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1

Haleakala SW Rift Zone Exploration | Open Energy Information  

Open Energy Info (EERE)

Haleakala SW Rift Zone Exploration Haleakala SW Rift Zone Exploration Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Development Project: Haleakala SW Rift Zone Exploration Project Location Information Coordinates 20.63144440367°, -156.37383611407° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":20.63144440367,"lon":-156.37383611407,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

2

Mercury Vapor At Haleakala Volcano Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mercury Vapor At Haleakala Volcano Area (Thomas, 1986) Mercury Vapor At Haleakala Volcano Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Mercury Vapor Activity Date Usefulness not indicated DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles. Geophysical and geochemical surveys along this rift (southwest) were limited by difficult field conditions and access limitations. The geophysical program consisted of one Schlumberger sounding, one

3

Geothermometry At Haleakala Volcano Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Geothermometry At Haleakala Volcano Area (Thomas, 1986) Geothermometry At Haleakala Volcano Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Geothermometry At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Geothermometry Activity Date Usefulness not indicated DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles. Geophysical and geochemical surveys along this rift (southwest) were limited by difficult field conditions and access limitations. The geophysical program consisted of one Schlumberger sounding, one

4

Gas Flux Sampling At Haleakala Volcano Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Gas Flux Sampling At Haleakala Volcano Area (Thomas, 1986) Gas Flux Sampling At Haleakala Volcano Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Gas Flux Sampling Activity Date Usefulness useful DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles. Geophysical and geochemical surveys along this rift (southwest) were limited by difficult field conditions and access limitations. The geophysical program consisted of one Schlumberger sounding, one

5

Time-Domain Electromagnetics At Haleakala Volcano Area (Thomas, 1986) |  

Open Energy Info (EERE)

Time-Domain Electromagnetics At Haleakala Volcano Time-Domain Electromagnetics At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Time-Domain Electromagnetics Activity Date Usefulness useful DOE-funding Unknown Notes Controlled-source electromagnetic soundings were found to be substantially more successful in the southwest rift than either the Schlumberger or the self-potential studies. This was largely due to the ability of time-domain methods to penetrate high-resistivity surface layers and thus to define lower-resistivity sections at depth. The results of this sounding study, which was conducted at elevations ranging from 75 to 497 m a.s.l., generally indicated moderate- to lowresistivity (6 - 7 ohm.m) sections to depths of 1 km on the lower rift zone and higher resistivities (12-16

6

Direct-Current Resistivity Survey At Haleakala Volcano Area (Thomas, 1986)  

Open Energy Info (EERE)

Direct-Current Resistivity Survey At Haleakala Direct-Current Resistivity Survey At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles. Geophysical and geochemical surveys along this rift (southwest) were limited by difficult field conditions and access limitations. The geophysical program consisted of one Schlumberger sounding, one self-potential profile and one controlled-source electromagnetic sounding. The geochemical data collected included a reconnaissance soil mercury and

7

Direct-Current Resistivity At Haleakala Volcano Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

source source History View New Pages Recent Changes All Special Pages Semantic Search/Querying Get Involved Help Apps Datasets Community Login | Sign Up Search Page Edit History Facebook icon Twitter icon » Direct-Current Resistivity At Haleakala Volcano Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles.

8

Haleakala Volcano Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Haleakala Volcano Geothermal Area Haleakala Volcano Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Haleakala Volcano Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (7) 10 References Area Overview Geothermal Area Profile Location: Hawaii Exploration Region: Hawaii Geothermal Region GEA Development Phase: 2008 USGS Resource Estimate Mean Reservoir Temp: Estimated Reservoir Volume: Mean Capacity: Click "Edit With Form" above to add content History and Infrastructure Operating Power Plants: 0 No geothermal plants listed. Add a new Operating Power Plant

9

Rift Zone | Open Energy Information  

Open Energy Info (EERE)

Rift Zone Rift Zone Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Print PDF Rift Zone Dictionary.png Rift Zone: A divergent plate boundary within a continent Other definitions:Wikipedia Reegle Tectonic Settings List of tectonic settings known to host modern geothermal systems: Extensional Tectonics Subduction Zone Rift Zone Hot Spot Non-Tectonic Strike-Slip The Rio Grande Rift exemplifies rift zone tectonics - increased volcanic activity and the formation of graben structures (reference: science-art.com) Rift valleys occur at divergent plate boundaries, resulting in large graben structures and increased volcanism. The East African Rift is an example of a continental rift zone with increased volcanism, while the Atlantic's spreading Mid-Ocean Ridge is host to an enormous amount of geothermal

10

Gulf of California Rift Zone Geothermal Region | Open Energy...  

Open Energy Info (EERE)

of California Rift Zone Geothermal Region (Redirected from Gulf of California Rift Zone) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Gulf of California Rift Zone...

11

Hawaii/Geothermal | Open Energy Information  

Open Energy Info (EERE)

Hawaii/Geothermal Hawaii/Geothermal < Hawaii Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Print PDF Hawaii Geothermal General Regulatory Roadmap Geothermal Power Projects Under Development in Hawaii Developer Location Estimated Capacity (MW) Development Phase Geothermal Area Geothermal Region Haleakala SW Rift Zone Exploration Ormat Technologies Inc , US Department of Energy Haleakala Southwest Rift Zone Haleakala Volcano Geothermal Area Hawaii Geothermal Region Puna Geothermal Venture Ormat Technologies Inc Pahoa, Hawaii 38 MW38,000 kW 38,000,000 W 38,000,000,000 mW 0.038 GW 3.8e-5 TW Kilauea East Rift Geothermal Area Hawaii Geothermal Region Add a geothermal project. Operational Geothermal Power Plants in Hawaii Owner Facility Type Capacity (MW) Commercial Online

12

Structural style of the Turkana Rift, Kenya  

SciTech Connect

Multifold seismic reflection and geologic mapping in part of the eastern branch of the East African Rift system of northern Kenya reveal a major rift structure containing at least 3 km of Neogene sediment fill beneath Lake Turkana. This includes a series of half-graben basins, with centrally located quaternary volcanic centers, which are linked end-to-end by structural accommodation zones. Whereas the geometry of rifting is similar to that of the nonvolcanic western branch of the East African Rift system, the Turkana half-grabens are much smaller and may reflect extension of a thinner lithosphere or development of more closely spaced fracture patterns during rift evolution, or both.

Dunkelman, T.J.; Karson, J.A.; Rosendahl, B.R.

1988-03-01T23:59:59.000Z

13

Gulf of California Rift Zone Geothermal Region | Open Energy...  

Open Energy Info (EERE)

Gulf of California Rift Zone Geothermal Region Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Gulf of California Rift Zone Geothermal Region edit Details Areas (15)...

14

Rio Grande Rift Geothermal Region | Open Energy Information  

Open Energy Info (EERE)

Rift Geothermal Region Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Rio Grande Rift Geothermal Region edit Details Areas (21) Power Plants (0) Projects (2)...

15

Water Sampling At Hualalai Northwest Rift Area (Thomas, 1986...  

Open Energy Info (EERE)

Water Sampling At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Water Sampling Activity Date...

16

Delta Faucet: Data Request (2010-SW-1603) | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Delta Faucet: Data Request (2010-SW-1603) Delta Faucet: Data Request (2010-SW-1603) March 2, 2010 DOE requested test data from Delta Faucet Corporation for Delta Faucet's...

17

Mueller Streamline: Data Request (2011-SW-2802) | Department...  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Data Request (2011-SW-2802) Mueller Streamline: Data Request (2011-SW-2802) May 17, 2011 DOE requested water efficiency test data, including complete test reports, from Mueller...

18

Aeromagnetic Survey At Kilauea Southwest Rift And South Flank...  

Open Energy Info (EERE)

appears to substantiate the presence of a thermal resource; there is a marked bipolar magnetic anomaly paralleling the rift zone from the summit to the lower rift near the coast...

19

Remote Sensing for Biodiversity Conservation of the Albertine Rift  

E-Print Network (OSTI)

183 10 Remote Sensing for Biodiversity Conservation of the Albertine Rift in Eastern Africa Samuel 2003). The rapidly developing field of remote sensing has been invaluable to biodiversity conservation...............................................................................................184 10.3 Remote Sensing of the Albertine Rift .....................................................185

Wang, Y.Q. "Yeqiao"

20

Thermomechanical models of the Rio Grande rift  

SciTech Connect

Fully two-dimensional, coupled thermochemical solutions of a continental rift and platform are used to model the crust and mantle structure of a hot, buoyant mantle diapir beneath the Rio Grande rift. The thermomechanical model includes both linear and nonlinear laws of the Weertman type relating shear stress and creep strain rate, viscosity which depends on temperature and pressure, and activation energy, temperature-dependent thermal conductivity, temperature-dependent coefficient of thermal expansion, the Boussinesq approximation for thermal bouyancy, material convection using a stress rate that is invariant to rigid rotations, an elastically deformable crust, and a free surface. The model determines the free surface velocities, solid state flow field in the mantle, and viscosity structure of lithosphere and asthenosphere. Regional topography and crustal heat flow are simulated. A suite of symmetric models, assumes continental geotherms on the right and the successively increasing rift geotherms on the left. These models predict an asthenospheric flow field which transfers cold material laterally toward the rift at > 300 km, hot, buoyant material approx. 200 km wide which ascends vertically at rates of 1 km/my between 175 to 325 km, and spreads laterally away from the rift at the base of the lithosphere. Crustal spreading rates are similar to uplift rates. The lithosphere acts as stiff, elastic cap, damping upward motion through decreased velocities of 1 km/10 my and spreading uplift laterally. A parameter study varying material coefficients for the Weertman flow law suggests asthenospheric viscosities of approx. 10/sup 22/ to 10/sup 23/ poise. Similar studies predict crustal viscosities of approx. 10/sup 25/ poise. The buoyant process of mantle flow narrows and concentrates heat transport beneath the rift, increases upward velocity, and broadly arches the lithosphere. 10 figures, 1 table.

Bridwell, R.J.; Anderson, C.A.

1980-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


21

Zoe Industries: Data Request (2010-SW-1602) | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Data Request (2010-SW-1602) Zoe Industries: Data Request (2010-SW-1602) March 2, 2010 DOE requested test data from Zoe Industries, Inc., regarding the water consumption of a model...

22

SEM supports CMM-SW Level 2 | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

supports CMM-SW Level 2 More Documents & Publications SEM Supports CMM-SW Level 3 Systems Engineering Methodology (SEM) Planning for a Software Process Assessment Energy.gov...

23

Stratigraphy and rifting history of the Mesozoic-Cenozoic Anza rift, Kenya  

Science Conference Proceedings (OSTI)

Lithological and compositional relationships, thicknesses, and palynological data from drilling cuttings from five wells in the Anza rift, Kenya, indicate active rifting during the Late Cretaceous and Eocene-Oligocene. The earlier rifting possibly started in the Santonian-Coniacian, primarily occurred in the Campanian, and probably extended into the Maastrichtian. Anza rift sedimentation was in lacustrine, lacustrine-deltaic, fluvial, and flood-basin environments. Inferred synrift intervals in wells are shalier, thicker, more compositionally immature, and more poorly sorted than Lower Cretaceous ( )-lower Upper Cretaceous and upper Oligocene( )-Miocene interrift deposits. Synrift sandstone is mostly feldspathic or arkosic wacke. Sandstone deposited in the Anza basin during nonrift periods is mostly quartz arenite, and is coarser and has a high proportion of probable fluvial deposits relative to other facies. Volcanic debris is absent in sedimentary strata older than Pliocene-Holocene, although small Cretaceous intrusions are present in the basin. Cretaceous sandstone is cemented in places by laumontite, possibly recording Campanian extension. Early Cretaceous history of the Anza basin is poorly known because of the limited strata sampled; Jurassic units were not reached. Cretaceous rifting in the Anza basin was synchronous with rifting in Sudan and with the breakup and separation of South America and Africa; these events likely were related. Eocene-Oligocene extension in the Anza basin reflects different stresses. The transition from active rifting to passive subsidence in the Anza basin at the end of the Neogene, in turn, records a reconfigured response of east African plates to stresses and is correlated with formation of the East Africa rift.

Winn, R.D. Jr.; Steinmetz, J.C. (Marathon Oil Co., Littleton, CO (United States)); Kerekgyarto, W.L. (Marathon Oil Co., Houston, TX (United States))

1993-11-01T23:59:59.000Z

24

Security principles and management method for secure S/W introduction  

Science Conference Proceedings (OSTI)

An existing S/W development enterprises was negligent in S/W security problem because of imminent development period, insufficient fund and ignorance of security, and weakness problem of S/W almost has solved by beta test and a patch mostly. In addition, ... Keywords: S/W, S/W introduction, secure S/W, security

Jae Hong Han; Ho Seong Kim; Wan S. Yi; Yoo Jae Won

2008-11-01T23:59:59.000Z

25

Structure of continental rifts: Role of older features and magmatism  

SciTech Connect

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.

Keller, G.R. (Univ. of Texas, El Paso, TX (United States))

1996-01-01T23:59:59.000Z

26

Upstream -- SW92-03&  

Office of Legacy Management (LM)

09 09 This page intentionally left blank Upstream -- SW00-01 a _______________________________________________________________________________________________________________________________________________ Analyte Unit 04/18/00 07/17/00 10/20/00 04/17/01 07/11/01 10/09/01 04/07/05 10/05/05 04/28/06 10/02/06 04/11/07 10/08/07 04/09/08 g _______________________________________________________________________________________________________________________________________________ Field Measurements Alkalinity b mg/L 196 130 263 218 196 98 145 202 228 183 227 186 213 Conductivity c μmhos/cm 1544 847 8190 792 652 632 562 1389 1011 1332 959 1157 613

27

Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And...  

Open Energy Info (EERE)

Flank Area (Wyss, Et Al., 2001) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And...

28

Hualalai Northwest Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Hualalai Northwest Rift Geothermal Area Hualalai Northwest Rift Geothermal Area (Redirected from Hualalai Northwest Rift Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Hualalai Northwest Rift Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (9) 10 References Area Overview Geothermal Area Profile Location: Hawaii Exploration Region: Hawaii Geothermal Region GEA Development Phase: 2008 USGS Resource Estimate Mean Reservoir Temp: Estimated Reservoir Volume: Mean Capacity: Click "Edit With Form" above to add content History and Infrastructure Operating Power Plants: 0

29

Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea...  

Open Energy Info (EERE)

SURVEY, 2006 DOI Not Provided Check for DOI availability: http:crossref.org Online Internet link for Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano,...

30

Ground Gravity Survey At Kilauea East Rift Area (Broyles, Et...  

Open Energy Info (EERE)

Activity Details Location Kilauea East Rift Area Exploration Technique Ground Gravity Survey Activity Date Usefulness not indicated DOE-funding Unknown References M. L....

31

Modeling-Computer Simulations At Kilauea East Rift Area (Rudman...  

Open Energy Info (EERE)

navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Modeling-Computer Simulations At Kilauea East Rift Area (Rudman & Epp, 1983) Exploration Activity...

32

Direct-Current Resistivity Survey At Kilauea Southwest Rift And...  

Open Energy Info (EERE)

Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes The electrical resistivity data acquired on the southwest rift delineated two distinct...

33

Direct-Current Resistivity Survey At Mauna Loa Northeast Rift...  

Open Energy Info (EERE)

Details Location Mauna Loa Northeast Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes The vertical...

34

Watermark: Proposed Penalty (2011-SW-2908) | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Proposed Penalty (2011-SW-2908) Proposed Penalty (2011-SW-2908) Watermark: Proposed Penalty (2011-SW-2908) May 10, 2012 DOE alleged in a Notice of Proposed Civil Penalty that Watermark Designs, Ltd. manufactured and distributed noncompliant showerhead basic model SH-FAL90 in the U.S. Federal law subjects manufacturers and private labelers to civil penalties if those parties distribute in the U.S. products that do not meet applicable water conservation standards. This civil penalty notice advises the company of the potential penalties and DOE's administrative process, including the company's right to a hearing. Watermark: Proposed Penalty (2011-SW-2908) More Documents & Publications Watermark: Order (2011-SW-2908) Watermark: Noncompliance Determination (2011-SW-2908) ET Industries: Proposed Penalty (2012-SE-2902

35

NETL: 2010 SW PA Middle School Science Bowl  

NLE Websites -- All DOE Office Websites (Extended Search)

is open to middle school students (school, scouts, home school) from Southwestern Pennsylvania (SW PA). Complete eligibility requirements are located at the National...

