan, Robyn M.; Hudson, Mary K.; Woodger, Leslie A.; Smith, David M.; Chen, Yue; Friedel, Reiner; Rodriguez, Juan V.; Engebretson, Mark J.; Goldstein, Jerry; Fennell, Joseph F.; Spence, Harlan E.

    2014-12-23

    Electromagnetic ion cyclotron (EMIC) waves were observed at multiple observatory locations for several hours on 17 January 2013. During the wave activity period, a duskside relativistic electron precipitation (REP) event was observed by one of the Balloon Array for Radiation belt Relativistic Electron Losses (BARREL) balloons and was magnetically mapped close to Geostationary Operational Environmental Satellite (GOES) 13. We simulate the relativistic electron pitch angle diffusion caused by gyroresonant interactions with EMIC waves using wave and particle data measured by multiple instruments on board GOES 13 and the Van Allen Probes. We show that the count rate, the energy distribution, and the time variation of the simulated precipitation all agree very well with the balloon observations, suggesting that EMIC wave scattering was likely the cause for the precipitation event. The event reported here is the first balloon REP event with closely conjugate EMIC wave observations, and our study employs the most detailed quantitative analysis on the link of EMIC waves with observed REP to date.

  19. Vulnerability to closing of Hormuz

    SciTech Connect (OSTI)

    Not Available

    1984-03-07

    Tankers carrying roughly 8-million barrels per day (mmb/d) of crude oil, or some 16% of the non-communist world's oil supply, pass through the Strait of Hormuz. Experts agree that just 3-mmb/d of that could be exported through alternate routes. If the war between Iran and Iraq should result in their completely halting each other's production, this relatively limited supply curtailment would reduce world oil production by over 3.4-mmb/d. Since the two have not caused such mutual disaster during four years of war, many observers believe there has been a deliberate avoidance of the jugular squeeze. Nevertheless, the two combatants appear capable not only of cutting off their oil production, but escalating fighting to the point where Gulf traffic would be impeded. Potential results from a prolonged Iran-Iraq crisis are viewed in three scenarios. Also included in this issue are brief summaries of: (1) Mexico's new energy plan, internationalism, and OPEC; (2) update on Argentina's energy resource developments; (3) Venezuela: belt tightening; (4) Western Hemisphere oil production declines; (5) (6) days of oil supply for Canada, USA, Japan, France, Italy, and UK; and (6) US Department of Defense fuel consumption. The Energy Detente fuel price/tax series and principal industrial fuel prices are included for March for countries of the Eastern Hemisphere.

  20. Method of processing "BPS" glass ceramic and seals made therewith

    DOE Patents [OSTI]

    Reed, Scott T. (Albuquerque, NM); Stone, Ronald G. (Albuquerque, NM); McCollister, Howard L. (Albuquerque, NM); Wengert, deceased, Paul R. (late of Albuquerque, NM)

    1998-01-01

    A glass ceramic composition, a glass ceramic-to-metal seal, and more specifically a hermetic glass ceramic-to-metal seal prepared by subjecting a glass composition comprising, by weight percent, SiO.sub.2 (65-80%), LiO.sub.2 (8-16%), Al.sub.2 O.sub.3 (2-8%), K.sub.2 O (1-8%), P.sub.2 O.sub.5 (1-5%), B.sub.2 O.sub.3 (0.5-7%), and ZnO (0-5%) to the following processing steps: 1) heating the glass composition in a belt furnace to a temperature sufficient to melt the glass and crystallize lithium phosphate, 2) holding at a temperature and for a time sufficient to create cristobalite nuclei, 3) cooling at a controlled rate and to a temperature to cause crystallization of lithium silicates and growth of cristobalite, and 4) still further cooling in stages to ambient temperature. This process produces a glass ceramic whose high coefficient of thermal expansion (up to 200.times.10.sup.-7 in/in/.degree.C.) permits the fabrication of glass ceramic-to-metal seals, and particularly hermetic glass ceramic seals to nickel-based and stainless steel alloys and copper.

  1. Co-combustion feasibility study. Final report

    SciTech Connect (OSTI)

    Handcock, D.J.

    1995-01-01

    This report investigates the technical and economic feasibility of co-combusting municipal sewage sludge produced by the Saratoga County Sewer District No. 1 with paper mill sludge produced by the Cottrell Paper Company, Encore Paper Company, International Paper Company, Mohawk Paper Mills, and TAGSONS Papers at the Saratoga County Sewer District No. 1`s secondary wastewater treatment plant and recovering any available energy products. The co-combustion facility would consist of sludge and wood chip storage and conveying systems, belt filter presses, screw presses, fluidized-bed incinerators, venturi scrubbers and tray cooling systems, ash dewatering facilities, heat recovery steam generators, gas-fired steam superheaters, and a back-pressure steam turbine system. Clean waste wood chips would be used as an auxiliary fuel in the fluidized-bed incinerators. It is recommended that the ash produced by the proposed facility be beneficially used, potentially as a raw material in the manufacture of cement and/or as an interim barrier layer in landfills.

  2. Method and apparatus for container leakage testing

    DOE Patents [OSTI]

    Kronberg, James W. (Aiken, SC)

    1995-01-01

    An apparatus for use in one-hundred percent leak testing of food containers used in conjunction with a tracer gas. The apparatus includes a shell with entrance and exit air locks to create a controlled atmosphere through which a series of containers is conveyed by a conveyor belt. The pressure in the shell is kept lower than the pressure in the containers and the atmosphere is made to flow with the containers so that a tracer gas placed in the packages before sealing them will leak more readily, but the leaked tracer gas will remain associated with the leaking package as it moves through the shell. The leaks are detected with a sniffer probe in fluid communication with a gas chromatograph. The gas chromatograph issues a signal when it detects a leak to an ejector that will eject the leaking container from the conveyor. The system is timed so that the series of containers can move continuously into and out of the shell, past the probe and the ejector, without stopping, yet each package is tested for leaks and removed if leaking.

  3. Integration of geothermal data along the Balcones/Ouachita trend, central Texas. Final report

    SciTech Connect (OSTI)

    Woodruff, C.M. Jr.; Gever, C.; Snyder, Fred R.; Wuerch, David Robert

    1983-01-01

    This report presents data that address possible controls on warm-water resources. Data are presented on a series of maps, and interpretations appear in the brief text accompanying the maps. It is thought that structural controls provided by the Balcones Fault Zone on the west and by the Luling-Mexia-Talco Fault Zone on the east localize the warm waters. The ultimate controlling attribute is the foundered Ouachita structural belt, which, in turn, has controlled the orientation and magnitude of displacement of the superjacent normal fault systems. This thesis is supported by maps (in pocket) showing the following: distribution of thermal waters measured in wells along the Balcones/Ouachita structural trend showing water temperature in /sup 0/F, total depth of the well measured, water salinity in parts per million, and the geologic formation producing the water; structural contours on the base of the Cretaceous System showing the configuration of the Paleozoic Ouachita basement; structural configuration of the Balcones and Luling Fault Zone, Mexia and Talco Fault Zone, and foreland areas adjacent to the Ouachita Orogen using data from the Buda Limestone, Sligo Formation, and Ellenburger Group; Landsat lineaments and Bouguer gravity contours; and geothermal gradient contours of the Balcones/Ouachita trend based on thermal values from Paleozoic and selected Mesozoic formations.

  4. A background correction algorithm for Van Allen Probes MagEIS electron flux measurements

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Claudepierre, S. G.; O'Brien, T. P.; Blake, J. B.; Fennell, J. F.; Roeder, J. L.; Clemmons, J. H.; Looper, M. D.; Mazur, J. E.; Mulligan, T. M.; Spence, H. E.; et al

    2015-07-14

    We describe an automated computer algorithm designed to remove background contamination from the Van Allen Probes Magnetic Electron Ion Spectrometer (MagEIS) electron flux measurements. We provide a detailed description of the algorithm with illustrative examples from on-orbit data. We find two primary sources of background contamination in the MagEIS electron data: inner zone protons and bremsstrahlung X-rays generated by energetic electrons interacting with the spacecraft material. Bremsstrahlung X-rays primarily produce contamination in the lower energy MagEIS electron channels (~30–500 keV) and in regions of geospace where multi-M eV electrons are present. Inner zone protons produce contamination in all MagEIS energymore » channels at roughly L < 2.5. The background-corrected MagEIS electron data produce a more accurate measurement of the electron radiation belts, as most earlier measurements suffer from unquantifiable and uncorrectable contamination in this harsh region of the near-Earth space environment. These background-corrected data will also be useful for spacecraft engineering purposes, providing ground truth for the near-Earth electron environment and informing the next generation of spacecraft design models (e.g., AE9).« less

  5. Material handling systems for use in glovebox lines: A survey of Department of Energy facility experience

    SciTech Connect (OSTI)

    Teese, G.D.; Randall, W.J.

    1992-01-01

    The Nuclear Weapons Complex Reconfiguration Study has recommended that a new manufacturing facility be constructed to replace the Rocky Flats Plant. In the new facility, use of an automated material handling system for movement of components would reduce both the cost and radiation exposure associated with production and maintenance operations. Contamination control would be improved between process steps through the use of airlocks and portals. Part damage associated with improper transport would be reduced, and accountability would be increased. In-process workpieces could be stored in a secure vault, awaiting a request for parts at a production station. However, all of these desirable features rely on the proper implementation of an automated material handling system. The Department of Energy Weapons Production Complex has experience with a variety of methods for transporting discrete parts in glovebox lines. The authors visited several sites to evaluate the existing technologies for their suitability for the application of plutonium manufacturing. Technologies reviewed were Linear motors, belt conveyors, roller conveyors, accumulating roller conveyors, pneumatic transport, and cart systems. The sites visited were The Idaho National Engineering laboratory, the Hanford Site, and the Rocky Flats Plant. Linear motors appear to be the most promising technology observed for the movement of discrete parts, and further investigation is recommended.

  6. Project Overcoat An Exploration of Exterior Insulation Strategies for 1- Story Roof Applications in Cold Climates

    SciTech Connect (OSTI)

    Ojczyk, Cindy; Mosiman, Garrett; Huelman, Pat; Schirber, Tom; Yost, Peter; Murry, Tessa

    2013-04-01

    The development of an alternative method to interior-applied insulation strategies or exterior applied band-aids such as heat tapes and ice belts may help reduce energy needs of millions of 1-1/2 story homes while reducing the risk of ice dam formation. A potential strategy for energy improvement of the roof is borrowed from new construction best practices: Here an overcoat of a continuous air, moisture, and thermal barrier is applied on the outside of the roof structure for improved overall performance. The continuous insulation of this approach facilitates a reduction in thermal bridging which could further reduce energy consumption and bring existing homes closer to meeting the Building America goals for energy reduction. Research favors an exterior approach to deep energy retrofits and ice dam prevention in existing homes. The greatest amount of research focuses on whole house deep energy retrofits leaving a void in roof-only applications. The research is also void of data supporting the hygrothermal performance, durability, constructability, and cost of roof-only exterior overcoat strategies. Yet, contractors interviewed for this report indicate an understanding that exterior approaches are most promising for mitigating ice dams and energy loss and are able to sell these strategies to homeowners.

  7. Structural investigations of Great Basin geothermal fields: Applications and implications

    SciTech Connect (OSTI)

    Faulds, James E; Hinz, Nicholas H.; Coolbaugh, Mark F

    2010-11-01

    Because fractures and faults are commonly the primary pathway for deeply circulating hydrothermal fluids, structural studies are critical to assessing geothermal systems and selecting drilling targets for geothermal wells. Important tools for structural analysis include detailed geologic mapping, kinematic analysis of faults, and estimations of stress orientations. Structural assessments are especially useful for evaluating geothermal fields in the Great Basin of the western USA, where regional extension and transtension combine with high heat flow to generate abundant geothermal activity in regions having little recent volcanic activity. The northwestern Great Basin is one of the most geothermally active areas in the USA. The prolific geothermal activity is probably due to enhanced dilation on N- to NNE-striking normal faults induced by a transfer of NW-directed dextral shear from the Walker Lane to NW-directed extension. Analysis of several geothermal fields suggests that most systems occupy discrete steps in normal fault zones or lie in belts of intersecting, overlapping, and/or terminating faults. Most fields are associated with steeply dipping faults and, in many cases, with Quaternary faults. The structural settings favoring geothermal activity are characterized by subvertical conduits of highly fractured rock along fault zones oriented approximately perpendicular to the WNW-trending least principal stress. Features indicative of these settings that may be helpful in guiding exploration for geothermal resources include major steps in normal faults, interbasinal highs, groups of relatively low discontinuous ridges, and lateral jogs or terminations of mountain ranges.

  8. Material handling systems for use in glovebox lines: A survey of Department of Energy facility experience

    SciTech Connect (OSTI)

    Teese, G.D.; Randall, W.J.

    1992-12-31

    The Nuclear Weapons Complex Reconfiguration Study has recommended that a new manufacturing facility be constructed to replace the Rocky Flats Plant. In the new facility, use of an automated material handling system for movement of components would reduce both the cost and radiation exposure associated with production and maintenance operations. Contamination control would be improved between process steps through the use of airlocks and portals. Part damage associated with improper transport would be reduced, and accountability would be increased. In-process workpieces could be stored in a secure vault, awaiting a request for parts at a production station. However, all of these desirable features rely on the proper implementation of an automated material handling system. The Department of Energy Weapons Production Complex has experience with a variety of methods for transporting discrete parts in glovebox lines. The authors visited several sites to evaluate the existing technologies for their suitability for the application of plutonium manufacturing. Technologies reviewed were Linear motors, belt conveyors, roller conveyors, accumulating roller conveyors, pneumatic transport, and cart systems. The sites visited were The Idaho National Engineering laboratory, the Hanford Site, and the Rocky Flats Plant. Linear motors appear to be the most promising technology observed for the movement of discrete parts, and further investigation is recommended.

  9. Sensitivity of a global climate model to the critical Richardson number in the boundary layer parameterization

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Zhang, Ning; Liu, Yangang; Gao, Zhiqiu; Li, Dan

    2015-04-27

    The critical bulk Richardson number (Ricr) is an important parameter in planetary boundary layer (PBL) parameterization schemes used in many climate models. This paper examines the sensitivity of a Global Climate Model, the Beijing Climate Center Atmospheric General Circulation Model, BCC_AGCM to Ricr. The results show that the simulated global average of PBL height increases nearly linearly with Ricr, with a change of about 114 m for a change of 0.5 in Ricr. The surface sensible (latent) heat flux decreases (increases) as Ricr increases. The influence of Ricr on surface air temperature and specific humidity is not significant. The increasingmore » Ricr may affect the location of the Westerly Belt in the Southern Hemisphere. Further diagnosis reveals that changes in Ricr affect stratiform and convective precipitations differently. Increasing Ricr leads to an increase in the stratiform precipitation but a decrease in the convective precipitation. Significant changes of convective precipitation occur over the inter-tropical convergence zone, while changes of stratiform precipitation mostly appear over arid land such as North Africa and Middle East.« less

  10. Rhythmic bedding patterns for locating structural features, Niobrara Formation, United States western interior

    SciTech Connect (OSTI)

    Laferriere, A.P.; Hattin, D.E.

    1989-05-01

    Milankovitch-type bedding cycles are well developed in the Upper Cretaceous Fort Hays Limestone Member, Niobrara Formation. These time-equivalent cycles can be correlated across much of Colorado, Kansas, and northeastern New Mexico by combining subsurface and outcrop data. Documentation of thickness variations within the regionally persistent Fort Hays bedding sequences furnishes a basis for fine-scale analysis of Late Cretaceous crustal movements within the eastern ramp region of the Western Interior foreland basin. Regional thickness changes in groups of shale-limestone couplets were correlated and mapped in outcrop and in the subsurface to locate structural elements that influenced Fort Hays deposition. In the Denver-Julesburg basin of Colorado and western Kansas, up to 6.1 m (20 ft) of thinning of the section occurs dominantly along northeastwardly trending belts formed during Late Cretaceous reactivation of the Transcontinental arch. Mapping of these small-scale thickness changes in the Fort Hays demonstrates that Cretaceous reactivation of the Transcontinental arch was not restricted to the northern part of the Denver-Julesburg basin. Additional structures may occur as far south as the Colorado-New Mexico border. A northwestwardly thinning trend is also apparent and may have resulted from increased compaction and diagenesis, reduction of sediment input during transgression, or from uplift in the vicinity of the Colorado Front Range. 8 figures.

  11. Megaregional seismic approach to new play concept development

    SciTech Connect (OSTI)

    Bertagne, A.J.; Vuillermoz, C.; Maxwell, R.A.

    1989-03-01

    A megaregional seismic line is a continuous line that traverses more than one basin. After such a line is interpreted using well control, surface geology, and other available data, it serves as a concise expression of our understanding of the geology along a transect and provides a starting point for developing new play concepts. Megaregional seismic lines aid in the development of exploration concepts by providing new insights into (1) what is and is not basement, (2) maturation history and migration pathways, (3) regional structural geology, and (4) regional stratigraphy. An ongoing project to prepare a series of interpreted transcontinental megaregional seismic lines uses a segment that starts in the Arkoma basin of Oklahoma, traverses the Ouachita thrust belt, and terminates at the northern Texas Gulf coastal plain. This segment shows that several potential plays exist, both structural and stratigraphic, between areas of current exploration activity. Regional seismic lines from the Sacramento Valley and the Illinois basin further illustrate how interpretation of long seismic lines can lead to new exploration ideas.

  12. Productivity genefits from new energy technology: A case study of a paint manufacturing company

    SciTech Connect (OSTI)

    Raghunathan, P.; Capehart, B.L.

    1997-06-01

    In many cases, implementing new energy efficiency technologies not only helps facilities reduce their energy costs, but it also creates greater profits by increasing productivity. These added benefits from productivity improvements can sometimes be greater than the energy cost savings, and can result in an attractive overall payback period for implementing the new technology. This paper presents a case study of productivity improvement at a paint manufacturing company as a result of implementing new energy efficiency technology. During an industrial energy assessment, it was noted that the company had experienced frequent failures of motor belts and sheaves on five paint mixers resulting in significant replacement costs and labor costs. In addition, a bigger loss was being suffered due to lost potential profit associated with the frequent work stoppages. The IAC recommendation was to install motor soft starters (also known as motor voltage controllers) on the five mixing machines. Installation of soft starters would have the following benefits: lower energy costs, lower replacement costs for transmission components, lower labor costs, and higher production levels and increased profits. The total annual benefits were estimated at $122,659, of which the benefits from increased productivity were nearly $67,000. The overall simple payback period for installing the soft starters was less than 2 months.

  13. Adsorbed sulfur-gas methods for both near-surface exploration and downhole logging

    SciTech Connect (OSTI)

    Farwell, S.O.; Barinaga, C.J.; Dolenc, M.R.; Farwell, G.H.

    1986-08-01

    The use of sulfur-containing gases in petroleum exploration is supported by (1) the idea that sulfur may play a role in petroleum genesis, (2) the corresponding existence of sulfur-containing compounds in petroleum and the potential for vertical migration of the low-molecular-weight sulfur species from these reservoirs, (3) the production of H/sub 2/S by anaerobic microorganism populations that develop in the subsurface areas overlying petroleum reservoirs due to the concomitant supply of hydrocarbon nutrients, (4) the recent discovery of near-surface accumulations of pyrite and marcasite as the source of induction potential anomalies over certain fields, and (5) the strong adsorptive affinities of sulfur gases to solid surfaces, which enhance both the concentration and localization of such sulfur-expressed anomalies. During the past 3 years, numerous near-surface soil samples and well cuttings from the Utah-Wyoming Overthrust belt have been analyzed for adsorbed sulfur-gas content by two novel analytical techniques: thermal desorption/metal foil collection/flash desorption/sulfur-selective detection (TD/MFC/FD/SSD) and thermal desorption/cryogenic preconcentration/high-resolution-gas chromatography/optimized-flame photometry (TD/CP/HRGC/OFP).

  14. LANDSCAPE MANAGEMENT FOR SUSTAINABLE SUPPLIES OF BIOENERGY FEEDSTOCK AND ENHANCED SOIL QUALITY

    SciTech Connect (OSTI)

    Douglas L. Karlen; David J. Muth, Jr.

    2012-09-01

    Agriculture can simultaneously address global food, feed, fiber, and energy challenges provided our soil, water, and air resources are not compromised in doing so. As we embark on the 19th Triennial Conference of the International Soil and Tillage Research Organization (ISTRO), I am pleased to proclaim that our members are well poised to lead these endeavors because of our comprehensive understanding of soil, water, agricultural and bio-systems engineering processes. The concept of landscape management, as an approach for integrating multiple bioenergy feedstock sources, including biomass residuals, into current crop production systems, is used as the focal point to show how these ever-increasing global challenges can be met in a sustainable manner. Starting with the 2005 Billion Ton Study (BTS) goals, research and technology transfer activities leading to the 2011 U.S. Department of Energy (DOE) Revised Billion Ton Study (BT2) and development of a residue management tool to guide sustainable crop residue harvest will be reviewed. Multi-location USDA-Agricultural Research Service (ARS) Renewable Energy Assessment Project (REAP) team research and on-going partnerships between public and private sector groups will be shared to show the development of landscape management strategies that can simultaneously address the multiple factors that must be balanced to meet the global challenges. Effective landscape management strategies recognize the importance of natures diversity and strive to emulate those conditions to sustain multiple critical ecosystem services. To illustrate those services, the soil quality impact of harvesting crop residues are presented to show how careful, comprehensive monitoring of soil, water and air resources must be an integral part of sustainable bioenergy feedstock production systems. Preliminary analyses suggest that to sustain soil resources within the U.S. Corn Belt, corn (Zea mays L.) stover should not be harvested if average grain yields are less than 11 Mg ha-1 (175 bu ac-1) unless more intensive landscape management practices are implemented. Furthermore, although non-irrigated corn grain yields east and west of the primary Corn Belt may not consistently achieve the 11 Mg ha-1 yield levels, corn can still be part of an overall landscape approach for sustainable feedstock production. Another option for producers with consistently high yields (> 12.6 Mg ha-1 or 200 bu ac-1) that may enable them to sustainably harvest even more stover is to decrease their tillage intensity which will reduce fuel use, preserve rhizosphere carbon, and/or help maintain soil structure and soil quality benefits often attributed to no-till production systems. In conclusion, I challenge all ISTRO scientists to critically ask if your research is contributing to improved soil and crop management strategies that effectively address the complexity associated with sustainable food, feed, fiber and fuel production throughout the world.

  15. Sub-crop geologic map of pre-Tertiary rocks in the Yucca Flat and northern Frenchman Flat areas, Nevada Test Site, southern Nevada

    SciTech Connect (OSTI)

    Cole, J.C.; Harris, A.G.; Wahl, R.R.

    1997-10-02

    This map displays interpreted structural and stratigraphic relations among the Paleozoic and older rocks of the Nevada Test Site region beneath the Miocene volcanic rocks and younger alluvium in the Yucca Flat and northern Frenchman Flat basins. These interpretations are based on a comprehensive examination and review of data for more than 77 drillholes that penetrated part of the pre-Tertiary basement beneath these post-middle Miocene structural basins. Biostratigraphic data from conodont fossils were newly obtained for 31 of these holes, and a thorough review of all prior microfossil paleontologic data is incorporated in the analysis. Subsurface relationships are interpreted in light of a revised regional geologic framework synthesized from detailed geologic mapping in the ranges surrounding Yucca Flat, from comprehensive stratigraphic studies in the region, and from additional detailed field studies on and around the Nevada Test Site. All available data indicate the subsurface geology of Yucca Flat is considerably more complicated than previous interpretations have suggested. The western part of the basin, in particular, is underlain by relics of the eastward-vergent Belted Range thrust system that are folded back toward the west and thrust by local, west-vergent contractional structures of the CP thrust system. Field evidence from the ranges surrounding the north end of Yucca Flat indicate that two significant strike-slip faults track southward beneath the post-middle Miocene basin fill, but their subsurface traces cannot be closely defined from the available evidence. In contrast, the eastern part of the Yucca Flat basin is interpreted to be underlain by a fairly simple north-trending, broad syncline in the pre-Tertiary units. Far fewer data are available for the northern Frenchman Flat basin, but regional analysis indicates the pre-Tertiary structure there should also be relatively simple and not affected by thrusting. This new interpretation has implications for ground water flow through pre-Tertiary rocks beneath the Yucca Flat and northern Frenchman Flat areas, and has consequences for ground water modeling and model validation. Our data indicate that the Mississippian Chainman Shale is not laterally extensive confining unit in the western part of the basin because it is folded back onto itself by the convergent structures of the Belted Range and CP thrust systems. Early and Middle Paleozoic limestone and dolomite are present beneath most of both basins and, regardless of structural complications, are interpreted to form a laterally continuous and extensive carbonate aquifer. Structural culmination that marks the French Peak accommodation zone along the topographic divide between the two basins provides a lateral pathway through highly fractured rock between the volcanic aquifers of Yucca Flat and the regional carbonate aquifer. This pathway may accelerate the migration of ground-water contaminants introduced by underground nuclear testing toward discharge areas beyond the Nevada Test Site boundaries. Predictive three-dimensional models of hydrostratigraphic units and ground-water flow in the pre-Tertiary rocks of subsurface Yucca Flat are likely to be unrealistic due to the extreme structural complexities. The interpretation of hydrologic and geochemical data obtained from monitoring wells will be difficult to extrapolate through the flow system until more is known about the continuity of hydrostratigraphic units. 1 plate

  16. MAJOR OIL PLAYS IN UTAH AND VICINITY

    SciTech Connect (OSTI)

    Thomas C. Chidsey; Craig D. Morgan; Kevin McClure; Grant C. Willis

    2003-09-01

    Utah oil fields have produced over 1.2 billion barrels (191 million m{sup 3}). However, the 13.7 million barrels (2.2 million m{sup 3}) of production in 2002 was the lowest level in over 40 years and continued the steady decline that began in the mid-1980s. The Utah Geological Survey believes this trend can be reversed by providing play portfolios for the major oil-producing provinces (Paradox Basin, Uinta Basin, and thrust belt) in Utah and adjacent areas in Colorado and Wyoming. Oil plays are geographic areas with petroleum potential caused by favorable combinations of source rock, migration paths, reservoir rock characteristics, and other factors. The play portfolios will include: descriptions and maps of the major oil plays by reservoir; production and reservoir data; case-study field evaluations; summaries of the state-of-the-art drilling, completion, and secondary/tertiary techniques for each play; locations of major oil pipelines; descriptions of reservoir outcrop analogs; and identification and discussion of land use constraints. All play maps, reports, databases, and so forth, produced for the project will be published in interactive, menu-driven digital (web-based and compact disc) and hard-copy formats. This report covers research activities for the fourth quarter of the first project year (April 1 through June 30, 2003). This work included describing outcrop analogs to the Jurassic Nugget Sandstone and Pennsylvanian Paradox Formation, the major oil producers in the thrust belt and Paradox Basin, respectively. Production-scale outcrop analogs provide an excellent view, often in three dimensions, of reservoir-facies characteristics and boundaries contributing to the overall heterogeneity of reservoir rocks. They can be used as a ''template'' for evaluation of data from conventional core, geophysical and petrophysical logs, and seismic surveys. The Nugget Sandstone was deposited in an extensive dune field that extended from Wyoming to Arizona. Outcrop analogs are found in the stratigraphically equivalent Navajo Sandstone of southern Utah which displays large-scale dunal cross-strata with excellent reservoir properties and interdunal features such as oases, wadi, and playa lithofacies with poor reservoir properties. Hydrocarbons in the Paradox Formation are stratigraphically trapped in carbonate buildups (or phylloid-algal mounds). Similar carbonate buildups are exposed in the Paradox along the San Juan River of southeastern Utah. Reservoir-quality porosity may develop in the types of facies associated with buildups such as troughs, detrital wedges, and fans, identified from these outcrops. When combined with subsurface geological and production data, these outcrop analogs can improve (1) development drilling and production strategies such as horizontal drilling, (2) reservoir-simulation models, (3) reserve calculations, and (4) design and implementation of secondary/tertiary oil recovery programs and other best practices used in the oil fields of Utah and vicinity. During this quarter, technology transfer activities consisted of exhibiting the project plans, objectives, and products at a booth at the 2003 annual convention of the American Association of Petroleum Geologists. The project home page was updated on the Utah Geological Survey Internet web site.

  17. The Mississippian Leadville Limestone Exploration Play, Utah and Colorado-Exploration Techniques and Studies for Independents

    SciTech Connect (OSTI)

    Thomas Chidsey

    2008-09-30

    The Mississippian (late Kinderhookian to early Meramecian) Leadville Limestone is a shallow, open-marine, carbonate-shelf deposit. The Leadville has produced over 53 million barrels (8.4 million m{sup 3}) of oil/condensate from seven fields in the Paradox fold and fault belt of the Paradox Basin, Utah and Colorado. The environmentally sensitive, 7500-square-mile (19,400 km{sup 2}) area that makes up the fold and fault belt is relatively unexplored. Only independent producers operate and continue to hunt for Leadville oil targets in the region. The overall goal of this study is to assist these independents by (1) developing and demonstrating techniques and exploration methods never tried on the Leadville Limestone, (2) targeting areas for exploration, (3) increasing deliverability from new and old Leadville fields through detailed reservoir characterization, (4) reducing exploration costs and risk especially in environmentally sensitive areas, and (5) adding new oil discoveries and reserves. The final results will hopefully reduce exploration costs and risks, especially in environmentally sensitive areas, and add new oil discoveries and reserves. The study consists of three sections: (1) description of lithofacies and diagenetic history of the Leadville at Lisbon field, San Juan County, Utah, (2) methodology and results of a surface geochemical survey conducted over the Lisbon and Lightning Draw Southeast fields (and areas in between) and identification of oil-prone areas using epifluorescence in well cuttings from regional wells, and (3) determination of regional lithofacies, description of modern and outcrop depositional analogs, and estimation of potential oil migration directions (evaluating the middle Paleozoic hydrodynamic pressure regime and water chemistry). Leadville lithofacies at Libon field include open marine (crinoidal banks or shoals and Waulsortian-type buildups), oolitic and peloid shoals, and middle shelf. Rock units with open-marine and restricted-marine facies constitute a significant reservoir potential, having both effective porosity and permeability when dissolution of skeletal grains, followed by dolomitization, has occurred. Two major types of diagenetic dolomite are observed in the Leadville Limestone at Lisbon field: (1) tight 'early' dolomite consisting of very fine grained (<5 {micro}m), interlocking crystals that faithfully preserve depositional fabrics; and (2) porous, coarser (>100-250 {micro}m), rhombic and saddle crystals that discordantly replace limestone and earlier very fine grained dolomite. Predating or concomitant with late dolomite formation are pervasive leaching episodes that produced vugs and extensive microporosity. Most reservoir rocks within Lisbon field appear to be associated with the second, late type of dolomitization and associated leaching events. Other diagenetic products include pyrobitumen, syntaxial cement, sulfide minerals, anhydrite cement and replacement, and late macrocalcite. Fracturing (solution enlarged) and brecciation (autobrecciation) caused by hydrofracturing are widespread within Lisbon field. Sediment-filled cavities, related to karstification of the exposed Leadville, are present in the upper third of the formation. Pyrobitumen and sulfide minerals appear to coat most crystal faces of the rhombic and saddle dolomites. The fluid inclusion and mineral relationships suggest the following sequence of events: (1) dolomite precipitation, (2) anhydrite deposition, (3) anhydrite dissolution and quartz precipitation, (4) dolomite dissolution and late calcite precipitation, (5) trapping of a mobile oil phase, and (6) formation of bitumen. Fluid inclusions in calcite and dolomite display variable liquid to vapor ratios suggesting reequilibration at elevated temperatures (50 C). Fluid salinities exceed 10 weight percent NaCl equivalent. Low ice melting temperatures of quartz- and calcite-hosted inclusions suggest chemically complex Ca-Mg-bearing brines associated with evaporite deposits were responsible for mineral deposition. The overall conclusion from th

  18. Organic matter distribution in the flysch deposits of the Marnoso-Arenacea formation, miocene, northern Apennines, Italy

    SciTech Connect (OSTI)

    Mosca, F.; Stefano, D. )

    1993-09-01

    The Marnoso-Arenacea Formation represents the filling of the Miocene Apennine foredeep by widespread and thick turbidite systems. Based on stratigraphic and sedimentologic considerations, two major sequences, related to the development of the Apennine orogene and to migration toward northeast of the depocenters, have been recognized. In both these units, respectively, upper Burdigalian-Serravallian and uppermost Serravallian-Tortonian, a major foredeep and a piggyback basin belt coexisted. The former is characterized by the development of depositional lobes down current passing to basin plain deposits; the latter were filled mostly by channel-levee-slope fine-grained deposits. To evaluate the petroleum potential of the different facies associations recognized within the Marnoso-Arenacea Formation, 300 samples were collected along the Santerno Valley type section and analyzed by using the basic geochemical methods. A preliminary space-time model concerning the distribution and nature of the naphtogenic facies in a foredeep basin has been developed. In particular, the average organic carbon content vs. hydrogen index and petroleum potential shows that the preservation of organic matter seems to be better in the basin plain than in associations, but of different age, show significant variation in the petroleum potential (S2) and in the hydrogen index (HI). These variations do not reflect changes in the organic input, as pointed out by kerogen composition and gc-ms analyses, but are related to different sedimentation rates during the Miocene. The best condition for organic matter preservation seems to be related to medium to high sedimentation rates, whereas low rates lead to a more diffused oxidation. This is true for similar paleoenvironmental conditions with the same organic productivity. However, it is important to point that very high sedimentation rates can lead to a dilution of the organic matter in the siliciclastic fraction.

  19. Tectonic and sedimentary evolution of the Luna field area, Italy

    SciTech Connect (OSTI)

    Roveri, M. )

    1990-05-01

    The Luna gas field is located near Crotone (Calabria region, southern Italy) in a shallow-water/onshore area. It was discovered and put into production during the early 1970s. Up to now it has produced 19 {times} 10{sup 9} sm{sup 3} of gas; its productivity (50 {times} 10{sup 6} sm{sup 3}/y) has remained virtually unaltered since the beginning. The field is located on the axial culmination of a thrust-related anticline of the Apennine postcollisional thrust belt; it can be roughly subdivided into two areas characterized by different stratigraphic contexts. In the northern and central parts of the field is a structural trap. Reservoir rocks are Serravallian to Tortonian deep marine resedimented conglomerates and sandstones. These deposits represent part of the infill of a middle-upper Miocene foredeep. Reservoir rocks are now thrusted, eroded, and unconformably overlain by lower Pliocene shales, which are the most important seal in this part of the field. In the southern part of the field is a combination trap. Reservoir rocks are upper Tortonian shallow-water sandstones. They lap onto a Tortonian unconformity related to a tectonic phase which split the previous foredeep into minor piggyback basins. The upper Tortonian sandstones are overlain and sealed by Messinian shales and evaporites. Tectonosedimentary evolution of the area and, consequently, areal distribution and geometry of sedimentary bodies - both potential reservoirs and seals - have been reconstructed using a sequence stratigraphy approach. The sedimentary record has been informally subdivided into five main depositional sequences bounded by unconformities or their correlative conformities; classic facies analysis and petrophysical, seismic, and biostratigraphic data have been utilized to define the internal characteristics of each sequence.

  20. Cerreto di Spoleto (Umbria-Italy): Seismic amplification at the ENEA local array stations

    SciTech Connect (OSTI)

    Rinaldis, Dario

    2008-07-08

    The Nerina valley, where Borgo Cerreto is located, is surrounded by the Apennine mount chain at the top of which lies the historical centre of Cerreto di Spoleto. The study is part of a research project aiming at analysing natural disasters and their impact on the Italian cultural heritage. Within the framework of this research project, local seismic records were analysed for both the carbonate ridge and the bordering alluvial valley. The choice of Cerreto di Spoleto as a test site derives from the analysis of Italian seismic hazard maps, obtained in terms of peak ground velocity and taking into account regional geology. The maps highlight the considerable seismic hazard which characterises the Apennine belt and its possible increase due to the effect of alluvial deposits. To this aim, ENEA installed in the 80's an accelerometric array (CODISMA up to 2000 and, in the following years, ETNA; for more detailed description see [1]. The 14 October event, was recorded both at the roof of CSM and at BCT stations. This is important to check the features observed comparing the FAS of acceleration at CSM and BCT during the 26 September events. Unfortunately the station at CSM basement did not record the above mentioned events but several aftershocks were recorded at each array station. Velocimetric records of both ambient noise and small-magnitude earthquakes were analysed in order to identify amplification conditions. The analysis was carried out in the time domain, through directional energy evaluation, and in the frequency domain, through H/V spectral ratios and spectral ratios with respect to a reference station.

  1. Source of the tsunami associated with the Kalapana (Hawaii) earthquake of November 1975

    SciTech Connect (OSTI)

    Cox, D.C.

    1980-12-01

    The travel times of the tsunami generated on 29 November 1975 off the Kau-Puna coast of Hawaii to the tide gages at Hilo, Kahului, Honolulu, and Nawiliwili have been calculated from the arrival times indicated on the tide-gage records, applying gage-time corrections, assuming that the tsunami was generated at the time of the earthquake it accompanied. Travel times have also been calculated similarly to other places on the coast of Hawaii where arrival times of the tsunami were reported, and to Johnston Atoll. Inverse tsunami refraction diagrams have been constructed by graphical means for the path of the tsunami between the vicinity of its source and the places of known arrival times. The isochrones of the refraction diagrams corresponding to the respective calculated travel times for the tsunami front have been used to define the boundary of the area of upward sea-floor displacement from which the tsunami propagated. This area is about 15 or 20 miles long (parallel to the southeast coast of Hawaii) and on the order of 14 or 15 miles wide, considerably smaller than the area earlier considered the tsunami source. Coastal subsidence measured soon after the earthquake indicates that the area of initial upward displacement was separated from the coast by a narrow belt of downward displacement. Comparisons between the crest arrival times and the travel times indicated by the inverse refraction diagrams indicate a lag of about four minutes between the time of the earthquake and the accomplishment of the maximum upward displacement. Accuracies of estimation are insufficient to determine whether the maximum upward displacement occurred within the area of initial displacement or seaward of it within a distance of about 15 miles. Displacement resulting from a mega-landslide cannot be distinguished from strictly tectonic displacement by the comparison of arrival times and travel times. 14 references, 19 figures, 8 tables.

  2. Structure and time of deformation in the central Pancake Range, Nye County, Nevada

    SciTech Connect (OSTI)

    Perry, W.J.; Grow, J.A. )

    1993-04-01

    In east-central Nevada, the Portuguese Mountain area of the central Pancake Range directly west of Railroad Valley contains mapped thrust' faults that form part of the basis of the central Nevada thrust-belt oil play. The authors have mapped and field checked the structure of this area to determine if thrust-style hydrocarbon traps are likely. In this region, previously mapped thrusts have been found to be (1) normal faults, dipping more than 60[degree], (2) landslide masses of both Oligocene igneous rocks and Paleozoic carbonate rocks, and (3) low-angle attenuation faults that omit rather than duplicate stratigraphic section. Locally, the first two types (mapped Portuguese Mountain thrust') involve Oligocene igneous rocks and are therefore younger. The third is represented by a low-angle detachment system northeast of Portuguese Mountain that was first differentially eroded and then overlapped by thin limestone-clast conglomerate and red clays (terra rosa) of the Sheep Pass( ) Formation and overlying volcanic rocks. The possible Sheep Pass correlation would imply that the detachment system is Paleogene or older. Farther north, near McClure Spring, a similar terra rosa and subjacent thin limestone-clast conglomerate sequence is underlain paraconformably by gray claystone containing dinosaur bone fragments, similar to the type Newark Canyon Formation (Cretaceous) to the north. Sheep Pass( ) terra rosa of the upper part of this sequence rest with profound unconformity (nearly 90[degree]) on mid-Pennsylvanian limestone of the east limb of the McClure Spring syncline, a major recumbent syncline cored by Permian to Triassic( ) synorogenic conglomerates. These rocks contain outcrop-scale synorogenic angular unconformities of as much as 15[degree] suggesting that folding began in Permian time. These preliminary results suggest that contractional deformation of the McClure Spring syncline may be pre-Sevier and possibly of Permian-Triassic age.

  3. PLANETESIMAL COMPOSITIONS IN EXOPLANET SYSTEMS

    SciTech Connect (OSTI)

    Johnson, Torrence V. [Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109 (United States); Mousis, Olivier [Observatoire THETA, Institut UTINAM, UMR 6213 CNRS, Universite de Franche-Comte, BP 1615, F-25010 Besancon Cedex (France); Lunine, Jonathan I. [Center for Radiophysics and Space Research, Space Sciences Building, Cornell University, Ithaca, NY 14853 (United States); Madhusudhan, Nikku, E-mail: torrence.v.johnson@jpl.nasa.gov [Yale Center for Astronomy and Astrophysics, Department of Physics, Yale University, New Haven, CT 06511 (United States)

    2012-10-01

    We have used recent surveys of the composition of exoplanet host stars to investigate the expected composition of condensed material in planetesimals formed beyond the snow line in the circumstellar nebulae of these systems. Of the major solid-forming elements, C and O abundances (and particularly the C/O abundance ratio) strongly affect the amounts of volatile ices and refractory phases in icy planetesimals formed in these systems. This results from these elements' effects on the partitioning of O among gas, refractory solid and ice phases in the final condensate. The calculations use a self-consistent model for the condensation sequence of volatile ices from the nebula gas after refractory (silicate and metal) phases have condensed. The resultant mass fractions (compared to the total condensate) of refractory phases and ices were calculated for a range of nebular temperature structures and redox conditions. Planetesimals in systems with sub-solar C/O should be water ice-rich, with lower than solar mass fractions of refractory materials, while in super-solar C/O systems planetesimals should have significantly higher mass fractions of refractories, in some cases having little or no water ice. C-bearing volatile ices and clathrates also become increasingly important with increasing C/O depending on the assumed nebular temperatures. These compositional variations in early condensates in the outer portions of the nebula will be significant for the equivalent of the Kuiper Belt in these systems, icy satellites of giant planets, and the enrichment (over stellar values) of volatiles and heavy elements in giant planet atmospheres.

  4. Temporal and spatial variability of ooid sand shoals: Comparison of Mississippian of Kentucky and Quaternary of Bahamas

    SciTech Connect (OSTI)

    Boardman, M.R. (Miami Univ., Oxford, OH (USA))

    1989-08-01

    An examination of the lithology and topography of Andros Island, Bahamas, reveals it is a Pleistocene ooid sand shoal. A comparison with Joulters Cays (a modern ooid sand shoal directly to the north) shows that much of the original depositional topography is preserved through at least one cycle of sea level highstand and lowstand. Both the Pleistocene and the Holocene ooid sand bodies are a few kilometers to tens of kilometers wide. The total vertical relief of a single episode of Quaternary ooid sand deposition is more than 10 m and includes accumulation in tidal channels, shallow flat areas, and eolian dunes. Today, much of Andros Island is within 2 m of present sea level and is the site of a belt several kilometers wide consisting of muddy tidal flat sediments overlying an exposure surface. The site of ooid sand deposition and shoal complex formation is not continuous along shorelines, especially windward margins, but shifts abruptly along the margins of platforms as a result of minor fluctuations of sea level. Thus, it should be expected that ooid sand shoals (ancient and modern) should be in direct lateral and vertical contact with lagoons, tidal flats, and reefs. The Mississippian Slade Formation contains many of the features of Quaternary ooid sand accumulation: abrupt vertical and lateral gradations between oolitic grainstones, packstones, and lime mudstones, vertical relief of individual oolitic sedimentary packages up to 30 m (perhaps with eolian dunes) and numerous exposure surfaces of varying intensities. These characteristics suggest that this formation represents a time of rapid fluctuations of relative sea level and abrupt shifts in the sites of ooid sand shoal complexes.

  5. Synthesis of one-dimensional porous Co{sub 3}O{sub 4} nanobelts and their ethanol gas sensing properties

    SciTech Connect (OSTI)

    Che, Hongwei; Liu, Aifeng; Hou, Junxian; Zhang, Xiaoliang; Bai, Yongmei; Mu, Jingbo; Wang, Renliang

    2014-11-15

    Graphical abstract: 1D porous porous Co{sub 3}O{sub 4} nanobelts were synthesized via a facile route without use of any surfactants or organic solvent, exhibiting ethanol gas sensing properties superior to the commercial Co{sub 3}O{sub 4} powders. - Highlights: One-dimensional porous Co{sub 3}O{sub 4} nanobelts were synthesized. The belt-like morphology can be finely controlled via adjusting the reaction parameters. The evolution process of porous Co{sub 3}O{sub 4} nanobelts was investigated. Porous Co{sub 3}O{sub 4} nanobelts exhibit superior ethanol gas sensing properties. - Abstract: In this paper, one-dimensional porous Co{sub 3}O{sub 4} nanobelts were synthesized via a facile template-free hydrothermal method and subsequent the thermal decomposition. Their microstructures and morphologies were characterized by X-ray diffraction, scanning electron microscopy, transmission electron microscopy, thermogravimetric analysis, fourier transform infrared spectroscopy, X-ray photoelectron spectroscopy and N{sub 2} adsorptiondesorption techniques. The results indicate that the reaction parameters such as the molar ratio of Co(NO{sub 3}){sub 2}6H{sub 2}O to C{sub 2}H{sub 4}N{sub 4}, the amount of Co(NO{sub 3}){sub 2}6H{sub 2}O, the hydrothermal temperature and time play crucial rules in controlling the microstructures and morphologies of the as-prepared cobalt precursors. A possible formation mechanism was proposed. Moreover, the obtained porous Co{sub 3}O{sub 4} nanobelts exhibit ethanol gas sensing properties superior to the commercial Co{sub 3}O{sub 4} powders at a working temperature of 200 C, suggesting their potential applications as nanosensors.

  6. Silver Peak Innovative Exploration Project (Ram Power Inc.)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Miller, Clay

    2010-01-01

    Data generated from the Silver Peak Innovative Exploration Project, in Esmeralda County, Nevada, encompasses a “deep-circulation (amagmatic)” meteoric-geothermal system circulating beneath basin-fill sediments locally blanketed with travertine in western Clayton Valley (lithium-rich brines from which have been mined for several decades). Spring- and shallow-borehole thermal-water geochemistry and geothermometry suggest that a Silver Peak geothermal reservoir is very likely to attain the temperature range 260- 300oF (~125-150oC), and may reach 300-340oF (~150-170oC) or higher (GeothermEx, Inc., 2006). Results of detailed geologic mapping, structural analysis, and conceptual modeling of the prospect (1) support the GeothermEx (op. cit.) assertion that the Silver Peak prospect has good potential for geothermal-power production; and (2) provide a theoretical geologic framework for further exploration and development of the resource. The Silver Peak prospect is situated in the transtensional (regional shearing coupled with extension) Walker Lane structural belt, and squarely within the late Miocene to Pliocene (11 Ma to ~5 Ma) Silver Peak-Lone Mountain metamorphic core complex (SPCC), a feature that accommodated initial displacement transfer between major right-lateral strike- slip fault zones on opposite sides of the Walker Lane. The SPCC consists essentially of a ductiley-deformed lower plate, or “core,” of Proterozoic metamorphic tectonites and tectonized Mesozoic granitoids separated by a regionally extensive, low-angle detachment fault from an upper plate of severely stretched and fractured structural slices of brittle, Proterozoic to Miocene-age lithologies. From a geothermal perspective, the detachment fault itself and some of the upper-plate structural sheets could function as important, if secondary, subhorizontal thermal-fluid aquifers in a Silver Peak hydrothermal system.

  7. Structure of continental rifts: Role of older features and magmatism

    SciTech Connect (OSTI)

    Keller, G.R.

    1996-12-31

    Recent geological and geophysical studies in several continental rifts have begun to shed light on the details of the processes which govern the structural evolution of these important exploration targets. In Kenya and Tanzania, the classic East African rift has been the object of several investigations which reveal that its location follows the boundary (suture ?) between the Tanzanian craton (Archean) and Mozambiquan belt (Proterozoic), The Baikal rift also follows a similar boundary, and the Mid-continent rift of North America appears to do the same. Rifts themselves often act as zones of weakness which are reactivated by younger tectonic regimes. The classic North American example of this effect is the Eocambrian Southern Oklahoma aulacogen which was deformed to create the Anadarko basin and Wichita uplift in the late Paleozoic. The Central basin platform has a similar history although the original rift formed at {approximately}1,100Ma. Integration of geophysical data with petrologic and geochemical data from several rift zones has also provided a new picture of the nature and extent of magmatic modification of the crust. An interesting contradiction is that Phanerozoic rifts, except the Afar region, show little evidence for major magmatic modification of the crust whereas, at least in North America, many Precambrian rifts are associated with very large mafic bodies in the crust. The Kenya rift displays evidence for modification of the lower crust in a two-phase magmatic history, but upper crustal magmatic features are limited to local intrusions associated with volcanoes. In this rift, complex basement structure plays a much more important role than previously realized, and the geophysical signatures of basement structure and magmatism are easy to confuse. If this is also the case in other rifts, additional rift basins remain to be discovered.

  8. Structure of continental rifts: Role of older features and magmatism

    SciTech Connect (OSTI)

    Keller, G.R. )

    1996-01-01

    Recent geological and geophysical studies in several continental rifts have begun to shed light on the details of the processes which govern the structural evolution of these important exploration targets. In Kenya and Tanzania, the classic East African rift has been the object of several investigations which reveal that its location follows the boundary (suture ) between the Tanzanian craton (Archean) and Mozambiquan belt (Proterozoic), The Baikal rift also follows a similar boundary, and the Mid-continent rift of North America appears to do the same. Rifts themselves often act as zones of weakness which are reactivated by younger tectonic regimes. The classic North American example of this effect is the Eocambrian Southern Oklahoma aulacogen which was deformed to create the Anadarko basin and Wichita uplift in the late Paleozoic. The Central basin platform has a similar history although the original rift formed at [approximately]1,100Ma. Integration of geophysical data with petrologic and geochemical data from several rift zones has also provided a new picture of the nature and extent of magmatic modification of the crust. An interesting contradiction is that Phanerozoic rifts, except the Afar region, show little evidence for major magmatic modification of the crust whereas, at least in North America, many Precambrian rifts are associated with very large mafic bodies in the crust. The Kenya rift displays evidence for modification of the lower crust in a two-phase magmatic history, but upper crustal magmatic features are limited to local intrusions associated with volcanoes. In this rift, complex basement structure plays a much more important role than previously realized, and the geophysical signatures of basement structure and magmatism are easy to confuse. If this is also the case in other rifts, additional rift basins remain to be discovered.

  9. Facies distributions within contrasting structural components of a rift lake: Lake Tanganyika, Africa

    SciTech Connect (OSTI)

    Soreghan, M.J.; Cohen, A.S. )

    1991-03-01

    Lake Tanganyika is the most widely cited modern analog for interpreting ancient rift lakes; thus, understanding controls on its facies distribution is critical for refining stratigraphic models for rifts. Four recurrent margin types occur along the alternating half-graben structure of the lake: rift axes, platforms, escarpments, and accommodation zones. Data from study sites in the northern part of the lake suggest that predictable facies differences exist between these structural margin types. The rift axis site comprises a low-gradient, clastic (wave/current)-dominated deltaic system, with strong facies asymmetry and minor carbonate accumulations on raised benches. The platform margin site comprises a series of structurally controlled benches over which long, continuous facies tracts occur. Carbonate sands, muds, and shell gravel dominate; clastics are limited to moderate-sized silty deltas and long, narrow shoreface sands. The escarpment margin site is a steep-gradient system along which small ({lt}1 km{sup 2}) fan deltas alternate with cemented talus. The accommodation zone margin sites are also dominated by rugged structural relief, generally small fan deltas, and semicontinuous shoreface sand belts ({gt}5 km) onshore and poorly sorted silts offshore. TOC from fine-grained samples reflects the contrast in margin types. TOC values for the platform and rift axis range from 0.4 - 2.1 wt. % (avg. 1.3%), whereas accommodation zone and escarpment margin values range from 0.5-5.5% (avg. 3.0%). Acid insoluble sulfur shows a similar trend. Although all data are significantly correlated with depth, the relative area of the lake margin above and below the oxicline is directly controlled by the structural style of the lake margin.

  10. The discovery of cometary activity in near-Earth asteroid (3552) Don Quixote

    SciTech Connect (OSTI)

    Mommert, Michael; Harris, Alan W.; Hora, Joseph L.; Smith, Howard A.; Reach, William T.; Emery, Joshua P.; Thomas, Cristina A.; Mueller, Michael; Cruikshank, Dale P.; Trilling, David E.; Delbo, Marco

    2014-01-20

    The near-Earth object (NEO) population, which mainly consists of fragments from collisions between asteroids in the main asteroid belt, is thought to include contributions from short-period comets as well. One of the most promising NEO candidates for a cometary origin is near-Earth asteroid (3552) Don Quixote, which has never been reported to show activity. Here we present the discovery of cometary activity in Don Quixote based on thermal-infrared observations made with the Spitzer Space Telescope in its 3.6 and 4.5 ?m bands. Our observations clearly show the presence of a coma and a tail in the 4.5 ?m but not in the 3.6 ?m band, which is consistent with molecular band emission from CO{sub 2}. Thermal modeling of the combined photometric data on Don Quixote reveals a diameter of 18.4{sub ?0.4}{sup +0.3} km and an albedo of 0.03{sub ?0.01}{sup +0.02}, which confirms Don Quixote to be the third-largest known NEO. We derive an upper limit on the dust production rate of 1.9 kg s{sup 1} and derive a CO{sub 2} gas production rate of (1.1 0.1) 10{sup 26} molecules s{sup 1}. Spitzer Infrared Spectrograph spectroscopic observations indicate the presence of fine-grained silicates, perhaps pyroxene rich, on the surface of Don Quixote. Our discovery suggests that CO{sub 2} can be present in near-Earth space over a long time. The presence of CO{sub 2} might also explain that Don Quixote's cometary nature remained hidden for nearly three decades.

  11. USING RUNNING DIFFERENCE IMAGES TO TRACK PROPER MOTIONS OF XUV CORONAL INTENSITY ON THE SUN

    SciTech Connect (OSTI)

    Sheeley, N. R. Jr.; Warren, H. P.; Lee, J. E-mail: harry.warren@nrl.navy.mil; Chung, S.; Katz, J.; Namkung, M

    2014-12-20

    We have developed a procedure for observing and tracking proper motions of faint XUV coronal intensity on the Sun and have applied this procedure to study the collective motions of cellular plumes and the shorter-period waves in sunspots. Our space/time maps of cellular plumes show a series of tracks with the same 5-8minute repetition times and ?100kms{sup 1} sky-plane speeds found previously in active-region fans and in coronal hole plumes. By synchronizing movies and space/time maps, we find that the tracks are produced by elongated ejections from the unipolar flux concentrations at the bases of the cellular plumes and that the phases of these ejections are uncorrelated from cell to cell. Thus, the large-scale motion is not a continuous flow, but is more like a system of independent conveyor belts all moving in the same direction along the magnetic field. In contrast, the proper motions in sunspots are clearly waves resulting from periodic disturbances in the sunspot umbras. The periods are ?2.6minutes, but the sky-plane speeds and wavelengths depend on the heights of the waves above the sunspot. In the chromosphere, the waves decelerate from 35-45kms{sup 1} in the umbra to 7-8kms{sup 1} toward the outer edge of the penumbra, but in the corona, the waves accelerate to ?60-100kms{sup 1}. Because chromospheric and coronal tracks originate from the same space/time locations, the coronal waves must emerge from the same umbral flashes that produce the chromospheric waves.

  12. Flow of formation waters in the cretaceous-miocene succession of the Llanos basin, Colombia

    SciTech Connect (OSTI)

    Villegas, M.E.; Ramon, J.C.; Bachu, S.; Underschultz, J.R.

    1994-12-01

    This study presents the hydrogeological characteristics and flow of formation waters in the post-Paleozoic succession of the Llanos basin, a mainly siliciclastic foreland sub-Andean sedimentary basin located in Columbia between the Cordillera Oriental and the Guyanan Precambrian shield. The porosity of the sandy formations is generally high, in the range of 16-20% on average, with a trend of decreasing values with depth. Permeabilities are also relatively high, in the 10{sup 2} and 10{sup 3} md range. THe salinity (total dissolved solids) of formation waters is generally low, in the 10,000-20,000 mg/L range, suggesting that at least some strata in the basin have been flushed by metoeoric water. The shaly units in the sedimentary succession are weak aquitards in the eastern and southern parts of the basin, but are strong in the central-western part. The pressure in the basin is close to or slightly subdepth, particularly in the central-western area. The flow of formation waters in the upper units is driven mainly by topography from highs in the southwest to lows in the northeast. Local systems from the foothills and from local topographic highs in the east feed into this flow system. The flow of formation waters in the lower units is driven by topography only in the southern, eastern, and northern parts of the basin. In the central-western part, the flow is downdip toward the thrust-fold belt, driven probably by pore-space rebound induced by erosional unloading, which also is the cause of underpressuring. Hydrocarbons generated in the Cretaceous organic-rich, shaly Gacheta Formation probably have migrated updip and to the north-northeast, driven by buoyancy and entrained by the topography-driven flow of formation waters in Cretaceous-Oligocene strata in the central-western part of the basin could have created conditions for hydrodynamic entrapment of hydrocarbons.

  13. ON THE SIZE, SHAPE, AND DENSITY OF DWARF PLANET MAKEMAKE

    SciTech Connect (OSTI)

    Brown, M. E.

    2013-04-10

    A recent stellar occultation by the dwarf planet Makemake provided an excellent opportunity to measure the size and shape of one of the largest objects in the Kuiper belt. The analysis of these results provided what were reported to be precise measurements of the lengths of the projected axes, the albedo, and even the density of Makemake, but these results were, in part, derived from qualitative arguments. We reanalyzed the occultation timing data using a quantitative statistical description, and, in general, found the previously reported results on the shape of Makemake to be unjustified. In our solution, in which we use our inference from photometric data that Makemake is being viewed nearly pole-on, we find a 1{sigma} upper limit to the projected elongation of Makemake of 1.02, with measured equatorial diameter of 1434 {+-} 14 km and a projected polar diameter of 1422 {+-} 14 km, yielding an albedo of 0.81{sup +0.01}{sub -0.02}. If we remove the external constraint on the pole position of Makemake, we find instead a 1{sigma} upper limit to the elongation of 1.06, with a measured equatorial diameter of 1434{sup +48}{sub -18} km and a projected polar diameter of 1420{sup +18}{sub -24} km, yielding an albedo of 0.81{sup +0.03}{sub -0.05}. Critically, we find that the reported measurement of the density of Makemake was based on the misapplication of the volatile retention models. A corrected analysis shows that the occultation measurements provide no meaningful constraint on the density of Makemake.

  14. Description of the BDD-IIR: Electron and proton sensors on the GPS

    SciTech Connect (OSTI)

    Cayton, T.E.; Drake, D.M.; Spencer, K.M.; Herrin, M.; Wehner, T.J.; Reedy, R.C.

    1998-09-01

    The Burst Detector Dosimeter (Block) IIR (BDD-IIR) is a multipurpose silicon detector system that is scheduled to fly on two of the first 12 spacecraft of the Global Positioning System (GPS) Block 2 Replenishment series as an alternative to the Burst Detector X-ray (BDX) instrument. This instrument measures energetic-particle fluxes impinging on the GPS space vehicle (SV), primarily energetic electrons trapped in the Earth`s radiation belt, but also solar energetic particles and galactic cosmic rays. Absorbers located in front of eight separate silicon sensors determine energy thresholds for measuring incident particle fluxes, and the magnitude of energy loss in each sensor provides an imperfect but very good separation between ions and electrons over a wide range of energies. For each of two sensors, a conical collimator with a very small opening is used for low-energy particles. For four sensors, five small holes in a thick shield limits the flux on each sensor to manageable levels. For two sensors, solid domes are used to measure high-energy electrons and protons. These eight sensors provide eight channels that determine the electron energy spectrum from 77 keV to > 5 MeV and eight channels determine the proton spectrum from 1.3 to > 54 MeV. The radiation dose rate and total dose for a wide range of equivalent shielding thicknesses is inferred directly from the measured electron energy spectrum. Accumulations times are usually 240 s but can also be 24, 120, or 4,608 s. This report describes the BDD-IIR`s important mechanical and electronic features, its system tests and calibrations, the commands that can be sent to it, and the data that it returns.

  15. V405 ANDROMEDA REVISITED

    SciTech Connect (OSTI)

    Ribeiro, T.; Kafka, S.

    2011-10-15

    We present a multi-epoch time-resolved high-resolution optical spectroscopy study of the short-period (P{sub orb} = 11.2 hr) eclipsing M0V+M5V RS CVn binary V405 Andromeda. By means of indirect imaging techniques, namely Doppler imaging, we study the surface activity features of the M0V component of the system. A modified version of a Doppler imaging code, which takes into account the tidal distortion of the surface of the star, is applied to the multi-epoch data set in order to provide indirect images of the stellar surface. The multi-epoch surface brightness distributions show a low intensity 'belt' of spots at latitudes {+-}40{sup 0} and a noticeable absence of high latitude features or polar spots on the primary star of V405 Andromeda. They also reveal slow evolution of the spot distribution over {approx}4 yr. An entropy landscape procedure is used in order to find the set of binary parameters that lead to the smoothest surface brightness distributions. As a result, we find M{sub 1} = 0.51 {+-} 0.03 M{sub sun}, M{sub 2} = 0.21 {+-} 0.01 M{sub sun}, R{sub 1} = 0.71 {+-} 0.01 R{sub sun}, and an inclination i = 65{sup 0} {+-} 1{sup 0}. The resulting systemic velocity is distinct for different epochs, raising the possibility of the existence of a third body in the system.

  16. Opportunities for Automated Demand Response in Wastewater Treatment Facilities in California - Southeast Water Pollution Control Plant Case Study

    SciTech Connect (OSTI)

    Olsen, Daniel; Goli, Sasank; Faulkner, David; McKane, Aimee

    2012-12-20

    This report details a study into the demand response potential of a large wastewater treatment facility in San Francisco. Previous research had identified wastewater treatment facilities as good candidates for demand response and automated demand response, and this study was conducted to investigate facility attributes that are conducive to demand response or which hinder its implementation. One years' worth of operational data were collected from the facility's control system, submetered process equipment, utility electricity demand records, and governmental weather stations. These data were analyzed to determine factors which affected facility power demand and demand response capabilities The average baseline demand at the Southeast facility was approximately 4 MW. During the rainy season (October-March) the facility treated 40% more wastewater than the dry season, but demand only increased by 4%. Submetering of the facility's lift pumps and centrifuges predicted load shifts capabilities of 154 kW and 86 kW, respectively, with large lift pump shifts in the rainy season. Analysis of demand data during maintenance events confirmed the magnitude of these possible load shifts, and indicated other areas of the facility with demand response potential. Load sheds were seen to be possible by shutting down a portion of the facility's aeration trains (average shed of 132 kW). Load shifts were seen to be possible by shifting operation of centrifuges, the gravity belt thickener, lift pumps, and external pump stations These load shifts were made possible by the storage capabilities of the facility and of the city's sewer system. Large load reductions (an average of 2,065 kW) were seen from operating the cogeneration unit, but normal practice is continuous operation, precluding its use for demand response. The study also identified potential demand response opportunities that warrant further study: modulating variable-demand aeration loads, shifting operation of sludge-processing equipment besides centrifuges, and utilizing schedulable self-generation.

  17. Cameron synthetic fuels report

    SciTech Connect (OSTI)

    Not Available

    1980-06-01

    The increasing scarcity of conventional crude oil resources, as well as the sharply higher prices of crude oil, will generate increased interest in heavy oil, tar sands, and oil shale as potential substitutes. For all of these unconventional oil resources, extraction will be much more difficult, time consuming, and costly than for conventional crude oil. Although the inplace resources are vast and exist in many areas including the United States, the USSR, western Europe, Canada, and Latin America, probably only a small fraction of the inplace resources will prove to be economically extractable. These unconventional oil resources are now being developed in several locations around the world, and depending upon the exact definition probably account for less than 1 percent of current world oil supplies. The major current developments include: Canadian tar sands. Heavy oil production at Yarega in the Komi Autonomous Republic in the Soviet Union. The USSR also burns shale for power generation in Estonia. Venezuelan production of heavy oil in the Orinoco Heavy Oil Belt is currently about 15,000 b/d. Oil shale is likely to prove much less important than heavy oil and tar sands over the next 20 years. Further development of these unconventional resources is planned, and many projects are under way or under study. On the basis of current planning, world output of heavy oils and oil from tar sands and shale will be unlikely to exceed 2 million b/d by 1990, roughly five time today's level. However, both of these resources will require the development of new technologies for any large increases in output above what is now planned. The bulk of Canada's tar sands exists at great depths and will require the development of in situ processes for extraction. In the Orinoco, heavy metals contained in the oil make it difficult to refine with existing technology.

  18. Investigation of the thermal regime and geologic history of the Cascade volcanic arc: First phase of a program for scientific drilling in the Cascade Range

    SciTech Connect (OSTI)

    Priest, G.R.

    1987-01-01

    A phased, multihole drilling program with associated science is proposed as a means of furthering our understanding of the thermal regime and geologic history of the Cascade Range of Washington, Oregon, and northern California. The information obtained from drilling and ancillary geological and geophysical investigations will contribute to our knowledge in the following general areas: (1) the magnitude of the regional background heat flow of parts of the Quaternary volcanic belt dominated by the most abundant volcanic rock types, basalt and basaltic andesite; (2) the nature of the heat source responsible for the regional heat-flow anomaly; (3) the characteristics of the regional hydrothermal and cold-water circulation; the rates of volcanism for comparison with models for the rate and direction of plate convergence of the Cascades; (5) the history of deformation and volcanism in the volcanic arc that can be related to subduction; (6) the present-day stress regime of the volcanic arc and the relation of these stresses to plate interactions and possible large earthquakes; and the current geometry of the subducted oceanic plate below the Cascade Range and the relationship of the plate to the distribution of heat flow, Quaternary volcanism, and Quaternary deformation. Phase I research will be directed toward a detailed investigation of the Santiam Pass segment. In concert with the Santiam Pass research, a detailed study of the nearby Breitenbush Hot Springs area is also recommended as a component of Phase I. The object of the Breitenbush research is to study one of the hottest known Cascade hydrothermal systems, which coincidentally also has a good geological and geophysical data base. A coordinated program of drilling, sampling, subsurface measurements, and surface surveys will be associated with the drilling of several holes.

  19. Refrigeration system with a compressor-pump unit and a liquid-injection desuperheating line

    DOE Patents [OSTI]

    Gaul, Christopher J. (Thornton, CO)

    2001-01-01

    The refrigeration system includes a compressor-pump unit and/or a liquid-injection assembly. The refrigeration system is a vapor-compression refrigeration system that includes an expansion device, an evaporator, a compressor, a condenser, and a liquid pump between the condenser and the expansion device. The liquid pump improves efficiency of the refrigeration system by increasing the pressure of, thus subcooling, the liquid refrigerant delivered from the condenser to the expansion device. The liquid pump and the compressor are driven by a single driving device and, in this regard, are coupled to a single shaft of a driving device, such as a belt-drive, an engine, or an electric motor. While the driving device may be separately contained, in a preferred embodiment, the liquid pump, the compressor, and the driving device (i.e., an electric motor) are contained within a single sealable housing having pump and driving device cooling paths to subcool liquid refrigerant discharged from the liquid pump and to control the operating temperature of the driving device. In another aspect of the present invention, a liquid injection assembly is included in a refrigeration system to divert liquid refrigerant from the discharge of a liquid pressure amplification pump to a compressor discharge pathway within a compressor housing to desuperheat refrigerant vapor to the saturation point within the compressor housing. The liquid injection assembly includes a liquid injection pipe with a control valve to meter the volume of diverted liquid refrigerant. The liquid injection assembly may also include a feedback controller with a microprocessor responsive to a pressure sensor and a temperature sensor both positioned between the compressor to operate the control valve to maintain the refrigerant at or near saturation.

  20. The cretaceous source rocks in the Zagros Foothills of Iran: An example of a large size intracratonic basin

    SciTech Connect (OSTI)

    Bordenave, M.L. ); Huc, A.Y. )

    1993-02-01

    The Zagros orogenic belt of Iran is one of the world most prolific petroleum producing area. However, most of the oil production is originated from a relatively small area, the 60,000 km[sup 2] wide Dezful Embayment which contains approximately 12% of the proven oil global reserves. The distribution of the oil and gas fields results from the area extent of six identified source rock layers, their thermal history and reservoir, cap rock and trap availability. In this paper, the emphasis is three of the layers of Cretaceous sources rocks. The Garau facies was deposited during the Neocomian to Albian interval over Lurestan, Northeast Khuzestan and extends over the extreme northeast part of Fars, the Kazhdumi source rock which deposited over the Dezful Embayment, and eventually the Senonian Gurpi Formation which has marginal source rock characteristics in limited areas of Khuzestan and Northern Fars. The deposition environment of these source rock layers corresponds to semipermanent depressions, included in an overall shallow water intracratonic basin communicating with the South Tethys Ocean. These depressions became anoxic when climatic oceanographical and geological conditions were adequate, i.e., humid climate, high stand water, influxes of fine grained clastics and the existence of sills separating the depression from the open sea. Distribution maps of these source rock layers resulting from extensive field work and well control are also given. The maturation history of source rocks is reconstructed from a set of isopachs. It was found that the main contributor to the oil reserves is the Kazhdumi source rock which is associated with excellent calcareous reservoirs.

  1. A critical evaluation of the upper ocean heat budget in the Climate Forecast System Reanalysis data for the south central equatorial Pacific

    SciTech Connect (OSTI)

    Liu H.; Lin W.; Liu, X.; Zhang, M.

    2011-08-26

    Coupled ocean-atmospheric models suffer from the common bias of a spurious rain belt south of the central equatorial Pacific throughout the year. Observational constraints on key processes responsible for this bias are scarce. The recently available reanalysis from a coupled model system for the National Centers for Environmental Prediction (NCEP) Climate Forecast System Reanalysis (CFSR) data is a potential benchmark for climate models in this region. Its suitability for model evaluation and validation, however, needs to be established. This paper examines the mixed layer heat budget and the ocean surface currents - key factors for the sea surface temperature control in the double Inter-Tropical Convergence Zone in the central Pacific - from 5{sup o}S to 10{sup o}S and 170{sup o}E to 150{sup o}W. Two independent approaches are used. The first approach is through comparison of CFSR data with collocated station observations from field experiments; the second is through the residual analysis of the heat budget of the mixed layer. We show that the CFSR overestimates the net surface flux in this region by 23 W m{sup -2}. The overestimated net surface flux is mainly due to an even larger overestimation of shortwave radiation by 44 W m{sup -2}, which is compensated by a surface latent heat flux overestimated by 14 W m{sup -2}. However, the quality of surface currents and the associated oceanic heat transport in CFSR are not compromised by the surface flux biases, and they agree with the best available estimates. The uncertainties of the observational data from field experiments are also briefly discussed in the present study.

  2. Silver Peak Innovative Exploration Project (Ram Power Inc.)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Miller, Clay

    2010-01-01

    Data generated from the Silver Peak Innovative Exploration Project, in Esmeralda County, Nevada, encompasses a deep-circulation (amagmatic) meteoric-geothermal system circulating beneath basin-fill sediments locally blanketed with travertine in western Clayton Valley (lithium-rich brines from which have been mined for several decades). Spring- and shallow-borehole thermal-water geochemistry and geothermometry suggest that a Silver Peak geothermal reservoir is very likely to attain the temperature range 260- 300oF (~125-150oC), and may reach 300-340oF (~150-170oC) or higher (GeothermEx, Inc., 2006). Results of detailed geologic mapping, structural analysis, and conceptual modeling of the prospect (1) support the GeothermEx (op. cit.) assertion that the Silver Peak prospect has good potential for geothermal-power production; and (2) provide a theoretical geologic framework for further exploration and development of the resource. The Silver Peak prospect is situated in the transtensional (regional shearing coupled with extension) Walker Lane structural belt, and squarely within the late Miocene to Pliocene (11 Ma to ~5 Ma) Silver Peak-Lone Mountain metamorphic core complex (SPCC), a feature that accommodated initial displacement transfer between major right-lateral strike- slip fault zones on opposite sides of the Walker Lane. The SPCC consists essentially of a ductiley-deformed lower plate, or core, of Proterozoic metamorphic tectonites and tectonized Mesozoic granitoids separated by a regionally extensive, low-angle detachment fault from an upper plate of severely stretched and fractured structural slices of brittle, Proterozoic to Miocene-age lithologies. From a geothermal perspective, the detachment fault itself and some of the upper-plate structural sheets could function as important, if secondary, subhorizontal thermal-fluid aquifers in a Silver Peak hydrothermal system.

  3. Silver Peak Innovative Exploration Project (Ram Power Inc.)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Miller, Clay

    Data generated from the Silver Peak Innovative Exploration Project, in Esmeralda County, Nevada, encompasses a deep-circulation (amagmatic) meteoric-geothermal system circulating beneath basin-fill sediments locally blanketed with travertine in western Clayton Valley (lithium-rich brines from which have been mined for several decades). Spring- and shallow-borehole thermal-water geochemistry and geothermometry suggest that a Silver Peak geothermal reservoir is very likely to attain the temperature range 260- 300oF (~125-150oC), and may reach 300-340oF (~150-170oC) or higher (GeothermEx, Inc., 2006). Results of detailed geologic mapping, structural analysis, and conceptual modeling of the prospect (1) support the GeothermEx (op. cit.) assertion that the Silver Peak prospect has good potential for geothermal-power production; and (2) provide a theoretical geologic framework for further exploration and development of the resource. The Silver Peak prospect is situated in the transtensional (regional shearing coupled with extension) Walker Lane structural belt, and squarely within the late Miocene to Pliocene (11 Ma to ~5 Ma) Silver Peak-Lone Mountain metamorphic core complex (SPCC), a feature that accommodated initial displacement transfer between major right-lateral strike- slip fault zones on opposite sides of the Walker Lane. The SPCC consists essentially of a ductiley-deformed lower plate, or core, of Proterozoic metamorphic tectonites and tectonized Mesozoic granitoids separated by a regionally extensive, low-angle detachment fault from an upper plate of severely stretched and fractured structural slices of brittle, Proterozoic to Miocene-age lithologies. From a geothermal perspective, the detachment fault itself and some of the upper-plate structural sheets could function as important, if secondary, subhorizontal thermal-fluid aquifers in a Silver Peak hydrothermal system.