36

Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical  

Open Energy Info (EERE)

Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical Characteristics And The Effects Of Gas On Well Performance Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical Characteristics And The Effects Of Gas On Well Performance Details Activities (0) Areas (0) Regions (0) Abstract: This study, which focuses on the Aluto-Langano geothermal field, is part of the ongoing investigations of the geothermal systems in the Ethiopian Rift Valley. Aluto-Langano is a water-dominated gas-rich geothermal field, with a maximum temperature close to 360°C, in the Lakes District region of the Ethiopian Rift Valley. The upflow zone for the system lies along a deep, young NNE trending fault and is characterized by

37

Aeromagnetic Survey At Hualalai Northwest Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Aeromagnetic Survey At Hualalai Northwest Rift Area Aeromagnetic Survey At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness useful DOE-funding Unknown Notes Aeromagnetic survey data for Hualalai (Godson et al., 1981) clearly indicate an elongate northwest to southeast trending zone of extremely low total magnetic field over the summit region of Hualalai that extends into the upper northwest rift zone. It is extremely unlikely that the summit region is underlain by intrusive material old enough (greater than 700,000 years of age) to have been emplaced during a period of reversed magnetic field; therefore, the only alternative explanation possible (presuming the data are accurate) is that this region is underlain by material with very

38

Development Overview of Geothermal Resources In Kilauea East Rift Zone |  

Open Energy Info (EERE)

Development Overview of Geothermal Resources In Kilauea East Rift Zone Development Overview of Geothermal Resources In Kilauea East Rift Zone Jump to: navigation, search OpenEI Reference LibraryAdd to library Report: Development Overview of Geothermal Resources In Kilauea East Rift Zone Abstract This study reviews the geothermal resources associatedwith the Kilauea East Rift Zone (KERZ) of Hawaii islandby focusing on a holistic development strategy for additionalgeothermal production. A review of existing literature inthe fields of geology, drilling, power production and policychallenges, highlights critical issues for geothermalenterprises. A geological assessment of the hydrology,geochemistry, and structural features that characterize theregion is discussed. Available data are interpreted includinggeology, geochemistry, well depth and temperature.

39

Geothermometry At Mauna Loa Northeast Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Geothermometry At Mauna Loa Northeast Rift Area (Thomas, 1986) Geothermometry At Mauna Loa Northeast Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Geothermometry At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Geothermometry Activity Date Usefulness useful DOE-funding Unknown Notes A reexamination of all groundwater sources in the Keaau area was undertaken in an effort to confirm the chemical and temperature anomalies that formed the primary basis on which the Keaau area was identified during the preliminary assessment survey. The data generated by this survey (Table 9) determined that all of the anomalous data present in the earlier data base were spurious and that the groundwater chemistry and temperatures in this

40

Mauna Loa Northeast Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Mauna Loa Northeast Rift Geothermal Area Mauna Loa Northeast Rift Geothermal Area (Redirected from Mauna Loa Northeast Rift Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Mauna Loa Northeast Rift Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (6) 10 References Area Overview Geothermal Area Profile Location: Hawaii Exploration Region: Hawaii Geothermal Region GEA Development Phase: 2008 USGS Resource Estimate Mean Reservoir Temp: Estimated Reservoir Volume: Mean Capacity: Click "Edit With Form" above to add content History and Infrastructure Operating Power Plants: 0

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


41

Thermal and mechanical development of the East African Rift System  

E-Print Network (OSTI)

The deep basins, uplifted flanks, and volcanoes of the Western and Kenya rift systems have developed along the western and eastern margins of the 1300 km-wide East African plateau. Structural patterns deduced from field, ...

Ebinger, Cynthia Joan

1988-01-01T23:59:59.000Z

42

Refraction Survey At Kilauea East Rift Area (Broyles, Et Al....  

Open Energy Info (EERE)

Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii, From Seismic And Gravity Data Retrieved from "http:en.openei.orgwindex.php?titleRefractionSurveyAtKila...

43

Zoe Industries: Noncompliance Determination (2011-SW-2912) | Department of  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Zoe Industries: Noncompliance Determination (2011-SW-2912) Zoe Industries: Noncompliance Determination (2011-SW-2912) Zoe Industries: Noncompliance Determination (2011-SW-2912) September 28, 2011 DOE issued a Notice of Noncompliance Determination to Zoe Industries, Inc. finding that Giessdorf 150043 model, a showerhead, does not comport with the water conservation standards. DOE determined the product was noncompliant based on DOE testing. Zoe must immediately notify each person (or company) to whom Zoe distributed the noncompliant products that the product does not meet Federal standards. In addition, Zoe must provide to DOE documents and records showing the number of units Zoe distributed and to whom. The manufacturer and/or private labeler of the product may be subject to civil penalties. Zoe Industries: Noncompliance Determination (2011-SW-2912)

44

SW(A)93-006 STATEMENT OF CONSIDERATIONS  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

SW(A)93-006 STATEMENT OF CONSIDERATIONS Request by Cummins Power Generation, Inc. for an Advance Waiver of Domestic and Foreign Patent Rights to Inventions made under the Dish...

45

Hudson-Reed: Noncompliance Determination (2011-SW-2909) | Department of  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Noncompliance Determination (2011-SW-2909) Noncompliance Determination (2011-SW-2909) Hudson-Reed: Noncompliance Determination (2011-SW-2909) September 28, 2011 DOE issued a Notice of Noncompliance Determination, finding that Hudson-Reed Limited's "HEAD16" showerhead does not meet the applicable water conservation standard. DOE determined the showerhead was noncompliant based on DOE testing. Hudson-Reed must immediately notify each person (or company) to whom Hudson-Reed distributed the noncompliant products that the product does not meet Federal standards. In addition, Hudson-Reed must provide to DOE documents and records showing the number of units Hudson-Reed distributed and to whom. The manufacturer and/or private labeler of the product may be subject to civil penalties. Hudson-Reed: Noncompliance Determination (2011-SW-2909)

46

An Integrated Geophysical Study Of The Northern Kenya Rift | Open Energy  

Open Energy Info (EERE)

Kenya Rift Kenya Rift Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: An Integrated Geophysical Study Of The Northern Kenya Rift Details Activities (0) Areas (0) Regions (0) Abstract: The Kenyan part of the East African rift is among the most studied rift zones in the world. It is characterized by: (1) a classic rift valley, (2) sheer escarpments along the faulted borders of the rift valley, (3) voluminous volcanics that flowed from faults and fissures along the rift, and (4) axial and flank volcanoes where magma flow was most intense. In northern Kenya, the rift faults formed in an area where the lithosphere was weakened and stretched by Cretaceous-Paleogene extension, and in central and southern Kenya, it formed along old zones of weakness at the

47

Field Studies of Geothermal Reservoirs Rio Grande Rift, New Mexico  

DOE Green Energy (OSTI)

The Rio Grande rift provides an excellent field laboratory to study the nature of geothermal systems in an extensional environment. Much of the geologic complexity that is found in the Basin and Range is absent because the rift is located on cratonic crust with a thin and well-characterized Phanerozoic stratigraphy and tectonic history. On the other hand, the Neogene thermo-tectonic history of the rift has many parallels with the Basin and Range to the west. The geology of the southern Rio Grande rift is among the best characterized of any rift system in the world. Also, most geologic maps for the region are rather unique in that detailed analyses of Quaternary stratigraphic and surficial unit are added in concert with the details of bedrock geology. Pleistocene to Holocene entrenchment of the Rio Grande and tributaries unroofs the alteration signatures and permeability attributes of paleo outflow plumes and upflow zones, associated with present-day, but hidden or ''blind,'' hydrothermal systems at Rincon and San Diego Mountain.

James C Witcher

2002-07-30T23:59:59.000Z

48

Aeromagnetic Survey At Mauna Loa Northeast Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Rift Area (Thomas, 1986) Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Aeromagnetic Survey At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness useful DOE-funding Unknown Notes Aeromagnetic data (Godson et al., 1981) for the lower northeast rift of Mauna Loa tend to substantiate this conclusion as well. The lower extension of the rift zone does not exhibit any significant magnetic features that would correspond to a thermal source within the inferred trace of the rift zone. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Aeromagnetic_Survey_At_Mauna_Loa_Northeast_Rift_Area_(Thomas,_1986)&oldid=40242

49

Patterson: Noncompliance Determination (2011-SW-2911) | Department of  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Patterson: Noncompliance Determination (2011-SW-2911) Patterson: Noncompliance Determination (2011-SW-2911) Patterson: Noncompliance Determination (2011-SW-2911) July 12, 2013 DOE issued a Notice of Noncompliance Determination to Dan Patterson finding that the "ThunderHead" showerhead basic model manufactured by ET Industries, Inc. and imported by Dan Patterson does not comport with the water conservation standards. DOE determined the product was noncompliant based on DOE testing. Patterson must immediately notify each person (or company) to whom Patterson distributed the noncompliant products that the product does not meet Federal standards. In addition, Patterson must provide to DOE documents and records showing the number of units Patterson distributed and to whom. The manufacturer and/or private labeler of the

50

Watermark: Noncompliance Determination (2011-SW-2908) | Department of  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Noncompliance Determination (2011-SW-2908) Noncompliance Determination (2011-SW-2908) Watermark: Noncompliance Determination (2011-SW-2908) September 26, 2011 DOE issued a Notice of Noncompliance Determination to Watermark Designs, Ltd. finding that model SH-FAL-90, a showerhead, does not comport with the water conservation standards. DOE determined the product was noncompliant based on DOE testing. Watermark Designs must immediately notify each person (or company) to whom Watermark Designs distributed the noncompliant products that the product does not meet Federal standards. In addition, Watermark Designs must provide to DOE documents and records showing the number of units Watermark Designs distributed and to whom. The manufacturer and/or private labeler of the product may be subject to civil

51

Sioux Valley SW Elec Coop | Open Energy Information  

Open Energy Info (EERE)

SW Elec Coop SW Elec Coop Jump to: navigation, search Name Sioux Valley SW Elec Coop Place Colman, South Dakota Utility Id 17267 Utility Location Yes Ownership C NERC Location MRO NERC MRO Yes Activity Distribution Yes References EIA Form EIA-861 Final Data File for 2010 - File1_a[1] SGIC[2] LinkedIn Connections CrunchBase Profile No CrunchBase profile. Create one now! This article is a stub. You can help OpenEI by expanding it. Sioux Valley Southwestern Electric Cooperative, Inc. Smart Grid Project was awarded $4,016,368 Recovery Act Funding with a total project value of $8,032,736. Utility Rate Schedules Grid-background.png commercial electric heat rate Commercial commercial general service - single phase Commercial commercial general service - three phase Commercial

52

Kilauea Southwest Rift And South Flank Geothermal Area | Open Energy  

Open Energy Info (EERE)

form form View source History View New Pages Recent Changes All Special Pages Semantic Search/Querying Get Involved Help Apps Datasets Community Login | Sign Up Search Page Edit with form History Facebook icon Twitter icon » Kilauea Southwest Rift And South Flank Geothermal Area (Redirected from Kilauea Southwest Rift And South Flank Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Kilauea Southwest Rift And South Flank Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (8) 10 References Area Overview Geothermal Area Profile Location: Hawaii

53

Magnetotellurics At Kilauea East Rift Area (Laney, 2005) | Open Energy  

Open Energy Info (EERE)

Magnetotellurics At Kilauea East Rift Area (Laney, Magnetotellurics At Kilauea East Rift Area (Laney, 2005) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Magnetotellurics Activity Date Usefulness not indicated DOE-funding Unknown Notes Magnetotelluric Imaging, G. Michael Hoversten. The project title derived from its inception. The project however moved from the application of MT on Kilauea in 2003 to the use of combined SP and conductivity mapping (MT) in 2004. The beginning of 2004 saw the completions of the Kilauea MT experiment by the acquisition of an additional 45 MT stations on Kilauea. We therefore decided to use the funds available to work at the Fort Bidwell Indian reservation where characterization work could be done at relatively low cost. We decided to perform a time lapse SP survey during a flow test

54

Kilauea Southwest Rift And South Flank Geothermal Area | Open Energy  

Open Energy Info (EERE)

Kilauea Southwest Rift And South Flank Geothermal Area Kilauea Southwest Rift And South Flank Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Kilauea Southwest Rift And South Flank Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (8) 10 References Area Overview Geothermal Area Profile Location: Hawaii Exploration Region: Hawaii Geothermal Region GEA Development Phase: 2008 USGS Resource Estimate Mean Reservoir Temp: Estimated Reservoir Volume: Mean Capacity: Click "Edit With Form" above to add content History and Infrastructure Operating Power Plants: 0 No geothermal plants listed.

55

Thermal Gradient Holes At Hualalai Northwest Rift Area (Thomas, 1986) |  

Open Energy Info (EERE)

Hualalai Northwest Rift Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Thermal Gradient Holes Activity Date Usefulness not useful DOE-funding Unknown Notes Although not part of the current effort, two deep (approximately 2000 m) exploratory wells were drilled on the north flank of Hualalai near Puu Waawaa cinder cone. The geophysical data used for siting these wells were proprietary and hence unavailable for publication; however, the temperatures measured at the bottoms of the wells were reported to be below 20degrees C. Chemical analysis of water samples taken from these wells did not provide useful geothermal data due to contamination of the well water with drilling muds References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

56

Mauna Loa Northeast Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Mauna Loa Northeast Rift Geothermal Area Mauna Loa Northeast Rift Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Mauna Loa Northeast Rift Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (6) 10 References Area Overview Geothermal Area Profile Location: Hawaii Exploration Region: Hawaii Geothermal Region GEA Development Phase: 2008 USGS Resource Estimate Mean Reservoir Temp: Estimated Reservoir Volume: Mean Capacity: Click "Edit With Form" above to add content History and Infrastructure Operating Power Plants: 0 No geothermal plants listed. Add a new Operating Power Plant

57

Mauna Loa Southwest Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Mauna Loa Southwest Rift Geothermal Area Mauna Loa Southwest Rift Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Mauna Loa Southwest Rift Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (2) 10 References Area Overview Geothermal Area Profile Location: Hawaii Exploration Region: Hawaii Geothermal Region GEA Development Phase: 2008 USGS Resource Estimate Mean Reservoir Temp: Estimated Reservoir Volume: Mean Capacity: Click "Edit With Form" above to add content History and Infrastructure Operating Power Plants: 0 No geothermal plants listed. Add a new Operating Power Plant

58

Hualalai Northwest Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Hualalai Northwest Rift Geothermal Area Hualalai Northwest Rift Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Hualalai Northwest Rift Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (9) 10 References Area Overview Geothermal Area Profile Location: Hawaii Exploration Region: Hawaii Geothermal Region GEA Development Phase: 2008 USGS Resource Estimate Mean Reservoir Temp: Estimated Reservoir Volume: Mean Capacity: Click "Edit With Form" above to add content History and Infrastructure Operating Power Plants: 0 No geothermal plants listed. Add a new Operating Power Plant

59

Intermittent upwelling of asthenosphere beneath the Gregory Rift, Kenya  

Science Conference Proceedings (OSTI)

K-Ar dates and chemical compositions of basalts in the Gregory Rift, Kenya, demonstrate marked secular variation of lava chemistry. Two magmatic cycles characterized by incompatible element relative depletion are recognized; both occurring immediately after the peak of basaltic volcanism and coeval with both trachyte/phonolite volcanism and domal uplift of the region. These cycles may be attributed to increasing degree of partial melting of mantle source material in association with thinning of the lithosphere by thermal erosion through contact with hot upwelling asthenospheric mantle. Cyclic variation in asthenosphere upwelling may be considered an important controlling process in the evolution of the Gregory Rift.

Tatsumi, Yoshiyuki (Univ. of Tasmania (Australia) Kyoto Univ. (Japan)); Kimura, Nobukazu (Kyoto Univ. (Japan)); Itaya, Tetsumaru (Okayama Univ. of Science (Japan)); Koyaguchi, Takehiro (Kumamoto Univ. (Japan)); Suwa, Kanenori (Nagoya Univ. (Japan))

1991-06-01T23:59:59.000Z

60

Direct-Current Resistivity Survey At Hualalai Northwest Rift Area (Thomas,  

Open Energy Info (EERE)

Hualalai Northwest Rift Area (Thomas, Hualalai Northwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes A total of seven Schlumberger soundings were performed on Hualalai. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Direct-Current_Resistivity_Survey_At_Hualalai_Northwest_Rift_Area_(Thomas,_1986)&oldid=510528" Category: Exploration Activities What links here Related changes

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


61

Kilauea East Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Kilauea East Rift Geothermal Area Kilauea East Rift Geothermal Area (Redirected from Kilauea East Rift Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Kilauea East Rift Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Heat Source 8 Geofluid Geochemistry 9 NEPA-Related Analyses (0) 10 Exploration Activities (28) 11 References Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"TERRAIN","zoom":6,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"500px","height":"300px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":19.47836,"lon":-154.8883,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

62

U.S. DEPARTMENT OF ENERGY 1000 Independence Ave, SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

1000 Independence Ave, SW 1000 Independence Ave, SW Washington, DC 20585 In the Matter of: ) Case Number: 2010-SE-2301 Leader Electronics Inc. ) NOTICE OF ALLOWANCE TO RESUME DISTRIBUTION Date issued : September 13, 2010 Manufacturers of certain covered products which have been determined by the Department of Energy (DOE) to be non-compliant with the applicable energy conservation standard may be allowed to resume distribution, per 10 CFR § 430.70 (a)(6)(v), if additional testing results supplied by the manufacturer results in a determination of compliance. On August 24, 2010, DOE issued a Notice of Non-Compliance Determination based on test results submitted by Leader Electronics showing that certain models were noncompliant. After an internal review, Leader Electronics determined that the original test results reported to DOE were incorrect.