  4. Sequence stratigraphic analysis of individual depositional successions: Effects of marine/nonmarine sediment partitioning and longitudinal sediment transport, Mannville Group, Alberta Foreland Basin, Canada

    SciTech Connect (OSTI)

    Cant, D.J.

    1995-05-01

    In the Falher Member of the Mannville Group (Aptian-Albian) of western Canada, two shoreline successions contain the reservoir conglomerates for the giant Elmworth gas field. The Falher B succession has basal sheetlike shoreface unit of hummocky cross-stratified sandstone that thins seaward and terminates about 30km north (seaward) of the landward limit of the transgression. Another 25 km farther basinward, the succession shows a 20-30-m-thick sandstone, unattached to the prograding shoreface, and an overlying coarsening-upward shoreface succession with thin muds and coals, interpreted as back-barrier deposits. In the upper (Falher A) succession, immediately landward (south) of the barriers, fluvial valleys were incised into nonmarine mudstones and coals during the base-level fall. As relative sea level subsequently rose, in nonmarine areas the valleys were filled by estuarine and fluvial sands, then a widespread sheet of fine-grained nonmarine sediment was deposited. At the same time, the shoreline migrated back across the shelf. As it reached the original shorezone (structurally controlled), reworking of underlying deposits successively generated three gravelly barrier islands superimposed on the sandy shoreface succession. The conglomeratic reservoirs all rest above the unconformities, in the transgressive depositional system. Westward (alongshore) toward the thrust belt, no falling or lowstand sea level succession developed. Instead, a wide regressive shoreface sandstone with a transgressive cap occurs. Subsidence rates were higher in this area, and relative sea level appears always to have risen, but at varying rates. Any two-dimensional sequence stratigraphic model, therefore, is inadequate to describe the lateral variation of the sequence and distribution of shoreface sandstones, because the subsidence gradient was not parallel to the direction of shoreface progradation.

  5. Regional analysis of rhythmic bedding in the Fort Hays limestone member, Niobrara Formation (Upper Cretaceous), US western interior

    SciTech Connect (OSTI)

    Laferriere, A.P.

    1987-01-01

    Results of a regional stratigraphic investigation of the rhythmically bedded Fort Hays limestone member of Kansas, Colorado, and New Mexico indicate at least two levels of cyclicity. Regional development of these cycles strongly supports the hypothesis that they are climatic in origin. Departures from simple cyclical patterns resulted from sedimentary effects of Late Cretaceous orogenic activity, erosional events associated with eustatic sea level changes, diagenetic modification, and possibly from interference between orbital parameters having different periodicities. The vulnerability of Milankovitch-type cyclicity to overprinting by tectono-sedimentologic effects makes units such as the Fort Hays useful as indicators of subtle tectonic activity. Regional thickness changes in groups of shale-limestone couplets were identified, correlated, and mapped in the subsurface using geophysical well log information in order to locate subtle structural elements that influenced Fort Hays sedimentation. In the Denver-Julesburg Basin of Colorado and western Kansas, thinning of the section between Fort Hays marker horizons occurs dominantly along northeastwardly trending belts that resulted apparently from Late Cretaceous reactivation of the Transcontinental Arch. Isotopic and petrographic analyses were conducted on pelagic (carbonate matrix) and benthic (inoceramid bivalve) constituents of selected shale/limestone couplets. These data suggest that there was little difference in temperature or salinity between times of terrigenous detrital input and times of nearly pure carbonate deposition. Isotopic information from matrix samples suggests a westward decrease in salinity of surface water in the Western Interior Sea. Isotopic data from largely unaltered inoceramid bivalves indicate bottom-water conditions of near-normal marine salinity.

  6. Geology and geophysics of Proterozoic basement rocks in the eastern midcontinent of the United States

    SciTech Connect (OSTI)

    Lidiak, E.G. )

    1992-01-01

    Upper crustal Proterozoic rocks of the eastern midcontinent of the U.S. are part of the transcontinental Proterozoic province, a 3,000 km-long belt of anorogenic igneous rocks that extends from western Ohio to southern California. Regional magnetic and gravity anomaly maps reveal a variety of prominent anomalies and gradients that reflect major basement or intrabasement structures. Widespread are pronounced (10--20 km diameter), high-amplitude (600--700 gamma) circular to elliptical positive magnetic anomalies that are associated with magnetite-series granites and coeval rhyolites. Also present (in Indiana) are a series of ring-shaped magnetic anomalies that have a diameter of about 50 km and form circular to elliptical patterns of narrow positive anomalies bordered by negative anomalies and ringing a central minimum. Modeling of the anomalies suggests that they may be ring dike complexes associated with calderas. Two prominent circular gravity lows associated with large granitic batholiths have also been identified. The larger of these, the Wisconsin gravity minimum, has a diameter of about 250 km and an amplitude of about [minus]65 mgals and is associated with the Wolf River batholith. The second gravity low has a diameter of about 75 km and an amplitude of about [minus]25 mgals and is in east-central Kentucky. Several major rift zones are present in the eastern midcontinent. The most prominent of these is the New Madrid rift complex, a failed-arm structure that extends into the craton beneath the Mississippi embayment. Also present are linear arrays of positive magnetic and gravity anomalies that are associated with basaltic rift zones. These include the mid-Michigan rift and the Ft. Wayne rift, as well as with possible rifts associated with the mid-Tennessee and Louisville positive anomalies.

  7. Subsurface cross section of lower Paleozoic rocks, Powder River basin, Wyoming and Montana

    SciTech Connect (OSTI)

    Macke, D.L.

    1988-07-01

    The Powder River basin is one of the most actively explored Rocky Mountain basins for hydrocarbons, yet the lower Paleozoic (Cambrian through Mississippian) rocks of this interval remain little studied. As a part of a program studying the evolution of sedimentary basins, approximately 3200 km of cross section, based on more than 50 combined geophysical and lithologic logs, have been constructed covering an area of about 200,000 km/sup 2/. The present-day basin is a Cenozoic structural feature located between the stable interior of the North American craton and the Cordilleran orogenic belt. At various times during the early Paleozoic, the basin area was not distinguishable from either the stable craton, the Williston basin, the Central Montana trough, or the Cordilleran miogeocline. Both deposition and preservation in the basin have been greatly influenced by the relative uplift of the Transcontinental arch. Shows of oil and dead oil in well cuttings confirm that hydrocarbons have migrated through at least parts of the basin's lower Paleozoic carbonate section. These rocks may have been conduits for long-distance migration of hydrocarbons as early as Late Cretaceous, based on (1) the probable timing of thermal maturation of hydrocarbon-source rocks within the basin area and to the west, (2) the timing of Laramide structural events, (3) the discontinuous nature of the reservoirs in the overlying, highly productive Pennsylvanian-Permian Minnelusa Formation, and (4) the under-pressuring observed in some Minnelusa oil fields. Vertical migration into the overlying reservoirs could have been through deep fractures within the basin, represented by major lineament systems. Moreover, the lower Paleozoic rocks themselves may also be hydrocarbon reservoirs.

  8. WHAT DETERMINES THE DENSITY STRUCTURE OF MOLECULAR CLOUDS? A CASE STUDY OF ORION B WITH HERSCHEL

    SciTech Connect (OSTI)

    Schneider, N.; Andre, Ph.; Koenyves, V.; Motte, F.; Arzoumanian, D.; Didelon, P.; Hennemann, M.; Hill, T.; Palmeirim, P.; Peretto, N.; Roy, A.; Ward-Thompson, D.; Benedettini, M.; Pezzuto, S.; Rygl, K. L. J.; Bressert, E.; Di Francesco, J.; Griffin, M.; and others

    2013-04-01

    A key parameter to the description of all star formation processes is the density structure of the gas. In this Letter, we make use of probability distribution functions (PDFs) of Herschel column density maps of Orion B, Aquila, and Polaris, obtained with the Herschel Gould Belt survey (HGBS). We aim to understand which physical processes influence the PDF shape, and with which signatures. The PDFs of Orion B (Aquila) show a lognormal distribution for low column densities until A{sub V} {approx} 3 (6), and a power-law tail for high column densities, consistent with a {rho}{proportional_to}r {sup -2} profile for the equivalent spherical density distribution. The PDF of Orion B is broadened by external compression due to the nearby OB stellar aggregates. The PDF of a quiescent subregion of the non-star-forming Polaris cloud is nearly lognormal, indicating that supersonic turbulence governs the density distribution. But we also observe a deviation from the lognormal shape at A{sub V} > 1 for a subregion in Polaris that includes a prominent filament. We conclude that (1) the point where the PDF deviates from the lognormal form does not trace a universal A{sub V} -threshold for star formation, (2) statistical density fluctuations, intermittency, and magnetic fields can cause excess from the lognormal PDF at an early cloud formation stage, (3) core formation and/or global collapse of filaments and a non-isothermal gas distribution lead to a power-law tail, and (4) external compression broadens the column density PDF, consistent with numerical simulations.

  9. Repository site definition in basalt: Pasco Basin, Washington

    SciTech Connect (OSTI)

    Guzowski, R.V.; Nimick, F.B.; Muller, A.B.

    1982-03-01

    Discussion of the regional setting, geology, hydrology, and geochemistry of the Pasco Basin are included in this report. Pasco basin is a structural and topographic basin of approximately 2000 mi/sup 2/ (5180 km/sup 2/) located within the Yakima Fold Belt Subprovince of the Columbia Plateau. The stratigraphic sequence within the basin consists of an undetermined thickness of lower Miocene and younger flood basalts with interbedded and overlying sedimentary units. This sequence rests upon a basement of probably diverse rock types that may range in age from precambrian through early Tertiary. Although a large amount of information is available on the hydrology of the unconfined aquifer system, ground-water flow within the basin is, in general, poorly understood. Recharge areas for the Mabton interbed and the Saddle Mountains Formation are the highlands surrounding the basin with the flow for these units toward Gable Butte - Gable Mountain and Lake Wallula. Gable Butte - Gable Mountain probably is a ground-water sink, although the vertical flow direction in this zone is uncertain. The amount of upward vertical leakage from the Saddle Mountains Formation into the overlying sediments or to the Columbia River is unknown. Units underlying the Mabton interbed may have a flow scheme similar to those higher units or a flow scheme dominated by interbasin flow. Upward vertical leakage either throughout the basin, dominantly to the Columbia River, or dominantly to Lake Wallula has been proposed for the discharge of the lower units. None of these proposals is verified. The lateral and vertical distribution of major and minor ions in solution, Eh and pH, and ion exchange between basalt and ground-water are not well defined for the basin. Changes in the redox potential from the level of the subsurface facility to the higher stratigraphic levels along with the numerous other factors influencing K/sub d/, result in a poor understanding of the retardation process.

  10. Wafer screening device and methods for wafer screening

    DOE Patents [OSTI]

    Sopori, Bhushan; Rupnowski, Przemyslaw

    2014-07-15

    Wafer breakage is a serious problem in the photovoltaic industry because a large fraction of wafers (between 5 and 10%) break during solar cell/module fabrication. The major cause of this excessive wafer breakage is that these wafers have residual microcracks--microcracks that were not completely etched. Additional propensity for breakage is caused by texture etching and incomplete edge grinding. To eliminate the cost of processing the wafers that break, it is best to remove them prior to cell fabrication. Some attempts have been made to develop optical techniques to detect microcracks. Unfortunately, it is very difficult to detect microcracks that are embedded within the roughness/texture of the wafers. Furthermore, even if such detection is successful, it is not straightforward to relate them to wafer breakage. We believe that the best way to isolate the wafers with fatal microcracks is to apply a stress to wafers--a stress that mimics the highest stress during cell/module processing. If a wafer survives this stress, it has a high probability of surviving without breakage during cell/module fabrication. Based on this, we have developed a high throughput, noncontact method for applying a predetermined stress to a wafer. The wafers are carried on a belt through a chamber that illuminates the wafer with an intense light of a predetermined intensity distribution that can be varied by changing the power to the light source. As the wafers move under the light source, each wafer undergoes a dynamic temperature profile that produces a preset elastic stress. If this stress exceeds the wafer strength, the wafer will break. The broken wafers are separated early, eliminating cost of processing into cell/module. We will describe details of the system and show comparison of breakage statistics with the breakage on a production line.

  11. Deep structure of the Texas Gulf passive margin and its Ouachita-Precambrian basement: Results of the COCORP San Marcos arch survey

    SciTech Connect (OSTI)

    Culotta, R.; Latham, T.; Oliver, J.; Brown, L.; Kaufman, S. (Cornell Univ., Ithaca, NY (United States)); Sydow, M. (Pennzoil, Houston, TX (United States))

    1992-02-01

    This COCORP deep seismic survey provides a comprehensive image of the southeast-Texas part of the Gulf passive margin and its accreted Ouachita arc foundation. Beneath the updip limit of the Cenozoic sediment wedge, a prominent antiformal structure is imaged within the interior zone of the buried late Paleozoic Ouachita orogen. The structure appears to involve Precambrian Grenville basement. The crest of the antiform is coincident with the Cretaceous-Tertiary Luling-Mexia-Talco fault zone. Some of these faults dip to the northwest, counter to the general regional pattern of down-to-the-basin faulting, and appear to sole into the top of the antiform, suggesting that the Ouachita structure has been reactivated as a hingeline to the subsiding passive margin. The antiform may be tied via this fault system and the Ouachita gravity gradient to the similar Devils River, Waco, and Benton uplifts, interpreted as Precambrian basement-cored massifs. Above the Paleozoic sequence, a possible rift-related graben is imaged near the updip limit of Jurassic salt. Paleoshelf edges of the major Tertiary depositional sequences are marked by expanded sections disrupted by growth faults and shale diapirs. Within the Wilcox Formation, the transect crosses the mouth of the 900-m-deep Yoakum Canyon, a principal pathway of sediment delivery from the Laramide belt to the Gulf. Beneath the Wilcox, the Comanchean (Lower Cretaceous) shelf edge, capped by the Stuart City reef, is imaged as a pronounced topographic break onlapped by several moundy sediment packages. Because this segment of the line parallels strike, the topographic break may be interpreted as a 2,000-m-deep embayment in the Cretaceous shelf-edge, and possibly a major submarine canyon older and deeper than the Yoakum Canyon.

  12. Integration of space weather into space situational awareness

    SciTech Connect (OSTI)

    Reeves, Geoffrey D

    2010-11-09

    Rapid assessment of space weather effects on satellites is a critical step in anomaly resolution and satellite threat assessment. That step, however, is often hindered by a number of factors including timely collection and delivery of space weather data and the inherent com plexity of space weather information. As part of a larger, integrated space situational awareness program, Los Alamos National Laboratory has developed prototype operational space weather tools that run in real time and present operators with customized, user-specific information. The Dynamic Radiation Environment Assimilation Model (DREAM) focuses on the penetrating radiation environment from natural or nuclear-produced radiation belts. The penetrating radiation environment is highly dynamic and highly orbit-dependent. Operators often must rely only on line plots of 2 MeV electron flux from the NOAA geosynchronous GOES satellites which is then assumed to be representative of the environment at the satellite of interest. DREAM uses data assimilation to produce a global, real-time, energy dependent specification. User tools are built around a distributed service oriented architecture (SOA) which will allow operators to select any satellite from the space catalog and examine the environment for that specific satellite and time of interest. Depending on the application operators may need to examine instantaneous dose rates and/or dose accumulated over various lengths of time. Further, different energy thresholds can be selected depending on the shielding on the satellite or instrument of interest. In order to rapidly assess the probability that space weather was the cause of anomalous operations, the current conditions can be compared against the historical distribution of radiation levels for that orbit. In the simplest operation a user would select a satellite and time of interest and immediately see if the environmental conditions were typical, elevated, or extreme based on how often those conditions occur in that orbit. This allows users to rapidly rule in or out environmental causes of anomalies. The same user interface can also allow users to drill down for more detailed quantitative information. DREAM can be run either from a distributed web-based user interface or as a stand-alone application for secure operations. In this paper we discuss the underlying structure of the DREAM model and demonstrate the user interface that we have developed . We also present some prototype data products and user interfaces for DREAM and discuss how space environment information can be seamlessly integrated into operational SSA systems.

  13. Continuous Emissions Monitoring System Monitoring Plan for the Y-12 Steam Plant

    SciTech Connect (OSTI)

    2003-02-28

    The Oak Ridge Y-12 National Security Complex (Y-12), managed by BWXT, is submitting this Continuous Emissions Monitoring System (CEMS) Monitoring Plan in conformance with the requirements of Title 40 of the U.S. Code of Federal Regulations (CFR) Part 75. The state of Tennessee identified the Y-12 Steam Plant in Oak Ridge, Tennessee, as a non-electrical generation unit (EGU) nitrogen oxides (NO{sub x}) budget source as a result of the NO{sub x} State Implementation Plan (SIP) under the Tennessee Department of Environment and Conservation (TDEC) Rule 1200-3-27. Following this introduction, the monitoring plan contains the following sections: CEMS details, NO{sub x} emissions, and quality assurance (QA)/quality control (QC). The following information is included in the attachments: fuel and flue gas diagram, system layout, data flow diagrams, Electronic Monitoring Plan printouts, vendor information on coal and natural gas feed systems, and the Certification Test Protocol. The Y-12 Steam Plant consists of four Wickes boilers. Each is rated at a maximum heat input capacity of 296.8 MMBtu/hour or 250,000 lb/hour of 250-psig steam. Although pulverized coal is the principal fuel, each of the units can fire natural gas or a combination of coal and gas. Each unit is equipped with a Joy Manufacturing Company reverse air baghouse to control particulate emissions. Flue gases travel out of the baghouse, through an induced draft fan, then to one of two stacks. Boilers 1 and 2 exhaust through Stack 1. Boilers 3 and 4 exhaust through Stack 2. A dedicated CEMS will be installed in the ductwork of each boiler, downstream of the baghouse. The CEMS will be designed, built, installed, and started up by URS Group, Inc. (URS). Data acquisition and handling will be accomplished using a data acquisition and handling system (DAHS) designed, built, and programmed by Environmental Systems Corporation (ESC). The installed CEMS will continuously monitor NO{sub x}, flue gas flowrate, and carbon dioxide (CO{sub 2}). The CEMS will be utilized to report emissions from each unit for each ozone season starting May 1, 2003. Each boiler has independent coal and natural gas metering systems. Coal is fed to each boiler by belt-type coal feeders. Each boiler has two dedicated coal feeders. Natural gas may be burned along with coal for flame stability. The boilers may also be fired on natural gas alone. Orifice meters measure the natural gas flow to each boiler.

  14. Reduction of Non-CO2 Gas Emissions Through The In Situ Bioconversion of Methane

    SciTech Connect (OSTI)

    Scott, A R; Mukhopadhyay, B; Balin, D F

    2012-09-06

    The primary objectives of this research were to seek previously unidentified anaerobic methanotrophs and other microorganisms to be collected from methane seeps associated with coal outcrops. Subsurface application of these microbes into anaerobic environments has the potential to reduce methane seepage along coal outcrop belts and in coal mines, thereby preventing hazardous explosions. Depending upon the types and characteristics of the methanotrophs identified, it may be possible to apply the microbes to other sources of methane emissions, which include landfills, rice cultivation, and industrial sources where methane can accumulate under buildings. Finally, the microbes collected and identified during this research also had the potential for useful applications in the chemical industry, as well as in a variety of microbial processes. Sample collection focused on the South Fork of Texas Creek located approximately 15 miles east of Durango, Colorado. The creek is located near the subsurface contact between the coal-bearing Fruitland Formation and the underlying Pictured Cliffs Sandstone. The methane seeps occur within the creek and in areas adjacent to the creek where faulting may allow fluids and gases to migrate to the surface. These seeps appear to have been there prior to coalbed methane development as extensive microbial soils have developed. Our investigations screened more than 500 enrichments but were unable to convince us that anaerobic methane oxidation (AMO) was occurring and that anaerobic methanotrophs may not have been present in the samples collected. In all cases, visual and microscopic observations noted that the early stage enrichments contained viable microbial cells. However, as the levels of the readily substrates that were present in the environmental samples were progressively lowered through serial transfers, the numbers of cells in the enrichments sharply dropped and were eliminated. While the results were disappointing we acknowledge that anaerobic methane oxidizing (AOM) microorganisms are predominantly found in marine habitats and grow poorly under most laboratory conditions. One path for future research would be to use a small rotary rig to collect samples from deeper soil horizons, possibly adjacent to the coal-bearing horizons that may be more anaerobic.

  15. OPERATING THE WAND AND HERCULES PROTOTYPE SYSTEMS

    SciTech Connect (OSTI)

    K. GRUETZMACHER; ET AL

    2001-01-01

    Two prototype systems for low-density Green is Clean (GIC) waste at Los Alamos National Laboratory (LANL) have been in operation for three years at the Solid Waste Operation's (SWOs) non-destructive assay (NDA) building. The Waste Assay for Nonradioactive Disposal (WAND) and the High Efficiency Radiation Counters for Ultimate Low Emission Sensitivity (HERCULES) are used to verify the waste generator's acceptable knowledge (AK) that low-density waste is nonradioactive. GIC waste includes all non-regulated waste generated in radiological controlled areas (RCAs) that has been actively segregated as ''clean'' (i.e., nonradioactive) through the use of waste generator AK. GIC waste that is verified clean can be disposed of at the Los Alamos County Landfill. It is estimated that 50-90% of the low-density room trash from RCAs at LANL might be free of contamination. To date, with pilot programs at five facilities at LANL, 3000 cubic feet of GIC waste has been verified clean by these two prototype systems. Both the WAND and HERCULES systems are highly sensitive measurement systems optimized to detect very small quantities of common LANL radionuclides. Both of the systems use a set of phoswich scintillation detectors in close proximity to the waste, which have the capability of detecting plutonium-239 concentrations below 3 pCi per gram of low density waste. Both systems detect low-energy x-rays and a broad range of gamma rays (10-2000 keV), while the WAND system also detects high energy beta particles (>100 keV). The WAND system consists of a bank of six shielded detectors which screen low density shredded waste or stacked sheets of paper moving under the detectors in a twelve inch swath on a conveyor belt. The WAND system was developed and tested at the Los Alamos Plutonium Facility in conjunction with instrument system designers from the Los Alamos Safeguards Science and Technology group. The HERCULES system consists of a bank of three shielded detectors which screen low-density waste in two cubic foot cardboard boxes or in bags sitting on a turntable. Waste that does not pass the verification process can be examined within the facility to determine the type and quantity of the contamination and its origin within a waste container. The paper discusses lessons learned that have helped generators improve their AK segregation.

  16. Fuel-cycle assessment of selected bioethanol production.

    SciTech Connect (OSTI)

    Wu, M.; Wang, M.; Hong, H.; Energy Systems

    2007-01-31

    A large amount of corn stover is available in the U.S. corn belt for the potential production of cellulosic bioethanol when the production technology becomes commercially ready. In fact, because corn stover is already available, it could serve as a starting point for producing cellulosic ethanol as a transportation fuel to help reduce the nation's demand for petroleum oil. Using the data available on the collection and transportation of corn stover and on the production of cellulosic ethanol, we have added the corn stover-to-ethanol pathway in the GREET model, a fuel-cycle model developed at Argonne National Laboratory. We then analyzed the life-cycle energy use and emission impacts of corn stover-derived fuel ethanol for use as E85 in flexible fuel vehicles (FFVs). The analysis included fertilizer manufacturing, corn farming, farming machinery manufacturing, stover collection and transportation, ethanol production, ethanol transportation, and ethanol use in light-duty vehicles (LDVs). Energy consumption of petroleum oil and fossil energy, emissions of greenhouse gases (carbon dioxide [CO{sub 2}], nitrous oxide [N{sub 2}O], and methane [CH{sub 4}]), and emissions of criteria pollutants (carbon monoxide [CO], volatile organic compounds [VOCs], nitrogen oxide [NO{sub x}], sulfur oxide [SO{sub x}], and particulate matter with diameters smaller than 10 micrometers [PM{sub 10}]) during the fuel cycle were estimated. Scenarios of ethanol from corn grain, corn stover, and other cellulosic feedstocks were then compared with petroleum reformulated gasoline (RFG). Results showed that FFVs fueled with corn stover ethanol blends offer substantial energy savings (94-95%) relative to those fueled with RFG. For each Btu of corn stover ethanol produced and used, 0.09 Btu of fossil fuel is required. The cellulosic ethanol pathway avoids 86-89% of greenhouse gas emissions. Unlike the life cycle of corn grain-based ethanol, in which the ethanol plant consumes most of the fossil fuel, farming consumes most of the fossil fuel in the life cycle of corn stover-based ethanol.

  17. Integrating Nuclear Energy to Oilfield Operations – Two Case Studies

    SciTech Connect (OSTI)

    Eric P. Robertson; Lee O. Nelson; Michael G. McKellar; Anastasia M. Gandrik; Mike W. Patterson

    2011-11-01

    Fossil fuel resources that require large energy inputs for extraction, such as the Canadian oil sands and the Green River oil shale resource in the western USA, could benefit from the use of nuclear power instead of power generated by natural gas combustion. This paper discusses the technical and economic aspects of integrating nuclear energy with oil sands operations and the development of oil shale resources. A high temperature gas reactor (HTGR) that produces heat in the form of high pressure steam (no electricity production) was selected as the nuclear power source for both fossil fuel resources. Both cases were based on 50,000 bbl/day output. The oil sands case was a steam-assisted, gravity-drainage (SAGD) operation located in the Canadian oil sands belt. The oil shale development was an in-situ oil shale retorting operation located in western Colorado, USA. The technical feasibility of the integrating nuclear power was assessed. The economic feasibility of each case was evaluated using a discounted cash flow, rate of return analysis. Integrating an HTGR to both the SAGD oil sands operation and the oil shale development was found to be technically feasible for both cases. In the oil sands case, integrating an HTGR eliminated natural gas combustion and associated CO2 emissions, although there were still some emissions associated with imported electrical power. In the in situ oil shale case, integrating an HTGR reduced CO2 emissions by 88% and increased natural gas production by 100%. Economic viabilities of both nuclear integrated cases were poorer than the non-nuclear-integrated cases when CO2 emissions were not taxed. However, taxing the CO2 emissions had a significant effect on the economics of the non-nuclear base cases, bringing them in line with the economics of the nuclear-integrated cases. As we move toward limiting CO2 emissions, integrating non-CO2-emitting energy sources to the development of energy-intense fossil fuel resources is becoming increasingly important. This paper attempts to reduce the barriers that have traditionally separated fossil fuel development and application of nuclear power and to promote serious discussion of ideas about hybrid energy systems.

  18. 2015 Los Alamos Space Weather Summer School Research Reports

    SciTech Connect (OSTI)

    Cowee, Misa; Chen, Yuxi; Desai, Ravindra; Hassan, Ehab; Kalmoni, Nadine; Lin, Dong; Depascuale, Sebastian; Hughes, Randall Scott; Zhou, Hong

    2015-11-24

    The fifth Los Alamos Space Weather Summer School was held June 1st - July 24th, 2015, at Los Alamos National Laboratory (LANL). With renewed support from the Institute of Geophysics, Planetary Physics, and Signatures (IGPPS) and additional support from the National Aeronautics and Space Administration (NASA) and the Department of Energy (DOE) Office of Science, we hosted a new class of five students from various U.S. and foreign research institutions. The summer school curriculum includes a series of structured lectures as well as mentored research and practicum opportunities. Lecture topics including general and specialized topics in the field of space weather were given by a number of researchers affiliated with LANL. Students were given the opportunity to engage in research projects through a mentored practicum experience. Each student works with one or more LANL-affiliated mentors to execute a collaborative research project, typically linked with a larger ongoing research effort at LANL and/or the student’s PhD thesis research. This model provides a valuable learning experience for the student while developing the opportunity for future collaboration. This report includes a summary of the research efforts fostered and facilitated by the Space Weather Summer School. These reports should be viewed as work-in-progress as the short session typically only offers sufficient time for preliminary results. At the close of the summer school session, students present a summary of their research efforts. Titles of the papers included in this report are as follows: Full particle-in-cell (PIC) simulation of whistler wave generation, Hybrid simulations of the right-hand ion cyclotron anisotropy instability in a sub-Alfvénic plasma flow, A statistical ensemble for solar wind measurements, Observations and models of substorm injection dispersion patterns, Heavy ion effects on Kelvin-Helmholtz instability: hybrid study, Simulating plasmaspheric electron densities with a two-component electric field model, Ion and electron heating by whistler turbulence: parametric studies via particle-in-cell simulation, and The statistics of relativistic electron pitch angle distribution in the Earth’s radiation belt based on the Van Allen Probes measurements.

  19. Transport of anthropogenic and biomass burning aerosols from Europe to the Arctic during spring 2008

    SciTech Connect (OSTI)

    Marelle, L.; Raut, Jean-Christophe; Thomas, J. L.; Law, K. S.; Quennehen, Boris; Ancellet, G.; Pelon, J.; Schwarzenboeck, A.; Fast, Jerome D.

    2015-04-10

    During the POLARCAT-France airborne campaign in April 2008, pollution originating from anthropogenic and biomass burning emissions was measured in the European Arctic. We compare these aircraft measurements with simulations using the WRF-Chem model to investigate model representation of aerosols transported from Europe to the Arctic. Modeled PM2.5 is evaluated using European Monitoring and Evaluation Programme (EMEP) measurements in source regions and POLARCAT aircraft measurements in the Scandinavian Arctic. Total PM2.5 agrees well with the measurements, although the model overestimates nitrate and underestimates organic carbon in source regions. Using WRF-Chem in combination with the Lagrangian model FLEXPART-WRF, we find that during the campaign the research aircraft sampled two different types of European plumes: mixed anthropogenic and fire plumes from eastern Europe and Russia transported below 2 km, and anthropogenic plumes from central Europe uplifted by warm conveyor belt circulations to 56 km. Both modeled plume types had undergone significant wet scavenging (> 50% PM10) during transport. Modeled aerosol vertical distributions and optical properties below the aircraft are evaluated in the Arctic using airborne lidar measurements. Model results show that the pollution event transported aerosols into the Arctic (> 66.6 N) for a 4-day period. During this 4-day period, biomass burning emissions have the strongest influence on concentrations between 2.5 and 3 km altitudes, while European anthropogenic emissions influence aerosols at both lower (~ 1.5 km) and higher altitudes (~ 4.5 km). As a proportion of PM2.5, modeled black carbon and SO4= concentrations are more enhanced near the surface in anthropogenic plumes. The European plumes sampled during the POLARCAT-France campaign were transported over the region of springtime snow cover in northern Scandinavia, where they had a significant local atmospheric warming effect. We find that, during this transport event, the average modeled top-of-atmosphere (TOA) shortwave direct and semi-direct radiative effect (DSRE) north of 60 N over snow and ice-covered surfaces reaches +0.58 W m?2, peaking at +3.3 W m?2 at noon over Scandinavia and Finland.

  20. Geologic Controls of Hydrocarbon Occurrence in the Appalachian Basin in Eastern Tennessee, Southwestern Virginia, Eastern Kentucky, and Southern West Virginia

    SciTech Connect (OSTI)

    Hatcher, Robert D

    2005-11-30

    This report summarizes the accomplishments of a three-year program to investigate the geologic controls of hydrocarbon occurrence in the southern Appalachian basin in eastern Tennessee, southwestern Virginia, eastern Kentucky, and southern West Virginia. The project: (1) employed the petroleum system approach to understand the geologic controls of hydrocarbons; (2) attempted to characterize the P-T parameters driving petroleum evolution; (3) attempted to obtain more quantitative definitions of reservoir architecture and identify new traps; (4) is worked with USGS and industry partners to develop new play concepts and geophysical log standards for subsurface correlation; and (5) geochemically characterized the hydrocarbons (cooperatively with USGS). Third-year results include: All project milestones have been met and addressed. We also have disseminated this research and related information through presentations at professional meetings, convening a major workshop in August 2003, and the publication of results. Our work in geophysical log correlation in the Middle Ordovician units is bearing fruit in recognition that the criteria developed locally in Tennessee and southern Kentucky are more extendible than anticipated earlier. We have identified a major 60 mi-long structure in the western part of the Valley and Ridge thrust belt that has been successfully tested by a local independent and is now producing commercial amounts of hydrocarbons. If this structure is productive along strike, it will be one of the largest producing structures in the Appalachians. We are completing a more quantitative structural reconstruction of the Valley and Ridge and Cumberland Plateau than has been made before. This should yield major dividends in future exploration in the southern Appalachian basin. Our work in mapping, retrodeformation, and modeling of the Sevier basin is a major component of the understanding of the Ordovician petroleum system in this region. Prior to our undertaking this project, this system was the least understood in the Appalachian basin. This project, in contrast to many if not most programs undertaken in DOE laboratories, has a major educational component wherein three Ph.D. students have been partially supported by this grant, one M.S. student partially supported, and another M.S. student fully supported by the project. These students will be well prepared for professional careers in the oil and gas industry.

  1. Development of Continuous, Direct Feedback Control Systems for Sintering of Metallic Components

    SciTech Connect (OSTI)

    Diran Apelian; Marc M. Baum

    2006-09-18

    N,N.-Ethylenebisstearimide (EBS) is one of the most commonlyused lubricants in the powder metallurgy (PM) industry in the sintering process. During sintering, the lubricated powder compacts are heat-treated to temperatures in excess of 1,200 C thus fusing adjacent particles and yielding a part with improved mechanical strength. Delubrication commonly is achieved in the first zone of a sintering furnace by heating the part to temperatures in the 500-600 C temperature range at a fixed rate and under controlled atmospheric conditions; this strategy minimizes defects, carbon contamination, and compact deformation. The de-lubricated part then enters the second zone (commonly in the 1200-1300 C temperature range) for sintering. The third zone cools the sintered part at a desired rate to obtain the requisite micro-structural properties. Controlled delubrication is imperative towards achieving high quality parts for the following reasons: the elevated thermal gradient at the transition between the first and second zones can cause parts to expand rapidly and develop microscopic fissures (.blistering.); improper gas flows and belt speeds can lead to carbon deposition on the part and at the grain boundaries (sooting); delubrication products deposit throughout the furnace, even in the coolers, which are far removed from the preheating chamber, leading to significant maintenance costs; pollutants emitted in the exhaust stream of furnaces operating inefficiently are increasingly of environmental concern. In practice, lubricant removal is difficult to control, which often leads to reduced yields in PM manufacturing processes. Throughput is another important issue: process control ideally should lead to a delubrication cycle that yields defect-free parts in a minimum of furnace time, thereby increasing productivity and reducing the net energy consumption. Efficient process control requires rapid monitoring of suitable indicators, preferably gasphase products of delubrication. EBS thermolyzes relatively cleanly in a range of furnace atmospheres, but the mechanism governing the pyrolysis of EBS, compacted with iron powder, is not known and needs to be investigated to determine the parameters important for industrial control, as well as the optimal conditions of delubrication. In addition, a thorough understanding of the pre-sintering chemistry will enable the development of a process control sensor.

  2. Transport of anthropogenic and biomass burning aerosols from Europe to the Arctic during spring 2008

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Marelle, L.; Raut, Jean-Christophe; Thomas, J. L.; Law, K. S.; Quennehen, Boris; Ancellet, G.; Pelon, J.; Schwarzenboeck, A.; Fast, Jerome D.

    2015-04-10

    During the POLARCAT-France airborne campaign in April 2008, pollution originating from anthropogenic and biomass burning emissions was measured in the European Arctic. We compare these aircraft measurements with simulations using the WRF-Chem model to investigate model representation of aerosols transported from Europe to the Arctic. Modeled PM2.5 is evaluated using European Monitoring and Evaluation Programme (EMEP) measurements in source regions and POLARCAT aircraft measurements in the Scandinavian Arctic. Total PM2.5 agrees well with the measurements, although the model overestimates nitrate and underestimates organic carbon in source regions. Using WRF-Chem in combination with the Lagrangian model FLEXPART-WRF, we find that duringmore » the campaign the research aircraft sampled two different types of European plumes: mixed anthropogenic and fire plumes from eastern Europe and Russia transported below 2 km, and anthropogenic plumes from central Europe uplifted by warm conveyor belt circulations to 5–6 km. Both modeled plume types had undergone significant wet scavenging (> 50% PM10) during transport. Modeled aerosol vertical distributions and optical properties below the aircraft are evaluated in the Arctic using airborne lidar measurements. Model results show that the pollution event transported aerosols into the Arctic (> 66.6° N) for a 4-day period. During this 4-day period, biomass burning emissions have the strongest influence on concentrations between 2.5 and 3 km altitudes, while European anthropogenic emissions influence aerosols at both lower (~ 1.5 km) and higher altitudes (~ 4.5 km). As a proportion of PM2.5, modeled black carbon and SO4= concentrations are more enhanced near the surface in anthropogenic plumes. The European plumes sampled during the POLARCAT-France campaign were transported over the region of springtime snow cover in northern Scandinavia, where they had a significant local atmospheric warming effect. We find that, during this transport event, the average modeled top-of-atmosphere (TOA) shortwave direct and semi-direct radiative effect (DSRE) north of 60° N over snow and ice-covered surfaces reaches +0.58 W m−2, peaking at +3.3 W m−2 at noon over Scandinavia and Finland.« less

  3. Overview of interstate hydrogen pipeline systems.

    SciTech Connect (OSTI)

    Gillette, J .L.; Kolpa, R. L

    2008-02-01

    The use of hydrogen in the energy sector of the United States is projected to increase significantly in the future. Current uses are predominantly in the petroleum refining sector, with hydrogen also being used in the manufacture of chemicals and other specialized products. Growth in hydrogen consumption is likely to appear in the refining sector, where greater quantities of hydrogen will be required as the quality of the raw crude decreases, and in the mining and processing of tar sands and other energy resources that are not currently used at a significant level. Furthermore, the use of hydrogen as a transportation fuel has been proposed both by automobile manufacturers and the federal government. Assuming that the use of hydrogen will significantly increase in the future, there would be a corresponding need to transport this material. A variety of production technologies are available for making hydrogen, and there are equally varied raw materials. Potential raw materials include natural gas, coal, nuclear fuel, and renewables such as solar, wind, or wave energy. As these raw materials are not uniformly distributed throughout the United States, it would be necessary to transport either the raw materials or the hydrogen long distances to the appropriate markets. While hydrogen may be transported in a number of possible forms, pipelines currently appear to be the most economical means of moving it in large quantities over great distances. One means of controlling hydrogen pipeline costs is to use common rights-of-way (ROWs) whenever feasible. For that reason, information on hydrogen pipelines is the focus of this document. Many of the features of hydrogen pipelines are similar to those of natural gas pipelines. Furthermore, as hydrogen pipeline networks expand, many of the same construction and operating features of natural gas networks would be replicated. As a result, the description of hydrogen pipelines will be very similar to that of natural gas pipelines. The following discussion will focus on the similarities and differences between the two pipeline networks. Hydrogen production is currently concentrated in refining centers along the Gulf Coast and in the Farm Belt. These locations have ready access to natural gas, which is used in the steam methane reduction process to make bulk hydrogen in this country. Production centers could possibly change to lie along coastlines, rivers, lakes, or rail lines, should nuclear power or coal become a significant energy source for hydrogen production processes. Should electrolysis become a dominant process for hydrogen production, water availability would be an additional factor in the location of production facilities. Once produced, hydrogen must be transported to markets. A key obstacle to making hydrogen fuel widely available is the scale of expansion needed to serve additional markets. Developing a hydrogen transmission and distribution infrastructure would be one of the challenges to be faced if the United States is to move toward a hydrogen economy. Initial uses of hydrogen are likely to involve a variety of transmission and distribution methods. Smaller users would probably use truck transport, with the hydrogen being in either the liquid or gaseous form. Larger users, however, would likely consider using pipelines. This option would require specially constructed pipelines and the associated infrastructure. Pipeline transmission of hydrogen dates back to late 1930s. These pipelines have generally operated at less than 1,000 pounds per square inch (psi), with a good safety record. Estimates of the existing hydrogen transmission system in the United States range from about 450 to 800 miles. Estimates for Europe range from about 700 to 1,100 miles (Mohipour et al. 2004; Amos 1998). These seemingly large ranges result from using differing criteria in determining pipeline distances. For example, some analysts consider only pipelines above a certain diameter as transmission lines. Others count only those pipelines that transport hydrogen from a producer to a customer (e.g., t

  4. The genesis solar-wind sample return mission

    SciTech Connect (OSTI)

    Wiens, Roger C

    2009-01-01

    The compositions of the Earth's crust and mantle, and those of the Moon and Mars, are relatively well known both isotopically and elementally. The same is true of our knowledge of the asteroid belt composition, based on meteorite analyses. Remote measurements of Venus, the Jovian atmosphere, and the outer planet moons, have provided some estimates of their compositions. The Sun constitutes a large majority, > 99%, of all the matter in the solar system. The elemental composition of the photosphere, the visible 'surface' of the Sun, is constrained by absorption lines produced by particles above the surface. Abundances for many elements are reported to the {+-}10 or 20% accuracy level. However, the abundances of other important elements, such as neon, cannot be determined in this way due to a relative lack of atomic states at low excitation energies. Additionally and most importantly, the isotopic composition of the Sun cannot be determined astronomically except for a few species which form molecules above sunspots, and estimates derived from these sources lack the accuracy desired for comparison with meteoritic and planetary surface samples measured on the Earth. The solar wind spreads a sample of solar particles throughout the heliosphere, though the sample is very rarified: collecting a nanogram of oxygen, the third most abundant element, in a square centimeter cross section at the Earth's distance from the Sun takes five years. Nevertheless, foil collectors exposed to the solar wind for periods of hours on the surface of the Moon during the Apollo missions were used to determine the helium and neon solar-wind compositions sufficiently to show that the Earth's atmospheric neon was significantly evolved relative to the Sun. Spacecraft instruments developed subsequently have provided many insights into the composition of the solar wind, mostly in terms of elemental composition. These instruments have the advantage of observing a number of parameters simultaneously, including charge state distributions, velocities, and densities, all of which have been instrumental in characterizing the nature of the solar wind. However, these instruments have lacked the ability to make large dynamic range measurements of adjacent isotopes (i.e., {sup 17}O/{sup 16}O {approx} 2500) or provide the permil (tenths of percent) accuracy desirable for comparison with geochemical isotopic measurements. An accurate knowledge of the solar and solar-wind compositions helps to answer important questions across a number of disciplines. It aids in understanding the acceleration mechanisms of the solar wind, gives an improved picture of the charged particle environment near the photosphere, it constrains processes within the Sun over its history, and it provides a database by which to compare differences among planetary systems with the solar system's starting composition, providing key information on planetary evolution. For example, precise knowledge of solar isotopic and elemental compositions of volatile species in the Sun provides a baseline for models of atmospheric evolution over time for Earth, Venus, and Mars. Additionally, volatile and chemically active elements such as C, H, O, N, and S can tell us about processes active during the evolution of the solar nebula. A classic example of this is the oxygen isotope system. In the 1970s it was determined that the oxygen isotopic ratio in refractory inclusions in primitive meteorites was enriched {approx}4% in {sup 16}O relative to the average terrestrial, lunar, and thermally processed meteorite materials. In addition, all processed solar-system materials appeared to each have a unique oxygen isotopic composition (except the Moon and Earth, which are thought to be formed from the same materials), though differences are in the fraction of a percent range, much smaller than the refractory material {sup 16}O enrichment. Several theories were developed over the years to account for the oxygen isotope heterogeneity, each theory predicting a different solar isotopic composition and each invoking a differ

  5. A search for fast optical transients in the Pan-STARRS1 medium-deep survey: M-dwarf flares, asteroids, limits on extragalactic rates, and implications for LSST

    SciTech Connect (OSTI)

    Berger, E.; Leibler, C. N.; Chornock, R.; Foley, R. J.; Soderberg, A. M.; Rest, A.; Price, P. A.; Burgett, W. S.; Chambers, K. C.; Flewelling, H.; Huber, M. E.; Magnier, E. A.; Tonry, J. L.; Metcalfe, N.; Stubbs, C. W.

    2013-12-10

    We present a search for fast optical transients (? ? 0.5 hr-1 day) using repeated observations of the Pan-STARRS1 Medium-Deep Survey (PS1/MDS) fields. Our search takes advantage of the consecutive g {sub P1} r {sub P1} observations (16.5 minutes in each filter), by requiring detections in both bands, with non-detections on preceding and subsequent nights. We identify 19 transients brighter than 22.5 AB mag (S/N ? 10). Of these, 11 events exhibit quiescent counterparts in the deep PS1/MDS templates that we identify as M4-M9 dwarfs at d ? 0.2-1.2 kpc. The remaining eight transients lack quiescent counterparts, exhibit mild but significant astrometric shifts between the g {sub P1} and r {sub P1} images, colors of (g r){sub P1} ? 0.5-0.8 mag, non-varying light curves, and locations near the ecliptic plane with solar elongations of about 130, which are all indicative of main-belt asteroids near the stationary point of their orbits. With identifications for all 19 transients, we place an upper limit of R {sub FOT}(? ? 0.5 hr) ? 0.12 deg{sup 2} day{sup 1} (95% confidence level) on the sky-projected rate of extragalactic fast transients at ? 22.5 mag, a factor of 30-50 times lower than previous limits; the limit for a timescale of ?1 day is R {sub FOT} ? 2.4 10{sup 3} deg{sup 2} day{sup 1}. To convert these sky-projected rates to volumetric rates, we explore the expected peak luminosities of fast optical transients powered by various mechanisms, and find that non-relativistic events are limited to M ? 10 to ? 14 mag for a timescale of ?0.5 hr to ?1 day, while relativistic sources (e.g., gamma-ray bursts, magnetar-powered transients) can reach much larger luminosities. The resulting volumetric rates are ? 13 Mpc{sup 3} yr{sup 1} (M ? 10 mag), ? 0.05 Mpc{sup 3} yr{sup 1} (M ? 14 mag), and ? 10{sup 6} Mpc{sup 3} yr{sup 1} (M ? 24 mag), significantly above the nova, supernova, and gamma-ray burst rates, respectively, indicating that much larger surveys are required to provide meaningful constraints. Motivated by the results of our search, we discuss strategies for identifying fast optical transients in the Large Synoptic Survey Telescope main survey, and reach the optimistic conclusion that the veil of foreground contaminants can be lifted with the survey data, without the need for expensive follow-up observations.

  6. Phase I - Smart Grid Data Access Pilot Program: Utilizing STEM Education as a Catalyst for Residential Consumer Decision Making and Change

    SciTech Connect (OSTI)

    Lishness, Alan

    2014-11-19

    Under Phase I of the Smart Grid Data Access Pilot Program, the Gulf of Maine Research Institute (GMRI) partnered with Central Maine Power (CMP), and the Maine Mathematics and Science Alliance (MMSA) and engaged key vendors Tilson Government Services, LLC (Tilson), and Image Works to demonstrate the efficacy of PowerHouse, an interactive online learning environment linking middle school students with their home electricity consumption data provided through CMP’s Advanced Metering Infrastructure (AMI). The goal of the program is to harness the power of youth to alter home energy consumption behaviors using AMI data. Successful programs aimed at smoking cessation, recycling, and seat belt use have demonstrated the power of young people to influence household behaviors. In an era of increasing concern about energy costs, availability, and human impacts on global climate, GMRI sought to demonstrate the effectiveness of a student-focused approach to understanding and managing household energy use. We also sought to contribute to a solid foundation of science-literate students who can analyze evidence to find solutions to increasingly complex energy challenges. While technical hurdles prevented us from achieving the scale of student engagement projected in the original proposal, results from Phase I nevertheless demonstrate the effectiveness of PowerHouse to bring science and math home to the kitchen table and to help students and families understand and manage electricity consumption: • 144 teachers learned about PowerHouse through workshops or other events and 33 teachers engaged students in the PowerHouse curriculum in their classrooms over the duration of this project. Fifty teachers have shared plans to use PowerHouse during this calendar year (2015). • Over the duration of this project, 1630 students created accounts on PowerHouse and 295 of these students connected their CMP Energy Manager electricity data to PowerHouse. • During our most recent complete school year (2013-2014): o 9 teachers engaged their students in a 4 (or more) week experience using PowerHouse curriculum o Those 9 teachers represented 357 students o 114 of the 357 students were connected to their CMP Energy Manager data through PowerHouse; the remaining students used the PowerHouse program and curriculum without connecting to Energy Manager The number of student accounts connected to their CMP AMI electricity data through PowerHouse is far below the goal of 1000 accounts. This is primarily attributable to successive technical challenges described in more detail below. However, program staff continue to address all aspects of this challenge: ongoing recruitment of teachers into PowerHouse, classroom processes to smooth out communications with families, and streamlining the technology. We anticipate reaching the goal of 1000 total CMP-connected accounts by the close of the 2015-2016 school year.

  7. In-Line Crack and Stress Detection in Silicon Solar Cells Using Resonance Ultrasonic Vibrations

    SciTech Connect (OSTI)

    Ostapenko, Sergei

    2013-04-03

    Statement of Problem and Objectives. Wafer breakage in automated solar cell production lines is identified as a major technical problem and a barrier for further cost reduction of silicon solar module manufacturing. To the best of our knowledge, there are no commercial systems addressing critical needs for in-line inspection of the mechanical quality of solar wafers and cells. The principal objective of the SBIR program is to validate through experiments and computer modeling the applicability of the Resonance Ultrasonic Vibrations system, which ultimately can be used as a real-time in-line manufacturing quality control tool for fast detection of mechanically unstable silicon solar cells caused by cracks. The specific objective of Phase II is to move the technology of in-line crack detection from the laboratory level to commercial demonstration through development of a system prototype. The fragility of silicon wafers possessing low mechanical strength is attributed to peripheral and bulk millimeter-length cracks. The research program is based on feasibility results obtained during Phase I, which established that: (i) the Resonance Ultrasonic Vibrations method is applicable to as-cut, processed wafers and finished cells; (ii) the method sensitivity depends on the specific processing step; it is highest in as-cut wafers and lowest in wafers with metallization pattern and grid contacts; (iii) the system is capable of matching the 2.0 seconds per wafer throughput rate of state-of-art solar cell production lines; (iv) finite element modeling provides vibration mode analysis along with peak shift versus crack length and crack location dependence; (v) a high 91% crack rejection rate was confirmed through experimentation and statistical analysis. The Phase II project has the following specific tasks: (i) specify optimal configurations of the in-line system?¢????s component hardware and software; (ii) develop and justify a system prototype that meets major specifications for an in-line crack detection unit, such as high throughput rate, high level of stability, reproducibility of data acquisition and analysis, and high sensitivity with respect to crack length and crack location; (iii) design a system platform that allows easy integration within and adaptation to various solar cell belt-type production lines; (iv) develop a testing protocol providing quality certification of the production-grade system. Commercial Application of the proposed activity consists of bringing to the solar market a new high-tech product based on an innovative solution and patented methodology to contribute to cost reduction of silicon solar module production. The solar industry, with crystalline silicon as a dominant segment, shows outstanding performance, with approximately 25% yearly growth during the last years. Despite a slowdown with only 5.6 GW installations in 2009, solar module production for the 2010 and 2011 years was recovered. According to European Photonics Industry Consortium new solar PV installations grow by 56% compared to 2010 reached 64.7 GW in 2011. Revenues in the PV industry reached a record high of $93 billion in 2011, a 13.4 percent gain over 2010 â?? and 150 percent over 2009. This growth was forecasted to continue in 2013 with double digits growth. The solar industry is economically driven to make solar panels of the highest conversion efficiency and reliability at the lowest production cost. The Resonance Ultrasonic Vibration system addresses critical needs of the silicon-based solar industry by providing a quality control method and tool, which will improve productivity, increase reliability of products and reduce manufacturing cost of solar panels.

  8. INCREASED OIL PRODUCTION AND RESERVES UTILIZING SECONDARY/TERTIARY RECOVERY TECHNIQUES ON SMALL RESERVOIRS IN THE PARADOX BASIN, UTAH

    SciTech Connect (OSTI)

    Thomas C. Chidsey, Jr.

    2002-11-01

    The Paradox Basin of Utah, Colorado, and Arizona contains nearly 100 small oil fields producing from shallow-shelf carbonate buildups or mounds within the Desert Creek zone of the Pennsylvanian (Desmoinesian) Paradox Formation. These fields typically have one to four wells with primary production ranging from 700,000 to 2,000,000 barrels (111,300-318,000 m{sup 3}) of oil per field at a 15 to 20 percent recovery rate. Five fields in southeastern Utah were evaluated for waterflood or carbon-dioxide (CO{sub 2})-miscible flood projects based upon geological characterization and reservoir modeling. Geological characterization on a local scale focused on reservoir heterogeneity, quality, and lateral continuity as well as possible compartmentalization within each of the five project fields. The Desert Creek zone includes three generalized facies belts: (1) open-marine, (2) shallow-shelf and shelf-margin, and (3) intra-shelf, salinity-restricted facies. These deposits have modern analogs near the coasts of the Bahamas, Florida, and Australia, respectively, and outcrop analogs along the San Juan River of southeastern Utah. The analogs display reservoir heterogeneity, flow barriers and baffles, and lithofacies geometry observed in the fields; thus, these properties were incorporated in the reservoir simulation models. Productive carbonate buildups consist of three types: (1) phylloid algal, (2) coralline algal, and (3) bryozoan. Phylloid-algal buildups have a mound-core interval and a supra-mound interval. Hydrocarbons are stratigraphically trapped in porous and permeable lithotypes within the mound-core intervals of the lower part of the buildups and the more heterogeneous supramound intervals. To adequately represent the observed spatial heterogeneities in reservoir properties, the phylloid-algal bafflestones of the mound-core interval and the dolomites of the overlying supra-mound interval were subdivided into ten architecturally distinct lithotypes, each of which exhibits a characteristic set of reservoir properties obtained from outcrop analogs, cores, and geophysical logs. The Anasazi and Runway fields were selected for geostatistical modeling and reservoir compositional simulations. Models and simulations incorporated variations in carbonate lithotypes, porosity, and permeability to accurately predict reservoir responses. History matches tied previous production and reservoir pressure histories so that future reservoir performances could be confidently predicted. The simulation studies showed that despite most of the production being from the mound-core intervals, there were no corresponding decreases in the oil in place in these intervals. This behavior indicates gravity drainage of oil from the supra-mound intervals into the lower mound-core intervals from which the producing wells' major share of production arises. The key to increasing ultimate recovery from these fields (and similar fields in the basin) is to design either waterflood or CO{sub 2}-miscible flood projects capable of forcing oil from high-storage-capacity but low-recovery supra-mound units into the high-recovery mound-core units. Simulation of Anasazi field shows that a CO{sub 2} flood is technically superior to a waterflood and economically feasible. For Anasazi field, an optimized CO{sub 2} flood is predicted to recover a total 4.21 million barrels (0.67 million m3) of oil representing in excess of 89 percent of the original oil in place. For Runway field, the best CO{sub 2} flood is predicted to recover a total of 2.4 million barrels (0.38 million m3) of oil representing 71 percent of the original oil in place. If the CO{sub 2} flood performed as predicted, it is a financially robust process for increasing the reserves in the many small fields in the Paradox Basin. The results can be applied to other fields in the Rocky Mountain region, the Michigan and Illinois Basins, and the Midcontinent.

  9. Final Technical Report of project: "Contactless Real-Time Monitoring of Paper Mechanical Behavior During Papermaking"

    SciTech Connect (OSTI)

    Emmanuel Lafond; Paul Ridgway; Ted Jackson; Rick Russo; Ken Telschow; Vance Deason; Yves Berthelot; David Griggs; Xinya Zhang; Gary Baum

    2005-08-30

    The early precursors of laser ultrasonics on paper were Prof. Y. Berthelot from the Georgia Institute of Technology/Mechanical Engineering department, and Prof. P. Brodeur from the Institute of Paper Science and Technology, both located in Atlanta, Georgia. The first Ph.D. thesis that shed quite some light on the topic, but also left some questions unanswered, was completed by Mont A. Johnson in 1996. Mont Johnson was Prof. Berthelot's student at Georgia Tech. In 1997 P. Brodeur proposed a project involving himself, Y. Berthelot, Dr. Ken Telschow and Mr. Vance Deason from INL, Honeywell-Measurex and Dr. Rick Russo from LBNL. The first time the proposal was not accepted and P. Brodeur decided to re-propose it without the involvement from LBNL. Rick Russo proposed a separate project on the same topic on his side. Both proposals were finally accepted and work started in the fall of 1997 on the two projects. Early on, the biggest challenge was to find an optical detection method which could detect laser-induced displacements of the web surface that are of the order of .1 micron in the ultrasonic range. This was to be done while the web was having an out-of-plane amplitude of motion in the mm range due to web flutter; while moving at 10 m/s to 30 m/s in the plane of the web, on the paper machine. Both teams grappled with the same problems and tried similar methods in some cases, but came up with two similar but different solutions one year later. The IPST, GT, INL team found that an interferometer made by Lasson Technologies Inc. using the photo-induced electro-motive force in Gallium Arsenide was able to detect ultrasonic waves up to 12-15 m/s. It also developed in house an interferometer using the Two-Wave Mixing effect in photorefractive crystals that showed good promises for on-line applications, and experimented with a scanning mirror to reduce motion-induced texture noise from the web and improve signal to noise ratio. On its side, LBNL had the idea to combine a commercial Mach-Zehnder interferometer to a spinning mirror synchronized to the web speed, in order to make almost stationary measurements. The method was demonstrated at up to 10 m/s. Both teams developed their own version of a web simulator that was driving a web of paper at 10 m/s or higher. The Department of Energy and members of the Agenda 2020 started to make a push for merging the two projects. This made sense because their topics were really identical but this was not well received by Prof. Brodeur. Finally IPST decided to reassign the direction of the IPST-INL-GT project in the spring of 1999 to Prof. Chuck Habeger so that the two teams could work together. Also at this time, Honeywell-Measurex dropped as a member of the team. It was replaced by ABB Industrial Systems whose engineers had extensive previous experience of working with ultrasonic sensors on paperboard. INL also finished its work on the project as its competencies were partly redundant with LBNL. From the summer of 1999, the IPST-GT and LBNL teams were working together and helped each other often by collaborating and visiting either laboratory when was necessary. Around the beginning of 2000, began an effort at IPST to create an off-line laser-ultrasonics instrument that could perform automated measurements of paper and paperboard's bending stiffness. It was widely known that the mechanical bending tests of paper used for years by the paper industry were very inaccurate and exhibited poor reproducibility; therefore the team needed a new instrument of reference to validate its future on-line results. In 1999-2000, the focus of the on-line instrument was on a pre-industrial demonstration on a pilot coater while reducing the damage to the web caused by the generation laser, below the threshold where it could be visible by the naked eye. During the spring of 2000 Paul Ridgway traveled to IPST and brought with him a redesigned system still using the same Mach-Zehnder interferometer as before, but this time employing an electric motor-driven spinning mirror instead of the previously belt-driven m

  10. 11,23,1,1,,19,10,"BANGOR HYDRO ELECTRIC CO","ELLSWORTH",0,,1179,"0A",1294,,,95,2941,0,0,3518,0,0,4870,0,0,1732,0,0,3252,0,0,2193,0,0,134,0,0,447,0,0,465,0,0,538,0,0,4295,0,0,3601,0,0,1469,6,50159,"WAT","HY"