63

SW(A)93-006 STATEMENT OF CONSIDERATIONS  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

SW(A)93-006 SW(A)93-006 STATEMENT OF CONSIDERATIONS Request by Cummins Power Generation, Inc. for an Advance Waiver of Domestic and Foreign Patent Rights to Inventions made under the Dish/Stirling Joint Venture Program between Sandia National Laboratories and Cummins Power Generation, Inc. in response to Contract No. 69-7763, DOE Docket No. W(A)93-006. The Petitioner, Cummins Power Generation (CPG), Inc., has requested a waiver of all domestic and foreign patent rights to inventions which it may conceive or first actually reduce to practice in the course of work under the Dish/Stirling Joint Venture Program between Petitioner and Sandia National Laboratories Contract No. 69-7763. Sandia National Laboratories is operated by Sandia Corporation for the U.S. Department of

64

File:Sw swppp guide.pdf | Open Energy Information  

Open Energy Info (EERE)

Sw swppp guide.pdf Sw swppp guide.pdf Jump to: navigation, search File File history File usage File:Sw swppp guide.pdf Size of this preview: 463 × 599 pixels. Other resolution: 464 × 600 pixels. Go to page 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 Go! next page → next page → Full resolution ‎(1,275 × 1,650 pixels, file size: 2.7 MB, MIME type: application/pdf, 50 pages) File history Click on a date/time to view the file as it appeared at that time. Date/Time Thumbnail Dimensions User Comment current 10:54, 13 November 2012 Thumbnail for version as of 10:54, 13 November 2012 1,275 × 1,650, 50 pages (2.7 MB) Dklein2012 (Talk | contribs) You cannot overwrite this file. Edit this file using an external application (See the setup

65

Magnetotellurics At Kilauea Southwest Rift And South Flank Area (Laney,  

Open Energy Info (EERE)

Laney, Laney, 2005) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Kilauea Southwest Rift And South Flank Area (Laney, 2005) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Magnetotellurics Activity Date Usefulness not indicated DOE-funding Unknown Notes Magnetotelluric Imaging, G. Michael Hoversten. The project title derived from its inception. The project however moved from the application of MT on Kilauea in 2003 to the use of combined SP and conductivity mapping (MT) in 2004. The beginning of 2004 saw the completions of the Kilauea MT experiment by the acquisition of an additional 45 MT stations on Kilauea. We therefore decided to use the funds available to work at the Fort Bidwell

66

Direct-Current Resistivity At Kilauea Southwest Rift And South Flank Area  

Open Energy Info (EERE)

Direct-Current Resistivity At Kilauea Southwest Rift And South Flank Area Direct-Current Resistivity At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes The electrical resistivity data acquired on the southwest rift delineated two distinct basement resistivity structures northwest of the rift zone: a high-resistivity basement at approximately 60 m a.s.l, and located north of a prehistoric fissure, and a low-resistivity deep basement (20 m a.s.1.) to the south and east of this fissure (Figs 48, 49). These data suggest that a

67

Ground Magnetics At Kilauea East Rift Area (Leslie, Et Al., 2004) | Open  

Open Energy Info (EERE)

Ground Magnetics At Kilauea East Rift Area (Leslie, Et Al., 2004) Ground Magnetics At Kilauea East Rift Area (Leslie, Et Al., 2004) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Ground Magnetics At Kilauea East Rift Area (Leslie, Et Al., 2004) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Ground Magnetics Activity Date Usefulness useful DOE-funding Unknown Notes Paper states "magnetic data" - no further clarification regarding type of magnetic survey. References Stephen C. Leslie, Gregory F. Moore, Julia K. Morgan (2004) Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone Of Kilauea Volcano, Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Ground_Magnetics_At_Kilauea_East_Rift_Area_(Leslie,_Et_Al.,_2004)&oldid=390100"

68

Self Potential At Mauna Loa Southwest Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Southwest Rift Area (Thomas, 1986) Southwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Self Potential At Mauna Loa Southwest Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Southwest Rift Area Exploration Technique Self Potential Activity Date Usefulness not indicated DOE-funding Unknown Notes Field surveys in the South Point area were limited to a series of Schlumberger soundings and a self-potential traverse across the rift zone. The absence of groundwater wells and time and funding constraints precluded any geochemical field surveys. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Self_Potential_At_Mauna_Loa_Southwest_Rift_Area_(Thomas,_1986)&oldid=389751

69

A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano,  

Open Energy Info (EERE)

A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, Hawaii Jump to: navigation, search OpenEI Reference LibraryAdd to library == A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, HawaiiThesis/Dissertation == Author Catherine King Skokan Organization Colorado School of Mines Published Publisher Not Provided, 1974 DOI Not Provided Check for DOI availability: http://crossref.org Online Internet link for A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, Hawaii Citation [[Citation::Catherine King Skokan. 1974. A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, Hawaii []. [ (!) ]: Colorado School of Mines.]] Retrieved from "http://en.openei.org/w/index.php?title=A_Time-Domain_Electromagnetic_Survey_of_the_East_Rift_Zone_Kilauea_Volcano,_Hawaii&oldid=682585"

70

Field Mapping At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Field Mapping At Kilauea East Rift Area (Thomas, Field Mapping At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Field Mapping Activity Date Usefulness useful DOE-funding Unknown Notes Geologic mapping on the East Rift Zone (ERZ) conducted by Peterson (1967), J. Moore (1971), and Wright and Fiske (1971) detailed historic lava flows originating in the ERZ and developed structural models of the rift based on the locations and progressions of recorded eruptive cycles. These studies have more recently been expanded by Holcomb (1980, 1981) and R. Moore (1982, 1983) who have presented more detailed mapping of all surface flows (historic and prehistoric), fissures and faulting on the eastern flank of the Kilauea shield. The model developed from these studies is of a rift

71

Refraction Survey At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Kilauea East Rift Area (Thomas, 1986) Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Refraction Survey At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Refraction Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Seismic refraction surveys conducted by Broyles and Furumoto (1978) and Suyenaga et al. (1978) developed a cross-sectional model of the rift zone near the present site of HGP-A that proposed a 12- 17 km wide dike complex lying at a depth of 2 to 3 km (Fig. 51). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Refraction_Survey_At_Kilauea_East_Rift_Area_(Thomas,_1986)&oldid=386690"

72

Direct-Current Resistivity Survey At Kilauea Southwest Rift And South Flank  

Open Energy Info (EERE)

Direct-Current Resistivity Survey At Kilauea Southwest Rift And South Flank Direct-Current Resistivity Survey At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes The electrical resistivity data acquired on the southwest rift delineated two distinct basement resistivity structures northwest of the rift zone: a high-resistivity basement at approximately 60 m a.s.l, and located north of a prehistoric fissure, and a low-resistivity deep basement (20 m a.s.1.) to

73

A geochemical model of the Kilauea east rift zone | Open Energy Information  

Open Energy Info (EERE)

A geochemical model of the Kilauea east rift zone A geochemical model of the Kilauea east rift zone Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: A geochemical model of the Kilauea east rift zone Abstract N/A Author Donald Thomas Published Journal US Geological Survey Professional Paper 1350, 1987 DOI Not Provided Check for DOI availability: http://crossref.org Online Internet link for A geochemical model of the Kilauea east rift zone Citation Donald Thomas. 1987. A geochemical model of the Kilauea east rift zone. US Geological Survey Professional Paper 1350. (!) . Retrieved from "http://en.openei.org/w/index.php?title=A_geochemical_model_of_the_Kilauea_east_rift_zone&oldid=682589" Categories: Missing Required Information References Uncited References Geothermal References

74

Haleakala Volcano Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Well Field Information Development Area: Number of Production Wells: Number of Injection Wells: Number of Replacement Wells: Average Temperature of Geofluid: Sanyal...

75

Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii...  

Open Energy Info (EERE)

a complex of dikes containing solidified magma from past volcanic eruptions that provide energy for the hydrothermal processes associated with the rift zone. Analysis of gravity...

76

Ground Gravity Survey At Kilauea East Rift Area (Leslie, Et Al...  

Open Energy Info (EERE)

to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Ground Gravity Survey At Kilauea East Rift Area (Leslie, Et Al., 2004) Exploration Activity Details...

77

Forrestal Building, 1000 Independence Avenue, S.W.,  

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

THURSDAY, THURSDAY, APRIL 3, 2003 + + + + + The Committee met in Room 8E089 in the Forrestal Building, 1000 Independence Avenue, S.W., Washington, D.C., at 8:30 a.m., Jay Breidt, Chair, presiding. PRESENT: F. JAY BREIDT Chair MARK BERNSTEIN Committee Member JOHNNY BLAIR Committee Member JAE EDMONDS Committee Member MOSHE FEDER Committee Member JAMES K. HAMMITT Committee Member NEHA KHANNA Committee Member WILLIAM G. MOSS Committee Member NAGARAJ K. NEERCHAL Committee Member POLLY A. PHIPPS Committee Member RANDY R. SITTER Committee Member ALSO PRESENT: GUY CARUSO Administrator, Energy Information Administration HOWARD GRUENSPECHT Deputy Administrator, EIA BILL WEINIG EIA CALVIN KENT Invited Guest CRYSTAL LINKLETTER Invited Guest

78

Microsoft Word - Appendix C SW Samples.doc  

Office of Legacy Management (LM)

Analytical Results for Surface Water Samples, Analytical Results for Surface Water Samples, January 2000 through April 2011 This page intentionally left blank Upstream -- SW00-01 a _______________________________________________________________________________________________________________________________________________ Analyte Unit 04/18/00 07/17/00 10/20/00 04/17/01 07/11/01 10/09/01 04/07/05 10/05/05 04/28/06 10/02/06 04/11/07 10/08/07 04/09/08 g _______________________________________________________________________________________________________________________________________________ Field Measurements Alkalinity c mg/L -- -- -- -- -- -- -- -- -- -- -- -- -- Alkalinity b mg/L 196 130 263 218 196 98 145 202 228 183 227 186 213

79

Basinfill of The Permian Tanqua depocentre, SW Karoo basin, South Africa.  

E-Print Network (OSTI)

??ENGLISH ABSTRACT: Basin subsidence analysis, employing the backstripping method, indicates that fundamentally two different basin-generating mechanisms controlled Tanqua depocentre development in SW Karoo Basin. The (more)

Alao, Abosede Olubukunola

2012-01-01T23:59:59.000Z

80

Mercury Vapor At Mauna Loa Northeast Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mauna Loa Northeast Rift Area (Thomas, 1986) Mauna Loa Northeast Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Mercury Vapor Activity Date Usefulness not indicated DOE-funding Unknown Notes Soil mercury and radon emanometry sampling conducted in the Keaau prospect were similarly unable to define any anomalies that could reasonably be interpreted to be due to subsurface thermal effects. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Mercury_Vapor_At_Mauna_Loa_Northeast_Rift_Area_(Thomas,_1986)&oldid=390060

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


81

Mercury Vapor At Hualalai Northwest Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mercury Vapor At Hualalai Northwest Rift Area (Thomas, 1986) Mercury Vapor At Hualalai Northwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Mercury Vapor Activity Date Usefulness not indicated DOE-funding Unknown Notes The Hualalai lower northwest rift and southern flank were sampled for soil mercury concentration and radon emanation rates (Cox and Cuff, 1981d). The data generated by these surveys yielded complex patterns of mercury concentrations and radon emanation rates that generally did not show coincident anomalies (Figs 42, 43). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

82

Isotopic Analysis At Kilauea East Rift Area (Quane, Et Al., 2000) | Open  

Open Energy Info (EERE)

source source History View New Pages Recent Changes All Special Pages Semantic Search/Querying Get Involved Help Apps Datasets Community Login | Sign Up Search Page Edit History Facebook icon Twitter icon » Isotopic Analysis At Kilauea East Rift Area (Quane, Et Al., 2000) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Isotopic Analysis- Rock At Kilauea East Rift Area (Quane, Et Al., 2000) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Isotopic Analysis- Rock Activity Date Usefulness not indicated DOE-funding Unknown References S. L. Quane, M. O. Garcia, H. Guillou, T. P. Hulsebosch (2000) Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Drill Core From Soh 1 Retrieved from "http://en.openei.org/w/index.php?title=Isotopic_Analysis_At_Kilauea_East_Rift_Area_(Quane,_Et_Al.,_2000)&oldid=687735"

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Thermal Gradient Holes At Kilauea East Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Thermal Gradient Holes At Kilauea East Rift Area (Thomas, 1986) Thermal Gradient Holes At Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Thermal Gradient Holes At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Thermal Gradient Holes Activity Date Usefulness useful DOE-funding Unknown Notes Two separate phases of geothermal exploratory drilling have occurred on the lower East Rift. The first was essentially a wildcat venture with relatively little surface exploratory data having been gathered, whereas the second was initiated after somewhat more geoscience information had been acquired under the Hawaii Geothermal Project. The results of the successful exploratory drilling program on the Kilauea

84

Ground Gravity Survey At Rio Grande Rift Region (Aiken & Ander, 1981) |  

Open Energy Info (EERE)

Rio Grande Rift Region (Aiken & Ander, 1981) Rio Grande Rift Region (Aiken & Ander, 1981) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Ground Gravity Survey At Rio Grande Rift Region (Aiken & Ander, 1981) Exploration Activity Details Location Rio Grande Rift Geothermal Region Exploration Technique Ground Gravity Survey Activity Date Usefulness useful DOE-funding Unknown References Carlos L.V. Aiken, Mark E. Ander (1981) A Regional Strategy For Geothermal Exploration With Emphasis On Gravity And Magnetotellurics Retrieved from "http://en.openei.org/w/index.php?title=Ground_Gravity_Survey_At_Rio_Grande_Rift_Region_(Aiken_%26_Ander,_1981)&oldid=401473" Category: Exploration Activities What links here Related changes Special pages Printable version

85

Gas Flux Sampling At Mauna Loa Northeast Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Gas Flux Sampling At Mauna Loa Northeast Rift Area (Thomas, 1986) Gas Flux Sampling At Mauna Loa Northeast Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Gas Flux Sampling Activity Date Usefulness not indicated DOE-funding Unknown Notes Soil mercury and radon emanometry sampling conducted in the Keaau prospect were similarly unable to define any anomalies that could reasonably be interpreted to be due to subsurface thermal effects. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Gas_Flux_Sampling_At_Mauna_Loa_Northeast_Rift_Area_(Thomas,_1986)&oldid=389039"

86

Time-Domain Electromagnetics At Kilauea Southwest Rift And South Flank Area  

Open Energy Info (EERE)

And South Flank Area And South Flank Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Time-Domain Electromagnetics At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Time-Domain Electromagnetics Activity Date Usefulness useful DOE-funding Unknown Notes The assessment effort consisted of a reexamination of existing Schlumberger sounding (Hussong and Cox, 1967; Adams et al., 1970) and time-domain electromagnetic (Klein and Kauahikaua, 1975) data for the rift area (Kauahikaua and Mattice, 1981) The electrical resistivity data acquired on the southwest rift delineated two distinct basement resistivity structures northwest of the rift zone: a high-resistivity basement at approximately 60

87

Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano,  

Open Energy Info (EERE)

Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, Hawaii Jump to: navigation, search OpenEI Reference LibraryAdd to library : Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, HawaiiInfo Graphic/Map/Chart Authors Frank A. Trusdell and Richard B. Moore Published U.S. GEOLOGICAL SURVEY, 2006 DOI Not Provided Check for DOI availability: http://crossref.org Online Internet link for Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, Hawaii Citation Frank A. Trusdell,Richard B. Moore. Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, Hawaii. []. Place of publication not provided. U.S. GEOLOGICAL SURVEY. 2006. Available from: http://pubs.usgs.gov/imap/2614/downloads/pdf/2614map_508.pdf.

88

Direct-Current Resistivity At Kilauea East Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Kilauea East Rift Area (Thomas, 1986) Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes Electrical resistivity studies performed on the Kilauea East Rift Zone have employed a variety of techniques. Bipole mapping was conducted by Keller et al. (1977a) as part of the Hawaii Geothermal Project (HGP) geoscience program and was able to provide data on the regional resistivity structure of the summit and eastern flank of Kilauea. The model developed indicated several different types of resistivity sections depending on the location

89

Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone  

Open Energy Info (EERE)

Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone Of Kilauea Volcano, Hawaii Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone Of Kilauea Volcano, Hawaii Details Activities (3) Areas (1) Regions (0) Abstract: Multichannel seismic reflection, sonobuoy, gravity and magnetics data collected over the submarine length of the 75 km long Puna Ridge, Hawaii, resolve the internal structure of the active rift zone. Laterally continuous reflections are imaged deep beneath the axis of the East Rift Zone (ERZ) of Kilauea Volcano. We interpret these reflections as a layer of abyssal sediments lying beneath the volcanic edifice of Kilauea. Early

90

Gas Flux Sampling At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

source source History View New Pages Recent Changes All Special Pages Semantic Search/Querying Get Involved Help Apps Datasets Community Login | Sign Up Search Page Edit History Facebook icon Twitter icon » Gas Flux Sampling At Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Gas Flux Sampling Activity Date Usefulness not indicated DOE-funding Unknown Notes Radon emanometry data for the same locality (Fig. 61) (Cox, 1980) similarly presented a complicated pattern of radon outgassing along the lower rift zone. Even though complexities are present within the rift zone, there

91

Direct-Current Resistivity Survey At Kilauea East Rift Area (Thomas, 1986)  

Open Energy Info (EERE)

Kilauea East Rift Area (Thomas, 1986) Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes Electrical resistivity studies performed on the Kilauea East Rift Zone have employed a variety of techniques. Bipole mapping was conducted by Keller et al. (1977a) as part of the Hawaii Geothermal Project (HGP) geoscience program and was able to provide data on the regional resistivity structure of the summit and eastern flank of Kilauea. The model developed indicated several different types of resistivity sections depending on the location

92

Aeromagnetic Survey At Kilauea Southwest Rift And South Flank Area (Thomas,  

Open Energy Info (EERE)

Thomas, Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Aeromagnetic Survey At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness useful DOE-funding Unknown Notes Aeromagnetic data (Godson et al., 1981) for the southwest rift appears to substantiate the presence of a thermal resource; there is a marked bipolar magnetic anomaly paralleling the rift zone from the summit to the lower rift near the coast suggesting either that intense hydrothermal alteration has occurred or that subsurface temperatures exceed the Curie temperature. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

93

Mercury Vapor At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mercury Vapor At Kilauea East Rift Area (Thomas, Mercury Vapor At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Mercury Vapor Activity Date Usefulness not indicated DOE-funding Unknown Notes The sampling network for soil mercury concentrations undertaken by Cox (1981) identified a complicated pattern of mercury concentrations throughout the lower Puna area (Fig. 60). The highest soil mercury concentrations found were generally located within the rift zone, but an analysis of the data showed that soil type and soil pH also had a marked impact on mercury concentration. Making corrections for these effects improved the correspondence between the surface geological expression of the rift zone and the mercury concentrations observed; interpretation of

94

Ground Gravity Survey At Kilauea East Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Ground Gravity Survey At Kilauea East Rift Area Ground Gravity Survey At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Ground Gravity Survey Activity Date Usefulness useful DOE-funding Unknown Notes This model was later expanded through the examination of detailed and regional gravity data (Krivoy and Eaton, 1961) and regional aeromagnetic data (Malahoff and Woollard, 1966) to a three-dimensional map of the rift zone (Furumoto, 1978b). This model projected a dike complex (presumably at high temperatures) which has a width of approximately 20 km near the summit of Kilauea that narrows to approximately 12 km at the lower quarter of the subaerial portion of the rift (Fig. 52). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

95

Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii, From  

Open Energy Info (EERE)

Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii, From Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii, From Seismic And Gravity Data Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii, From Seismic And Gravity Data Details Activities (2) Areas (1) Regions (0) Abstract: Two seismic refraction surveys were carried out in 1976 and 1977 on the east rift zone of Kilauea volcano as part of an exploratory program for geothermal resources. The short traverse seismic refraction survey of January 1976 delineated the upper surface structure of the east rift, revealing velocities of 2.5 km/s under the Kalapana line and 3.1 km/s under the Leilani line beneath a surface layer of low, but variable velocity. This survey was not successful in determining the depth of the

96

Gas Flux Sampling At Hualalai Northwest Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Hualalai Northwest Rift Area (Thomas, 1986) Hualalai Northwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Gas Flux Sampling Activity Date Usefulness not indicated DOE-funding Unknown Notes The Hualalai lower northwest rift and southern flank were sampled for soil mercury concentration and radon emanation rates (Cox and Cuff, 1981d). The data generated by these surveys yielded complex patterns of mercury concentrations and radon emanation rates that generally did not show coincident anomalies (Figs 42, 43). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

97

Self Potential At Hualalai Northwest Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Self Potential At Hualalai Northwest Rift Area (Thomas, 1986) Self Potential At Hualalai Northwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Self Potential At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Self Potential Activity Date Usefulness not indicated DOE-funding Unknown Notes Self-potential surveys conducted over the summit and flank of Hualalai (Jackson and Sako, 1982; D. B. Jackson, pers. commun., 1983) indicate an elongate self-potential anomaly extending across the summit and down the northwest rift to Kaupulehu Crater. The positively polarized anomaly extends over an area of approximately 6 km 2 and has been interpreted to be the result of one or more buried high-temperature intrusive bodies (Jackson

98

Kilauea East Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Page Page Edit with form History Facebook icon Twitter icon » Kilauea East Rift Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Kilauea East Rift Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Heat Source 8 Geofluid Geochemistry 9 NEPA-Related Analyses (0) 10 Exploration Activities (28) 11 References Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"TERRAIN","zoom":6,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"500px","height":"300px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":19.47836,"lon":-154.8883,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

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U.S. Department of Energy 1000 Independence Ave., SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

3, 2009 3, 2009 18809.03YK Submitted electronically to GC-62@hq.doe.gov Office of the Assistant General Counsel for Technology Transfer U.S. Department of Energy 1000 Independence Ave., SW Washington, DC 20585 Dear Mr. Gottlieb, Subject: Notice of Inquiry: Technology Transfer Practices at Department of Energy Laboratories (75 FR 72036) We are pleased to respond to the questions published in the Federal Register. The Lawrence Livermore National Laboratory (LLNL) is committed to DOE's mission to improve the Nation's global competitive posture and believes that the Lab's ability to partner and collaborate with industry, universities and others around the globe is key to achieving that goal. As Secretary Chu expressed in his statement to the Committee on

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Mary's River SW Geothermal Project | Open Energy Information  

Open Energy Info (EERE)

Geothermal Project Geothermal Project Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Development Project: Mary's River SW Geothermal Project Project Location Information Coordinates 41.750555555556°, -115.30194444444° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":41.750555555556,"lon":-115.30194444444,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

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101

U.S. Department of Energy 1000 Independence Ave, SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

U.S. Department of Energy 1000 Independence Ave, SW Washington, DC 20585 In the Matter of: Fuzhou Sunlight Lighting Electrical Appliance Co., Ltd. ) ) ) ) Case Number: 2010-SE-1402 NOTICE OF NONCOMPLIANCE DETERMINATION CERTIFICATION Manufacturers of certain covered products are required to certify compliance with the applicable energy conservation standards through submission of a compliance statement and a certification report. 10 CFR § 430.62. See 42 U.S.C. 6296. On June 4, 2010, Westinghouse provided to DOE copies of NVLAP test reports for a variety of models of incandescent reflector lamps. Westinghouse also provided a spreadsheet summarizing the information from the test reports. In relevant part, the spreadsheet (and test reports) details the following information:

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NETL: 2010 SW PA High School Science Bowl  

NLE Websites -- All DOE Office Websites (Extended Search)

High School Science Bowl High School Science Bowl The U.S. Department of Energy's National Energy Technology Laboratory (DOE/NETL), and the Community College of Allegheny County (CCAC), South Campus, would like to invite you to participate in one of the premier scientific events for high school students, the Southwestern Pennsylvania High School Science Bowl 2010 on February 20, 2010. This will be NETL's 19th year sponsoring the high school competition. There is a change this year in the registration process from past years, all teams who are registering to complete, must do so through the National Science Bowl website by January 7, 2010. For those who are not familiar with the Science Bowl here are some highlights: The competition is open to high school students (school, scouts, home school) from Southwestern Pennsylvania (SW PA). Complete eligibility requirements are located at the National Science Bowl website.

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K.Grill: Proposed Penalty (2011-SW-2902) | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

K.Grill: Proposed Penalty (2011-SW-2902) K.Grill: Proposed Penalty (2011-SW-2902) K.Grill: Proposed Penalty (2011-SW-2902) June 10, 2011 DOE alleged in a Notice of Proposed Civil Penalty that Kenneth Grill manufactured and distributed noncompliant showerheads in the U.S. Federal law subjects manufacturers and private labelers to civil penalties if those parties distribute in the U.S. products that do not meet applicable water conservation standards. This civil penalty notice advises the company of the potential penalties and DOE's administrative process, including the company's right to a hearing. K.Grill: Proposed Penalty (2011-SW-2902) More Documents & Publications K.Grill: Order (2011-SW-2902) Mackle Company: Proposed Penalty (2010-SE-0106) Nationwide Industries: Proposed Penalty (2011-CW-2803

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A Cell-Integrated Semi-Lagrangian Semi-Implicit Shallow-Water Model (CSLAM-SW) with Conservative and Consistent Transport  

Science Conference Proceedings (OSTI)

A Cartesian semi-implicit solver using the Conservative Semi-Lagrangian Multitracer (CSLAM) transport scheme is constructed and tested for shallow-water (SW) flows. The SW equations solver (CSLAM-SW) uses a discrete semi-implicit continuity ...

May Wong; William C. Skamarock; Peter H. Lauritzen; Roland B. Stull

2013-07-01T23:59:59.000Z

105

Compound and Elemental Analysis At Kilauea Southwest Rift And South Flank  

Open Energy Info (EERE)

Flank Flank Area (Coombs, Et Al., 2006) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Compound and Elemental Analysis At Kilauea Southwest Rift And South Flank Area (Coombs, Et Al., 2006) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Compound and Elemental Analysis Activity Date Usefulness not indicated DOE-funding Unknown References Michelle L. Coombs, Thomas W. Sisson, Peter W. Lipman (2006) Growth History Of Kilauea Inferred From Volatile Concentrations In Submarine-Collected Basalts Retrieved from "http://en.openei.org/w/index.php?title=Compound_and_Elemental_Analysis_At_Kilauea_Southwest_Rift_And_South_Flank_Area_(Coombs,_Et_Al.,_2006)&oldid=510423"

106

Data Acquisition-Manipulation At Rio Grande Rift Region (Morgan, Et Al.,  

Open Energy Info (EERE)

Morgan, Et Al., Morgan, Et Al., 2010) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Data Acquisition-Manipulation At Rio Grande Rift Region (Morgan, Et Al., 2010) Exploration Activity Details Location Rio Grande Rift Geothermal Region Exploration Technique Data Acquisition-Manipulation Activity Date Usefulness useful regional reconnaissance DOE-funding Unknown Notes San Luis Basin (south-central CO) regional study. References Paul Morgan, Peter Barkmann, Charles Kluth, Matthew Sares (2010) Prospects For Electricity Generation In The San Luis Basin, Colorado, Usa Retrieved from "http://en.openei.org/w/index.php?title=Data_Acquisition-Manipulation_At_Rio_Grande_Rift_Region_(Morgan,_Et_Al.,_2010)&oldid=401472" Category: Exploration

107

History and Results of Surface Exploration in the Kilauea East Rift Zone |  

Open Energy Info (EERE)

History and Results of Surface Exploration in the Kilauea East Rift Zone History and Results of Surface Exploration in the Kilauea East Rift Zone Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Paper: History and Results of Surface Exploration in the Kilauea East Rift Zone Abstract Government-funded surveys of the Kilauea East Rift Zone have resulted in a wealth of geophysical and geochemical data from an active volcanic area. All data are clearly of academic interest; Hawaii was used as a testing ground for various geophysical methods in the early days of geothermal exploration. Some surveys, such as gravity and magnetic, are useful a regional perspective for determining broad structural trends and grossly identifying magmatic intrusions. Seismic data are currently being used for a more sitespecific purpose: to determine fault locations and geometries.

108

Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And South Flank  

Open Energy Info (EERE)

Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And South Flank Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And South Flank Area (Wyss, Et Al., 2001) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And South Flank Area (Wyss, Et Al., 2001) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Teleseismic-Seismic Monitoring Activity Date Usefulness could be useful with more improvements DOE-funding Unknown Notes In spite of the complications discovered in this b-value analysis of Kilauea's South Flank, there are many similarities with the case histories of the other volcanoes we have studied, and the correlation of high b-value anomalies withmagma reservoirs is confirmed.

109

Self Potential At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Self Potential At Kilauea East Rift Area (Thomas, Self Potential At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Self Potential Activity Date Usefulness useful DOE-funding Unknown Notes An extensive network of self-potential surveys have been performed over the summit and flanks of Kilauea as part of the HGP exploration surveys and in separate studies of the source mechanism for the potential anomalies observed (Zablocki, 1976, 1977). The geothermal exploration surveys were performed primarily on the lower East Rift Zone and identified four separate self-potential anomalies (Fig. 59) (Zablocki, 1977). The source mechanism for the anomalies observed was inferred to be the result of electrokinetic phenomena; thermal groundwater escaping from a geothermal

110

Micro-Earthquake At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Micro-Earthquake At Kilauea East Rift Area (Thomas, Micro-Earthquake At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Micro-Earthquake Activity Date Usefulness not indicated DOE-funding Unknown Notes Microseismic and ground noise studies were performed along the East Rift Zone in an effort to identify areas in which earthquake activity might suggest rock fracturing as a result of cold water coming into contact with heated reservoir rocks (Furumoto, 1978a). One of the microseismic surveys utilized an array of seven seismometers to monitor earthquake activity in the vicinity of the then proposed site of the HGP-A well (Fig. 53) (Suyenaga and Furumoto, 1978). The second microearthquake study utilized only two seismometers located near the junction of the Pahoa-Kalapana and

111

Water Sampling At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Water Sampling At Kilauea East Rift Area (Thomas, Water Sampling At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Water Sampling Activity Date Usefulness useful DOE-funding Unknown Notes Studies of groundwater and coastal spring- sources that have identified thermal fluids on the lower East Rift Zone date back to the early part of this century (Guppy, 1906). More recent investigations of temperature and groundwater chemistry were performed for the HGP geoscience program (Macdonald, 1977; McMurtry et al., 1977; Epp and Halunen, 1979). Epp and Halunen (1979) identified several warm water wells, one having a temperature in excess of 90degrees C, and coastal springs in lower Puna; temperature profiles obtained by this study indicated that in some

112

Geoelectric Studies on the East Rift, Kilauea Volcano, Hawaii Island | Open  

Open Energy Info (EERE)

Geoelectric Studies on the East Rift, Kilauea Volcano, Hawaii Island Geoelectric Studies on the East Rift, Kilauea Volcano, Hawaii Island Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: Geoelectric Studies on the East Rift, Kilauea Volcano, Hawaii Island Abstract Three geophysical research organizations, working together under the auspices of the Hawaii Geothermal Project, have used several electrical and electromagnetic exploration techniques on Kilauea volcano, Hawaii to assess its geothermal resources. This volume contains four papers detailing their methods and conclusions. Keller et al. of the Colorado School of Mines used the dipole mapping and time-domain EM sounding techniques to define low resistivity areas around the summit and flanks of Kilauea. Kauahikaua and Klein of the Hawaii Institute of Geophysics then detailed the East Rift

113

Time-Domain Electromagnetics At Kilauea East Rift Area (Thomas, 1986) |  

Open Energy Info (EERE)

Time-Domain Electromagnetics At Kilauea East Rift Time-Domain Electromagnetics At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Time-Domain Electromagnetics Activity Date Usefulness useful DOE-funding Unknown Notes A series of time-domain electromagnetic (TDEM) soundings were also performed in the lower East Rift Zone as part of the HGP exploration program (Klein and Kauahikaua, 1975; Kauahikaua and Klein, 1977); this work was recently expanded to include additional TDEM and vertical electrical soundings, and the entire data set was reinterpreted (Kauahikaua, 1981b; Kauahikaua and Mattice, 1981). The resistivity model presented by Kauahikaua (1981b) suggests that moderate to high basement resistivities, corresponding to cold freshwater saturated basalts, are present north of

114

Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On  

Open Energy Info (EERE)

Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Drill Core From Soh 1 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Drill Core From Soh 1 Details Activities (4) Areas (1) Regions (0) Abstract: Deep drilling has allowed for the first time an examination of most of the shield stage of a Hawaiian volcano when it is centered over the hotspot and most of its volume is produced. We determined the lithologies, ages, geochemical characteristics and accumulation rates of rocks from the continuously cored, ~1.7 km deep Scientific Observation Hole (SOH) 1, which was drilled into Kilauea's East Rift Zone. The uppermost ~750 m of this hole contain relatively unaltered subaerially quenched lavas; the lower

115

Static Temperature Survey At Kilauea East Rift Area (Rudman & Epp, 1983) |  

Open Energy Info (EERE)

Static Temperature Survey At Kilauea East Rift Area (Rudman & Epp, 1983) Static Temperature Survey At Kilauea East Rift Area (Rudman & Epp, 1983) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Static Temperature Survey At Kilauea East Rift Area (Rudman & Epp, 1983) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Static Temperature Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Drilling of HGP-A was completed on April 28, 1976. An equilibrium temperature was not measured in HGP-A; the well was flashed before the drilling disturbance was dissipated. However, before the mud was pumped out, temperatures in the well were measured at 15, 75, 97,145, and 193 hours, and at 13, 21, and 22 days after circulation of the drilling mud stopped. These temperature data are shown in Fig. 2. Between 305 m and 914

116

Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii...  