    U.S. Energy Information Administration (EIA) Indexed Site

    NAD_UTIL","FILLER","EFFDATE","STATUS","MULTIST","YEAR","GEN01","CON01","STK01","GEN02","CON02","STK02","GEN03","CON03","STK03","GEN04","CON04","STK04","GEN05","CON05","STK05","GEN06","CON06","STK06","GEN07","CON07","STK07","GEN08","CON08","STK08","GEN09","CON09","STK09","GEN10","CON10","STK10","GEN11","CON11","STK11","GEN12","CON12","STK12","PCODE","NERC","UTILCODE","FUELDESC","PMDESC" 11,23,1,1,,19,10,"BANGOR HYDRO ELECTRIC CO","ELLSWORTH",0,,1179,"0A",1294,,,95,2941,0,0,3518,0,0,4870,0,0,1732,0,0,3252,0,0,2193,0,0,134,0,0,447,0,0,465,0,0,538,0,0,4295,0,0,3601,0,0,1469,6,50159,"WAT","HY" 11,23,1,1,,19,15,"BANGOR HYDRO ELECTRIC CO","HOWLAND",0,,1179,"0A",1294,,,95,772,0,0,858,0,0,1012,0,0,727,0,0,1061,0,0,917,0,0,385,0,0,118,0,0,0,0,0,657,0,0,905,0,0,820,0,0,1472,6,50159,"WAT","HY" 11,23,1,1,,19,30,"BANGOR HYDRO ELECTRIC CO","MEDWAY",0,,1179,"0A",1294,,,95,2116,0,0,1715,0,0,1459,0,0,1821,0,0,1946,0,0,2134,0,0,2157,0,0,1797,0,0,1745,0,0,1829,0,0,2224,0,0,2386,0,0,1474,6,50159,"WAT","HY" 11,23,1,3,2,19,30,"BANGOR HYDRO ELECTRIC CO","MEDWAY",0,"LIGHT OIL",1179,"0A",1294,,,95,0,0,553,181,307,419,0,0,593,31,55,538,66,120,418,219,399,383,324,598,481,313,579,614,97,178,575,1,2,573,0,0,608,98,171,611,1474,6,50159,"FO2","IC" 11,23,1,1,,19,35,"BANGOR HYDRO ELECTRIC CO","MILFORD",0,,1179,"0A",1294,,,95,3843,0,0,3348,0,0,4177,0,0,3759,0,0,4855,0,0,4740,0,0,2971,0,0,2432,0,0,1786,0,0,1561,0,0,3510,0,0,4606,0,0,1475,6,50159,"WAT","HY" 11,23,1,1,,19,45,"BANGOR HYDRO ELECTRIC CO","ORONO",0,,1179,"0A",1294,,,95,895,0,0,836,0,0,966,0,0,576,0,0,624,0,0,736,0,0,684,0,0,464,0,0,408,0,0,616,0,0,849,0,0,896,0,0,1476,6,50159,"WAT","HY" 11,23,1,1,,19,55,"BANGOR HYDRO ELECTRIC CO","STILLWATER",0,,1179,"0A",1294,,,95,1191,0,0,844,0,0,939,0,0,1021,0,0,1114,0,0,1181,0,0,1170,0,0,878,0,0,818,0,0,880,0,0,923,0,0,950,0,0,1478,6,50159,"WAT","HY" 11,23,1,1,,19,60,"BANGOR HYDRO ELECTRIC CO","VEAZIE A",0,,1179,"0A",1294,,,95,4314,0,0,3855,0,0,5043,0,0,5153,0,0,6053,0,0,5342,0,0,3542,0,0,2651,0,0,2281,0,0,3932,0,0,5128,0,0,3842,0,0,1479,6,50159,"WAT","HY" 11,23,1,1,,19,62,"BANGOR HYDRO ELECTRIC CO","VEAZIE B",0,,1179,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,7199,6,50159,"WAT","HY" 11,23,1,3,2,19,68,"BANGOR HYDRO ELECTRIC CO","BAR HARBOR",0,"LIGHT OIL",1179,"0A",1294,,,95,42,73,538,379,659,574,0,0,574,73,128,446,69,125,512,225,420,440,312,579,556,449,813,455,32,60,586,49,89,497,6,10,487,152,264,571,1466,6,50159,"FO2","IC" 11,23,1,3,2,19,75,"BANGOR HYDRO ELECTRIC CO","EASTPORT",0,"LIGHT OIL",1179,"0A",1294,,,95,39,70,576,80,139,412,0,0,586,10,18,557,32,58,494,111,204,464,172,317,495,182,334,509,19,36,472,0,0,470,15,29,429,67,117,460,1468,6,50159,"FO2","IC" 11,23,1,1,,37,5,"CENTRAL MAINE POWER CO","ANDROSCOG 3",0,,3266,"0M",1294,,,95,2536,0,0,2573,0,0,2732,0,0,2703,0,0,2639,0,0,2235,0,0,2379,0,0,2201,0,0,1657,0,0,2352,0,0,2282,0,0,2805,0,0,1480,6,50491,"WAT","HY" 11,23,1,1,,37,10,"CENTRAL MAINE POWER CO","BAR MILLS",0,,3266,"0M",1294,,,95,2420,0,0,1389,0,0,2414,0,0,2364,0,0,2584,0,0,1195,0,0,623,0,0,586,0,0,293,0,0,1310,0,0,2401,0,0,2056,0,0,1481,6,50491,"WAT","HY" 11,23,1,1,,37,20,"CENTRAL MAINE POWER CO","BONNY EAGLE",0,,3266,"0M",1294,,,95,6041,0,0,3654,0,0,5858,0,0,5255,0,0,4575,0,0,2217,0,0,1233,0,0,1084,0,0,592,0,0,3323,0,0,7098,0,0,4100,0,0,1482,6,50491,"WAT","HY" 11,23,1,1,,37,40,"CENTRAL MAINE POWER CO","CATARACT",0,,3266,"0M",1294,,,95,5330,0,0,4194,0,0,4953,0,0,4656,0,0,4888,0,0,5331,0,0,818,0,0,662,0,0,102,0,0,2232,0,0,5064,0,0,4090,0,0,1486,6,50491,"WAT","HY" 11,23,1,1,,37,42,"CENTRAL MAINE POWER CO","CONTINENTAL",0,,3266,"0M",1294,,,95,-14,0,0,-15,0,0,322,0,0,72,0,0,147,0,0,12,0,0,3,0,0,13,0,0,15,0,0,109,0,0,555,0,0,-18,0,0,1487,6,50491,"WAT","HY" 11,23,1,1,,37,50,"CENTRAL MAINE POWER CO","DEER RIP 1",0,,3266,"0M",1294,,,95,2694,0,0,2434,0,0,4080,0,0,3776,0,0,4034,0,0,2023,0,0,686,0,0,215,0,0,83,0,0,1916,0,0,3984,0,0,3453,0,0,1488,6,50491,"WAT","HY" 11,23,1,1,,37,60,"CENTRAL MAINE POWER CO","FT HALIFAX",0,,3266,"0M",1294,,,95,959,0,0,424,0,0,1026,0,0,961,0,0,925,0,0,526,0,0,51,0,0,5,0,0,155,0,0,380,0,0,977,0,0,659,0,0,1490,6,50491,"WAT","HY" 11,23,1,1,,37,75,"CENTRAL MAINE POWER CO","GULF ISLAND",0,,3266,"0M",1294,,,95,10764,0,0,9131,0,0,13512,0,0,13282,0,0,13485,0,0,8299,0,0,5537,0,0,4070,0,0,2892,0,0,9130,0,0,15549,0,0,11464,0,0,1491,6,50491,"WAT","HY" 11,23,1,1,,37,80,"CENTRAL MAINE POWER CO","HARRIS",0,,3266,"0M",1294,,,95,14325,0,0,24479,0,0,22937,0,0,6538,0,0,5448,0,0,21283,0,0,13285,0,0,11928,0,0,12813,0,0,10770,0,0,19708,0,0,26783,0,0,1492,6,50491,"WAT","HY" 11,23,1,1,,37,85,"CENTRAL MAINE POWER CO","HIRAM",0,,3266,"0M",1294,,,95,5791,0,0,3447,0,0,5873,0,0,6762,0,0,6516,0,0,2778,0,0,1397,0,0,1182,0,0,155,0,0,2992,0,0,7160,0,0,4285,0,0,1493,6,50491,"WAT","HY" 11,23,1,1,,37,90,"CENTRAL MAINE POWER CO","MESALONSK 2",0,,3266,"0M",1294,,,95,1280,0,0,585,0,0,1625,0,0,606,0,0,869,0,0,350,0,0,2,0,0,-1,0,0,9,0,0,710,0,0,1668,0,0,745,0,0,1497,6,50491,"WAT","HY" 11,23,1,1,,37,95,"CENTRAL MAINE POWER CO","MESALONSK 3",0,,3266,"0M",1294,,,95,753,0,0,330,0,0,977,0,0,349,0,0,507,0,0,180,0,0,0,0,0,-6,0,0,0,0,0,414,0,0,1038,0,0,416,0,0,1498,6,50491,"WAT","HY" 11,23,1,1,,37,100,"CENTRAL MAINE POWER CO","MESALONSK 4",0,,3266,"0M",1294,,,95,405,0,0,183,0,0,451,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1499,6,50491,"WAT","HY" 11,23,1,1,,37,105,"CENTRAL MAINE POWER CO","MESALONSK 5",0,,3266,"0M",1294,,,95,699,0,0,292,0,0,0,0,0,378,0,0,0,0,0,203,0,0,13,0,0,9,0,0,4,0,0,408,0,0,923,0,0,390,0,0,1500,6,50491,"WAT","HY" 11,23,1,1,,37,110,"CENTRAL MAINE POWER CO","NO GORHAM",0,,3266,"0M",1294,,,95,1215,0,0,963,0,0,842,0,0,520,0,0,455,0,0,503,0,0,595,0,0,604,0,0,413,0,0,340,0,0,740,0,0,1180,0,0,1501,6,50491,"WAT","HY" 11,23,1,1,,37,125,"CENTRAL MAINE POWER CO","SHAWMUT",0,,3266,"0M",1294,,,95,5226,0,0,5495,0,0,6547,0,0,5776,0,0,5295,0,0,4910,0,0,3475,0,0,2346,0,0,2571,0,0,3529,0,0,4803,0,0,6066,0,0,1504,6,50491,"WAT","HY" 11,23,1,1,,37,130,"CENTRAL MAINE POWER CO","SKELTON",0,,3266,"0M",1294,,,95,13276,0,0,8614,0,0,12134,0,0,11304,0,0,11550,0,0,5199,0,0,2833,0,0,2610,0,0,687,0,0,6731,0,0,13037,0,0,9456,0,0,1505,6,50491,"WAT","HY" 11,23,1,1,,37,145,"CENTRAL MAINE POWER CO","WEST BUXTON",0,,3266,"0M",1294,,,95,4424,0,0,2556,0,0,4381,0,0,3723,0,0,3292,0,0,1602,0,0,798,0,0,745,0,0,418,0,0,1944,0,0,4334,0,0,3045,0,0,1508,6,50491,"WAT","HY" 11,23,1,1,,37,150,"CENTRAL MAINE POWER CO","WESTON",0,,3266,"0M",1294,,,95,8095,0,0,8443,0,0,9513,0,0,8520,0,0,7843,0,0,7850,0,0,5819,0,0,4618,0,0,4257,0,0,5361,0,0,7925,0,0,9347,0,0,1509,6,50491,"WAT","HY" 11,23,1,1,,37,155,"CENTRAL MAINE POWER CO","WILLIAMS",0,,3266,"0M",1294,,,95,9171,0,0,9162,0,0,10255,0,0,6585,0,0,7543,0,0,8658,0,0,6098,0,0,5593,0,0,5308,0,0,5891,0,0,8857,0,0,10646,0,0,1510,6,50491,"WAT","HY" 11,23,1,1,,37,160,"CENTRAL MAINE POWER CO","WYMAN HYDRO",0,,3266,"0M",1294,,,95,30298,0,0,37016,0,0,38382,0,0,18735,0,0,24745,0,0,31774,0,0,20433,0,0,17564,0,0,16353,0,0,19735,0,0,40234,0,0,38504,0,0,1511,6,50491,"WAT","HY" 11,23,1,4,2,37,175,"CENTRAL MAINE POWER CO","CAPE",0,"LIGHT OIL",3266,"0M",1294,,,95,40,282,7937,40,336,7601,-57,44,7557,-40,24,7533,5,162,7371,38,208,7316,611,1872,6581,497,1571,5887,-24,32,5855,-32,27,5828,-45,25,5803,-25,145,5552,1484,6,50491,"FO2","GT" 11,23,1,2,2,37,200,"CENTRAL MAINE POWER CO","WYMAN STEAM",0,"LIGHT OIL",3266,"0M",1294,,,95,707,1587,1149,810,1542,1579,117,264,1534,980,1825,1680,366,883,1468,854,1640,1807,783,1460,2327,653,1307,1677,115,266,1410,20,76,1335,486,1282,2039,604,1177,2212,1507,6,50491,"FO2","ST" 11,23,1,2,3,37,200,"CENTRAL MAINE POWER CO","WYMAN STEAM",0,"HEAVY OIL",3266,"0M",1294,,,95,47051,97029,319010,122493,214459,275338,22777,47240,228098,127804,222606,207728,22560,50003,278752,79660,140051,253816,153893,263859,173676,74046,134076,202289,16596,35140,288543,3258,10955,197963,18538,44437,353526,107031,192190,308382,1507,6,50491,"FO6","ST" 11,23,1,3,2,37,204,"CENTRAL MAINE POWER CO","ISLESBORO",0,"LIGHT OIL",3266,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1494,6,50491,"FO2","IC" 11,23,1,3,2,37,206,"CENTRAL MAINE POWER CO","PEAK IS",0,"LIGHT OIL",3266,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1502,6,50491,"FO2","IC" 11,23,1,1,,37,210,"CENTRAL MAINE POWER CO","BRUNSWICK",0,,3266,"0M",1294,,,95,7964,0,0,6898,0,0,11266,0,0,10237,0,0,10095,0,0,6009,0,0,3698,0,0,2974,0,0,2429,0,0,6541,0,0,12216,0,0,8541,0,0,1483,6,50491,"WAT","HY" 11,23,1,1,,37,215,"CENTRAL MAINE POWER CO","W CHANNEL",0,,3266,"0M",1294,,,95,0,0,0,-33,0,0,-20,0,0,-22,0,0,-1,0,0,-1,0,0,-1,0,0,-21,0,0,-1,0,0,19,0,0,-11,0,0,-22,0,0,695,6,50491,"WAT","HY" 11,23,1,1,,37,220,"CENTRAL MAINE POWER CO","BATES UPPER",0,,3266,"0M",1294,,,95,-41,0,0,-34,0,0,610,0,0,144,0,0,273,0,0,15,0,0,1,0,0,15,0,0,18,0,0,217,0,0,4223,0,0,-30,0,0,7044,6,50491,"WAT","HY" 11,23,1,1,,37,225,"CENTRAL MAINE POWER CO","BATES LOWER",0,,3266,"0M",1294,"S",,95,-17,0,0,-16,0,0,-8,0,0,-2,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,-1,0,0,-3,0,0,-17,0,0,7045,6,50491,"WAT","HY" 11,23,1,1,,37,235,"CENTRAL MAINE POWER CO","ANDRO LOWER",0,,3266,"0M",1294,,,95,23,0,0,-11,0,0,21,0,0,-2,0,0,12,0,0,0,0,0,-1,0,0,0,0,0,0,0,0,5,0,0,38,0,0,-14,0,0,7047,6,50491,"WAT","HY" 11,23,1,1,,37,240,"CENTRAL MAINE POWER CO","HILL MILL",0,,3266,"0M",1294,,,95,-3,0,0,-2,0,0,183,0,0,-6,0,0,60,0,0,2,0,0,1,0,0,0,0,0,1,0,0,105,0,0,467,0,0,-6,0,0,7048,6,50491,"WAT","HY" 11,23,1,1,,37,245,"CENTRAL MAINE POWER CO","C E MONTY",0,,3266,"0M",1294,,,95,11840,0,0,10124,0,0,14280,0,0,13297,0,0,13808,0,0,8324,0,0,5496,0,0,4271,0,0,3199,0,0,9333,0,0,15686,0,0,12247,0,0,805,6,50491,"WAT","HY" 11,23,1,1,,37,250,"CENTRAL MAINE POWER CO","SMELT HILL",0,,3266,"0M",294,"A",,95,0,0,0,400,0,0,352,0,0,239,0,0,180,0,0,162,0,0,191,0,0,178,0,0,-608,0,0,766,0,0,224,0,0,283,0,0,7514,6,50491,"WAT","HY" 11,23,1,2,"B",37,255,"CENTRAL MAINE POWER CO","AROOSTOOK V",0,"WOOD",3266,"0M",294,"A",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,165,0,0,134,0,0,0,0,0,0,0,0,7513,6,50491,"WD","ST" 11,23,1,1,,94,5,"MAINE PUBLIC SERVICE CO","CARIBOU",0,,11522,"0M",1294,,,95,454,0,0,469,0,0,519,0,0,451,0,0,454,0,0,410,0,0,48,0,0,1,0,0,-2,0,0,178,0,0,536,0,0,504,0,0,1513,6,51747,"WAT","HY" 11,23,1,2,3,94,5,"MAINE PUBLIC SERVICE CO","CARIBOU",0,"HEAVY OIL",11522,"0M",1294,,,95,343,903,9375,592,1410,7984,-32,0,8005,-29,0,7995,-26,6,8015,-27,4,8057,-26,0,8067,222,644,7448,-28,0,7396,-29,0,7390,857,1841,5557,2237,4973,2370,1513,6,51747,"FO6","ST" 11,23,1,3,2,94,5,"MAINE PUBLIC SERVICE CO","CARIBOU",0,"LIGHT OIL",11522,"0M",1294,,,95,50,251,1746,5,143,1693,-65,0,1583,78,225,1932,-18,17,1865,-9,6,1829,38,115,1683,233,500,1802,86,210,1776,-6,65,2071,-56,28,1948,244,599,2098,1513,6,51747,"FO2","IC" 11,23,1,1,,94,10,"MAINE PUBLIC SERVICE CO","SQUA PAN",0,,11522,"0M",1294,,,95,115,0,0,363,0,0,152,0,0,-10,0,0,-7,0,0,-3,0,0,-3,0,0,-4,0,0,-6,0,0,-7,0,0,3,0,0,223,0,0,1516,6,51747,"WAT","HY" 11,23,1,3,2,94,23,"MAINE PUBLIC SERVICE CO","FLOS INN",0,"LIGHT OIL",11522,"0M",1294,,,95,27,115,314,19,82,232,-29,0,232,19,79,373,-23,2,371,-16,0,371,13,80,290,124,284,232,74,135,323,-3,51,272,-25,8,264,217,451,388,1514,6,51747,"FO2","IC" 11,23,1,3,2,94,25,"MAINE PUBLIC SERVICE CO","HOULTON",0,"LIGHT OIL",11522,"0M",1294,,,95,6,28,13,-8,1,12,-8,2,10,-8,0,10,-6,0,10,-3,0,10,-2,0,10,-3,0,10,-3,0,10,-4,0,11,-4,2,8,14,34,6,1515,6,51747,"FO2","IC" 11,23,1,2,1,97,1,"MAINE YANKEE ATOMIC PWR C","MAIN YANKEE",0,"NUCLEAR",11525,"0M",1294,,,95,197577,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1517,6,51748,"UR","ST" 11,23,1,3,2,116,10,"PUB SERV CO OF NEW HAMP","SWANS FALLS",0,"LIGHT OIL",15472,"0M",1294,"R",180,95,-7,0,2,-7,0,2,-6,0,2,-3,0,2,-2,0,2,-1,0,2,-1,0,2,-1,0,2,-1,0,2,-1,0,2,-3,0,2,0,0,0,1518,6,52411,"FO2","IC" 11,23,5,1,,525,1,"LEWISTON (CITY OF)","ANDRO UPPER",0,,10963,"0A",1294,,,95,296,0,0,378,0,0,310,0,0,424,0,0,264,0,0,390,0,0,256,0,0,258,0,0,304,0,0,270,0,0,342,0,0,324,0,0,7046,6,54168,"WAT","HY" 11,23,5,1,,566,1,"MADISON (CITY OF)","NORRIDGEWCK",0,,11477,"0A",1294,,,95,306,0,0,241,0,0,261,0,0,291,0,0,379,0,0,277,0,0,75,0,0,0,0,0,26,0,0,121,0,0,197,0,0,224,0,0,6701,6,51737,"WAT","HY" 11,23,8,3,2,835,5,"EASTERN MAINE ELEC COOP","PORTABLE",0,"LIGHT OIL",5609,"0A",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,6366,6,50848,"FO2","IC" 11,23,8,3,2,940,1,"SWANS ISLAND ELEC COOP","MINTURN",0,"LIGHT OIL",18368,"0A",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1550,6,52863,"FO2","IC" 12,33,1,1,,106,5,"NEW ENGLAND POWER CO","COMERFORD",0,,13433,"0M",1294,,90,95,34273,0,0,19125,0,0,43429,0,0,11874,0,0,22700,0,0,13853,0,0,5565,0,0,11061,0,0,5412,0,0,30636,0,0,45527,0,0,18948,0,0,2349,6,52007,"WAT","HY" 12,33,1,1,,106,10,"NEW ENGLAND POWER CO","MCINDOES",0,,13433,"0M",1294,,90,95,4420,0,0,3434,0,0,6350,0,0,3330,0,0,4648,0,0,2664,0,0,1453,0,0,2497,0,0,1353,0,0,4755,0,0,7050,0,0,3740,0,0,6483,6,52007,"WAT","HY" 12,33,1,1,,106,13,"NEW ENGLAND POWER CO","S C MOORE",0,,13433,"0M",1294,,90,95,29434,0,0,15866,0,0,34014,0,0,9521,0,0,19359,0,0,12124,0,0,4787,0,0,9805,0,0,4357,0,0,27013,0,0,40020,0,0,16551,0,0,2351,6,52007,"WAT","HY" 12,33,1,1,,106,15,"NEW ENGLAND POWER CO","VERNON",0,,13433,"0M",1294,,90,95,7120,0,0,5523,0,0,9186,0,0,7993,0,0,7582,0,0,3197,0,0,1355,0,0,2525,0,0,19,0,0,5912,0,0,9702,0,0,7342,0,0,2352,6,52007,"WAT","HY" 12,33,1,1,,106,20,"NEW ENGLAND POWER CO","WILDER",0,,13433,"0M",1294,,90,95,1974,0,0,3326,0,0,18722,0,0,7773,0,0,8911,0,0,4713,0,0,4047,0,0,5176,0,0,2849,0,0,9330,0,0,12667,0,0,7471,0,0,2353,6,52007,"WAT","HY" 12,33,1,2,1,123,1,"PUB SERV CO OF NEW HAMP","SEABROOK",0,"NUCLEAR",15472,"0M",1294,,180,95,857441,0,0,778373,0,0,863021,0,0,832472,0,0,865152,0,0,495425,0,0,690261,0,0,805711,0,0,800410,0,0,828658,0,0,60958,0,0,501494,0,0,6115,6,52411,"UR","ST" 12,33,1,1,,123,4,"PUB SERV CO OF NEW HAMP","AMOSKEAG",0,,15472,"0M",1294,,180,95,10690,0,0,7028,0,0,11425,0,0,749,0,0,15769,0,0,4245,0,0,2251,0,0,3257,0,0,434,0,0,5760,0,0,11044,0,0,6264,0,0,2354,6,52411,"WAT","HY" 12,33,1,1,,123,6,"PUB SERV CO OF NEW HAMP","AYERS IS",0,,15472,"0M",1294,,180,95,3909,0,0,2249,0,0,4743,0,0,3555,0,0,4487,0,0,1520,0,0,1448,0,0,1727,0,0,380,0,0,3303,0,0,5711,0,0,2632,0,0,2355,6,52411,"WAT","HY" 12,33,1,1,,123,16,"PUB SERV CO OF NEW HAMP","EASTMAN FLS",0,,15472,"0M",1294,,180,95,2843,0,0,1293,0,0,2781,0,0,2587,0,0,2725,0,0,1214,0,0,1763,0,0,10079,0,0,-9794,0,0,1729,0,0,3266,0,0,1701,0,0,2356,6,52411,"WAT","HY" 12,33,1,1,,123,20,"PUB SERV CO OF NEW HAMP","GARVIN FLS",0,,15472,"0M",1294,,180,95,5209,0,0,3143,0,0,5693,0,0,4388,0,0,3956,0,0,2019,0,0,755,0,0,1667,0,0,350,0,0,3233,0,0,6336,0,0,3913,0,0,2357,6,52411,"WAT","HY" 12,33,1,1,,123,22,"PUB SERV CO OF NEW HAMP","GORHAM",0,,15472,"0M",1294,,180,95,989,0,0,1031,0,0,1249,0,0,885,0,0,1193,0,0,756,0,0,568,0,0,530,0,0,580,0,0,864,0,0,1116,0,0,1202,0,0,2358,6,52411,"WAT","HY" 12,33,1,1,,123,28,"PUB SERV CO OF NEW HAMP","HOOKSETT",0,,15472,"0M",1294,,180,95,787,0,0,865,0,0,912,0,0,1164,0,0,1141,0,0,791,0,0,156,0,0,317,0,0,43,0,0,751,0,0,952,0,0,776,0,0,2359,6,52411,"WAT","HY" 12,33,1,1,,123,30,"PUB SERV CO OF NEW HAMP","JACKMAN",0,,15472,"0M",1294,,180,95,1997,0,0,535,0,0,1239,0,0,236,0,0,557,0,0,305,0,0,191,0,0,722,0,0,-8,0,0,1339,0,0,2326,0,0,864,0,0,2360,6,52411,"WAT","HY" 12,33,1,1,,123,50,"PUB SERV CO OF NEW HAMP","SMITH STA",0,,15472,"0M",1294,,180,95,8143,0,0,9737,0,0,11648,0,0,6108,0,0,8349,0,0,6172,0,0,4454,0,0,4871,0,0,3742,0,0,6861,0,0,10860,0,0,10308,0,0,2368,6,52411,"WAT","HY" 12,33,1,4,2,123,57,"PUB SERV CO OF NEW HAMP","LOST NATION",0,"LIGHT OIL",15472,"0M",1294,,180,95,-15,0,2159,79,306,1853,-15,0,1853,-12,0,1853,42,125,1728,50,140,1587,209,595,1527,275,828,1235,-11,0,1235,-11,0,1235,-10,0,1235,111,338,1076,2362,6,52411,"FO2","GT" 12,33,1,2,2,123,59,"PUB SERV CO OF NEW HAMP","MERRIMACK",0,"LIGHT OIL",15472,"0M",1294,,180,95,27,45,275,16,29,156,22,38,180,23,38,218,0,0,0,29,52,151,6,14,205,30,55,180,52,96,222,62,108,185,57,96,176,20,35,176,2364,6,52411,"FO2","ST" 12,33,1,2,6,123,59,"PUB SERV CO OF NEW HAMP","MERRIMACK",0,"BIT COAL",15472,"0M",1294,,180,95,266403,101539,253077,274308,103830,266334,256612,98157,263978,216443,80934,278945,76504,17154,315133,246563,95683,297713,281671,111493,247571,263463,95839,235114,181335,71786,264069,207269,81066,275589,253852,96425,269715,287608,108204,247069,2364,6,52411,"BIT","ST" 12,33,1,4,2,123,59,"PUB SERV CO OF NEW HAMP","MERRIMACK",0,"LIGHT OIL",15472,"0M",1294,,180,95,-47,0,3032,411,1048,3032,-21,0,1984,-18,0,1984,112,282,1702,122,334,1367,613,1576,1494,582,1554,2033,-14,0,2033,-11,20,2013,-20,0,2013,242,603,1411,2364,6,52411,"FO2","GT" 12,33,1,2,3,123,63,"PUB SERV CO OF NEW HAMP","SCHILLER",0,"HEAVY OIL",15472,"0M",1294,,180,95,1350,2702,31413,820,1554,92325,2073,4352,187620,1454,2823,184796,1826,3479,189663,2478,4626,184835,4062,7903,176932,2011,4193,53637,1321,2911,170000,1885,4329,165671,5233,10859,154812,3538,6785,118334,2367,6,52411,"FO6","ST" 12,33,1,2,6,123,63,"PUB SERV CO OF NEW HAMP","SCHILLER",0,"BIT COAL",15472,"0M",1294,,180,95,53534,27148,87087,68779,32692,50318,47008,24972,52027,65230,33724,53967,55312,27020,32185,49976,24400,75043,55074,26887,62380,30313,18396,42154,18241,9931,51974,16092,9642,54786,30357,16856,90418,65541,32424,72200,2367,6,52411,"BIT","ST" 12,33,1,4,2,123,63,"PUB SERV CO OF NEW HAMP","SCHILLER",0,"LIGHT OIL",15472,"0M",1294,,180,95,-13,0,804,95,260,723,-12,0,723,-9,0,723,57,118,604,-7,0,604,90,262,723,242,963,714,-7,0,714,0,0,714,-9,0,714,120,301,794,2367,6,52411,"FO2","GT" 12,33,1,4,9,123,63,"PUB SERV CO OF NEW HAMP","SCHILLER",0,"NAT GAS",15472,"0M",1294,,180,95,19,240,0,12,140,0,24,310,0,25,300,0,22,264,0,17,210,0,219,2700,0,121,2803,0,14,190,0,15,220,0,24,320,0,22,260,0,2367,6,52411,"NG","GT" 12,33,1,4,2,123,70,"PUB SERV CO OF NEW HAMP","WHITE LAKE",0,"LIGHT OIL",15472,"0M",1294,,180,95,-17,0,2383,97,350,2033,-14,4,2029,-7,0,2029,48,94,1935,136,341,1595,147,405,1763,357,924,1410,-3,0,1410,-3,0,1410,-13,0,1410,-6,129,1281,2369,6,52411,"FO2","GT" 12,33,1,2,2,123,72,"PUB SERV CO OF NEW HAMP","NEWINGTON",0,"LIGHT OIL",15472,"0M",1294,,180,95,2141,4247,1577,1729,3274,1766,1111,2327,1824,1584,4149,1209,1580,3072,1209,1589,3168,1640,1162,2239,1856,1703,3313,1598,1134,2258,1388,173,817,1751,1894,3703,1630,507,3096,1651,8002,6,52411,"FO2","ST" 12,33,1,2,3,123,72,"PUB SERV CO OF NEW HAMP","NEWINGTON",0,"HEAVY OIL",15472,"0M",1294,,180,95,73391,138116,328850,119485,206586,321529,32827,62816,434361,89003,159420,245596,100291,177704,321055,73382,134661,317462,125529,216497,100965,57182,118647,2305699,45699,82009,405756,1560,6611,399144,100544,177099,222046,136392,231245,388270,8002,6,52411,"FO6","ST" 12,33,1,2,9,123,72,"PUB SERV CO OF NEW HAMP","NEWINGTON",0,"NAT GAS",15472,"0M",1294,,180,95,1463,17053,0,0,0,0,0,0,0,0,0,0,35353,394385,0,45744,527451,0,57696,624462,0,48968,544320,0,10747,122302,0,57,1545,0,742,8312,0,0,0,0,8002,6,52411,"NG","ST" 13,50,1,1,,22,2,"CENTRAL VT PUB SERV CORP","ARNOLD FLS",0,,3292,"0A",1294,,350,95,112,0,0,27,0,0,168,0,0,290,0,0,100,0,0,18,0,0,33,0,0,37,0,0,17,0,0,172,0,0,245,0,0,135,0,0,3707,6,50503,"WAT","HY" 13,50,1,1,,22,10,"CENTRAL VT PUB SERV CORP","CAVENDISH",0,,3292,"0A",1294,,350,95,534,0,0,309,0,0,847,0,0,607,0,0,267,0,0,83,0,0,0,0,0,134,0,0,-3,0,0,391,0,0,928,0,0,383,0,0,3710,6,50503,"WAT","HY" 13,50,1,1,,22,11,"CENTRAL VT PUB SERV CORP","CLARKS FLS",0,,3292,"0A",1294,,350,95,1404,0,0,1026,0,0,1689,0,0,1865,0,0,1729,0,0,855,0,0,596,0,0,1076,0,0,567,0,0,1648,0,0,1970,0,0,1412,0,0,3711,6,50503,"WAT","HY" 13,50,1,1,,22,15,"CENTRAL VT PUB SERV CORP","FAIRFAX",0,,3292,"0A",1294,,350,95,1873,0,0,1589,0,0,2321,0,0,2516,0,0,2499,0,0,1241,0,0,878,0,0,1432,0,0,744,0,0,2114,0,0,2573,0,0,2233,0,0,3712,6,50503,"WAT","HY" 13,50,1,1,,22,16,"CENTRAL VT PUB SERV CORP","GAGE",0,,3292,"0A",1294,,350,95,221,0,0,24,0,0,244,0,0,307,0,0,290,0,0,73,0,0,85,0,0,38,0,0,48,0,0,305,0,0,523,0,0,226,0,0,3713,6,50503,"WAT","HY" 13,50,1,1,,22,18,"CENTRAL VT PUB SERV CORP","GLEN",0,,3292,"0A",1294,,350,95,1041,0,0,605,0,0,731,0,0,367,0,0,238,0,0,98,0,0,83,0,0,323,0,0,183,0,0,629,0,0,1307,0,0,401,0,0,3714,6,50503,"WAT","HY" 13,50,1,1,,22,22,"CENTRAL VT PUB SERV CORP","LW MIDLEBRY",0,,3292,"0A",1294,,350,95,725,0,0,534,0,0,1054,0,0,920,0,0,550,0,0,286,0,0,79,0,0,150,0,0,104,0,0,524,0,0,1220,0,0,492,0,0,3716,6,50503,"WAT","HY" 13,50,1,1,,22,26,"CENTRAL VT PUB SERV CORP","MILTON",0,,3292,"0A",1294,,350,95,3538,0,0,2446,0,0,4215,0,0,4336,0,0,3864,0,0,1806,0,0,1204,0,0,2514,0,0,1210,0,0,4046,0,0,4879,0,0,3192,0,0,3717,6,50503,"WAT","HY" 13,50,1,1,,22,28,"CENTRAL VT PUB SERV CORP","PASSUMPSIC",0,,3292,"0A",1294,,350,95,315,0,0,97,0,0,378,0,0,435,0,0,415,0,0,90,0,0,51,0,0,150,0,0,94,0,0,370,0,0,434,0,0,44,0,0,3718,6,50503,"WAT","HY" 13,50,1,1,,22,30,"CENTRAL VT PUB SERV CORP","PATCH",0,,3292,"0A",1294,,350,95,107,0,0,58,0,0,59,0,0,21,0,0,7,0,0,5,0,0,5,0,0,28,0,0,7,0,0,42,0,0,158,0,0,30,0,0,3719,6,50503,"WAT","HY" 13,50,1,1,,22,34,"CENTRAL VT PUB SERV CORP","PIERCE MLS",0,,3292,"0A",1294,,350,95,113,0,0,81,0,0,121,0,0,180,0,0,161,0,0,59,0,0,47,0,0,47,0,0,17,0,0,102,0,0,181,0,0,116,0,0,3721,6,50503,"WAT","HY" 13,50,1,1,,22,36,"CENTRAL VT PUB SERV CORP","PITTSFORD",0,,3292,"0A",1294,,350,95,1275,0,0,941,0,0,158,0,0,47,0,0,-2,0,0,9,0,0,0,0,0,489,0,0,354,0,0,726,0,0,1999,0,0,679,0,0,3722,6,50503,"WAT","HY" 13,50,1,1,,22,38,"CENTRAL VT PUB SERV CORP","SALISBURY",0,,3292,"0A",1294,,350,95,325,0,0,210,0,0,191,0,0,62,0,0,141,0,0,65,0,0,25,0,0,72,0,0,111,0,0,88,0,0,-6,0,0,303,0,0,3724,6,50503,"WAT","HY" 13,50,1,1,,22,40,"CENTRAL VT PUB SERV CORP","SILVER LAKE",0,,3292,"0A",1294,,350,95,800,0,0,508,0,0,722,0,0,405,0,0,402,0,0,227,0,0,103,0,0,275,0,0,84,0,0,500,0,0,973,0,0,535,0,0,3725,6,50503,"WAT","HY" 13,50,1,1,,22,41,"CENTRAL VT PUB SERV CORP","TAFTSVILLE",0,,3292,"0A",1294,,350,95,150,0,0,135,0,0,208,0,0,200,0,0,119,0,0,12,0,0,0,0,0,17,0,0,-1,0,0,55,0,0,175,0,0,162,0,0,3727,6,50503,"WAT","HY" 13,50,1,1,,22,44,"CENTRAL VT PUB SERV CORP","WEYBRIDGE",0,,3292,"0A",1294,,350,95,1391,0,0,616,0,0,1819,0,0,1459,0,0,991,0,0,370,0,0,156,0,0,354,0,0,167,0,0,1042,0,0,2031,0,0,856,0,0,3728,6,50503,"WAT","HY" 13,50,1,1,,22,45,"CENTRAL VT PUB SERV CORP","PETERSON",0,,3292,"0A",1294,,350,95,2522,0,0,1281,0,0,3601,0,0,3092,0,0,2335,0,0,1090,0,0,702,0,0,1605,0,0,681,0,0,2814,0,0,4021,0,0,1742,0,0,3720,6,50503,"WAT","HY" 13,50,1,4,2,22,48,"CENTRAL VT PUB SERV CORP","RUTLAND",0,"LIGHT OIL",3292,"0A",1294,,350,95,13,125,4525,45,327,4198,40,218,3979,19,143,3836,20,127,3709,101,381,3328,272,898,2430,277,932,1498,34,167,3475,-8,46,3429,32,195,3234,152,651,2583,3723,6,50503,"FO2","GT" 13,50,1,4,2,22,49,"CENTRAL VT PUB SERV CORP","ASCUTNEY",0,"LIGHT OIL",3292,"0A",1294,,350,95,27,136,2572,77,326,2246,69,300,1946,18,96,1851,8,65,1786,41,144,1641,268,895,2175,226,765,1409,-1,38,3277,-15,0,3277,-3,71,3206,88,353,2853,3708,6,50503,"FO2","GT" 13,50,1,3,2,22,60,"CENTRAL VT PUB SERV CORP","ST ALBANS",0,"LIGHT OIL",3292,"0A",1294,,350,95,-14,0,89,5,38,214,-11,4,210,-10,5,205,7,17,188,21,40,148,72,149,234,59,123,111,-1,2,110,-3,0,110,-6,0,108,9,42,236,3726,6,50503,"FO2","IC" 13,50,1,1,,22,65,"CENTRAL VT PUB SERV CORP","SMITH",0,,3292,"0A",1294,,350,95,361,0,0,154,0,0,495,0,0,658,0,0,519,0,0,163,0,0,121,0,0,123,0,0,72,0,0,258,0,0,692,0,0,170,0,0,3709,6,50503,"WAT","HY" 13,50,1,1,,22,70,"CENTRAL VT PUB SERV CORP","EAST BARNET",0,,3292,"0A",1294,,350,95,595,0,0,399,0,0,900,0,0,1046,0,0,922,0,0,325,0,0,322,0,0,358,0,0,203,0,0,790,0,0,1148,0,0,702,0,0,788,6,50503,"WAT","HY" 13,50,1,1,,24,5,"CITIZENS UTILITIES CO","CHARLESTON",0,,3611,"0A",1294,,,95,339,0,0,244,0,0,393,0,0,445,0,0,409,0,0,252,0,0,154,0,0,192,0,0,90,0,0,382,0,0,461,0,0,314,0,0,3729,6,50560,"WAT","HY" 13,50,1,1,,24,10,"CITIZENS UTILITIES CO","NEWPORT",0,,3611,"0A",1294,,,95,1625,0,0,946,0,0,1961,0,0,1655,0,0,1645,0,0,917,0,0,474,0,0,1107,0,0,331,0,0,1614,0,0,2652,0,0,1235,0,0,3731,6,50560,"WAT","HY" 13,50,1,3,2,24,15,"CITIZENS UTILITIES CO","NEWPORT DSL",0,"LIGHT OIL",3611,"0A",1294,,,95,0,0,377,16,33,290,0,0,259,0,0,229,0,0,206,0,0,206,0,0,206,7,12,194,8,16,177,0,0,177,0,0,137,0,0,85,3730,6,50560,"FO2","IC" 13,50,1,1,,24,20,"CITIZENS UTILITIES CO","TROY",0,,3611,"0A",1294,,,95,150,0,0,72,0,0,150,0,0,267,0,0,209,0,0,71,0,0,28,0,0,30,0,0,3,0,0,74,0,0,244,0,0,128,0,0,3733,6,50560,"WAT","HY" 13,50,1,1,,47,10,"GREEN MOUNTAIN POWER CORP","ESSEX 19",0,,7601,"0M",1294,,,95,2888,0,0,2870,0,0,4338,0,0,3931,0,0,3261,0,0,980,0,0,333,0,0,1531,0,0,936,0,0,2161,0,0,3540,0,0,2964,0,0,3737,6,51169,"WAT","HY" 13,50,1,3,2,47,10,"GREEN MOUNTAIN POWER CORP","ESSEX 19",0,"LIGHT OIL",7601,"0M",1294,,,95,0,0,311,11,27,284,1,1,283,0,0,283,7,16,267,28,61,385,45,85,300,33,65,235,9,19,394,0,0,394,0,0,394,12,25,369,3737,6,51169,"FO2","IC" 13,50,1,1,,47,15,"GREEN MOUNTAIN POWER CORP","GORGE NO 18",0,,7601,"0M",1294,,,95,901,0,0,986,0,0,1573,0,0,1661,0,0,1125,0,0,122,0,0,113,0,0,692,0,0,0,0,0,0,0,0,0,0,0,0,0,0,6475,6,51169,"WAT","HY" 13,50,1,1,,47,20,"GREEN MOUNTAIN POWER CORP","MARSHFIELD6",0,,7601,"0M",1294,,,95,891,0,0,1188,0,0,245,0,0,107,0,0,0,0,0,3,0,0,2,0,0,54,0,0,53,0,0,604,0,0,1300,0,0,430,0,0,3739,6,51169,"WAT","HY" 13,50,1,1,,47,25,"GREEN MOUNTAIN POWER CORP","MIDDLESEX 2",0,,7601,"0M",1294,,,95,1134,0,0,848,0,0,1580,0,0,1697,0,0,1156,0,0,150,0,0,111,0,0,717,0,0,45,0,0,1158,0,0,2061,0,0,1133,0,0,3740,6,51169,"WAT","HY" 13,50,1,1,,47,40,"GREEN MOUNTAIN POWER CORP","VERGENNES 9",0,,7601,"0M",1294,,,95,972,0,0,799,0,0,1171,0,0,1224,0,0,968,0,0,441,0,0,247,0,0,499,0,0,318,0,0,590,0,0,1307,0,0,899,0,0,6519,6,51169,"WAT","HY" 13,50,1,3,2,47,40,"GREEN MOUNTAIN POWER CORP","VERGENNES 9",0,"LIGHT OIL",7601,"0M",1294,,,95,15,27,282,68,118,164,15,24,319,5,8,311,4,25,465,108,264,200,174,319,417,163,302,294,20,35,437,3,2,436,2,4,432,35,62,370,6519,6,51169,"FO2","IC" 13,50,1,1,,47,53,"GREEN MOUNTAIN POWER CORP","WATRBRY 22",0,,7601,"0M",1294,,,95,2101,0,0,2029,0,0,1441,0,0,318,0,0,823,0,0,444,0,0,464,0,0,1190,0,0,485,0,0,2251,0,0,2609,0,0,1566,0,0,6520,6,51169,"WAT","HY" 13,50,1,1,,47,55,"GREEN MOUNTAIN POWER CORP","W DANVIL 15",0,,7601,"0M",1294,,,95,445,0,0,146,0,0,507,0,0,509,0,0,301,0,0,77,0,0,87,0,0,220,0,0,103,0,0,544,0,0,661,0,0,151,0,0,3743,6,51169,"WAT","HY" 13,50,1,4,2,47,58,"GREEN MOUNTAIN POWER CORP","BERLIN NO 5",0,"LIGHT OIL",7601,"0M",1294,,,95,32,270,10962,606,1501,9460,21,72,9388,0,0,9338,254,677,8711,731,1834,7632,1214,3039,11011,1354,3377,12369,189,463,14376,681,1521,12855,79,209,12646,389,879,11767,3734,6,51169,"FO2","GT" 13,50,1,4,2,47,60,"GREEN MOUNTAIN POWER CORP","COLCHSTR 16",0,"LIGHT OIL",7601,"0M",1294,,,95,7,28,1071,86,296,775,5,25,750,0,0,750,9,33,717,6,26,1583,117,472,1112,76,320,791,0,0,1506,0,0,1506,0,0,1507,0,0,1506,3735,6,51169,"FO2","GT" 13,50,1,1,,47,65,"GREEN MOUNTAIN POWER CORP","BOLTON FALL",0,,7601,"0M",1294,,,95,3020,0,0,2253,0,0,3823,0,0,2884,0,0,2258,0,0,636,0,0,502,0,0,1603,0,0,428,0,0,2596,0,0,4478,0,0,2430,0,0,7056,6,51169,"WAT","HY" 13,50,1,7,"D",47,70,"GREEN MOUNTAIN POWER CORP","CARTHUSIANS",0,"N/A",7601,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,7260,6,51169,"WI","WI" 13,50,1,1,,73,5,"NEW ENGLAND POWER CO","BELLOWS FLS",0,,13433,"0M",1294,,90,95,22299,0,0,16448,0,0,28735,0,0,22260,0,0,21635,0,0,10244,0,0,6175,0,0,10541,0,0,3991,0,0,19464,0,0,30239,0,0,18843,0,0,3745,6,52007,"WAT","HY" 13,50,1,1,,73,10,"NEW ENGLAND POWER CO","HARRIMAN",0,,13433,"0M",1294,,90,95,14391,0,0,13610,0,0,13092,0,0,2630,0,0,807,0,0,1394,0,0,2040,0,0,2968,0,0,2416,0,0,10136,0,0,16468,0,0,11713,0,0,3746,6,52007,"WAT","HY" 13,50,1,1,,73,15,"NEW ENGLAND POWER CO","SEARSBURG",0,,13433,"0M",1294,,90,95,3120,0,0,2878,0,0,3094,0,0,1942,0,0,1012,0,0,853,0,0,152,0,0,1319,0,0,954,0,0,2077,0,0,3042,0,0,2675,0,0,6529,6,52007,"WAT","HY" 13,50,1,1,,73,18,"NEW ENGLAND POWER CO","VERNON",0,,13433,"0M",1294,,90,95,4592,0,0,4182,0,0,5197,0,0,4922,0,0,4427,0,0,2397,0,0,1604,0,0,3525,0,0,1667,0,0,3876,0,0,4946,0,0,3693,0,0,8904,6,52007,"WAT","HY" 13,50,1,1,,73,20,"NEW ENGLAND POWER CO","WILDER",0,,13433,"0M",1294,,90,95,9053,0,0,5888,0,0,8525,0,0,1765,0,0,2559,0,0,1204,0,0,21,0,0,1756,0,0,407,0,0,4556,0,0,8802,0,0,2669,0,0,8905,6,52007,"WAT","HY" 13,50,1,1,,98,5,"PUB SERV CO OF NEW HAMP","CANAAN",0,,15472,"0M",1294,,180,95,729,0,0,718,0,0,805,0,0,483,0,0,569,0,0,345,0,0,252,0,0,190,0,0,195,0,0,728,0,0,765,0,0,738,0,0,3750,6,52411,"WAT","HY" 13,50,1,2,1,135,1,"VT YANKEE NUCLEAR PR CORP","VT YANKEE",0,"NUCLEAR",19796,"0M",1294,,,95,384928,0,0,346136,0,0,192519,0,0,0,0,0,335965,0,0,365673,0,0,371198,0,0,375476,0,0,363210,0,0,389313,0,0,379730,0,0,354361,0,0,3751,6,53128,"UR","ST" 13,50,1,1,,304,1,"VERMONT MARBLE CO","PROCTOR",0,,19794,"0A",1294,,,95,3213,0,0,2009,0,0,3559,0,0,3058,0,0,2032,0,0,1143,0,0,395,0,0,893,0,0,294,0,0,1839,0,0,3796,0,0,1853,0,0,6450,6,53127,"WAT","HY" 13,50,1,1,,304,5,"VERMONT MARBLE CO","CTR RUTLAND",0,,19794,"0A",1294,,,95,161,0,0,164,0,0,188,0,0,211,0,0,211,0,0,121,0,0,26,0,0,62,0,0,19,0,0,85,0,0,190,0,0,184,0,0,6453,6,53127,"WAT","HY" 13,50,1,1,,304,10,"VERMONT MARBLE CO","BELDENS",0,,19794,"0A",1294,,,95,2174,0,0,1009,0,0,2729,0,0,1624,0,0,972,0,0,405,0,0,95,0,0,369,0,0,149,0,0,1679,0,0,2997,0,0,1013,0,0,6451,6,53127,"WAT","HY" 13,50,1,4,2,304,15,"VERMONT MARBLE CO","FLORENCE",0,"LIGHT OIL",19794,"0A",1294,,,95,-2,95,12708,118,200,12076,184,475,11934,674,1762,7457,74,191,4607,157,358,9260,354,1040,6925,210,559,6363,167,435,4707,-11,3,10761,-13,60,8428,167,550,7887,7337,6,53127,"FO2","GT" 13,50,5,1,,520,1,"BARTON (VILLAGE OF)","W CHARLESTN",0,,1299,"0A",1294,,,95,477,0,0,231,0,0,556,0,0,533,0,0,570,0,0,256,0,0,132,0,0,351,0,0,83,0,0,382,0,0,680,0,0,196,0,0,3753,6,50178,"WAT","HY" 13,50,5,3,2,520,1,"BARTON (VILLAGE OF)","W CHARLESTN",0,"LIGHT OIL",1299,"0A",1294,,,95,0,0,206,14,34,172,0,0,172,0,0,172,1,3,169,19,51,118,39,103,190,42,112,78,7,19,59,0,0,59,0,0,118,10,86,32,3753,6,50178,"FO2","IC" 13,50,5,4,2,536,1,"BURLINGTON (CITY OF)","GAS TURB",0,"LIGHT OIL",2548,"0M",1294,,,95,0,1,1628,248,707,868,0,4,2022,0,0,2015,19,66,1949,459,1365,1742,608,1830,1698,485,1472,1476,56,189,1287,0,0,1285,84,242,1001,165,472,1772,3754,6,50375,"FO2","GT" 13,50,5,2,"B",536,10,"BURLINGTON (CITY OF)","J C MC NEIL",0,"WOD CHIPS",2548,"0M",1294,,,95,7742,0,0,12138,0,0,4790,0,0,12108,0,0,15618,0,0,11949,0,0,14425,0,0,8887,0,0,5359,0,0,3746,0,0,10817,0,0,19589,0,0,589,6,50375,"WOD","ST" 13,50,5,2,2,536,10,"BURLINGTON (CITY OF)","J C MC NEIL",0,"LIGHT OIL",2548,"0M",1294,,,95,136,326,2416,132,350,1989,41,99,1826,0,216,1559,0,39,1448,0,22,1351,4,23,1264,0,81,1183,0,52,1021,0,40,945,19,99,3170,24,98,2994,589,6,50375,"FO2","ST" 13,50,5,2,9,536,10,"BURLINGTON (CITY OF)","J C MC NEIL",0,"NAT GAS",2548,"0M",1294,,,95,1750,24386,0,816,12632,0,1337,18689,0,0,2252,0,0,3244,0,0,3721,0,177,4800,0,0,2471,0,0,2396,0,0,2708,0,449,13380,0,2064,47618,0,589,6,50375,"NG","ST" 13,50,5,1,,551,5,"ENOSBURG FALLS (VILLAGE)","KENDALL",0,,5915,"0A",1294,,,95,52,0,0,126,0,0,145,0,0,160,0,0,164,0,0,130,0,0,102,0,0,121,0,0,68,0,0,109,0,0,147,0,0,64,0,0,3757,6,50910,"WAT","HY" 13,50,5,3,2,551,10,"ENOSBURG FALLS (VILLAGE)","DIESEL PLT",0,"LIGHT OIL",5915,"0A",1294,,,95,1,5,320,14,24,296,0,1,296,1,3,293,4,13,280,16,34,246,20,37,351,23,44,307,2,6,301,0,0,301,0,0,0,12,21,279,4247,6,50910,"FO2","IC" 13,50,5,1,,551,15,"ENOSBURG FALLS (VILLAGE)","VILLAGE PLT",0,,5915,"0A",1294,,,95,370,0,0,204,0,0,298,0,0,433,0,0,408,0,0,218,0,0,87,0,0,140,0,0,45,0,0,324,0,0,364,0,0,395,0,0,4246,6,50910,"WAT","HY" 13,50,5,1,,567,1,"HARDWICK (VILLAGE OF)","WOLCOTT",0,,8104,"0A",1294,,,95,228,0,0,139,0,0,381,0,0,480,0,0,332,0,0,55,0,0,41,0,0,20,0,0,22,0,0,331,0,0,526,0,0,262,0,0,6477,6,51238,"WAT","HY" 13,50,5,3,2,567,5,"HARDWICK (VILLAGE OF)","HARDWICK",0,"LIGHT OIL",8104,"0A",1294,,,95,0,0,451,0,0,451,0,0,451,0,0,451,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,6476,6,51238,"FO2","IC" 13,50,5,1,,644,5,"LYNDONVILLE (CITY OF)","GREAT FALLS",0,,11359,"0A",1294,,,95,160,0,0,115,0,0,308,0,0,489,0,0,746,0,0,350,0,0,273,0,0,122,0,0,171,0,0,457,0,0,558,0,0,437,0,0,3762,6,51721,"WAT","HY" 13,50,5,1,,644,10,"LYNDONVILLE (CITY OF)","VAIL",0,,11359,"0A",1294,,,95,100,0,0,71,0,0,99,0,0,123,0,0,225,0,0,93,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,107,0,0,3763,6,51721,"WAT","HY" 13,50,5,1,,659,5,"MORRISVILLE (VILLAGE OF)","CADYS FALLS",0,,12989,"0A",1294,,,95,396,0,0,268,0,0,387,0,0,226,0,0,403,0,0,133,0,0,101,0,0,2,0,0,71,0,0,356,0,0,337,0,0,160,0,0,3765,6,51943,"WAT","HY" 13,50,5,1,,659,10,"MORRISVILLE (VILLAGE OF)","MORRISVILLE",0,,12989,"0A",1294,,,95,250,0,0,312,0,0,619,0,0,801,0,0,581,0,0,131,0,0,-1,0,0,-1,0,0,-1,0,0,-1,0,0,-2,0,0,227,0,0,3764,6,51943,"WAT","HY" 13,50,5,1,,659,15,"MORRISVILLE (VILLAGE OF)","W K SANDERS",0,,12989,"0A",1294,,,95,-5,0,0,114,0,0,24,0,0,13,0,0,33,0,0,10,0,0,-1,0,0,38,0,0,-2,0,0,83,0,0,177,0,0,7,0,0,678,6,51943,"WAT","HY" 13,50,5,1,,737,5,"SWANTON (VILLAGE OF)","HIGHGATE FL",0,,18371,"0A",1294,,,95,3846,0,0,2084,0,0,5329,0,0,5012,0,0,4484,0,0,2556,0,0,711,0,0,1431,0,0,444,0,0,4486,0,0,6056,0,0,2920,0,0,6618,6,52864,"WAT","HY" 13,50,8,1,,800,5,"VERMONT ELECTRIC COOP","N HARTLAND",0,,19791,"0A",1294,,,95,1260,0,0,415,0,0,212,0,0,990,0,0,623,0,0,190,0,0,90,0,0,4,0,0,8,0,0,484,0,0,1466,0,0,734,0,0,590,6,53125,"WAT","HY" 13,50,8,1,,810,5,"WASHINGTON ELECTRIC COOP","WRIGHTSVILE",0,,20151,"0A",1294,,,95,270,0,0,88,0,0,334,0,0,327,0,0,246,0,0,50,0,0,54,0,0,128,0,0,47,0,0,3224,0,0,418,0,0,153,0,0,7051,6,58100,"WAT","HY" 14,25,1,2,1,23,1,"BOSTON EDISON CO","PILGRIM",0,"NUCLEAR",1998,"0M",1294,,,95,494219,0,0,433548,0,0,370903,0,0,0,0,0,0,0,0,313826,0,0,476983,0,0,486906,0,0,466384,0,0,470820,0,0,479805,0,0,492451,0,0,1590,6,50300,"UR","ST" 14,25,1,4,2,23,15,"BOSTON EDISON CO","EDGAR",0,"LIGHT OIL",1998,"0M",1294,,,95,43,139,1048,160,393,893,25,79,1053,64,124,929,28,74,855,110,379,953,323,950,955,245,760,910,38,108,1040,37,107,933,56,139,1032,134,337,934,1585,6,50300,"FO2","GT" 14,25,1,4,2,23,17,"BOSTON EDISON CO","FRAMINGHAM",0,"LIGHT OIL",1998,"0M",1294,,,95,141,378,1770,276,681,1804,67,203,1601,44,165,1674,70,215,1698,449,1329,1559,788,2383,1819,766,2306,1658,95,258,1630,53,142,1734,74,277,1695,278,761,1649,1586,6,50300,"FO2","GT" 14,25,1,4,2,23,20,"BOSTON EDISON CO","L STREET",0,"LIGHT OIL",1998,"0M",1294,,,95,18,71,606,223,524,481,31,74,586,101,254,571,64,181,628,302,790,611,232,657,597,450,1241,537,70,195,581,33,121,579,41,95,603,202,478,601,1587,6,50300,"FO2","GT" 14,25,1,2,2,23,25,"BOSTON EDISON CO","MYSTIC",0,"LIGHT OIL",1998,"0M",1294,,,95,251,519,1723,2082,3518,560,0,0,2480,874,1565,1748,1508,2858,1987,1285,2470,2852,2284,4277,1789,1325,2537,1992,119,230,1762,111,219,2019,220,439,1580,238,420,1327,1588,6,50300,"FO2","ST" 14,25,1,2,3,23,25,"BOSTON EDISON CO","MYSTIC",0,"HEAVY OIL",1998,"0M",1294,,,95,112692,212897,634701,250006,389639,396000,28170,35809,578539,46219,75659,622498,47350,81843,540595,74633,131731,529651,114158,195470,453259,65504,114254,339850,9543,16899,623019,18574,33314,589243,137777,234264,549412,333744,539006,466193,1588,6,50300,"FO6","ST" 14,25,1,2,9,23,25,"BOSTON EDISON CO","MYSTIC",0,"NAT GAS",1998,"0M",1294,,,95,54301,611365,0,41760,387451,0,199825,2260608,0,223483,2242300,0,121095,1295784,0,76698,835115,0,229079,2424349,0,221936,2420968,0,166749,1844575,0,138588,1545200,0,1185,12271,0,4690,47014,0,1588,6,50300,"NG","ST" 14,25,1,4,2,23,25,"BOSTON EDISON CO","MYSTIC",0,"LIGHT OIL",1998,"0M",1294,,,95,27,56,491,103,175,435,20,57,497,61,110,506,37,71,435,192,369,532,279,524,365,264,506,455,27,53,523,26,52,471,36,92,498,52,92,444,1588,6,50300,"FO2","GT" 14,25,1,2,2,23,30,"BOSTON EDISON CO","NEW BOSTON",0,"LIGHT OIL",1998,"0M",1294,,,95,0,0,60,0,0,60,0,0,60,0,0,60,0,0,60,0,0,60,0,0,60,0,0,60,0,0,60,0,0,60,0,0,60,0,0,60,1589,6,50300,"FO2","ST" 14,25,1,2,3,23,30,"BOSTON EDISON CO","NEW BOSTON",0,"HEAVY OIL",1998,"0M",1294,,,95,215120,320592,70394,155709,225131,71506,167349,258313,38374,0,0,38374,0,0,38374,0,0,38374,0,0,38403,0,0,38403,0,0,38403,0,0,38808,0,0,73197,633,1026,94600,1589,6,50300,"FO6","ST" 14,25,1,2,9,23,30,"BOSTON EDISON CO","NEW BOSTON",0,"NAT GAS",1998,"0M",1294,,,95,0,0,0,151,1334,0,2301,23751,0,201560,2042478,0,231080,2303282,0,366745,3613841,0,376840,3697457,0,381210,3746576,0,337660,3311625,0,328300,3254233,0,343010,3322669,0,159417,1573389,0,1589,6,50300,"NG","ST" 14,25,1,4,2,23,40,"BOSTON EDISON CO","WEST MEDWAY",0,"LIGHT OIL",1998,"0M",1294,,,95,532,1305,6724,2615,5858,6588,305,882,6659,441,1064,6548,648,1783,6907,1922,5806,5619,2304,7193,6789,2376,1139,6841,43,153,6688,33,101,6587,199,636,6665,2492,6199,6929,1592,6,50300,"FO2","GT" 14,25,1,4,9,23,40,"BOSTON EDISON CO","WEST MEDWAY",0,"NAT GAS",1998,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,963,16262,0,363,42170,0,305,906,0,134,2149,0,0,0,0,0,0,0,1592,6,50300,"NG","GT" 14,25,1,2,3,25,5,"COMMONWEALTH ENERGY SYS","BLACKSTONE",0,"HEAVY OIL",4120,"0M",1294,,80,95,12,9,1622,622,891,254,0,0,0,12,11,3277,4,9,3067,8,31,3303,19,66,3122,71,286,2313,8,25,2707,0,0,2900,388,267,2375,216,151,3016,1594,6,50412,"FO6","ST" 14,25,1,2,9,25,5,"COMMONWEALTH ENERGY SYS","BLACKSTONE",0,"NAT GAS",4120,"0M",1294,,80,95,643,3052,0,809,7234,0,0,0,0,329,1924,0,176,2782,0,306,7064,0,840,18553,0,641,16359,0,98,2009,0,0,0,0,26,113,0,3,12,0,1594,6,50412,"NG","ST" 14,25,1,2,3,25,10,"COMMONWEALTH ENERGY SYS","KENDALL SQ",0,"HEAVY OIL",4120,"0M",1294,,80,95,1966,3331,44639,4440,7426,46357,571,1025,43350,551,1184,40895,279,518,39729,76,146,39422,226,384,45928,178,367,45253,473,969,43288,91,206,42859,6937,10643,43043,10035,14044,33074,1595,6,50412,"FO6","ST" 14,25,1,2,9,25,10,"COMMONWEALTH ENERGY SYS","KENDALL SQ",0,"NAT GAS",4120,"0M",1294,,80,95,8305,87563,0,5498,57215,0,7487,85115,0,6963,94695,0,6096,81153,0,7445,90078,0,8638,93009,0,7941,103714,0,6154,79756,0,5898,84299,0,580,5629,0,447,3954,0,1595,6,50412,"NG","ST" 14,25,1,4,2,25,10,"COMMONWEALTH ENERGY SYS","KENDALL SQ",0,"LIGHT OIL",4120,"0M",1294,,80,95,0,0,1889,173,442,1930,0,0,1930,10,26,1904,381,951,1671,340,886,1969,587,1240,1863,822,2088,2078,160,754,1323,0,0,1561,0,0,1561,183,453,1925,1595,6,50412,"FO2","GT" 14,25,1,2,3,25,15,"COMMONWEALTH ENERGY SYS","CANAL",0,"HEAVY OIL",4120,"0M",1294,,80,95,162391,279085,64428,147412,254620,37606,178077,310890,35916,210807,342420,34150,172965,296386,68134,149960,274442,64297,204907,357210,66759,386648,623547,65078,202416,316252,66152,59087,109907,66707,307766,492512,64272,421791,645524,63446,1599,6,50412,"FO6","ST" 14,25,1,3,2,25,25,"COMMONWEALTH ENERGY SYS","OAK BLUFFS",0,"LIGHT OIL",4120,"0M",1294,,80,95,0,0,1131,70,125,1006,0,0,1006,3,6,1000,58,98,1011,55,97,1035,183,321,1005,196,350,1036,1,4,1032,0,0,1159,6,15,1144,63,118,1026,1597,6,50412,"FO2","IC" 14,25,1,3,2,25,30,"COMMONWEALTH ENERGY SYS","W TISBURY",0,"LIGHT OIL",4120,"0M",1294,,80,95,0,0,2023,42,87,1936,0,0,1936,2,4,1932,38,68,1918,40,70,1848,243,439,1711,204,373,1827,0,0,1827,0,0,2044,5,18,2026,47,98,1928,6049,6,50412,"FO2","IC" 14,25,1,3,2,25,35,"COMMONWEALTH ENERGY SYS","AIRPORT DIE",0,"LIGHT OIL",4120,"0M",1294,,80,95,2,4,65,20,32,57,6,9,48,14,26,23,3,17,6,0,6,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,7184,6,50412,"FO2","IC" 14,25,1,4,2,46,1,"FITCHBURG GAS & ELEC LGT","FITCHBURG",0,"LIGHT OIL",6374,"0M",1294,,,95,113,320,1233,544,1372,812,0,0,1289,68,210,1079,120,416,1139,539,1444,1109,663,1798,2154,708,1974,1126,70,191,2125,49,166,1960,0,0,1960,461,1173,2216,1601,6,50990,"FO2","GT" 14,25,1,1,,59,5,"HOLYOKE WTR PWR CO","BB HOLBROOK",0,,8779,"0M",1294,,554,95,215,0,0,12,0,0,439,0,0,48,0,0,0,0,0,-4,0,0,-2,0,0,111,0,0,7,0,0,88,0,0,177,0,0,95,0,0,1602,6,51327,"WAT","HY" 14,25,1,1,,59,7,"HOLYOKE WTR PWR CO","CHEMICAL",0,,8779,"0M",1294,,554,95,390,0,0,65,0,0,264,0,0,560,0,0,1378,0,0,-3,0,0,-2,0,0,33,0,0,-2,0,0,199,0,0,228,0,0,152,0,0,1604,6,51327,"WAT","HY" 14,25,1,1,,59,10,"HOLYOKE WTR PWR CO","HADLEY FLLS",0,,8779,"0M",1294,,554,95,19318,0,0,16252,0,0,20835,0,0,17997,0,0,1047,0,0,10005,0,0,4815,0,0,8945,0,0,1536,0,0,13795,0,0,19251,0,0,19209,0,0,1605,6,51327,"WAT","HY" 14,25,1,1,,59,15,"HOLYOKE WTR PWR CO","RIVERSIDE",0,,8779,"0M",1294,,554,95,2283,0,0,798,0,0,2407,0,0,2806,0,0,1058,0,0,-32,0,0,-28,0,0,236,0,0,-31,0,0,991,0,0,1475,0,0,1658,0,0,1607,6,51327,"WAT","HY" 14,25,1,1,,59,20,"HOLYOKE WTR PWR CO","BOATLOCK",0,,8779,"0M",1294,,554,95,1401,0,0,440,0,0,1465,0,0,1749,0,0,-1985,0,0,-45,0,0,34,0,0,364,0,0,188,0,0,1015,0,0,1030,0,0,1719,0,0,1603,6,51327,"WAT","HY" 14,25,1,1,,59,21,"HOLYOKE WTR PWR CO","SKINNER",0,,8779,"0M",1294,,554,95,1087,0,0,-990,0,0,135,0,0,122,0,0,0,0,0,-3,0,0,-3,0,0,10,0,0,-5,0,0,48,0,0,88,0,0,144,0,0,1608,6,51327,"WAT","HY" 14,25,1,2,2,59,23,"HOLYOKE WTR PWR CO","MT TOM",0,"LIGHT OIL",8779,"0M",1294,,554,95,253,312,334,85,74,223,86,144,363,96,161,0,210,338,471,128,216,400,63,106,0,319,575,0,148,244,0,283,596,339,311,528,442,268,461,289,1606,6,51327,"FO2","ST" 14,25,1,2,6,59,23,"HOLYOKE WTR PWR CO","MT TOM",0,"BIT COAL",8779,"0M",1294,,554,95,83436,31625,65901,94304,36568,48767,100316,38568,48417,92219,34981,57613,86828,32256,68520,89522,33641,55040,96838,37232,50903,67013,26869,64337,58083,21428,72102,20300,9635,85211,75120,28714,96373,83498,33548,87268,1606,6,51327,"BIT","ST" 14,25,1,2,3,85,1,"MONTAUP ELECTRIC COMPANY","SOMERSET",0,"HEAVY OIL",12833,"0M",1294,,,95,5362,8778,70647,3605,6271,64376,3682,6389,57987,572,894,57093,4068,7388,49705,3861,6474,101371,1808,3090,98281,1729,8455,89825,4071,6826,83000,7484,12748,70251,8762,14647,55605,1259,3587,97942,1613,6,56511,"FO6","ST" 14,25,1,2,6,85,1,"MONTAUP ELECTRIC COMPANY","SOMERSET",0,"BIT COAL",12833,"0M",1294,,,95,57318,21462,76767,61443,26125,64290,61730,25219,52529,14739,5125,47404,25607,10149,50811,58410,21998,42203,65563,26654,42553,52228,21241,48670,53057,20314,65856,44642,17190,76089,48433,18499,83931,70559,26084,98563,1613,6,56511,"BIT","ST" 14,25,1,4,2,85,1,"MONTAUP ELECTRIC COMPANY","SOMERSET",0,"LIGHT OIL",12833,"0M",1294,,,95,143,374,5116,433,1118,3998,115,229,3769,65,186,3583,285,740,4510,629,1593,4110,1349,3410,5229,1777,4429,5348,136,348,5000,0,0,4999,5,26,5687,653,1369,4318,1613,6,56511,"FO2","GT" 14,25,1,3,2,90,15,"NANTUCKET ELEC CO","NANTUCKET",0,"LIGHT OIL",13206,"0M",1294,,,95,7539,12658,2602,7625,13184,8503,7218,12056,5494,6969,12757,2261,7465,13354,7937,7820,14759,9687,10453,19444,7486,10644,19689,5848,7894,13523,10626,6823,12246,7898,7832,14492,3042,9557,16800,2912,1615,6,51977,"FO2","IC" 14,25,1,1,,96,5,"NEW ENGLAND POWER CO","DEERFIELD 2",0,,13433,"0M",1294,,90,95,3908,0,0,2952,0,0,3971,0,0,2045,0,0,1064,0,0,520,0,0,442,0,0,617,0,0,404,0,0,2016,0,0,3583,0,0,2747,0,0,6047,6,52007,"WAT","HY" 14,25,1,1,,96,10,"NEW ENGLAND POWER CO","DEERFIELD 3",0,,13433,"0M",1294,,90,95,4040,0,0,3243,0,0,4233,0,0,2293,0,0,1182,0,0,848,0,0,445,0,0,722,0,0,460,0,0,1885,0,0,3570,0,0,3116,0,0,6083,6,52007,"WAT","HY" 14,25,1,1,,96,15,"NEW ENGLAND POWER CO","DEERFIELD 4",0,,13433,"0M",1294,,90,95,3691,0,0,2835,0,0,3555,0,0,1674,0,0,865,0,0,673,0,0,414,0,0,621,0,0,420,0,0,1920,0,0,3135,0,0,2638,0,0,6119,6,52007,"WAT","HY" 14,25,1,1,,96,20,"NEW ENGLAND POWER CO","DEERFIELD 5",0,,13433,"0M",1294,,90,95,8684,0,0,6946,0,0,8699,0,0,2314,0,0,807,0,0,564,0,0,515,0,0,177,0,0,0,0,0,0,0,0,3382,0,0,5810,0,0,1620,6,52007,"WAT","HY" 14,25,1,1,,96,25,"NEW ENGLAND POWER CO","SHERMAN",0,,13433,"0M",1294,,90,95,4117,0,0,3467,0,0,4264,0,0,1151,0,0,407,0,0,439,0,0,377,0,0,602,0,0,527,0,0,2183,0,0,3889,0,0,2917,0,0,6012,6,52007,"WAT","HY" 14,25,1,2,3,96,27,"NEW ENGLAND POWER CO","BRAYTON PT",0,"HEAVY OIL",13433,"0M",1294,,90,95,40093,74054,435541,65951,116563,318656,49098,75749,438283,41100,69916,368366,2212,5326,519600,0,0,519442,0,0,519401,488,4266,515767,0,0,516617,0,0,516584,7553,10954,505630,71672,125949,379784,1619,6,52007,"FO6","ST" 14,25,1,2,6,96,27,"NEW ENGLAND POWER CO","BRAYTON PT",0,"BIT COAL",13433,"0M",1294,,90,95,657136,245754,255528,538158,200282,277893,335153,130042,379361,336389,128159,523785,552184,203304,520224,709319,259373,461575,714608,267126,390587,681408,256270,431828,600517,222478,518312,676108,250140,322224,643066,226804,159986,692743,256541,166201,1619,6,52007,"BIT","ST" 14,25,1,2,9,96,27,"NEW ENGLAND POWER CO","BRAYTON PT",0,"NAT GAS",13433,"0M",1294,,90,95,2475,65992,0,19895,234494,0,87264,1046891,0,115149,1305242,0,165738,1925331,0,192541,2159965,0,121121,1465806,0,138514,1578722,0,90677,1067560,0,7950,208839,0,642,50267,0,499,65467,0,1619,6,52007,"NG","ST" 14,25,1,3,2,96,27,"NEW ENGLAND POWER CO","BRAYTON PT",0,"LIGHT OIL",13433,"0M",1294,,90,95,48,91,0,168,321,0,49,91,0,66,120,0,149,212,0,229,427,0,434,803,0,429,813,0,49,97,0,17,33,0,0,0,0,122,221,0,1619,6,52007,"FO2","IC" 14,25,1,2,3,96,33,"NEW ENGLAND POWER CO","SALEM HABR",0,"HEAVY OIL",13433,"0M",1294,,90,95,4216,6811,427550,19621,51462,372000,43825,80929,296042,52176,100975,196885,88546,157427,294207,74155,134469,405510,143472,245061,157683,78033,135040,315193,15952,29894,481681,10242,22800,451257,31856,63264,446411,130138,177251,300301,1626,6,52007,"FO6","ST" 14,25,1,2,6,96,33,"NEW ENGLAND POWER CO","SALEM HABR",0,"BIT COAL",13433,"0M",1294,,90,95,170230,67910,116594,174526,68827,87604,182421,75469,107334,180983,73494,87888,123760,53441,145441,149482,64633,132065,157915,67184,148469,169338,69504,116124,140768,59871,93091,133365,56779,72780,147538,65216,99054,158287,70574,72828,1626,6,52007,"BIT","ST" 14,25,1,3,2,96,40,"NEW ENGLAND POWER CO","GLOUCESTER",0,"LIGHT OIL",13433,"0M",1294,,90,95,180,400,1027,365,1056,1255,495,500,1183,191,320,863,798,1430,1148,331,615,1333,398,757,1219,767,1957,1197,100,165,1033,0,0,1031,2,3,1465,491,918,1190,1624,6,52007,"FO2","IC" 14,25,1,3,2,96,50,"NEW ENGLAND POWER CO","NEWBURYPORT",0,"LIGHT OIL",13433,"0M",1294,,90,95,23,31,898,242,431,942,1,0,943,124,222,720,79,135,986,279,516,828,384,714,746,466,834,770,24,47,723,5,10,715,0,0,929,200,360,998,1625,6,52007,"FO2","IC" 14,25,1,1,,96,55,"NEW ENGLAND POWER CO","FIFE BROOK",0,,13433,"0M",1294,,90,95,4107,0,0,3775,0,0,4880,0,0,1321,0,0,312,0,0,338,0,0,198,0,0,494,0,0,291,0,0,2274,0,0,4150,0,0,3161,0,0,8004,6,52007,"WAT","HY" 14,25,1,1,,96,60,"NEW ENGLAND POWER CO","BEAR SWAMP",0,"P-PUMPSTG",13433,"0M",1294,,90,95,-17861,61325,0,-15324,57381,0,-16082,58258,0,-15241,53916,0,-14630,56226,0,-16812,61971,0,-18159,63682,0,-15902,62948,0,-16995,61404,0,-17477,62001,0,-15650,58713,0,-16215,58454,0,8005,6,52007,"WAT","HY" 14,25,1,1,,145,5,"W MASSACHUSETTS ELEC CO","CABOT",0,,20455,"0M",1294,,555,95,27350,0,0,20962,0,0,33562,0,0,28813,0,0,2450,0,0,11373,0,0,5730,0,0,10888,0,0,1060,0,0,21360,0,0,32264,0,0,23532,0,0,1629,6,53266,"WAT","HY" 14,25,1,1,,145,10,"W MASSACHUSETTS ELEC CO","COBBLE MT",0,,20455,"0M",1294,,555,95,2687,0,0,2401,0,0,3134,0,0,1490,0,0,613,0,0,1371,0,0,1579,0,0,2606,0,0,404,0,0,934,0,0,679,0,0,2257,0,0,1630,6,53266,"WAT","HY" 14,25,1,1,,145,12,"W MASSACHUSETTS ELEC CO","DWIGHT",0,,20455,"0M",1294,,555,95,541,0,0,520,0,0,744,0,0,709,0,0,972,0,0,422,0,0,241,0,0,219,0,0,137,0,0,316,0,0,187,0,0,450,0,0,6378,6,53266,"WAT","HY" 14,25,1,1,,145,20,"W MASSACHUSETTS ELEC CO","GARDER FLS",0,,20455,"0M",1294,,555,95,1535,0,0,1501,0,0,2140,0,0,1273,0,0,591,0,0,393,0,0,159,0,0,373,0,0,244,0,0,740,0,0,1394,0,0,1292,0,0,1634,6,53266,"WAT","HY" 14,25,1,1,,145,30,"W MASSACHUSETTS ELEC CO","IND ORCHARD",0,,20455,"0M",1294,,555,95,1913,0,0,854,0,0,1614,0,0,786,0,0,661,0,0,177,0,0,8,0,0,59,0,0,4,0,0,434,0,0,1375,0,0,741,0,0,6379,6,53266,"WAT","HY" 14,25,1,1,,145,32,"W MASSACHUSETTS ELEC CO","PUTTS BRDGE",0,,20455,"0M",1294,,555,95,224,0,0,252,0,0,1368,0,0,249,0,0,550,0,0,741,0,0,249,0,0,393,0,0,186,0,0,1233,0,0,1150,0,0,251,0,0,1637,6,53266,"WAT","HY" 14,25,1,1,,145,33,"W MASSACHUSETTS ELEC CO","RED BRIDGE",0,,20455,"0M",1294,,555,95,2265,0,0,1259,0,0,1699,0,0,1592,0,0,1025,0,0,689,0,0,212,0,0,256,0,0,150,0,0,1248,0,0,7724,0,0,1271,0,0,1638,6,53266,"WAT","HY" 14,25,1,1,,145,35,"W MASSACHUSETTS ELEC CO","TURNERS FL",0,,20455,"0M",1294,,555,95,1180,0,0,-9,0,0,2580,0,0,457,0,0,2357,0,0,3,0,0,320,0,0,753,0,0,1529,0,0,1437,0,0,3487,0,0,96,0,0,6388,6,53266,"WAT","HY" 14,25,1,1,,145,37,"W MASSACHUSETTS ELEC CO","NORTHFLD MT",0,"P-PUMPSTG",20455,"0M",1294,,555,95,-40582,142177,0,-33131,122422,0,-34507,127754,0,-38191,123876,0,-53574,130653,0,-54650,139615,0,-65287,149806,0,-58299,150495,0,-60095,144418,0,-65178,152081,0,-51403,135668,0,-54958,140849,0,547,6,53266,"WAT","HY" 14,25,1,4,2,145,38,"W MASSACHUSETTS ELEC CO","DOREEN",0,"LIGHT OIL",20455,"0M",1294,,555,95,50,156,956,319,789,738,14,84,997,11,135,1029,31,63,967,166,460,863,117,360,1099,422,1231,1099,69,204,1073,-10,0,1073,34,122,951,162,418,771,1631,6,53266,"FO2","GT" 14,25,1,2,2,145,55,"W MASSACHUSETTS ELEC CO","W SPRINGFLD",0,"LIGHT OIL",20455,"0M",1294,,555,95,0,0,533,101,224,458,0,0,458,19,36,411,0,0,411,0,0,411,0,0,411,0,0,411,0,0,411,0,0,411,0,0,411,0,0,379,1642,6,53266,"FO2","ST" 14,25,1,2,3,145,55,"W MASSACHUSETTS ELEC CO","W SPRINGFLD",0,"HEAVY OIL",20455,"0M",1294,,555,95,3033,6175,75421,4119,8425,75374,344,607,80604,1867,3252,77352,19,33,77318,750,1321,75997,1456,2596,73401,758,1343,72058,0,0,72058,0,0,72923,2320,5181,76520,13739,24402,55074,1642,6,53266,"FO6","ST" 14,25,1,2,9,145,55,"W MASSACHUSETTS ELEC CO","W SPRINGFLD",0,"NAT GAS",20455,"0M",1294,,555,95,2167,27681,0,81,1046,0,24872,278755,0,28674,316564,0,33801,372726,0,33691,376470,0,34950,395433,0,39329,440670,0,21443,242289,0,3420,45099,0,110,1547,0,158,1773,0,1642,6,53266,"NG","ST" 