Open Energy Info (EERE)

Page Edit with form History Facebook icon Twitter icon Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Drill Core From Soh 1 Jump to: navigation,...

117

A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea...  

Open Energy Info (EERE)

1974 DOI Not Provided Check for DOI availability: http:crossref.org Online Internet link for A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano,...

118

Direct-Current Resistivity Survey At Mauna Loa Southwest Rift Area (Thomas,  

Open Energy Info (EERE)

Area (Thomas, Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Mauna Loa Southwest Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Southwest Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Field surveys in the South Point area were limited to a series of Schlumberger soundings and a self-potential traverse across the rift zone. The absence of groundwater wells and time and funding constraints precluded any geochemical field surveys. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Direct-Current_Resistivity_Survey_At_Mauna_Loa_Southwest_Rift_Area_(Thomas,_1986)&oldid=510541"

119

Microsoft Word - RFLMA CR 2010-06 Monitoring Results at SW027 Final.doc  

Office of Legacy Management (LM)

Report of Steps Taken Regarding Monitoring Results at Surface Water Report of Steps Taken Regarding Monitoring Results at Surface Water Point of Evaluation (POE) SW027 and Contact Record 2010-06 This page intentionally left blank 1 of 16 Report of Steps Taken Regarding Monitoring Results at Surface Water Point of Evaluation (POE) SW027 August 31, 2010 Introduction Surface water location SW027 is the Rocky Flats Legacy Management Agreement (RFLMA) POE at the eastern (downstream) end of the South Interceptor Ditch (SID), upstream of Pond C-2. The plutonium-239/240 (Pu) concentration measured at SW027 in samples collected through April 27, 2010, indicated that the 12-month rolling average of data from this monitoring point for the full month of April 2010 would likely exceed the RFLMA surface water standard when the

120

Sediment infill within rift basins: Facies distribution and effects of deformation: Examples from the Kenya and Tanganyika Rifts, East Africa  

SciTech Connect

Oil is known from lacustrine basins of the east African rift. The geology of such basins is complex and different depending on location in the eastern and western branches. The western branch has little volcanism, leading to long-lived basins, such as Lake Tanganyika, whereas a large quantity of volcanics results in the eastern branch characterized by ephemeral basins, as the Baringo-Bogoria basin in Kenya. The Baringo-Bogoria basin is a north-south half graben formed in the middle Pleistocene and presently occupied by the hypersaline Lake Bogoria and the freshwater Lake Baringo. Lake Bogoria is fed by hot springs and ephemeral streams controlled by grid faults bounding the basin to the west. The sedimentary fill is formed by cycles of organic oozes having a good petroleum potential and evaporites. On the other hand, and as a consequence of the grid faults, Lake Baringo is fed by permanent streams bringing into the basin large quantities of terrigenous sediments. Lake Tanganyika is a meromictic lake 1470 m deep and 700 km long, of middle Miocene age. It is subdivided into seven asymmetric half grabens separated by transverse ridges. The sedimentary fill is thick and formed by organic oozes having a very good petroleum potential. In contrast to Bogoria, the lateral distribution of organic matter is characterized by considerable heterogeneity due to the existence of structural blocks or to redepositional processes.

Tiercelin, J.J.; Lezzar, K.E. (Universite de Bretagne Occidentale, Brest (France)); Richert, J.P. (Elf Aquitaine, Pau (France))

1994-07-01T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


121

Control of Well Ks-8 in the Kilauea Lower East Rift Zone | Open Energy  

Open Energy Info (EERE)

of Well Ks-8 in the Kilauea Lower East Rift Zone of Well Ks-8 in the Kilauea Lower East Rift Zone Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Paper: Control of Well Ks-8 in the Kilauea Lower East Rift Zone Abstract In June 1991, a well located in Hawaii kicked and unloaded at 3,476 ft (1,059 m). This well was estimatedto have a possible bottomhole temperature of 650°F (343°C)and a reservoir pressure approaching 2,300 psi 5,858 Immediate attempts to kill the well were unsuccessful, and the long processof well control was started. Besides the harsh geological and reservoir conditions encountered,the scarce availability of materials in a remote location and long distance transportation of necessary equipment figured heavily in to the time delay of the final kill procedure of the

122

Conduction Models Of The Temperature Distribution In The East Rift Zone Of  

Open Energy Info (EERE)

Conduction Models Of The Temperature Distribution In The East Rift Zone Of Conduction Models Of The Temperature Distribution In The East Rift Zone Of Kilauea Volcano Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Conduction Models Of The Temperature Distribution In The East Rift Zone Of Kilauea Volcano Details Activities (2) Areas (1) Regions (0) Abstract: Temperature variations in the 1966-meter Hawaii Geothermal Project well HGP-A are simulated by model studies using a finite element code for conductive heat flow. Three models were generated: a constant temperature source from a vertical dike; a constant heat-generating magma chamber; and a transient heat source from a tapered vertical dike. Fair correlation is obtained between the HGP-A well temperature and the tapered dike 125 years after it is injected with an initial (transient) 1200°C

123

Time-Domain Electromagnetics At Hualalai Northwest Rift Area (Thomas, 1986)  

Open Energy Info (EERE)

Time-Domain Electromagnetics At Hualalai Northwest Time-Domain Electromagnetics At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Time-Domain Electromagnetics Activity Date Usefulness useful DOE-funding Unknown Notes Three time-domain electromagnetic soundings were conducted on the middle northwest rift at elevations of 280-320 m (Fig. 40) (Kauahikaua and Mattice, 1981). These soundings penetrated to a greater depth than the Schlumberger soundings and two of them were able to resolve basement resistivities ranging from 9 to 12 ohm-m at depths of 1500 to 1800 m. One sounding detected a 9 ohm.m layer at 600 m depth that was underlain by a more resistive basement. These results suggest that thermal fluids may be responsible for the low-resistivity basement, whereas the high-resistivity

124

Aeromagnetic Survey At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Thomas, 1986) Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Aeromagnetic Survey At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness useful DOE-funding Unknown Notes More recent aeromagnetic data (Godson et al., 1981) generally substantiate the presence of a nearly continuous rift zone from the Kilauea summit down to sea level; the apparent width of the magnetic anomaly does not appear to match that projected by Furumoto (1978a) or Broyles et al. (1979); however, to date, no detailed analysis of the more recent data has been completed (R. B. Moore, pers. commun., 1984). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

125

An Improved Daylight Correction for IR Loss in ARM Diffuse SW Measurements  

NLE Websites -- All DOE Office Websites (Extended Search)

An Improved Daylight Correction for IR Loss An Improved Daylight Correction for IR Loss in ARM Diffuse SW Measurements C. N. Long, K. Younkin, and K. L. Gaustad Pacific Northwest National Laboratory Richland, Washington J. A. Augustine National Oceanic and Atmospheric Administration Air Resources Laboratory Surface Radiation Research Branch Boulder, Colorado Introduction A paper by Cess et al. (2000) notes that some clear-sky diffuse shortwave (SW) measurements they were using from the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site exhibited less than Rayleigh magnitude. Remarking that this is a physical impossibility, the obvious conclusion forwarded by the authors was that there was some problem with the ARM SGP diffuse SW data. Shortly thereafter, the problem of infrared (IR) loss from thermopile-based single black detector

126

Development and Evaluation of RRTMG_SW, a Shortwave Radiative Transfer Model for GCM Applications  

NLE Websites -- All DOE Office Websites (Extended Search)

Development and Evaluation of RRTMG_SW, Development and Evaluation of RRTMG_SW, a Shortwave Radiative Transfer Model for General Circulation Model Applications M. J. Iacono, J. S. Delamere, E. J. Mlawer, and S. A. Clough Atmospheric and Environmental Research, Inc. Lexington, Massachusetts J.-J. Morcrette European Center for Medium-Range Weather Forecasts Reading, United Kingdom Y.-T. Hou National Centers for Environmental Prediction Camp Springs, Maryland Introduction The k-distribution shortwave radiation model developed for the Atmospheric Radiation Measurement (ARM) Program, RRTM_SW_V2.4 (Clough et al. 2004), utilizes the discrete ordinates radiative transfer model, DISORT, for scattering calculations and 16 g-points in each of its 16 spectral bands. DISORT provides agreement with line-by-line flux calculations to within 1 Wm

127

Anomalous subsidence on the rifted volcanic margin of Pakistan: No influence from Deccan plume  

E-Print Network (OSTI)

Anomalous subsidence on the rifted volcanic margin of Pakistan: No influence from Deccan plume, Clifton, Karachi 75600, Pakistan A B S T R A C TA R T I C L E I N F O Article history: Received 28 October

Clift, Peter

128

Wilson cycles, tectonic inheritance, and rifting of the North American Gulf of Mexico continental margin  

E-Print Network (OSTI)

Wilson cycles, tectonic inheritance, and rifting of the North American Gulf of Mexico continental during opening of the Gulf of Mexico. Unlike the Atlantic margins, where Wilson cycles were first recognized, breakup in the Gulf of Mexico did not initially focus within the orogen, but was instead

Huerta, Audrey D.

129

Hydrogen Storage Systems Analysis Meeting 955 L'Enfant Plaza North, SW, Suite 6000  

E-Print Network (OSTI)

Hydrogen Storage Systems Analysis Meeting 955 L'Enfant Plaza North, SW, Suite 6000 Washington, DC, 2005 #12;SUMMARY REPORT Hydrogen Storage Systems Analysis Meeting March 29, 2005 955 L'Enfant Plaza was to familiarize the DOE research community involved in hydrogen storage materials and process development

130

Supporting document for the SW Quadrant Historical Tank Content Estimate for U-Tank Farm  

Science Conference Proceedings (OSTI)

This Supporting Document provides historical characterization information gathered on U-Tank Farm, such as historical waste transfer and level data, tank physical information, temperature data, sampling data, and drywell and liquid observation well data for Historical Tank Content Estimate of the SW Quadrant at the Hanford 200 West Area.

Brevick, C.H.; Gaddis, L.A.; Johnson, E.D.

1994-06-01T23:59:59.000Z

131

Evolution of oceanic margins : rifting in the Gulf of California and sediment diapirism and mantle hydration during subduction  

E-Print Network (OSTI)

This thesis investigates three processes that control the evolution of oceanic margins. Chapter 2 presents seismic images of a ~2-km-thick evaporite body in Guaymas Basin, central Gulf of California. In rifts, evaporites ...

Miller, Nathaniel Clark

2013-01-01T23:59:59.000Z

132

Direct-Current Resistivity Survey At Mauna Loa Northeast Rift Area (Thomas,  

Open Energy Info (EERE)

Direct-Current Resistivity Survey At Mauna Loa Direct-Current Resistivity Survey At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes The vertical electrical sounding surveys encountered few difficulties and were able to resolve basement resistivities in all locations. The resistivity sections derived indicated a 3000- 20,000 ohm.m surface layer underlain by a 500- 900 ohm-m cold freshwatersaturated layer and a basement layer of less than 100 ohm.m (Kauahikaua and Mattice, 1981). The depth of penetration of these soundings was estimated to be about 800 m to 900 m b.s.1. and thus the basement resistivities probably correspond to basalts

133

Modeling-Computer Simulations At Kilauea East Rift Area (Rudman & Epp,  

Open Energy Info (EERE)

Rudman & Epp, Rudman & Epp, 1983) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Modeling-Computer Simulations At Kilauea East Rift Area (Rudman & Epp, 1983) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Modeling-Computer Simulations Activity Date Usefulness useful DOE-funding Unknown Notes Three models were generated: a constant temperature source from a vertical dike; a constant heat-generating magma chamber; and a transient heat source from a tapered vertical dike. Fair correlation is obtained between the HGP-A well temperature and the tapered dike 125 years after it is injected with an initial (transient) 1200degrees C temperature. Results provide background information from which to evaluate the importance of water

134

File:Const SW swppp template.pdf | Open Energy Information  

Open Energy Info (EERE)

Const SW swppp template.pdf Const SW swppp template.pdf Jump to: navigation, search File File history File usage File:Const SW swppp template.pdf Size of this preview: 463 × 599 pixels. Other resolution: 464 × 600 pixels. Go to page 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 Go! next page → next page → Full resolution ‎(1,275 × 1,650 pixels, file size: 542 KB, MIME type: application/pdf, 40 pages) File history Click on a date/time to view the file as it appeared at that time. Date/Time Thumbnail Dimensions User Comment current 10:53, 13 November 2012 Thumbnail for version as of 10:53, 13 November 2012 1,275 × 1,650, 40 pages (542 KB) Dklein2012 (Talk | contribs) You cannot overwrite this file. Edit this file using an external application (See the setup

135

File:Construction SW NOI modified 7-18-2011.pdf | Open Energy Information  

Open Energy Info (EERE)

SW NOI modified 7-18-2011.pdf SW NOI modified 7-18-2011.pdf Jump to: navigation, search File File history File usage File:Construction SW NOI modified 7-18-2011.pdf Size of this preview: 463 × 599 pixels. Other resolution: 464 × 600 pixels. Go to page 1 2 3 Go! next page → next page → Full resolution ‎(1,275 × 1,650 pixels, file size: 100 KB, MIME type: application/pdf, 3 pages) File history Click on a date/time to view the file as it appeared at that time. Date/Time Thumbnail Dimensions User Comment current 10:47, 13 November 2012 Thumbnail for version as of 10:47, 13 November 2012 1,275 × 1,650, 3 pages (100 KB) Dklein2012 (Talk | contribs) You cannot overwrite this file. Edit this file using an external application (See the setup instructions for more information) File usage There are no pages that link to this file.

136

The Use of New Parameterizations for Gaseous Absorption in the CLIRAD-SW Solar Radiation Code for Models  

Science Conference Proceedings (OSTI)

The new gaseous absorption parameterizations are incorporated in the CLIRAD-SW solar radiation code for models, openly distributed for the scientific community. In the new parameterizations, the magnitude of absorption coefficients in each ...

T. A. Tarasova; B. A. Fomin

2007-06-01T23:59:59.000Z

137

Opaline cherts associated with sublacustrine hydrothermal springs at Lake Bogoria, Kenya Rift valley  

SciTech Connect

An unusual group of cherts found at saline, alkaline Lake Bogoria in the Kenya Rift differs from the Magadi-type cherts commonly associated with saline, alkaline lakes. The cherts are opaline, rich in diatoms, and formed from a siliceous, probably gelatinous, precursor that precipitated around submerged alkaline hot springs during a Holocene phase of high lake level. Silica precipitation resulted from rapid drop in the temperature of the spring waters and, possibly, pH. Lithification began before subaerial exposure. Ancient analogous cherts are likely to be localized deposits along fault lines.

Renaut, R.W.; Owen, R.B.

1988-08-01T23:59:59.000Z

138

Bull. Disas. Prey. Res. Inst., Kyoto Univ., Vol. 45, Part 2, 3 No. 389, February, 1996 27 Active Rift System in the Okinawa Trough and Its Northeastern  

E-Print Network (OSTI)

Active Rift System in the Okinawa Trough and Its Northeastern Continuation By Masaaki KIMURA (Manuscript investigations have revealed that the present central rift system of the Okinawa Trough which is an active Okinawa Trough can be distinguished. The crustal thinning and thus eastward drifting of the Ryukyu Arc may

Takada, Shoji

139

Business Ymwet Centlsaem: Enclosed is AEC Special Nuclear Material License Yo. SW-551, as  

Office of Legacy Management (LM)

c-ii 3-y c-ii 3-y !WL?DF!i 70.424 SW-551, 9s renewed AUG 9 196s cmhustian En&merin~, Inc. %.lelcar Division tYindter, Connecticut ,~ttentionr ?tr. 5. ff. Shfp,penbmg: Business Ymwet Centlsaem: Enclosed is AEC Special Nuclear Material License Yo. SW-551, as renewed. Very tTuly yours, fkmald A. Nusshauaer, Chief Saurce 4 Specfel Wcleer Yaterials Brmch Ofvision of Meterbls Licensing EnClOSUWl W W m , as renwed DISTRIBUTION: Ccaplianee, HQs 2 w/encl. H. j. McAlduff, OR00 w/encl. D. George, ?MM w/mcl. N. Dtilos, ML w/emCl, C. Luke, ML w/end. Br. RF w/encl. Div. RF w/o encl. UNITED STATES ATOMIC ENERGY COMMISSION SPECIAL NUCLEAR MATERIAL LICENSE Pursuant to the Atomic Energy Act of 1954 and Title 10, Code of Federal Regulations, Chapter 1, Part 70, "Special Nuclear Material Regulations," a license is hereby issued authorizing the licensee

140

A NUMERICAL ANALYSIS OF THE SINGLE-WELL STEAM ASSISTED GRAVITY DRAINAGE (SW-SAGD) PROCESS  

SciTech Connect

Steam assisted gravity drainage (SAGD) is an effective method to produce heavy oil and bitumen which are important energy resources. In a typical SAGD approach, steam is injected into a horizontal well located directly above a horizontal producer helping to displace heated oil. Single-well (SW) SAGD attempts to create a similar process using only one horizontal well. To improve early-time response of SW-SAGD, it is necessary to heat the near-wellbore area to reduce oil viscosity and allow gravity drainage to begin. Ideally heating should occur with minimal circulation or bypassing of steam. We have investigated early-time processes to improve reservoir heating. A numerical simulation study was performed to gauge combinations of cyclic steam injection and steam circulation prior to SAGD in an effort to better understand and improve early-time performance. Results from this study, include cumulative recoveries, temperature distributions, and production rates. It is found that cyclic steaming of the reservoir offers the most favorable option for heating the near-wellbore area to create conditions that improve initial SAGD response. More favorable reservoir conditions such as low viscosity, thick oil zones, and solution gas, improved reservoir response. Under unfavorable conditions, response was limited.

K.T. Elliot; A.R. Kovscek

2001-06-01T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


141

FAR-ULTRAVIOLET OBSERVATION OF THE AQUILA RIFT WITH FIMS/SPEAR  

Science Conference Proceedings (OSTI)

We present the results of far ultraviolet (FUV) observations of the broad region around the Aquila Rift including the Galactic plane. As compared with various wavelength data sets, dust scattering is found to be the major origin of the diffuse FUV continuum in this region. The FUV intensity clearly correlates with the dust extinction level for E(B - V) 0.2 due to heavy dust extinction combined with the effect of nonuniform interstellar radiation fields. The FUV intensity also correlates well with H{alpha} intensity, implying that at least some fraction of the observed H{alpha} emission could be the dust-scattered light of H{alpha} photons originating elsewhere in the Galaxy. Most of the Aquila Rift region is seen devoid of diffuse FUV continuum due to heavy extinction while strong emission is observed in the surrounding regions. Molecular hydrogen fluorescent emission lines are clearly seen in the spectrum of 'Aquila-Serpens', while 'Aquila-East' does not show any apparent line features. CO emission intensity is also found to be higher in the 'Aquila-Serpens' region than in the 'Aquila-East' region. In this regard, we note that regions of star formation have been found in 'Aquila-Serpens' but not in 'Aquila-East'.

Park, S.-J.; Min, K.-W. [Korea Advanced Institute of Science and Technology, Daejeon 305-701 (Korea, Republic of); Seon, K.-I.; Han, W.; Lee, D.-H. [Korea Astronomy and Space Science Institute, Daejeon 305-348 (Korea, Republic of); Edelstein, J., E-mail: einpark75@kaist.ac.kr [Space Sciences Laboratory, University of California, Berkeley, CA 94720 (United States)

2012-07-20T23:59:59.000Z

142

1000 Independence Avenue, SW, Washington, D.C., Carol G. Crawford, Chair,  

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

FRIDAY, FRIDAY, OCTOBER 25, 2002 The meeting was held at 8:30 in Room 8E-089 of the Department of Energy, 1000 Independence Avenue, SW, Washington, D.C., Carol G. Crawford, Chair, presiding. PRESENT: CAROL G. CRAWFORD, Ph.D. Chair F. JAY BREIDT, Ph.D. Vice Chair MARK BERNSTEIN, Ph.D. JOHNNY BLAIR JAE EDMONDS, Ph.D. JAMES K. HAMMITT, Ph.D. NICHOLAS W. HENGARTNER CALVIN A. KENT, Ph.D. WILLIAM G. MOSS, Ph.D. POLLY A. PHIPPS, Ph.D. RANDY R. SITTER, Ph.D. ROY WHITMORE, Ph.D. ALSO PRESENT: CALVIN A. KENT, Ph.D. Former Committee Member and EIA Administrator ENERGY INFORMATION ADMINISTRATION REPRESENTATIVES: GUY F. CARUSO Administrator MARY J. HUTZLER Acting Deputy Administrator NANCY J. KIRKENDALL Director, Statistics and Methods Group PAUL McARDLE, Ph.D.

143

Secretary Steven Chu U.S. Department of Energy 1000 Independence Avenue, S.W.  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

3, 2009 3, 2009 Secretary Steven Chu U.S. Department of Energy 1000 Independence Avenue, S.W. Washington, D.C. 20585 Dear Secretary Chu: As a condition of receiving Florida's share of the $3.1 billion funding for the State Energy Program (SEP), pursuant to Section 41 0, Division A - Title IV of the American Recovery and Renewal Act of 2009 ( A R M ) , I am providing the following notification. I have received written assurance from the Florida Public Service Commission (FPSC) that it believes that the Florida Energy Efficiency and Conservation Act (Chapter 366, Florida Statutes) as implemented by the FPSC satisfies the requirements in Section 410(1) of the ARRA. Specifically, Florida's general policies ensure that utility financial incentives are aligned with helping their customers use energy more efficiently

144

U.S. Department of Energy Office of General Counsel GC-52 1000 Independence Avenue, SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

7, 1998 7, 1998 U.S. Department of Energy Office of General Counsel GC-52 1000 Independence Avenue, SW Washington, D.C. 20585 REPORT TO CONGRESS ON THE PRICE-ANDERSON ACT I appreciate the opportunity on behalf of Battelle Memorial Institute to respond to the Department of Energy's December 31, 1997 Federal Register "Notice of inquiry concerning preparation of report to Congress on the Price-Anderson Act." Battelle is a nonprofit charitable trust, devoted principally to research and development, education, technology transfer and scientific innovation. Battelle has a vital interest in this report in view of its operational role at two national laboratories and other DOE facilities. Battelle also supports DOE and other Federal agency activities in international nuclear non-proliferation and related

145

Adesso Inc. U.S. DEPARTMENT OF ENERGY 1000 INDEPENDENCE A VE., SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Adesso Inc. Adesso Inc. U.S. DEPARTMENT OF ENERGY 1000 INDEPENDENCE A VE., SW WASHINGTON, DC 20585 ) ) ) SUBPOENA Case Number: 2010-SE-2002 FOR INFORMATION AND PRODUCTION OF DOCUMENTS To: Margaret Traub, CEO Adesso Inc. 21 Penn Plaza Suite 909 New York, NY 10001 Issued: March 23, 2010 Service by certified mail The U.S. Department of Energy (DOE) issues this Subpoena for Information and Production of Documents to Adesso Inc. (Adesso) pursuant to 42 U.S.C. § 6299 of the Energy Policy and Conservation Act (EPCA) and the regulations promulgated thereunder (10 C.F.R. § 430. 72). As you should be aware, pursuant to EPCA, DOE has established an energy conservation standard applicable to torchieres. See 42 U.S.C. § 6295(x); 10 CFR 430.32(t). Manufacturers and private

146

PUBLIC ACCESS: 955 LEnfant Plaza North, SW, Suite 1500, Washington, DC  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

th th Meeting Unconventional Resources Technology Advisory Committee July 14, 2009 1:00 p.m. EASTERN WebEx/Conference Call Meeting PUBLIC ACCESS: 955 L'Enfant Plaza North, SW, Suite 1500, Washington, DC AGENDA 12:30 Registration; Begin call in to 800-number and login to WebEx Members, Chair, Designated Federal Officer, and Committee Manager 1:00 Call to Order - Welcome Chris Hall, Committee Chair Member Roll Call and the presence of a quorum Elena Melchert Committee Manager Meeting purpose and review of the agenda; Insights regarding future funding and other pending legislation; Draft 2010 Annual Plan delivery, and pending meetings in September and October 2009 Guido DeHoratiis Designated Federal Officer 1:25 Report from the Standing Subcommittee and

147

J.G. Tobin and S.-W. Yu Lawrence Livermore National Laboratory, Livermore, CA, USA  

National Nuclear Security Administration (NNSA)

Differentiation of 5f and 6d Components Differentiation of 5f and 6d Components in the Unoccupied Electronic Structure of UO 2 J.G. Tobin and S.-W. Yu Lawrence Livermore National Laboratory, Livermore, CA, USA Summary: One of the crucial questions of all actinide electronic structure determinations is the issue of 5f versus 6d character and the distribution of these components across the density of states. Here, two break-though experiments will be discussed, which have allowed the direct determination of the U5f and U6d contributions to the unoccupied density of states (UDOS) in Uranium Dioxide (UO 2 ). [1] First, a combined soft X-ray Absorption and Bremstrahlung Isochromat Spectroscopy (XAS and BIS, respectively) study of UO 2 will be discussed. [2] Second, a novel Resonant Inverse Photoelectron and X-ray Emission Spectroscopy (RIPES and

148

PUBLIC ACCESS: 955 LEnfant Plaza North, SW, Suite 1500, Washington, DC  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

10 10 th Meeting Ultra-Deepwater Advisory Committee July 15, 2009, 8:00 a.m. EASTERN, WebEx/Conference Call Meeting PUBLIC ACCESS: 955 L'Enfant Plaza North, SW, Suite 1500, Washington, DC AGENDA 7:30 Registration; Begin Member call in 8:00 Call to Order - Welcome Arnis Judzis, Vice-Chair Member Roll Call and the presence of a quorum Elena Melchert, Committee Manager Meeting purpose and review of the agenda; Insights regarding future funding and other pending legislation; Draft 2010 Annual Plan delivery, and pending meetings in September and October 2009 Guido DeHoratiis Designated Federal Officer 8:25 Report from the Standing Subcommittee regarding Process; Member Q/A and Discussion Mary Jane Wilson

149

Remote sensing studies and morphotectonic investigations in an arid rift setting, Baja California, Mexico  

E-Print Network (OSTI)

The Gulf of California and its surrounding land areas provide a classic example of recently rifted continental lithosphere. The recent tectonic history of eastern Baja California has been dominated by oblique rifting that began at ~12 Ma. Thus, extensional tectonics, bedrock lithology, long-term climatic changes, and evolving surface processes have controlled the tectono-geomorphological evolution of the eastern part of the peninsula since that time. In this study, digital elevation data from the Shuttle Radar Topography Mission (SRTM) from Baja California were corrected and enhanced by replacing artifacts with real values that were derived using a series of geostatistical techniques. The next step was to generate accurate thematic geologic maps with high resolution (15-m) for the entire eastern coast of Baja California. The main approach that we used to clearly represent all the lithological units in the investigated area was objectoriented classification based on fuzzy logic theory. The area of study was divided into twenty-two blocks; each was classified independently on the basis of its own defined membership function. Overall accuracies were 89.6 %, indicating that this approach was highly recommended over the most conventional classification techniques. The third step of this study was to assess the factors that affected the geomorphologic development along the eastern side of Baja California, where thirty-four drainage basins were extracted from a 15-m-resolution absolute digital elevation model (DEM). Thirty morphometric parameters were extracted; these parameters were then reduced using principal component analysis (PCA). Cluster analysis classification defined four major groups of basins. We extracted stream length-gradient indices, which highlight the differential rock uplift that has occurred along fault escarpments bounding the basins. Also, steepness and concavity indices were extracted for bedrock channels within the thirty-four drainage basins. The results were highly correlated with stream length-gradient indices for each basin. Nine basins, exhibiting steepness index values greater than 0.07, indicated a strong tectonic signature and possible higher uplift rates in these basins. Further, our results indicated that drainage basins in the eastern rift province of Baja California could be classified according to the dominant geomorphologic controlling factors (i.e., faultcontrolled, lithology-controlled, or hybrid basins).

El-Sobky, Hesham Farouk

2007-08-01T23:59:59.000Z

150

A Numerical Analysis of the Single-Well Steam Assisted Gravity Drainage Process (SW-SAGD)1  

E-Print Network (OSTI)

1 A Numerical Analysis of the Single-Well Steam Assisted Gravity Drainage Process (SW-SAGD)1 K. T. Elliot and A. R. Kovscek Department of Petroleum Engineering, Stanford University?U.S.A. Abstract Steam approach, steam is injected into a horizontal well located directly above a horizontal producer. A steam

151

Isotopic evidence for neogene hominid paleoenvironments in the Kenya Rift Valley  

Science Conference Proceedings (OSTI)

Bipedality, the definitive characteristic of the earliest hominids, has been regarded as an adaptive response to a transition from forested to more-open habitats in East Africa sometime between 12 million and 5 million years ago. Analyses of the stable carbon isotopic composition ([delta][sup 13]C) of paleosol carbonate and organic matter from the Tugen Hills succession in Kenya indicate that a heterogeneous environment with a mix of C3 and C4 plants has persisted for the last 15.5 million years. Open grasslands at no time dominated this portion of the rift valley. The observed [delta][sup 13]C values offer no evidence for a shift from more-closed C3 environments to C4 grasslands habitats. If hominids evolved in East Africa during the Late Miocene, they did so in an ecologically diverse setting.

Kingston, J.D.; Hill, A. (Yale Univ., New Haven, CT (United States)); Marino, B.D. (Harvard Univ., Cambridge, MA (United States))

1994-05-13T23:59:59.000Z

152

Geologic Characterization of the South Georgia Rift Basin for Source Proximal CO2 Storage  

NLE Websites -- All DOE Office Websites (Extended Search)

Georgia Rift Basin for Source Proximal CO 2 Storage Michael G. Waddell and John M. Shafer Earth Sciences and Resources Institute University of South Carolina - Columbia Carbon Storage Program Infrastructure Annual Review Meeting Pittsburgh, PA November 15-17, 2011 Carbon Storage Program Infrastructure Annual Review Meeting - November 15-17, 2011 Research Team Carbon Storage Program Infrastructure Annual Review Meeting - November 15-17, 2011 John Shafer and Michael Waddell James Knapp and Camelia Knapp Lee Kurtzweil and Phil VanHollebeke C.W. "Bill" Clendenin Richard Berg James Rine Integrated Services Contract for Drilling/Coring/Logging - TBD Study Area Carbon Storage Program Infrastructure Annual Review Meeting - November 15-17, 2011

153

The origin of hydrothermal and other gases in the Kenya Rift Valley  

SciTech Connect

The Kenya Rift Valley (KRV) is part of a major continental rift system from which much outgassing is presently occurring. Previous research on gases in the KRV has tended to concentrate on their geothermal implications; the present paper is an attempt to broaden the interpretation by consideration of new data including helium and carbon isotope analyses from a wide cross-section of sites. In order to do this, gases have been divided into categories dependent on origin. N{sub 2} and noble gases are for the most part atmospherically derived, although their relative concentrations may be altered from ASW ratios by various physical processes. Reduced carbon (CH{sub 4} and homologues) appears to be exclusively derived from the shallow crust, with thermogenic {delta}{sup 13}C values averaging -25{per_thousand} PDB for CH{sub 4}. H{sub 2} is likely also to be crustally formed. CO{sub 2}, generally a dominant constituent, has a narrow {delta}{sup 13}C range averaging -3.7{per_thousand} PDB, and is likely to be derived with little modification from the upper mantle. Consideration of the ratio C/{sup 3}He supports this view in most cases. Sulphur probably also originates there. Ratios of {sup 3}He/{sup 4}He reach a MORB-like maximum of 8.0 R/R{sub A} and provide the best indication of an upper mantle source of gases beneath the KRV. A correlation between {sup 3}He/{sup 4}He and the hydrocarbon parameter log (C{sub 1}/{Sigma}C{sub 2-4}) appears to be primarily temperature related. The highest {sup 3}He/{sup 4}He ratios in spring waters are associated with basalts, perhaps because of the leaching of basalt glasses. There may be a structural control on {sup 3}He/{sup 4}He ratios in the KRV as a whole.