14,25,1,4,2,145,55,"W MASSACHUSETTS ELEC CO","W SPRINGFLD",0,"LIGHT OIL",20455,"0M",1294,,555,95,45,159,682,84,220,801,-17,0,801,-12,0,801,-3,12,789,108,297,6777,282,717,1096,319,633,977,0,0,977,0,0,977,0,0,977,0,0,977,1642,6,53266,"FO2","GT" 14,25,1,4,2,145,60,"W MASSACHUSETTS ELEC CO","WOODLAND RD",0,"LIGHT OIL",20455,"0M",1294,,555,95,38,127,1027,218,623,814,3,20,1144,11,96,1048,22,56,992,219,604,924,341,963,1130,373,1030,1017,32,105,1090,-7,0,1090,5,59,1032,156,398,534,1643,6,53266,"FO2","GT" 14,25,5,3,2,532,5,"BRAINTREE (CITY OF)","POTTER",0,"LIGHT OIL",2144,"0M",1294,,,95,1,3,0,40,86,0,2,4,0,8,15,0,18,33,0,0,0,0,66,37,0,90,173,0,8,15,0,16,29,0,0,0,0,47,86,0,1660,6,50315,"FO2","IC" 14,25,5,5,9,532,5,"BRAINTREE (CITY OF)","POTTER",0,"WASTE HT",2144,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1660,6,50315,"NG","CC" 14,25,5,6,2,532,5,"BRAINTREE (CITY OF)","POTTER",0,"LIGHT OIL",2144,"0M",1294,,,95,597,1163,3860,1950,3916,4922,529,946,3897,722,1243,2632,0,0,2595,0,0,2595,0,0,0,0,0,0,0,0,0,418,803,0,0,0,0,563,1271,0,1660,6,50315,"FO2","CT" 14,25,5,6,9,532,5,"BRAINTREE (CITY OF)","POTTER",0,"NAT GAS",2144,"0M",1294,,,95,6985,76876,0,16116,164048,0,4161,42418,0,25648,268544,0,6647,61554,0,0,0,0,6439,68107,0,22225,231091,0,11633,125960,0,2826,30097,0,605,6473,0,2795,30378,0,1660,6,50315,"NG","CT" 14,25,5,1,,597,5,"HOLYOKE (CITY OF)","HOLYOKE",0,,8776,"0M",1294,,,95,1039,0,0,94,0,0,1200,0,0,538,0,0,244,0,0,216,0,0,169,0,0,308,0,0,243,0,0,308,0,0,843,0,0,63,0,0,9864,6,51325,"WAT","HY" 14,25,5,2,3,597,5,"HOLYOKE (CITY OF)","HOLYOKE",0,"HEAVY OIL",8776,"0M",1294,,,95,-34,8,21223,-7,161,18597,-32,0,17335,-149,242,9944,-157,0,11105,-26,144,12014,197,918,10400,173,751,10383,0,0,21744,-26,2,23445,-45,21,21407,48,571,24539,9864,6,51325,"FO6","ST" 14,25,5,2,9,597,5,"HOLYOKE (CITY OF)","HOLYOKE",0,"NAT GAS",8776,"0M",1294,,,95,-406,548,0,-47,7095,0,-432,0,0,-151,1508,0,-180,0,0,-82,2775,0,358,10343,0,495,13260,0,-282,0,0,-300,136,0,-310,907,0,116,8617,0,9864,6,51325,"NG","ST" 14,25,5,3,2,602,1,"HUDSON (CITY OF)","CHERRY ST",0,"LIGHT OIL",8973,"0A",1294,,,95,126,216,6535,468,801,5733,24,47,5687,49,79,5608,60,99,5509,136,242,5267,334,576,4687,237,442,10028,21,36,9992,0,0,9992,0,0,9992,0,613,9379,9038,6,51362,"FO2","IC" 14,25,5,3,9,602,1,"HUDSON (CITY OF)","CHERRY ST",0,"NAT GAS",8973,"0A",1294,,,95,16,177,0,0,0,0,0,0,0,27,276,0,223,2327,0,514,5353,0,813,8555,0,1067,10973,0,248,2679,0,0,0,0,0,0,0,0,0,0,9038,6,51362,"NG","IC" 14,25,5,3,2,613,1,"IPSWICH (CITY OF)","IPSWICH",0,"LIGHT OIL",9442,"0A",1294,,,95,3,144,1524,185,504,1020,-44,84,928,26,97,839,45,81,751,112,229,1817,221,430,1388,171,335,1053,42,71,981,0,0,1991,0,13,1901,70,285,1616,1670,6,51411,"FO2","IC" 14,25,5,3,9,613,1,"IPSWICH (CITY OF)","IPSWICH",0,"NAT GAS",9442,"0A",1294,,,95,0,0,0,0,0,0,-7,91,0,26,564,0,193,2049,0,356,4180,0,540,6225,0,488,5467,0,218,2149,0,0,0,0,0,164,0,0,0,0,1670,6,51411,"NG","IC" 14,25,5,3,2,630,20,"MARBLEHEAD (CITY OF)","COMM ST 2",0,"LIGHT OIL",11624,"0A",1294,,,95,0,0,134,30,54,153,0,0,124,1,4,109,8,23,86,22,43,163,30,67,96,40,77,139,3,3,134,0,0,129,0,0,107,16,31,153,6585,6,51769,"FO2","IC" 14,25,5,3,2,630,25,"MARBLEHEAD (CITY OF)","WILKINS STA",0,"LIGHT OIL",11624,"0A",1294,,,95,24,42,422,242,404,495,3,4,490,17,25,466,41,67,398,140,249,387,184,331,532,214,384,390,17,34,833,0,0,831,0,0,833,105,187,646,6586,6,51769,"FO2","IC" 14,25,5,4,2,640,5,"MASS MUN WHOLESALE ELEC","STONY BROOK",0,"LIGHT OIL",11806,"0M",1294,,,95,868,1812,0,3250,6760,0,1070,2159,0,1016,2152,0,1531,3641,0,3583,7206,0,6923,15010,0,5440,12228,0,1296,2825,0,251,525,0,0,0,0,2081,4355,0,6081,6,56516,"FO2","GT" 14,25,5,5,2,640,5,"MASS MUN WHOLESALE ELEC","STONY BROOK",0,"LIGHT OIL",11806,"0M",1294,,,95,4867,0,0,4882,0,0,1895,0,0,0,0,0,1645,0,0,1298,0,0,2909,0,0,2231,0,0,542,0,0,137,0,0,778,0,0,7866,0,0,6081,6,56516,"FO2","CC" 14,25,5,5,9,640,5,"MASS MUN WHOLESALE ELEC","STONY BROOK",0,"WASTE HT",11806,"0M",1294,,,95,667,6409,0,33,225,0,713,7903,0,38860,226425,0,32080,282829,0,30410,271547,0,30355,268417,0,22281,199679,0,16911,152536,0,13731,126250,0,649,6336,0,0,0,0,6081,6,56516,"NG","CC" 14,25,5,6,2,640,5,"MASS MUN WHOLESALE ELEC","STONY BROOK",0,"LIGHT OIL",11806,"0M",1294,,,95,16765,34499,275954,17076,35625,171066,1732,3145,164811,15194,31318,130811,4458,10049,117055,3259,6474,203614,7129,14689,223923,5719,12097,199458,1427,2966,193410,406,852,191674,2974,6318,192851,24527,50346,140778,6081,6,56516,"FO2","CT" 14,25,5,6,9,640,5,"MASS MUN WHOLESALE ELEC","STONY BROOK",0,"NAT GAS",11806,"0M",1294,,,95,2298,22081,0,33,225,0,7123,78947,0,38860,226425,0,85133,750563,0,75927,677993,0,74156,655728,0,57044,511219,0,44278,399380,0,38588,354794,0,2475,24166,0,0,0,0,6081,6,56516,"NG","CT" 14,25,5,4,2,668,10,"PEABODY (CITY OF)","WATERS RIVR",0,"LIGHT OIL",14605,"0M",1294,,,95,4,11,7009,461,990,6019,3,13,6006,114,218,5789,218,411,5378,259,572,4806,1447,3081,5724,79,204,5787,0,0,5770,0,0,5770,0,0,5770,751,1304,4214,1678,6,52270,"FO2","GT" 14,25,5,4,9,668,10,"PEABODY (CITY OF)","WATERS RIVR",0,"NAT GAS",14605,"0M",1294,,,95,71,948,0,818,8676,0,0,0,0,298,3898,0,500,6079,0,1161,14052,0,735,10563,0,2810,34245,0,871,10971,0,16,244,0,0,0,0,136,1612,0,1678,6,52270,"NG","GT" 14,25,5,3,2,695,1,"SHREWSBURY (CITY OF)","SHREWSBURY",0,"LIGHT OIL",17127,"0A",1294,,,95,-48,53,1717,-20,96,1621,-72,0,1621,-59,0,1621,-27,43,1577,28,133,1444,206,450,994,393,793,1630,-12,58,1571,-52,4,1568,-66,0,1568,5,146,1421,6125,6,52653,"FO2","IC" 14,25,5,2,3,711,10,"TAUNTON (CITY OF)","CLRY FLOOD",0,"HEAVY OIL",18488,"0M",1294,,,95,707,1487,45484,117,274,41056,124,1171,40232,227,881,38944,154,338,18232,1782,3821,13122,1997,4404,13146,1671,3714,26632,1017,1981,30701,285,1042,41468,209,665,43572,1269,2308,3691,1682,6,52885,"FO6","ST" 14,25,5,5,3,711,10,"TAUNTON (CITY OF)","CLRY FLOOD",0,"HEAVY OIL",18488,"0M",1294,,,95,2588,4259,0,3074,4987,0,7,71,0,264,1016,0,10569,21610,0,5376,8750,0,7132,10296,0,7761,11325,0,6430,8473,0,269,1218,0,135,435,0,7563,7563,0,1682,6,52885,"FO6","CC" 14,25,5,5,9,711,10,"TAUNTON (CITY OF)","CLRY FLOOD",0,"NAT GAS",18488,"0M",1294,,,95,0,0,0,88,2162,0,0,0,0,0,7,0,70,898,0,11828,118101,0,7953,72245,0,11517,102477,0,3409,38796,0,275,3743,0,0,0,0,0,0,0,1682,6,52885,"NG","CC" 14,25,5,6,2,711,10,"TAUNTON (CITY OF)","CLRY FLOOD",0,"LIGHT OIL",18488,"0M",1294,,,95,600,1721,500,1175,3321,414,0,10,405,0,0,405,23,155,250,230,719,0,424,1426,393,75,247,983,20,69,920,0,0,922,172,601,798,1596,4611,881,1682,6,52885,"FO2","CT" 14,25,5,6,3,711,10,"TAUNTON (CITY OF)","CLRY FLOOD",0,"HEAVY OIL",18488,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1682,6,52885,"FO6","CT" 14,25,5,6,9,711,10,"TAUNTON (CITY OF)","CLRY FLOOD",0,"NAT GAS",18488,"0M",1294,,,95,215,3547,0,0,0,0,0,0,0,9,220,0,91,2523,0,3269,55134,0,3573,59309,0,4974,79500,0,4776,58796,0,188,2751,0,2,41,0,0,0,0,1682,6,52885,"NG","CT" 15,44,1,3,2,59,1,"BLOCK ISLAND POWER CO","BLOCK ISL",0,"LIGHT OIL",1857,"0A",1294,,,95,640,929,1894,560,757,1368,454,801,1953,666,926,2412,871,1183,2384,728,1492,1815,1748,2173,1258,1686,2317,1251,852,1532,1104,890,1214,1044,683,904,1044,537,1042,1378,6567,6,50270,"FO2","IC" 15,44,1,2,3,60,5,"NEW ENGLAND POWER CO","MANCHSTR ST",0,"HEAVY OIL",13433,"0M",1294,,90,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,6954,6984,12805,21121,8031,15471,21089,11950,17787,9381,10642,17134,20900,3236,6,52007,"FO6","ST" 15,44,1,2,6,60,5,"NEW ENGLAND POWER CO","MANCHSTR ST",0,"BIT COAL",13433,"0M",1294,,90,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3236,6,52007,"BIT","ST" 15,44,1,2,9,60,5,"NEW ENGLAND POWER CO","MANCHSTR ST",0,"NAT GAS",13433,"0M",1294,,90,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,185,6790,0,5496,108488,0,22180,283931,0,57696,544903,0,43911,426261,0,200212,1571059,0,273062,2060878,0,3236,6,52007,"NG","ST" 15,44,1,3,2,71,5,"NEWPORT ELECTRIC CORP","ELDRED",0,"LIGHT OIL",13549,"0A",1294,,,95,0,0,912,146,241,919,0,0,916,14,24,893,280,476,872,38,285,806,254,445,603,431,759,765,53,97,884,0,0,884,30,55,818,186,311,942,3240,6,52046,"FO2","IC" 15,44,1,3,2,71,15,"NEWPORT ELECTRIC CORP","JEPSON",0,"LIGHT OIL",13549,"0A",1294,,,95,10,19,1047,104,179,864,0,0,1112,13,24,1094,58,103,998,35,303,926,228,421,966,339,620,1037,31,56,977,0,0,977,0,0,977,162,273,920,3241,6,52046,"FO2","IC" 15,44,5,1,,600,1,"PROVIDENCE (CITY OF)","PROVIDENCE",0,,15440,"0A",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3245,6,52404,"WAT","HY" 16,9,1,1,,21,1,"GILMAN BROTHERS CO","GILMAN",0,,6885,"0A",1294,"R",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,536,6,50309,"WAT","HY" 16,9,1,1,,37,5,"CONNECTICUT LGT & PWR CO","BULLS BRDGE",0,,4176,"0M",1294,,550,95,4542,0,0,3859,0,0,4535,0,0,4526,0,0,711,0,0,1545,0,0,596,0,0,576,0,0,83,0,0,3291,0,0,5258,0,0,4512,0,0,541,6,50651,"WAT","HY" 16,9,1,1,,37,15,"CONNECTICUT LGT & PWR CO","ROBERTSVLE",0,,4176,"0M",1294,,550,95,228,0,0,144,0,0,74,0,0,117,0,0,0,0,0,23,0,0,4,0,0,14,0,0,1,0,0,58,0,0,0,0,0,7,0,0,549,6,50651,"WAT","HY" 16,9,1,1,,37,20,"CONNECTICUT LGT & PWR CO","ROCKY RIVER",0,"C-PUMPSTG",4176,"0M",1294,,550,95,-532,573,0,-108,831,0,-5011,4942,0,-3890,3881,0,-2483,2464,0,-30,0,0,-50,160,0,-45,941,0,-34,0,0,-295,262,0,3242,0,0,3543,0,0,539,6,50651,"WAT","HY" 16,9,1,1,,37,25,"CONNECTICUT LGT & PWR CO","SCOTLAND DM",0,,4176,"0M",1294,,550,95,1196,0,0,762,0,0,1285,0,0,753,0,0,65,0,0,169,0,0,32,0,0,83,0,0,9,0,0,401,0,0,43,0,0,524,0,0,551,6,50651,"WAT","HY" 16,9,1,1,,37,28,"CONNECTICUT LGT & PWR CO","SHEPAUG",0,,4176,"0M",1294,,550,95,19987,0,0,8510,0,0,16746,0,0,8668,0,0,479,0,0,3113,0,0,1323,0,0,1665,0,0,561,0,0,4280,0,0,17593,0,0,9586,0,0,552,6,50651,"WAT","HY" 16,9,1,1,,37,30,"CONNECTICUT LGT & PWR CO","STEVENSON",0,,4176,"0M",1294,,550,95,14594,0,0,6873,0,0,12878,0,0,7022,0,0,5946,0,0,2333,0,0,1155,0,0,1565,0,0,585,0,0,7574,0,0,15018,0,0,7269,0,0,553,6,50651,"WAT","HY" 16,9,1,1,,37,33,"CONNECTICUT LGT & PWR CO","TAFTVILLE",0,,4176,"0M",1294,,550,95,1047,0,0,773,0,0,1181,0,0,662,0,0,0,0,0,286,0,0,106,0,0,168,0,0,58,0,0,376,0,0,802,0,0,539,0,0,554,6,50651,"WAT","HY" 16,9,1,1,,37,35,"CONNECTICUT LGT & PWR CO","TUNNEL",0,,4176,"0M",1294,,550,95,1344,0,0,790,0,0,1127,0,0,808,0,0,808,0,0,130,0,0,51,0,0,62,0,0,13,0,0,528,0,0,1238,0,0,756,0,0,557,6,50651,"WAT","HY" 16,9,1,4,2,37,35,"CONNECTICUT LGT & PWR CO","TUNNEL",0,"LIGHT OIL",4176,"0M",1294,,550,95,92,241,1121,148,413,1052,-10,0,1052,8,34,1017,-9,0,1017,174,492,1054,399,1075,1028,391,1123,1060,-10,0,1060,-9,0,1060,-8,0,1060,247,642,1013,557,6,50651,"FO2","GT" 16,9,1,4,2,37,37,"CONNECTICUT LGT & PWR CO","COS COB",0,"LIGHT OIL",4176,"0M",1294,,550,95,338,879,6366,1004,2550,5530,-6,0,6730,61,328,6402,100,252,6836,1043,2766,6164,1606,4183,6744,1574,4512,6417,89,372,6045,10,115,5931,-7,47,5884,478,1250,6205,542,6,50651,"FO2","GT" 16,9,1,2,2,37,40,"CONNECTICUT LGT & PWR CO","DEVON",0,"LIGHT OIL",4176,"0M",1294,,550,95,4,7,607,26,48,738,10,19,719,8,14,705,6,12,693,5,10,683,12,21,662,5,10,652,35,67,586,12,21,564,10,19,545,126,250,652,544,6,50651,"FO2","ST" 16,9,1,2,3,37,40,"CONNECTICUT LGT & PWR CO","DEVON",0,"HEAVY OIL",4176,"0M",1294,,550,95,1691,2896,140820,5317,8938,131882,6310,10503,160145,2309,3909,156236,1040,1748,154488,1026,1746,152742,366,624,152118,0,0,152118,0,0,152118,1119,1895,186866,0,0,223227,52715,95704,164704,544,6,50651,"FO6","ST" 16,9,1,2,9,37,40,"CONNECTICUT LGT & PWR CO","DEVON",0,"NAT GAS",4176,"0M",1294,,550,95,139882,1480772,0,125833,1333372,0,140034,1484076,0,74718,805341,0,129292,1364215,0,113222,1209824,0,134347,1440396,0,141005,1520883,0,84240,919763,0,92690,988325,0,85651,910220,0,1027,11734,0,544,6,50651,"NG","ST" 16,9,1,4,2,37,40,"CONNECTICUT LGT & PWR CO","DEVON",0,"LIGHT OIL",4176,"0M",1294,,550,95,-8,0,826,52,143,1016,-6,0,1016,11,41,975,15,50,924,93,252,873,213,464,899,323,840,1155,12,42,1113,14,46,864,-8,0,864,126,312,755,544,6,50651,"FO2","GT" 16,9,1,2,2,37,45,"CONNECTICUT LGT & PWR CO","MONTVILLE",0,"LIGHT OIL",4176,"0M",1294,,550,95,79,187,224,71,184,282,0,0,277,35,81,316,26,52,254,126,275,254,225,460,205,169,342,281,13,78,193,-9,27,344,11,35,57,248,530,404,546,6,50651,"FO2","ST" 16,9,1,2,3,37,45,"CONNECTICUT LGT & PWR CO","MONTVILLE",0,"HEAVY OIL",4176,"0M",1294,,550,95,19404,42123,179930,11903,28403,229734,496,984,267130,8852,18669,287361,73,131,287230,16090,31789,255441,33046,60820,194621,29759,54794,250449,448,2452,286041,-459,1261,284780,4782,14127,272628,50192,96782,219079,546,6,50651,"FO6","ST" 16,9,1,2,9,37,45,"CONNECTICUT LGT & PWR CO","MONTVILLE",0,"NAT GAS",4176,"0M",1294,,550,95,2644,35575,0,1337,19886,0,14239,177907,0,15760,209674,0,26332,300080,0,15321,191070,0,33080,384304,0,29657,341116,0,660,22744,0,-410,7132,0,948,17617,0,2622,31910,0,546,6,50651,"NG","ST" 16,9,1,3,2,37,45,"CONNECTICUT LGT & PWR CO","MONTVILLE",0,"LIGHT OIL",4176,"0M",1294,,550,95,5,11,429,51,91,429,3,5,429,21,47,429,5,10,429,32,60,429,47,88,429,44,82,429,5,10,429,0,0,429,7,15,429,14,27,429,546,6,50651,"FO2","IC" 16,9,1,2,2,37,46,"CONNECTICUT LGT & PWR CO","NORWALK HAR",0,"LIGHT OIL",4176,"0M",1294,,550,95,1942,3751,1166,1049,1831,1166,1411,2570,1166,801,1409,746,830,1566,1275,1306,2393,1275,1212,2164,1208,1005,1793,1129,448,996,1090,743,1549,1201,1863,3623,816,1573,2830,1073,548,6,50651,"FO2","ST" 16,9,1,2,3,37,46,"CONNECTICUT LGT & PWR CO","NORWALK HAR",0,"HEAVY OIL",4176,"0M",1294,,550,95,61485,109340,281515,116317,186438,251428,53269,89422,277523,112195,177490,244461,49615,86635,387526,72024,117143,423659,87276,142042,395624,69104,110519,365065,12764,26032,444868,12966,24423,458286,56112,97835,437824,98414,160154,343905,548,6,50651,"FO6","ST" 16,9,1,4,2,37,46,"CONNECTICUT LGT & PWR CO","NORWALK HAR",0,"LIGHT OIL",4176,"0M",1294,"R",550,95,0,0,0,0,0,0,-12,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,548,6,50651,"FO2","GT" 16,9,1,1,,37,60,"CONNECTICUT LGT & PWR CO","BANTAM",0,,4176,"0M",1294,,550,95,166,0,0,122,0,0,177,0,0,99,0,0,0,0,0,24,0,0,2,0,0,9,0,0,0,0,0,66,0,0,182,0,0,126,0,0,6457,6,50651,"WAT","HY" 16,9,1,1,,37,65,"CONNECTICUT LGT & PWR CO","FLS VILLAGE",0,,4176,"0M",1294,,550,95,6485,0,0,3067,0,0,6148,0,0,4269,0,0,57,0,0,1043,0,0,359,0,0,386,0,0,86,0,0,3283,0,0,6134,0,0,3241,0,0,560,6,50651,"WAT","HY" 16,9,1,4,2,37,70,"CONNECTICUT LGT & PWR CO","FRANKLIN DR",0,"LIGHT OIL",4176,"0M",1294,,550,95,87,251,1073,112,303,770,-21,0,770,6,41,429,9,45,1229,156,508,1033,386,937,931,385,1480,880,-11,0,808,-12,0,808,-14,0,0,109,306,1000,561,6,50651,"FO2","GT" 16,9,1,2,2,37,75,"CONNECTICUT LGT & PWR CO","MIDDLETOWN",0,"LIGHT OIL",4176,"0M",1294,,550,95,52,116,72,106,200,205,37,72,134,69,119,181,93,171,177,62,115,62,142,274,121,143,283,195,159,331,184,25,61,123,89,174,116,58,124,159,562,6,50651,"FO2","ST" 16,9,1,2,3,37,75,"CONNECTICUT LGT & PWR CO","MIDDLETOWN",0,"HEAVY OIL",4176,"0M",1294,,550,95,28156,57773,619646,82338,144562,470965,28954,52136,494722,112799,180932,367774,91771,154447,321716,103385,178821,285273,180564,315539,192342,120265,219668,308678,14240,27382,395204,9172,20697,432521,29631,53865,465010,116423,197687,379501,562,6,50651,"FO6","ST" 16,9,1,4,2,37,75,"CONNECTICUT LGT & PWR CO","MIDDLETOWN",0,"LIGHT OIL",4176,"0M",1294,,550,95,0,0,986,60,155,998,2,12,986,0,0,986,18,56,1096,133,235,803,220,518,962,326,864,969,6,21,948,0,0,946,0,0,936,0,0,936,562,6,50651,"FO2","GT" 16,9,1,2,"C",37,80,"CONNECTICUT LGT & PWR CO","S MEADOW",0,"REFUSE",4176,"0M",1294,,550,95,36668,0,0,31584,0,0,30750,0,0,36558,0,0,4988,0,0,38064,0,0,35273,0,0,35840,0,0,37803,0,0,39379,0,0,36583,0,0,40236,0,0,563,6,50651,"GEO","ST" 16,9,1,4,2,37,80,"CONNECTICUT LGT & PWR CO","S MEADOW",0,"LIGHT OIL",4176,"0M",1294,,550,95,547,1286,33605,2263,5797,27807,-4,195,27613,257,794,4952,465,1373,43574,2527,6621,35953,4081,8784,28189,3486,11650,34410,234,1143,29931,-49,0,29931,56,271,29660,2479,6072,23588,563,6,50651,"FO2","GT" 16,9,1,4,2,37,85,"CONNECTICUT LGT & PWR CO","TORRINGTN T",0,"LIGHT OIL",4176,"0M",1294,,550,95,80,183,802,-19,0,802,9,49,753,4,24,729,-6,0,1062,163,373,867,4081,6864,28189,583,1059,947,4,16,931,-7,0,931,-8,0,931,173,446,1006,565,6,50651,"FO2","GT" 16,9,1,4,2,37,90,"CONNECTICUT LGT & PWR CO","BRANFORD",0,"LIGHT OIL",4176,"0M",1294,,550,95,-23,0,993,-11,0,993,-12,0,983,-9,0,993,-12,0,993,-15,0,963,303,888,1170,580,1248,981,112,115,1073,-7,12,1061,12,62,999,103,312,1042,540,6,50651,"FO2","GT" 16,9,1,2,1,45,1,"CONN YANKEE ATOMIC PWR CO","HADDAM NECK",0,"NUCLEAR",4187,"0M",1294,,551,95,349804,0,0,-2724,0,0,-2714,0,0,80321,0,0,411060,0,0,385019,0,0,346822,0,0,397229,0,0,404771,0,0,427136,0,0,421633,0,0,435253,0,0,558,6,50652,"UR","ST" 16,9,1,1,,70,1,"FARMINGTON RIVER POWER CO","RAINBOW",0,,6207,"0A",1294,,,95,4465,0,0,2602,0,0,3654,0,0,2574,0,0,1712,0,0,1108,0,0,787,0,0,842,0,0,700,0,0,2530,0,0,4222,0,0,2756,0,0,559,6,50970,"WAT","HY" 16,9,1,2,1,85,1,"NORTHEAST NUCL ENERGY CO","MILLSTONE",0,"NUCLEAR",21687,"0M",1294,,553,95,474794,0,0,424364,0,0,479164,0,0,452923,0,0,470915,0,0,397551,0,0,307242,0,0,369216,0,0,459416,0,0,478184,0,0,46176,0,0,-2630,0,0,566,6,50005,"UR","ST" 16,9,1,2,1,85,2,"NORTHEAST NUCL ENERGY CO","MILLSTONE",0,"NUCLEAR",21687,"0M",1294,,553,95,-2968,0,0,-3117,0,0,-2841,0,0,12840,0,0,0,0,0,0,0,0,-8427,0,0,340333,0,0,625348,0,0,645987,0,0,618792,0,0,511064,0,0,566,6,50005,"UR","ST" 16,9,1,2,1,85,3,"NORTHEAST NUCL ENERGY CO","MILLSTONE",0,"NUCLEAR",21687,"0M",1294,,553,95,853882,0,0,758672,0,0,851613,0,0,328284,0,0,0,0,0,594786,0,0,853005,0,0,844847,0,0,822134,0,0,852985,0,0,817800,0,0,422956,0,0,566,6,50005,"UR","ST" 16,9,1,2,2,159,3,"UNITED ILLUMINATING CO","BRDGEPT HBR",0,"LIGHT OIL",19497,"0M",1294,,,95,289,498,533,83,144,555,103,183,538,278,575,297,94,164,466,159,276,523,127,224,632,239,436,363,60,105,591,207,368,557,52,92,465,58,101,530,568,6,53003,"FO2","ST" 16,9,1,2,3,159,3,"UNITED ILLUMINATING CO","BRDGEPT HBR",0,"HEAVY OIL",19497,"0M",1294,,,95,12678,20036,157706,31465,49414,142873,1716,2749,140124,28015,51807,143380,11615,18496,124884,34707,55499,150609,43253,69685,122107,18699,30642,149294,6814,10677,163242,4908,7842,155400,4195,6665,148735,54634,86347,0,568,6,53003,"FO6","ST" 16,9,1,2,6,159,3,"UNITED ILLUMINATING CO","BRDGEPT HBR",0,"BIT COAL",19497,"0M",1294,,,95,193441,73716,182983,223214,85285,166858,221070,86802,148636,4755,2176,201542,224862,86475,170775,217578,84500,168741,225684,88542,121774,166492,67303,123827,199715,77070,157924,143992,56780,199095,198867,77375,176894,249682,95223,163986,568,6,53003,"BIT","ST" 16,9,1,4,2,159,3,"UNITED ILLUMINATING CO","BRDGEPT HBR",0,"LIGHT OIL",19497,"0M",1294,,,95,4,8,549,151,259,469,0,0,647,5,12,635,10,18,617,12,22,595,145,256,696,308,560,493,63,111,560,0,0,560,9,16,545,75,130,594,568,6,53003,"FO2","GT" 16,9,1,2,2,159,5,"UNITED ILLUMINATING CO","ENGLISH",0,"LIGHT OIL",19497,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,569,6,53003,"FO2","ST" 16,9,1,2,3,159,5,"UNITED ILLUMINATING CO","ENGLISH",0,"HEAVY OIL",19497,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,569,6,53003,"FO6","ST" 16,9,1,2,2,159,12,"UNITED ILLUMINATING CO","N HAVEN HBR",0,"LIGHT OIL",19497,"0M",1294,,,95,876,1540,484,437,731,468,424,737,445,327,564,583,511,892,406,254,441,667,361,632,570,401,702,762,359,651,646,23,502,680,959,1741,546,779,1314,482,6156,6,53003,"FO2","ST" 16,9,1,2,3,159,12,"UNITED ILLUMINATING CO","N HAVEN HBR",0,"HEAVY OIL",19497,"0M",1294,,,95,104071,166097,286634,171042,260046,151260,95848,151028,241794,147390,227183,379543,69013,110799,306351,74009,117219,286218,97251,153426,333078,88533,139665,374595,39346,64393,310202,163,3184,307018,72476,120773,186245,162959,252660,0,6156,6,53003,"FO6","ST" 16,9,1,2,9,159,12,"UNITED ILLUMINATING CO","N HAVEN HBR",0,"NAT GAS",19497,"0M",1294,,,95,0,0,0,0,0,0,31250,307224,0,64504,630374,0,76077,749979,0,81590,800742,0,99404,985733,0,49501,489902,0,13044,134068,0,34,4180,0,0,0,0,0,0,0,6156,6,53003,"NG","ST" 16,9,5,1,,556,5,"NORWICH (CITY OF)","SECOND ST",0,,13831,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,5,0,0,174,0,0,101,0,0,67,0,0,17,0,0,180,0,0,272,0,0,324,0,0,580,6,52123,"WAT","HY" 16,9,5,1,,556,10,"NORWICH (CITY OF)","OCCUM",0,,13831,"0A",1294,,,95,516,0,0,356,0,0,529,0,0,370,0,0,225,0,0,257,0,0,63,0,0,95,0,0,42,0,0,215,0,0,420,0,0,292,0,0,582,6,52123,"WAT","HY" 16,9,5,1,,556,13,"NORWICH (CITY OF)","TENTH ST",0,,13831,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,83,0,0,0,0,0,113,0,0,54,0,0,255,0,0,534,0,0,636,0,0,583,6,52123,"WAT","HY" 16,9,5,4,2,556,20,"NORWICH (CITY OF)","N MAIN ST",0,"LIGHT OIL",13831,"0A",1294,,,95,0,0,1935,53,168,1767,0,0,1767,0,0,1767,23,56,1711,62,161,1550,402,1007,1693,531,1325,1518,0,0,1518,0,0,1518,0,0,1518,117,296,2388,581,6,52123,"FO2","GT" 16,9,5,3,2,560,1,"SOUTH NORWALK (CITY OF)","SO NORWALK",0,"LIGHT OIL",17569,"0A",1294,,,95,50,90,1114,84,147,1614,27,49,1523,27,45,1455,71,123,1331,70,125,1235,242,444,819,209,351,1604,20,34,1570,2,4,1736,9,13,1671,98,158,1418,6598,6,52704,"FO2","IC" 16,9,5,2,3,567,1,"WALLINGFORD (CITY OF)","PIERCE",0,"HEAVY OIL",20038,"0A",1294,,,95,0,15,1540,368,1067,2318,0,0,2318,0,0,2318,0,0,2318,0,0,2318,0,0,2318,0,0,2318,146,445,1873,0,0,1873,0,0,1873,0,0,1873,6635,6,53175,"FO6","ST" 21,36,1,1,,35,10,"CENTRAL HUDSON GAS & ELEC","DASHVILLE",0,,3249,"0M",1294,,,95,2381,0,0,502,0,0,1130,0,0,814,0,0,844,0,0,273,0,0,156,0,0,52,0,0,6,0,0,1173,0,0,1735,0,0,901,0,0,2481,6,50484,"WAT","HY" 21,36,1,1,,35,18,"CENTRAL HUDSON GAS & ELEC","NEVERSINK",0,,3249,"0M",1294,,,95,4408,0,0,4221,0,0,4645,0,0,2716,0,0,2618,0,0,2849,0,0,10968,0,0,9289,0,0,3298,0,0,2724,0,0,2482,0,0,4970,0,0,2483,6,50484,"WAT","HY" 21,36,1,1,,35,20,"CENTRAL HUDSON GAS & ELEC","STURGEON PL",0,,3249,"0M",1294,,,95,9300,0,0,4140,0,0,8251,0,0,4665,0,0,3127,0,0,1123,0,0,872,0,0,359,0,0,111,0,0,5834,0,0,7954,0,0,3663,0,0,2486,6,50484,"WAT","HY" 21,36,1,2,3,35,25,"CENTRAL HUDSON GAS & ELEC","DANSKAMMER",0,"HEAVY OIL",3249,"0M",1294,,,95,0,0,10567,2887,4585,13091,0,0,13091,0,0,13091,377,619,12472,1176,2123,10349,198,406,9943,0,0,9943,0,0,9943,0,0,9943,16,30,9913,0,0,9913,2480,6,50484,"FO6","ST" 21,36,1,2,6,35,25,"CENTRAL HUDSON GAS & ELEC","DANSKAMMER",0,"BIT COAL",3249,"0M",1294,,,95,180547,67912,176943,208851,77841,149786,144579,54893,173619,180437,67955,164986,58267,23110,161831,149627,57630,163884,131893,51114,152154,127793,49654,170960,144488,55872,134561,60315,24424,150152,137406,60589,138420,208309,77898,129136,2480,6,50484,"BIT","ST" 21,36,1,2,9,35,25,"CENTRAL HUDSON GAS & ELEC","DANSKAMMER",0,"NAT GAS",3249,"0M",1294,,,95,12788,136338,0,5348,58875,0,52133,554622,0,1003,12881,0,26410,269381,0,9355,110458,0,50047,563362,0,64005,727957,0,42268,475832,0,72329,806049,0,21208,238996,0,526,5007,0,2480,6,50484,"NG","ST" 21,36,1,3,2,35,25,"CENTRAL HUDSON GAS & ELEC","DANSKAMMER",0,"LIGHT OIL",3249,"0M",1294,,,95,38,70,119,10,15,278,29,38,240,10,9,231,5,9,222,30,55,167,29,60,281,48,81,200,48,99,274,48,83,191,38,76,289,9,16,273,2480,6,50484,"FO2","IC" 21,36,1,4,2,35,35,"CENTRAL HUDSON GAS & ELEC","SOUTH CAIRO",0,"LIGHT OIL",3249,"0M",1294,,,95,74,178,2486,0,0,2486,0,0,2486,0,0,2486,13,31,2455,198,577,1878,16,34,1844,70,197,1647,0,0,2719,0,0,2719,39,93,2626,18,49,2577,2485,6,50484,"FO2","GT" 21,36,1,4,2,35,40,"CENTRAL HUDSON GAS & ELEC","W COXSACKIE",0,"LIGHT OIL",3249,"0M",1294,,,95,0,0,2176,0,0,2176,0,0,2176,0,0,2176,0,0,2176,0,0,2176,0,0,2176,0,0,2176,0,0,2176,0,0,2176,0,0,2176,0,0,2176,2487,6,50484,"FO2","GT" 21,36,1,4,9,35,40,"CENTRAL HUDSON GAS & ELEC","W COXSACKIE",0,"NAT GAS",3249,"0M",1294,,,95,90,1181,0,32,427,0,0,0,0,45,632,0,59,962,0,631,9351,0,109,1557,0,530,7243,0,0,0,0,52,789,0,180,2430,0,69,1043,0,2487,6,50484,"NG","GT" 21,36,1,2,2,35,45,"CENTRAL HUDSON GAS & ELEC","ROSETON JO",0,"LIGHT OIL",3249,"0M",1294,,,95,1744,3069,2289,782,1361,3014,1071,2036,2369,0,0,2542,0,0,2542,0,0,2542,0,0,2542,0,0,2542,0,0,2542,0,17,2525,654,2512,1229,581,1004,2137,8006,6,50484,"FO2","ST" 21,36,1,2,3,35,45,"CENTRAL HUDSON GAS & ELEC","ROSETON JO",0,"HEAVY OIL",3249,"0M",1294,,,95,49649,80148,781308,157108,249990,495225,13890,23984,478029,0,0,478029,0,0,478029,0,0,604069,0,0,604069,0,0,604069,0,0,604069,0,0,589640,1356,4755,599314,189513,299562,451927,8006,6,50484,"FO6","ST" 21,36,1,2,9,35,45,"CENTRAL HUDSON GAS & ELEC","ROSETON JO",0,"NAT GAS",3249,"0M",1294,,,95,33526,336575,0,69660,692555,0,24026,260204,0,0,0,0,177930,1880760,0,186946,1950511,0,310122,3310810,0,247281,2627847,0,0,0,0,0,0,0,2849,61824,0,7068,69278,0,8006,6,50484,"NG","ST" 21,36,1,1,,35,50,"CENTRAL HUDSON GAS & ELEC","HIGH FALLS",0,,3249,"0M",1294,,,95,1184,0,0,92,0,0,1122,0,0,69,0,0,143,0,0,23,0,0,26,0,0,0,0,0,0,0,0,340,0,0,1057,0,0,170,0,0,579,6,50484,"WAT","HY" 21,36,1,1,,37,5,"CENTRAL VT PUB SERV CORP","CARVERS FLS",0,,3292,"0A",1294,,350,95,921,0,0,597,0,0,1182,0,0,1121,0,0,691,0,0,250,0,0,18,0,0,58,0,0,0,0,0,391,0,0,1196,0,0,502,0,0,6456,6,50503,"WAT","HY" 21,36,1,2,3,40,1,"CONSOL EDISON CO N Y INC","ARTHUR KILL",0,"HEAVY OIL",4226,"0M",1294,,,95,0,0,5711,0,0,5711,0,0,5711,0,0,5711,0,0,5711,0,0,5711,0,0,5711,7328,11940,18519,0,0,18519,0,0,18519,0,0,18513,0,0,18513,2490,6,50653,"FO6","ST" 21,36,1,2,9,40,1,"CONSOL EDISON CO N Y INC","ARTHUR KILL",0,"NAT GAS",4226,"0M",1294,,,95,-1408,17220,0,-1393,16473,0,-1276,5546,0,42517,495291,0,55216,582417,0,194234,1938196,0,301093,2957985,0,278373,2754690,0,147636,1480827,0,-1783,3561,0,-1398,5,0,-1433,5,0,2490,6,50653,"NG","ST" 21,36,1,4,2,40,1,"CONSOL EDISON CO N Y INC","ARTHUR KILL",0,"LIGHT OIL",4226,"0M",1294,,,95,13,44,1913,67,194,1823,0,0,1823,36,79,1744,215,635,1882,298,918,2083,566,1739,2154,371,1201,1884,0,0,0,0,0,0,0,0,0,0,0,0,2490,6,50653,"FO2","GT" 21,36,1,2,1,40,2,"CONSOL EDISON CO N Y INC","INDIAN PT",0,"NUCLEAR",4226,"0M",1294,,,95,562851,0,0,52711,0,0,-6970,0,0,-3790,0,0,-13730,0,0,241777,0,0,674078,0,0,678357,0,0,681364,0,0,661697,0,0,694091,0,0,636105,0,0,2497,6,50653,"UR","ST" 21,36,1,2,3,40,3,"CONSOL EDISON CO N Y INC","ASTORIA",0,"HEAVY OIL",4226,"0M",1294,,,95,44284,69523,204071,87234,136417,162405,51168,80603,150832,37361,58624,135192,36339,59441,192317,36196,59149,130130,89762,143025,106180,87335,138221,98117,59995,93814,117887,54037,87216,125085,64568,101738,117638,289554,461968,161157,8906,6,50653,"FO6","ST" 21,36,1,2,9,40,3,"CONSOL EDISON CO N Y INC","ASTORIA",0,"NAT GAS",4226,"0M",1294,,,95,270672,2666431,0,244705,2376465,0,354262,3528212,0,241575,2383868,0,275033,2732177,0,466083,4630924,0,417404,4132582,0,422777,4216725,0,331846,3235732,0,333120,3377003,0,267480,2653281,0,78615,787377,0,8906,6,50653,"NG","ST" 21,36,1,4,2,40,3,"CONSOL EDISON CO N Y INC","ASTORIA",0,"LIGHT OIL",4226,"0M",1294,,,95,1484,3523,70541,935,2176,68112,695,1314,66869,1270,3125,63744,1033,2385,61076,1517,3666,57410,5121,12698,44790,1655,4191,48468,794,1989,67296,758,1842,65454,651,1541,63965,4785,11328,52945,8906,6,50653,"FO2","GT" 21,36,1,4,9,40,3,"CONSOL EDISON CO N Y INC","ASTORIA",0,"NAT GAS",4226,"0M",1294,,,95,1238,16825,0,4723,63317,0,9436,102713,0,19761,279920,0,13199,175023,0,14602,203072,0,50641,721027,0,30754,443611,0,22755,324431,0,10683,150198,0,29807,410036,0,1300,17862,0,8906,6,50653,"NG","GT" 21,36,1,2,3,40,5,"CONSOL EDISON CO N Y INC","EAST RIVER",0,"HEAVY OIL",4226,"0M",1294,,,95,48411,100447,260377,52328,112594,251467,22577,46041,196293,14368,29471,111609,10915,20599,75923,9443,18148,129321,17347,33410,143239,17145,35799,154704,57,119,208820,391,883,155405,24581,53489,125358,26299,56899,135819,2493,6,50653,"FO6","ST" 21,36,1,2,9,40,5,"CONSOL EDISON CO N Y INC","EAST RIVER",0,"NAT GAS",4226,"0M",1294,,,95,22936,297706,0,16423,222129,0,33740,432005,0,32894,424765,0,83114,976015,0,52018,626673,0,74759,901280,0,43540,571392,0,62070,814818,0,38780,549257,0,26334,362630,0,4079,55677,0,2493,6,50653,"NG","ST" 21,36,1,2,3,40,8,"CONSOL EDISON CO N Y INC","59TH STREET",0,"HEAVY OIL",4226,"0M",1294,,,95,134,711,28019,-168,0,13932,-186,0,17029,-180,0,14663,-186,0,16921,-180,0,14962,-186,0,34238,-186,0,28013,0,0,18655,-186,0,24175,-180,0,21506,-186,0,15408,2503,6,50653,"FO6","ST" 21,36,1,2,9,40,8,"CONSOL EDISON CO N Y INC","59TH STREET",0,"NAT GAS",4226,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,-180,0,0,0,0,0,0,0,0,0,0,0,2503,6,50653,"NG","ST" 21,36,1,4,2,40,8,"CONSOL EDISON CO N Y INC","59TH STREET",0,"LIGHT OIL",4226,"0M",1294,,,95,0,0,2421,12,43,2379,0,0,2379,34,63,2315,382,920,2169,220,532,2101,517,1422,2132,154,399,2018,0,0,2018,0,0,2018,0,0,2019,0,0,2019,2503,6,50653,"FO2","GT" 21,36,1,4,2,40,10,"CONSOL EDISON CO N Y INC","GOWANUS",0,"LIGHT OIL",4226,"0M",1294,,,95,3431,10187,54995,3032,8863,61517,3332,9885,51514,5596,16946,54888,9656,30399,58173,10867,35156,51183,35078,112111,54362,18095,69179,54055,9925,32320,51120,3062,9091,61678,11850,35551,63660,11082,31386,52408,2494,6,50653,"FO2","GT" 21,36,1,4,2,40,17,"CONSOL EDISON CO N Y INC","INDIAN PT",0,"LIGHT OIL",4226,"0M",1294,,,95,10,470,1357,110,334,1476,0,0,1438,10,26,1387,190,648,1553,120,502,1367,618,1994,1429,339,1276,1561,10,65,1518,10,49,1466,70,568,1361,10,79,1524,2497,6,50653,"FO2","GT" 21,36,1,2,3,40,18,"CONSOL EDISON CO N Y INC","HUDSON AVE",0,"HEAVY OIL",4226,"0M",1294,,,95,13942,16640,116475,22892,27677,121761,19571,25683,88715,5881,7513,112117,13579,17821,145862,8960,11221,121321,17004,23012,156902,16358,21789,184711,8488,11589,233738,9039,12876,207818,15377,22058,190563,21649,30797,210122,2496,6,50653,"FO6","ST" 21,36,1,4,2,40,18,"CONSOL EDISON CO N Y INC","HUDSON AVE",0,"LIGHT OIL",4226,"0M",1294,,,95,32,106,3790,262,520,3270,24,63,4088,0,0,4088,318,932,4131,366,1254,4363,1154,3982,3948,684,2253,4361,44,148,4212,7,28,4185,255,954,4157,0,0,4471,2496,6,50653,"FO2","GT" 21,36,1,4,2,40,23,"CONSOL EDISON CO N Y INC","NARROWS BAY",0,"LIGHT OIL",4226,"0M",1294,,,95,1815,5002,70995,2374,6488,64363,3121,8503,70742,4829,13085,57595,4696,13259,61188,7112,20641,70359,14360,43802,86922,0,0,86754,113,310,61193,358,1046,60146,2527,7040,53007,5977,17365,64411,2499,6,50653,"FO2","GT" 21,36,1,4,9,40,23,"CONSOL EDISON CO N Y INC","NARROWS BAY",0,"NAT GAS",4226,"0M",1294,,,95,160,2545,0,0,0,0,1437,23105,0,3151,50378,0,5478,91177,0,7841,132409,0,26727,472807,0,23321,410674,0,8725,137237,0,6684,112244,0,14121,266734,0,726,12168,0,2499,6,50653,"NG","GT" 21,36,1,2,3,40,25,"CONSOL EDISON CO N Y INC","RAVENSWOOD",0,"HEAVY OIL",4226,"0M",1294,,,95,56562,96769,43835,156038,248776,28947,15866,27428,34677,22910,42845,42500,30055,54093,37926,31922,55970,39660,31596,55334,44269,54612,90412,42941,11656,19796,32055,4144,7555,26939,45172,77641,44297,97823,181018,43354,2500,6,50653,"FO6","ST" 21,36,1,2,9,40,25,"CONSOL EDISON CO N Y INC","RAVENSWOOD",0,"NAT GAS",4226,"0M",1294,,,95,209768,2234824,0,193780,1928735,0,161992,1747544,0,161776,1895581,0,200509,2260799,0,241862,2659354,0,377330,4132582,0,492580,5112387,0,269868,2872681,0,121326,1378858,0,190022,2065045,0,34903,408143,0,2500,6,50653,"NG","ST" 21,36,1,4,2,40,25,"CONSOL EDISON CO N Y INC","RAVENSWOOD",0,"LIGHT OIL",4226,"0M",1294,,,95,317,1144,40469,1114,3166,37304,412,1109,36195,1364,3752,32443,0,0,32613,292,765,31848,1020,2785,39004,707,2001,37003,43,116,38759,232,819,37940,91,256,37684,3105,8078,40525,2500,6,50653,"FO2","GT" 21,36,1,4,9,40,25,"CONSOL EDISON CO N Y INC","RAVENSWOOD",0,"NAT GAS",4226,"0M",1294,,,95,699,14506,0,461,7543,0,1614,25061,0,3849,61087,0,2639,36379,0,6191,93115,0,11215,178768,0,7292,120354,0,2766,43431,0,1873,38571,0,2782,45521,0,533,8123,0,2500,6,50653,"NG","GT" 21,36,1,2,3,40,30,"CONSOL EDISON CO N Y INC","74TH STREET",0,"HEAVY OIL",4226,"0M",1294,,,95,4001,11849,37330,7337,16422,1428,4042,7539,1190,6302,7774,1190,11192,14181,1190,8567,12004,1190,7521,9483,1190,3846,5472,1365,3937,4892,1428,-949,0,1429,3253,6242,1429,3602,5677,1429,2504,6,50653,"FO6","ST" 21,36,1,4,2,40,30,"CONSOL EDISON CO N Y INC","74TH STREET",0,"LIGHT OIL",4226,"0M",1294,,,95,-13,0,1690,-11,0,2143,-12,0,2083,-12,0,1952,-3,12,1881,-12,0,1762,-12,24,1738,-13,0,1747,-12,0,1548,-12,0,1524,-12,0,1595,-12,0,2202,2504,6,50653,"FO2","GT" 21,36,1,2,3,40,40,"CONSOL EDISON CO N Y INC","WATERSIDE",0,"HEAVY OIL",4226,"0M",1294,,,95,3119,5797,0,25178,41438,0,1003,1798,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,146,266,0,2502,6,50653,"FO6","ST" 21,36,1,2,9,40,40,"CONSOL EDISON CO N Y INC","WATERSIDE",0,"NAT GAS",4226,"0M",1294,,,95,59934,697096,0,47441,490868,0,53623,603408,0,39082,449151,0,37250,448243,0,36423,288224,0,55999,633276,0,55829,627391,0,38346,480259,0,35286,396996,0,48220,540897,0,63071,723341,0,2502,6,50653,"NG","ST" 21,36,1,2,3,40,50,"CONSOL EDISON CO N Y INC","OIL STORAGE",0,"HEAVY OIL",4226,"0M",1294,,,95,0,0,2766499,0,0,2324286,0,0,2545579,0,0,2254272,0,0,1899927,0,0,1649376,0,0,1484314,0,0,1332860,0,0,1420463,0,0,1532278,0,0,1814997,0,0,1473629,8801,6,50653,"FO6","ST" 21,36,1,4,2,40,60,"CONSOL EDISON CO N Y INC","OIL STORAGE",0,"LIGHT OIL",4226,"0M",1294,,,95,0,0,204071,0,0,265070,0,0,259969,0,0,242953,0,0,247234,0,0,245330,0,0,259288,0,0,251578,0,0,241219,0,0,257945,0,0,250930,0,0,243796,8802,6,50653,"FO2","GT" 21,36,1,4,2,40,65,"CONSOL EDISON CO N Y INC","BUCHANAN",0,"LIGHT OIL",4226,"0M",1294,,,95,55,213,3746,295,599,4326,12,22,4481,20,42,4440,199,586,4211,634,1857,4497,979,2573,4452,907,2783,4475,35,172,4303,63,247,4282,398,1093,4230,56,191,4039,4233,6,50653,"FO2","GT" 21,36,1,1,,49,5,"HYDRO DEV GROUP INC","DEXTER",0,,9145,"0A",1294,,,95,2082,0,0,1260,0,0,2412,0,0,1860,0,0,1134,0,0,690,0,0,834,0,0,558,0,0,666,0,0,1998,0,0,2619,0,0,1908,0,0,2505,6,50785,"WAT","HY" 21,36,1,1,,49,10,"HYDRO DEV GROUP INC","PYRITES #1",0,,9145,"0A",1294,,,95,228,0,0,53,0,0,337,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2506,6,50785,"WAT","HY" 21,36,1,1,,49,12,"HYDRO DEV GROUP INC","PYRITES #2",0,,9145,"0A",1294,,,95,2658,0,0,1453,0,0,3335,0,0,2856,0,0,2370,0,0,1044,0,0,630,0,0,678,0,0,606,0,0,2458,0,0,3186,0,0,2166,0,0,7031,6,50785,"WAT","HY" 21,36,1,1,,49,15,"HYDRO DEV GROUP INC","HAILESBORO",0,,9145,"0A",1294,,,95,1037,0,0,706,0,0,1087,0,0,1097,0,0,854,0,0,509,0,0,415,0,0,624,0,0,389,0,0,982,0,0,1159,0,0,780,0,0,6573,6,50785,"WAT","HY" 21,36,1,1,,49,20,"HYDRO DEV GROUP INC","FOWLER",0,,9145,"0A",1294,,,95,426,0,0,394,0,0,515,0,0,491,0,0,515,0,0,316,0,0,245,0,0,349,0,0,250,0,0,398,0,0,507,0,0,434,0,0,6572,6,50785,"WAT","HY" 21,36,1,1,,49,25,"HYDRO DEV GROUP INC","#6 MILL",0,,9145,"0A",1294,,,95,471,0,0,407,0,0,463,0,0,491,0,0,394,0,0,231,0,0,201,0,0,313,0,0,208,0,0,384,0,0,494,0,0,499,0,0,453,6,50785,"WAT","HY" 21,36,1,1,,49,50,"HYDRO DEV GROUP INC","COPENHAGEN",0,,9145,"0A",1294,,,95,1176,0,0,560,0,0,1460,0,0,1532,0,0,460,0,0,108,0,0,360,0,0,112,0,0,312,0,0,1396,0,0,1884,0,0,924,0,0,742,6,50785,"WAT","HY" 21,36,1,1,,49,55,"HYDRO DEV GROUP INC","DIAMOND IS",0,,9145,"0A",1294,,,95,665,0,0,468,0,0,733,0,0,702,0,0,504,0,0,251,0,0,228,0,0,190,0,0,239,0,0,583,0,0,773,0,0,616,0,0,2553,6,50785,"WAT","HY" 21,36,1,1,,49,60,"HYDRO DEV GROUP INC","THERESA",0,,9145,"0A",1294,,,95,752,0,0,606,0,0,800,0,0,836,0,0,556,0,0,150,0,0,78,0,0,202,0,0,34,0,0,710,0,0,842,0,0,794,0,0,2618,6,50785,"WAT","HY" 21,36,1,1,,49,70,"HYDRO DEV GROUP INC","#3 MILL",0,,9145,"0A",1294,,,95,456,0,0,350,0,0,485,0,0,483,0,0,398,0,0,240,0,0,157,0,0,294,0,0,180,0,0,283,0,0,456,0,0,346,0,0,743,6,50785,"WAT","HY" 21,36,1,1,,49,75,"HYDRO DEV GROUP INC","GOODYEAR LK",0,,9145,"0A",1294,,,95,640,0,0,400,0,0,757,0,0,542,0,0,315,0,0,166,0,0,49,0,0,25,0,0,19,0,0,171,0,0,575,0,0,550,0,0,7358,6,50785,"WAT","HY" 21,36,1,3,2,59,1,"FISHERS IS ELEC CORP (THE","FISHERS ISL",0,"LIGHT OIL",6369,"0A",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,6575,6,50989,"FO2","IC" 21,36,1,4,2,87,1,"LONG ISLAND LIGHTING CO","W BABYLON",0,"LIGHT OIL",11172,"0M",1294,,,95,-9,0,10978,184,398,10580,-10,0,10580,-8,0,10580,-10,0,10580,-10,0,10580,1589,3799,6781,1012,2525,9994,-8,0,9994,23,63,9931,12,52,9878,-6,0,9878,2521,6,51685,"FO2","GT" 21,36,1,2,2,87,2,"LONG ISLAND LIGHTING CO","E F BARRETT",0,"LIGHT OIL",11172,"0M",1294,,,95,0,0,382,0,0,382,0,0,382,0,0,382,0,0,382,0,0,382,0,0,382,0,0,382,189,351,31,0,0,31,0,0,0,0,0,0,2511,6,51685,"FO2","ST" 21,36,1,2,3,87,2,"LONG ISLAND LIGHTING CO","E F BARRETT",0,"HEAVY OIL",11172,"0M",1294,,,95,7679,13204,183912,19277,32691,151221,6888,12026,167809,7622,13054,154755,21364,35883,118872,5001,8521,110351,0,0,100351,0,0,150055,0,0,176621,0,0,176621,4499,7876,168745,30931,52133,130983,2511,6,51685,"FO6","ST" 21,36,1,2,9,87,2,"LONG ISLAND LIGHTING CO","E F BARRETT",0,"NAT GAS",11172,"0M",1294,,,95,88641,923891,0,72376,743992,0,119516,1265049,0,108791,1129535,0,161464,1644681,0,176300,1817157,0,201713,2124759,0,207176,2182914,0,194067,2023621,0,176719,1855067,0,152642,1622397,0,111293,1143313,0,2511,6,51685,"NG","ST" 21,36,1,4,2,87,2,"LONG ISLAND LIGHTING CO","E F BARRETT",0,"LIGHT OIL",11172,"0M",1294,,,95,0,0,21322,0,0,21322,0,0,21322,0,0,21322,0,0,21322,0,0,21322,0,0,21322,0,0,21322,0,0,21322,0,0,21322,0,0,21322,89,272,21050,2511,6,51685,"FO2","GT" 21,36,1,4,9,87,2,"LONG ISLAND LIGHTING CO","E F BARRETT",0,"NAT GAS",11172,"0M",1294,,,95,2584,48858,0,2455,39578,0,396,9580,0,7540,115964,0,15423,241318,0,13024,203027,0,13183,202506,0,13611,214090,0,2215,41056,0,3367,60239,0,3070,49795,0,1324,23100,0,2511,6,51685,"NG","GT" 21,36,1,2,3,87,5,"LONG ISLAND LIGHTING CO","FAR ROCKWAY",0,"HEAVY OIL",11172,"0M",1294,,,95,0,0,630,0,0,630,0,0,630,0,0,630,0,0,630,0,0,630,0,0,630,0,0,630,0,0,630,0,0,630,0,0,630,0,0,630,2513,6,51685,"FO6","ST" 21,36,1,2,9,87,5,"LONG ISLAND LIGHTING CO","FAR ROCKWAY",0,"NAT GAS",11172,"0M",1294,,,95,35652,370173,0,-382,0,0,37901,413154,0,47344,499677,0,39814,418408,0,43785,454694,0,44918,522402,0,46370,490439,0,46043,485717,0,32114,356625,0,40424,437203,0,48243,507731,0,2513,6,51685,"NG","ST" 21,36,1,2,3,87,15,"LONG ISLAND LIGHTING CO","GLENWOOD",0,"HEAVY OIL",11172,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2514,6,51685,"FO6","ST" 21,36,1,2,9,87,15,"LONG ISLAND LIGHTING CO","GLENWOOD",0,"NAT GAS",11172,"0M",1294,,,95,57152,656357,0,88875,989013,0,43090,513102,0,64609,758501,0,65972,764067,0,85437,987225,0,91585,1053103,0,91614,1044546,0,87436,984844,0,70615,831640,0,65930,771090,0,72860,814525,0,2514,6,51685,"NG","ST" 21,36,1,4,2,87,15,"LONG ISLAND LIGHTING CO","GLENWOOD",0,"LIGHT OIL",11172,"0M",1294,,,95,-13,0,28987,348,833,28155,-2,113,28042,-10,0,28042,-15,0,28042,308,112,27929,1020,3353,24576,1330,3635,20941,-16,0,20941,52,122,20819,-18,0,20787,-15,0,20787,2514,6,51685,"FO2","GT" 21,36,1,3,2,87,17,"LONG ISLAND LIGHTING CO","E HAMPTON",0,"LIGHT OIL",11172,"0M",1294,,,95,-6,0,971,33,69,902,-4,4,898,-6,0,898,-1,8,890,2,12,878,464,935,369,527,862,816,51,112,705,-6,0,705,-1,4,915,0,3,911,2512,6,51685,"FO2","IC" 21,36,1,4,2,87,17,"LONG ISLAND LIGHTING CO","E HAMPTON",0,"LIGHT OIL",11172,"0M",1294,,,95,-17,0,2876,-11,17,2859,-15,0,2859,-9,0,2859,-4,25,2834,34,116,2718,2330,5851,265,2246,5851,2259,76,212,2471,-10,0,2471,27,113,2789,-12,0,2789,2512,6,51685,"FO2","GT" 21,36,1,4,2,87,18,"LONG ISLAND LIGHTING CO","SOUTHOLD",0,"LIGHT OIL",11172,"0M",1294,,,95,-8,0,2716,-15,0,2716,-15,0,2716,-11,0,2716,-9,0,2716,14,79,2637,79,316,2534,39,174,2784,-8,0,2784,-8,0,2784,33,160,2624,-15,0,2624,2520,6,51685,"FO2","GT" 21,36,1,2,2,87,21,"LONG ISLAND LIGHTING CO","NORTHPORT",0,"LIGHT OIL",11172,"0M",1294,,,95,393,703,2446,1919,3360,10568,787,1448,10918,244,438,10694,0,0,10694,1255,2346,10708,543,987,10787,859,1604,10653,1224,1286,10857,0,0,11070,42,78,10992,866,1558,10948,2516,6,51685,"FO2","ST" 21,36,1,2,3,87,21,"LONG ISLAND LIGHTING CO","NORTHPORT",0,"HEAVY OIL",11172,"0M",1294,,,95,251839,410183,917940,419721,669714,545119,137170,230153,627264,93546,156459,751601,4614,7948,743653,138528,235371,730114,232571,387065,831393,198326,339587,780654,65679,111985,948390,0,0,1048629,13006,22156,1026473,263245,435054,787488,2516,6,51685,"FO6","ST" 21,36,1,2,9,87,21,"LONG ISLAND LIGHTING CO","NORTHPORT",0,"NAT GAS",11172,"0M",1294,,,95,161173,1656185,0,109357,1099738,0,179917,1902183,0,179876,1858552,0,249772,2620522,0,277680,2980882,0,392501,4094975,0,395601,4243388,0,332956,3533654,0,339896,3613412,0,310631,3313635,0,259449,2673147,0,2516,6,51685,"NG","ST" 21,36,1,4,2,87,21,"LONG ISLAND LIGHTING CO","NORTHPORT",0,"LIGHT OIL",11172,"0M",1294,,,95,-16,0,2030,-16,0,2030,11,87,1943,-13,0,1943,-12,0,1943,-8,15,1928,10,25,1904,24,175,1729,-2,17,1712,-7,0,0,-15,0,1290,-10,0,1506,2516,6,51685,"FO2","GT" 21,36,1,3,2,87,23,"LONG ISLAND LIGHTING CO","SHOREHAM",0,"LIGHT OIL",11172,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2518,6,51685,"FO2","IC" 21,36,1,4,2,87,23,"LONG ISLAND LIGHTING CO","SHOREHAM",0,"LIGHT OIL",11172,"0M",1294,,,95,-4,0,10375,81,259,11414,11,38,11377,-7,0,11377,340,528,10848,91,128,10720,441,1417,9303,551,846,15679,5,41,15638,18,32,15605,-4,0,15605,-7,3,15602,2518,6,51685,"FO2","GT" 21,36,1,2,2,87,24,"LONG ISLAND LIGHTING CO","P JEFFERSON",0,"LIGHT OIL",11172,"0M",1294,,,95,505,940,248,368,651,173,451,865,267,430,769,71,340,624,210,273,507,271,308,573,265,205,379,265,120,230,224,260,511,310,181,337,162,173,317,229,2517,6,51685,"FO2","ST" 21,36,1,2,3,87,24,"LONG ISLAND LIGHTING CO","P JEFFERSON",0,"HEAVY OIL",11172,"0M",1294,,,95,83231,142447,374658,116002,187180,292517,84682,149701,363973,88134,146337,217636,86246,147673,240914,86540,147162,367784,119762,202643,388397,116504,197519,283029,62653,110443,267311,37059,67418,404544,57551,98596,305948,73017,122780,291514,2517,6,51685,"FO6","ST" 21,36,1,4,2,87,24,"LONG ISLAND LIGHTING CO","P JEFFERSON",0,"LIGHT OIL",11172,"0M",1294,,,95,14,70,2055,36,150,1905,-16,0,1905,-11,0,1905,30,100,1805,15,79,1726,94,282,1444,49,175,2118,-8,0,2118,2,49,2069,-12,0,2069,-14,0,2069,2517,6,51685,"FO2","GT" 21,36,1,4,2,87,26,"LONG ISLAND LIGHTING CO","SOUTHAMPTON",0,"LIGHT OIL",11172,"0M",1294,,,95,-16,0,2575,22,137,2438,-17,0,2438,-9,0,2438,-4,9,2430,36,153,2277,200,649,2266,170,698,2628,-11,0,2628,-8,0,2628,-2,0,2628,-18,0,2628,2519,6,51685,"FO2","GT" 21,36,1,3,2,87,29,"LONG ISLAND LIGHTING CO","MONTAUK",0,"LIGHT OIL",11172,"0M",1294,,,95,-6,0,685,34,66,619,-6,0,619,-6,0,619,0,0,619,2,46,572,274,574,424,184,319,529,57,109,420,-6,0,420,0,23,611,-6,0,611,2515,6,51685,"FO2","IC" 21,36,1,4,2,87,30,"LONG ISLAND LIGHTING CO","HOLTSVILLE",0,"LIGHT OIL",11172,"0M",1294,,,95,3418,7966,65483,2730,6945,98989,1349,3183,95807,3573,8991,86815,1220,3009,83806,4957,12317,71489,13538,28073,71475,15481,41712,89159,785,2396,86763,-94,234,86529,427,1487,85042,2296,5778,79264,8007,6,51685,"FO2","GT" 21,36,1,4,2,87,35,"LONG ISLAND LIGHTING CO","BROOKHAVEN",0,"LIGHT OIL",11172,"0M",1294,,,95,2290,4982,38416,2652,6010,38901,226,279,38622,3165,6704,37310,6210,13571,28376,6235,12488,40846,9816,21210,30472,9736,19194,39142,-52,0,39142,113,688,40071,528,1470,40751,2660,5996,37572,7146,6,51685,"FO2","GT" 21,36,1,1,,100,1,"N Y STATE ELEC & GAS CORP","CADYVILLE",0,,13511,"0M",1294,,,95,2289,0,0,1760,0,0,2697,0,0,2249,0,0,2033,0,0,1277,0,0,1043,0,0,1271,0,0,873,0,0,1835,0,0,2411,0,0,1256,0,0,2522,6,52036,"WAT","HY" 21,36,1,1,,100,3,"N Y STATE ELEC & GAS CORP","MILL 'C'",0,,13511,"0M",1294,,,95,1082,0,0,1120,0,0,1325,0,0,1217,0,0,1424,0,0,918,2,0,782,0,0,1153,0,0,591,0,0,1982,0,0,2696,0,0,728,0,0,6486,6,52036,"WAT","HY" 21,36,1,1,,100,8,"N Y STATE ELEC & GAS CORP","HIGH FALLS",0,,13511,"0M",1294,,,95,8036,0,0,6467,0,0,9348,0,0,7548,0,0,6945,0,0,4111,0,0,3127,0,0,4402,0,0,2270,0,0,1885,0,0,8998,0,0,6023,0,0,2530,6,52036,"WAT","HY" 21,36,1,1,,100,9,"N Y STATE ELEC & GAS CORP","KENT FALLS",0,,13511,"0M",1294,,,95,4267,0,0,3614,0,0,5729,0,0,4500,0,0,4403,0,0,2459,0,0,1821,0,0,2011,0,0,1112,0,0,2429,0,0,0,0,0,2462,0,0,2532,6,52036,"WAT","HY" 21,36,1,1,,100,11,"N Y STATE ELEC & GAS CORP","KEUKA",0,,13511,"0M",1294,,,95,479,0,0,618,0,0,1104,0,0,424,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,246,0,0,368,0,0,87,0,0,2533,6,52036,"WAT","HY" 21,36,1,1,,100,18,"N Y STATE ELEC & GAS CORP","RAINBOW FLS",0,,13511,"0M",1294,,,95,844,0,0,484,0,0,1136,0,0,1424,0,0,2008,0,0,1044,0,0,972,0,0,828,0,0,572,0,0,920,0,0,1432,0,0,800,0,0,6526,6,52036,"WAT","HY" 21,36,1,1,,100,20,"N Y STATE ELEC & GAS CORP","SENECA FLS",0,,13511,"0M",1294,,,95,929,0,0,0,0,0,237,0,0,418,0,0,57,0,0,12,0,0,35,0,0,0,0,0,0,0,0,144,0,0,1097,0,0,1515,0,0,6525,6,52036,"WAT","HY" 21,36,1,1,,100,26,"N Y STATE ELEC & GAS CORP","WATERLOO",0,,13511,"0M",1294,,,95,218,0,0,0,0,0,91,0,0,167,0,0,47,0,0,38,0,0,63,0,0,15,0,0,0,0,0,28,0,0,273,0,0,435,0,0,2538,6,52036,"WAT","HY" 21,36,1,2,2,100,28,"N Y STATE ELEC & GAS CORP","GOUDEY",0,"LIGHT OIL",13511,"0M",1294,,,95,4,6,902,7,12,922,38,860,816,166,1093,889,115,412,787,23,40,755,14,25,726,19,34,1012,88,159,674,17,29,652,15,27,781,57,99,755,2526,6,52036,"FO2","ST" 21,36,1,2,6,100,28,"N Y STATE ELEC & GAS CORP","GOUDEY",0,"BIT COAL",13511,"0M",1294,,,95,49140,18404,38386,47957,17309,33487,38535,14154,31196,29944,11570,19706,47570,19243,17396,46082,17833,16951,48114,18609,8401,48907,19270,14458,47509,18547,11816,46734,17563,21803,47743,17962,29205,49938,18814,16951,2526,6,52036,"BIT","ST" 21,36,1,2,2,100,30,"N Y STATE ELEC & GAS CORP","GREENIDGE",0,"LIGHT OIL",13511,"0M",1294,,,95,49,84,1482,143,249,1673,49,85,1663,69,118,1503,97,194,1276,101,268,963,140,255,1024,312,565,929,134,232,1184,28,65,1082,27,47,1003,135,254,963,2527,6,52036,"FO2","ST" 21,36,1,2,6,100,30,"N Y STATE ELEC & GAS CORP","GREENIDGE",0,"BIT COAL",13511,"0M",1294,,,95,59064,22369,46139,64896,24628,34337,56536,21560,33567,61588,23327,27754,60141,23147,16512,44718,17812,44179,56844,23346,35975,63282,25535,39483,33115,12718,51031,52461,19935,48906,51733,19814,48981,79778,32545,44179,2527,6,52036,"BIT","ST" 21,36,1,2,6,100,32,"N Y STATE ELEC & GAS CORP","HICKLING",0,"BIT COAL",13511,"0M",1294,,,95,29937,25353,59845,37278,28317,42388,31428,24287,26231,36848,29367,9739,25540,20965,7417,26619,21486,11619,19927,15033,13417,19292,17747,12211,16109,14260,19398,15799,13125,25995,15584,11444,38506,16518,14020,11619,2529,6,52036,"BIT","ST" 21,36,1,2,"B",100,34,"N Y STATE ELEC & GAS CORP","JENNISON",0,"WOOD CHIP",13511,"0M",1294,,,95,1937,0,0,2506,0,0,1706,0,0,446,0,0,510,0,0,631,0,0,0,0,0,966,0,0,1443,0,0,1357,0,0,215,0,0,517,0,0,2531,6,52036,"WOD","ST" 21,36,1,2,6,100,34,"N Y STATE ELEC & GAS CORP","JENNISON",0,"BIT COAL",13511,"0M",1294,,,95,18813,12027,31771,27918,18374,13300,18598,13682,9272,12405,9568,1166,10568,8258,1035,8066,6810,737,10639,7167,2889,9803,7780,5121,7664,6371,9926,7104,5362,9933,11173,7198,8195,18436,12369,737,2531,6,52036,"BIT","ST" 21,36,1,2,2,100,35,"N Y STATE ELEC & GAS CORP","MILLIKEN",0,"LIGHT OIL",13511,"0M",1294,,,95,206,337,1812,188,320,1856,273,465,1873,142,244,1879,53,94,1978,249,452,1841,116,209,1815,158,288,1863,211,385,1831,258,462,1670,59,105,1738,26,47,1841,2535,6,52036,"FO2","ST" 21,36,1,2,6,100,35,"N Y STATE ELEC & GAS CORP","MILLIKEN",0,"BIT COAL",13511,"0M",1294,,,95,192258,68792,79141,180255,67185,80127,183681,68408,89806,153861,58397,69230,98273,37927,98714,132074,52498,118633,185234,73165,90889,184163,73756,101056,131693,53020,97110,185372,73940,102961,167135,65625,99048,191784,76075,118633,2535,6,52036,"BIT","ST" 21,36,1,3,2,100,35,"N Y STATE ELEC & GAS CORP","MILLIKEN",0,"LIGHT OIL",13511,"0M",1294,,,95,0,1,0,20,38,0,3,84,0,104,107,0,54,144,0,1,38,0,-64,39,0,10,20,0,0,1,0,12,39,0,11,44,0,17,32,0,2535,6,52036,"FO2","IC" 21,36,1,3,2,100,40,"N Y STATE ELEC & GAS CORP","HARRIS LAKE",0,"LIGHT OIL",13511,"0M",1294,,,95,-11,0,405,0,0,349,0,0,0,-4,0,313,0,0,260,0,0,242,64,122,269,12,25,244,2,0,436,0,0,357,0,0,290,-13,0,242,2528,6,52036,"FO2","IC" 21,36,1,1,,100,43,"N Y STATE ELEC & GAS CORP","MECHANICVLE",0,,13511,"0M",1294,,,95,9072,0,0,6867,0,0,9702,0,0,6867,0,0,4347,0,0,2961,0,0,1134,0,0,2331,0,0,1953,0,0,5670,0,0,12663,0,0,8946,0,0,625,6,52036,"WAT","HY" 21,36,1,2,2,100,50,"N Y STATE ELEC & GAS CORP","KINTIGH",0,"LIGHT OIL",13511,"0M",1294,,,95,219,378,4169,770,1322,2904,474,811,3335,953,1656,3113,165,283,2839,314,543,2288,879,1523,3426,394,685,2738,627,1087,4124,1183,2162,2118,626,1094,4657,509,873,2288,6082,6,52036,"FO2","ST" 21,36,1,2,6,100,50,"N Y STATE ELEC & GAS CORP","KINTIGH",0,"BIT COAL",13511,"0M",1294,,,95,429496,166336,132032,393694,148405,142690,419527,160683,178911,416807,160659,178855,418612,159916,174957,381565,146069,162034,348178,133246,124345,413546,158604,73112,376458,141570,75380,181079,73253,130474,363691,142233,133771,423315,159637,162034,6082,6,52036,"BIT","ST" 21,36,1,2,1,105,1,"NIAGARA MOHAWK POWER CORP","NINE MILE P",0,"NUCLEAR",13573,"0M",1294,,190,95,368414,0,0,58742,0,0,0,0,0,332154,0,0,459193,0,0,439571,0,0,434942,0,0,437261,0,0,420930,0,0,452099,0,0,441551,0,0,459844,0,0,2589,6,52053,"UR","ST" 21,36,1,2,1,105,2,"NIAGARA MOHAWK POWER CORP","NINE MILE P",0,"NUCLEAR",13573,"0M",1294,,190,95,694823,0,0,533574,0,0,742888,0,0,149501,0,0,0,0,0,575400,0,0,821880,0,0,766368,0,0,443850,0,0,845303,0,0,824493,0,0,841323,0,0,2589,6,52053,"UR","ST" 21,36,1,1,,105,5,"NIAGARA MOHAWK POWER CORP","ALLENS FLS",0,,13573,"0M",1294,,190,95,2087,0,0,1758,0,0,2479,0,0,2662,0,0,2344,0,0,1289,0,0,1268,0,0,1240,0,0,1099,0,0,2308,0,0,2305,0,0,2092,0,0,2540,6,52053,"WAT","HY" 21,36,1,1,,105,10,"NIAGARA MOHAWK POWER CORP","BALDWINSVLE",0,,13573,"0M",1294,,190,95,205,0,0,112,0,0,221,0,0,171,0,0,60,0,0,7,0,0,-3,0,0,16,0,0,1,0,0,57,0,0,217,0,0,140,0,0,2542,6,52053,"WAT","HY" 21,36,1,1,,105,15,"NIAGARA MOHAWK POWER CORP","BELFORT",0,,13573,"0M",1294,,190,95,861,0,0,751,0,0,805,0,0,464,0,0,550,0,0,561,0,0,714,0,0,764,0,0,730,0,0,557,0,0,1171,0,0,1354,0,0,2544,6,52053,"WAT","HY" 