Darling, W.G. [British Geological Survey, Wallingford (United Kingdom)] [British Geological Survey, Wallingford (United Kingdom); Griesshaber, E. [Max-Planck Institut fuer Chemie, Mainz (Germany)] [Max-Planck Institut fuer Chemie, Mainz (Germany); Andrews, J.N. [Univ. of Reading (United Kingdom)] [and others] [Univ. of Reading (United Kingdom); and others

1995-06-01T23:59:59.000Z

154

Analysis of Convective Activity and Its Relationship to the Rainfall over the Rift Valley Lakes of East Africa during 198390 Using the Meteosat Infrared Channel  

Science Conference Proceedings (OSTI)

The convective activity over the Rift Valley lakes of East Africa, as deduced from cloud tops colder than a predefined threshold, is examined. Relationships between satellite-derived convective indices and rainfall measurements are also examined. ...

Mamoudou B. Ba; Sharon E. Nicholson

1998-10-01T23:59:59.000Z

155

Associated production of $?(1S)W$ at LHC in next-to-leading order QCD  

E-Print Network (OSTI)

We investigate the complete next-to-leading order (NLO) QCD corrections to $\\Upsilon(1S) +W$ production at the LHC, and predict theoretically the distribution of the $\\Upsilon(1S)$ transverse momentum. We analyse the contributions from different components up to the QCD NLO in the \\ppUW process. Our results show that the \\ppUW process has a large production rate and could be potentially detected at the LHC. We see that the differential cross section for the $\\Upsilon(1S)$ direct-production at the LO is significantly enhanced by the QCD corrections, and the $b\\bar{b} [ ^3S_1^{(8)} ]$ contribution component dominates in the whole plotted $p_T^{\\Upsilon(1S)}$ region. We have also calculated the $\\Upsilon(1S)$ meson indirect-productions via feed-down decays of $\\Upsilon(2S)$, $\\Upsilon(3S)$, $\\chi_{b1}(1P)$, $\\chi_{b2}(1P)$, $\\chi_{b1}(2P)$, and $\\chi_{b2}(2P)$ mesons. We find that the $\\Upsilon(1S)$ indirect-productions can give important contributions to the distribution of $p_T^{\\Upsilon(1S)}$ for the \\ppUW process at the NLO. We conclude that the studying the $\\Upsilon(1S)+W$ production at the LHC could provide an interesting opportunity in testing the nonrelativistic QCD factorization formalism.

Li Gang; Ma Wen-Gan; Song Mao; Zhang Ren-You; Guo Jian-You

2012-12-11T23:59:59.000Z

156

Advanced Biofuels Workshop U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585  

Gasoline and Diesel Fuel Update (EIA)

U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585 U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585 August 1, 2012 Presenter Bios (Arranged in presentation order) Anthony Radich Tony Radich is an economist with the Energy Information Administration. He is currently a member of the Biofuels and Emerging Technologies Team in the Petroleum, Natural Gas and Biofuels Analysis group of the Office of Energy Analysis. Dr. Radich has worked on biofuels issues since he joined EIA in 2001. He developed the cost models for the production of ethanol and biodiesel, the National Energy Modeling System, which is used to produce the EIA Annual Energy Outlook. He has served as a contributing author to numerous EIA publications, including the Annual Energy Outlook and the Short-Term

157

Top-of-Atmosphere Radiance-to-Flux Conversion in the SW Domain for the ScaRaB-3 Instrument on Megha-Tropiques  

Science Conference Proceedings (OSTI)

The earth radiation budget (ERB) is the difference between the solar absorbed flux and the terrestrial emitted flux. These fluxes are calculated from satellite measurements of outgoing shortwave (SW) and longwave (LW) radiances using empirical or ...

Michel Viollier; Carsten Standfuss; Olivier Chomette; Arnaud Quesney

2009-10-01T23:59:59.000Z

158

Report for Treating Hanford LAW and WTP SW Simulants: Pilot Plant Mineralizing Flowsheet  

SciTech Connect

The US Department of Energy is responsible for managing the disposal of radioactive liquid waste in underground storage tanks at the Hanford site in Washington State. The Hanford waste treatment and immobilization plant (WPT) will separate the waste into a small volume of high level waste (HLW), containing most of the radioactive constituents, and a larger volume of low activity waste (LAW), containing most of the non-radioactive chemical and hazardous constituents. The HLW and LAW will be converted into immobilized waste forms for disposal. Currently there is inadequate LAW vitrification capacity planned at the WTP to complete the mission within the required timeframe. Therefore additional LAW capacity is required. One candidate supplemental treatment technology is the fluidized bed steam reformer process (FBSR). This report describes the demonstration testing of the FBSR process using a mineralizing flowsheet for treating simulated Hanford LAW and secondary waste from the WTP (WTP SW). The FBSR testing project produced leach-resistant solid products and environmentally compliant gaseous effluents. The solid products incorporated normally soluble ions into an alkali alumino-silicate (NaS) mineral matrix. Gaseous emissions were found to be within regulatory limits. Cesium and rhenium were captured in the mineralized products with system removal efficiencies of 99.999% and 99.998 respectively. The durability and leach performance of the FBSR granular solid were superior to the low activity reference material (LMR) glass standards. Normalized product consistency test (PCT) release rates for constituents of concern were approximately 2 orders of magnitude less than that of sodium in the Hanford glass [standard].

Arlin Olson

2012-02-28T23:59:59.000Z

159

Seismic attribute analyses of lower Permian (Wolfcampian-Leonardian) carbonate buildups, SW Midland, Texas  

E-Print Network (OSTI)

A trend of Wolfcampian-Leonardian carbonate buildups is located in the southwestern Midland Basin, Upton County, Texas. The buildup trend is located east of the eastern faulted margin of the Central Basin Platform and north of the Ozona Arch. Carbonate deposition began during lowstand times, within or just below wave base. In the Southwestern Midland Basin, the Wolfcampian-Leonardian carbonate interval is lithologically heterogeneous due to the presence of abundant lithoclastic debris that was shed from the uplifted Central Basin Platform. The lithologic heterogeneity makes it difficult to identify the buildups on seismic profiles. Several inferred buildups have been drilled in the past, but many boreholes only penetrated lithoclastic facies, not true buildup facies. Analyses of various seismic attributes were conducted for the Wolfcampian-Leonardian interval in the SW Midland Basin in an attempt to improve the recognition and imaging of the carbonate buildups. The objective was to identify a set of attributes that directly indicate the buildup locations. After extensive trial of various attributes, the variance attribute was selected as the optimum seismic attribute. The resultant 3D variance volume was used to detect the buildup locations, and some aspects of their internal stratigraphy, and to establish the fault framework in the Amacker survey. The instantaneous frequency attribute, combined with the variance attribute was also marginally useful for imaging the buildups. The variance attribute and instantaneous frequency were compared. Images generated from the variance attribute are better than those generated using the instantaneous frequency because on these images, it is possible to localize the buildups. The instantaneous frequency attribute combined with the variance attribute allows recognition of lithologic heterogeneities inside the buildup interval.

Decalf, Carole Christiane

2001-01-01T23:59:59.000Z

160

Origin of platy calcite crystals in hot-spring deposits in the Kenya Rift Valley  

SciTech Connect

Platy calcite crystals, which have their c axis parallel to their shortest length axis, are common components of travertine deposits found around some hot springs in the Kenya Rift Valley. They are composite crystals formed of numerous paper-thin subcrystals. Individual plates allowed to grow without obstruction develop a hexagonal motif. The Kenyan crystals typically form in hot (>75 C) waters that have a low Ca content (<10 mg/l), a high CO{sub 2} content, and a high rate of CO{sub 2} degassing. At Chemurkeu, aggregates of numerous small platy crystals collectively form lattice crystals that superficially resemble ray crystals. The walls of the lattice crystals are formed of large platy crystals that have their long and intermediate length axes aligned parallel to the plane of the long axis of the lattice crystal. Internally, the lattice crystals are formed of small platy calcite crystals arranged in a boxlike pattern that creates the appearance of a lattice when viewed in thin section. Lattice crystals are highly porous, with each pore being enclosed by platy crystals. At Lorusio, travertines are mainly formed of pseudodentrites that are constructed by numerous small platy crystals attached to a main stem which is a large platy crystal that commonly curves along its long axis. The pseudodentrites are the main construction blocks in ledges and lilypads that form in the vent pool and spring outflow channels, where the water is too hot for microbes other than hyperthermophiles. The platy calcite crystals in the Kenyan travertines are morphologically similar to platy calcite crystals that form as scale in pipes in the geothermal fields of New Zealand and hydrothermal angel wing calcite from the La Fe mine in Mexico. Comparison of the Kenyan and New Zealand crystals indicates that platy calcite crystals form from waters with a low Ca{sup 2+} content and a high CO{sub 3}/Ca ratio due to rapid rates of CO{sub 2} degassing.

Jones, B. [Univ. of Alberta, Edmonton, Alberta (Canada). Dept. of Earth and Atmospheric Sciences; Renault, R.W. [Univ. of Saskatchewan, Saskatoon, Saskatchewan (Canada). Dept. of Geological Sciences

1998-09-01T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


161

Trace element and isotope geochemistry of geothermal fluids, East Rift Zone, Kilauea, Hawaii  

DOE Green Energy (OSTI)

A research program has been undertaken in an effort to better characterize the composition and the precipitation characteristic of the geothermal fluids produced by the HGP-A geothermal well located on the Kilauea East Rift Zone on the Island of Hawaii. The results of these studies have shown that the chemical composition of the fluids changed over the production life of the well and that the fluids produced were the result of mixing of at least two, and possibly three, source fluids. These source fluids were recognized as: a sea water composition modified by high temperature water-rock reactions; meteoric recharge; and a hydrothermal fluid that had been equilibrated with high temperature reservoir rocks and magmatic volatiles. Although the major alkali and halide elements show clearly increasing trends with time, only a few of the trace transition metals show a similar trend. The rare earth elements, were typically found at low concentrations and appeared to be highly variable with time. Studies of the precipitation characteristics of silica showed that amorphous silica deposition rates were highly sensitive to fluid pH and that increases in fluid pH above about 8.5 could flocculate more than 80% of the suspended colloidal silica in excess of its solubility. Addition of transition metal salts were also found to enhance the recovery fractions of silica from solution. The amorphous silica precipitate was also found to strongly scavenge the alkaline earth and transition metal ions naturally present in the brines; mild acid treatments were shown to be capable of removing substantial fractions of the scavenged metals from the silica flocs yielding a moderately pure gelatinous by-product. Further work on the silica precipitation process is recommended to improve our ability to control silica scaling from high temperature geothermal fluids or to recover a marketable silica by-product from these fluids prior to reinjection.

West, H.B.; Delanoy, G.A.; Thomas, D.M. (Hawaii Univ., Honolulu, HI (United States). Hawaii Inst. of Geophysics); Gerlach, D.C. (Lawrence Livermore National Lab., CA (United States)); Chen, B.; Takahashi, P.; Thomas, D.M. (Hawaii Univ., Honolulu, HI (United States) Evans (Charles) and Associates, Redwood City, CA (United States))

1992-01-01T23:59:59.000Z

162

Human adrenal tumor cell line SW-13 contains a natriuretic peptide receptor system that responds preferentially to ANP among various natriuretic peptides  

SciTech Connect

A new type of ANP receptor system which clearly distinguishes natriuretic peptides A and B (ANP and BNP) has been identified in the human adrenal tumor cell line SW-13 and characterized. SW-13 cells responded to nanomolar concentrations of ANP with large increases in cGMP levels but in the case of BNP, much higher concentrations were required to produce the same extent of response. This property is unique since the 140-kDa ANP receptors so far characterized do not discriminate between ANP and BNP. For comparison, various natriuretic peptide receptors were also re-characterized using the recently identified CNP.

Mizuno, T.; Katafuchi, T.; Hagiwara, H.; Ito, T.; Kangawa, K.; Matsuo, H.; Hirose, S. (Tokyo Institute of Technology (Japan))

1990-12-31T23:59:59.000Z

163

Earth and Planetary Science Letters 134 (1995) 527-544 The effect of rift shoulder erosion on strata1 patterns at passive  

E-Print Network (OSTI)

displays a characteristic offlap pattern. When the rift shoulder is largely eroded, onlap Parameters for ail models PElIax 1i-sed If-bas Kdiff-bas Kdirr-sed,area! Kdirr-sed,marine 3.0 50 km 5km 1 m

van der Beek, Peter

164

U.S. Department of Energy Office of General Counsel, GC-52 1000 Independence Avenue, S.W.  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

U.S. Department of Energy Office of General Counsel, GC-52 1000 Independence Avenue, S.W. Washington, D.C. 20585 RE: University of California Comments on Price-Anderson Act Notice of Inquiry The University appreciates the opportunity to comment on the Notice of Inquiry (NOI) concerning preparation of a report to Congress on the Price-Anderson Act. The NOI poses a number of questions that attempt to identify potential issues that might arise in developing the report. The University includes its general comments in this letter and offers its responses to the specific questions in an attachment. The Price-Anderson Act provides an important guarantee to American citizens that they will be compensated for injuries sustained as a result of exposure to nuclear materials. This guarantee must remain in effect regardless of how the

165

Advanced Biofuels Workshop U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585  

Gasoline and Diesel Fuel Update (EIA)

Advanced Biofuels Workshop Advanced Biofuels Workshop U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585 August 1, 2012 Contact Information Hosts: Mindi Farber-DeAnda Team Lead, Energy Information Administration, Biofuels and Emerging Technologies Mindi.Farber-DeAnda@eia.gov 202-586-6419 Vishakh Mantri, Ph.D, P.E. Chemical Engineer, Energy Information Administration, Biofuels and Emerging Technologies Team Vishakh.Mantri@eia.gov 202-586-4815 Presenters Biofuels Year in Review Anthony Radich Analyst, Energy Information Administration Anthony.Radich@eia.gov 202-586-0504 Biofuels Outlook Terrence Higgins Hart Downstream Energy Services thiggins@hartenergy.com 703-891-4815 703-891-4815 Sustainability of Biofuels

166

Regional seismic reflection line, southern Illinois Basin, provides new data on Cambrian rift geometry, Hicks Dome genesis, and the Fluorspar Area Fault Complex  

SciTech Connect

Detailed studies of the subsurface structure of the Cambrian Reelfoot rift (RFR) in the Midwestern US provide important insights into continental rifting processes and into the structural fabric of a zone of modern intracratonic seismicity (New Madrid zone). High-quality oil industry seismic reflection data show that in the area of transition between the RFR and the Rough Creek Graben (RCG) the geometry of the Cambrian rift system is that of a half-graben that thickens to the southeast. This contrasts with the northward-thickening half-graben observed to the east in the RCG and with the more symmetric graben to the south in the RFR. An 82.8-km segment of a northwest-southeast seismic reflection profile in southeastern Illinois and western Kentucky shows that near Hicks Dome, Illinois, Middle and Lower Cambrian syn-rift sedimentary rocks occupy about 0.35 s (two-way travel time) on the seismic reflection section (corresponding to a thickness of about 970 m). This stratigraphic interval occupies about 0.45 s (1,250 m) near the Ohio river and is thickest against the Tabb Fault System (TFS) in Kentucky, where it occupies 0.7 s (1,940 m). The seismic data show that in this part of the Cambrian rift the master fault was part of the TFS and that normal displacement on the TFS continued through middle Paleozoic time. The seismic data also provide new information on the late Paleozoic development of Hicks-Dome and the surrounding Fluorspar Area Fault Complex (FAFC) in southeastern Illinois and western Kentucky. A series of grabens and horsts in the FAFC document a late Paleozoic reactivation of the RFR. Comparison of the reflection data with surface mineralization patterns shows that in most cases mineralized graben-bounding faults clearly cut basement or are splays from faults that cut basement.