21,36,1,1,,105,20,"NIAGARA MOHAWK POWER CORP","BENNETTS B",0,,13573,"0M",1294,,190,95,10231,0,0,5759,0,0,9838,0,0,5346,0,0,4404,0,0,1938,0,0,-33,0,0,313,0,0,5443,0,0,9001,0,0,13335,0,0,6313,0,0,2545,6,52053,"WAT","HY" 21,36,1,1,,105,25,"NIAGARA MOHAWK POWER CORP","BLACK RIVER",0,,13573,"0M",1294,,190,95,3477,0,0,2422,0,0,3823,0,0,3907,0,0,2562,0,0,1270,0,0,1501,0,0,948,0,0,1559,0,0,3563,0,0,4456,0,0,3477,0,0,2546,6,52053,"WAT","HY" 21,36,1,1,,105,30,"NIAGARA MOHAWK POWER CORP","BLAKE",0,,13573,"0M",1294,,190,95,6604,0,0,6486,0,0,5072,0,0,2962,0,0,3721,0,0,3715,0,0,672,0,0,2828,0,0,1682,0,0,3534,0,0,9144,0,0,6300,0,0,2547,6,52053,"WAT","HY" 21,36,1,1,,105,35,"NIAGARA MOHAWK POWER CORP","BROWNS FLS",0,,13573,"0M",1294,,190,95,6785,0,0,3738,0,0,4510,0,0,1724,0,0,1746,0,0,1866,0,0,545,0,0,2901,0,0,1160,0,0,4896,0,0,7492,0,0,3767,0,0,2548,6,52053,"WAT","HY" 21,36,1,1,,105,40,"NIAGARA MOHAWK POWER CORP","CHASM",0,,13573,"0M",1294,,190,95,1902,0,0,1138,0,0,1426,0,0,1777,0,0,1751,0,0,1323,0,0,994,0,0,1236,0,0,1014,0,0,1752,0,0,1795,0,0,1489,0,0,2550,6,52053,"WAT","HY" 21,36,1,1,,105,45,"NIAGARA MOHAWK POWER CORP","COLTON",0,,13573,"0M",1294,,190,95,20600,0,0,18761,0,0,20043,0,0,13701,0,0,15937,0,0,15548,0,0,9456,0,0,14510,0,0,7469,0,0,15049,0,0,2073,0,0,19935,0,0,2551,6,52053,"WAT","HY" 21,36,1,1,,105,50,"NIAGARA MOHAWK POWER CORP","DEFERIET",0,,13573,"0M",1294,,190,95,4478,0,0,3495,0,0,5869,0,0,5234,0,0,3642,0,0,1740,0,0,1638,0,0,1204,0,0,1248,0,0,5355,0,0,7027,0,0,4656,0,0,2552,6,52053,"WAT","HY" 21,36,1,1,,105,65,"NIAGARA MOHAWK POWER CORP","EAGLE",0,,13573,"0M",1294,,190,95,2653,0,0,2021,0,0,2505,0,0,1200,0,0,1421,0,0,1737,0,0,2331,0,0,1979,0,0,2045,0,0,1398,0,0,3203,0,0,3777,0,0,2555,6,52053,"WAT","HY" 21,36,1,1,,105,70,"NIAGARA MOHAWK POWER CORP","EEL WEIR",0,,13573,"0M",1294,,190,95,866,0,0,622,0,0,964,0,0,803,0,0,524,0,0,203,0,0,115,0,0,125,0,0,7,0,0,655,0,0,1332,0,0,994,0,0,2556,6,52053,"WAT","HY" 21,36,1,1,,105,75,"NIAGARA MOHAWK POWER CORP","EFFLEY",0,,13573,"0M",1294,,190,95,1093,0,0,986,0,0,1153,0,0,580,0,0,694,0,0,845,0,0,905,0,0,982,0,0,900,0,0,740,0,0,1558,0,0,1767,0,0,2557,6,52053,"WAT","HY" 21,36,1,1,,105,80,"NIAGARA MOHAWK POWER CORP","ELMER",0,,13573,"0M",1294,,190,95,812,0,0,575,0,0,796,0,0,380,0,0,439,0,0,552,0,0,441,0,0,640,0,0,593,0,0,496,0,0,1010,0,0,1135,0,0,2559,6,52053,"WAT","HY" 21,36,1,1,,105,85,"NIAGARA MOHAWK POWER CORP","ET NORFOLK",0,,13573,"0M",1294,,190,95,2479,0,0,1995,0,0,2559,0,0,1703,0,0,1975,0,0,1859,0,0,1059,0,0,1731,0,0,851,0,0,1883,0,0,2471,0,0,2519,0,0,2561,6,52053,"WAT","HY" 21,36,1,1,,105,90,"NIAGARA MOHAWK POWER CORP","FIVE FALLS",0,,13573,"0M",1294,,190,95,10795,0,0,10405,0,0,8347,0,0,4782,0,0,5926,0,0,5896,0,0,3396,0,0,5619,0,0,2631,0,0,5807,0,0,14654,0,0,10198,0,0,2562,6,52053,"WAT","HY" 21,36,1,1,,105,95,"NIAGARA MOHAWK POWER CORP","FLAT ROCK",0,,13573,"0M",1294,,190,95,1503,0,0,871,0,0,1489,0,0,592,0,0,450,0,0,401,0,0,136,0,0,528,0,0,169,0,0,1414,0,0,1912,0,0,876,0,0,2563,6,52053,"WAT","HY" 21,36,1,1,,105,98,"NIAGARA MOHAWK POWER CORP","FRANKLIN F",0,,13573,"0M",1294,,190,95,775,0,0,767,0,0,1052,0,0,613,0,0,385,0,0,496,0,0,336,0,0,352,0,0,-1,0,0,-1,0,0,-1,0,0,-1,0,0,2564,6,52053,"WAT","HY" 21,36,1,1,,105,100,"NIAGARA MOHAWK POWER CORP","FULTON",0,,13573,"0M",1294,,190,95,464,0,0,333,0,0,608,0,0,437,0,0,459,0,0,300,0,0,406,0,0,363,0,0,304,0,0,474,0,0,653,0,0,625,0,0,2566,6,52053,"WAT","HY" 21,36,1,1,,105,105,"NIAGARA MOHAWK POWER CORP","GRANBY",0,,13573,"0M",1294,,190,95,5845,0,0,3502,0,0,6558,0,0,1324,0,0,640,0,0,477,0,0,-38,0,0,491,0,0,-42,0,0,3025,0,0,5404,0,0,5157,0,0,2569,6,52053,"WAT","HY" 21,36,1,1,,105,110,"NIAGARA MOHAWK POWER CORP","HANNAWA",0,,13573,"0M",1294,,190,95,5253,0,0,4772,0,0,5248,0,0,3332,0,0,4051,0,0,3941,0,0,2329,0,0,3797,0,0,1747,0,0,1086,0,0,2696,0,0,5321,0,0,2571,6,52053,"WAT","HY" 21,36,1,1,,105,115,"NIAGARA MOHAWK POWER CORP","HERRINGS",0,,13573,"0M",1294,,190,95,1980,0,0,1586,0,0,2151,0,0,2116,0,0,1509,0,0,629,0,0,705,0,0,371,0,0,337,0,0,1747,0,0,2341,0,0,2187,0,0,2572,6,52053,"WAT","HY" 21,36,1,1,,105,120,"NIAGARA MOHAWK POWER CORP","HEUVELTON",0,,13573,"0M",1294,,190,95,458,0,0,468,0,0,484,0,0,556,0,0,455,0,0,254,0,0,195,0,0,277,0,0,149,0,0,433,0,0,506,0,0,588,0,0,2573,6,52053,"WAT","HY" 21,36,1,1,,105,125,"NIAGARA MOHAWK POWER CORP","HIGH DAM 6",0,,13573,"0M",1294,,190,95,0,0,0,0,0,0,1863,0,0,2023,0,0,1494,0,0,922,0,0,725,0,0,989,0,0,179,0,0,2024,0,0,2607,0,0,3766,0,0,2574,6,52053,"WAT","HY" 21,36,1,1,,105,126,"NIAGARA MOHAWK POWER CORP","HIGH FALLS",0,,13573,"0M",1294,,190,95,2622,0,0,1900,0,0,2648,0,0,1268,0,0,1439,0,0,1814,0,0,2106,0,0,1998,0,0,1847,0,0,1571,0,0,3045,0,0,3527,0,0,2575,6,52053,"WAT","HY" 21,36,1,1,,105,130,"NIAGARA MOHAWK POWER CORP","HIGLEY",0,,13573,"0M",1294,,190,95,3414,0,0,2999,0,0,3075,0,0,1774,0,0,2177,0,0,2037,0,0,1416,0,0,2086,0,0,1120,0,0,2315,0,0,3556,0,0,3242,0,0,2576,6,52053,"WAT","HY" 21,36,1,1,,105,135,"NIAGARA MOHAWK POWER CORP","HOGANSBURG",0,,13573,"0M",1294,,190,95,98,0,0,143,0,0,192,0,0,192,0,0,148,0,0,129,0,0,87,0,0,146,0,0,79,0,0,113,0,0,186,0,0,218,0,0,2577,6,52053,"WAT","HY" 21,36,1,1,,105,140,"NIAGARA MOHAWK POWER CORP","KAMARGO",0,,13573,"0M",1294,,190,95,2374,0,0,1857,0,0,2750,0,0,2638,0,0,1924,0,0,960,0,0,1034,0,0,398,0,0,612,0,0,2497,0,0,3433,0,0,1788,0,0,2581,6,52053,"WAT","HY" 21,36,1,1,,105,145,"NIAGARA MOHAWK POWER CORP","LIGHTHOUSE",0,,13573,"0M",1294,,190,95,2431,0,0,1342,0,0,2514,0,0,1178,0,0,925,0,0,399,0,0,-14,0,0,-14,0,0,1080,0,0,1999,0,0,3282,0,0,1507,0,0,2582,6,52053,"WAT","HY" 21,36,1,1,,105,155,"NIAGARA MOHAWK POWER CORP","MACOMB",0,,13573,"0M",1294,,190,95,434,0,0,398,0,0,641,0,0,569,0,0,481,0,0,319,0,0,-4,0,0,-4,0,0,132,0,0,534,0,0,627,0,0,520,0,0,2583,6,52053,"WAT","HY" 21,36,1,1,,105,160,"NIAGARA MOHAWK POWER CORP","MINETTO",0,,13573,"0M",1294,,190,95,3847,0,0,2604,0,0,4467,0,0,2022,0,0,1607,0,0,940,0,0,602,0,0,800,0,0,427,0,0,1690,0,0,4151,0,0,4554,0,0,2586,6,52053,"WAT","HY" 21,36,1,1,,105,165,"NIAGARA MOHAWK POWER CORP","MOSHIER",0,,13573,"0M",1294,,190,95,2698,0,0,2561,0,0,2447,0,0,1064,0,0,1751,0,0,2554,0,0,2993,0,0,2896,0,0,2791,0,0,736,0,0,3994,0,0,5506,0,0,2588,6,52053,"WAT","HY" 21,36,1,1,,105,170,"NIAGARA MOHAWK POWER CORP","NORFOLK",0,,13573,"0M",1294,,190,95,2391,0,0,2156,0,0,2979,0,0,1872,0,0,2207,0,0,2139,0,0,1223,0,0,2018,0,0,958,0,0,2054,0,0,3088,0,0,2630,0,0,2590,6,52053,"WAT","HY" 21,36,1,1,,105,175,"NIAGARA MOHAWK POWER CORP","NORWOOD",0,,13573,"0M",1294,,190,95,1536,0,0,1408,0,0,1536,0,0,938,0,0,1146,0,0,1136,0,0,605,0,0,1104,0,0,480,0,0,1072,0,0,1232,0,0,1488,0,0,2591,6,52053,"WAT","HY" 21,36,1,1,,105,180,"NIAGARA MOHAWK POWER CORP","OSWEGATCHIE",0,,13573,"0M",1294,,190,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2593,6,52053,"WAT","HY" 21,36,1,1,,105,182,"NIAGARA MOHAWK POWER CORP","OSWEGO FL E",0,,13573,"0M",1294,,190,95,2890,0,0,2449,0,0,2510,0,0,1688,0,0,1604,0,0,996,0,0,637,0,0,679,0,0,550,0,0,1991,0,0,2836,0,0,2816,0,0,2595,6,52053,"WAT","HY" 21,36,1,1,,105,183,"NIAGARA MOHAWK POWER CORP","OSWEGO FL W",0,,13573,"0M",1294,,190,95,1223,0,0,423,0,0,1212,0,0,176,0,0,-1,0,0,28,0,0,-2,0,0,47,0,0,14,0,0,385,0,0,730,0,0,1172,0,0,2596,6,52053,"WAT","HY" 21,36,1,1,,105,185,"NIAGARA MOHAWK POWER CORP","PARISHVILLE",0,,13573,"0M",1294,,190,95,0,0,0,690,0,0,1562,0,0,1603,0,0,1516,0,0,848,0,0,849,0,0,763,0,0,749,0,0,1395,0,0,1488,0,0,1298,0,0,2597,6,52053,"WAT","HY" 21,36,1,1,,105,187,"NIAGARA MOHAWK POWER CORP","PIERCEFIELD",0,,13573,"0M",1294,,190,95,1488,0,0,1283,0,0,1529,0,0,1482,0,0,1341,0,0,627,0,0,429,0,0,881,0,0,370,0,0,1195,0,0,1783,0,0,1527,0,0,2598,6,52053,"WAT","HY" 21,36,1,1,,105,192,"NIAGARA MOHAWK POWER CORP","PROSPECT",0,,13573,"0M",1294,,190,95,1704,0,0,0,0,0,4257,0,0,5788,0,0,3672,0,0,2881,0,0,2386,0,0,1689,0,0,184,0,0,6691,0,0,11309,0,0,6904,0,0,2599,6,52053,"WAT","HY" 21,36,1,1,,105,195,"NIAGARA MOHAWK POWER CORP","RAINBOW",0,,13573,"0M",1294,,190,95,10771,0,0,10270,0,0,8298,0,0,4779,0,0,5959,0,0,5843,0,0,3452,0,0,5583,0,0,2641,0,0,5774,0,0,14120,0,0,9950,0,0,2600,6,52053,"WAT","HY" 21,36,1,1,,105,200,"NIAGARA MOHAWK POWER CORP","RAYMONDVLE",0,,13573,"0M",1294,,190,95,932,0,0,816,0,0,1452,0,0,926,0,0,670,0,0,1102,0,0,674,0,0,1036,0,0,530,0,0,1056,0,0,1404,0,0,1120,0,0,2601,6,52053,"WAT","HY" 21,36,1,1,,105,210,"NIAGARA MOHAWK POWER CORP","S EDWARDS",0,,13573,"0M",1294,,190,95,1404,0,0,1076,0,0,1387,0,0,973,0,0,1018,0,0,736,0,0,427,0,0,1020,0,0,558,0,0,1359,0,0,1919,0,0,1392,0,0,2604,6,52053,"WAT","HY" 21,36,1,1,,105,215,"NIAGARA MOHAWK POWER CORP","SEWALLS",0,,13573,"0M",1294,,190,95,1372,0,0,889,0,0,1518,0,0,1486,0,0,1205,0,0,544,0,0,246,0,0,320,0,0,319,0,0,1211,0,0,1489,0,0,1514,0,0,2608,6,52053,"WAT","HY" 21,36,1,1,,105,220,"NIAGARA MOHAWK POWER CORP","SOFT MAPLE",0,,13573,"0M",1294,,190,95,2633,0,0,1616,0,0,2359,0,0,882,0,0,1236,0,0,1714,0,0,2341,0,0,1918,0,0,1850,0,0,1760,0,0,3432,0,0,4125,0,0,2610,6,52053,"WAT","HY" 21,36,1,1,,105,225,"NIAGARA MOHAWK POWER CORP","SOTH COLTON",0,,13573,"0M",1294,,190,95,8860,0,0,8292,0,0,6906,0,0,3510,0,0,4607,0,0,4842,0,0,2861,0,0,4595,0,0,2211,0,0,4731,0,0,12247,0,0,8305,0,0,2611,6,52053,"WAT","HY" 21,36,1,1,,105,230,"NIAGARA MOHAWK POWER CORP","STARK",0,,13573,"0M",1294,,190,95,10035,0,0,10162,0,0,7531,0,0,4401,0,0,5629,0,0,5788,0,0,3281,0,0,5363,0,0,2475,0,0,5187,0,0,14852,0,0,9960,0,0,2613,6,52053,"WAT","HY" 21,36,1,1,,105,235,"NIAGARA MOHAWK POWER CORP","SUGAR IS",0,,13573,"0M",1294,,190,95,2908,0,0,2519,0,0,2995,0,0,2818,0,0,2884,0,0,2757,0,0,1893,0,0,2754,0,0,1376,0,0,2667,0,0,2781,0,0,2983,0,0,2616,6,52053,"WAT","HY" 21,36,1,1,,105,240,"NIAGARA MOHAWK POWER CORP","TAYLORVILLE",0,,13573,"0M",1294,,190,95,2219,0,0,1663,0,0,2176,0,0,1051,0,0,1247,0,0,1560,0,0,1566,0,0,1692,0,0,1630,0,0,1392,0,0,2700,0,0,3109,0,0,2617,6,52053,"WAT","HY" 21,36,1,1,,105,250,"NIAGARA MOHAWK POWER CORP","TRENTON",0,,13573,"0M",1294,,190,95,12363,0,0,10763,0,0,12685,0,0,10309,0,0,6711,0,0,6004,0,0,5262,0,0,4565,0,0,3995,0,0,8295,0,0,14603,0,0,11617,0,0,2619,6,52053,"WAT","HY" 21,36,1,1,,105,255,"NIAGARA MOHAWK POWER CORP","VARICK",0,,13573,"0M",1294,,190,95,3510,0,0,2348,0,0,3552,0,0,1467,0,0,836,0,0,546,0,0,363,0,0,629,0,0,211,0,0,2344,0,0,3490,0,0,3553,0,0,2621,6,52053,"WAT","HY" 21,36,1,1,,105,265,"NIAGARA MOHAWK POWER CORP","YALEVILLE",0,,13573,"0M",1294,,190,95,293,0,0,255,0,0,406,0,0,320,0,0,373,0,0,341,0,0,243,0,0,407,0,0,242,0,0,346,0,0,275,0,0,248,0,0,2624,6,52053,"WAT","HY" 21,36,1,3,2,105,270,"NIAGARA MOHAWK POWER CORP","NINE MILE P",0,"LIGHT OIL",13573,"0M",1294,,190,95,6,136,4435,3,121,4470,11,87,4380,0,100,4256,13,323,4316,10,36,4349,6,164,4288,7,218,4320,6,11,535,6,12,573,6,13,557,6,12,543,2589,6,52053,"FO2","IC" 21,36,1,2,3,105,275,"NIAGARA MOHAWK POWER CORP","OSWEGO",0,"HEAVY OIL",13573,"0M",1294,,190,95,0,0,632933,120407,215553,417380,0,0,417380,26504,46741,370639,0,0,370639,1371,4130,366508,44092,30232,330715,13690,33269,298197,9883,21973,276183,0,0,276183,0,0,542213,0,0,542213,2594,6,52053,"FO6","ST" 21,36,1,2,9,105,275,"NIAGARA MOHAWK POWER CORP","OSWEGO",0,"NAT GAS",13573,"0M",1294,,190,95,999,22854,0,10635,117884,0,0,0,0,0,0,0,0,0,0,0,0,0,108,461,0,38513,570000,0,15497,213000,0,0,0,0,0,0,0,0,0,0,2594,6,52053,"NG","ST" 21,36,1,3,2,105,275,"NIAGARA MOHAWK POWER CORP","OSWEGO",0,"LIGHT OIL",13573,"0M",1294,,190,95,0,0,2149,0,0,2149,0,0,2149,0,0,2149,0,0,2149,0,0,2149,0,0,2149,0,0,2149,4,11,2138,0,0,2138,0,0,2138,0,0,2138,2594,6,52053,"FO2","IC" 21,36,1,1,,105,285,"NIAGARA MOHAWK POWER CORP","BEARDSLEE F",0,,13573,"0M",1294,,190,95,5266,0,0,1946,0,0,6556,0,0,4417,0,0,2463,0,0,1946,0,0,895,0,0,759,0,0,741,0,0,5400,0,0,6369,0,0,2631,0,0,2543,6,52053,"WAT","HY" 21,36,1,1,,105,290,"NIAGARA MOHAWK POWER CORP","BAKER FALLS",0,,13573,"0M",1294,"R",190,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2541,6,52053,"WAT","HY" 21,36,1,1,,105,300,"NIAGARA MOHAWK POWER CORP","EL J WEST",0,,13573,"0M",1294,,190,95,5989,0,0,5250,0,0,1580,0,0,972,0,0,1241,0,0,3218,0,0,3059,0,0,2326,0,0,4257,0,0,1425,0,0,10684,0,0,8834,0,0,6527,6,52053,"WAT","HY" 21,36,1,1,,105,305,"NIAGARA MOHAWK POWER CORP","EPHRATAH",0,,13573,"0M",1294,,190,95,2045,0,0,902,0,0,1493,0,0,780,0,0,337,0,0,463,0,0,97,0,0,147,0,0,127,0,0,1599,0,0,1298,0,0,1198,0,0,2560,6,52053,"WAT","HY" 21,36,1,1,,105,315,"NIAGARA MOHAWK POWER CORP","GLEN FALLS",0,,13573,"0M",1294,,190,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2567,6,52053,"WAT","HY" 21,36,1,1,,105,317,"NIAGARA MOHAWK POWER CORP","GREEN ISL",0,,13573,"0M",1294,,190,95,3672,0,0,3067,0,0,3470,0,0,3478,0,0,2678,0,0,2110,0,0,1303,0,0,1440,0,0,1476,0,0,2837,0,0,2513,0,0,3722,0,0,6528,6,52053,"WAT","HY" 21,36,1,1,,105,320,"NIAGARA MOHAWK POWER CORP","INGHAMS",0,,13573,"0M",1294,,190,95,2951,0,0,1446,0,0,3570,0,0,3006,0,0,1806,0,0,1403,0,0,605,0,0,518,0,0,480,0,0,2716,0,0,3695,0,0,1829,0,0,2579,6,52053,"WAT","HY" 21,36,1,1,,105,325,"NIAGARA MOHAWK POWER CORP","JOHNSONVLE",0,,13573,"0M",1294,,190,95,783,0,0,709,0,0,698,0,0,730,0,0,706,0,0,415,0,0,84,0,0,196,0,0,71,0,0,754,0,0,1347,0,0,777,0,0,2580,6,52053,"WAT","HY" 21,36,1,1,,105,340,"NIAGARA MOHAWK POWER CORP","MOREAU",0,,13573,"0M",1294,"R",190,95,0,0,0,2501,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2587,6,52053,"WAT","HY" 21,36,1,1,,105,350,"NIAGARA MOHAWK POWER CORP","SCH ST COHS",0,,13573,"0M",1294,,190,95,17365,0,0,13801,0,0,18549,0,0,16246,0,0,8330,0,0,6836,0,0,4087,0,0,3410,0,0,3303,0,0,14028,0,0,23804,0,0,15352,0,0,2605,6,52053,"WAT","HY" 21,36,1,1,,105,355,"NIAGARA MOHAWK POWER CORP","SCHAGHTICKE",0,,13573,"0M",1294,,190,95,6959,0,0,4628,0,0,1779,0,0,7008,0,0,3998,0,0,2703,0,0,925,0,0,1694,0,0,513,0,0,4157,0,0,7065,0,0,4122,0,0,2606,6,52053,"WAT","HY" 21,36,1,1,,105,360,"NIAGARA MOHAWK POWER CORP","SCHUYLERVLE",0,,13573,"0M",1294,,190,95,766,0,0,454,0,0,951,0,0,408,0,0,291,0,0,185,0,0,26,0,0,77,0,0,-5,0,0,527,0,0,1089,0,0,771,0,0,2607,6,52053,"WAT","HY" 21,36,1,1,,105,365,"NIAGARA MOHAWK POWER CORP","SHERMAN",0,,13573,"0M",1294,,190,95,14937,0,0,11480,0,0,11483,0,0,9158,0,0,6495,0,0,5892,0,0,5453,0,0,6179,0,0,6999,0,0,9121,0,0,7996,0,0,9198,0,0,2609,6,52053,"WAT","HY" 21,36,1,1,,105,370,"NIAGARA MOHAWK POWER CORP","SPIER FALLS",0,,13573,"0M",1294,,190,95,22054,0,0,16130,0,0,18521,0,0,13202,0,0,8844,0,0,7373,0,0,6467,0,0,7246,0,0,8844,0,0,15741,0,0,12177,0,0,20353,0,0,2612,6,52053,"WAT","HY" 21,36,1,1,,105,380,"NIAGARA MOHAWK POWER CORP","STEWARTS BR",0,,13573,"0M",1294,,190,95,10770,0,0,11203,0,0,3959,0,0,1818,0,0,5172,0,0,2348,0,0,5366,0,0,4271,0,0,7737,0,0,2666,0,0,19084,0,0,17328,0,0,2614,6,52053,"WAT","HY" 21,36,1,1,,105,385,"NIAGARA MOHAWK POWER CORP","STUYVESANT",0,,13573,"0M",1294,,190,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2615,6,52053,"WAT","HY" 21,36,1,2,2,105,395,"NIAGARA MOHAWK POWER CORP","ALBANY",0,"LIGHT OIL",13573,"0M",1294,,190,95,0,0,220,0,0,220,0,0,220,0,0,220,0,0,220,0,0,220,0,0,201,0,0,201,0,0,195,0,0,192,0,0,189,0,0,185,2539,6,52053,"FO2","ST" 21,36,1,2,3,105,395,"NIAGARA MOHAWK POWER CORP","ALBANY",0,"HEAVY OIL",13573,"0M",1294,,190,95,58267,97691,332532,62750,94595,237938,5641,8097,184840,0,0,184840,0,0,184840,1711,4230,180610,0,0,180610,0,0,180610,0,0,180610,0,0,180610,18591,30657,149952,25930,42050,107902,2539,6,52053,"FO6","ST" 21,36,1,2,9,105,395,"NIAGARA MOHAWK POWER CORP","ALBANY",0,"NAT GAS",13573,"0M",1294,,190,95,57789,665226,0,58253,669709,0,144263,1550322,0,53054,571524,0,31237,333909,0,47841,524896,0,130139,1434248,0,147338,1604315,0,50979,541649,0,49257,521886,0,6001,121469,0,5994,104410,0,2539,6,52053,"NG","ST" 21,36,1,3,2,105,395,"NIAGARA MOHAWK POWER CORP","ALBANY",0,"LIGHT OIL",13573,"0M",1294,,190,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2539,6,52053,"FO2","IC" 21,36,1,4,2,105,395,"NIAGARA MOHAWK POWER CORP","ALBANY",0,"LIGHT OIL",13573,"0M",1294,,190,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2539,6,52053,"FO2","GT" 21,36,1,4,9,105,395,"NIAGARA MOHAWK POWER CORP","ALBANY",0,"NAT GAS",13573,"0M",1294,,190,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2539,6,52053,"NG","GT" 21,36,1,1,,105,420,"NIAGARA MOHAWK POWER CORP","GLENWOOD",0,,13573,"0M",1294,,190,95,584,0,0,584,0,0,712,0,0,35,0,0,602,0,0,501,0,0,510,0,0,499,0,0,459,0,0,493,0,0,412,0,0,213,0,0,2568,6,52053,"WAT","HY" 21,36,1,1,,105,425,"NIAGARA MOHAWK POWER CORP","HYDRAULIC R",0,,13573,"0M",1294,,190,95,0,0,0,0,0,0,0,0,0,247,0,0,1980,0,0,1737,0,0,1757,0,0,1761,0,0,1655,0,0,1715,0,0,209,0,0,0,0,0,2578,6,52053,"WAT","HY" 21,36,1,1,,105,440,"NIAGARA MOHAWK POWER CORP","WATERPORT",0,,13573,"0M",1294,,190,95,1372,0,0,1372,0,0,1447,0,0,69,0,0,924,0,0,779,0,0,723,0,0,727,0,0,684,0,0,922,0,0,936,0,0,428,0,0,2623,6,52053,"WAT","HY" 21,36,1,2,2,105,445,"NIAGARA MOHAWK POWER CORP","DUNKIRK",0,"LIGHT OIL",13573,"0M",1294,,190,95,1601,2790,0,653,1081,0,675,1178,0,599,1017,0,1403,2417,0,539,896,0,638,1090,0,1031,1725,0,723,1216,0,997,1731,0,914,1625,0,396,651,0,2554,6,52053,"FO2","ST" 21,36,1,2,6,105,445,"NIAGARA MOHAWK POWER CORP","DUNKIRK",0,"BIT COAL",13573,"0M",1294,,190,95,254022,99455,112963,311173,114689,97723,298538,114582,80138,317020,119632,52831,259603,99967,52456,255038,95545,74556,311521,120965,80149,307244,117398,77577,307482,116339,76599,257442,99939,138351,253614,100750,153571,354614,131876,151153,2554,6,52053,"BIT","ST" 21,36,1,3,2,105,445,"NIAGARA MOHAWK POWER CORP","DUNKIRK",0,"LIGHT OIL",13573,"0M",1294,,190,95,0,0,1079,0,0,1334,0,0,1300,0,0,1323,0,0,635,0,0,1174,0,0,1343,0,0,1234,0,0,1317,0,0,1090,0,0,1325,0,0,1484,2554,6,52053,"FO2","IC" 21,36,1,2,2,105,450,"NIAGARA MOHAWK POWER CORP","C R HUNTLEY",0,"LIGHT OIL",13573,"0M",1294,,190,95,681,1256,1160,349,688,1247,690,1294,1076,1705,3207,1221,704,1326,1175,1004,1818,1727,1072,1981,1452,554,1037,1301,324,570,1193,1215,2237,1180,832,1567,1213,253,461,1135,2549,6,52053,"FO2","ST" 21,36,1,2,6,105,450,"NIAGARA MOHAWK POWER CORP","C R HUNTLEY",0,"BIT COAL",13573,"0M",1294,,190,95,272246,110975,103175,276497,121255,106086,220640,91915,179212,270614,112094,162277,265384,109603,157439,267756,107734,190733,286378,118727,131748,337035,139658,120591,316597,122391,136393,245260,100618,129570,236599,99435,197282,339259,137453,168549,2549,6,52053,"BIT","ST" 21,36,1,3,2,105,450,"NIAGARA MOHAWK POWER CORP","C R HUNTLEY",0,"LIGHT OIL",13573,"0M",1294,,190,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2549,6,52053,"FO2","IC" 21,36,1,1,,105,460,"NIAGARA MOHAWK POWER CORP","OAK ORCHARD",0,,13573,"0M",1294,,190,95,0,0,0,0,0,0,0,0,0,0,0,0,178,0,0,186,0,0,185,0,0,187,0,0,174,0,0,176,0,0,46,0,0,0,0,0,2592,6,52053,"WAT","HY" 21,36,1,1,,105,465,"NIAGARA MOHAWK POWER CORP","BEEBEE IS",0,,13573,"0M",1294,,190,95,3633,0,0,2768,0,0,5208,0,0,4383,0,0,3010,0,0,1959,0,0,2292,0,0,1754,0,0,2115,0,0,4754,0,0,5881,0,0,3959,0,0,6434,6,52053,"WAT","HY" 21,36,1,1,,105,470,"NIAGARA MOHAWK POWER CORP","FEEDER DAM",0,,13573,"0M",1294,,190,95,3058,0,0,0,0,0,2491,0,0,1680,0,0,1085,0,0,869,0,0,595,0,0,648,0,0,1046,0,0,1795,0,0,3058,0,0,2885,0,0,2666,6,52053,"WAT","HY" 21,36,1,1,,115,3,"ORANGE & ROCKLAND UTL INC","GRAHAMSVILE",0,,14154,"0M",1294,,,95,7995,0,0,10213,0,0,10828,0,0,5471,0,0,3765,0,0,6843,0,0,11715,0,0,11385,0,0,6049,0,0,6915,0,0,5017,0,0,7158,0,0,2627,6,52181,"WAT","HY" 21,36,1,1,,115,5,"ORANGE & ROCKLAND UTL INC","MONGAUP FLS",0,,14154,"0M",1294,,,95,1849,0,0,830,0,0,1994,0,0,1152,0,0,218,0,0,502,0,0,749,0,0,605,0,0,91,0,0,475,0,0,1859,0,0,1637,0,0,2630,6,52181,"WAT","HY" 21,36,1,1,,115,10,"ORANGE & ROCKLAND UTL INC","RIO",0,,14154,"0M",1294,,,95,4380,0,0,1792,0,0,4911,0,0,2578,0,0,759,0,0,986,0,0,1125,0,0,978,0,0,116,0,0,1041,0,0,4467,0,0,3352,0,0,2631,6,52181,"WAT","HY" 21,36,1,1,,115,15,"ORANGE & ROCKLAND UTL INC","SWING BR 1",0,,14154,"0M",1294,,,95,1041,0,0,442,0,0,1445,0,0,608,0,0,266,0,0,374,0,0,391,0,0,409,0,0,76,0,0,299,0,0,1316,0,0,873,0,0,2633,6,52181,"WAT","HY" 21,36,1,1,,115,20,"ORANGE & ROCKLAND UTL INC","SWING BR 2",0,,14154,"0M",1294,,,95,687,0,0,340,0,0,661,0,0,428,0,0,16,0,0,-84,0,0,164,0,0,42,0,0,-68,0,0,68,0,0,889,0,0,593,0,0,2634,6,52181,"WAT","HY" 21,36,1,2,3,115,25,"ORANGE & ROCKLAND UTL INC","BOWLINE PT",0,"HEAVY OIL",14154,"0M",1294,,,95,43906,73730,656595,138605,222519,509921,36874,60431,690856,47123,77864,612992,171664,281797,399693,132603,218077,395393,121658,204130,412273,93622,159538,457749,16475,28676,564249,22772,39554,562775,23802,41159,590697,87447,145316,516559,2625,6,52181,"FO6","ST" 21,36,1,2,9,115,25,"ORANGE & ROCKLAND UTL INC","BOWLINE PT",0,"NAT GAS",14154,"0M",1294,,,95,168974,1723560,0,82272,1239913,0,246716,2463200,0,218627,2199380,0,99656,966090,0,197607,1984380,0,277722,2939140,0,259468,2692570,0,188365,2000250,0,195838,2071510,0,142378,1499610,0,41983,424600,0,2625,6,52181,"NG","ST" 21,36,1,2,3,115,30,"ORANGE & ROCKLAND UTL INC","LOVETT",0,"HEAVY OIL",14154,"0M",1294,,,95,8,15,100319,1955,3363,96956,1,1,96927,0,0,96968,162,289,96714,7,13,96701,10,18,96682,5,10,96706,6,11,96717,0,0,96732,0,0,96732,5,10,96723,2629,6,52181,"FO6","ST" 21,36,1,2,6,115,30,"ORANGE & ROCKLAND UTL INC","LOVETT",0,"BIT COAL",14154,"0M",1294,,,95,111799,49067,63359,155251,65603,75519,116513,50062,70545,69873,29960,67950,67316,29174,75567,80224,36666,84715,138923,58882,82515,118307,52178,76055,140703,61690,59229,113469,49704,60388,125569,51656,62679,132749,58514,56774,2629,6,52181,"BIT","ST" 21,36,1,2,9,115,30,"ORANGE & ROCKLAND UTL INC","LOVETT",0,"NAT GAS",14154,"0M",1294,,,95,29773,323525,0,26698,280445,0,15824,169812,0,33214,357965,0,35392,384353,0,65900,754578,0,47901,513697,0,42001,470557,0,20369,222754,0,24743,268834,0,21096,220661,0,31665,346005,0,2629,6,52181,"NG","ST" 21,36,1,4,2,115,35,"ORANGE & ROCKLAND UTL INC","HILLBURN",0,"LIGHT OIL",14154,"0M",1294,,,95,0,0,4238,0,0,4238,0,0,4238,0,0,4238,0,9,4229,0,0,4229,52,164,4065,108,334,3731,0,0,3731,0,0,3731,0,0,3731,0,0,3731,2628,6,52181,"FO2","GT" 21,36,1,4,9,115,35,"ORANGE & ROCKLAND UTL INC","HILLBURN",0,"NATURAL G",14154,"0M",1294,,,95,44,1217,0,0,0,0,37,1143,0,565,8996,0,-13,1208,0,256,5250,0,276,4745,0,945,15862,0,444,6906,0,-18,82,0,-27,456,0,24,430,0,2628,6,52181,"NG","GT" 21,36,1,4,2,115,40,"ORANGE & ROCKLAND UTL INC","SHOEMAKER",0,"LIGHT OIL",14154,"0M",1294,,,95,0,0,4599,73,30,4569,29,103,4466,-1,30,4485,1,2,4463,45,124,4068,0,0,4068,1,3,4065,0,0,4065,22,81,3984,84,247,3738,0,0,3738,2632,6,52181,"FO2","GT" 21,36,1,4,9,115,40,"ORANGE & ROCKLAND UTL INC","SHOEMAKER",0,"NAT GAS",14154,"0M",1294,,,95,217,4023,0,342,7789,0,599,11559,0,-31,207,0,1856,30143,0,3256,49008,0,4402,75566,0,4597,74746,0,2492,42150,0,713,14586,0,45,456,0,53,1654,0,2632,6,52181,"NG","GT" 21,36,1,2,1,135,1,"ROCHESTER GAS & ELEC CORP","GINNA",0,"NUCLEAR",16183,"0M",1294,,,95,351805,0,0,321771,0,0,293087,0,0,-2750,0,0,299117,0,0,334397,0,0,342637,0,0,305248,0,0,336763,0,0,353447,0,0,342871,0,0,354889,0,0,6122,6,52501,"UR","ST" 21,36,1,1,,135,5,"ROCHESTER GAS & ELEC CORP","MILLS M 172",0,,16183,"0M",1294,,,95,68,0,0,0,0,0,79,0,0,31,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2636,6,52501,"WAT","HY" 21,36,1,1,,135,10,"ROCHESTER GAS & ELEC CORP","MT MORR 160",0,,16183,"0M",1294,,,95,0,0,0,75,0,0,0,0,0,0,0,0,49,0,0,121,0,0,87,0,0,44,0,0,16,0,0,124,0,0,132,0,0,67,0,0,2637,6,52501,"WAT","HY" 21,36,1,1,,135,15,"ROCHESTER GAS & ELEC CORP","ROCHESTER 2",0,,16183,"0M",1294,,,95,3983,0,0,3890,0,0,4861,0,0,4119,0,0,4073,0,0,2681,0,0,1898,0,0,1483,0,0,708,0,0,3228,0,0,4230,0,0,3509,0,0,2639,6,52501,"WAT","HY" 21,36,1,1,,135,25,"ROCHESTER GAS & ELEC CORP","ROCHESTER 5",0,,16183,"0M",1294,,,95,18727,0,0,8869,0,0,21670,0,0,13445,0,0,7303,0,0,4173,0,0,5885,0,0,2422,0,0,1347,0,0,9730,0,0,15462,0,0,12738,0,0,2641,6,52501,"WAT","HY" 21,36,1,1,,135,28,"ROCHESTER GAS & ELEC CORP","RCHESTER 26",0,,16183,"0M",1294,,,95,596,0,0,1040,0,0,1215,0,0,1302,0,0,1083,0,0,420,0,0,405,0,0,282,0,0,135,0,0,726,0,0,1174,0,0,1054,0,0,2638,6,52501,"WAT","HY" 21,36,1,1,,135,35,"ROCHESTER GAS & ELEC CORP","WISCOY 170",0,,16183,"0M",1294,,,95,517,0,0,408,0,0,590,0,0,391,0,0,204,0,0,97,0,0,121,0,0,83,0,0,55,0,0,240,0,0,470,0,0,462,0,0,2646,6,52501,"WAT","HY" 21,36,1,2,2,135,45,"ROCHESTER GAS & ELEC CORP","ROCHESTER 3",0,"LIGHT OIL",16183,"0M",394,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,102,143,2305,77,143,2008,122,214,1718,91,167,1882,68,119,1700,27,58,1645,2640,6,52501,"FO2","ST" 21,36,1,2,3,135,45,"ROCHESTER GAS & ELEC CORP","ROCHESTER 3",0,"HEAVY OIL",16183,"0M",1294,"R",,95,27,48,2860,14,24,2809,14,24,2745,14,24,2703,0,0,2703,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2640,6,52501,"FO6","ST" 21,36,1,2,6,135,45,"ROCHESTER GAS & ELEC CORP","ROCHESTER 3",0,"BIT COAL",16183,"0M",1294,,,95,36334,13900,770,42264,15300,1458,40715,15300,1556,45572,16900,817,17481,6500,1591,36715,14100,1438,41179,15700,936,37637,15017,1800,37010,13802,1800,27740,10832,1630,33466,12558,1431,34731,13210,1105,2640,6,52501,"BIT","ST" 21,36,1,4,2,135,45,"ROCHESTER GAS & ELEC CORP","ROCHESTER 3",0,"LIGHT OIL",16183,"0M",1294,,,95,26,81,0,4,27,0,13,41,0,3,18,0,0,0,0,6,34,0,4,6,0,46,154,0,25,76,0,8,26,0,13,63,0,1,7,0,2640,6,52501,"FO2","GT" 21,36,1,2,2,135,50,"ROCHESTER GAS & ELEC CORP","ROCHESTER 7",0,"LIGHT OIL",16183,"0M",1294,,,95,299,571,1111,90,167,1127,375,690,1162,173,310,1211,249,452,1299,566,1071,1121,331,643,1190,434,833,1065,37,71,1065,373,738,1065,345,643,958,311,571,1102,2642,6,52501,"FO2","ST" 21,36,1,2,6,135,50,"ROCHESTER GAS & ELEC CORP","ROCHESTER 7",0,"BIT COAL",16183,"0M",1294,,,95,66357,27700,114902,86515,35300,90431,90609,36600,83204,137634,53400,75835,121093,47500,85250,104898,43000,113923,112687,47700,112973,116634,48507,127749,110993,45157,153399,77990,33362,173353,81051,33064,173047,90029,35948,150667,2642,6,52501,"BIT","ST" 21,36,1,4,2,135,60,"ROCHESTER GAS & ELEC CORP","ROCHESTER 9",0,"LIGHT OIL",16183,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2644,6,52501,"FO2","GT" 21,36,1,4,9,135,60,"ROCHESTER GAS & ELEC CORP","ROCHESTER 9",0,"NAT GAS",16183,"0M",1294,,,95,26,383,0,2,74,0,14,216,0,4,174,0,0,0,0,8,290,0,17,280,0,3,89,0,24,381,0,0,0,0,3,98,0,8,143,0,2644,6,52501,"NG","GT" 21,36,5,3,2,578,5,"FREEPORT (VILLAGE OF)","PLANT NO 2",0,"LIGHT OIL",6775,"0M",1294,,,95,1463,3067,3172,1434,3271,2622,413,1557,2551,-162,121,3525,-118,217,5782,984,2264,6164,3712,7100,3595,3729,7301,5720,584,1625,6684,895,1423,5789,787,2037,3752,1869,3903,3213,2679,6,51057,"FO2","IC" 21,36,5,4,2,578,5,"FREEPORT (VILLAGE OF)","PLANT NO 2",0,"LIGHT OIL",6775,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2,12,0,13,58,0,18,95,0,0,0,0,0,0,0,0,0,0,0,0,0,2679,6,51057,"FO2","GT" 21,36,5,3,2,578,10,"FREEPORT (VILLAGE OF)","PLANT NO 1",0,"LIGHT OIL",6775,"0M",1294,,,95,182,658,1479,376,1032,1630,468,1254,1391,320,920,1697,251,803,1542,452,1093,1119,571,1281,1220,740,1757,1321,639,1551,1424,175,575,1295,402,1078,1704,465,1231,1436,2678,6,51057,"FO2","IC" 21,36,5,1,,586,1,"GOUVERNEUR (CITY OF)","GOUVERNEUR",0,,7422,"0A",1294,,,95,46,0,0,92,0,0,47,0,0,50,0,0,50,0,0,38,0,0,13,0,0,45,0,0,29,0,0,20,0,0,26,0,0,41,0,0,2680,6,51137,"WAT","HY" 21,36,5,3,2,599,1,"GREENPORT (CITY OF)","GREENPORT",0,"LIGHT OIL",7630,"0A",1294,,,95,-32,0,183,-32,0,183,-27,0,183,0,2,181,0,0,0,0,1,180,-20,0,180,-4,28,152,-10,14,182,-19,0,182,0,0,182,-1,26,181,2681,6,51177,"FO2","IC" 21,36,5,2,2,624,1,"JAMESTOWN (CITY OF)","S A CARLSON",0,"LIGHT OIL",9645,"0M",1294,,,95,105,273,377,41,102,275,21,59,394,24,59,335,20,54,281,26,64,394,57,144,250,59,144,281,26,66,215,26,69,323,44,114,209,51,136,250,2682,6,51437,"FO2","ST" 21,36,5,2,6,624,1,"JAMESTOWN (CITY OF)","S A CARLSON",0,"BIT COAL",9645,"0M",1294,,,95,17974,10638,3526,17648,10013,3826,11794,7305,3597,9844,5439,3428,9879,6006,2629,11487,6255,2811,13511,7717,2530,13208,7291,3578,9538,5398,3370,10505,6096,2827,12704,7245,3946,16956,10165,3924,2682,6,51437,"BIT","ST" 21,36,5,3,2,675,1,"ROCKVILLE CTR(VILLAGE OF)","ROCKVILLE C",0,"LIGHT OIL",16217,"0M",1294,,,95,105,294,2332,321,741,2091,43,283,1808,-60,82,1726,-18,114,2338,244,637,2368,957,2138,1919,2160,4073,1884,560,1129,2277,20,216,2061,38,213,2151,101,381,1770,2695,6,52509,"FO2","IC" 21,36,5,3,9,675,1,"ROCKVILLE CTR(VILLAGE OF)","ROCKVILLE C",0,"NAT GAS",16217,"0M",1294,,,95,642,7257,0,510,5912,0,15,471,0,0,325,0,-11,282,0,1931,20033,0,4455,46010,0,2523,26516,0,352,4031,0,47,1369,0,46,1025,0,450,5750,0,2695,6,52509,"NG","IC" 21,36,5,3,2,700,5,"SKANEATELES VILLAGE OF","SKANEATELES",0,"LIGHT OIL",17280,"0A",1294,"R",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2697,6,52670,"FO2","IC" 21,36,5,1,,712,1,"SPRINGVILLE (CITY OF)","SPRINGVILLE",0,,17846,"0A",1294,,,95,145,0,0,118,0,0,104,0,0,166,0,0,172,0,0,129,0,0,84,0,0,63,0,0,12,0,0,39,0,0,110,0,0,124,0,0,2698,6,52772,"WAT","HY" 21,36,5,1,,725,1,"WATERTOWN (CITY OF)","WATERTOWN",0,,20188,"0A",1294,,,95,2508,0,0,1826,0,0,2861,0,0,2520,0,0,2042,0,0,715,0,0,684,0,0,252,0,0,458,0,0,1925,0,0,2671,0,0,2141,0,0,2700,6,53199,"WAT","HY" 21,36,9,1,,668,1,"POWER AUTHY OF ST OF N Y","LEWISTON PG",0,"C-PUMPSTG",15296,"0M",1294,,,95,-23392,48481,0,-16321,48107,0,-18062,52914,0,-34170,75041,0,-32754,81523,0,-35246,84639,0,-35971,80543,0,-31970,78905,0,-33926,76500,0,-34404,82531,0,-25619,66689,0,-26848,63831,0,2692,6,52375,"WAT","HY" 21,36,9,2,1,668,1,"POWER AUTHY OF ST OF N Y","FITZPATRICK",0,"NUCLEAR",15296,"0M",1294,,,95,0,0,0,0,0,0,34055,0,0,544665,0,0,562170,0,0,384520,0,0,579310,0,0,577530,0,0,402855,0,0,590100,0,0,572680,0,0,580835,0,0,6110,6,52375,"UR","ST" 21,36,9,1,,668,3,"POWER AUTHY OF ST OF N Y","MOSES NIAG",0,,15296,"0M",1294,,,95,1463973,0,0,1230590,0,0,1418230,0,0,1163933,0,0,1279083,0,0,1132981,0,0,1197133,0,0,1148436,0,0,1021706,0,0,1145560,0,0,1382957,0,0,1354956,0,0,2693,6,52375,"WAT","HY" 21,36,9,2,1,668,3,"POWER AUTHY OF ST OF N Y","INDIAN PT 3",0,"NUCLEAR",15296,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,17,0,0,434533,0,0,716433,0,0,320544,0,0,0,0,0,0,0,0,-2,0,0,8907,6,52375,"UR","ST" 21,36,9,1,,668,5,"POWER AUTHY OF ST OF N Y","MOSES PR DM",0,,15296,"0M",1294,,,95,524759,0,0,481624,0,0,585412,0,0,549618,0,0,532348,0,0,526743,0,0,545520,0,0,559232,0,0,538635,0,0,554432,0,0,576778,0,0,569302,0,0,2694,6,52375,"WAT","HY" 21,36,9,1,,668,8,"POWER AUTHY OF ST OF N Y","BLENHEIM G",0,"P-PUMPSTG",15296,"0M",1294,,,95,-80117,223900,0,-66116,187582,0,-64757,198518,0,-71547,180530,0,-58305,185571,0,-61293,196731,0,-78558,215353,0,-75753,237341,0,-63547,183628,0,-66325,194141,0,-57795,177791,0,-70135,192222,0,2691,6,52375,"WAT","HY" 21,36,9,2,3,668,15,"POWER AUTHY OF ST OF N Y","POLETTI",0,"HEAVY OIL",15296,"0M",1294,,,95,33400,61649,303226,126069,209523,203682,20403,35475,168236,17269,37577,130679,19806,35708,94972,47803,62254,32718,36004,60668,68293,14149,23707,150452,35247,61190,430389,17481,30727,459549,62862,110242,349307,252627,421942,245156,2491,6,52375,"FO6","ST" 21,36,9,2,9,668,15,"POWER AUTHY OF ST OF N Y","POLETTI",0,"NAT GAS",15296,"0M",1294,,,95,99454,1128061,0,99940,1020449,0,202945,2167293,0,211435,2738075,0,258894,2862705,0,324525,2604689,0,262599,2721610,0,310920,3222176,0,205757,2168448,0,224611,2374781,0,128580,1368464,0,2466,25078,0,2491,6,52375,"NG","ST" 21,36,9,1,,668,20,"POWER AUTHY OF ST OF N Y","ASHOKAN",0,,15296,"0M",1294,,,95,1615,0,0,587,0,0,1045,0,0,2214,0,0,2450,0,0,2277,0,0,2117,0,0,2126,0,0,1756,0,0,1286,0,0,1083,0,0,1303,0,0,88,6,52375,"WAT","HY" 21,36,9,1,,668,25,"POWER AUTHY OF ST OF N Y","KENSICO",0,,15296,"0M",1294,,,95,802,0,0,73,0,0,0,0,0,1521,0,0,150,0,0,271,0,0,1411,0,0,1244,0,0,1418,0,0,1191,0,0,880,0,0,0,0,0,650,6,52375,"WAT","HY" 21,36,9,1,,668,30,"POWER AUTHY OF ST OF N Y","JARVIS",0,,15296,"0M",1294,,,95,4048,0,0,2165,0,0,2416,0,0,2485,0,0,1720,0,0,1501,0,0,1162,0,0,1003,0,0,575,0,0,2833,0,0,5091,0,0,2476,0,0,808,6,52375,"WAT","HY" 21,36,9,1,,668,35,"POWER AUTHY OF ST OF N Y","CRESCENT",0,,15296,"0M",1294,,,95,6303,0,0,4034,0,0,7316,0,0,4624,0,0,3019,0,0,2031,0,0,104,0,0,713,0,0,703,0,0,3132,0,0,6120,0,0,4690,0,0,2685,6,52375,"WAT","HY" 21,36,9,1,,668,40,"POWER AUTHY OF ST OF N Y","VISCHER FER",0,,15296,"0M",1294,,,95,5945,0,0,3714,0,0,6024,0,0,4504,0,0,2789,0,0,1833,0,0,986,0,0,123,0,0,654,0,0,2259,0,0,5980,0,0,4591,0,0,2686,6,52375,"WAT","HY" 21,36,9,5,9,668,45,"POWER AUTHY OF ST OF N Y","FLYNN",0,"WASTE HT",15296,"0M",1294,,,95,24819,192100,0,17369,134483,0,27383,211172,0,18948,146928,0,26056,199854,0,24430,188777,0,23492,184084,0,25126,194127,0,24424,188668,0,23749,183457,0,20261,158951,0,19720,154115,0,7314,6,52375,"WH","CC" 21,36,9,6,2,668,45,"POWER AUTHY OF ST OF N Y","FLYNN",0,"LIGHT OIL",15296,"0M",1294,,,95,7722,10369,101959,21462,28859,72145,0,0,72242,14,20,72083,0,0,72104,0,0,72094,0,0,72044,0,0,72052,0,0,72062,157,211,71873,9447,12866,58992,27271,36998,78070,7314,6,52375,"FO2","CT" 21,36,9,6,9,668,45,"POWER AUTHY OF ST OF N Y","FLYNN",0,"NAT GAS",15296,"0M",1294,,,95,74458,576302,0,52111,403450,0,82153,633518,0,56849,440785,0,78170,599562,0,73293,566331,0,71470,552251,0,75381,582382,0,73276,566005,0,71251,550371,0,60784,476853,0,59162,462344,0,7314,6,52375,"NG","CT" 22,34,1,2,2,24,1,"ATLANTIC CITY ELEC CO","DEEPWATER",0,"LIGHT OIL",963,"0M",1294,,181,95,0,0,123,81,130,93,0,0,131,0,0,138,14,28,165,67,129,202,80,160,147,5,10,137,40,91,189,0,29,160,0,29,131,4,8,123,2384,3,56513,"FO2","ST" 22,34,1,2,3,24,1,"ATLANTIC CITY ELEC CO","DEEPWATER",0,"HEAVY OIL",963,"0M",1294,,181,95,1345,2425,95467,4563,6516,88951,0,0,88951,0,0,88261,0,0,88261,1177,2026,86235,3361,5958,80277,5273,9351,70926,5555,8624,62302,0,0,62302,0,0,62302,0,0,62302,2384,3,56513,"FO6","ST" 22,34,1,2,6,24,1,"ATLANTIC CITY ELEC CO","DEEPWATER",0,"BIT COAL",963,"0M",1294,,181,95,29945,12519,39313,35838,15203,23710,8276,3561,20149,0,0,34389,5810,3059,52665,34469,14723,52014,42129,18253,40567,44451,19515,27979,11926,4625,44084,33654,13941,51248,53859,21346,70836,57721,22974,63900,2384,3,56513,"BIT","ST" 22,34,1,2,9,24,1,"ATLANTIC CITY ELEC CO","DEEPWATER",0,"NAT GAS",963,"0M",1294,,181,95,1491,16310,0,0,0,0,944,9940,0,1878,22040,0,11307,122240,0,11062,117040,0,27862,302860,0,29442,321050,0,12534,120040,0,807,8090,0,1552,15370,0,0,0,0,2384,3,56513,"NG","ST" 22,34,1,4,2,24,1,"ATLANTIC CITY ELEC CO","DEEPWATER",0,"LIGHT OIL",963,"0M",1294,,181,95,-8,0,770,27,44,729,14,39,690,20,103,587,0,0,587,0,0,587,0,0,587,0,0,587,0,0,587,0,0,587,0,0,587,0,0,0,2384,3,56513,"FO2","GT" 22,34,1,4,9,24,1,"ATLANTIC CITY ELEC CO","DEEPWATER",0,"NAT GAS",963,"0M",1294,,181,95,-8,0,0,0,0,0,0,0,0,0,0,0,0,0,0,629,6657,0,3831,41649,0,3649,39793,0,1027,14649,0,628,9167,0,1061,10505,0,694,6875,0,2384,3,56513,"NG","GT" 22,34,1,4,2,24,2,"ATLANTIC CITY ELEC CO","MISSOURI AV",0,"LIGHT OIL",963,"0M",1294,,181,95,-4,100,9869,278,791,9635,3,53,9582,-21,5,9576,-17,8,9568,177,455,9113,2101,5546,7361,1882,5382,8451,605,2439,10201,-18,16,10185,-16,19,10167,2,70,10097,2383,3,56513,"FO2","GT" 22,34,1,2,2,24,5,"ATLANTIC CITY ELEC CO","B L ENGLAND",0,"LIGHT OIL",963,"0M",1294,,181,95,510,999,1734,317,596,1818,213,395,1756,107,200,1734,125,224,1843,424,778,1734,424,814,1508,552,1027,1647,500,1086,1588,450,958,1654,643,1122,1377,242,442,1435,2378,3,56513,"FO2","ST" 22,34,1,2,3,24,5,"ATLANTIC CITY ELEC CO","B L ENGLAND",0,"HEAVY OIL",963,"0M",1294,,181,95,4583,8307,99579,7833,13643,103560,0,0,103560,0,0,103560,0,0,103560,8731,14731,88829,37756,66914,51324,29729,50813,69931,850,2842,113855,18800,33751,80103,0,0,80103,15770,26499,87607,2378,3,56513,"FO6","ST" 22,34,1,2,6,24,5,"ATLANTIC CITY ELEC CO","B L ENGLAND",0,"BIT COAL",963,"0M",1294,,181,95,68381,30282,165387,127521,54088,125492,123787,53379,95025,85963,36061,88754,176115,72435,61413,155554,64926,62658,185411,80134,49009,173888,73305,41509,130330,53650,71904,83030,32962,118367,145947,62033,109160,196038,81549,81843,2378,3,56513,"BIT","ST" 22,34,1,3,2,24,5,"ATLANTIC CITY ELEC CO","B L ENGLAND",0,"LIGHT OIL",963,"0M",1294,,181,95,0,0,0,5,11,0,0,0,0,0,0,0,0,0,0,12,23,0,133,257,0,321,597,0,5,10,0,0,0,0,0,0,0,0,0,0,2378,3,56513,"FO2","IC" 22,34,1,4,2,24,20,"ATLANTIC CITY ELEC CO","MIDDLE STA",0,"LIGHT OIL",963,"0M",1294,,181,95,-834,144,15410,-227,1590,15128,-1342,459,14669,-815,159,14510,-333,16,14494,-558,315,9113,2009,5421,12193,2243,7786,14637,-670,677,15327,-729,232,15284,-745,423,15069,-730,254,14814,2382,3,56513,"FO2","GT" 22,34,1,4,2,24,25,"ATLANTIC CITY ELEC CO","CEDAR STA",0,"LIGHT OIL",963,"0M",1294,,181,95,-474,179,21675,-321,918,21875,-42,70,21804,-546,56,21748,-110,38,21710,62,61,21650,3843,9672,14702,3756,10444,18151,-253,1075,20407,-631,431,21246,-535,219,21027,-679,322,20705,2380,3,56513,"FO2","GT" 22,34,1,4,2,24,30,"ATLANTIC CITY ELEC CO","CARLL CORNR",0,"LIGHT OIL",963,"0M",1294,,181,95,-28,8,13554,78,379,13175,-43,0,13175,-20,0,13175,-965,8,13167,-121,166,13002,1394,2899,10102,1615,4499,9171,-32,0,13713,-16,0,14849,-44,0,14849,49,332,14517,2379,3,56513,"FO2","GT" 22,34,1,4,9,24,30,"ATLANTIC CITY ELEC CO","CARLL CORNR",0,"NAT GAS",963,"0M",1294,,181,95,35,1120,0,452,8170,0,-76,50,0,-19,1010,0,73,2450,0,835,15970,0,6072,93380,0,5324,82370,0,-117,28460,0,861,14250,0,-44,7170,0,172,150,0,2379,3,56513,"NG","GT" 22,34,1,4,2,24,32,"ATLANTIC CITY ELEC CO","MICKETON ST",0,"LIGHT OIL",963,"0M",1294,,181,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,8008,3,56513,"FO2","GT" 22,34,1,4,9,24,32,"ATLANTIC CITY ELEC CO","MICKETON ST",0,"NAT GAS",963,"0M",1294,,181,95,665,11020,0,1084,16250,0,714,11030,0,1017,15170,0,334,6070,0,2355,35610,0,9801,143090,0,8665,129480,0,2856,42750,0,30,1480,0,2277,33340,0,276,5380,0,8008,3,56513,"NG","GT" 22,34,1,4,2,24,33,"ATLANTIC CITY ELEC CO","CUMBERLAND",0,"LIGHT OIL",963,"0M",1294,,181,95,-76,0,18141,-10,0,18141,-38,0,18141,-31,0,18141,-30,0,18141,0,0,18141,5894,12888,17367,7323,16647,12470,3,249,14661,0,0,17077,-158,198,17249,60,412,16838,5083,3,56513,"FO2","GT" 22,34,1,4,9,24,33,"ATLANTIC CITY ELEC CO","CUMBERLAND",0,"NAT GAS",963,"0M",1294,,181,95,-76,0,0,-10,0,0,-38,0,0,-31,0,0,0,0,0,-27,130,0,342,4020,0,16,200,0,1,380,0,-93,0,0,0,0,0,101,3810,0,5083,3,56513,"NG","GT" 22,34,1,4,2,24,35,"ATLANTIC CITY ELEC CO","MANTU DEPOT",0,"LIGHT OIL",963,"0M",1294,,181,95,0,0,53843,0,0,50861,0,0,80853,0,0,80853,0,0,80853,0,0,80853,0,0,58245,0,0,12871,0,0,12871,0,0,52645,0,0,52645,0,0,82122,8803,3,56513,"FO2","GT" 22,34,1,4,3,24,40,"ATLANTIC CITY ELEC CO","MANTU DEPOT",0,"HEAVY OIL",963,"0M",1294,,181,95,0,0,128847,0,0,111223,0,0,111223,0,0,111223,0,0,111223,0,0,111223,0,0,81814,0,0,111865,0,0,111865,0,0,115694,0,0,115694,0,0,131074,8804,3,56513,"FO6","GT" 22,34,1,4,2,24,45,"ATLANTIC CITY ELEC CO","SHERMAN AVE",0,"LIGHT OIL",963,"0M",1294,,181,95,70,186,14708,-45,0,14708,-30,0,14708,0,0,14708,-11,0,14708,0,0,14708,0,0,14708,-190,0,14708,0,0,14708,0,0,14708,76,193,14515,232,590,14513,7288,3,56513,"FO2","GT" 22,34,1,4,9,24,45,"ATLANTIC CITY ELEC CO","SHERMAN AVE",0,"NAT GAS",963,"0M",1294,,181,95,1386,19950,0,-45,0,0,-30,0,0,0,0,0,0,0,0,0,0,0,0,0,0,-190,0,0,0,0,0,0,0,0,1704,23780,0,2984,41500,0,7288,3,56513,"NG","GT" 22,34,1,2,1,50,1,"GPU NUCLEAR CORP","OYSTER CRK",0,"NUCLEAR",7423,"0M",1294,,,95,471880,0,0,400185,0,0,466040,0,0,457427,0,0,440064,0,0,447364,0,0,438119,0,0,420825,0,0,447572,0,0,468215,0,0,428423,0,0,307964,0,0,2388,3,58850,"UR","ST" 22,34,1,1,,78,5,"JERSEY CENTRAL PWR & LGT","YARDS CR JO",0,"P-PUMPSTG",9726,"0M",1294,,,95,-9476,31075,0,-6121,19602,0,-8606,30644,0,-9596,30043,0,-9800,36086,0,-15417,52655,0,-13938,46076,0,-11848,42668,0,-7525,27636,0,0,0,0,0,0,0,-2205,5358,0,6522,3,56512,"WAT","HY" 22,34,1,4,2,78,7,"JERSEY CENTRAL PWR & LGT","GLEN GARDNR",0,"LIGHT OIL",9726,"0M",1294,,,95,357,1074,17830,457,1242,16588,29,247,16340,30,141,16199,0,0,16199,360,1062,15138,0,0,15138,0,0,15138,149,445,14693,21,60,14633,69,223,14409,10,63,16838,8227,3,56512,"FO2","GT" 22,34,1,4,9,78,7,"JERSEY CENTRAL PWR & LGT","GLEN GARDNR",0,"NAT GAS",9726,"0M",1294,,,95,1,10,0,31,485,0,2,90,0,0,0,0,0,0,0,698,11690,0,15562,248730,0,18982,309960,0,4246,71580,0,3046,50662,0,1111,20594,0,10,377,0,8227,3,56512,"NG","GT" 22,34,1,2,3,78,9,"JERSEY CENTRAL PWR & LGT","GILBERT",0,"HEAVY OIL",9726,"0M",1294,,,95,268,611,153901,2150,4403,149484,0,0,149488,0,0,149544,0,0,149379,0,0,150080,0,0,150051,0,0,149974,0,0,150075,0,0,149949,0,0,149926,8990,12417,137518,2393,3,56512,"FO6","ST" 22,34,1,2,9,78,9,"JERSEY CENTRAL PWR & LGT","GILBERT",0,"NAT GAS",9726,"0M",1294,,,95,1658,32084,0,198,3865,0,-452,0,0,-364,0,0,-363,0,0,6011,80854,0,28213,364986,0,24888,306021,0,915,14545,0,340,8670,0,825,13717,0,331,2840,0,2393,3,56512,"NG","ST" 22,34,1,4,2,78,9,"JERSEY CENTRAL PWR & LGT","GILBERT",0,"LIGHT OIL",9726,"0M",1294,,,95,150,431,0,803,2747,0,39,127,0,0,0,0,0,0,0,1,8,0,1,3,0,791,2604,0,31,88,0,0,0,0,0,0,0,0,0,0,2393,3,56512,"FO2","GT" 22,34,1,4,9,78,9,"JERSEY CENTRAL PWR & LGT","GILBERT",0,"NAT GAS",9726,"0M",1294,,,95,1,16,0,0,0,0,1,15,0,0,0,0,0,0,0,3,79,0,2862,50800,0,6493,121452,0,911,15880,0,4,174,0,979,364,0,29,249,0,2393,3,56512,"NG","GT" 22,34,1,5,2,78,9,"JERSEY CENTRAL PWR & LGT","GILBERT",0,"LIGHT OIL",9726,"0M",1294,,,95,728,0,0,3136,0,0,1259,0,0,1612,0,0,-587,0,0,5741,0,0,26058,0,0,28272,0,0,20554,0,0,8047,0,0,19296,0,0,18926,0,0,2393,3,56512,"FO2","CC" 22,34,1,5,9,78,9,"JERSEY CENTRAL PWR & LGT","GILBERT",0,"WASTE HT",9726,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2393,3,56512,"NG","CC" 22,34,1,6,2,78,9,"JERSEY CENTRAL PWR & LGT","GILBERT",0,"LIGHT OIL",9726,"0M",1294,,,95,1147,2566,252704,5572,11989,236313,1136,2545,232067,367,826,230086,0,0,229824,2660,6112,221348,82,189,219853,2038,4709,211204,942,1977,207539,163,373,205587,83,183,203671,5739,8660,193069,2393,3,56512,"FO2","CT" 22,34,1,6,9,78,9,"JERSEY CENTRAL PWR & LGT","GILBERT",0,"NAT GAS",9726,"0M",1294,,,95,5385,68331,0,8729,106467,0,6306,80671,0,7352,94029,0,-100,0,0,15594,203104,0,61026,877903,0,70864,931070,0,54572,701754,0,24094,329931,0,60664,796524,0,81101,693848,0,2393,3,56512,"NG","CT" 22,34,1,2,3,78,10,"JERSEY CENTRAL PWR & LGT","SAYREVILLE",0,"HEAVY OIL",9726,"0M",1294,,,95,4224,7914,90214,19448,37587,72103,7,16,72200,0,0,72163,792,1710,90373,6448,15362,75189,42812,86857,27305,24793,50118,55888,1650,3646,52242,0,0,71301,7,18,90540,10844,23847,66865,2390,3,56512,"FO6","ST" 22,34,1,2,9,78,10,"JERSEY CENTRAL PWR & LGT","SAYREVILLE",0,"NAT GAS",9726,"0M",1294,,,95,20137,245800,0,2651,32100,0,6917,89800,0,-727,100,0,-407,2800,0,141,2100,0,224,4900,0,16338,199000,0,1429,25400,0,-704,0,0,2904,47900,0,306,4100,0,2390,3,56512,"NG","ST" 22,34,1,4,2,78,10,"JERSEY CENTRAL PWR & LGT","SAYREVILLE",0,"LIGHT OIL",9726,"0M",1294,,,95,93,224,31996,752,2238,29758,0,0,29758,0,0,29758,139,640,29118,0,0,29118,0,0,29118,0,0,29118,0,0,29118,0,0,29118,0,0,29118,0,0,29118,2390,3,56512,"FO2","GT" 22,34,1,4,9,78,10,"JERSEY CENTRAL PWR & LGT","SAYREVILLE",0,"NAT GAS",9726,"0M",1294,,,95,1500,19800,0,1294,21300,0,831,12100,0,898,13300,0,187,4800,0,2507,37100,0,16534,266200,0,24165,379300,0,3245,51100,0,2451,37300,0,265,3800,0,22,300,0,2390,3,56512,"NG","GT" 22,34,1,2,3,78,15,"JERSEY CENTRAL PWR & LGT","WERNER",0,"HEAVY OIL",9726,"0M",1294,,,95,259,628,28845,5405,11437,18060,1926,4703,13792,-265,311,13764,-275,69,13780,1352,3366,28845,10346,20351,28459,7922,15595,12784,55,70,13159,-271,197,32022,-298,546,32144,3509,7954,24818,2385,3,56512,"FO6","ST" 22,34,1,4,2,78,15,"JERSEY CENTRAL PWR & LGT","WERNER",0,"LIGHT OIL",9726,"0M",1294,,,95,44,115,40240,398,1664,37864,88,236,37615,0,0,37379,13,702,36473,348,618,35855,2640,8238,27453,4764,13326,33888,215,290,33598,10,269,33202,0,25,42792,3,278,41910,2385,3,56512,"FO2","GT" 22,34,1,4,2,78,20,"JERSEY CENTRAL PWR & LGT","FORKED RVR",0,"LIGHT OIL",9726,"0M",1294,,,95,0,0,16388,1066,2219,17602,713,1618,15984,0,0,15971,0,0,15989,0,0,15969,0,0,15974,0,0,15980,0,0,15980,5,12,15970,0,0,15994,221,489,15505,7138,3,56512,"FO2","GT" 22,34,1,4,9,78,20,"JERSEY CENTRAL PWR & LGT","FORKED RVR",0,"NAT GAS",9726,"0M",1294,,,95,364,4569,0,160,1908,0,1306,15609,0,1647,20147,0,1120,14174,0,2225,28309,0,12875,162923,0,11844,149957,0,4227,53220,0,1880,23454,0,1759,25611,0,749,9475,0,7138,3,56512,"NG","GT" 22,34,1,2,1,131,1,"PUBLIC SERV ELEC & GAS CO","SALEM",0,"NUCLEAR",15477,"0M",1294,,,95,818199,0,0,47631,0,0,687443,0,0,753981,0,0,247176,0,0,-8310,0,0,-7985,0,0,-5500,0,0,-3133,0,0,-2112,0,0,-2002,0,0,-2639,0,0,2410,3,52414,"UR","ST" 22,34,1,2,1,131,1,"PUBLIC SERV ELEC & GAS CO","HOPE CREEK",0,"NUCLEAR",15477,"0M",1294,,,95,778188,0,0,711976,0,0,566874,0,0,750262,0,0,767051,0,0,742345,0,0,309223,0,0,760021,0,0,742281,0,0,733449,0,0,210606,0,0,-8357,0,0,6118,3,52414,"UR","ST" 22,34,1,2,1,131,2,"PUBLIC SERV ELEC & GAS CO","SALEM",0,"NUCLEAR",15477,"0M",1294,,,95,-17867,0,0,12090,0,0,369001,0,0,767911,0,0,765246,0,0,157494,0,0,-5523,0,0,-7400,0,0,-4042,0,0,-4499,0,0,-4002,0,0,-3638,0,0,2410,3,52414,"UR","ST" 22,34,1,4,2,131,2,"PUBLIC SERV ELEC & GAS CO","BAYONNE 1",0,"LIGHT OIL",15477,"0M",1294,,,95,-19,40,3837,74,282,453,-9,0,453,-44,0,1097,-18,0,3930,-2,0,3930,252,805,3125,134,585,2744,-24,0,3373,-42,0,3744,0,26,3744,-33,25,3898,2397,3,52414,"FO2","GT" 22,34,1,2,9,131,3,"PUBLIC SERV ELEC & GAS CO","BERGEN",0,"NAT GAS",15477,"0M",1294,,,95,-2112,0,0,-2514,3702,0,8759,159907,0,3706,93882,0,82739,754972,0,167861,1271630,0,281448,2131152,0,334990,2488678,0,184434,1379778,0,154884,1248547,0,151551,1232638,0,151368,1176288,0,2398,3,52414,"NG","ST" 22,34,1,4,2,131,3,"PUBLIC SERV ELEC & GAS CO","BERGEN",0,"LIGHT OIL",15477,"0M",1294,,,95,0,0,0,0,0,21622,0,0,21622,0,0,38592,0,0,38592,0,0,61623,2310,3197,102565,0,0,118429,0,0,118396,3765,5367,113029,4832,7091,116664,465,652,117805,2398,3,52414,"FO2","GT" 22,34,1,4,9,131,3,"PUBLIC SERV ELEC & GAS CO","BERGEN",0,"NAT GAS",15477,"0M",1294,,,95,-13,0,0,0,0,0,-6,664,0,-6,644,0,-9,0,0,0,0,0,347,35845,0,505,5090,0,0,0,0,-7,0,0,-7,0,0,-8,0,0,2398,3,52414,"NG","GT" 22,34,1,2,2,131,5,"PUBLIC SERV ELEC & GAS CO","BURLINGTON",0,"LIGHT OIL",15477,"0M",1294,,,95,922,1740,0,1014,1683,0,707,1131,0,668,1366,0,0,0,0,911,1528,0,1631,2761,0,200,501,0,0,0,0,0,0,0,0,0,0,0,0,0,2399,3,52414,"FO2","ST" 22,34,1,2,3,131,5,"PUBLIC SERV ELEC & GAS CO","BURLINGTON",0,"HEAVY OIL",15477,"0M",1294,,,95,9046,15688,55522,11250,17153,88452,0,0,88452,0,0,88452,-534,0,88437,2949,4515,83916,25958,40320,43596,1803,5025,88868,-545,0,88868,-541,0,88868,-541,0,88868,-573,0,88868,2399,3,52414,"FO6","ST" 22,34,1,4,2,131,5,"PUBLIC SERV ELEC & GAS CO","BURLINGTON",0,"LIGHT OIL",15477,"0M",1294,,,95,1176,2221,83444,10436,17314,64340,158,253,93381,55,114,91811,-75,14,91811,57,96,90581,102,173,81026,4040,11276,88868,-82,16,87601,-75,58,86367,29,348,84382,4578,8912,83631,2399,3,52414,"FO2","GT" 22,34,1,4,9,131,5,"PUBLIC SERV ELEC & GAS CO","BURLINGTON",0,"NAT GAS",15477,"0M",1294,,,95,60222,642634,0,62039,580691,0,60695,548854,0,9404,108237,0,42361,363894,0,31693,299006,0,63357,605299,0,60174,537745,0,21155,187254,0,17575,158420,0,24156,217635,0,18363,172905,0,2399,3,52414,"NG","GT" 22,34,1,6,2,131,5,"PUBLIC SERV ELEC & GAS CO","BURLINGTON",0,"LIGHT OIL",15477,"0M",894,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,144,235,0,0,0,0,0,0,0,0,0,0,0,0,0,2399,3,52414,"FO2","CT" 22,34,1,4,2,131,7,"PUBLIC SERV ELEC & GAS CO","EDISON",0,"LIGHT OIL",15477,"0M",1294,,,95,152,366,106308,281,513,105795,252,403,105392,7,135,105257,0,0,105257,88,644,104610,675,1783,102827,687,1976,100851,0,0,110803,0,0,110803,126,444,110359,742,2206,108153,2400,3,52414,"FO2","GT" 22,34,1,4,9,131,7,"PUBLIC SERV ELEC & GAS CO","EDISON",0,"NAT GAS",15477,"0M",1294,,,95,-33,582,0,70,992,0,-80,345,0,0,0,0,-162,750,0,0,0,0,3046,44211,0,2441,36716,0,-100,537,0,120,3310,0,89,2079,0,28,428,0,2400,3,52414,"NG","GT" 22,34,1,4,2,131,8,"PUBLIC SERV ELEC & GAS CO","ESSEX",0,"LIGHT OIL",15477,"0M",1294,,,95,0,0,112211,4598,10660,104446,0,0,104446,0,0,103802,0,0,96326,4,10,91990,0,0,91990,0,0,91990,0,0,112914,2,185,112914,234,400,112327,894,2118,110210,2401,3,52414,"FO2","GT" 22,34,1,4,9,131,8,"PUBLIC SERV ELEC & GAS CO","ESSEX",0,"NAT GAS",15477,"0M",1294,,,95,20171,250330,0,38746,466002,0,28312,330527,0,6195,75506,0,7086,87770,0,17745,236062,0,65291,864255,0,62756,803138,0,18682,243317,0,3599,40505,0,3163,40505,0,1420,2118,0,2401,3,52414,"NG","GT" 22,34,1,2,2,131,13,"PUBLIC SERV ELEC & GAS CO","HUDSON",0,"LIGHT OIL",15477,"0M",1294,,,95,119,251,0,0,0,0,0,0,0,0,0,0,0,0,0,3,6,0,4,9,0,4,9,0,0,0,0,0,0,0,0,0,0,0,0,0,2403,3,52414,"FO2","ST" 22,34,1,2,3,131,13,"PUBLIC SERV ELEC & GAS CO","HUDSON",0,"HEAVY OIL",15477,"0M",1294,,,95,11188,21576,147242,40039,87268,59974,0,0,59974,158,379,13064,0,0,13064,0,0,13064,0,0,13064,0,0,0,0,0,0,0,0,0,0,0,0,-2401,3164,109182,2403,3,52414,"FO6","ST" 22,34,1,2,6,131,13,"PUBLIC SERV ELEC & GAS CO","HUDSON",0,"BIT COAL",15477,"0M",1294,,,95,0,0,239403,0,0,239403,46093,19713,219690,82549,35226,208484,158939,68702,225010,141427,62425,162585,235608,99546,193639,263396,110928,173063,10310,4383,258904,0,0,349753,57703,21908,369380,339660,132744,293504,2403,3,52414,"BIT","ST" 22,34,1,2,9,131,13,"PUBLIC SERV ELEC & GAS CO","HUDSON",0,"NAT GAS",15477,"0M",1294,,,95,30599,362930,0,7194,97478,0,122788,1378604,0,43966,500739,0,16188,203737,0,20750,232325,0,137870,1458255,0,96187,1102638,0,1254,45160,0,-3375,2793,0,356,3383,0,1493,16683,0,2403,3,52414,"NG","ST" 22,34,1,4,2,131,13,"PUBLIC SERV ELEC & GAS CO","HUDSON",0,"LIGHT OIL",15477,"0M",1294,,,95,119,251,352215,256,609,34606,-63,0,34606,-54,0,34597,-48,0,34597,0,0,34597,1239,2320,32262,396,2283,29962,-50,0,29962,-46,0,29962,-55,0,29962,-71,0,29959,2403,3,52414,"FO2","GT" 22,34,1,4,9,131,13,"PUBLIC SERV ELEC & GAS CO","HUDSON",0,"NAT GAS",15477,"0M",1294,,,95,0,0,0,7,103,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3,38,0,0,0,0,0,0,0,0,0,0,0,0,0,2403,3,52414,"NG","GT" 22,34,1,2,2,131,16,"PUBLIC SERV ELEC & GAS CO","KEARNY",0,"LIGHT OIL",15477,"0M",1294,,,95,0,0,0,47,160,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2404,3,52414,"FO2","ST" 22,34,1,2,3,131,16,"PUBLIC SERV ELEC & GAS CO","KEARNY",0,"HEAVY OIL",15477,"0M",1294,,,95,-1419,0,47358,3162,9747,46218,-1264,0,46218,-811,0,43218,-763,0,46218,2322,7151,47602,25660,53229,45133,22324,46979,41775,-837,0,41775,-758,0,41755,-1135,0,41775,-1308,0,46698,2404,3,52414,"FO6","ST" 22,34,1,4,2,131,16,"PUBLIC SERV ELEC & GAS CO","KEARNY",0,"LIGHT OIL",15477,"0M",1294,,,95,375,941,65441,656,2205,61502,0,175,60444,-48,459,59831,-54,459,66419,-11,40,64109,2241,5425,58552,1592,6227,53502,-37,0,73227,-117,0,73054,-84,226,71810,-19,331,69761,2404,3,52414,"FO2","GT" 22,34,1,4,9,131,16,"PUBLIC SERV ELEC & GAS CO","KEARNY",0,"NAT GAS",15477,"0M",1294,,,95,778,10891,0,531,10070,0,-183,586,0,-132,928,0,-131,324,0,1324,24641,0,4064,67350,0,6293,99804,0,-119,0,0,-6,0,0,-8,139,0,-23,0,0,2404,3,52414,"NG","GT" 22,34,1,2,3,131,18,"PUBLIC SERV ELEC & GAS CO","LINDEN",0,"HEAVY OIL",15477,"0M",1294,,,95,-2975,0,169370,18699,47791,121579,1724,8149,41900,-1941,0,88431,-2550,0,88431,1771,15138,11078,59268,130643,95281,51534,115049,125814,-2711,0,128815,-1641,0,126134,-2551,10434,115700,-1747,0,115700,2406,3,52414,"FO6","ST" 22,34,1,4,2,131,18,"PUBLIC SERV ELEC & GAS CO","LINDEN",0,"LIGHT OIL",15477,"0M",1294,,,95,26,253,53370,313,1361,52009,448,1157,50882,3498,6627,44255,6478,14170,30085,0,0,30085,0,0,30085,564,1160,28925,0,0,49924,-37,195,49604,202,372,49037,451,1756,51571,2406,3,52414,"FO2","GT" 22,34,1,4,9,131,18,"PUBLIC SERV ELEC & GAS CO","LINDEN",0,"NAT GAS",15477,"0M",1294,,,95,-96,0,0,43,2616,0,3961,49847,0,1854,18696,0,15141,180135,0,13553,160573,0,33255,393680,0,32192,409006,0,8666,121819,0,8374,103539,0,3980,41596,0,1468,15561,0,2406,3,52414,"NG","GT" 22,34,1,2,6,131,22,"PUBLIC SERV ELEC & GAS CO","MERCER",0,"BIT COAL",15477,"0M",1294,,,95,260338,90961,263541,283481,98338,252219,105820,38401,312566,69927,25278,364038,58034,23857,399943,121372,47152,419711,144178,55677,392291,111773,44297,360087,169493,64917,301841,40666,17201,334307,135703,47712,346850,209008,71876,359245,2408,3,52414,"BIT","ST" 22,34,1,2,9,131,22,"PUBLIC SERV ELEC & GAS CO","MERCER",0,"NAT GAS",15477,"0M",1294,,,95,15072,160572,0,10698,100608,0,12860,134613,0,17393,171693,0,23606,242604,0,33578,373796,0,130882,1357300,0,110572,1186167,0,12727,142016,0,7184,77196,0,1387,12188,0,362,30224,0,2408,3,52414,"NG","ST" 22,34,1,4,2,131,22,"PUBLIC SERV ELEC & GAS CO","MERCER",0,"LIGHT OIL",15477,"0M",1294,,,95,58,452,0,99,166,0,-80,45,0,-80,22,0,-90,0,0,-84,0,0,174,1003,0,1250,2375,0,-74,0,0,-89,0,0,-86,0,0,65,504,0,2408,3,52414,"FO2","GT" 22,34,1,4,9,131,22,"PUBLIC SERV ELEC & GAS CO","MERCER",0,"NAT GAS",15477,"0M",1294,,,95,0,0,0,11,107,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,23,252,0,0,0,0,0,0,0,0,0,0,0,0,0,2408,3,52414,"NG","GT" 22,34,1,4,2,131,24,"PUBLIC SERV ELEC & GAS CO","NATIONAL PK",0,"LIGHT OIL",15477,"0M",1294,,,95,-7,0,2850,-5,0,2850,-6,0,168,-6,0,167,-7,0,1390,-6,0,3548,-6,0,3548,33,67,3481,-6,0,3481,3,25,3456,2,22,3434,-6,0,3434,2409,3,52414,"FO2","GT" 22,34,1,2,3,131,25,"PUBLIC SERV ELEC & GAS CO","SEWAREN",0,"HEAVY OIL",15477,"0M",1294,,,95,915,2021,98313,16425,33366,104241,341,778,103613,0,0,103613,1016,2372,101241,0,0,101241,128,279,100962,2211,4787,96175,4969,9343,86832,2764,7861,78971,2025,6536,72435,11423,30324,105394,2411,3,52414,"FO6","ST" 22,34,1,2,9,131,25,"PUBLIC SERV ELEC & GAS CO","SEWAREN",0,"NAT GAS",15477,"0M",1294,,,95,30968,435199,0,63113,771440,0,13222,183529,0,3478,58360,0,10032,124996,0,30077,426413,0,86401,1129748,0,69754,958979,0,7865,101861,0,-868,15021,0,1354,26896,0,943,15389,0,2411,3,52414,"NG","ST" 22,34,1,4,2,131,25,"PUBLIC SERV ELEC & GAS CO","SEWAREN",0,"LIGHT OIL",15477,"0M",1294,,,95,51,704,34543,121,263,34280,-71,0,34280,-133,0,34280,-130,0,34280,-22,30,38575,438,1523,37052,831,2943,34109,-123,0,34109,-124,0,34109,23,82,34027,80,208,33819,2411,3,52414,"FO2","GT" 22,34,1,4,9,131,25,"PUBLIC SERV ELEC & GAS CO","SEWAREN",0,"NAT GAS",15477,"0M",1294,,,95,0,0,0,2,31,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,16,0,0,0,0,2411,3,52414,"NG","GT" 22,34,1,4,2,131,27,"PUBLIC SERV ELEC & GAS CO","SALEM JO",0,"LIGHT OIL",15477,"0M",1294,,,95,-18,3,16640,85,264,16528,-5,49,16528,-14,28,17721,-15,0,17581,0,0,17581,398,125,32262,152,455,31807,-6,0,16295,2764,7861,78971,-14,0,14970,54,170,12261,2410,3,52414,"FO2","GT" 22,34,5,2,3,645,1,"VINELAND (CITY OF)","HOWARD DOWN",0,"HEAVY OIL",19856,"0M",1294,,,95,0,0,24261,803,2139,23900,486,1664,22238,294,1029,21209,2656,6649,16338,890,2102,21318,4629,11673,9645,3246,7549,10200,0,0,10347,0,0,10397,0,0,10320,2429,6628,6595,2434,3,53140,"FO6","ST" 22,34,5,2,6,645,1,"VINELAND (CITY OF)","HOWARD DOWN",0,"BIT COAL",19856,"0M",1294,,,95,7844,4284,7953,7472,4143,6788,3415,1988,9938,0,0,9849,2186,1111,8737,7260,3928,6843,6950,3861,9709,3584,3042,7673,388,209,9251,1581,798,8709,5259,2954,5755,3724,2035,5931,2434,3,53140,"BIT","ST" 22,34,5,4,2,645,10,"VINELAND (CITY OF)","WEST",0,"LIGHT OIL",19856,"0M",1294,,,95,74,199,9430,353,887,8543,45,128,8417,0,0,8417,0,0,8417,315,901,7389,2079,6227,5808,2543,5808,3568,151,900,3206,36,73,3061,6,80,2981,129,339,2818,6776,3,53140,"FO2","GT" 23,42,1,2,1,52,1,"DUQUESNE LGT CO","B VALLEY",0,"NUCLEAR",5487,"0M",1294,,,95,17240,0,0,-6300,0,0,367420,0,0,596300,0,0,615700,0,0,589500,0,0,604900,0,0,561482,0,0,591490,0,0,614130,0,0,582150,0,0,452460,0,0,6040,1,50827,"UR","ST" 23,42,1,2,1,52,2,"DUQUESNE LGT CO","B VALLEY",0,"NUCLEAR",5487,"0M",1294,,,95,610052,0,0,558397,0,0,377306,0,0,-2502,0,0,358108,0,0,592883,0,0,609130,0,0,296500,0,0,598381,0,0,622939,0,0,557126,0,0,601216,0,0,6040,1,50827,"UR","ST" 23,42,1,2,6,52,5,"DUQUESNE LGT CO","CHESWICK",0,"BIT COAL",5487,"0M",1294,,,95,355392,137291,317861,331090,126419,307477,249582,96410,291500,17430,8507,318494,299247,119774,288017,339756,132948,261655,256633,102182,276100,296500,118467,263069,297357,118900,201464,311698,126308,186349,351416,139379,173501,306740,121467,188856,8226,1,50827,"BIT","ST" 23,42,1,2,9,52,5,"DUQUESNE LGT CO","CHESWICK",0,"NAT GAS",5487,"0M",1294,,,95,1427,13928,0,331,3531,0,1002,9220,0,1172,14418,0,1806,18532,0,1364,13508,0,1549,14158,0,2639,26716,0,2701,26104,0,1881,19412,0,1411,14459,0,1232,12044,0,8226,1,50827,"NG","ST" 23,42,1,2,2,52,13,"DUQUESNE LGT CO","ELRAMA",0,"LIGHT OIL",5487,"0M",1294,,,95,1941,3768,1508,1330,2779,1204,1589,3262,979,1253,2681,1633,1006,2112,1445,803,1634,1382,1389,3062,1487,1368,2719,1591,1136,2443,1644,986,1991,1570,898,1981,1539,1195,2526,782,3098,1,50827,"FO2","ST" 23,42,1,2,6,52,13,"DUQUESNE LGT CO","ELRAMA",0,"BIT COAL",5487,"0M",1294,,,95,240736,111790,172599,220356,101044,171860,197080,90684,191628,207597,94541,190808,200161,89633,171686,159939,73949,169611,197010,95313,150545,226664,107371,139013,188236,90982,151708,97661,45101,189092,223530,101521,181601,237771,106889,154459,3098,1,50827,"BIT","ST" 23,42,1,2,2,52,15,"DUQUESNE LGT CO","F PHILLIPS",0,"LIGHT OIL",5487,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3099,1,50827,"FO2","ST" 23,42,1,2,6,52,15,"DUQUESNE LGT CO","F PHILLIPS",0,"BIT COAL",5487,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3099,1,50827,"BIT","ST" 23,42,1,4,2,52,27,"DUQUESNE LGT CO","BRUNOT ILND",0,"LIGHT OIL",5487,"0M",1294,,,95,-733,567,24237,-801,692,23545,-848,9,23536,-662,220,23316,-662,0,23316,-579,460,22856,1005,4706,18150,5198,15710,17539,-587,0,19993,-604,0,19993,-808,0,19993,-777,582,20583,3096,1,50827,"FO2","GT" 23,42,1,5,2,52,27,"DUQUESNE LGT CO","BRUNOT ILND",0,"LIGHT OIL",5487,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3096,1,50827,"FO2","CC" 23,42,1,6,2,52,27,"DUQUESNE LGT CO","BRUNOT ILND",0,"LIGHT OIL",5487,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3096,1,50827,"FO2","CT" 23,42,1,2,1,100,1,"GPU NUCLEAR CORP","3 MI ISLAND",0,"NUCLEAR",7423,"0M",1294,,,95,611412,0,0,552321,0,0,609022,0,0,586279,0,0,599986,0,0,573186,0,0,584601,0,0,586748,0,0,144888,0,0,338797,0,0,590553,0,0,610193,0,0,8011,3,58850,"UR","ST" 23,42,1,1,,114,15,"METROPOLITAN EDISON CO","YORK HAVEN",0,,12390,"0M",1294,,,95,8890,0,0,9724,0,0,12867,0,0,10005,0,0,12383,0,0,12781,0,0,10950,0,0,1654,0,0,3141,0,0,8336,0,0,12409,0,0,9435,0,0,3117,3,54020,"WAT","HY" 23,42,1,4,2,114,24,"METROPOLITAN EDISON CO","HAMILTON",0,"LIGHT OIL",12390,"0M",1294,,,95,0,44,4643,342,858,4499,38,102,4397,28,68,4330,-2,0,4330,0,0,4330,432,1398,2932,1179,2884,2369,143,356,3085,0,0,3085,47,129,3491,190,511,4606,3109,3,54020,"FO2","GT" 23,42,1,4,2,114,25,"METROPOLITAN EDISON CO","HUNTERSTOWN",0,"LIGHT OIL",12390,"0M",1294,,,95,44,117,8244,904,2365,9808,139,361,9448,53,150,8583,0,1,8583,0,0,8582,1,3,8579,16,42,8895,2,7,9067,19,50,9017,7,22,8995,281,706,8304,3110,3,54020,"FO2","GT" 23,42,1,4,9,114,25,"METROPOLITAN EDISON CO","HUNTERSTOWN",0,"NAT GAS",12390,"0M",1294,,,95,1133,17680,0,1048,17830,0,7,180,0,729,13320,0,504,8500,0,1339,19320,0,3546,41940,0,6556,84500,0,3434,53290,0,1503,23470,0,1262,20430,0,1780,27282,0,3110,3,54020,"NG","GT" 23,42,1,4,2,114,27,"METROPOLITAN EDISON CO","MOUNTAIN",0,"LIGHT OIL",12390,"0M",1294,,,95,71,188,6429,964,2523,5157,48,126,5031,4,12,5912,0,0,5912,0,1,5911,0,2,5910,0,0,5910,36,175,5913,0,0,6270,0,2,6804,367,1234,6575,3111,3,54020,"FO2","GT" 23,42,1,4,9,114,27,"METROPOLITAN EDISON CO","MOUNTAIN",0,"NATURAL G",12390,"0M",1294,,,95,297,5940,0,476,8360,0,443,6390,0,469,7770,0,208,3710,0,328,5630,0,1743,26610,0,3541,53620,0,894,14500,0,170,2840,0,572,8810,0,1301,18260,0,3111,3,54020,"NG","GT" 23,42,1,4,2,114,31,"METROPOLITAN EDISON CO","ORRTANNA",0,"LIGHT OIL",12390,"0M",1294,,,95,48,116,4401,346,875,4418,88,218,4200,26,66,4135,0,0,4135,0,0,4135,593,1575,2917,1316,3402,1824,159,409,2667,26,65,3674,0,7,5453,229,581,4898,3112,3,54020,"FO2","GT" 23,42,1,2,2,114,32,"METROPOLITAN EDISON CO","PORTLAND",0,"LIGHT OIL",12390,"0M",1294,,,95,1210,2219,56721,612,1085,51313,671,1307,49944,1587,3013,45429,432,812,42830,190,349,41500,955,1701,39591,434,783,37499,499,951,35882,161,335,60358,2066,4127,57233,222,397,56872,3113,3,54020,"FO2","ST" 23,42,1,2,6,114,32,"METROPOLITAN EDISON CO","PORTLAND",0,"BIT COAL",12390,"0M",1294,,,95,132808,53399,109521,182821,71489,66961,66747,28478,108572,54477,22914,130642,57698,23989,150827,144768,58703,134821,179344,71804,85267,178789,70856,51093,83228,35019,46481,11852,5425,93489,58689,25583,120272,183470,71507,85462,3113,3,54020,"BIT","ST" 23,42,1,4,2,114,32,"METROPOLITAN EDISON CO","PORTLAND",0,"LIGHT OIL",12390,"0M",1294,,,95,77,142,2671,1704,3020,3973,50,98,3938,790,1501,3938,951,1787,3938,662,1215,3705,281,501,3412,727,1310,3410,2125,4049,3409,1,3,3407,122,245,3406,1839,3288,3291,3113,3,54020,"FO2","GT" 23,42,1,4,9,114,32,"METROPOLITAN EDISON CO","PORTLAND",0,"NAT GAS",12390,"0M",1294,,,95,7,72,0,1596,15661,0,2973,32178,0,2051,22130,0,3978,42351,0,12035,125176,0,33248,336088,0,28922,295790,0,5224,56353,0,750,8818,0,2029,22553,0,597,5955,0,3113,3,54020,"NG","GT" 23,42,1,4,2,114,34,"METROPOLITAN EDISON CO","SHAWNEE",0,"LIGHT OIL",12390,"0M",1294,,,95,73,171,6099,265,687,6483,16,27,6472,20,60,6412,44,112,6301,35,90,6211,135,371,5839,869,2245,3594,68,177,3417,0,0,4845,68,117,5622,0,0,5679,3114,3,54020,"FO2","GT" 23,42,1,2,2,114,35,"METROPOLITAN EDISON CO","TITUS",0,"LIGHT OIL",12390,"0M",1294,,,95,102,198,885,73,138,926,387,772,869,487,933,1186,472,874,1205,168,334,1228,294,559,1026,220,409,617,291,530,803,369,699,998,321,614,560,227,431,880,3115,3,54020,"FO2","ST" 23,42,1,2,6,114,35,"METROPOLITAN EDISON CO","TITUS",0,"BIT COAL",12390,"0M",1294,,,95,73788,31030,99475,51570,21149,100003,47245,20126,101173,38103,15904,107895,66063,26455,103387,95872,40846,84743,118659,48529,57453,118052,46687,37871,105060,41177,26170,83805,34936,50826,103029,42373,57757,128752,52966,41217,3115,3,54020,"BIT","ST" 23,42,1,4,2,114,35,"METROPOLITAN EDISON CO","TITUS",0,"LIGHT OIL",12390,"0M",1294,,,95,58,114,4000,793,1492,4117,0,0,4117,1,2,4115,0,0,4115,4,8,4106,65,124,3983,133,248,3983,0,0,3983,131,248,3734,20,39,3695,0,0,3755,3115,3,54020,"FO2","GT" 23,42,1,4,9,114,35,"METROPOLITAN EDISON CO","TITUS",0,"NAT GAS",12390,"0M",1294,,,95,53,575,0,23,240,0,80,890,0,60,640,0,52,541,0,22,250,0,1587,16770,0,2936,30250,0,319,3230,0,110,1190,0,149,1590,0,5,60,0,3115,3,54020,"NG","GT" 23,42,1,4,2,114,38,"METROPOLITAN EDISON CO","TOLNA",0,"LIGHT OIL",12390,"0M",1294,,,95,68,175,6400,563,1516,6278,90,224,6054,0,1,6053,0,0,6053,0,0,6053,759,2033,4020,2323,6134,2677,164,447,5438,64,349,6339,62,101,6238,114,281,6229,3116,3,54020,"FO2","GT" 23,42,1,2,2,133,1,"PENNSYLVANIA ELEC CO","CONMAUGH JO",0,"LIGHT OIL",14711,"0M",1294,,250,95,514,827,5361,559,930,4122,454,736,6813,810,1319,5181,459,747,4344,78,121,4153,878,1456,2385,538,892,3017,74,121,5479,0,0,5356,3148,5217,7748,383,627,6559,3118,3,54025,"FO2","ST" 23,42,1,2,6,133,1,"PENNSYLVANIA ELEC CO","CONMAUGH JO",0,"BIT COAL",14711,"0M",1294,,250,95,1122156,419851,722958,925303,359096,640938,1076935,406220,574117,992331,375372,600365,1073542,404411,660222,1082614,409954,586984,1087889,419782,543363,1144736,439047,524854,727433,274855,587632,579871,221827,735222,799742,308937,733868,1107177,421853,608881,3118,3,54025,"BIT","ST" 23,42,1,2,9,133,1,"PENNSYLVANIA ELEC CO","CONMAUGH JO",0,"NAT GAS",14711,"0M",1294,,250,95,1516,13798,0,1026,9654,0,566,5184,0,1707,15719,0,1710,15719,0,264,2319,0,2347,22035,0,3446,32313,0,452,4120,0,258,2408,0,2434,22766,0,571,5283,0,3118,3,54025,"NG","ST" 23,42,1,3,2,133,1,"PENNSYLVANIA ELEC CO","CONMAUGH JO",0,"LIGHT OIL",14711,"0M",1294,,250,95,59,96,0,34,57,0,59,97,0,181,295,0,54,89,0,45,71,0,187,311,0,146,243,0,46,75,0,31,52,0,78,130,0,46,76,0,3118,3,54025,"FO2","IC" 23,42,1,1,,133,5,"PENNSYLVANIA ELEC CO","PINEY",0,,14711,"0M",1294,,250,95,7087,0,0,2980,0,0,8315,0,0,7025,0,0,7405,0,0,7866,0,0,1807,0,0,900,0,0,618,0,0,1506,0,0,5259,0,0,4760,0,0,3124,3,54025,"WAT","HY" 23,42,1,1,,133,13,"PENNSYLVANIA ELEC CO","SENECA JO",0,"C-PUMPSTG",14711,"0M",1294,,250,95,-18038,60718,0,-12762,44459,0,-13759,53339,0,-14476,46086,0,-10189,43886,0,-20535,71955,0,-32632,124316,0,-31819,130160,0,-23462,98242,0,-26851,110227,0,-17180,96885,0,-19235,101307,0,8225,3,54025,"WAT","HY" 23,42,1,4,9,133,17,"PENNSYLVANIA ELEC CO","BLOSSBURG",0,"NAT GAS",14711,"0M",1294,,250,95,-5,0,0,248,3769,0,-4,0,0,0,0,0,0,0,0,0,0,0,502,7485,0,846,9556,0,243,7354,0,-5,0,0,-4,0,0,-4,0,0,3120,3,54025,"NG","GT" 23,42,1,2,2,133,25,"PENNSYLVANIA ELEC CO","HOMER CTYJO",0,"LIGHT OIL",14711,"0M",1294,,250,95,724,1106,10724,239,368,10825,1397,2089,8613,678,1026,8717,2469,3709,5517,3227,5084,7324,1158,1765,5736,474,737,6933,1569,3909,7274,769,1187,8528,7523,12170,9104,4070,6343,6965,3122,3,54025,"FO2","ST" 23,42,1,2,6,133,25,"PENNSYLVANIA ELEC CO","HOMER CTYJO",0,"BIT COAL",14711,"0M",1294,,250,95,1185616,454082,568142,1188794,455176,479305,1210546,457862,391125,1087359,409749,340123,685495,258590,520058,1050104,414471,562956,1147586,445483,356766,1213094,474606,228657,448257,271599,331273,758425,290978,460056,823682,334855,431770,991225,388795,409243,3122,3,54025,"BIT","ST" 23,42,1,2,2,133,45,"PENNSYLVANIA ELEC CO","SEWARD",0,"LIGHT OIL",14711,"0M",1294,,250,95,662,1281,675,306,595,618,281,535,616,145,261,535,122,305,409,432,940,535,285,552,414,274,531,585,416,789,657,463,878,671,432,834,724,340,657,600,3130,3,54025,"FO2","ST" 23,42,1,2,6,133,45,"PENNSYLVANIA ELEC CO","SEWARD",0,"BIT COAL",14711,"0M",1294,,250,95,101596,46820,104963,110101,50567,86392,110470,50520,76721,54307,23628,78208,29270,17347,91227,52721,27510,83682,115539,53769,77789,119322,55517,67991,102723,46904,73094,107866,49063,74467,105367,48397,85472,116951,53923,61526,3130,3,54025,"BIT","ST" 23,42,1,2,2,133,48,"PENNSYLVANIA ELEC CO","SHAWVILLE",0,"LIGHT OIL",14711,"0M",1294,,250,95,1123,1920,8833,2602,4605,6882,3250,5700,8490,1312,2317,8459,872,1542,9545,917,1633,7965,912,1584,7411,1122,2141,8065,1665,3195,7890,1607,2973,8086,2444,4275,8035,3504,6399,6379,3131,3,54025,"FO2","ST" 23,42,1,2,6,133,48,"PENNSYLVANIA ELEC CO","SHAWVILLE",0,"BIT COAL",14711,"0M",1294,,250,95,269348,109338,102763,256827,107901,105884,326710,136132,96046,350160,145852,80632,328883,137262,84982,336010,141689,79617,350851,144610,79435,304942,138068,76369,248206,112475,83476,317261,138069,65107,346273,142913,61290,323453,141293,48123,3131,3,54025,"BIT","ST" 23,42,1,3,2,133,48,"PENNSYLVANIA ELEC CO","SHAWVILLE",0,"LIGHT OIL",14711,"0M",1294,,250,95,31,54,764,42,75,689,26,47,797,22,39,757,20,37,721,29,52,669,42,74,740,203,388,705,22,43,662,24,46,763,18,32,731,24,44,819,3131,3,54025,"FO2","IC" 23,42,1,2,2,133,60,"PENNSYLVANIA ELEC CO","WARREN",0,"LIGHT OIL",14711,"0M",1294,,250,95,101,246,375,38,94,281,58,147,313,65,158,336,29,123,391,38,93,297,45,104,725,30,76,657,8,20,637,47,126,511,41,109,402,38,97,482,3132,3,54025,"FO2","ST" 23,42,1,2,6,133,60,"PENNSYLVANIA ELEC CO","WARREN",0,"BIT COAL",14711,"0M",1294,,250,95,23223,13460,34201,30943,18008,26672,17000,10379,34033,20947,11998,35372,16865,16419,30837,28698,16502,23133,35556,19496,14235,32084,18799,17943,18322,10742,21117,17556,10786,25392,16779,10295,31120,32207,19202,23049,3132,3,54025,"BIT","ST" 23,42,1,4,2,133,60,"PENNSYLVANIA ELEC CO","WARREN",0,"LIGHT OIL",14711,"0M",1294,,250,95,2,7,9205,924,2260,9835,124,314,9521,0,1,9519,94,389,9130,154,374,8757,2078,4788,7154,3447,8693,6033,514,1272,7934,0,0,7934,105,276,7658,393,986,9466,3132,3,54025,"FO2","GT" 23,42,1,4,9,133,60,"PENNSYLVANIA ELEC CO","WARREN",0,"NAT GAS",14711,"0M",1294,,250,95,0,10,0,0,10,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3132,3,54025,"NG","GT" 23,42,1,3,2,133,75,"PENNSYLVANIA ELEC CO","BENTON",0,"LIGHT OIL",14711,"0M",1294,"R",250,95,-3,0,0,-2,0,0,-3,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3119,3,54025,"FO2","IC" 23,42,1,4,2,133,87,"PENNSYLVANIA ELEC CO","WAYNE",0,"LIGHT OIL",14711,"0M",1294,,250,95,-99,18,20263,508,1505,18758,-92,0,18758,-86,0,18758,-70,1,18757,-54,0,18757,1349,3469,15288,3798,9355,11397,490,1027,13199,-52,0,13199,141,1098,14037,154,691,18031,3134,3,54025,"FO2","GT" 23,42,1,2,2,133,90,"PENNSYLVANIA ELEC CO","KEYSTONE JO",0,"LIGHT OIL",14711,"0M",1294,,250,95,2244,3690,6503,1272,2084,8137,0,0,8969,4533,7554,9207,714,1204,9434,965,1623,9346,2145,3684,9013,3083,5243,9005,923,1553,9324,753,1254,8496,1264,2066,8810,0,0,8724,3136,3,54025,"FO2","ST" 23,42,1,2,6,133,90,"PENNSYLVANIA ELEC CO","KEYSTONE JO",0,"BIT COAL",14711,"0M",1294,,250,95,1102214,423987,311858,582793,225211,453587,563417,222247,605342,809149,315890,648804,1078337,426399,648546,1084349,429852,601163,1034268,420581,454702,938657,378854,582342,1033031,410618,649687,1088547,426659,795799,1058746,408591,711979,1180880,456067,560683,3136,3,54025,"BIT","ST" 23,42,1,3,2,133,90,"PENNSYLVANIA ELEC CO","KEYSTONE JO",0,"LIGHT OIL",14711,"0M",1294,,250,95,349,575,0,349,573,0,34,59,0,204,341,0,100,170,0,35,60,0,207,356,0,870,1480,0,155,262,0,66,110,0,178,291,0,46,86,0,3136,3,54025,"FO2","IC" 23,42,1,2,2,135,1,"PENNSYLVANIA POWER CO","NEW CASTLE",0,"LIGHT OIL",14716,"0M",1294,,,95,157,295,104,61,118,158,276,532,107,184,352,158,327,657,138,250,493,138,176,344,140,152,297,106,171,327,131,192,372,116,117,218,145,156,288,161,3138,1,52289,"FO2","ST" 23,42,1,2,6,135,1,"PENNSYLVANIA POWER CO","NEW CASTLE",0,"BIT COAL",14716,"0M",1294,,,95,167856,72057,99647,154279,67443,98213,130534,58811,77871,125682,55847,86191,67772,31976,90113,98557,45757,95531,118202,53998,90022,140629,64008,74786,116270,52148,73949,88872,40250,91385,140709,61724,82726,150687,61716,63171,3138,1,52289,"BIT","ST" 23,42,1,3,2,135,1,"PENNSYLVANIA POWER CO","NEW CASTLE",0,"LIGHT OIL",14716,"0M",1294,,,95,22,56,1012,6,7,1012,7,22,863,1,3,991,4,9,875,1,7,1095,68,120,980,348,650,769,21,48,895,12,25,914,9,4,978,1,5,846,3138,1,52289,"FO2","IC" 23,42,1,2,2,135,12,"PENNSYLVANIA POWER CO","MANSFLD JO",0,"LIGHT OIL",14716,"0M",1294,,,95,1007,1692,29171,723,1155,27861,1506,2563,20232,2103,3540,37005,3377,5991,30895,1363,2382,49447,1396,2364,47084,1578,2757,44327,1128,2011,40209,852,1442,3868,625,1076,37528,5978,10675,26852,6094,1,52289,"FO2","ST" 23,42,1,2,6,135,12,"PENNSYLVANIA POWER CO","MANSFLD JO",0,"BIT COAL",14716,"0M",1294,,,95,1000025,404047,691181,900788,348267,715644,764097,314521,842427,1018498,413184,894368,1102944,466816,876286,1268001,530524,794307,1358940,556273,756092,1346419,567300,719388,816664,349651,802659,889136,365870,922037,897824,373667,888666,766127,330985,1035343,6094,1,52289,"BIT","ST" 23,42,1,2,1,137,1,"PENNSYLVANIA PWR & LGT CO","SUSQUEHANNA",0,"NUCLEAR",14715,"0M",1294,,,95,784581,0,0,707744,0,0,597267,0,0,-6623,0,0,455272,0,0,764570,0,0,800626,0,0,807866,0,0,781516,0,0,816456,0,0,256044,0,0,663200,0,0,6103,3,52288,"UR","ST" 23,42,1,2,1,137,2,"PENNSYLVANIA PWR & LGT CO","SUSQUEHANNA",0,"NUCLEAR",14715,"0M",1294,,,95,819260,0,0,744537,0,0,809836,0,0,572523,0,0,800757,0,0,763767,0,0,784244,0,0,790491,0,0,327567,0,0,158303,0,0,801099,0,0,820399,0,0,6103,3,52288,"UR","ST" 23,42,1,1,,137,8,"PENNSYLVANIA PWR & LGT CO","HOLTWOOD",0,,14715,"0M",1294,,,95,63368,0,0,44815,0,0,66767,0,0,61784,0,0,47914,0,0,44060,0,0,38745,0,0,15029,0,0,8892,0,0,3395,0,0,54454,0,0,52183,0,0,3145,3,52288,"WAT","HY" 23,42,1,2,2,137,8,"PENNSYLVANIA PWR & LGT CO","HOLTWOOD",0,"LIGHT OIL",14715,"0M",1294,,,95,2,293,307,92,564,453,76,299,502,6,12,486,9,103,375,64,316,412,48,185,402,32,69,513,156,340,542,105,324,374,44,96,457,71,158,639,3145,3,52288,"FO2","ST" 23,42,1,2,4,137,8,"PENNSYLVANIA PWR & LGT CO","HOLTWOOD",0,"ANTH COAL",14715,"0M",1294,,,95,16657,10967,92177,28295,20094,81874,38352,28374,83310,37995,26901,93553,28887,20504,97262,21957,15483,110941,27038,19535,107719,38254,26848,105902,36692,25935,106839,27783,20333,110563,38411,27438,93901,40473,29360,79473,3145,3,52288,"ANT","ST" 23,42,1,2,5,137,8,"PENNSYLVANIA PWR & LGT CO","HOLTWOOD",0,"COKE",14715,"0M",1294,,,95,5600,3687,7954,10386,7347,6463,12376,9136,6569,13390,9479,6750,10455,7419,8863,7778,5469,5689,9256,6676,3115,13170,9235,2168,11989,8438,3400,7495,5464,2289,8623,7102,1550,11704,5956,0,3145,3,52288,"PC","ST" 23,42,1,1,,137,14,"PENNSYLVANIA PWR & LGT CO","WALLENPAUPK",0,,14715,"0M",1294,,,95,12278,0,0,38773,0,0,4171,0,0,-24207,0,0,735,0,0,560,0,0,5204,0,0,2717,0,0,244,0,0,24,0,0,11908,0,0,11545,0,0,3153,3,52288,"WAT","HY" 23,42,1,4,2,137,15,"PENNSYLVANIA PWR & LGT CO","ALLENTOWN",0,"LIGHT OIL",14715,"0M",1294,,,95,64,195,4597,200,523,4444,0,0,4446,40,90,4355,0,0,4356,122,333,4024,199,561,4006,2797,7611,4017,44,168,4389,12,34,4355,0,0,4351,134,369,4531,3139,3,52288,"FO2","GT" 23,42,1,2,2,137,20,"PENNSYLVANIA PWR & LGT CO","BRUNNER ISL",0,"LIGHT OIL",14715,"0M",1294,,,95,5215,9667,5220,2811,6985,2945,2623,7457,4341,1006,3274,4688,1673,5855,4747,623,3511,4635,1145,3027,3800,192,491,4638,1850,4455,1752,956,1998,4421,1497,3195,3955,6348,15226,4765,3140,3,52288,"FO2","ST" 23,42,1,2,6,137,20,"PENNSYLVANIA PWR & LGT CO","BRUNNER ISL",0,"BIT COAL",14715,"0M",1294,,,95,726861,278333,624176,797416,299207,615563,638681,243796,659948,618218,235042,726562,483331,182515,843219,636052,246917,774595,729927,280541,565746,770922,293672,454478,661164,258193,418744,632910,240757,448356,500569,201629,451028,542332,211139,476821,3140,3,52288,"BIT","ST" 23,42,1,3,2,137,20,"PENNSYLVANIA PWR & LGT CO","BRUNNER ISL",0,"LIGHT OIL",14715,"0M",1294,,,95,43,75,0,27,35,0,29,50,0,11,33,0,29,50,0,27,47,0,38,66,0,41,123,0,30,52,0,27,47,0,21,37,0,28,47,0,3140,3,52288,"FO2","IC" 23,42,1,4,2,137,26,"PENNSYLVANIA PWR & LGT CO","FISHBACH",0,"LIGHT OIL",14715,"0M",1294,,,95,0,0,2203,37,115,2088,0,0,2076,11,33,2043,0,0,2039,16,52,1987,102,265,2080,1274,3289,1978,63,218,2105,0,0,2095,0,0,2105,13,33,2071,3142,3,52288,"FO2","GT" 23,42,1,4,2,137,28,"PENNSYLVANIA PWR & LGT CO","HARWOOD",0,"LIGHT OIL",14715,"0M",1294,,,95,0,0,2216,83,240,2157,0,0,2152,44,152,2171,0,0,2171,13,61,2272,289,883,2098,1064,3093,1958,134,415,2230,60,205,2217,0,0,2217,0,0,2208,3144,3,52288,"FO2","GT" 23,42,1,4,2,137,29,"PENNSYLVANIA PWR & LGT CO","HARRISBURG",0,"LIGHT OIL",14715,"0M",1294,,,95,0,0,4184,328,916,4530,0,0,4528,34,103,4425,7,31,4394,111,326,4426,221,659,4486,3286,9229,3610,329,960,4424,0,0,4424,8,0,4410,101,283,4486,3143,3,52288,"FO2","GT" 23,42,1,2,2,137,32,"PENNSYLVANIA PWR & LGT CO","MARTINS CRK",0,"LIGHT OIL",14715,"0M",1294,,,95,1397,3966,1367,1654,3961,905,487,1818,1153,845,3118,1197,886,4111,1282,1222,4052,1400,1679,4825,803,2026,5349,775,303,753,1408,633,2680,1365,1511,3919,1485,2510,5735,1078,3148,3,52288,"FO2","ST" 23,42,1,2,3,137,32,"PENNSYLVANIA PWR & LGT CO","MARTINS CRK",0,"HEAVY OIL",14715,"0M",1294,,,95,3313,20105,1792976,137098,246817,1537637,4594,16136,1518993,7837,26024,1486208,0,0,1482804,46574,94076,1387076,225007,410380,970823,241933,469387,1094662,32635,57250,1132457,11373,23775,1505839,59422,125764,1590347,265457,506756,1125474,3148,3,52288,"FO6","ST" 23,42,1,2,6,137,32,"PENNSYLVANIA PWR & LGT CO","MARTINS CRK",0,"BIT COAL",14715,"0M",1294,,,95,77736,33553,94127,107453,45145,78631,33245,15373,94972,56476,25532,79013,56350,25210,63411,56558,24356,57931,77903,34985,45157,72539,34251,53601,19134,10553,62015,28384,12765,56271,68305,31511,46146,107135,53235,34362,3148,3,52288,"BIT","ST" 23,42,1,3,2,137,32,"PENNSYLVANIA PWR & LGT CO","MARTINS CRK",0,"LIGHT OIL",14715,"0M",1294,,,95,19,33,0,53,92,0,70,124,0,63,90,0,15,57,0,18,30,0,7,12,0,39,74,0,10,20,0,7,13,0,4,7,0,20,9,0,3148,3,52288,"FO2","IC" 23,42,1,4,2,137,32,"PENNSYLVANIA PWR & LGT CO","MARTINS CRK",0,"LIGHT OIL",14715,"0M",1294,,,95,0,0,5154,253,713,4491,0,0,4487,23,66,4408,0,0,4408,97,271,4056,301,924,3141,2928,8451,3433,332,1023,4044,0,0,4797,34,92,6619,47,134,6156,3148,3,52288,"FO2","GT" 23,42,1,4,2,137,34,"PENNSYLVANIA PWR & LGT CO","JENKINS",0,"LIGHT OIL",14715,"0M",1294,,,95,0,0,2287,49,143,2325,0,0,2326,12,59,2267,0,0,2265,0,0,2261,285,831,1773,1377,3617,2093,62,169,2280,17,50,2230,0,0,2177,0,0,2170,3146,3,52288,"FO2","GT" 23,42,1,4,2,137,36,"PENNSYLVANIA PWR & LGT CO","LOCK HAVEN",0,"LIGHT OIL",14715,"0M",1294,,,95,2,17,2072,0,0,2072,0,0,2071,0,0,2072,0,0,2231,19,50,2181,47,187,2160,309,776,1940,29,62,2234,0,0,2233,0,0,2229,0,0,2223,3147,3,52288,"FO2","GT" 23,42,1,2,2,137,38,"PENNSYLVANIA PWR & LGT CO","MONTOUR",0,"LIGHT OIL",14715,"0M",1294,,,95,5284,3061,15269,1120,9829,7128,603,1538,7267,606,3951,8198,13,2000,6913,5227,30521,8337,1368,7253,4923,878,2071,5843,1573,7626,7055,7633,17598,7723,1969,8730,7062,7059,10859,7500,3149,3,52288,"FO2","ST" 23,42,1,2,6,137,38,"PENNSYLVANIA PWR & LGT CO","MONTOUR",0,"BIT COAL",14715,"0M",1294,,,95,847074,335924,519372,875346,340631,445625,780698,304571,380887,372505,141113,452083,435583,162563,503087,625764,248102,531404,836431,328954,481373,911902,352540,306054,690630,264412,407406,817637,314073,299288,838531,328858,291789,880367,352324,220532,3149,3,52288,"BIT","ST" 23,42,1,2,2,137,40,"PENNSYLVANIA PWR & LGT CO","SUNBURY",0,"LIGHT OIL",14715,"0M",1294,,,95,120,1018,953,89,415,868,270,1417,1025,212,1169,913,362,1349,784,121,240,1084,94,305,938,95,427,967,167,1398,1038,316,896,961,315,1038,893,516,1056,864,3152,3,52288,"FO2","ST" 23,42,1,2,4,137,40,"PENNSYLVANIA PWR & LGT CO","SUNBURY",0,"ANTH COAL",14715,"0M",1294,,,95,59791,48178,418732,52800,43904,407593,42379,34783,387855,56229,44534,380823,54876,44151,401119,43071,35250,457310,34960,27900,513983,38518,30044,586494,54062,41683,635399,58158,44699,652259,58144,45249,613424,56311,42856,591156,3152,3,52288,"ANT","ST" 23,42,1,2,5,137,40,"PENNSYLVANIA PWR & LGT CO","SUNBURY",0,"COKE",14715,"0M",1294,,,95,32080,14266,18014,37875,17579,8930,34489,14591,2989,39190,17032,15602,35966,15206,24516,28052,11818,24368,21736,9175,21882,27009,11174,25559,37827,15339,20820,35544,14870,22116,40820,17176,11347,43815,18422,22426,3152,3,52288,"PC","ST" 23,42,1,2,6,137,40,"PENNSYLVANIA PWR & LGT CO","SUNBURY",0,"BIT COAL",14715,"0M",1294,,,95,38602,20937,145827,50229,27422,136935,127350,62833,126363,110076,53702,131074,110470,54187,128876,117078,56381,126273,137002,67568,99984,129986,64144,93470,121920,58717,95585,117436,55949,93435,118781,56941,78649,145641,68789,57848,3152,3,52288,"BIT","ST" 23,42,1,3,2,137,40,"PENNSYLVANIA PWR & LGT CO","SUNBURY",0,"LIGHT OIL",14715,"0M",1294,,,95,29,54,0,17,32,0,22,41,0,12,22,0,18,33,0,15,28,0,10,19,0,41,76,0,14,26,0,21,39,0,16,30,0,15,28,0,3152,3,52288,"FO2","IC" 23,42,1,4,2,137,40,"PENNSYLVANIA PWR & LGT CO","SUNBURY",0,"LIGHT OIL",14715,"0M",1294,,,95,0,0,4196,0,0,4357,0,0,4367,0,0,4367,0,0,4367,12,34,4284,56,161,4122,1269,3772,3896,136,375,4425,0,0,4425,0,0,4304,59,188,4116,3152,3,52288,"FO2","GT" 23,42,1,4,2,137,41,"PENNSYLVANIA PWR & LGT CO","WEST SHORE",0,"LIGHT OIL",14715,"0M",1294,,,95,0,0,1981,146,397,2124,0,0,2125,23,63,2063,0,0,2063,27,85,2157,93,275,2060,1581,3944,1664,97,247,1948,0,0,1948,0,0,1943,0,0,1936,3154,3,52288,"FO2","GT" 23,42,1,4,2,137,42,"PENNSYLVANIA PWR & LGT CO","WILLIAMPORT",0,"LIGHT OIL",14715,"0M",1294,,,95,11,25,2095,108,303,2299,33,89,2120,24,80,2130,0,0,1062,31,83,2085,166,469,2282,1685,4637,1796,229,615,2348,0,1,2347,0,0,2347,47,129,2218,3155,3,52288,"FO2","GT" 23,42,1,2,4,137,44,"PENNSYLVANIA PWR & LGT CO","COAL STORAG",0,"ANTH COAL",14715,"0M",1294,,,95,0,0,4326102,0,0,4287048,0,0,4250306,0,0,4192077,0,0,4116068,0,0,4024607,0,0,3949307,0,0,3858966,0,0,3770991,0,0,3712178,0,0,3655315,0,0,3627389,8805,3,52288,"ANT","ST" 23,42,1,2,1,144,1,"PECO ENERGY CO","LIMERICK",0,"NUCLEAR",14940,"0M",1294,,260,95,758738,0,0,649503,0,0,788638,0,0,741991,0,0,644273,0,0,749037,0,0,735331,0,0,472319,0,0,293869,0,0,781359,0,0,758883,0,0,774008,0,0,6105,3,52304,"UR","ST" 23,42,1,2,1,144,2,"PECO ENERGY CO","LIMERICK",0,"NUCLEAR",14940,"0M",1294,,260,95,305997,0,0,145495,0,0,841460,0,0,792169,0,0,828631,0,0,759339,0,0,812705,0,0,648469,0,0,793584,0,0,839715,0,0,794719,0,0,838665,0,0,6105,3,52304,"UR","ST" 23,42,1,2,1,144,2,"PECO ENERGY CO","PEACHBOTTOM",0,"NUCLEAR",14940,"0M",1294,,260,95,835865,0,0,758077,0,0,833805,0,0,783656,0,0,813085,0,0,767048,0,0,814131,0,0,781700,0,0,787889,0,0,812587,0,0,755502,0,0,620649,0,0,3166,3,52304,"UR","ST" 23,42,1,1,,144,3,"PECO ENERGY CO","MUDDY RUN",0,"P-PUMPSTG",14940,"0M",1294,,260,95,-58588,197635,0,-48050,161907,0,-57936,201052,0,-62063,184331,0,-54454,193555,0,-64502,219733,0,-77254,238571,0,-71435,248510,0,-71632,228867,0,-151911,225998,0,-140643,200522,0,-140747,207063,0,3164,3,52304,"WAT","HY" 23,42,1,2,1,144,3,"PECO ENERGY CO","PEACHBOTTOM",0,"NUCLEAR",14940,"0M",1294,,260,95,777483,0,0,711496,0,0,640321,0,0,740258,0,0,699846,0,0,588449,0,0,497410,0,0,423621,0,0,284823,0,0,314451,0,0,800042,0,0,695148,0,0,3166,3,52304,"UR","ST" 23,42,1,4,2,144,10,"PECO ENERGY CO","CHESTER",0,"LIGHT OIL",14940,"0M",1294,,260,95,40,143,6303,283,871,5973,4,13,5960,0,0,5960,0,0,5960,134,251,5709,1965,3097,5088,2547,9094,4622,135,622,5417,6,46,5371,9,117,5615,0,0,5615,3157,3,52304,"FO2","GT" 23,42,1,2,2,144,18,"PECO ENERGY CO","CROMBY",0,"LIGHT OIL",14940,"0M",1294,,260,95,552,1065,739,136,247,742,559,972,675,596,1108,639,800,1555,694,542,1023,717,107,204,786,442,846,656,532,1027,700,390,751,648,1349,2625,514,669,1263,679,3159,3,52304,"FO2","ST" 23,42,1,2,3,144,18,"PECO ENERGY CO","CROMBY",0,"HEAVY OIL",14940,"0M",1294,,260,95,2359,4204,37192,40300,66566,38230,6132,9753,28477,2439,4170,38531,1755,3147,35384,2326,3992,31392,2427,4219,27173,2684,4698,32767,5362,9562,23250,2962,5168,40075,2887,5164,35070,3164,5422,36172,3159,3,52304,"FO6","ST" 23,42,1,2,6,144,18,"PECO ENERGY CO","CROMBY",0,"BIT COAL",14940,"0M",1294,,260,95,74489,31603,37801,84553,33984,30569,59404,28393,32942,68130,28446,39783,56042,24391,55616,62095,25757,51736,68743,28828,37015,81385,34554,29542,73288,31653,35675,82081,34906,31898,75734,32689,34891,88164,36436,31030,3159,3,52304,"BIT","ST" 23,42,1,2,9,144,18,"PECO ENERGY CO","CROMBY",0,"NAT GAS",14940,"0M",1294,,260,95,71643,785884,0,61834,634083,0,79727,785913,0,51172,541950,0,54177,597370,0,81502,865110,0,111181,1192120,0,110008,1192120,0,68568,752990,0,0,0,0,0,0,0,69,740,0,3159,3,52304,"NG","ST" 23,42,1,3,2,144,18,"PECO ENERGY CO","CROMBY",0,"LIGHT OIL",14940,"0M",1294,,260,95,0,0,425,2,5,382,1,2,380,1,3,377,0,0,377,0,1,376,6,13,363,0,0,363,2,5,358,0,0,358,3,6,352,0,0,352,3159,3,52304,"FO2","IC" 23,42,1,2,2,144,20,"PECO ENERGY CO","DELAWARE",0,"LIGHT OIL",14940,"0M",1294,,260,95,83,167,285,230,443,159,379,1037,262,0,1258,270,63,112,285,407,948,313,503,939,296,248,512,251,125,311,303,0,535,306,0,1886,292,1548,3097,274,3160,3,52304,"FO2","ST" 23,42,1,2,3,144,20,"PECO ENERGY CO","DELAWARE",0,"HEAVY OIL",14940,"0M",1294,,260,95,7566,13842,54536,40968,72617,57755,6149,15501,61363,-988,853,60510,1023,1674,58836,10372,22370,60784,73226,125872,59240,61586,116298,48551,3817,8670,64382,-880,0,64382,-848,109,64273,42071,77005,46160,3160,3,52304,"FO6","ST" 23,42,1,3,2,144,20,"PECO ENERGY CO","DELAWARE",0,"LIGHT OIL",14940,"0M",1294,,260,95,4,8,0,6,12,0,0,0,0,8,4,0,0,0,0,0,0,0,0,0,0,5,12,0,0,0,0,0,0,0,3,6,0,0,0,0,3160,3,52304,"FO2","IC" 23,42,1,4,2,144,20,"PECO ENERGY CO","DELAWARE",0,"LIGHT OIL",14940,"0M",1294,,260,95,14,29,4606,471,908,4510,16,46,5120,42,103,4834,0,0,5221,137,321,4998,1693,3157,5919,4022,8277,4823,175,434,5097,11,64,4495,0,0,4139,3,6,3960,3160,3,52304,"FO2","GT" 23,42,1,2,2,144,23,"PECO ENERGY CO","EDDYSTONE",0,"LIGHT OIL",14940,"0M",1294,,260,95,2860,5785,8309,7265,14150,6730,691,1392,5338,656,1353,6842,1090,2439,5446,1497,2992,3502,265,545,7647,1122,2234,5367,200,403,4943,1397,2645,5855,940,1740,11279,4634,8834,12016,3161,3,52304,"FO2","ST" 23,42,1,2,3,144,23,"PECO ENERGY CO","EDDYSTONE",0,"HEAVY OIL",14940,"0M",1294,,260,95,28189,52308,219884,149450,269038,232369,3289,6168,226201,212,405,225796,779,1602,224194,12605,22920,225716,34139,63954,190796,58828,107390,228949,6004,24353,228406,13370,23208,205198,25814,43623,161575,159697,281810,186014,3161,3,52304,"FO6","ST" 23,42,1,2,6,144,23,"PECO ENERGY CO","EDDYSTONE",0,"BIT COAL",14940,"0M",1294,,260,95,230611,102377,114701,145600,63304,115351,142036,63132,95986,141196,64796,114142,75987,37394,136129,72749,31969,156190,38241,17251,161746,115645,50809,196139,101095,70609,237844,255413,106924,214128,279475,114586,204428,343647,144382,154263,3161,3,52304,"BIT","ST" 23,42,1,2,9,144,23,"PECO ENERGY CO","EDDYSTONE",0,"NAT GAS",14940,"0M",1294,,260,95,44577,509816,0,75572,836629,0,64058,732536,0,42770,502085,0,37425,473140,0,199205,2238826,0,248894,2876189,0,290649,3273871,0,116178,2028607,0,136486,1466691,0,26917,282787,0,17773,193338,0,3161,3,52304,"NG","ST" 23,42,1,4,2,144,23,"PECO ENERGY CO","EDDYSTONE",0,"LIGHT OIL",14940,"0M",1294,,260,95,88,179,7824,301,588,7236,23,47,7189,0,0,7189,59,133,7056,38,77,6979,2082,4276,7703,5802,11553,9393,213,2838,8159,40,77,8082,74,138,7944,162,310,8951,3161,3,52304,"FO2","GT" 23,42,1,2,3,144,25,"PECO ENERGY CO","OIL STORAGE",0,"HEAVY OIL",14940,"0M",1294,,260,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,8806,3,52304,"FO6","ST" 23,42,1,4,2,144,26,"PECO ENERGY CO","FALLS",0,"LIGHT OIL",14940,"0M",1294,,260,95,6,16,10772,174,460,10312,0,0,10312,0,0,10312,0,0,10312,323,626,9686,1716,2316,9307,2167,6952,8374,53,261,8289,8,112,8177,0,0,8503,0,0,8503,3162,3,52304,"FO2","GT" 23,42,1,4,2,144,27,"PECO ENERGY CO","MOSER",0,"LIGHT OIL",14940,"0M",1294,,260,95,62,154,10920,416,1304,10329,2,7,10322,0,0,10322,0,0,10322,174,159,10163,2401,3681,8582,3033,9617,8076,165,385,7691,0,0,7691,49,1948,8854,0,0,8854,3163,3,52304,"FO2","GT" 23,42,1,4,2,144,30,"PECO ENERGY CO","RICHMOND",0,"LIGHT OIL",14940,"0M",1294,,260,95,73,705,25225,1538,2518,24154,176,209,23945,0,0,23945,0,0,23945,546,1092,22853,7883,15050,19654,8358,22812,19604,1489,4282,16208,573,1391,19605,1780,4530,22192,2646,5558,20232,3168,3,52304,"FO2","GT" 23,42,1,2,2,144,35,"PECO ENERGY CO","SCHUYLKILL",0,"LIGHT OIL",14940,"0M",1294,,260,95,10,31,177,29,55,282,0,13,330,0,0,58,5,32,173,21,41,260,32,63,204,31,64,224,0,0,285,0,0,204,0,13,117,174,366,292,3169,3,52304,"FO2","ST" 23,42,1,2,3,144,35,"PECO ENERGY CO","SCHUYLKILL",0,"HEAVY OIL",14940,"0M",1294,,260,95,2569,7049,0,27433,47982,0,-514,221,0,-442,0,0,787,4441,0,7540,12988,0,45149,79435,0,40737,74952,0,2171,4408,0,-450,0,0,-487,0,0,33696,64594,0,3169,3,52304,"FO6","ST" 23,42,1,3,2,144,35,"PECO ENERGY CO","SCHUYLKILL",0,"LIGHT OIL",14940,"0M",1294,,260,95,0,0,0,11,21,0,1,6,0,0,0,0,0,0,0,0,0,0,0,0,0,4,9,0,2,8,0,0,0,0,0,0,0,0,0,0,3169,3,52304,"FO2","IC" 23,42,1,4,2,144,35,"PECO ENERGY CO","SCHUYLKILL",0,"LIGHT OIL",14940,"0M",1294,,260,95,0,0,4077,183,347,4272,0,0,4454,0,0,4454,16,102,4352,25,48,4304,1060,2033,4025,3086,6214,3655,57,113,3542,0,0,3542,0,0,4435,0,0,4435,3169,3,52304,"FO2","GT" 23,42,1,4,2,144,39,"PECO ENERGY CO","SOUTHWARK",0,"LIGHT OIL",14940,"0M",1294,,260,95,7,10,6164,245,786,6101,28,123,5978,0,0,5978,0,0,5978,21,33,5945,2299,3702,5765,2572,9427,4876,120,646,4593,9,18,4592,0,0,5461,12,32,5429,3170,3,52304,"FO2","GT" 23,42,1,4,2,144,62,"PECO ENERGY CO","CROYDON",0,"LIGHT OIL",14940,"0M",1294,,260,95,908,1378,96105,5368,13129,82976,1206,2774,80202,185,1674,78528,-30,449,78079,2904,7166,70913,28748,58359,102954,34047,90855,75978,5816,17011,58967,4006,14190,124677,9344,33758,90919,20108,59103,81811,8012,3,52304,"FO2","GT" 23,42,1,1,,166,1,"SAFE HARBOR WATERPOWER CO","SAFE HARBOR",0,,16537,"0M",1294,,,95,143384,0,0,59393,0,0,126476,0,0,89759,0,0,63828,0,0,55553,0,0,43077,0,0,14256,0,0,7655,0,0,60191,0,0,112079,0,0,82918,0,0,3175,3,52553,"WAT","HY" 23,42,1,2,2,182,5,"UNITED GAS IMP CO (THE)","HUNLOCK CRK",0,"LIGHT OIL",19390,"0M",1294,,,95,513,820,149,94,161,167,202,328,185,435,618,244,11,18,226,1,2,224,140,230,170,0,0,170,514,892,135,73,127,175,21,35,140,24,41,99,3176,3,52988,"FO2","ST" 23,42,1,2,4,182,5,"UNITED GAS IMP CO (THE)","HUNLOCK CRK",0,"ANTH COAL",19390,"0M",1294,,,95,22922,15408,12384,27213,18489,14764,29884,19399,26578,8930,5383,44202,31976,21379,41110,31087,20919,40663,28632,19193,37106,32217,21657,39145,28079,19274,38194,32138,21308,38517,32139,20464,33331,30924,20327,26649,3176,3,52988,"ANT","ST" 23,42,1,2,2,187,1,"WEST PENN POWER CO","ARMSTRONG",0,"LIGHT OIL",20387,"0M",1294,,71,95,1137,2044,435,250,438,461,208,349,465,208,340,516,357,602,494,249,434,577,87,154,405,77,134,448,175,297,469,719,1212,478,755,1324,33,100,171,531,3178,1,54030,"FO2","ST" 23,42,1,2,6,187,1,"WEST PENN POWER CO","ARMSTRONG",0,"BIT COAL",20387,"0M",1294,,71,95,116602,48997,133134,169087,69152,118235,94695,37329,143043,106738,41224,154005,90547,35992,160453,93589,37605,145126,109058,44341,133889,108429,43934,141795,50453,20094,155423,132983,52637,143306,163282,66595,118118,227115,90923,97838,3178,1,54030,"BIT","ST" 23,42,1,2,2,187,5,"WEST PENN POWER CO","HATFIELD",0,"LIGHT OIL",20387,"0M",1294,,71,95,431,715,4466,429,677,4860,16,26,4860,109,176,5175,295,498,4642,232,393,4202,112,193,4003,116,200,3858,440,729,3846,625,1001,3653,200,324,4266,345,551,4530,3179,1,54030,"FO2","ST" 23,42,1,2,6,187,5,"WEST PENN POWER CO","HATFIELD",0,"BIT COAL",20387,"0M",1294,,71,95,924993,349235,573422,796344,286253,580468,654622,239981,562743,652050,240234,569141,751057,287421,561772,807472,310567,503117,873489,338429,425399,814220,315517,429242,611272,228129,438816,665375,244419,472140,717809,264457,471668,976850,352523,470255,3179,1,54030,"BIT","ST" 23,42,1,2,2,187,15,"WEST PENN POWER CO","MITCHELL",0,"LIGHT OIL",20387,"0M",1294,,71,95,1099,1660,62781,14264,26130,36652,9573,16358,20294,0,0,95,0,0,20294,0,0,20294,2975,5533,14761,9534,17307,37248,0,0,37248,370,623,36693,0,0,102,0,0,36712,3181,1,54030,"FO2","ST" 23,42,1,2,6,187,15,"WEST PENN POWER CO","MITCHELL",0,"BIT COAL",20387,"0M",1294,,71,95,133543,54702,81824,96423,41467,82859,153555,62524,77796,125039,49503,90740,49588,20363,93045,53622,23986,82955,92131,39751,72392,131370,55646,87997,44218,20045,99480,112797,45127,97501,86006,35430,95483,91125,37261,96203,3181,1,54030,"BIT","ST" 23,42,1,2,9,187,15,"WEST PENN POWER CO","MITCHELL",0,"NAT GAS",20387,"0M",1294,,71,95,997,8782,0,512,5468,0,649,6574,0,362,3518,0,98,1012,0,493,5639,0,384,4175,0,352,3732,0,608,6884,0,229,2287,0,632,6538,0,411,4215,0,3181,1,54030,"NG","ST" 23,42,1,2,3,187,25,"WEST PENN POWER CO","SPRINGDALE",0,"HEAVY OIL",20387,"0M",1294,"S",71,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,3182,1,54030,"FO6","ST" 23,42,8,1,,800,5,"ALLEGHENY ELECTRIC COOP","RAYSTOWN",0,,332,"0A",1294,,,95,10581,0,0,4872,0,0,10420,0,0,7145,0,0,9214,0,0,7292,0,0,7823,0,0,1871,0,0,1862,0,0,6232,0,0,13092,0,0,11263,0,0,7128,1,58500,"WAT","HY" 31,39,1,2,2,30,5,"CARDINAL OPERATING CO","CARDINAL",0,"LIGHT OIL",3006,"0M",1294,,365,95,1506,2512,16004,1987,3269,21891,793,1326,20561,810,1358,18998,750,1207,17783,5623,9537,7493,587,994,18460,1462,2531,15746,996,1682,14054,1293,2176,11850,586,984,10858,3751,6207,17605,2828,1,50359,"FO2","ST" 31,39,1,2,6,30,5,"CARDINAL OPERATING CO","CARDINAL",0,"BIT COAL",3006,"0M",1294,,365,95,964403,385031,651565,952635,371878,631820,970861,386058,589923,907026,357640,591393,523077,201759,670651,745173,300966,631446,1013299,410501,467099,1010121,415926,370224,984185,397240,345127,996339,400914,397108,987234,392815,487317,940659,377797,434608,2828,1,50359,"BIT","ST" 31,39,1,4,2,43,1,"CINCINNATI GAS ELEC CO","DICKS CREEK",0,"LIGHT OIL",3542,"0M",1294,,210,95,20,1175,6144,23,332,5811,9,35,5776,18,399,5377,0,0,5377,10,47,5330,233,987,4343,377,1342,3001,3,41,5373,8,49,5325,18,65,5260,1,7,5253,2831,1,50556,"FO2","GT" 31,39,1,4,9,43,1,"CINCINNATI GAS ELEC CO","DICKS CREEK",0,"NAT GAS",3542,"0M",1294,,210,95,74,4943,0,-217,0,0,17,13,0,-138,563,0,-109,0,0,227,871,0,3843,78877,0,4803,89226,0,-34,0,0,-101,1423,0,240,6693,0,672,17724,0,2831,1,50556,"NG","GT" 31,39,1,2,2,43,2,"CINCINNATI GAS ELEC CO","WC BECKJORD",0,"LIGHT OIL",3542,"0M",1294,,210,95,1063,1868,0,520,909,0,1246,2193,0,616,1040,0,909,1575,0,1694,2920,0,83,148,0,648,1175,0,673,1200,0,1185,2032,0,1335,2313,0,1124,2076,0,2830,1,50556,"FO2","ST" 31,39,1,2,6,43,2,"CINCINNATI GAS ELEC CO","WC BECKJORD",0,"BIT COAL",3542,"0M",1294,,210,95,376000,158991,137317,393834,167236,139827,297378,127194,171002,437582,181317,177440,274678,116442,192793,481664,200911,197721,528583,228082,195580,602321,260506,195850,213081,91113,206835,487454,202145,200676,427365,176777,196004,493746,218176,193234,2830,1,50556,"BIT","ST" 31,39,1,4,2,43,2,"CINCINNATI GAS ELEC CO","WC BECKJORD",0,"LIGHT OIL",3542,"0M",1294,,210,95,904,1589,30711,253,443,29179,30,54,26769,24,41,25499,30,53,23746,206,356,41971,10845,19305,22349,18056,32731,31385,523,933,29084,23,40,26796,38,67,23956,1551,2863,41821,2830,1,50556,"FO2","GT" 31,39,1,2,2,43,5,"CINCINNATI GAS ELEC CO","MIAMI FORT",0,"LIGHT OIL",3542,"0M",1294,,210,95,1008,1795,0,465,820,0,830,1457,0,436,757,0,862,1538,0,1665,3001,0,1804,3164,0,3368,6051,0,1292,2324,0,260,450,0,548,956,0,3202,5528,0,2832,1,50556,"FO2","ST" 31,39,1,2,6,43,5,"CINCINNATI GAS ELEC CO","MIAMI FORT",0,"BIT COAL",3542,"0M",1294,,210,95,637745,262491,294369,502865,207419,302760,559242,231277,318869,305741,124954,357678,414341,174583,369622,502174,211728,359534,599203,248510,325680,672906,285623,264937,557339,235511,249465,607306,250021,246891,553335,226505,248836,594845,241403,260437,2832,1,50556,"BIT","ST" 31,39,1,4,2,43,5,"CINCINNATI GAS ELEC CO","MIAMI FORT",0,"LIGHT OIL",3542,"0M",1294,,210,95,184,328,29994,104,184,28839,51,90,27190,104,182,26060,90,161,23971,260,470,20424,2604,4567,34307,5930,10654,29284,0,0,26912,56,98,26221,132,231,25022,4,7,19483,2832,1,50556,"FO2","GT" 31,39,1,2,2,43,10,"CINCINNATI GAS ELEC CO","W H ZIMMER",0,"LIGHT OIL",3542,"0M",1294,,210,95,387,627,43117,405,662,42455,266,437,42018,446,721,41297,544,908,40390,5437,9067,40610,3869,6259,34351,2406,3947,30404,654,1074,29331,0,0,28641,10375,17945,31644,228,326,31318,6019,1,50556,"FO2","ST" 31,39,1,2,6,43,10,"CINCINNATI GAS ELEC CO","W H ZIMMER",0,"BIT COAL",3542,"0M",1294,,210,95,945287,364436,470303,860575,334587,468422,931671,360276,429932,905494,345488,449089,895923,353208,433131,685071,269191,462164,813824,313887,471999,817013,315668,465279,858265,326707,439814,-6015,0,440306,643755,258809,446427,954218,369625,445092,6019,1,50556,"BIT","ST" 31,39,1,4,2,43,15,"CINCINNATI GAS ELEC CO","WOODSDALE",0,"PROPANE",3542,"0M",1294,,210,95,3264,17257,47281,251,6836,40445,206,1875,39359,655,3378,35981,0,2040,33941,765,1976,31965,599,1450,30515,128,307,30208,2,8,30200,22,122,30078,2291,8079,47000,9027,29590,47410,7158,1,50556,"FO2","GT" 31,39,1,4,9,43,15,"CINCINNATI GAS ELEC CO","WOODSDALE",0,"NAT GAS",3542,"0M",1294,,210,95,150,4500,0,6,900,0,329,16900,0,549,16100,0,-24,5400,0,8444,123700,0,78223,1073891,0,127374,1732000,0,11241,209600,0,798,24900,0,8079,161217,0,5288,98400,0,7158,1,50556,"NG","GT" 31,39,1,2,1,47,1,"CLEVELAND ELEC ILLUM CO","PERRY",0,"NUCLEAR",3755,"0M",1294,,,95,876776,0,0,768903,0,0,819283,0,0,488364,0,0,856246,0,0,825532,0,0,844484,0,0,836109,0,0,563058,0,0,867378,0,0,562127,0,0,802040,0,0,6020,1,50587,"UR","ST" 31,39,1,2,2,47,5,"CLEVELAND ELEC ILLUM CO","ASHTABULA",0,"LIGHT OIL",3755,"0M",1294,,,95,42,104,847,0,0,847,118,290,165,18,45,836,36,88,1105,993,2435,781,1126,2764,920,735,1805,1069,508,1246,1250,554,1359,961,372,912,1126,318,78,1063,2835,1,50587,"FO2","ST" 31,39,1,2,6,47,5,"CLEVELAND ELEC ILLUM CO","ASHTABULA",0,"BIT COAL",3755,"0M",1294,,,95,52796,31491,71024,49964,29829,71024,55761,34212,70589,75864,42918,70589,57256,34078,70589,75393,41494,70589,152351,73482,69602,185535,87655,62911,92554,48842,63273,134786,62671,50375,152108,70363,39853,183631,84228,39391,2835,1,50587,"BIT","ST" 31,39,1,2,2,47,10,"CLEVELAND ELEC ILLUM CO","AVON",0,"LIGHT OIL",3755,"0M",1294,,,95,545,1336,12357,217,533,11823,334,820,11003,71,175,13126,623,1529,11274,103,252,10337,204,501,9328,209,514,12564,219,537,11551,455,1117,10529,439,1076,9330,211,518,8657,2836,1,50587,"FO2","ST" 31,39,1,2,6,47,10,"CLEVELAND ELEC ILLUM CO","AVON",0,"BIT COAL",3755,"0M",1294,,,95,418792,166008,147432,412531,162705,122460,424163,169344,131476,363532,138488,180398,251231,98651,203325,203947,82859,218224,353614,137703,162497,424161,173437,95914,388690,173071,75855,373672,144052,89758,227150,92153,101135,197850,84233,81208,2836,1,50587,"BIT","ST" 31,39,1,4,2,47,10,"CLEVELAND ELEC ILLUM CO","AVON",0,"LIGHT OIL",3755,"0M",1294,,,95,-48,0,1833,46,308,1525,-44,0,1525,16,93,1432,-27,0,1432,51,171,1260,97,283,1453,726,2175,826,-20,0,1302,-23,0,1326,-40,0,1326,-55,0,1861,2836,1,50587,"FO2","GT" 31,39,1,2,2,47,15,"CLEVELAND ELEC ILLUM CO","EASTLAKE",0,"LIGHT OIL",3755,"0M",1294,,,95,1497,3674,9572,911,2234,8964,764,1874,9624,751,1842,8674,1166,2861,7850,1418,3479,8310,853,2092,5787,966,2369,13472,911,2234,13178,758,1860,11437,682,1673,13358,1121,2750,10965,2837,1,50587,"FO2","ST" 31,39,1,2,6,47,15,"CLEVELAND ELEC ILLUM CO","EASTLAKE",0,"BIT COAL",3755,"0M",1294,,,95,563066,214828,125324,531721,201833,127529,552063,214200,127558,603752,229103,113946,476696,183152,148312,528305,201681,134280,545020,211638,133115,580108,227637,126504,418750,164875,155538,237147,95621,161064,619540,234785,116588,554005,216330,121544,2837,1,50587,"BIT","ST" 31,39,1,4,2,47,15,"CLEVELAND ELEC ILLUM CO","EASTLAKE",0,"LIGHT OIL",3755,"0M",1294,,,95,-26,411,1392,-34,64,1328,-7,96,1232,-39,0,1232,-17,48,1184,80,272,913,110,487,2330,416,1227,1642,-21,0,1642,-29,0,1642,-48,0,1642,-62,0,1642,2837,1,50587,"FO2","GT" 31,39,1,2,2,47,20,"CLEVELAND ELEC ILLUM CO","LAKE SHORE",0,"LIGHT OIL",3755,"0M",1294,,,95,1807,4433,0,1095,2687,0,655,1878,10867,822,2016,9030,822,2016,9030,822,2016,9030,822,2016,9030,0,0,9030,0,0,9030,0,0,9030,0,0,9030,0,0,9030,2838,1,50587,"FO2","ST" 31,39,1,2,3,47,20,"CLEVELAND ELEC ILLUM CO","LAKE SHORE",0,"HEAVY OIL",3755,"0M",1294,,,95,-1345,0,0,-1121,0,0,-1101,0,0,-967,0,0,-1013,0,0,-1144,0,0,-1177,0,0,-1109,0,0,-1101,0,0,-886,0,0,-1113,0,0,-1190,0,0,2838,1,50587,"FO6","ST" 31,39,1,2,6,47,20,"CLEVELAND ELEC ILLUM CO","LAKE SHORE",0,"BIT COAL",3755,"0M",1294,,,95,-2869,0,0,-2051,0,0,-8655,0,0,-1765,0,0,-1630,0,0,-1592,0,0,-1511,0,0,-680,0,0,-664,0,0,-785,0,0,-839,0,0,-939,0,0,2838,1,50587,"BIT","ST" 31,39,1,3,2,47,20,"CLEVELAND ELEC ILLUM CO","LAKE SHORE",0,"LIGHT OIL",3755,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2838,1,50587,"FO2","IC" 31,39,1,2,2,50,5,"COLUMBUS SOUTHERN PWR CO","CONESVILLE",0,"LIGHT OIL",4062,"0M",1294,,369,95,781,1346,11167,848,1487,10088,1527,2569,9973,647,1108,10480,1150,1863,10818,808,1412,11137,1992,3195,10638,911,1520,12206,2980,5206,7444,848,1360,7419,1411,2362,6092,1247,2194,6515,2840,1,50633,"FO2","ST" 31,39,1,2,6,50,5,"COLUMBUS SOUTHERN PWR CO","CONESVILLE",0,"BIT COAL",4062,"0M",1294,,369,95,839897,361439,480236,776708,341510,409270,577474,241703,450938,516809,220156,545479,471259,188870,589930,540735,233443,590510,666114,292069,537443,960463,414977,380548,748475,319718,311923,775359,307972,333993,824448,339869,356943,594247,257598,411899,2840,1,50633,"BIT","ST" 31,39,1,2,2,50,15,"COLUMBUS SOUTHERN PWR CO","PICWAY",0,"LIGHT OIL",4062,"0M",1294,,369,95,77,157,318,80,151,162,0,0,158,0,0,163,0,0,150,271,581,410,67,164,258,153,329,279,86,168,293,52,109,355,102,206,330,71,149,354,2843,1,50633,"FO2","ST" 31,39,1,2,6,50,15,"COLUMBUS SOUTHERN PWR CO","PICWAY",0,"BIT COAL",4062,"0M",1294,,369,95,24098,12576,18902,17338,8355,10547,0,0,10547,0,0,10547,0,0,10547,12062,7059,8508,8499,5099,16411,33626,17892,7051,12493,6357,14305,11264,6148,20174,12256,6425,23762,14575,8110,25135,2843,1,50633,"BIT","ST" 31,39,1,3,2,56,15,"DAYTON PWR & LGT CO (THE)","FRANK TAIT",0,"LIGHT OIL",4922,"0M",1294,,,95,10,18,2118,30,55,1880,24,44,4879,67,123,5809,5,9,5601,0,0,8437,59,128,8308,638,1170,6968,8,15,6953,0,0,6953,4,31,12908,0,0,12704,2847,1,50752,"FO2","IC" 31,39,1,4,2,56,15,"DAYTON PWR & LGT CO (THE)","FRANK TAIT",0,"LIGHT OIL",4922,"0M",494,,,95,0,0,0,0,0,0,0,0,0,8,31,0,2615,5585,0,2094,4660,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,87,204,0,2847,1,50752,"FO2","GT" 31,39,1,4,9,56,15,"DAYTON PWR & LGT CO (THE)","FRANK TAIT",0,"NAT GAS",4922,"0M",494,,,95,0,0,0,0,0,0,0,0,0,206,4610,0,2453,30366,0,2250,29020,0,2757,33743,0,5899,80360,0,392,7740,0,65,1370,0,35,1210,0,1279,17010,0,2847,1,50752,"NG","GT" 31,39,1,2,6,56,20,"DAYTON PWR & LGT CO (THE)","HUTCHINGS",0,"BIT COAL",4922,"0M",1294,,,95,1189,1204,103680,11354,5882,97799,-864,0,97799,0,0,97799,-467,0,97799,38657,18515,85185,73119,34885,59277,140943,65371,20520,7427,3975,45638,4351,2521,84275,3553,2065,93826,62576,27616,66210,2848,1,50752,"BIT","ST" 31,39,1,2,9,56,20,"DAYTON PWR & LGT CO (THE)","HUTCHINGS",0,"NAT GAS",4922,"0M",1294,,,95,408,9899,0,595,6448,0,0,0,0,-804,48,0,4,164,0,1487,14801,0,2254,22264,0,5404,59821,0,688,9010,0,440,6133,0,353,5099,0,1464,15898,0,2848,1,50752,"NG","ST" 31,39,1,4,2,56,20,"DAYTON PWR & LGT CO (THE)","HUTCHINGS",0,"LIGHT OIL",4922,"0M",1294,,,95,71,303,1433,82,157,1275,0,1,1275,0,0,1275,0,0,1274,0,0,1274,0,0,1274,0,1,1274,0,0,1274,0,0,1274,58,147,1127,49,94,1395,2848,1,50752,"FO2","GT" 31,39,1,4,9,56,20,"DAYTON PWR & LGT CO (THE)","HUTCHINGS",0,"NAT GAS",4922,"0M",1294,,,95,0,10,0,0,0,0,5,1130,0,16,400,0,8,327,0,0,0,0,140,1384,0,423,4690,0,0,0,0,0,0,0,0,0,0,41,453,0,2848,1,50752,"NG","GT" 31,39,1,2,2,56,23,"DAYTON PWR & LGT CO (THE)","J M STUART",0,"LIGHT OIL",4922,"0M",1294,,,95,1332,2321,1749,646,1073,2134,623,1061,2140,1223,2081,1858,1631,2823,2062,975,1647,2197,223,358,2194,623,1047,2043,1054,1794,2183,2669,4498,2177,1035,1708,1924,2772,4191,2252,2850,1,50752,"FO2","ST" 31,39,1,2,6,56,23,"DAYTON PWR & LGT CO (THE)","J M STUART",0,"BIT COAL",4922,"0M",1294,,,95,1324209,556655,951299,1313535,540148,931841,981133,406226,1101726,963505,397393,1210633,1235488,518718,880851,1223521,506083,868835,1340550,537277,869585,1339861,554937,815555,984147,409972,981044,990034,409244,867049,1361690,549068,888832,1361213,508529,976472,2850,1,50752,"BIT","ST" 31,39,1,3,2,56,23,"DAYTON PWR & LGT CO (THE)","J M STUART",0,"LIGHT OIL",4922,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2850,1,50752,"FO2","IC" 31,39,1,4,2,56,28,"DAYTON PWR & LGT CO (THE)","YANKEE ST",0,"LIGHT OIL",4922,"0M",1294,,,95,392,1042,6368,143,449,7390,1,3,5791,0,0,5791,0,1,5790,0,2,5788,0,0,5788,0,2,6395,2,7,6388,0,1,6388,60,192,6195,298,738,6316,2854,1,50752,"FO2","GT" 31,39,1,4,9,56,28,"DAYTON PWR & LGT CO (THE)","YANKEE ST",0,"NAT GAS",4922,"0M",1294,,,95,10,160,0,62,1100,0,162,1963,0,84,1410,0,82,1499,0,110,1913,0,390,6135,0,2583,45005,0,16,299,0,118,2067,0,15,279,0,1,15,0,2854,1,50752,"NG","GT" 31,39,1,3,2,56,34,"DAYTON PWR & LGT CO (THE)","MONUMENT",0,"LIGHT OIL",4922,"0M",1294,,,95,48,88,666,38,70,596,24,44,749,8,15,735,20,37,698,0,0,698,0,0,698,868,1591,510,12,22,679,8,15,664,3,6,658,23,73,586,2851,1,50752,"FO2","IC" 31,39,1,3,2,56,38,"DAYTON PWR & LGT CO (THE)","SIDNEY",0,"LIGHT OIL",4922,"0M",1294,,,95,36,66,654,39,72,582,19,35,547,12,22,525,27,50,476,38,70,594,200,367,418,928,1701,298,12,22,467,14,26,441,11,20,599,27,50,550,2852,1,50752,"FO2","IC" 31,39,1,2,2,56,40,"DAYTON PWR & LGT CO (THE)","KILLEN",0,"LIGHT OIL",4922,"0M",1294,,,95,1515,2654,38401,2032,3512,34941,568,957,33906,811,1364,32383,2303,3935,28369,2103,3623,24697,1150,1949,22638,3905,6750,39224,3140,5527,33621,140,241,33352,1226,2214,31022,7796,9042,43816,6031,1,50752,"FO2","ST" 31,39,1,2,6,56,40,"DAYTON PWR & LGT CO (THE)","KILLEN",0,"BIT COAL",4922,"0M",1294,,,95,396655,162048,146219,299969,123570,141430,380134,154283,172985,326056,132202,166969,335211,138111,191956,337194,139038,170239,357281,145509,178055,407089,168349,129255,293108,123208,110897,435673,179182,98466,52201,22774,186101,115941,32572,227624,6031,1,50752,"BIT","ST" 31,39,1,2,2,133,10,"OHIO EDISON CO","EDGEWATER",0,"LIGHT OIL",13998,"0M",1294,"A",,95,0,0,0,0,0,0,255,723,33,159,366,33,0,0,0,308,793,33,68,152,33,5,124,33,27,86,33,7,17,33,1286,2860,33,3,6,33,2857,1,52154,"FO2","ST" 31,39,1,2,9,133,10,"OHIO EDISON CO","EDGEWATER",0,"NAT GAS",13998,"0M",394,,,95,0,0,0,0,0,0,7097,98907,0,15050,194824,0,0,0,0,5911,86537,0,13656,173637,0,24053,289252,0,13182,151945,0,7495,97750,0,13698,169535,0,9290,104799,0,2857,1,52154,"NG","ST" 31,39,1,4,2,133,10,"OHIO EDISON CO","EDGEWATER",0,"LIGHT OIL",13998,"0M",1294,,,95,39,51,10875,58,329,9555,-8,73,8938,-14,44,9839,0,0,9464,200,693,10736,984,3224,10487,1718,5378,9687,120,437,8935,-17,0,8918,15,18,8748,20,140,9834,2857,1,52154,"FO2","GT" 31,39,1,2,2,133,15,"OHIO EDISON CO","GORGE STEAM",0,"LIGHT OIL",13998,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2858,1,52154,"FO2","ST" 31,39,1,2,6,133,15,"OHIO EDISON CO","GORGE STEAM",0,"BIT COAL",13998,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2858,1,52154,"BIT","ST" 31,39,1,4,2,133,30,"OHIO EDISON CO","MAD RIVER",0,"LIGHT OIL",13998,"0M",1294,,,95,-78,0,15547,-26,273,15273,-54,0,15273,-54,0,15273,363,2822,15479,99,426,15053,1080,3857,14177,3295,9983,13051,179,602,14577,62,386,15260,60,421,14839,73,357,15562,2860,1,52154,"FO2","GT" 31,39,1,2,2,133,43,"OHIO EDISON CO","NILES",0,"LIGHT OIL",13998,"0M",1294,,,95,5,9,253,86,166,190,142,266,280,33,64,216,17,38,406,275,522,253,67,130,224,50,97,303,45,88,221,63,123,320,28,54,266,27,53,213,2861,1,52154,"FO2","ST" 31,39,1,2,6,133,43,"OHIO EDISON CO","NILES",0,"BIT COAL",13998,"0M",1294,,,95,123871,55965,73387,98573,45856,68795,100911,45527,84171,102317,46469,88241,6938,3797,109930,76341,34497,104722,105408,49207,76769,73326,33732,70283,103996,47562,47231,111221,52359,33613,108872,49872,33134,113766,51273,29923,2861,1,52154,"BIT","ST" 31,39,1,4,2,133,43,"OHIO EDISON CO","NILES",0,"LIGHT OIL",13998,"0M",1294,,,95,55,295,7474,75,333,7682,-36,56,7626,-41,0,7626,-25,30,7596,100,416,7180,647,2274,6851,1403,4579,5630,65,256,6970,-7,118,6852,3,124,6728,61,335,7293,2861,1,52154,"FO2","GT" 31,39,1,2,2,133,45,"OHIO EDISON CO","R E BURGER",0,"LIGHT OIL",13998,"0M",1294,,,95,101,204,570,57,119,629,70,132,675,95,173,502,63,117,562,95,188,374,81,156,558,51,100,633,44,83,549,46,91,458,2,3,632,119,296,336,2864,1,52154,"FO2","ST" 31,39,1,2,6,133,45,"OHIO EDISON CO","R E BURGER",0,"BIT COAL",13998,"0M",1294,,,95,220103,104240,157034,164294,78521,184267,126512,54034,193327,150997,63973,186573,81596,35961,201217,96775,43949,193287,127163,56391,181386,166656,74197,142563,130934,57102,99030,67387,30839,87088,93946,40429,64542,82572,48775,54306,2864,1,52154,"BIT","ST" 31,39,1,3,2,133,45,"OHIO EDISON CO","R E BURGER",0,"LIGHT OIL",13998,"0M",1294,,,95,7,10,1284,23,46,1417,9,11,1407,0,0,1407,0,0,1407,34,84,1323,236,429,1243,566,1044,904,17,35,1224,23,43,1181,0,0,1181,30,77,1647,2864,1,52154,"FO2","IC" 31,39,1,2,2,133,57,"OHIO EDISON CO","W H SAMMIS",0,"LIGHT OIL",13998,"0M",1294,,,95,1482,2546,867,528,903,1046,558,954,844,550,932,638,695,1199,912,544,955,1493,706,1274,1304,451,1354,1217,1142,2017,1181,1316,2293,1036,94,160,983,2104,3601,973,2866,1,52154,"FO2","ST" 31,39,1,2,6,133,57,"OHIO EDISON CO","W H SAMMIS",0,"BIT COAL",13998,"0M",1294,,,95,1276095,514756,525945,1279324,511426,457910,1239563,502275,472374,1278563,515393,459047,1160892,479648,563045,1211972,504994,605054,1203599,510803,549162,1367687,590999,470321,991825,414819,354704,1017793,422778,445492,1052538,422578,399901,1094820,447068,288610,2866,1,52154,"BIT","ST" 31,39,1,3,2,133,57,"OHIO EDISON CO","W H SAMMIS",0,"LIGHT OIL",13998,"0M",1294,,,95,21,47,2208,62,132,2422,24,52,2506,21,51,2619,18,49,2690,84,169,2569,424,916,2504,994,1895,1445,56,115,2687,17,62,1885,61,120,2363,49,78,2264,2866,1,52154,"FO2","IC" 31,39,1,5,2,133,80,"OHIO EDISON CO","W LORAIN JO",0,"LIGHT OIL",13998,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2869,1,52154,"FO2","CC" 31,39,1,6,2,133,80,"OHIO EDISON CO","W LORAIN JO",0,"LIGHT OIL",13998,"0M",1294,"A",,95,0,0,0,0,0,0,18,114,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2869,1,52154,"FO2","CT" 31,39,1,2,2,141,28,"OHIO POWER CO","MUSKINGUM R",0,"LIGHT OIL",14006,"0M",1294,,364,95,3882,6525,18086,2171,3713,17991,1663,2732,19038,2100,3500,20732,2616,4271,21458,2357,4274,22882,1323,2298,23072,3025,5284,24028,1082,2039,25141,1349,2367,24554,1527,2671,21638,6433,9974,10617,2872,1,54028,"FO2","ST" 31,39,1,2,6,141,28,"OHIO POWER CO","MUSKINGUM R",0,"BIT COAL",14006,"0M",1294,,364,95,535201,215186,421884,537048,220375,419768,597967,235236,427281,521184,207858,375208,449068,175136,430680,464394,194776,458208,580017,239178,402984,570215,237224,362814,265479,117802,367772,240284,100504,368567,286463,120853,342833,504050,190482,323803,2872,1,54028,"BIT","ST" 31,39,1,2,2,141,30,"OHIO POWER CO","GAVIN",0,"LIGHT OIL",14006,"0M",1294,,364,95,3763,6775,47403,769,1320,46083,4239,7491,38592,399,722,37870,719,1203,36667,2089,3543,33123,1042,1767,31357,1100,2128,29229,787,1372,39659,1447,2509,37150,1827,3076,34074,190,326,33748,8102,1,54028,"FO2","ST" 31,39,1,2,6,141,30,"OHIO POWER CO","GAVIN",0,"BIT COAL",14006,"0M",1294,,364,95,64858,30038,1931820,651490,284413,2186971,988276,436625,1888556,1196488,552083,1872871,1419448,615414,1838157,1182854,513910,1760692,1417031,613808,1615051,1643009,713610,1363516,1514789,657244,1159863,1269184,559173,1152059,1395530,601427,1176037,1375641,605361,1157372,8102,1,54028,"BIT","ST" 31,39,1,1,,141,35,"OHIO POWER CO","RACINE",0,,14006,"0M",1294,,364,95,18331,0,0,19396,0,0,21002,0,0,26318,0,0,19638,0,0,23776,0,0,16330,0,0,12023,0,0,7551,0,0,14526,0,0,23751,0,0,24817,0,0,6006,1,54028,"WAT","HY" 31,39,1,2,6,141,40,"OHIO POWER CO","TIDD",0,"BIT COAL",14006,"0M",1294,"S",364,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2874,1,54028,"BIT","ST" 31,39,1,2,2,147,1,"OHIO VALLEY ELEC CORP","KYGER CREEK",0,"LIGHT OIL",14015,"0M",1294,,506,95,214,364,1335,346,582,1079,478,772,930,80,131,1631,298,520,1248,203,342,1489,97,168,1464,0,0,1642,55,92,1550,582,973,577,236,390,1258,83,146,1373,2876,1,52156,"FO2","ST" 31,39,1,2,6,147,1,"OHIO VALLEY ELEC CORP","KYGER CREEK",0,"BIT COAL",14015,"0M",1294,,506,95,702913,271965,605907,555922,215202,643003,623778,230327,685798,645615,237897,675827,712862,278407,639864,676683,252935,580389,702720,270228,524058,722985,274975,470824,637930,231881,406765,609383,225508,431319,645928,235364,421426,715380,277692,649924,2876,1,52156,"BIT","ST" 31,39,1,2,1,168,1,"TOLEDO EDISON CO (THE)","DAVIS-BESSE",0,"NUCLEAR",18997,"0M",1294,,,95,658580,0,0,596841,0,0,657111,0,0,620608,0,0,643953,0,0,629968,0,0,645923,0,0,643124,0,0,630210,0,0,652469,0,0,633467,0,0,645496,0,0,6149,1,52927,"UR","ST" 31,39,1,2,2,168,9,"TOLEDO EDISON CO (THE)","ACME",0,"PROPANE",18997,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2877,1,52927,"FO2","ST" 31,39,1,2,6,168,9,"TOLEDO EDISON CO (THE)","ACME",0,"BIT COAL",18997,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2877,1,52927,"BIT","ST" 31,39,1,2,9,168,9,"TOLEDO EDISON CO (THE)","ACME",0,"NAT GAS",18997,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2877,1,52927,"NG","ST" 31,39,1,2,2,168,11,"TOLEDO EDISON CO (THE)","BAY SHORE",0,"LIGHT OIL",18997,"0M",1294,,,95,136,448,525,273,439,445,156,255,550,380,622,464,160,607,393,170,407,521,159,530,700,226,457,598,155,367,588,238,402,364,76,315,588,112,197,572,2878,1,52927,"FO2","ST" 31,39,1,2,6,168,11,"TOLEDO EDISON CO (THE)","BAY SHORE",0,"BIT COAL",18997,"0M",1294,,,95,271495,103216,169716,328463,121979,150035,259418,97335,167411,220548,81660,204738,228937,86543,252579,283830,108691,226673,265296,101256,155041,323077,180415,73781,309205,109740,75119,176674,67648,106761,254611,97258,111939,278242,107020,82847,2878,1,52927,"BIT","ST" 31,39,1,4,2,168,11,"TOLEDO EDISON CO (THE)","BAY SHORE",0,"LIGHT OIL",18997,"0M",1294,,,95,14,64,566,36,59,688,0,0,782,14,24,758,0,0,758,17,30,1086,46,267,997,175,646,886,8,62,825,2,5,820,0,19,979,1,53,926,2878,1,52927,"FO2","GT" 31,39,1,4,2,168,18,"TOLEDO EDISON CO (THE)","RICHLAND",0,"LIGHT OIL",18997,"0M",1294,,,95,0,40,2793,0,0,2793,0,0,2793,0,25,2768,0,3,2764,27,124,2641,49,260,2380,192,729,1652,0,0,1652,0,44,1607,0,0,2325,0,0,2325,2880,1,52927,"FO2","GT" 31,39,1,4,9,168,18,"TOLEDO EDISON CO (THE)","RICHLAND",0,"NAT GAS",18997,"0M",1294,,,95,0,276,0,0,594,0,0,324,0,0,621,0,0,756,0,25,675,0,71,2079,0,345,7385,0,0,215,0,0,3046,0,0,92,0,2,392,0,2880,1,52927,"NG","GT" 31,39,1,4,2,168,19,"TOLEDO EDISON CO (THE)","STRYKER",0,"LIGHT OIL",18997,"0M",1294,,,95,10,159,1191,0,0,1191,0,0,1191,0,0,1191,0,0,1191,0,0,1191,0,0,1191,0,8,1183,0,0,1183,16,41,1142,0,0,92,0,29,1113,2881,1,52927,"FO2","GT" 31,39,5,3,2,522,1,"ARCANUM (CITY OF)","ARCANUM",0,"LIGHT OIL",768,"0A",1294,,,95,27,51,203,49,90,186,15,31,155,4,8,148,3,5,143,17,33,110,14,27,82,52,101,101,4,8,93,3,6,87,4,13,74,8,21,171,2902,1,50096,"FO2","IC" 31,39,5,3,2,552,1,"BRYAN (CITY OF)","BRYAN",0,"LIGHT OIL",2439,"0M",1294,,,95,14,23,355,14,25,329,0,0,329,178,304,378,39,68,310,12,21,289,145,250,215,87,158,235,29,50,179,16,27,153,37,63,268,9,32,237,2903,1,50356,"FO2","IC" 31,39,5,4,2,552,1,"BRYAN (CITY OF)","BRYAN",0,"LIGHT OIL",2439,"0M",1294,,,95,22,50,6950,0,0,6950,2,156,6795,0,0,6790,0,0,6790,0,0,6790,0,0,6790,0,0,6790,0,0,6760,0,0,6720,6,12,6690,1,5,6682,2903,1,50356,"FO2","GT" 31,39,5,4,9,552,1,"BRYAN (CITY OF)","BRYAN",0,"NAT GAS",2439,"0M",1294,,,95,22,566,0,82,2330,0,0,0,0,254,4926,0,3992,62915,0,6018,86797,0,4936,89292,0,8968,190437,0,6094,104355,0,104,2299,0,132,2762,0,420,8161,0,2903,1,50356,"NG","GT" 31,39,5,4,2,561,2,"CLEVELAND (CITY OF)","COLLINWOOD",0,"LIGHT OIL",3762,"0M",1294,,,95,0,1,1070,0,4,1066,83,263,803,0,0,803,4,238,565,0,0,922,0,0,922,50,256,1022,0,0,1022,0,0,1022,0,0,1022,0,0,1022,2906,1,50589,"FO2","GT" 31,39,5,4,9,561,2,"CLEVELAND (CITY OF)","COLLINWOOD",0,"NAT GAS",3762,"0M",1294,,,95,27,729,0,0,0,0,1,32,0,0,33,0,0,0,0,674,8563,0,274,8962,0,32,941,0,17,380,0,0,3,0,0,7,0,0,4,0,2906,1,50589,"NG","GT" 31,39,5,2,2,561,10,"CLEVELAND (CITY OF)","LAKE ROAD",0,"LIGHT OIL",3762,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2908,1,50589,"FO2","ST" 31,39,5,2,6,561,10,"CLEVELAND (CITY OF)","LAKE ROAD",0,"BIT COAL",3762,"0M",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2908,1,50589,"BIT","ST" 31,39,5,4,2,561,20,"CLEVELAND (CITY OF)","W 41ST ST",0,"LIGHT OIL",3762,"0M",1294,,,95,0,1,1995,0,0,1994,0,0,1994,0,0,1993,0,0,1993,0,0,1992,0,1,1992,0,1,1991,0,0,1990,0,0,1990,0,1,1989,0,0,1989,2909,1,50589,"FO2","GT" 31,39,5,4,9,561,20,"CLEVELAND (CITY OF)","W 41ST ST",0,"NAT GAS",3762,"0M",1294,,,95,477,14950,0,526,10745,0,431,12673,0,247,6523,0,221,6443,0,340,8176,0,1197,15109,0,4074,94135,0,593,26459,0,537,13366,0,668,16240,0,628,17345,0,2909,1,50589,"NG","GT" 31,39,5,2,6,579,1,"DOVER (CITY OF)","DOVER",0,"BIT COAL",5336,"0M",1294,,,95,7510,5164,474,5838,3935,612,7700,4900,592,6987,4742,130,0,7,150,0,0,623,5223,3579,213,7330,5046,506,6122,4199,218,2658,1764,200,6852,5320,346,7262,4963,413,2914,1,50806,"BIT","ST" 31,39,5,2,9,579,1,"DOVER (CITY OF)","DOVER",0,"NAT GAS",5336,"0M",794,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,27,403,0,884,12716,0,410,6737,0,110,1163,0,663,9798,0,637,9130,0,2914,1,50806,"NG","ST" 31,39,5,3,2,579,1,"DOVER (CITY OF)","DOVER",0,"LIGHT OIL",5336,"0M",1294,,,95,0,0,66,0,0,66,4,9,61,0,0,66,0,0,57,18,228,79,36,74,109,29,75,101,0,0,101,0,0,101,0,0,101,0,0,101,2914,1,50806,"FO2","IC" 31,39,5,4,9,579,5,"DOVER (CITY OF)","DOVER",0,"NAT GAS",5336,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,65,1022,0,0,0,0,0,0,0,0,0,0,48,698,0,0,0,0,0,0,0,0,0,0,0,0,0,2914,1,50806,"NG","GT" 31,39,5,2,2,605,1,"HAMILTON (CITY OF)","HAM MUN EL",0,"LIGHT OIL",7977,"0M",1294,,,95,5,11,1751,1,3,1749,1,4,1747,1,5,1744,1,4,1743,4,10,1737,3,7,1734,4,9,1730,4,11,1724,1,4,1722,1,6,1719,7,16,1711,2917,1,51225,"FO2","ST" 31,39,5,2,6,605,1,"HAMILTON (CITY OF)","HAM MUN EL",0,"BIT COAL",7977,"0M",1294,,,95,22703,11176,13737,252,146,15989,5474,3315,16142,8640,5428,12982,9803,5101,7881,11553,6584,1297,16363,9478,2000,22973,9375,5688,24478,13592,4621,4956,3752,6715,4870,4046,7024,23079,11772,7422,2917,1,51225,"BIT","ST" 31,39,5,2,9,605,1,"HAMILTON (CITY OF)","HAM MUN EL",0,"NAT GAS",7977,"0M",1294,,,95,157,1874,0,13990,195116,0,5260,76784,0,483,7231,0,4563,57272,0,9310,123945,0,17338,207709,0,14384,141922,0,1816,24404,0,676,12116,0,270,5334,0,784,9339,0,2917,1,51225,"NG","ST" 31,39,5,4,2,605,1,"HAMILTON (CITY OF)","HAM MUN EL",0,"LIGHT OIL",7977,"0M",1294,,,95,0,0,1751,0,0,1749,0,0,1748,0,0,1745,0,0,1742,0,0,1738,0,0,1735,0,0,1730,0,0,1725,0,0,1723,0,0,1719,0,0,1711,2917,1,51225,"FO2","GT" 31,39,5,4,9,605,1,"HAMILTON (CITY OF)","HAM MUN EL",0,"NAT GAS",7977,"0M",1294,,,95,11,142,0,174,2439,0,83,1220,0,26,393,0,18,234,0,55,745,0,1064,12754,0,1170,28673,0,18,250,0,134,2411,0,10,207,0,18,217,0,2917,1,51225,"NG","GT" 31,39,5,1,,605,5,"HAMILTON (CITY OF)","HMLTN HYDRO",0,,7977,"0M",1294,"R",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,7807,1,51225,"WAT","HY" 31,39,5,3,2,629,1,"LEBANON (CITY OF)","LEBANON",0,"LIGHT OIL",10830,"0M",1294,,,95,3,23,1067,0,0,1067,90,268,799,0,0,799,0,0,799,0,0,799,29,63,734,52,106,805,0,0,805,0,0,805,0,0,805,0,0,805,2921,1,51615,"FO2","IC" 31,39,5,4,2,629,1,"LEBANON (CITY OF)","LEBANON",0,"LIGHT OIL",10830,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2921,1,51615,"FO2","GT" 31,39,5,3,2,684,1,"OBERLIN (CITY OF)","OBERLIN",0,"LIGHT OIL",13949,"0A",1294,,,95,5,65,637,21,41,596,0,37,558,8,17,528,0,0,509,33,80,429,17,210,218,239,528,405,11,41,364,8,17,348,194,525,358,145,391,324,2933,1,52140,"FO2","IC" 31,39,5,3,9,684,1,"OBERLIN (CITY OF)","OBERLIN",0,"NAT GAS",13949,"0A",1294,,,95,275,2724,0,260,2802,0,5,1676,0,75,826,0,13,132,0,200,1734,0,339,3535,0,552,5958,0,39,487,0,82,884,0,969,9721,0,63,1533,0,2933,1,52140,"NG","IC" 31,39,5,2,6,689,1,"ORRVILLE (CITY OF)","ORRVILLE",0,"BIT COAL",14194,"0M",1294,,,95,30925,20332,2401,27128,23359,528,19190,7163,1721,22147,13962,524,29670,13038,1437,23583,15893,1741,24259,14697,2641,28372,19561,2485,22121,14691,1281,18235,13105,1557,28993,15643,959,24197,16177,783,2935,1,52192,"BIT","ST" 31,39,5,2,9,689,1,"ORRVILLE (CITY OF)","ORRVILLE",0,"NAT GAS",14194,"0M",1294,,,95,45,744,0,42,811,0,122,1020,0,127,1797,0,112,1116,0,51,780,0,63,856,0,72,1126,0,22,331,0,46,762,0,78,961,0,76,1181,0,2935,1,52192,"NG","ST" 31,39,5,2,2,691,1,"PAINESVILLE (CITY OF)","PAINESVILLE",0,"LIGHT OIL",14381,"0M",1294,,,95,0,0,1518,0,0,1518,0,0,1518,36,100,1776,5,13,1762,0,0,1048,0,0,1762,25,73,1689,25,73,1616,4,14,1602,17,53,1548,10,20,1528,2936,1,52227,"FO2","ST" 31,39,5,2,6,691,1,"PAINESVILLE (CITY OF)","PAINESVILLE",0,"BIT COAL",14381,"0M",1294,,,95,17099,10622,1607,15231,10037,2990,13188,8922,6467,12361,8060,7830,13138,7996,7962,15287,8544,8154,15901,9966,8093,12362,8310,8580,11176,7757,8780,11298,8213,9293,8336,6116,9293,7235,5099,7825,2936,1,52227,"BIT","ST" 31,39,5,2,9,691,1,"PAINESVILLE (CITY OF)","PAINESVILLE",0,"NAT GAS",14381,"0M",1294,,,95,16,258,0,29,464,0,152,2440,0,67,1072,0,27,394,0,18,254,0,42,658,0,113,1904,0,81,1386,0,46,839,0,100,1812,0,97,1715,0,2936,1,52227,"NG","ST" 31,39,5,2,2,700,10,"PIQUA (CITY OF)","PIQUA",0,"LIGHT OIL",15095,"0M",1294,,,95,0,1,33,1,9,24,0,0,35,1,7,27,0,0,32,0,1,31,0,1,30,0,0,30,0,0,30,0,4,26,0,3,23,1,6,36,2937,1,52334,"FO2","ST" 31,39,5,2,6,700,10,"PIQUA (CITY OF)","PIQUA",0,"BIT COAL",15095,"0M",1294,,,95,2963,3832,1560,2779,3526,1061,2427,2994,1038,1970,2648,582,2418,2789,195,1914,2556,734,1374,2211,15,1611,2421,41,1481,2312,382,2468,3140,627,2650,3515,1751,2688,3569,2090,2937,1,52334,"BIT","ST" 31,39,5,4,2,700,10,"PIQUA (CITY OF)","PIQUA",0,"LIGHT OIL",15095,"0M",1294,,,95,24,119,2949,51,239,3071,-37,127,2947,119,588,2896,109,897,3032,277,1359,2730,469,2758,2645,595,2956,2720,-11,101,2619,37,176,2979,59,288,3048,121,591,2992,2937,1,52334,"FO2","GT" 31,39,5,2,6,722,1,"SAINT MARYS (CITY OF)","ST MARYS",0,"BIT COAL",17891,"0M",1294,,,95,1250,698,645,3927,2565,332,4111,3269,140,0,0,150,0,0,150,1641,1050,490,5298,3368,489,222,149,638,1630,1068,419,4646,3274,449,4461,2807,449,4928,3119,495,2942,1,52789,"BIT","ST" 31,39,5,4,2,722,1,"SAINT MARYS (CITY OF)","ST MARYS",0,"LIGHT OIL",17891,"0M",1294,,,95,1,12,318,0,0,307,28,146,352,0,0,352,0,0,352,1,4,348,59,83,428,3,8,420,1,24,396,0,0,520,1,3,518,2,6,512,2942,1,52789,"FO2","GT" 31,39,5,2,6,726,1,"SHELBY (CITY OF)","SHELBY",0,"BIT COAL",17043,"0M",1294,,,95,8039,5710,300,7249,5098,300,7132,4852,300,6141,3985,300,6694,4389,300,8103,4859,300,6796,4831,300,7378,5266,0,6897,3944,300,6844,4580,300,7615,5188,300,8726,5206,300,2943,1,52637,"BIT","ST" 31,39,5,2,9,726,1,"SHELBY (CITY OF)","SHELBY",0,"NAT GAS",17043,"0M",1294,,,95,134,1996,0,47,686,0,36,517,0,9,134,0,0,0,0,30,381,0,96,1415,0,11,164,0,19,230,0,41,576,0,48,685,0,44,555,0,2943,1,52637,"NG","ST" 31,39,5,3,2,726,1,"SHELBY (CITY OF)","SHELBY",0,"LIGHT OIL",17043,"0M",1294,,,95,0,0,73,0,0,73,0,0,73,0,0,103,0,0,103,0,0,103,1,5,93,1,4,83,2,5,78,0,1,77,0,1,76,0,1,45,2943,1,52637,"FO2","IC" 31,39,5,3,9,726,1,"SHELBY (CITY OF)","SHELBY",0,"NAT GAS",17043,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2943,1,52637,"NG","IC" 31,39,5,3,2,774,1,"WOODSFIELD (CITY OF)","WOODSFIELD",0,"LIGHT OIL",20977,"0A",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2945,1,53350,"FO2","IC" 31,39,5,3,9,774,1,"WOODSFIELD (CITY OF)","WOODSFIELD",0,"NAT GAS",20977,"0A",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2945,1,53350,"NG","IC" 31,39,8,2,6,800,1,"AMER MUN POWER-OHIO INC","R GORSUCH",0,"BIT COAL",40577,"0M",1294,,,95,99037,64265,81413,104738,67228,84252,126378,79745,86718,63579,42733,100556,123281,76701,94920,115392,69307,101317,117333,72018,101225,121473,79176,86641,108722,66669,90892,126955,78956,87022,103717,67360,86260,126485,80616,78276,7286,1,58910,"BIT","ST" 31,39,8,2,9,800,1,"AMER MUN POWER-OHIO INC","R GORSUCH",0,"NAT GAS",40577,"0M",1294,,,95,1576,22702,0,1469,21157,0,638,9083,0,541,8226,0,767,10634,0,1094,14686,0,877,12191,0,505,7352,0,810,11188,0,528,7439,0,733,10544,0,821,11624,0,7286,1,58910,"NG","ST" 32,18,1,2,6,25,1,"COMMONWEALTH ED CO IND","STATE LINE",0,"BIT COAL",4111,"0M",1294,,101,95,111368,64033,111935,149730,82697,41943,169301,90886,94463,49952,30907,197006,107334,61118,203229,185763,102059,199201,147171,80912,167481,211732,117972,103696,93902,54629,131796,97942,56647,95060,141995,78255,74660,93050,52182,100094,981,4,54003,"BIT","ST" 32,18,1,2,9,25,1,"COMMONWEALTH ED CO IND","STATE LINE",0,"NAT GAS",4111,"0M",1294,,101,95,6077,64670,0,5326,53012,0,4895,48146,0,1349,14775,0,4538,48258,0,4988,51500,0,4470,45645,0,4498,45907,0,2972,32243,0,3706,39699,0,5098,51893,0,3793,39849,0,981,4,54003,"NG","ST" 32,18,1,2,2,45,1,"INDIANA-KENTUCKY EL CORP","CLIFTY CRK",0,"LIGHT OIL",9269,"0M",1294,,505,95,186,351,3905,152,276,3630,241,444,3700,377,692,3522,263,551,3142,200,360,3468,175,320,4005,93,171,4177,112,189,3988,183,330,3658,234,419,3925,187,321,3947,983,1,54010,"FO2","ST" 32,18,1,2,6,45,1,"INDIANA-KENTUCKY EL CORP","CLIFTY CRK",0,"BIT COAL",9269,"0M",1294,,505,95,680000,340288,711560,681685,332462,794224,771872,377298,719124,715568,349771,768331,774831,394798,790608,706890,347717,739042,846234,432529,698423,836401,439085,664104,841295,424266,608234,755940,378632,751924,859900,416889,759244,867253,423226,804472,983,1,54010,"BIT","ST" 32,18,1,1,,57,5,"INDIANA MICHIGAN POWER CO","ELKHART",0,,9324,"0M",1294,,363,95,1650,0,0,1194,0,0,1755,0,0,1250,0,0,1341,0,0,1179,0,0,1157,0,0,1230,0,0,728,0,0,610,0,0,606,0,0,1138,0,0,986,1,57745,"WAT","HY" 32,18,1,1,,57,15,"INDIANA MICHIGAN POWER CO","TWIN BRANCH",0,,9324,"0M",1294,,363,95,2749,0,0,2559,0,0,3177,0,0,3035,0,0,3169,0,0,2570,0,0,2394,0,0,2550,0,0,1769,0,0,1707,0,0,2868,0,0,2542,0,0,989,1,57745,"WAT","HY" 32,18,1,2,2,57,40,"INDIANA MICHIGAN POWER CO","TANNERS CRK",0,"LIGHT OIL",9324,"0M",1294,,363,95,1203,1922,5959,701,1134,5915,1180,2025,6714,1059,1682,6177,1112,1829,5848,1144,1978,6336,1259,2060,7095,1078,1912,5713,665,1191,4522,206,409,5361,886,1592,4308,1326,2011,4418,988,1,57745,"FO2","ST" 32,18,1,2,6,57,40,"INDIANA MICHIGAN POWER CO","TANNERS CRK",0,"BIT COAL",9324,"0M",1294,,363,95,432338,162155,420217,485332,183170,404434,427268,171172,375261,371083,146417,383926,364601,144830,374644,383224,158993,372917,442272,183537,275408,494886,200826,195877,151186,61682,248353,10073,4559,312659,189477,75997,327350,330050,118848,262047,988,1,57745,"BIT","ST" 32,18,1,4,2,57,55,"INDIANA MICHIGAN POWER CO","FOURTH ST",0,"LIGHT OIL",9324,"0M",1294,,363,95,0,0,90,0,0,90,0,0,90,0,0,90,0,0,90,0,0,90,0,0,90,0,0,90,0,0,90,0,0,90,0,0,90,0,0,90,1025,1,57745,"FO2","GT" 32,18,1,2,2,57,60,"INDIANA MICHIGAN POWER CO","ROCKPORT",0,"LIGHT OIL",9324,"0M",1294,,363,95,1253,2167,36532,1335,2320,34384,3886,6841,48740,4321,7609,41131,3580,6420,34711,5662,10180,45654,3887,6888,38767,4216,7569,31198,1478,2587,28611,1002,1634,26976,690,1194,25782,1723,4126,33355,6166,1,57745,"FO2","ST" 32,18,1,2,6,57,60,"INDIANA MICHIGAN POWER CO","ROCKPORT",0,"BIT COAL",9324,"0M",1294,,363,95,1749008,1032186,1725862,1579775,933220,1565332,1339465,797497,1717887,1321428,787392,1749794,910898,553161,1861348,1507665,916281,1691338,1420244,862282,1685879,1514621,918947,1761783,1599963,954251,1694782,1691163,933949,1738612,1640828,959611,1762887,1464158,854236,1918162,6166,1,57745,"BIT","ST" 32,18,1,2,2,63,5,"INDIANAPOLIS PWR & LGT CO","E W STOUT",0,"LIGHT OIL",9273,"0M",1294,,,95,566,1401,20541,856,1914,17945,116,609,17337,446,1143,15565,419,1038,14023,233,762,13073,334,805,11083,970,3484,18728,223,679,18049,471,1101,16948,1380,2012,14910,618,1456,13138,990,1,51394,"FO2","ST" 32,18,1,2,6,63,5,"INDIANAPOLIS PWR & LGT CO","E W STOUT",0,"BIT COAL",9273,"0M",1294,,,95,194584,90056,252587,180919,84581,279836,140480,66420,317709,160947,73882,318796,235268,109052,299888,217930,103073,287645,259644,122601,267666,349367,162431,221093,272895,126479,196285,244308,112170,197708,270443,125748,220391,253279,116842,274191,990,1,51394,"BIT","ST" 32,18,1,3,2,63,5,"INDIANAPOLIS PWR & LGT CO","E W STOUT",0,"LIGHT OIL",9273,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,990,1,51394,"FO2","IC" 32,18,1,4,2,63,5,"INDIANAPOLIS PWR & LGT CO","E W STOUT",0,"LIGHT OIL",9273,"0M",1294,,,95,1107,4856,0,-42,681,0,-50,0,0,112,628,0,182,504,0,-7,189,0,293,1179,0,349,1894,0,-35,0,0,-43,0,0,-50,26,0,-11,317,0,990,1,51394,"FO2","GT" 32,18,1,4,9,63,5,"INDIANAPOLIS PWR & LGT CO","E W STOUT",0,"NAT GAS",9273,"0M",1294,,,95,1286,11256,0,10,1339,0,-53,1880,0,93,2875,0,1102,18630,0,448,8470,0,4489,66365,0,11695,166046,0,-64,3722,0,-37,1618,0,3205,49273,0,3710,54428,0,990,1,51394,"NG","GT" 32,18,1,2,2,63,15,"INDIANAPOLIS PWR & LGT CO","PERRY K",0,"LIGHT OIL",9273,"0M",1294,,,95,0,0,4682,0,0,4553,0,0,4331,0,0,4301,0,0,4287,0,0,3841,0,0,3636,0,0,5062,0,0,5057,0,0,5051,0,0,5042,0,0,4762,992,1,51394,"FO2","ST" 32,18,1,2,6,63,15,"INDIANAPOLIS PWR & LGT CO","PERRY K",0,"BIT COAL",9273,"0M",1294,,,95,0,0,79574,-1610,0,80083,0,0,75101,0,0,73147,0,0,75348,0,0,76456,766,826,73924,340,352,74885,1152,1362,75776,0,0,74934,0,0,77090,0,0,71176,992,1,51394,"BIT","ST" 32,18,1,2,9,63,15,"INDIANAPOLIS PWR & LGT CO","PERRY K",0,"NAT GAS",9273,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,17,437,0,7,193,0,32,957,0,0,0,0,0,0,0,0,0,0,992,1,51394,"NG","ST" 32,18,1,5,9,63,15,"INDIANAPOLIS PWR & LGT CO","PERRY K",0,"WASTE HT",9273,"0M",1294,,,95,-782,0,0,0,0,0,1330,0,0,1056,0,0,2878,0,0,887,0,0,1971,0,0,1192,0,0,1301,0,0,1055,0,0,-372,0,0,-854,0,0,992,1,51394,"WT","CC" 32,18,1,2,2,63,20,"INDIANAPOLIS PWR & LGT CO","PERRY W",0,"LIGHT OIL",9273,"0M",1294,,,95,-49,0,697,-71,0,697,-71,0,697,-67,0,697,-59,0,697,-46,0,697,-51,0,697,-47,0,697,-42,0,697,-44,0,697,-59,0,697,-65,0,697,993,1,51394,"FO2","ST" 32,18,1,2,9,63,20,"INDIANAPOLIS PWR & LGT CO","PERRY W",0,"NAT GAS",9273,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,993,1,51394,"NG","ST" 32,18,1,5,9,63,20,"INDIANAPOLIS PWR & LGT CO","PERRY W",0,"WASTE HT",9273,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,993,1,51394,"WH","CC" 32,18,1,2,2,63,23,"INDIANAPOLIS PWR & LGT CO","PETERSBURG",0,"LIGHT OIL",9273,"0M",1294,,,95,610,1111,6386,445,819,5517,317,533,4940,401,748,8963,2218,4082,4553,637,1151,5787,377,687,4945,1822,3221,6367,801,1483,4763,545,999,3635,1447,2637,5880,1975,3581,4564,994,1,51394,"FO2","ST" 32,18,1,2,6,63,23,"INDIANAPOLIS PWR & LGT CO","PETERSBURG",0,"BIT COAL",9273,"0M",1294,,,95,1040025,481608,951198,910590,421941,973809,942914,432679,1023657,783657,368727,1096578,667135,315158,1184238,973163,448245,1179213,992610,460767,1051137,936517,439379,945966,722162,339012,925268,812107,376653,886087,794558,370468,820716,931266,431118,719090,994,1,51394,"BIT","ST" 32,18,1,3,2,63,23,"INDIANAPOLIS PWR & LGT CO","PETERSBURG",0,"LIGHT OIL",9273,"0M",1294,,,95,2,5,0,0,0,0,25,44,0,102,178,0,189,328,0,45,76,0,52,90,0,74,131,0,46,80,0,67,116,0,39,43,0,31,78,0,994,1,51394,"FO2","IC" 32,18,1,2,2,63,25,"INDIANAPOLIS PWR & LGT CO","H T PRTCHRD",0,"LIGHT OIL",9273,"0M",1294,,,95,318,680,5661,350,656,4975,104,195,4685,436,902,7879,417,829,7014,283,586,6386,443,914,5445,1802,3787,7417,307,627,7108,203,431,6547,316,654,5835,499,993,4785,991,1,51394,"FO2","ST" 32,18,1,2,6,63,25,"INDIANAPOLIS PWR & LGT CO","H T PRTCHRD",0,"BIT COAL",9273,"0M",1294,,,95,39918,21829,172846,38399,18739,164110,25730,13890,166007,31554,16614,192907,62657,32105,189004,38978,20477,189810,89346,46785,168301,129720,68988,123731,61410,31642,119624,29705,15920,161259,67519,35572,171574,68221,34547,157787,991,1,51394,"BIT","ST" 32,18,1,3,2,63,25,"INDIANAPOLIS PWR & LGT CO","H T PRTCHRD",0,"LIGHT OIL",9273,"0M",1294,,,95,10,18,0,10,18,0,11,19,0,10,19,0,10,19,0,10,18,0,9,18,0,10,18,0,9,18,0,3,5,0,10,11,0,10,16,0,991,1,51394,"FO2","IC" 32,18,1,1,,97,25,"NORTHERN IND PUB SERV CO","NORWAY",0,,13756,"0M",1294,,,95,2951,0,0,1754,0,0,3112,0,0,3813,0,0,3505,0,0,2903,0,0,2206,0,0,1230,0,0,509,0,0,-5,0,0,935,0,0,741,0,0,998,1,52101,"WAT","HY" 32,18,1,1,,97,30,"NORTHERN IND PUB SERV CO","OAKDALE",0,,13756,"0M",1294,,,95,4302,0,0,2658,0,0,4495,0,0,5358,0,0,4552,0,0,4225,0,0,3387,0,0,1840,0,0,1214,0,0,492,0,0,1566,0,0,1435,0,0,999,1,52101,"WAT","HY" 32,18,1,2,5,97,35,"NORTHERN IND PUB SERV CO","BAILLY",0,"COKE",13756,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,995,1,52101,"PC","ST" 32,18,1,2,6,97,35,"NORTHERN IND PUB SERV CO","BAILLY",0,"BIT COAL",13756,"0M",1294,,,95,255092,122559,79738,278804,133215,33213,188964,93227,81145,300874,140721,83750,249838,120767,64124,246937,117749,44162,235477,114020,45186,281196,134308,37119,206770,100042,54350,171878,84048,49037,248313,118863,34340,215434,105042,32995,995,1,52101,"BIT","ST" 32,18,1,2,9,97,35,"NORTHERN IND PUB SERV CO","BAILLY",0,"NAT GAS",13756,"0M",1294,,,95,2509,26046,0,1617,16709,0,6960,74244,0,364,3631,0,132,1380,0,473,4895,0,3976,41921,0,11155,116087,0,295,3099,0,9000,94567,0,731,7651,0,10008,106430,0,995,1,52101,"NG","ST" 32,18,1,4,2,97,35,"NORTHERN IND PUB SERV CO","BAILLY",0,"LIGHT OIL",13756,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,995,1,52101,"FO2","GT" 32,18,1,4,9,97,35,"NORTHERN IND PUB SERV CO","BAILLY",0,"NAT GAS",13756,"0M",1294,,,95,260,4325,0,239,4585,0,197,4652,0,73,729,0,0,0,0,128,2648,0,1309,27718,0,1556,27641,0,86,2797,0,94,990,0,0,0,0,0,0,0,995,1,52101,"NG","GT" 32,18,1,2,6,97,50,"NORTHERN IND PUB SERV CO","MICH CITY",0,"BIT COAL",13756,"0M",1294,,,95,236420,123317,103301,234123,120234,148075,251278,135807,162546,205743,116541,177892,112253,67389,170049,124057,76284,129959,232893,135633,114125,231506,135299,93596,234187,129907,86183,254454,138881,100596,227408,129965,87044,241351,131616,87326,997,1,52101,"BIT","ST" 32,18,1,2,9,97,50,"NORTHERN IND PUB SERV CO","MICH CITY",0,"NAT GAS",13756,"0M",1294,,,95,22888,245981,0,12315,127428,0,7313,77250,0,2223,23885,0,17374,195664,0,14491,167133,0,33790,372448,0,46983,516773,0,57,601,0,277,2894,0,14761,158089,0,7779,81844,0,997,1,52101,"NG","ST" 32,18,1,2,6,97,54,"NORTHERN IND PUB SERV CO","D MITCHELL",0,"BIT COAL",13756,"0M",1294,,,95,145857,82802,116751,116897,65893,113729,119863,69185,152487,141199,84936,154502,149654,87531,159194,148998,85732,121077,153374,92272,109798,153611,89672,90907,105137,61906,133520,134131,77926,126283,118138,72811,149593,119904,77033,120350,996,1,52101,"BIT","ST" 32,18,1,2,9,97,54,"NORTHERN IND PUB SERV CO","D MITCHELL",0,"NAT GAS",13756,"0M",1294,,,95,9050,99836,0,19988,219179,0,4693,51173,0,2044,22775,0,681,7679,0,15253,169699,0,31855,357533,0,49912,561059,0,1836,21192,0,688,7733,0,17585,198980,0,12007,137527,0,996,1,52101,"NG","ST" 32,18,1,4,2,97,54,"NORTHERN IND PUB SERV CO","D MITCHELL",0,"LIGHT OIL",13756,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,996,1,52101,"FO2","GT" 32,18,1,4,9,97,54,"NORTHERN IND PUB SERV CO","D MITCHELL",0,"NAT GAS",13756,"0M",1294,,,95,0,0,0,62,1005,0,19,314,0,61,972,0,59,947,0,23,381,0,1109,18451,0,787,13562,0,0,0,0,17,200,0,19,316,0,40,614,0,996,1,52101,"NG","GT" 32,18,1,2,2,97,60,"NORTHERN IND PUB SERV CO","SCHAHFER",0,"LIGHT OIL",13756,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,6085,1,52101,"FO2","ST" 32,18,1,2,5,97,60,"NORTHERN IND PUB SERV CO","SCHAHFER",0,"COKE",13756,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,5680,2361,3668,16726,6787,383,17831,7291,7,6085,1,52101,"PC","ST" 32,18,1,2,6,97,60,"NORTHERN IND PUB SERV CO","SCHAHFER",0,"BIT COAL",13756,"0M",1294,,,95,535261,312105,335057,389163,229937,440028,546548,302317,415959,448635,246990,395514,597050,350998,454670,756850,452731,337454,682007,398333,335076,754511,435319,290970,649742,383628,258615,683709,390480,291948,637992,357548,247219,681946,380639,238033,6085,1,52101,"BIT","ST" 32,18,1,2,9,97,60,"NORTHERN IND PUB SERV CO","SCHAHFER",0,"NAT GAS",13756,"0M",1294,,,95,3899,42407,0,6373,71396,0,4950,53485,0,5022,55321,0,9160,101163,0,8473,94946,0,11416,127138,0,11318,127241,0,6765,76948,0,5330,59832,0,10465,114654,0,16610,183389,0,6085,1,52101,"NG","ST" 32,18,1,4,2,97,60,"NORTHERN IND PUB SERV CO","SCHAHFER",0,"LIGHT OIL",13756,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,6085,1,52101,"FO2","GT" 32,18,1,4,9,97,60,"NORTHERN IND PUB SERV CO","SCHAHFER",0,"NAT GAS",13756,"0M",1294,,,95,723,10302,0,782,11325,0,1650,23018,0,308,4700,0,805,15657,0,1994,32783,0,15126,225451,0,13726,215839,0,142,2242,0,733,10618,0,280,4262,0,601,10905,0,6085,1,52101,"NG","GT" 32,18,1,1,,115,10,"PSI ENERGY, INC","MARKLAND",0,,15470,"0M",1294,,,95,25874,0,0,30535,0,0,30427,0,0,34190,0,0,21420,0,0,33483,0,0,37429,0,0,31238,0,0,21329,0,0,31723,0,0,32028,0,0,33480,0,0,1005,1,52410,"WAT","HY" 32,18,1,2,2,115,20,"PSI ENERGY, INC","CAYUGA",0,"LIGHT OIL",15470,"0M",1294,,,95,132,235,5513,571,1037,4367,530,968,3231,360,648,6046,1268,2286,3656,1673,3058,5188,191,340,4690,456,897,3714,450,808,2757,116,203,4365,648,1159,3695,1043,1890,4595,1001,1,52410,"FO2","ST" 32,18,1,2,6,115,20,"PSI ENERGY, INC","CAYUGA",0,"BIT COAL",15470,"0M",1294,,,95,560086,260374,595374,436002,205588,619769,507290,241920,579748,458167,216960,558238,273942,132145,579528,461324,222630,594519,529339,250671,586438,553167,264792,531310,481498,229472,498542,556861,260068,435186,538773,254635,379746,560196,264529,360124,1001,1,52410,"BIT","ST" 32,18,1,3,2,115,20,"PSI ENERGY, INC","CAYUGA",0,"LIGHT OIL",15470,"0M",1294,,,95,52,94,835,80,146,689,46,85,604,32,59,546,48,87,793,40,74,719,187,332,719,345,632,893,44,79,814,57,100,714,46,83,810,52,95,715,1001,1,52410,"FO2","IC" 32,18,1,4,2,115,20,"PSI ENERGY, INC","CAYUGA",0,"LIGHT OIL",15470,"0M",1294,,,95,94,169,5321,0,0,5313,0,0,5287,0,0,5295,9,17,5278,0,0,5274,0,0,5261,0,0,5256,0,0,5278,0,0,5291,0,0,5304,0,0,5321,1001,1,52410,"FO2","GT" 32,18,1,4,9,115,20,"PSI ENERGY, INC","CAYUGA",0,"NAT GAS",15470,"0M",1294,,,95,2346,23310,0,1913,19353,0,1506,15557,0,1635,16714,0,1240,12674,0,4044,41468,0,15842,159433,0,18202,212550,0,0,0,0,0,0,0,2097,21202,0,3527,35908,0,1001,1,52410,"NG","GT" 32,18,1,2,2,115,30,"PSI ENERGY, INC","EDWARDSPORT",0,"LIGHT OIL",15470,"0M",1294,,,95,209,496,4820,64,150,4672,155,373,4297,0,0,4295,0,0,4292,97,238,4052,689,1571,2481,2502,5818,2869,342,868,2002,0,0,2002,0,0,1997,147,370,1625,1004,1,52410,"FO2","ST" 32,18,1,2,6,115,30,"PSI ENERGY, INC","EDWARDSPORT",0,"BIT COAL",15470,"0M",1294,,,95,17730,11048,72080,19934,11948,70647,12688,8051,74559,-527,0,75232,-535,0,75232,15454,10259,64973,35050,21901,43072,52741,33340,15650,4173,2912,38766,-602,0,62015,-609,0,63195,16335,10947,52274,1004,1,52410,"BIT","ST" 32,18,1,2,2,115,32,"PSI ENERGY, INC","R GALLAGHER",0,"LIGHT OIL",15470,"0M",1294,,,95,2035,3891,1605,1454,2810,1394,1851,3297,1699,1757,3179,1643,2068,3708,1567,1765,3297,1717,1740,3339,1643,1698,3478,1699,628,1171,1662,1918,3473,1772,1054,1957,1432,2452,4557,1662,1008,1,52410,"FO2","ST" 32,18,1,2,6,115,32,"PSI ENERGY, INC","R GALLAGHER",0,"BIT COAL",15470,"0M",1294,,,95,228795,101724,280677,208492,94433,264483,157312,68908,321856,177541,78622,327010,219815,95103,325222,282888,123689,301473,287606,128632,273012,307948,143686,219622,142108,60394,233330,173570,72509,241738,224846,92953,254240,214410,90070,255848,1008,1,52410,"BIT","ST" 32,18,1,2,2,115,35,"PSI ENERGY, INC","NOBLESVILLE",0,"LIGHT OIL",15470,"0M",1294,,,95,51,112,562,83,160,505,48,112,674,66,152,531,0,0,490,110,229,643,81,169,664,55,117,548,22,64,674,58,167,474,0,43,548,34,71,476,1007,1,52410,"FO2","ST" 32,18,1,2,6,115,35,"PSI ENERGY, INC","NOBLESVILLE",0,"BIT COAL",15470,"0M",1294,,,95,11044,6031,55495,9455,4868,50627,3897,2460,49399,4036,2484,49078,-19,344,48734,11688,6456,42278,26318,14879,27399,34289,19561,18825,965,758,32438,3085,2324,49315,-104,155,61612,12274,6417,55744,1007,1,52410,"BIT","ST" 32,18,1,2,2,115,38,"PSI ENERGY, INC","WABASH RIVR",0,"LIGHT OIL",15470,"0M",1294,,,95,2430,4476,2106,1459,2739,2128,1389,2692,1967,1849,3579,2218,1434,2758,1631,681,1290,2176,1683,3263,2148,2465,4797,2269,945,1807,2338,1000,1900,2380,729,1435,2430,2010,3862,1720,1010,1,52410,"FO2","ST" 32,18,1,2,6,115,38,"PSI ENERGY, INC","WABASH RIVR",0,"BIT COAL",15470,"0M",1294,,,95,269453,126688,229629,237554,115161,230254,111825,56100,288778,84991,42415,325474,75621,37146,348471,305101,147377,290801,239625,122121,244288,280979,141633,160506,165651,82144,169356,117517,58071,210036,143505,72409,218547,185588,91761,206945,1010,1,52410,"BIT","ST" 32,18,1,3,2,115,38,"PSI ENERGY, INC","WABASH RIVR",0,"LIGHT OIL",15470,"0M",1294,,,95,22,41,295,6,12,283,29,57,226,36,71,155,22,43,283,17,33,250,46,91,336,25,50,286,1,2,283,16,31,37,14,29,343,5,10,333,1010,1,52410,"FO2","IC" 32,18,1,3,2,115,40,"PSI ENERGY, INC","MIAMI WBASH",0,"LIGHT OIL",15470,"0M",1294,,,95,-10,953,9190,166,743,8447,-197,894,7552,-39,60,7493,16,281,7212,81,612,6600,891,3627,5277,1034,3669,3913,-3,92,3821,-25,12,3809,-92,165,3644,-114,427,3217,1006,1,52410,"FO2","IC" 32,18,1,4,2,115,43,"PSI ENERGY, INC","CONNERSVILE",0,"LIGHT OIL",15470,"0M",1294,,,95,598,1430,6151,267,338,5812,185,528,5284,-1,88,5196,74,91,5105,363,946,4160,1734,3950,0,1728,5143,7132,123,299,6833,35,74,6797,36,197,6601,68,309,6291,1002,1,52410,"FO2","GT" 32,18,1,2,2,115,47,"PSI ENERGY, INC","GIBSON STA",0,"LIGHT OIL",15470,"0M",1294,,,95,3573,6225,8026,3627,6211,8525,2908,4962,6089,2299,3933,7385,2638,4537,9046,4608,8201,6236,1193,2069,8692,1020,1752,9495,2262,3909,8491,2394,4067,6679,1306,2237,7725,1788,3105,5067,6113,1,52410,"FO2","ST" 32,18,1,2,6,115,47,"PSI ENERGY, INC","GIBSON STA",0,"BIT COAL",15470,"0M",1294,,,95,1411040,662768,2861774,1615449,737476,2742578,1641475,746285,2737505,1326993,600387,2789580,1389674,630387,2844473,1353290,632853,2819275,1781130,810634,2543921,1880261,844888,2374175,1610199,724136,2280260,1401722,620957,2297336,1703790,761235,2101523,1647889,748548,1888232,6113,1,52410,"BIT","ST" 32,18,1,4,2,127,1,"SOUTHERN INDIANA G & E CO","BROADWAY",0,"LIGHT OIL",17633,"0M",1294,,,95,0,0,801,0,0,801,0,0,801,0,0,801,0,0,801,0,0,801,0,0,801,0,0,801,0,0,801,0,0,801,0,0,801,0,0,801,1011,1,52727,"FO2","GT" 32,18,1,4,9,127,1,"SOUTHERN INDIANA G & E CO","BROADWAY",0,"NAT GAS",17633,"0M",1294,,,95,108,1488,0,31,496,0,72,936,0,66,992,0,675,9932,0,358,9922,0,3822,54621,0,11701,173627,0,131,4946,0,181,9912,0,586,4959,0,0,0,0,1011,1,52727,"NG","GT" 32,18,1,2,2,127,3,"SOUTHERN INDIANA G & E CO","CULLEY",0,"LIGHT OIL",17633,"0M",1294,,,95,0,0,350,0,0,350,0,0,350,0,0,350,0,0,350,0,0,250,0,0,250,0,0,250,0,0,250,0,0,250,0,0,250,0,0,250,1012,1,52727,"FO2","ST" 32,18,1,2,6,127,3,"SOUTHERN INDIANA G & E CO","CULLEY",0,"BIT COAL",17633,"0M",1294,,,95,122067,60600,138140,167988,82419,159735,169634,79436,181228,114459,53639,191704,165848,81055,168418,184693,87570,154235,207611,100070,138520,218589,105190,134359,160446,77417,139667,174664,86907,135057,217251,106316,124021,205575,102713,115674,1012,1,52727,"BIT","ST" 32,18,1,2,9,127,3,"SOUTHERN INDIANA G & E CO","CULLEY",0,"NAT GAS",17633,"0M",1294,,,95,285,3090,0,126,1344,0,136,1410,0,300,3116,0,121,1311,0,107,1123,0,101,1082,0,285,3040,0,412,4406,0,312,3443,0,180,1935,0,153,1681,0,1012,1,52727,"NG","ST" 32,18,1,4,9,127,9,"SOUTHERN INDIANA G & E CO","NORTHEAST",0,"NAT GAS",17633,"0M",1294,,,95,24,992,0,48,5399,0,0,0,0,0,0,0,0,0,0,22,2492,0,0,0,0,562,10295,0,0,0,0,0,0,0,23,3023,0,26,4467,0,1013,1,52727,"NG","GT" 32,18,1,2,6,127,20,"SOUTHERN INDIANA G & E CO","WARRICK",0,"BIT COAL",17633,"0M",1294,,,95,95617,41510,100212,86572,39259,87257,96250,42312,89684,93020,40228,97629,96270,44344,83127,82739,38242,69870,89329,39892,44260,100497,44406,41656,97103,42826,35874,28941,12332,66823,92060,41077,55982,99718,45727,57793,6705,1,52727,"BIT","ST" 32,18,1,2,9,127,20,"SOUTHERN INDIANA G & E CO","WARRICK",0,"NAT GAS",17633,"0M",1294,,,95,27,261,0,112,1120,0,11,112,0,29,276,0,5,50,0,0,0,0,136,1318,0,83,796,0,0,0,0,295,2822,0,57,575,0,62,639,0,6705,1,52727,"NG","ST" 32,18,1,2,2,127,25,"SOUTHERN INDIANA G & E CO","BROWN",0,"LIGHT OIL",17633,"0M",1294,,,95,0,0,1712,0,0,1437,0,0,2186,0,0,2151,0,0,1998,0,0,1988,0,0,2336,0,0,2336,0,0,2336,0,0,2336,0,0,2175,0,0,2175,6137,1,52727,"FO2","ST" 32,18,1,2,6,127,25,"SOUTHERN INDIANA G & E CO","BROWN",0,"BIT COAL",17633,"0M",1294,,,95,217766,95613,450544,147685,72927,476200,218223,106171,479883,196964,85661,485255,182235,86959,499237,216954,101195,498135,247301,113099,429991,275892,131703,360852,177911,84026,286413,238026,112468,229493,139223,67172,246596,170321,82481,189492,6137,1,52727,"BIT","ST" 32,18,1,2,9,127,25,"SOUTHERN INDIANA G & E CO","BROWN",0,"NAT GAS",17633,"0M",1294,,,95,728,7231,0,709,7962,0,465,5154,0,1271,12486,0,681,7404,0,869,9196,0,829,8558,0,910,9792,0,91,976,0,1005,9912,0,462,4959,0,1013,10609,0,6137,1,52727,"NG","ST" 32,18,1,4,2,127,25,"SOUTHERN INDIANA G & E CO","BROWN",0,"LIGHT OIL",17633,"0M",1294,,,95,0,0,0,139,275,0,10,21,0,20,35,0,75,144,0,155,289,0,4,9,0,0,0,0,0,0,0,0,0,0,84,161,0,0,0,0,6137,1,52727,"FO2","GT" 32,18,1,4,9,127,25,"SOUTHERN INDIANA G & E CO","BROWN",0,"NAT GAS",17633,"0M",1294,,,95,371,3684,0,237,2668,0,72,799,0,244,2399,0,872,9478,0,725,7671,0,3499,36107,0,8313,89423,0,835,8917,0,0,0,0,0,0,0,115,1208,0,6137,1,52727,"NG","GT" 32,18,5,3,2,529,15,"BLUFFTON (CITY OF)","BLUFFTON",0,"LIGHT OIL",1896,"0A",1294,,,95,1,60,1391,2,67,1322,61,54,1600,8,70,1533,12,90,1444,17,90,1361,5,46,0,16,58,1746,9,46,1693,5,45,1674,1,9,1658,1,20,1637,1023,1,54077,"FO2","IC" 32,18,5,3,9,529,15,"BLUFFTON (CITY OF)","BLUFFTON",0,"NAT GAS",1896,"0A",1294,,,95,252,951,0,283,1047,0,187,936,0,252,888,0,327,1129,0,322,1124,0,21,749,0,165,1201,0,79,956,0,14,141,0,8,282,0,62,1131,0,1023,1,54077,"NG","IC" 32,18,5,2,6,552,1,"CRAWFORDSVILLE (CITY OF)","CRAWFRDVIL",0,"BIT COAL",4508,"M",1294,,,95,2633,2217,2514,2446,2032,2094,1890,1637,1012,0,12,1693,0,9,2211,497,408,1961,0,0,1961,1383,1034,1775,0,0,2801,0,0,2783,0,0,2783,2446,2070,2457,1024,1,50698,"BIT","ST" 32,18,5,2,9,552,1,"CTAWFORDSVILLE (CITY OF)","CRAWFRDVIL",0,"NAT GAS",4508,"M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,11,198,0,0,9,0,25,397,0,0,0,0,0,0,0,0,0,0,0,0,0,1024,1,50698,"NG","ST" 32,18,5,3,2,552,1,"CRAWFORDSVILLE (CITY OF)","CRAWFRDVIL",0,"LIGHT OIL",4508,"M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1024,1,50698,"FO2","IC" 32,18,5,2,6,601,1,"JASPER (CITY OF)","JASPER",0,"BIT COAL",9667,"0A",1294,,,95,5717,4616,631,5399,3895,631,5890,4398,631,2952,2186,631,3065,2373,631,5988,4375,631,5621,4191,631,2798,2138,631,0,0,1075,5001,3514,1051,5782,4146,1096,5466,4050,1096,6225,1,51443,"BIT","ST" 32,18,5,2,9,601,1,"JASPER (CITY OF)","JASPER",0,"NAT GAS",9667,"0A",1294,,,95,20,339,0,0,0,0,0,0,0,0,0,0,16,267,0,0,0,0,0,0,0,0,0,0,0,0,0,14,206,0,0,0,0,0,0,0,6225,1,51443,"NG","ST" 32,18,5,2,6,622,1,"LOGANSPORT (CITY OF)","LOGANSPORT",0,"BIT COAL",11142,"0M",1294,,,95,16294,10401,3093,15182,9658,2825,130,68,5257,0,0,7057,2842,2773,7049,15721,9566,3565,18496,9015,1600,18517,10895,1421,17032,9835,4095,8771,5557,5126,12606,7370,5733,23315,13078,934,1032,1,51681,"BIT","ST" 32,18,5,4,2,622,1,"LOGANSPORT (CITY OF)","LOGANSPORT",0,"LIGHT OIL",11142,"0M",1294,,,95,0,0,1887,0,0,1887,0,0,1887,0,0,1887,0,0,1887,0,0,1887,0,0,1887,0,0,1887,0,0,1887,0,0,1887,0,0,1887,0,0,1887,1032,1,51681,"FO2","GT" 32,18,5,4,9,622,1,"LOGANSPORT (CITY OF)","LOGANSPORT",0,"NAT GAS",11142,"0M",1294,,,95,127,2771,0,0,0,0,0,0,0,0,0,0,0,0,0,75,2842,0,0,0,0,217,5351,0,0,0,0,0,0,0,0,0,0,0,0,0,1032,1,51681,"NG","GT" 32,18,5,2,2,658,1,"PERU UTILITIES","PERU",0,"LIGHT OIL",14839,"0M",1294,,,95,2,7,60,0,0,40,0,0,29,0,0,45,0,0,42,0,0,89,0,0,89,28,62,123,2,6,104,0,0,104,0,0,64,0,0,58,1037,1,52298,"FO2","ST" 32,18,5,2,6,658,1,"PERU UTILITIES","PERU",0,"BIT COAL",14839,"0M",1294,,,95,597,409,462,0,0,462,0,0,462,0,0,462,0,0,462,0,0,664,0,0,664,4138,2475,1193,1602,1122,71,0,0,71,0,0,71,0,0,71,1037,1,52298,"BIT","ST" 32,18,5,3,2,666,1,"RENSSELAER (CITY OF)","RENSSELAER",0,"LIGHT OIL",15860,"0A",1294,,,95,0,5,507,0,4,492,0,0,385,0,0,376,42,89,635,0,0,624,11,22,610,10,24,577,13,25,557,13,33,523,18,34,485,12,25,448,1038,1,52461,"FO2","IC" 32,18,5,3,9,666,1,"RENSSELAER (CITY OF)","RENSSELAER",0,"NAT GAS",15860,"0A",1294,,,95,12,2242,0,5,609,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1038,1,52461,"NG","IC" 32,18,5,2,2,669,10,"RICHMOND (CITY OF)","WHITEWATER",0,"LIGHT OIL",15989,"0M",1294,,,95,66,135,651,4,9,642,11,23,618,36,75,544,43,89,455,36,75,380,33,65,315,24,51,800,38,79,721,40,84,637,125,241,754,33,67,866,1040,1,52479,"FO2","ST" 32,18,5,2,6,669,10,"RICHMOND (CITY OF)","WHITEWATER",0,"BIT COAL",15989,"0M",1294,,,95,52567,26931,66546,54464,27521,59857,50869,26046,61570,37981,19323,61813,34761,18221,70185,50812,25880,63189,54367,27836,58351,55464,28592,56536,47367,24058,57432,31433,16236,61431,49216,24827,57518,55122,27935,65411,1040,1,52479,"BIT","ST" 32,18,8,2,2,849,5,"HOOSIER ENERGY RURAL","RATTS",0,"LIGHT OIL",9267,"0M",1294,,,95,36,63,331,24,42,427,57,99,328,82,143,185,157,271,264,220,383,175,69,123,225,64,116,273,67,119,314,72,130,300,169,298,360,213,374,345,1043,1,51339,"FO2","ST" 32,18,8,2,6,849,5,"HOOSIER ENERGY RURAL","RATTS",0,"BIT COAL",9267,"0M",1294,,,95,152672,68804,12521,138850,61631,20613,120820,54271,33350,149240,67046,34059,138601,62960,37387,104185,47642,37604,152193,70371,29049,149047,69157,33970,133611,61143,30823,84154,38731,32856,131727,59094,30160,146986,66592,32432,1043,1,51339,"BIT","ST" 32,18,8,2,2,849,10,"HOOSIER ENERGY RURAL","MEROM",0,"LIGHT OIL",9267,"0M",1294,,,95,195,354,6014,19,38,10415,677,1227,9188,41,76,9112,1799,3447,5664,1764,3378,7059,771,1387,5672,508,946,4725,1207,2219,7281,584,1062,6218,468,838,10208,592,1063,9145,6213,1,51339,"FO2","ST" 32,18,8,2,6,849,10,"HOOSIER ENERGY RURAL","MEROM",0,"BIT COAL",9267,"0M",1294,,,95,462676,222254,448322,417644,215416,460946,384780,184640,471566,246060,116767,519358,230592,116155,570294,429927,213604,544280,462605,221660,492415,499492,244053,429843,353022,171326,433018,376476,178855,429945,480027,227666,396833,503880,236844,364841,6213,1,51339,"BIT","ST" 32,18,9,4,2,900,5,"INDIANA MUN POWER AGENCY","ANDERSON",0,"LIGHT OIL",9234,"0M",1294,,,95,19,44,5010,33,68,4942,40,82,4860,14,24,4835,7,12,4824,25,62,4762,0,1,4761,1,4,4757,0,0,4757,14,27,4730,3,9,4721,10,13,4708,7336,1,19234,"FO2","GT" 32,18,9,4,9,900,5,"INDIANA MUN POWER AGENCY","ANDERSON",0,"NAT GAS",9234,"0M",1294,,,95,53,772,0,54,717,0,199,2578,0,66,914,0,31,416,0,481,7593,0,2482,36348,0,6354,89340,0,94,1557,0,64,1343,0,36,450,0,47,750,0,7336,1,19234,"NG","GT" 33,17,1,2,2,29,5,"CENTRAL ILLINOIS LIGHT CO","E D EDWARDS",0,"LIGHT OIL",3252,"0M",1294,,,95,580,979,551,369,645,642,581,1050,511,539,979,621,777,1362,571,696,1201,688,793,1392,574,425,792,507,571,980,634,610,991,501,329,558,506,455,759,491,856,4,50485,"FO2","ST" 33,17,1,2,6,29,5,"CENTRAL ILLINOIS LIGHT CO","E D EDWARDS",0,"BIT COAL",3252,"0M",1294,,,95,278723,111505,170727,240983,94522,156151,283715,115017,142278,219332,90164,180893,314512,130292,145461,303524,124741,120263,294912,127410,143742,416665,181855,115286,215994,93604,136103,343831,139588,97044,284797,118784,138306,257830,101322,144327,856,4,50485,"BIT","ST" 33,17,1,4,9,29,12,"CENTRAL ILLINOIS LIGHT CO","STERLING AV",0,"NAT GAS",3252,"0M",1294,,,95,91,1361,0,30,486,0,29,443,0,29,495,0,28,483,0,114,1973,0,236,4614,0,495,8477,0,62,1057,0,60,926,0,32,555,0,79,1259,0,860,4,50485,"NG","GT" 33,17,1,2,2,29,20,"CENTRAL ILLINOIS LIGHT CO","DUCK CREEK",0,"LIGHT OIL",3252,"0M",1294,,,95,464,794,607,155,264,573,38,67,506,39,69,437,368,658,640,47,83,557,76,135,598,252,429,597,203,353,523,461,865,374,191,334,581,221,383,548,6016,4,50485,"FO2","ST" 33,17,1,2,6,29,20,"CENTRAL ILLINOIS LIGHT CO","DUCK CREEK",0,"BIT COAL",3252,"0M",1294,,,95,186107,88236,146013,184996,85972,174445,212342,99989,207941,178133,85191,199728,101736,49494,191824,209741,99840,163763,218825,104416,121412,182815,87426,161492,205874,98086,126656,49432,25199,182072,221479,104789,147984,208001,98018,120664,6016,4,50485,"BIT","ST" 33,17,1,2,9,29,25,"CENTRAL ILLINOIS LIGHT CO","MIDWEST GRN",0,"NAT GAS",3252,"0M",694,"A",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1987,12379,0,4809,36302,0,4873,33446,0,2693,19047,0,0,0,0,3046,22292,0,4051,25863,0,7384,4,50485,"NG","ST" 33,17,1,2,2,32,2,"CENTRAL ILL PUBLIC SER CO","COFFEEN",0,"LIGHT OIL",3253,"0M",1294,,,95,281,528,4129,159,291,4010,394,749,4105,523,1002,3949,771,1637,3876,506,903,4329,271,491,4241,39,71,3944,249,436,4034,521,930,3986,417,729,4572,962,1745,3927,861,4,50486,"FO2","ST" 33,17,1,2,6,32,2,"CENTRAL ILL PUBLIC SER CO","COFFEEN",0,"BIT COAL",3253,"0M",1294,,,95,365821,196265,250663,291393,151752,268915,248792,134522,254062,79012,43562,287270,49602,29698,377234,331239,171527,392358,397070,207104,345747,370867,195382,346249,139189,69530,387149,251535,126615,387760,291764,143554,406398,266300,137380,362886,861,4,50486,"BIT","ST" 33,17,1,2,2,32,5,"CENTRAL ILL PUBLIC SER CO","GRAND TOWER",0,"LIGHT OIL",3253,"0M",1294,,,95,146,294,559,222,423,494,139,267,578,60,171,742,-59,75,667,310,600,753,324,626,481,405,753,769,154,287,834,78,162,672,389,761,607,217,428,533,862,4,50486,"FO2","ST" 33,17,1,2,6,32,5,"CENTRAL ILL PUBLIC SER CO","GRAND TOWER",0,"BIT COAL",3253,"0M",1294,,,95,19817,10029,48685,18173,8634,59296,12650,6089,70908,3933,2772,73473,-503,161,78207,17238,8399,74696,44644,21400,58784,77238,35607,26412,11609,5363,31994,11150,5893,34133,57466,27803,19044,47800,23991,32368,862,4,50486,"BIT","ST" 33,17,1,2,2,32,10,"CENTRAL ILL PUBLIC SER CO","HUTSONVILLE",0,"LIGHT OIL",3253,"0M",1294,,,95,72,148,1592,254,501,1092,252,532,1126,117,284,1556,421,883,1560,398,781,1662,440,832,1760,236,429,1331,196,323,1008,158,382,1338,346,655,1437,140,264,1173,863,4,50486,"FO2","ST" 33,17,1,2,6,32,10,"CENTRAL ILL PUBLIC SER CO","HUTSONVILLE",0,"BIT COAL",3253,"0M",1294,,,95,17493,9580,55605,13103,6803,61393,11330,6319,65444,3457,2220,70186,6929,4012,73260,18641,9997,71065,43752,22295,48771,75386,37255,19363,5801,2524,33120,7107,4480,39773,44924,22754,26665,48938,24435,23714,863,4,50486,"BIT","ST" 33,17,1,3,2,32,10,"CENTRAL ILL PUBLIC SER CO","HUTSONVILLE",0,"LIGHT OIL",3253,"0M",1294,,,95,5,10,124,0,0,126,0,0,130,5,9,121,5,9,106,0,0,106,15,30,72,10,21,233,0,0,229,0,0,228,5,9,225,0,0,227,863,4,50486,"FO2","IC" 33,17,1,2,2,32,15,"CENTRAL ILL PUBLIC SER CO","MEREDOSIA",0,"LIGHT OIL",3253,"0M",1294,,,95,276,524,1245,240,455,1295,109,257,1541,576,1050,1518,264,464,1396,272,471,1722,478,864,1170,665,1188,1390,137,250,1672,104,202,1469,-609,0,1671,636,1140,1388,864,4,50486,"FO2","ST" 33,17,1,2,3,32,15,"CENTRAL ILL PUBLIC SER CO","MEREDOSIA",0,"HEAVY OIL",3253,"0M",1294,,,95,-878,0,41246,-869,0,41246,-953,0,41246,-789,0,41246,-6,0,41246,1105,5986,35342,1753,6017,29342,6547,17169,22153,-808,333,23977,-646,0,42084,996,1890,42084,-711,0,42084,864,4,50486,"FO6","ST" 33,17,1,2,6,32,15,"CENTRAL ILL PUBLIC SER CO","MEREDOSIA",0,"BIT COAL",3253,"0M",1294,,,95,66774,32586,105182,41839,21008,131939,15303,9402,148998,70146,32222,148546,91295,40883,144840,111244,50699,134953,137571,64325,109649,184516,85228,55561,77698,37291,62196,86881,43240,73623,78143,41045,82454,97009,48373,93368,864,4,50486,"BIT","ST" 33,17,1,2,2,32,20,"CENTRAL ILL PUBLIC SER CO","NEWTON",0,"LIGHT OIL",3253,"0M",1294,,,95,844,1577,4500,512,956,5160,1182,2043,4716,553,984,5869,379,679,5723,681,1231,5199,190,328,5578,942,1748,4784,746,1331,5217,282,508,5420,60,105,5315,649,3661,4337,6017,4,50486,"FO2","ST" 33,17,1,2,6,32,20,"CENTRAL ILL PUBLIC SER CO","NEWTON",0,"BIT COAL",3253,"0M",1294,,,95,556271,262272,366063,518547,246265,373901,546762,245831,417351,503402,237591,446819,516641,244361,536330,468640,219703,623301,560024,252360,476964,466441,225593,612105,491641,228921,632582,454181,204761,666122,359030,160358,746315,378431,180592,722338,6017,4,50486,"BIT","ST" 33,17,1,1,,41,1,"COMMONWEALTH EDISON CO","DIXON",0,,4110,"0M",1294,,100,95,1217,0,0,1001,0,0,1400,0,0,1473,0,0,1443,0,0,1109,0,0,1264,0,0,1341,0,0,1211,0,0,1365,0,0,1603,0,0,1067,0,0,868,4,50643,"WAT","HY" 33,17,1,2,1,41,1,"COMMONWEALTH EDISON CO","QUAD CITIES",0,"NUCLEAR",4110,"0M",1294,,100,95,265985,0,0,516483,0,0,563772,0,0,556271,0,0,570166,0,0,541658,0,0,537742,0,0,552522,0,0,533277,0,0,383182,0,0,293985,0,0,571167,0,0,880,4,50643,"UR","ST" 33,17,1,2,1,41,1,"COMMONWEALTH EDISON CO","BRAIDWOOD",0,"NUCLEAR",4110,"0M",1294,,100,95,845089,0,0,487988,0,0,443133,0,0,527594,0,0,838888,0,0,802928,0,0,825056,0,0,825520,0,0,701927,0,0,-9715,0,0,-10027,0,0,307159,0,0,6022,4,50643,"UR","ST" 33,17,1,2,1,41,1,"COMMONWEALTH EDISON CO","BYRON",0,"NUCLEAR",4110,"0M",1294,,100,95,766116,0,0,735235,0,0,817602,0,0,779568,0,0,804172,0,0,742334,0,0,790248,0,0,800198,0,0,786058,0,0,542611,0,0,-9310,0,0,142399,0,0,6023,4,50643,"UR","ST" 33,17,1,2,1,41,1,"COMMONWEALTH EDISON CO","LASALLE CTY",0,"NUCLEAR",4110,"0M",1294,,100,95,813809,0,0,531418,0,0,813835,0,0,788528,0,0,782478,0,0,561931,0,0,750639,0,0,609485,0,0,617973,0,0,773354,0,0,684375,0,0,641459,0,0,6026,4,50643,"UR","ST" 33,17,1,2,1,41,1,"COMMONWEALTH EDISON CO","ZION",0,"NUCLEAR",4110,"0M",1294,,100,95,777628,0,0,706122,0,0,778794,0,0,744367,0,0,679639,0,0,751346,0,0,778214,0,0,771971,0,0,190946,0,0,-8633,0,0,-8349,0,0,290089,0,0,885,4,50643,"UR","ST" 33,17,1,2,1,41,2,"COMMONWEALTH EDISON CO","ZION",0,"NUCLEAR",4110,"0M",1294,,100,95,62829,0,0,-7517,0,0,-8823,0,0,214602,0,0,763695,0,0,707962,0,0,768388,0,0,745403,0,0,742149,0,0,737928,0,0,708434,0,0,471011,0,0,885,4,50643,"UR","ST" 33,17,1,2,1,41,2,"COMMONWEALTH EDISON CO","LASALLE CTY",0,"NUCLEAR",4110,"0M",1294,,100,95,805795,0,0,433271,0,0,-8184,0,0,-8016,0,0,-8927,0,0,375943,0,0,773928,0,0,744199,0,0,446327,0,0,816638,0,0,792434,0,0,804502,0,0,6026,4,50643,"UR","ST" 33,17,1,2,1,41,2,"COMMONWEALTH EDISON CO","BYRON",0,"NUCLEAR",4110,"0M",1294,,100,95,753651,0,0,166639,0,0,50362,0,0,767250,0,0,824285,0,0,786866,0,0,797334,0,0,811901,0,0,764206,0,0,832898,0,0,804540,0,0,823838,0,0,6023,4,50643,"UR","ST" 33,17,1,2,1,41,2,"COMMONWEALTH EDISON CO","BRAIDWOOD",0,"NUCLEAR",4110,"0M",1294,,100,95,839335,0,0,759006,0,0,840028,0,0,777131,0,0,635751,0,0,794146,0,0,802182,0,0,795885,0,0,801537,0,0,846700,0,0,810185,0,0,831152,0,0,6022,4,50643,"UR","ST" 33,17,1,2,1,41,2,"COMMONWEALTH EDISON CO","QUAD CITIES",0,"NUCLEAR",4110,"0M",1294,,100,95,501116,0,0,453211,0,0,58157,0,0,-5752,0,0,-5952,0,0,-5994,0,0,-6618,0,0,93771,0,0,422180,0,0,318808,0,0,77988,0,0,571746,0,0,880,4,50643,"UR","ST" 33,17,1,2,1,41,2,"COMMONWEALTH EDISON CO","DRESDEN",0,"NUCLEAR",4110,"0M",1294,,100,95,535595,0,0,493244,0,0,81638,0,0,302574,0,0,449851,0,0,27639,0,0,-3615,0,0,-4287,0,0,-5566,0,0,-5704,0,0,-5672,0,0,-5963,0,0,869,4,50643,"UR","ST" 33,17,1,2,1,41,3,"COMMONWEALTH EDISON CO","DRESDEN",0,"NUCLEAR",4110,"0M",1294,,100,95,420814,0,0,506779,0,0,533907,0,0,467390,0,0,432429,0,0,-5060,0,0,-3401,0,0,-3807,0,0,41448,0,0,138092,0,0,358426,0,0,577978,0,0,869,4,50643,"UR","ST" 33,17,1,4,2,41,4,"COMMONWEALTH EDISON CO","BLOOM",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,15589,0,0,15589,69,87,15502,0,0,15495,0,0,15495,0,0,15475,146,497,14951,792,2784,12167,0,0,15755,0,0,15755,0,0,15755,1,3,15739,865,4,50643,"FO2","GT" 33,17,1,4,2,41,6,"COMMONWEALTH EDISON CO","CALUMET",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,16437,0,0,16437,0,0,16437,145,127,16310,0,0,16310,0,0,16310,593,2028,14281,508,1365,12917,0,0,15298,0,0,15298,0,0,15298,0,0,15298,866,4,50643,"FO2","GT" 33,17,1,4,9,41,6,"COMMONWEALTH EDISON CO","CALUMET",0,"NAT GAS",4110,"0M",1294,,100,95,0,0,0,68,1045,0,0,8,0,0,0,0,62,540,0,0,0,0,2902,56071,0,3743,56299,0,1,46,0,106,1474,0,29,760,0,0,0,0,866,4,50643,"NG","GT" 33,17,1,2,6,41,10,"COMMONWEALTH EDISON CO","CRAWFORD",0,"BIT COAL",4110,"0M",1294,,100,95,79127,52566,254284,56492,34236,247898,154770,96060,204338,157819,95401,178999,77964,50034,154295,195593,125311,78949,167051,106642,75986,220876,140947,52693,111791,74002,178401,100936,63677,173394,171688,108863,144620,107184,68961,169485,867,4,50643,"BIT","ST" 33,17,1,2,9,41,10,"COMMONWEALTH EDISON CO","CRAWFORD",0,"NAT GAS",4110,"0M",1294,,100,95,4191,46278,0,3822,41541,0,6151,66002,0,6881,74296,0,3205,34575,0,3676,39819,0,4307,47007,0,11765,128609,0,2943,33297,0,3202,34374,0,2534,27690,0,3684,42386,0,867,4,50643,"NG","ST" 33,17,1,4,2,41,10,"COMMONWEALTH EDISON CO","CRAWFORD",0,"LIGHT OIL",4110,"0M",1294,,100,95,39,239,11718,31,208,15427,7,85,15342,60,196,15146,0,0,15146,145,654,14492,207,1709,12783,90,287,12496,0,0,12495,0,0,12495,5,41,12453,0,0,12451,867,4,50643,"FO2","GT" 33,17,1,4,9,41,10,"COMMONWEALTH EDISON CO","CRAWFORD",0,"NAT GAS",4110,"0M",1294,,100,95,99,3367,0,462,10721,0,90,6128,0,496,8920,0,41,832,0,2338,60078,0,1956,92769,0,6353,117178,0,232,23469,0,130,22477,0,606,26280,0,716,38106,0,867,4,50643,"NG","GT" 33,17,1,2,2,41,16,"COMMONWEALTH EDISON CO","JOLIET",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,874,4,50643,"FO2","ST" 33,17,1,2,6,41,16,"COMMONWEALTH EDISON CO","JOLIET",0,"BIT COAL",4110,"0M",1294,,100,95,122495,69041,120326,93234,54624,109729,118689,69742,107396,119799,68307,78398,7077,4459,86216,111744,65001,89393,128830,75618,81101,97034,56642,114450,105402,58755,119892,105052,56846,73967,38927,23143,87158,80786,46625,136310,874,4,50643,"BIT","ST" 33,17,1,2,9,41,16,"COMMONWEALTH EDISON CO","JOLIET",0,"NAT GAS",4110,"0M",1294,,100,95,2191,22095,0,1467,15220,0,2310,24340,0,2244,23500,0,166,1970,0,2208,24000,0,2239,22730,0,1106,11930,0,1732,18230,0,1439,14430,0,1402,15430,0,1598,17620,0,874,4,50643,"NG","ST" 33,17,1,3,2,41,16,"COMMONWEALTH EDISON CO","JOLIET",0,"LIGHT OIL",4110,"0M",1294,,100,95,28,24,0,19,36,0,26,24,0,38,121,0,42,65,0,45,88,0,191,342,0,177,323,0,43,60,8,25,36,0,50,114,0,33,48,0,874,4,50643,"FO2","IC" 33,17,1,4,2,41,16,"COMMONWEALTH EDISON CO","JOLIET",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,12982,0,0,12946,0,0,13461,0,0,13339,0,0,11260,0,0,11071,56,101,11058,0,0,11182,0,0,11123,0,0,11087,0,0,11349,0,0,11301,874,4,50643,"FO2","GT" 33,17,1,4,9,41,16,"COMMONWEALTH EDISON CO","JOLIET",0,"NAT GAS",4110,"0M",1294,,100,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1395,27871,0,8945,90787,0,8183,223338,0,866,13196,0,229,3746,0,131,5138,0,234,3377,0,874,4,50643,"NG","GT" 33,17,1,2,2,41,17,"COMMONWEALTH EDISON CO","JOLIET 7&8",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,384,4,50643,"FO2","ST" 33,17,1,2,6,41,17,"COMMONWEALTH EDISON CO","JOLIET 7&8",0,"BIT COAL",4110,"0M",1294,,100,95,520241,284540,251012,441016,243169,314690,475210,271066,278538,286729,169187,274394,417122,253105,368822,380291,234398,349806,434794,265270,338716,502962,304953,251022,375036,226403,245187,274949,166801,229512,204177,119561,295972,195022,118007,392005,384,4,50643,"BIT","ST" 33,17,1,2,9,41,17,"COMMONWEALTH EDISON CO","JOLIET 7&8",0,"NAT GAS",4110,"0M",1294,,100,95,11103,108953,0,8750,87209,0,12754,127880,0,12398,126498,0,15389,159604,0,14468,153070,0,34003,358096,0,38820,399592,0,12449,130392,0,5845,61103,0,9664,99401,0,15109,163833,0,384,4,50643,"NG","ST" 33,17,1,2,2,41,18,"COMMONWEALTH EDISON CO","KINCAID",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,876,4,50643,"FO2","ST" 33,17,1,2,6,41,18,"COMMONWEALTH EDISON CO","KINCAID",0,"BIT COAL",4110,"0M",1294,,100,95,55770,32758,306574,225554,110119,355485,177700,87847,323621,111716,54633,362527,59730,40786,398523,326434,167542,321546,302831,139901,261736,370353,171207,168914,152028,76179,217203,146493,75067,252142,105685,62572,325669,303394,153078,287687,876,4,50643,"BIT","ST" 33,17,1,2,9,41,18,"COMMONWEALTH EDISON CO","KINCAID",0,"NAT GAS",4110,"0M",1294,,100,95,1202,16174,0,747,8607,0,913,10721,0,996,11458,0,1078,14934,0,450,5024,0,586,6470,0,981,10590,0,742,8548,0,1541,18276,0,2200,30312,0,917,10402,0,876,4,50643,"NG","ST" 33,17,1,4,2,41,19,"COMMONWEALTH EDISON CO","LOMBARD",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,16204,0,0,16203,0,2,15828,0,0,15828,0,0,15471,0,0,15471,0,0,15471,0,0,15471,0,0,15471,0,0,15471,0,0,15471,0,0,15471,877,4,50643,"FO2","GT" 33,17,1,4,9,41,19,"COMMONWEALTH EDISON CO","LOMBARD",0,"NAT GAS",4110,"0M",1294,,100,95,0,0,0,0,0,0,216,9440,0,28,3677,0,45,1042,0,1545,52076,0,2695,90228,0,4011,66015,0,277,4570,0,110,2620,0,70,1556,0,6,1352,0,877,4,50643,"NG","GT" 33,17,1,4,2,41,22,"COMMONWEALTH EDISON CO","EL JUNCTION",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,16029,0,0,16029,0,0,16029,0,0,16029,0,0,16029,0,0,16029,0,0,16029,0,0,16029,0,0,16029,0,0,16029,0,0,16029,0,0,16029,870,4,50643,"FO2","GT" 33,17,1,4,9,41,22,"COMMONWEALTH EDISON CO","EL JUNCTION",0,"NAT GAS",4110,"0M",1294,,100,95,45,1465,0,255,9385,0,433,17490,0,266,17646,0,201,1306,0,3974,165292,0,3141,117346,0,6577,120875,0,317,6236,0,0,0,0,0,0,0,0,0,0,870,4,50643,"NG","GT" 33,17,1,2,2,41,25,"COMMONWEALTH EDISON CO","POWERTON",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,879,4,50643,"FO2","ST" 33,17,1,2,6,41,25,"COMMONWEALTH EDISON CO","POWERTON",0,"BIT COAL",4110,"0M",1294,,100,95,295687,209649,423935,447158,294017,440451,348046,239570,435308,212232,137447,636432,150582,105273,808681,358461,251527,710182,600064,381559,542202,449473,321219,483261,473891,314575,379942,711307,426764,426047,347462,223314,654319,369211,237119,790527,879,4,50643,"BIT","ST" 33,17,1,2,9,41,25,"COMMONWEALTH EDISON CO","POWERTON",0,"NAT GAS",4110,"0M",1294,,100,95,2163,27135,0,934,10806,0,1060,12568,0,352,4015,0,411,4960,0,1912,23178,0,1304,14277,0,344,4172,0,2982,34612,0,1175,12623,0,1089,12285,0,860,10186,0,879,4,50643,"NG","ST" 33,17,1,4,2,41,34,"COMMONWEALTH EDISON CO","SABROOKE",0,"LIGHT OIL",4110,"0M",1294,,100,95,0,0,10453,0,0,10453,0,0,10453,0,0,10453,0,0,10453,1060,4114,11113,2120,6610,10937,3819,12030,8749,0,0,10491,0,0,10491,92,332,10159,19,57,10102,882,4,50643,"FO2","GT" 33,17,1,2,6,41,35,"COMMONWEALTH EDISON CO","FISK ST",0,"BIT COAL",4110,"0M",1294,,100,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,1258,2813,0,64730,37523,0,49452,31868,0,82828,51049,0,0,0,0,0,0,0,886,4,50643,"BIT","ST" 33,17,1,2,9,41,35,"COMMONWEALTH EDISON CO","FISK ST",0,"NAT GAS",4110,"0M",1294,,100,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,950,35700,0,6315,65190,0,4278,50522,0,3262,35967,0,0,0,0,0,0,0,886,4,50643,"NG","ST" 33,17,1,3,2,41,35,"COMMONWEALTH EDISON CO","FISK ST",0,"LIGHT OIL",4110,"0M",1294,,100,95,45,155,416,0,0,416,77,84,332,39,37,295,68,30,266,66,86,180,134,219,491,125,84,407,40,16,391,17,100,291,19,95,196,0,0,174,886,4,50643,"FO2","IC" 33,17,1,4,2,41,35,"COMMONWEALTH EDISON CO","FISK ST",0,"LIGHT OIL",4110,"0M",1294,,100,95,1,5,23532,47,93,23145,99,257,23261,297,889,22373,31,91,22630,3411,9368,21922,4887,12963,23223,4869,20375,20364,0,0,20364,0,0,20364,335,1236,19127,365,1339,17788,886,4,50643,"FO2","GT" 33,17,1,2,2,41,40,"COMMONWEALTH EDISON CO","WAUKEGAN",0,"LIGHT OIL",4110,"0M",1294,,100,95,895,1547,2815,3612,6129,2742,4931,8714,2873,777,1407,3668,959,1672,3660,3946,7104,2494,3955,7041,2217,5282,9737,2829,3119,5998,3784,2859,5228,2552,3518,6749,3529,1606,3513,2435,883,4,50643,"FO2","ST" 33,17,1,2,6,41,40,"COMMONWEALTH EDISON CO","WAUKEGAN",0,"BIT COAL",4110,"0M",1294,,100,95,297287,177180,273721,300831,175220,239888,317665,191650,286982,225455,141450,324935,256271,154756,392524,243529,150801,389581,310909,188184,335255,296518,187813,197729,119579,79260,209183,165704,104633,209690,128110,85584,284788,41660,30532,414595,883,4,50643,"BIT","ST" 33,17,1,2,9,41,40,"COMMONWEALTH EDISON CO","WAUKEGAN",0,"NAT GAS",4110,"0M",1294,,100,95,1435,14340,0,1745,16984,0,6345,64552,0,12306,127984,0,2631,26534,0,2700,27935,0,4475,45751,0,8173,86616,0,1604,17712,0,0,0,0,0,0,0,1606,20058,0,883,4,50643,"NG","ST" 33,17,1,4,2,41,40,"COMMONWEALTH EDISON CO","WAUKEGAN",0,"LIGHT OIL",4110,"0M",1294,,100,95,311,627,9084,81,252,8832,0,0,8832,62,220,8612,0,0,8612,2971,8993,7575,4093,8993,10099,3465,12846,8690,217,650,9693,15,46,9832,388,721,9111,455,101,8825,883,4,50643,"FO2","GT" 33,17,1,2,2,41,45,"COMMONWEALTH EDISON CO","WILL COUNTY",0,"LIGHT OIL",4110,"0M",1294,,100,95,1062,18762,3939,7295,13109,3758,10624,18496,3941,8221,14895,3199,9084,16531,4090,8920,16134,4050,10413,17507,4073,8717,15307,3888,6246,11354,3823,8028,14057,4581,13300,23039,4265,11454,20638,3742,884,4,50643,"FO2","ST" 33,17,1,2,6,41,45,"COMMONWEALTH EDISON CO","WILL COUNTY",0,"BIT COAL",4110,"0M",1294,,100,95,339333,214481,728644,276729,163281,493423,436182,242324,418178,363653,209416,394195,307990,182353,450891,397251,238256,419768,378522,212664,447725,475303,276214,354866,276771,166573,326404,319122,188012,314278,367545,210217,297641,236545,145482,315427,884,4,50643,"BIT","ST" 33,17,1,2,2,41,60,"COMMONWEALTH EDISON CO","COLLINS",0,"LIGHT OIL",4110,"0M",1294,,100,95,44,168,8953,149,398,8555,143,315,8240,46,189,8051,8,33,9226,37,94,9132,118,236,8896,161,333,8562,33,186,8376,121,346,8030,407,870,7160,418,907,6253,6025,4,50643,"FO2","ST" 33,17,1,2,3,41,60,"COMMONWEALTH EDISON CO","COLLINS",0,"HEAVY OIL",4110,"0M",1294,,100,95,10708,14958,858168,17136,41575,816594,22453,44431,829903,5094,19291,887973,1621,6324,924611,37801,79457,874073,46886,87834,814064,170809,316836,497228,8876,46988,565732,30191,78409,602644,60143,118667,704727,63549,126751,840744,6025,4,50643,"FO6","ST" 33,17,1,2,9,41,60,"COMMONWEALTH EDISON CO","COLLINS",0,"NAT GAS",4110,"0M",1294,,100,95,39831,890044,0,143526,2177150,0,287955,3565711,0,53575,1269470,0,42336,1034381,0,242662,3192054,0,342245,4012183,0,559661,6496563,0,22424,742913,0,72437,1176239,0,234867,2894481,0,189527,2361026,0,6025,4,50643,"NG","ST" 33,17,1,2,2,59,5,"ELECTRIC ENERGY INC","JOPPA STEAM",0,"LIGHT OIL",5748,"0M",1294,,,95,200,374,1123,39,70,1273,99,185,1072,621,1113,2510,355,632,917,223,421,1063,108,203,1046,324,609,1093,203,369,937,141,253,1041,23,42,874,163,297,1013,887,4,50877,"FO2","ST" 33,17,1,2,6,59,5,"ELECTRIC ENERGY INC","JOPPA STEAM",0,"BIT COAL",5748,"0M",1294,,,95,714619,413405,218343,620332,359921,257338,581511,352021,367649,615267,357331,494389,555217,326921,554836,664604,410139,566371,692201,431949,348896,616065,383985,389108,610216,368490,418929,705090,420489,495502,724030,433000,497231,719491,431637,526478,887,4,50877,"BIT","ST" 33,17,1,2,9,59,5,"ELECTRIC ENERGY INC","JOPPA STEAM",0,"NAT GAS",5748,"0M",1294,,,95,3,39,0,3,32,0,2,31,0,4,42,0,2,29,0,3,39,0,2,28,0,2,25,0,2,30,0,3,33,0,4,43,0,2,27,0,887,4,50877,"NG","ST" 33,17,1,2,1,72,1,"ILLINOIS POWER CO","CLINTON",0,"NUCLEAR",9208,"0M",1294,,,95,606581,0,0,556463,0,0,137066,0,0,-6903,0,0,405888,0,0,658164,0,0,673318,0,0,670862,0,0,558375,0,0,682367,0,0,659454,0,0,500645,0,0,204,4,51385,"UR","ST" 33,17,1,2,"C",72,20,"ILLINOIS POWER CO","BALDWIN",0,"TIRES",9208,"0M",294,"A",,95,0,0,0,1818,0,0,3181,0,0,7099,0,0,6807,0,0,5350,0,0,7244,0,0,3493,0,0,6277,0,0,7534,0,0,10681,0,0,7569,0,0,889,4,51385,"TIR","ST" 33,17,1,2,2,72,20,"ILLINOIS POWER CO","BALDWIN",0,"LIGHT OIL",9208,"0M",1294,,,95,1081,1918,2086,605,1061,2802,687,1177,4303,886,1546,2758,788,1102,2909,1035,1849,3333,1018,1819,2723,194,347,3603,519,926,3761,917,1661,2395,449,802,2830,719,1288,2830,889,4,51385,"FO2","ST" 33,17,1,2,6,72,20,"ILLINOIS POWER CO","BALDWIN",0,"BIT COAL",9208,"0M",1294,,,95,660540,312984,326606,560194,261218,347154,721218,332734,317839,1001149,461485,170294,940043,347817,194365,784737,373003,199111,952571,453263,98640,1114689,528001,10906,767993,364295,81430,684089,329233,150289,880194,419001,132828,809209,388865,132828,889,4,51385,"BIT","ST" 33,17,1,2,2,72,35,"ILLINOIS POWER CO","HAVANA",0,"LIGHT OIL",9208,"0M",1294,,,95,910,1948,1153,666,1365,840,307,580,1330,461,889,1682,716,1472,1237,733,1517,1451,606,1199,1513,905,1843,2122,693,1487,1847,988,1998,879,1035,1991,1192,678,1527,1192,891,4,51385,"FO2","ST" 33,17,1,2,3,72,35,"ILLINOIS POWER CO","HAVANA",0,"HEAVY OIL",9208,"0M",1294,,,95,0,0,11893,0,0,11893,0,0,11893,0,0,11893,0,0,11893,0,0,11893,0,0,11893,0,0,11893,0,0,11893,0,0,11893,0,0,362,0,0,362,891,4,51385,"FO6","ST" 33,17,1,2,6,72,35,"ILLINOIS POWER CO","HAVANA",0,"BIT COAL",9208,"0M",1294,,,95,98112,49256,30789,118979,58411,50159,224224,102634,40379,160060,74936,66818,118264,58880,70245,116146,58574,89918,115561,56674,118529,151230,75783,90549,71688,37378,112421,88892,44663,121996,115087,53793,99387,131730,71564,99387,891,4,51385,"BIT","ST" 33,17,1,2,9,72,35,"ILLINOIS POWER CO","HAVANA",0,"NAT GAS",9208,"0M",1294,,,95,1067,12979,0,440,5089,0,63,677,0,179,1951,0,351,4046,0,300,3543,0,463,5170,0,355,4086,0,402,4873,0,559,6392,0,891,9670,0,763,9698,0,891,4,51385,"NG","ST" 33,17,1,2,2,72,37,"ILLINOIS POWER CO","HENNEPIN",0,"LIGHT OIL",9208,"0M",1294,,,95,0,0,139,0,0,118,0,0,98,0,0,73,0,0,226,0,0,198,0,0,171,0,0,143,0,0,124,0,0,81,0,0,206,0,0,206,892,4,51385,"FO2","ST" 33,17,1,2,6,72,37,"ILLINOIS POWER CO","HENNEPIN",0,"BIT COAL",9208,"0M",1294,,,95,87360,41868,110995,113939,53993,91245,148496,70812,66931,128982,61958,52605,126965,61905,34055,114742,56218,13963,122662,60852,24745,143091,72106,29954,79631,39909,56695,59580,30905,81408,39508,20500,71977,116352,56957,71977,892,4,51385,"BIT","ST" 33,17,1,2,9,72,37,"ILLINOIS POWER CO","HENNEPIN",0,"NAT GAS",9208,"0M",1294,,,95,32318,326516,0,1234,12249,0,1222,12243,0,808,8187,0,416,4252,0,2050,20916,0,733,7579,0,551,5765,0,776,8044,0,87,951,0,169,1816,0,493,5034,0,892,4,51385,"NG","ST" 33,17,1,4,2,72,39,"ILLINOIS POWER CO","OGLESBY",0,"LIGHT OIL",9208,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,8629,0,0,8629,0,0,8629,0,0,8629,0,0,8629,0,0,8629,0,0,8629,0,0,8805,0,0,8805,894,4,51385,"FO2","GT" 33,17,1,4,9,72,39,"ILLINOIS POWER CO","OGLESBY",0,"NAT GAS",9208,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,2951,33996,0,2725,56764,0,0,0,0,110,1650,0,0,0,0,519,7497,0,894,4,51385,"NG","GT" 33,17,1,4,2,72,40,"ILLINOIS POWER CO","STALLINGS",0,"LIGHT OIL",9208,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,895,4,51385,"FO2","GT" 33,17,1,4,9,72,40,"ILLINOIS POWER CO","STALLINGS",0,"NAT GAS",9208,"0M",1294,,,95,-5,0,0,0,0,0,-188,0,0,-57,0,0,-40,0,0,-31,0,0,556,11621,0,1460,27572,0,-38,0,0,-159,0,0,0,0,0,40,1636,0,895,4,51385,"NG","GT" 33,17,1,2,2,72,45,"ILLINOIS POWER CO","VERMILION",0,"LIGHT OIL",9208,"0M",1294,,,95,115,249,624,91,198,602,191,417,364,236,549,361,18,38,279,0,0,257,0,0,333,0,0,327,0,0,327,0,0,284,0,0,284,0,0,284,897,4,51385,"FO2","ST" 33,17,1,2,6,72,45,"ILLINOIS POWER CO","VERMILION",0,"BIT COAL",9208,"0M",1294,,,95,30154,17048,27000,17324,9743,30113,23022,12947,17166,26005,15643,2483,5797,3221,2966,977,640,2326,0,0,2326,0,0,2326,0,0,2326,0,0,2326,-194,0,2326,0,0,2326,897,4,51385,"BIT","ST" 33,17,1,2,9,72,45,"ILLINOIS POWER CO","VERMILION",0,"NAT GAS",9208,"0M",794,"A",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,35157,523154,0,35815,280703,0,5530,63136,0,-181,425,0,0,0,0,0,0,0,897,4,51385,"NG","ST" 33,17,1,4,2,72,45,"ILLINOIS POWER CO","VERMILION",0,"LIGHT OIL",9208,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,-967,0,0,13,1679,0,0,0,0,0,0,0,897,4,51385,"FO2","GT" 33,17,1,2,"B",72,50,"ILLINOIS POWER CO","WOOD RIVER",0,"WOOD",9208,"0M",294,"A",,95,0,0,0,16,0,0,178,0,0,229,0,0,90,0,0,216,0,0,58,0,0,48,0,0,0,0,0,0,0,0,0,0,0,18,0,0,898,4,51385,"WD","ST" 33,17,1,2,2,72,50,"ILLINOIS POWER CO","WOOD RIVER",0,"LIGHT OIL",9208,"0M",1294,,,95,44,79,5600,23,43,5507,47,83,5347,40,74,5395,21,44,5332,24,48,5204,12,23,5294,49,90,5144,25,46,5028,38,67,5235,0,0,4820,0,0,4820,898,4,51385,"FO2","ST" 33,17,1,2,6,72,50,"ILLINOIS POWER CO","WOOD RIVER",0,"BIT COAL",9208,"0M",1294,,,95,179203,74998,45031,134748,57471,69498,189897,79401,76252,58215,25205,85871,13578,6765,84103,56995,25313,99570,176787,75799,113318,203949,86831,93346,141728,61520,85883,170165,70959,78358,166564,67877,95046,152328,67698,95046,898,4,51385,"BIT","ST" 33,17,1,2,9,72,50,"ILLINOIS POWER CO","WOOD RIVER",0,"NAT GAS",9208,"0M",1294,,,95,2917,29530,0,3161,32758,0,2112,21194,0,620,6474,0,455,5401,0,3940,43447,0,1042,11274,0,7813,79539,0,841,8463,0,2100,20806,0,1416,13732,0,3310,34114,0,898,4,51385,"NG","ST" 33,17,1,1,,76,5,"MIDAMERICAN ENERGY","MOLINE",0,,9438,"0M",1294,,50,95,867,0,0,502,0,0,693,0,0,501,0,0,751,0,0,1306,0,0,1909,0,0,1606,0,0,1628,0,0,1499,0,0,1295,0,0,824,0,0,899,5,51406,"WAT","HY" 33,17,1,4,2,76,5,"MIDAMERICAN ENERGY","MOLINE",0,"LIGHT OIL",9438,"0M",1294,,50,95,-104,1,1972,-89,0,1972,-80,0,1972,0,0,1972,0,0,1972,0,0,1972,0,0,1972,0,0,1972,-1,0,1972,-33,0,1972,-32,0,1972,-41,0,1972,899,5,51406,"FO2","GT" 33,17,1,4,9,76,5,"MIDAMERICAN ENERGY","MOLINE",0,"NAT GAS",9438,"0M",1294,,50,95,0,0,0,0,0,0,0,0,0,0,0,0,-61,2,0,1064,18944,0,1548,27660,0,1838,32171,0,-50,33,0,-34,0,0,-33,0,0,-42,0,0,899,5,51406,"NG","GT" 33,17,1,1,,107,1,"NATIONAL HYDRO","DAYTON",0,,9366,"0A",1294,,,95,1202,0,0,1122,0,0,1638,0,0,1567,0,0,992,0,0,1383,0,0,911,0,0,403,0,0,0,0,0,0,0,0,1259,0,0,1438,0,0,901,4,52081,"WAT","HY" 33,17,1,1,,134,1,"SO BELOIT WTR GAS & ELEC","ROCKTON",0,,17535,"0A",1294,,521,95,467,0,0,390,0,0,678,0,0,788,0,0,728,0,0,505,0,0,154,0,0,655,0,0,616,0,0,694,0,0,698,0,0,536,0,0,903,4,54026,"WAT","HY" 33,17,1,2,2,151,15,"UNION ELECTRIC CO","VENICE",0,"LIGHT OIL",19436,"0M",1294,,150,95,-14,55,40501,-148,624,39877,0,0,39877,0,0,39877,1716,6693,33184,1509,6175,27009,165,558,26451,1421,5295,29829,0,0,33009,0,0,33009,63,822,32186,-598,1970,30216,913,4,52997,"FO2","ST" 33,17,1,2,9,151,15,"UNION ELECTRIC CO","VENICE",0,"NAT GAS",19436,"0M",1294,,150,95,-1037,23078,0,-714,17082,0,745,29759,0,2615,70964,0,3881,85875,0,3694,85747,0,12175,233282,0,18970,400955,0,1254,9297,0,1125,26918,0,146,10894,0,-478,8990,0,913,4,52997,"NG","ST" 33,17,1,4,2,151,15,"UNION ELECTRIC CO","VENICE",0,"LIGHT OIL",19436,"0M",1294,,150,95,-67,27,1614,-28,163,2000,-35,94,1906,-28,27,1879,-20,89,1790,-20,0,1790,170,758,2114,425,1509,1672,-19,2,1670,-26,4,1666,-54,3,1664,-53,1,1663,913,4,52997,"FO2","GT" 33,17,5,2,2,528,1,"BREESE (CITY OF)","BREESE",0,"LIGHT OIL",2188,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,934,4,50322,"FO2","ST" 33,17,5,3,2,528,1,"BREESE (CITY OF)","BREESE",0,"LIGHT OIL",2188,"0A",1294,,,95,0,54,940,18,32,905,18,33,866,22,40,817,30,30,781,17,32,740,176,328,755,261,482,780,19,35,911,19,35,872,19,34,835,13,22,811,934,4,50322,"FO2","IC" 33,17,5,3,9,528,1,"BREESE (CITY OF)","BREESE",0,"NAT GAS",2188,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,934,4,50322,"NG","IC" 33,17,5,3,2,530,1,"BUSHNELL (CITY OF)","BUSHNELL",0,"LIGHT OIL",2634,"0A",1294,,,95,0,1,838,7,14,824,0,0,824,0,0,824,0,0,824,0,0,824,29,58,766,0,0,766,0,0,766,0,0,766,0,0,766,0,0,766,935,4,50383,"FO2","IC" 33,17,5,3,9,530,1,"BUSHNELL (CITY OF)","BUSHNELL",0,"NAT GAS",2634,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,935,4,50383,"NG","IC" 33,17,5,3,2,534,1,"CARLYLE (CITY OF)","CARLYLE",0,"LIGHT OIL",3037,"0A",1294,,,95,12,16,176,0,13,163,9,11,151,9,13,138,12,10,121,51,53,404,141,155,248,144,203,381,11,12,368,10,17,351,11,18,333,0,0,333,936,4,50438,"FO2","IC" 33,17,5,3,9,534,1,"CARLYLE (CITY OF)","CARLYLE",0,"NAT GAS",3037,"0A",1294,,,95,0,3,0,0,2,0,0,2,0,0,3,0,0,3,0,1,11,0,10,64,0,4,38,0,0,6,0,0,6,0,0,0,0,0,0,0,936,4,50438,"NG","IC" 33,17,5,3,2,537,1,"CARMI (CITY OF)","CARMI",0,"LIGHT OIL",3040,"0A",1294,,,95,16,38,765,95,45,720,10,19,700,7,19,681,5,21,660,5,32,627,5,12,616,9,15,600,18,53,722,9,20,702,10,22,702,61,90,590,937,4,50440,"FO2","IC" 33,17,5,3,9,537,1,"CARMI (CITY OF)","CARMI",0,"NAT GAS",3040,"0A",1294,,,95,70,720,0,25,1014,0,15,177,0,17,350,0,16,125,0,26,162,0,15,157,0,11,87,0,40,313,0,11,92,0,8,100,0,83,985,0,937,4,50440,"NG","IC" 33,17,5,2,6,559,1,"FAIRFIELD (CITY OF)","FAIRFIELD",0,"BIT COAL",6141,"0A",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,940,4,50941,"BIT","ST" 33,17,5,3,2,559,1,"FAIRFIELD (CITY OF)","FAIRFIELD",0,"LIGHT OIL",6141,"0A",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,940,4,50941,"FO2","IC" 33,17,5,3,9,559,1,"FAIRFIELD (CITY OF)","FAIRFIELD",0,"NAT GAS",6141,"0A",1294,"S",,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,940,4,50941,"NG","IC" 33,17,5,3,2,562,1,"FARMER (CITY OF)","FARMER CITY",0,"LIGHT OIL",6192,"0A",1294,,,95,1,3,227,0,0,227,0,0,227,0,0,227,1,2,230,10,20,208,7,23,186,38,71,283,4,4,279,0,0,279,0,0,274,0,0,274,941,4,50955,"FO2","IC" 33,17,5,3,9,562,1,"FARMER (CITY OF)","FARMER CITY",0,"NAT GAS",6192,"0A",1294,,,95,3,26,0,0,0,0,0,0,0,0,0,0,6,58,0,46,504,0,0,0,0,163,1723,0,0,0,0,0,0,0,0,0,0,0,0,0,941,4,50955,"NG","IC" 33,17,5,3,2,571,1,"FREEBURG (CITY OF)","FREEBURG",0,"LIGHT OIL",6764,"0A",1294,,,95,1,2,129,17,33,214,173,298,93,12,23,70,12,23,47,13,26,197,81,158,39,110,201,200,13,177,0,8,16,161,8,10,151,8,21,130,943,4,51056,"FO2","IC" 33,17,5,3,9,571,1,"FREEBURG (CITY OF)","FREEBURG",0,"NAT GAS",6764,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,943,4,51056,"NG","IC" 33,17,5,3,2,574,1,"GENESEO (CITY OF)","GENESEO",0,"LIGHT OIL",7095,"0A",1294,,,95,2,16,314,4,11,301,0,13,290,5,13,281,0,0,294,15,26,446,65,111,339,78,133,383,0,0,389,0,0,388,0,0,389,2,4,385,944,4,51093,"FO2","IC" 33,17,5,3,9,574,1,"GENESEO (CITY OF)","GENESEO",0,"NAT GAS",7095,"0A",1294,,,95,7,250,0,2,57,0,7,527,0,2,52,0,0,0,0,93,1716,0,562,6490,0,735,8338,0,0,0,0,0,0,0,0,0,0,0,1,0,944,4,51093,"NG","IC" 33,17,5,3,2,589,1,"HIGHLAND (CITY OF)","HIGHLAND",0,"LIGHT OIL",8573,"0A",1294,,,95,21,37,490,4,5,486,0,0,486,4,9,823,0,0,825,47,78,792,28,140,634,472,536,371,24,46,371,0,0,322,11,21,755,8,15,754,946,4,51298,"FO2","IC" 33,17,5,3,9,589,1,"HIGHLAND (CITY OF)","HIGHLAND",0,"NAT GAS",8573,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,946,4,51298,"NG","IC" 33,17,5,3,2,606,15,"MCLEANSBORO (CITY OF)","MCLEANSBORO",0,"LIGHT OIL",12167,"0A",1294,,,95,19,48,201,15,25,176,12,30,322,14,21,301,14,29,272,11,29,243,22,38,205,14,48,336,43,88,246,25,45,201,27,51,325,20,34,291,948,4,51812,"FO2","IC" 33,17,5,3,2,612,10,"MASCOUTAH (CITY OF)","MASCOUTAH",0,"LIGHT OIL",11790,"0A",1294,,,95,0,0,815,0,0,815,0,0,814,1,12,803,24,59,563,0,0,563,4,56,859,30,64,967,0,0,967,0,0,967,0,0,965,0,0,966,950,4,51789,"FO2","IC" 33,17,5,3,9,612,10,"MASCOUTAH (CITY OF)","MASCOUTAH",0,"NAT GAS",11790,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,10,410,0,0,0,0,0,0,0,74,4890,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,950,4,51789,"NG","IC" 33,17,5,2,9,646,1,"PERU (CITY OF)","PERU",0,"NAT GAS",14840,"0M",1294,,,95,-15,0,0,-11,0,0,4,0,0,-13,0,0,-7,0,0,77,680,0,-9,0,0,-62,0,0,0,0,0,8,0,0,0,0,0,0,0,0,955,4,52299,"NG","ST" 33,17,5,3,2,646,1,"PERU (CITY OF)","PERU",0,"LIGHT OIL",14840,"0M",1294,,,95,-30,12,619,-13,24,595,-13,23,572,-6,24,548,-2,23,525,63,146,560,189,366,550,299,560,533,-14,0,533,-1,23,510,-22,12,498,-33,0,498,955,4,52299,"FO2","IC" 33,17,5,4,2,646,1,"PERU (CITY OF)","PERU",0,"LIGHT OIL",14840,"0M",1294,,,95,-17,5,621,-6,30,547,-28,31,516,-11,19,497,2,45,621,32,120,501,-5,0,501,78,277,563,-5,0,563,2,31,532,-6,34,498,-8,0,498,955,4,52299,"FO2","GT" 33,17,5,3,2,649,15,"PRINCETON (CITY OF)","PRINCETON",0,"LIGHT OIL",15388,"0M",1294,,,95,6,12,977,0,0,976,3,7,975,2,4,971,3,7,975,23,40,932,56,97,838,536,913,802,20,35,768,17,32,720,0,3,712,14,25,688,957,4,52397,"FO2","IC" 33,17,5,3,9,649,15,"PRINCETON (CITY OF)","PRINCETON",0,"NAT GAS",15388,"0M",1294,,,95,21,220,0,0,0,0,27,268,0,15,153,0,24,231,0,137,1308,0,636,6226,0,1790,17269,0,131,1265,0,82,827,0,0,106,0,75,752,0,957,4,52397,"NG","IC" 33,17,5,3,2,652,15,"RANTOUL (CITY OF)","RANTOUL",0,"LIGHT OIL",15686,"0A",1294,,,95,18,21,236,2,5,232,6,12,220,11,25,195,23,32,203,55,112,186,16,31,295,0,0,299,0,0,299,8,15,284,0,0,284,0,0,284,958,4,52436,"FO2","IC" 33,17,5,3,2,655,1,"RED BUD (CITY OF)","RED BUD",0,"LIGHT OIL",15772,"0A",1294,,,95,28,56,1047,2,5,1040,2,3,1034,0,1,1030,4,7,1021,15,26,993,6,9,981,14,25,956,0,0,956,0,0,953,0,0,949,0,0,948,959,4,52447,"FO2","IC" 33,17,5,3,9,655,1,"RED BUD (CITY OF)","RED BUD",0,"NAT GAS",15772,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,959,4,52447,"NG","IC" 33,17,5,3,2,661,5,"ROCHELLE (CITY OF)","N NINTH ST",0,"LIGHT OIL",16179,"0A",1294,,,95,0,0,0,5,15,779,0,0,0,3,0,771,0,0,764,12,23,741,59,110,631,112,214,527,0,0,416,0,0,415,0,24,711,0,25,686,960,4,52498,"FO2","IC" 33,17,5,3,9,661,5,"ROCHELLE (CITY OF)","N NINTH ST",0,"NAT GAS",16179,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,9,98,0,490,5142,0,1012,10917,0,0,0,0,0,0,0,0,1171,0,0,705,0,960,4,52498,"NG","IC" 33,17,5,2,6,661,10,"ROCHELLE (CITY OF)","S MAIN ST",0,"BIT COAL",16179,"0A",1294,,,95,182,283,317,0,0,1359,692,1123,1498,0,0,1498,0,0,1498,0,0,1498,0,0,1498,0,0,1498,0,0,1218,0,0,0,256,380,38,0,38,0,961,4,52498,"BIT","ST" 33,17,5,2,9,661,10,"ROCHELLE (CITY OF)","S MAIN ST",0,"NAT GAS",16179,"0A",1294,,,95,2606,84363,0,2941,19198,0,1831,61444,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,927,28450,0,0,0,0,961,4,52498,"NG","ST" 33,17,5,3,2,661,10,"ROCHELLE (CITY OF)","S MAIN ST",0,"LIGHT OIL",16179,"0A",1294,,,95,0,0,0,0,0,261,0,0,259,7,8,258,0,0,258,0,0,1498,0,0,1498,0,2,252,0,0,251,0,0,252,0,1,249,0,0,216,961,4,52498,"FO2","IC" 33,17,5,3,9,661,10,"ROCHELLE (CITY OF)","S MAIN ST",0,"NAT GAS",16179,"0A",1294,,,95,0,0,0,0,0,0,14,486,0,2,19,0,0,0,0,0,0,0,0,0,0,83,2186,0,0,0,0,0,0,0,10,323,0,0,0,0,961,4,52498,"NG","IC" 33,17,5,2,2,676,1,"SPRINGFIELD (CITY OF)","LAKESIDE",0,"LIGHT OIL",17828,"0M",1294,,,95,18,56,3309,-376,0,3847,35,123,3773,38,88,3309,8,21,2805,159,387,2233,123,292,1856,53,125,1641,42,111,1830,11,54,1641,16,39,2126,38,94,1910,964,4,52766,"FO2","ST" 33,17,5,2,6,676,1,"SPRINGFIELD (CITY OF)","LAKESIDE",0,"BIT COAL",17828,"0M",1294,,,95,1426,1194,2186,0,0,2186,1719,1619,3329,28971,18281,2724,3680,2612,1929,9405,6305,1526,17496,11431,1377,28851,18625,1401,2662,1934,379,394,523,1151,16922,10895,1211,7009,4720,1069,964,4,52766,"BIT","ST" 33,17,5,2,2,676,5,"SPRINGFIELD (CITY OF)","DALLMAN",0,"LIGHT OIL",17828,"0M",1294,,,95,300,585,0,76,148,0,85,123,0,184,376,0,278,544,0,98,185,0,43,85,0,46,90,0,194,381,0,69,134,0,98,191,0,62,121,0,963,4,52766,"FO2","ST" 33,17,5,2,6,676,5,"SPRINGFIELD (CITY OF)","DALLMAN",0,"BIT COAL",17828,"0M",1294,,,95,147822,79578,86892,139935,74982,79739,149373,60539,83519,84927,48213,88238,138529,75670,76947,148142,77066,75576,175826,96140,69655,181595,98487,70624,145723,79465,62150,147146,79567,66752,143295,77415,69089,189782,102492,71677,963,4,52766,"BIT","ST" 33,17,5,4,2,676,10,"SPRINGFIELD (CITY OF)","REYNOLDS",0,"LIGHT OIL",17828,"0M",1294,,,95,2,21,1499,1,19,1480,0,0,1480,22,120,1360,0,0,1360,12,77,1283,189,560,1401,222,713,1224,45,147,1077,0,0,1792,0,0,1792,21,66,1726,965,4,52766,"FO2","GT" 33,17,5,4,2,676,12,"SPRINGFIELD (CITY OF)","FACTORY",0,"LIGHT OIL",17828,"0M",1294,,,95,0,0,3559,57,277,3282,0,56,3226,0,0,3226,0,0,3226,0,15,3212,234,612,3502,337,1007,2674,0,0,0,1,40,2634,0,0,2634,6,18,2615,8016,4,52766,"FO2","GT" 33,17,5,3,2,685,1,"SULLIVAN (CITY OF)","SULLIVAN",0,"LIGHT OIL",18277,"0A",1294,,,95,64,126,1258,39,77,1181,15,30,1151,13,25,1301,205,430,1242,250,497,1265,287,569,1218,337,669,1235,211,418,1150,109,216,1446,94,187,1607,131,261,1346,969,4,52842,"FO2","IC" 33,17,5,3,9,685,1,"SULLIVAN (CITY OF)","SULLIVAN",0,"NAT GAS",18277,"0A",1294,,,95,417,4732,0,354,3991,0,175,2187,0,90,1200,0,2497,25139,0,3160,40149,0,3856,39252,0,4473,45978,0,2693,27195,0,1163,12837,0,1195,13294,0,1409,15384,0,969,4,52842,"NG","IC" 33,17,5,3,2,688,1,"WATERLOO (CITY OF)","WATERLOO",0,"LIGHT OIL",20180,"0A",1294,,,95,0,0,663,0,0,655,5,10,638,0,0,632,2,10,596,2,5,575,67,109,621,73,155,621,8,14,601,0,0,593,0,0,587,3,6,574,971,4,53196,"FO2","IC" 33,17,5,3,9,688,1,"WATERLOO (CITY OF)","WATERLOO",0,"NAT GAS",20180,"0A",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,2,17,0,3,26,0,77,912,0,83,788,0,0,0,0,0,0,0,0,0,0,0,0,0,971,4,53196,"NG","IC" 33,17,5,2,6,697,1,"WINNETKA (VILLAGE OF)","WINNEKA",0,"BIT COAL",20824,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,972,4,53319,"BIT","ST" 33,17,5,2,9,697,1,"WINNETKA (VILLAGE OF)","WINNEKA",0,"NAT GAS",20824,"0M",1294,,,95,76,1403,0,83,1602,0,0,0,0,61,1226,0,0,0,0,429,7918,0,1790,29451,0,3027,46315,0,83,1711,0,38,687,0,36,627,0,82,1282,0,972,4,53319,"NG","ST" 33,17,5,3,2,697,1,"WINNETKA (VILLAGE OF)","WINNEKA",0,"LIGHT OIL",20824,"0M",1294,,,95,9,15,1600,16,24,1576,15,27,2011,8,11,2038,15,27,2008,53,94,1879,81,146,1771,87,156,1614,39,65,1549,14,24,1525,21,36,1489,27,48,1441,972,4,53319,"FO2","IC" 33,17,8,3,2,835,5,"SOYLAND POWER COOP INC","PITTSFIELD",0,"LIGHT OIL",40307,"0M",1294,,,95,-86,19,362,-83,0,362,-84,0,362,-71,0,362,-22,0,362,-10,10,352,-13,0,352,-12,5,346,-10,0,346,-17,0,346,-27,0,346,-86,0,346,6237,4,53264,"FO2","IC" 33,17,8,3,2,835,10,"SOYLAND POWER COOP INC","WINCHESTER",0,"LIGHT OIL",40307,"0M",1294,"R",,95,-5,0,0,-4,0,0,-2,0,0,-4,0,0,-4,0,0,-3,0,0,-4,0,0,-4,0,0,-4,0,0,-3,0,0,-4,0,0,0,0,0,6236,4,53264,"FO2","IC" 33,17,8,2,2,835,20,"SOYLAND POWER COOP INC","PEARL",0,"LIGHT OIL",40307,"0M",1294,,,95,394,885,0,148,333,0,151,333,0,44,96,0,62,137,0,71,157,0,49,109,0,81,183,0,82,176,0,53,118,0,43,98,0,0,293,0,6238,4,53264,"FO2","ST" 33,17,8,2,6,835,20,"SOYLAND POWER COOP INC","PEARL",0,"BIT COAL",40307,"0M",1294,,,95,7480,4550,11696,6009,3668,13434,10811,6523,12395,9951,5859,11765,8686,5203,12183,10526,6310,12845,13881,8405,11170,12227,7501,11236,14144,8259,10522,14726,8807,6860,7789,4727,5629,-128,0,6213,6238,4,53264,"BIT","ST" 33,17,8,4,2,835,20,"SOYLAND POWER COOP INC","PEARL",0,"LIGHT OIL",40307,"0M",1294,,,95,0,0,3174,0,0,2841,0,0,2508,0,0,3312,0,0,3174,0,0,3018,198,439,4233,153,346,3704,0,0,3527,0,0,3410,0,0,3316,27,99,2920,6238,4,53264,"FO2","GT" 33,17,8,2,2,865,5,"SOUTHERN ILL PWR COOP","MARION",0,"LIGHT OIL",17632,"0M",1294,,,95,103,235,1930,398,937,1432,119,273,2109,54,114,1931,53,121,2200,40,89,1995,197,433,1909,516,982,1299,123,278,1355,138,291,1409,148,311,1983,116,228,2304,976,4,52726,"FO2","ST" 33,17,8,2,5,865,5,"SOUTHERN ILL PWR COOP","MARION",0,"COKE",17632,"0M",494,,,95,0,0,0,0,0,0,0,0,0,7100,5033,63,10577,7498,1080,12093,8573,883,18130,8251,340,24637,9801,5288,14975,6746,15187,18417,7751,15005,28435,11888,20057,29187,11536,36572,976,4,52726,"PC","ST" 33,17,8,2,6,865,5,"SOUTHERN ILL PWR COOP","MARION",0,"BIT COAL",17632,"0M",1294,,,95,99578,58899,343511,88921,53220,322269,67012,39679,313811,55683,32048,304374,67117,37520,306395,69155,37199,286872,84620,48755,270682,92636,56774,253743,47041,28911,281123,49349,30941,306445,68451,42435,291995,75427,45356,318016,976,4,52726,"BIT","ST" 34,26,1,2,1,21,1,"CONSUMERS POWER CO","BIG ROCK",0,"NUCLEAR",4254,"0M",1294,,95,95,49904,0,0,36125,0,0,47852,0,0,36194,0,0,51600,0,0,49866,0,0,50938,0,0,42590,0,0,45863,0,0,42825,0,0,30166,0,0,31731,0,0,1697,1,50658,"UR","ST" 34,26,1,2,1,21,1,"CONSUMERS POWER CO","PALISADES",0,"NUCLEAR",4254,"0M",1294,,95,95,583852,0,0,515599,0,0,577496,0,0,558296,0,0,349591,0,0,-2326,0,0,-2452,0,0,108144,0,0,474684,0,0,571773,0,0,561439,0,0,541156,0,0,1715,1,50658,"UR","ST" 34,26,1,1,,21,8,"CONSUMERS POWER CO","ALCONA",0,,4254,"0M",1294,,95,95,2490,0,0,1993,0,0,2704,0,0,2797,0,0,2622,0,0,1880,0,0,1902,0,0,2070,0,0,1760,0,0,2007,0,0,2376,0,0,2188,0,0,1693,1,50658,"WAT","HY" 34,26,1,1,,21,10,"CONSUMERS POWER CO","ALLEGAN",0,,4254,"0M",1294,,95,95,1357,0,0,1013,0,0,1394,0,0,1356,0,0,1410,0,0,981,0,0,946,0,0,1011,0,0,703,0,0,731,0,0,1154,0,0,994,0,0,1694,1,50658,"WAT","HY" 34,26,1,1,,21,19,"CONSUMERS POWER CO","C W TIPPY",0,,4254,"0M",1294,,95,95,5282,0,0,4150,0,0,6293,0,0,5440,0,0,5008,0,0,4326,0,0,4371,0,0,5203,0,0,4190,0,0,4573,0,0,5014,0,0,4570,0,0,1698,1,50658,"WAT","HY" 34,26,1,1,,21,25,"CONSUMERS POWER CO","COOKE",0,,4254,"0M",1294,,95,95,2367,0,0,1873,0,0,2687,0,0,2739,0,0,2539,0,0,1904,0,0,1946,0,0,2050,0,0,1790,0,0,2028,0,0,2329,0,0,2102,0,0,1700,1,50658,"WAT","HY" 34,26,1,1,,21,26,"CONSUMERS POWER CO","CROTON",0,,4254,"0M",1294,,95,95,4641,0,0,3300,0,0,4505,0,0,3399,0,0,3856,0,0,2193,0,0,2270,0,0,3054,0,0,2166,0,0,2146,0,0,3632,0,0,3031,0,0,1701,1,50658,"WAT","HY" 34,26,1,1,,21,28,"CONSUMERS POWER CO","FIVE CHANLS",0,,4254,"0M",1294,,95,95,2230,0,0,1812,0,0,2478,0,0,2479,0,0,2347,0,0,1784,0,0,1756,0,0,1920,0,0,1683,0,0,1895,0,0,2059,0,0,1961,0,0,1704,1,50658,"WAT","HY" 34,26,1,1,,21,29,"CONSUMERS POWER CO","FOOTE",0,,4254,"0M",1294,,95,95,2783,0,0,2213,0,0,3183,0,0,3182,0,0,2865,0,0,2239,0,0,2243,0,0,2387,0,0,2148,0,0,2381,0,0,2653,0,0,2564,0,0,1705,1,50658,"WAT","HY" 34,26,1,1,,21,32,"CONSUMERS POWER CO","HARDY",0,,4254,"0M",1294,,95,95,10721,0,0,6926,0,0,9337,0,0,6936,0,0,8622,0,0,4585,0,0,5199,0,0,7002,0,0,5021,0,0,5910,0,0,8935,0,0,6928,0,0,1707,1,50658,"WAT","HY" 34,26,1,1,,21,34,"CONSUMERS POWER CO","HODENPYL",0,,4254,"0M",1294,,95,95,3684,0,0,2846,0,0,4474,0,0,3916,0,0,3467,0,0,2500,0,0,2611,0,0,3740,0,0,2787,0,0,3279,0,0,4048,0,0,3474,0,0,1708,1,50658,"WAT","HY" 34,26,1,1,,21,38,"CONSUMERS POWER CO","LOUD",0,,4254,"0M",1294,,95,95,1690,0,0,1352,0,0,1882,0,0,1972,0,0,1822,0,0,1365,0,0,1424,0,0,1486,0,0,1265,0,0,1447,0,0,1654,0,0,1528,0,0,1712,1,50658,"WAT","HY" 34,26,1,1,,21,40,"CONSUMERS POWER CO","LD PUMP ST",0,"P-PUMPSTG",4254,"0M",1294,,95,95,-64589,233719,0,-57356,190758,0,-53950,195482,0,-71987,218971,0,-31897,115524,0,-60407,243003,0,-67008,223779,0,-77060,289960,0,-65130,213393,0,-70748,250623,0,-58089,197571,0,-53599,186916,0,1713,1,50658,"WAT","HY" 34,26,1,1,,21,42,"CONSUMERS POWER CO","MIO",0,,4254,"0M",1294,,95,95,1408,0,0,1113,0,0,1515,0,0,1563,0,0,1475,0,0,1064,0,0,1017,0,0,1161,0,0,991,0,0,1142,0,0,1213,0,0,1283,0,0,1714,1,50658,"WAT","HY" 34,26,1,1,,21,49,"CONSUMERS POWER CO","ROGERS",0,,4254,"0M",1294,,95,95,2752,0,0,1858,0,0,2142,0,0,2190,0,0,2657,0,0,1513,0,0,1706,0,0,2352,0,0,1808,0,0,1968,0,0,2874,0,0,2363,0,0,1716,1,50658,"WAT","HY" 34,26,1,1,,21,58,"CONSUMERS POWER CO","WEBBER",0,,4254,"0M",1294,,95,95,1914,0,0,1295,0,0,2105,0,0,2059,0,0,1759,0,0,836,0,0,748,0,0,1150,0,0,321,0,0,398,0,0,1321,0,0,928,0,0,1722,1,50658,"WAT","HY" 34,26,1,2,2,21,65,"CONSUMERS POWER CO","JH CAMPBELL",0,"LIGHT OIL",4254,"0M",1294,,95,95,376,598,4499,283,447,4052,1907,3068,3484,2100,3394,4019,519,835,7113,985,1571,5531,311,508,5023,954,1563,3460,1220,1999,3604,1817,2975,4007,1351,2181,3968,1278,2102,3566,1710,1,50658,"FO2","ST" 34,26,1,2,6,21,65,"CONSUMERS POWER CO","JH CAMPBELL",0,"BIT COAL",4254,"0M",1294,,95,95,688173,266958,245746,629424,250579,214312,554183,223280,253129,421848,167012,399301,597082,246292,477288,640613,258293,443746,603954,255371,374582,621938,269381,277933,502655,214049,299355,646510,274214,290900,687374,281291,323449,707593,291775,344669,1710,1,50658,"BIT","ST" 34,26,1,4,2,21,65,"CONSUMERS POWER CO","JH CAMPBELL",0,"LIGHT OIL",4254,"0M",1294,,95,95,3,18,3579,26,68,3511,5,2,3510,3,8,3501,14,105,3396,1,1,3395,89,352,3043,300,894,2816,0,0,2816,0,0,2780,12,29,2750,0,0,2750,1710,1,50658,"FO2","GT" 34,26,1,2,2,21,70,"CONSUMERS POWER CO","B C COBB",0,"LIGHT OIL",4254,"0M",1294,,95,95,119,201,0,106,183,0,15,25,0,151,260,0,15,25,0,11,20,0,1038,1787,0,616,1065,0,337,575,0,124,210,0,609,1027,0,116,197,0,1695,1,50658,"FO2","ST" 34,26,1,2,6,21,70,"CONSUMERS POWER CO","B C COBB",0,"BIT COAL",4254,"0M",1294,,95,95,171685,81705,303296,112559,55863,247433,173477,86683,160750,176230,89153,134091,171229,86036,137454,177787,81941,81399,152875,79003,128717,175209,87546,157003,143997,70790,171410,172337,82837,192966,174578,86518,170355,171682,85592,358752,1695,1,50658,"BIT","ST" 34,26,1,2,9,21,70,"CONSUMERS POWER CO","B C COBB",0,"NAT GAS",4254,"0M",1294,,95,95,921,9110,0,661,6660,0,735,7267,0,667,6715,0,387,3867,0,701,6993,0,490,4921,0,732,7388,0,377,3745,0,625,6179,0,826,8120,0,729,7244,0,1695,1,50658,"NG","ST" 34,26,1,4,9,21,71,"CONSUMERS POWER CO","B E MORROW",0,"NAT GAS",4254,"0M",1294,,95,95,21,1252,0,61,797,0,23,390,0,0,0,0,0,0,0,401,8324,0,371,9296,0,1149,25420,0,33,769,0,0,0,0,0,0,0,0,0,0,1696,1,50658,"NG","GT" 34,26,1,2,2,21,73,"CONSUMERS POWER CO","D E KARN",0,"LIGHT OIL",4254,"0M",1294,,95,95,95,155,4465,729,1211,3870,49,79,4192,1413,2315,3502,1471,2465,4192,323,528,4944,367,607,3918,3048,4972,4484,1078,1808,6755,441,718,5263,482,776,5343,208,340,5633,1702,1,50658,"FO2","ST" 34,26,1,2,3,21,73,"CONSUMERS POWER CO","D E KARN",0,"HEAVY OIL",4254,"0M",1294,,95,95,17263,41101,178646,32230,70799,144631,3259,14882,162100,3710,14639,204722,1348,4618,245418,27469,68422,203997,56064,119639,141693,95085,202123,111624,29250,66633,127707,-2403,604,148925,24960,66400,139076,24013,58612,178738,1702,1,50658,"FO6","ST" 34,26,1,2,6,21,73,"CONSUMERS POWER CO","D E KARN",0,"BIT COAL",4254,"0M",1294,,95,95,201703,83102,130505,120289,51141,110637,178823,75624,145086,292219,122156,106091,232390,98356,133690,313475,134010,126635,299344,128910,118120,335951,141190,65110,201053,86888,158744,293910,123720,122461,305821,124517,171638,315326,164076,152202,1702,1,50658,"BIT","ST" 34,26,1,2,9,21,73,"CONSUMERS POWER CO","D E KARN",0,"NAT GAS",4254,"0M",1294,,95,95,0,0,0,0,0,0,126,3486,0,7447,169068,0,10439,207703,0,12622,193255,0,50264,657734,0,101002,1316168,0,18325,257600,0,0,0,0,11460,187792,0,10071,152074,0,1702,1,50658,"NG","ST" 34,26,1,4,9,21,74,"CONSUMERS POWER CO","GAYLORD",0,"NAT GAS",4254,"0M",1294,,95,95,16,288,0,102,1836,0,15,332,0,0,0,0,0,0,0,515,9959,0,346,16592,0,3203,53480,0,4,2469,0,2,482,0,49,1700,0,0,0,0,1706,1,50658,"NG","GT" 34,26,1,4,9,21,79,"CONSUMERS POWER CO","STRAITS",0,"NAT GAS",4254,"0M",1294,,95,95,0,0,0,20,371,0,33,801,0,0,0,0,0,427,0,0,0,0,0,0,0,201,2828,0,203,2283,0,10,340,0,0,0,0,0,0,0,1718,1,50658,"NG","GT" 34,26,1,4,9,21,80,"CONSUMERS POWER CO","THETFORD",0,"NAT GAS",4254,"0M",1294,,95,95,-73,0,0,51,3065,0,-47,1801,0,-81,0,0,-11,1761,0,1724,48143,0,3577,74211,0,8176,149686,0,359,8949,0,103,2718,0,99,1204,0,-193,371,0,1719,1,50658,"NG","GT" 34,26,1,2,2,21,81,"CONSUMERS POWER CO","WEADOCK",0,"LIGHT OIL",4254,"0M",1294,,95,95,0,0,0,43,71,0,206,349,0,0,0,0,0,0,0,32,55,0,418,680,0,532,903,0,187,305,0,128,198,0,422,716,0,0,0,0,1720,1,50658,"FO2","ST" 34,26,1,2,6,21,81,"CONSUMERS POWER CO","WEADOCK",0,"BIT COAL",4254,"0M",1294,,95,95,192310,85708,45814,188975,83651,56497,190706,85006,57355,187037,83678,61516,177334,80278,58828,184095,83971,65159,155632,70970,60725,137329,63894,42030,160634,72475,36751,171924,77864,49121,139453,63086,78970,91065,41232,72440,1720,1,50658,"BIT","ST" 34,26,1,4,9,21,81,"CONSUMERS POWER CO","WEADOCK",0,"NAT GAS",4254,"0M",1294,,95,95,1,12,0,16,289,0,3,117,0,0,0,0,0,0,0,7,73,0,6,58,0,5,49,0,44,404,0,8,72,0,0,0,0,0,0,0,1720,1,50658,"NG","GT" 34,26,1,2,2,21,84,"CONSUMERS POWER CO","WHITING",0,"LIGHT OIL",4254,"0M",1294,,95,95,67,114,0,17,29,0,23,38,0,43,74,0,40,69,0,63,110,0,122,217,0,60,107,0,40,69,0,81,138,0,152,260,0,71,122,0,1723,1,50658,"FO2","ST" 34,26,1,2,6,21,84,"CONSUMERS POWER CO","WHITING",0,"BIT COAL",4254,"0M",1294,,95,95,187062,77616,89934,185094,74786,71016,195982,81145,69534,189147,74635,99630,151777,65376,105918,176546,69938,98910,159910,67506,87345,170468,72736,86560,153306,62762,86674,136600,57354,115439,140799,58953,146166,157205,64361,118168,1723,1,50658,"BIT","ST" 34,26,1,4,2,21,84,"CONSUMERS POWER CO","WHITING",0,"LIGHT OIL",4254,"0M",1294,,95,95,0,0,3383,0,0,3383,0,0,3383,0,0,3383,0,0,3383,13,41,3341,40,165,3176,586,1651,1525,5,60,3025,0,0,3037,0,0,3037,13,28,3009,1723,1,50658,"FO2","GT" 34,26,1,2,1,30,2,"DETROIT EDISON CO (THE)","FERMI 2",0,"NUCLEAR",5109,"0M",1294,,,95,57145,0,0,-2291,0,0,191112,0,0,332959,0,0,429952,0,0,318206,0,0,641286,0,0,646514,0,0,632787,0,0,629384,0,0,621966,0,0,597155,0,0,1729,1,50782,"UR","ST" 34,26,1,2,2,30,5,"DETROIT EDISON CO (THE)","HARBOR BECH",0,"LIGHT OIL",5109,"0M",1294,,,95,438,1013,575,399,920,291,337,838,431,226,616,443,208,409,330,272,533,404,256,504,456,402,782,347,137,284,368,256,520,468,392,891,512,324,728,420,1731,1,50782,"FO2","ST" 34,26,1,2,6,30,5,"DETROIT EDISON CO (THE)","HARBOR BECH",0,"BIT COAL",5109,"0M",1294,,,95,19026,9916,30527,16932,9323,21204,13176,7346,13858,2917,1770,26559,11229,4899,21660,24213,10667,10993,14172,6321,18792,27860,12241,19588,7804,3632,16168,5468,2542,33328,18662,9888,37691,11914,6187,42217,1731,1,50782,"BIT","ST" 34,26,1,3,2,30,5,"DETROIT EDISON CO (THE)","HARBOR BECH",0,"LIGHT OIL",5109,"0M",1294,,,95,0,0,0,-6,7,0,1,2,0,-9,2,0,-7,8,0,-8,5,0,10,38,0,215,410,0,-7,4,0,-10,0,0,-9,2,0,-4,5,0,1731,1,50782,"FO2","IC" 34,26,1,2,2,30,10,"DETROIT EDISON CO (THE)","BEACON",0,"LIGHT OIL",5109,"0M",1294,,,95,0,0,5557,0,0,6175,0,0,6175,0,0,6175,0,0,6175,0,0,6175,0,0,6175,0,0,6175,0,0,6175,0,0,6175,0,0,6175,0,0,6175,1724,1,50782,"FO2","ST" 34,26,1,2,6,30,10,"DETROIT EDISON CO (THE)","BEACON",0,"BIT COAL",5109,"0M",1294,,,95,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,0,