Potter, C.J.; Goldhaber, M.B.; Taylor, C.D. (U.S. Geological Survey, Denver, CO (United States)); Heigold, P.C. (Illinois State Geological Survey, Champaign, IL (United States))

1992-01-01T23:59:59.000Z

167

An inventory survey at the site of the proposed Kilauea Middle East Rift Zone (KMERZ), Well Site No. 2  

DOE Green Energy (OSTI)

At the request of True Mid Pacific Geothermal, Archaeological Consultants of Hawaii, Inc. has conducted an inventory survey at the site of the proposed Kilauea Middle East Rift Zone (KMERZ), Well Site No.2, TMK: 1-2-10:3. The Principal Investigator was Joseph Kennedy M.A., assisted by Jacob Kaio, Field Supervisor and field crew Mark Borrello B.A., Michael O'Shaughnessy B.A., and Randy Adric. This report supercedes all previous reports submitted to the Historic Presentation Section of the Department of Land and Natural Resources. In addition to 100% surface coverage of the 400 x 400 foot well pad itself, 100% surface coverage of a substantial buffer zone was also completed. This buffer zone was established by the Department of Land and Natural Resources, Historic Preservation personnel and extends 1000 feet east and west of the well site and 500 feet north and south of the well site.

Kennedy, Joseph

1991-03-01T23:59:59.000Z

168

Archaeology in the Kilauea East Rift Zone: Part 1, Land-use model and research design, Kapoho, Kamaili and Kilauea Geothermal Subzones, Puna District, Hawaii Island  

DOE Green Energy (OSTI)

The Puna Geothermal Resource Subzones (GRS) project area encompasses approximately 22,000 acres centered on the Kilauea East Rift Zone in Puna District, Hawaii Island. The area is divided into three subzones proposed for geothermal power development -- Kilauea Middle East Rift, Kamaili and Kapoho GRS. Throughout the time of human occupation, eruptive episodes along the rift have maintained a dynamic landscape. Periodic volcanic events, for example, have changed the coastline configuration, altered patterns of agriculturally suitable sediments, and created an assortment of periodically active, periodically quiescent, volcanic hazards. Because of the active character of the rift zone, then, the area`s occupants have always been obliged to organize their use of the landscape to accommodate a dynamic mosaic of lava flow types and ages. While the specific configuration of settlements and agricultural areas necessarily changed in response to volcanic events, it is possible to anticipate general patterns in the manner in which populations used the landscape through time. This research design offers a model that predicts the spatial results of long-term land-use patterns and relates them to the character of the archaeological record of that use. In essence, the environmental/land-use model developed here predicts that highest population levels, and hence the greatest abundance and complexity of identifiable prehistoric remains, tended to cluster near the coast at places that maximized access to productive fisheries and agricultural soils. With the possible exception of a few inland settlements, the density of archaeological remains expected to decrease with distance from the coastline. The pattern is generally supported in the regions existing ethnohistoric and archaeological record.

Burtchard, G.C.; Moblo, P. [International Archaeological Research Inst., Inc., Honolulu, HI (United States)

1994-07-01T23:59:59.000Z

169

Expression of CAR in SW480 and HepG2 cells during G1 is associated with cell proliferation  

Science Conference Proceedings (OSTI)

Constitutive androstane receptor (CAR) is a transcription factor to regulate the expression of several genes related to drug-metabolism. Here, we demonstrate that CAR protein accumulates during G1 in human SW480 and HepG2 cells. After the G1/S phase transition, CAR protein levels decreased, and CAR was hardly detected in cells by the late M phase. CAR expression in both cell lines was suppressed by RNA interference-mediated suppression of CDK4. Depletion of CAR by RNA interference in both cells and by hepatocyte growth factor treatment in HepG2 cells resulted in decreased MDM2 expression that led to p21 upregulation and repression of HepG2 cell growth. Thus, our results demonstrate that CAR expression is an early G1 event regulated by CDK4 that contributes to MDM2 expression; these findings suggest that CAR may influence the expression of genes involved in not only the metabolism of endogenous and exogenous substances but also in the cell proliferation.

Osabe, Makoto [Department of Pharmaco-Biochemistry, School of Pharmaceutical Sciences, University of Shizuoka, 52-1 Yada, Suruga-ku, Shizuoka 422-8526 (Japan); Sugatani, Junko [Department of Pharmaco-Biochemistry, School of Pharmaceutical Sciences, University of Shizuoka, 52-1 Yada, Suruga-ku, Shizuoka 422-8526 (Japan); Global COE Program, School of Pharmaceutical Sciences, University of Shizuoka, Shizuoka (Japan)], E-mail: sugatani@u-shizuoka-ken.ac.jp; Takemura, Akiko; Yamazaki, Yasuhiro; Ikari, Akira [Department of Pharmaco-Biochemistry, School of Pharmaceutical Sciences, University of Shizuoka, 52-1 Yada, Suruga-ku, Shizuoka 422-8526 (Japan); Kitamura, Naomi [Department of Biological Sciences, Graduate School of Bioscience and Biotechnology, Tokyo Institute of Technology, Yokohama (Japan); Negishi, Masahiko [Pharmacogenetics Section, Laboratory of Reproductive and Developmental Toxicology, National Institute of Environmental Health Sciences, National Institutes of Health, Research Triangle Park, NC (United States); Miwa, Masao [Department of Pharmaco-Biochemistry, School of Pharmaceutical Sciences, University of Shizuoka, 52-1 Yada, Suruga-ku, Shizuoka 422-8526 (Japan)

2008-05-16T23:59:59.000Z

170

Single-crystal sup 40 Ar/ sup 39 Ar dating of the Olorgesailie Formation, southern Kenya rift  

SciTech Connect

Single-crystal laser fusion {sup 40}Ar/{sup 39}Ar analyses and several conventional bulk fusion {sup 40}K- {sup 40}Ar dates have been used to determine the age of volcaniclastic strata within the Olorgesailie Formation and of associated volcanic and sedimentary units of the southern Kenya rift. In the principal exposures along the southern edge of the Legemunge Plain, the formation spans the interval from approximately 500 to 1,000 ka. Deposition continued to the east along the Ol Keju Nyiro river where a tuff near the top of the formation has been dated at 215 ka. In these exposures, the formation is unconformably overlain by sediments dated at 49 ka. A possible source for the Olorgesailie tephra, the Ol Doinyo Nyokie volcanic complex, contains as ash flow dated at {approximately} 1 Ma, extending the known age range of this complex to encompass that of virtually the entire Olorgesailie Formation in the Legemunge Plain. These geologic examples illustrate the importance of the single-crystal {sup 40}Ar/{sup 39}Ar dating technique whereby contaminant, altered, or otherwise aberrant grains can be identified and eliminated from the determination of eruptive ages for reworked or altered pyroclastic deposits. The authors have presented a computer-modeling procedure based on an inverse-isochron analysis that promotes a more objective approach to trimming {sup 40}Ar/{sup 39}Ar isotope data sets of this type.

Deino, A. (Geochronology Center of the Inst. of Human Origins, Berkeley, CA (United States)); Potts, R. (Smithsonian Institution, Washington, DC (United States))

1990-06-10T23:59:59.000Z

171

Geophysical study of the crust and upper mantle beneath the central Rio Grande rift and adjacent Great Plains and Colorado Plateau  

Science Conference Proceedings (OSTI)

As part of the national hot dry rock (HDR) geothermal program conducted by Los Alamos Scientific Laboratory, a regional deep magnetotelluric (MT) survey of Arizona and New Mexico was performed. The main objective of the MT project was to produce a regional geoelectric contour map of the pervasive deep electrical conductor within the crust and/or upper mantle beneath the Colorado Plateau, Basin and Range Province, and Rio Grande rift. Three MT profiles cross the Jemez lineament. Preliminary one-dimensional analysis of the data suggest the lineament is associated with anomalously high electrical conductivity very shallow in the crust. An MT/audiomagnetotelluric (AMT) study of a 161 km/sup 2/ HDR prospect was performed on the Zuni Indian Reservation, New Mexico. Two-dimensional gravity modeling of a 700-km gravity profile at 34/sup 0/30'N latitude was used to study the crust and upper mantle beneath the Rio Grande rift. Several models of each of three consecutive layers were produced using all available geologic and geophysical constraints. Two short-wavelength anomalies along the gravity profile were analyzed using linear optimization techniques.

Ander, M.E.

1981-03-01T23:59:59.000Z

172

RECONNAISSANCE ASSESSMENT OF CO2 SEQUESTRATION POTENTIAL IN THE TRIASSIC AGE RIFT BASIN TREND OF SOUTH CAROLINA, GEORGIA, AND NORTHERN FLORIDA  

SciTech Connect

A reconnaissance assessment of the carbon dioxide (CO{sub 2}) sequestration potential within the Triassic age rift trend sediments of South Carolina, Georgia and the northern Florida Rift trend was performed for the Office of Fossil Energy, National Energy Technology Laboratory (NETL). This rift trend also extends into eastern Alabama, and has been termed the South Georgia Rift by previous authors, but is termed the South Carolina, Georgia, northern Florida, and eastern Alabama Rift (SGFAR) trend in this report to better describe the extent of the trend. The objectives of the study were to: (1) integrate all pertinent geologic information (literature reviews, drilling logs, seismic data, etc.) to create an understanding of the structural aspects of the basin trend (basin trend location and configuration, and the thickness of the sedimentary rock fill), (2) estimate the rough CO{sub 2} storage capacity (using conservative inputs), and (3) assess the general viability of the basins as sites of large-scale CO{sub 2} sequestration (determine if additional studies are appropriate). The CO{sub 2} estimates for the trend include South Carolina, Georgia, and northern Florida only. The study determined that the basins within the SGFAR trend have sufficient sedimentary fill to have a large potential storage capacity for CO{sub 2}. The deeper basins appear to have sedimentary fill of over 15,000 feet. Much of this fill is likely to be alluvial and fluvial sedimentary rock with higher porosity and permeability. This report estimates an order of magnitude potential capacity of approximately 137 billion metric tons for supercritical CO{sub 2}. The pore space within the basins represent hundreds of years of potential storage for supercritical CO{sub 2} and CO{sub 2} stored in aqueous form. There are many sources of CO{sub 2} within the region that could use the trend for geologic storage. Thirty one coal fired power plants are located within 100 miles of the deepest portions of these basins. There are also several cement and ammonia plants near the basins. Sixteen coal fired power plants are present on or adjacent to the basins which could support a low pipeline transportation cost. The current geological information is not sufficient to quantify specific storage reservoirs, seals, or traps. There is insufficient hydrogeologic information to quantify the saline nature of the water present within all of the basins. Water data in the Dunbarton Basin of the Savannah River Site indicates dissolved solids concentrations of greater than 10,000 parts per million (not potential drinking water). Additional reservoir characterization is needed to take advantage of the SGFAR trend for anthropogenic CO{sub 2} storage. The authors of this report believe it would be appropriate to study the reservoir potential in the deeper basins that are in close proximity to the current larger coal fired power plants (Albany-Arabi, Camilla-Ocilla, Alamo-Ehrhardt, and Jedburg basin).

Blount, G.; Millings, M.

2011-08-01T23:59:59.000Z

173

Deep Production Well for Geothermal Direct-Use Heating of A Large Commercial Greenhouse, Radium Springs, Rio Grande Rift, New Mexico  

DOE Green Energy (OSTI)

Expansion of a large commercial geothermally-heated greenhouse is underway and requires additional geothermal fluid production. This report discusses the results of a cost-shared U.S. Department of Energy (DOE) and A.R. Masson, Inc. drilling project designed to construct a highly productive geothermal production well for expansion of the large commercial greenhouse at Radium Springs. The well should eliminate the potential for future thermal breakthrough from existing injection wells and the inducement of inflow from shallow cold water aquifers by geothermal production drawdown in the shallow reservoir. An 800 feet deep production well, Masson 36, was drilled on a US Bureau of Land Management (BLM) Geothermal Lease NM-3479 at Radium Springs adjacent to the A. R. Masson Radium Springs Farm commercial greenhouse 15 miles north of Las Cruces in Dona Ana County, New Mexico just west of Interstate 25 near the east bank of the Rio Grande. The area is in the Rio Grande rift, a tectonically-active region with high heat flow, and is one of the major geothermal provinces in the western United State.

James C. Witcher

2002-01-02T23:59:59.000Z

174

Evaluation of geothermal potential of Rio Grande rift and Basin and Range province, New Mexico. Final technical report, January 1, 1977-May 31, 1978  

DOE Green Energy (OSTI)

A study was made of the geological, geochemical and geophysical characteristics of potential geothermal areas in the Rio Grande rift and Basin and Range province of New Mexico. Both regional and site-specific information is presented. Data was collected by: (1) reconnaissance and detailed geologic mapping, emphasizing Neogene stratigraphy and structure; (2) petrologic studies of Neogene igneous rocks; (3) radiometric age-dating; (4) geochemical surveying, including regional and site-specific water chemistry, stable isotopic analyses of thermal waters, whole-rock and mineral isotopic studies, and whole-rock chemical analyses; and (5) detailed geophysical surveys, using electrical, gravity and magnetic techniques, with electrical resistivity playing a major role. Regional geochemical water studies were conducted for the whole state. Integrated site-specific studies included the Animas Valley, Las Cruces area (Radium Springs and Las Alturas Estates), Truth or Consequences region, the Albuquerque basin, the San Ysidro area, and the Abiquiu-Ojo Caliente region. The Animas Valley and Las Cruces areas have the most significant geothermal potential of the areas studied. The Truth or Consequences and Albuquerque areas need further study. The San Ysidro and Abiquiu-Ojo Caliente regions have less significant geothermal potential. 78 figs., 16 tabs.

Callender, J.F.

1985-04-01T23:59:59.000Z

175

www.elsevier.com/locate/tecto Diapiric emplacement in the upper crust of a granitic body: the La Bazana granite (SW Spain)  

E-Print Network (OSTI)

The ascent and emplacement of granites in the upper crust is a major geological phenomenon accomplished by a number of different processes. The active processes determine the final geometry of the bodies and, in some favourable cases, the inverse problem of deducing mechanisms can be undertaken by relying on the geometry of plutons. This is the case of the La Bazana granitic pluton, a small Variscan igneous body that intruded Cambrian rocks of the Ossa-Morena Zone (SW Iberian Massif) in the core of a large late upright antiform. The granite shows no appreciable solid-state deformation, but has a late magmatic foliation whose orientation, derived from field observations, defines a gentle dome. The regional attitude of the main foliation in the country rock (parallel to the axial plane of recumbent folds) is NWSE, but just around the granite, it accommodates to the dome shape of the pluton. Flattening in the host rock on top of the granite is indicated by boudinaged and folded veins, and appears to be caused by an upward pushing of the magma during its emplacement. The dome-shaped foliation of the granite, geometrically and kinematically congruent with the flattening in the host rock, can be related in the same way to the upward pushing of the magma. The level of final emplacement was deduced from the mineral associations in the thermal aureole to be of 710 km in depth. Models of the gravity anomaly related to the granite body show that the granite has a teardroppipe shape enlarged at its top. Diapiric ascent of the magma through the lower middle crust is inferred until reaching a high viscous level, where final emplacement accompanied by lateral expansion and vertical flattening took place. This natural example suggests

Elena Galad-enrquez; Jess Galindo-zaldvar; O Simancas; Inmaculada Expsito

2001-01-01T23:59:59.000Z

176

Upstream -- SW92-03&  

Office of Legacy Management (LM)

59 52 89 U b gL 267 272 185 227 297 313 323 175 258 284 260J 230J 320 V b gL 441 456 564 537 369 388 431 5.3 433 443 530 520 430 Radiological Alpha c,d pCiL -- -- 76.8J --...

177

Watermark: Order (2011-SW-2908)  

Energy.gov (U.S. Department of Energy (DOE))

DOE ordered Watermark Designs, Ltd. to pay a $4,200 civil penalty after finding Watermark Designs, Ltd. had manufactured and distributed in commerce in the U.S. sixty-three units of basic model SH-FAL90, a noncompliant showerhead.

178

SwA Overview Briefing  

Science Conference Proceedings (OSTI)

... Page 8. Automation is one piece ... Network Device ... distributed attack tools increase in wide-scale Trojan horse distribution Windows-based remote ...

2012-10-26T23:59:59.000Z

179

Exploratory energy research program of the University of Hawaii at Manoa. Progress report  

DOE Green Energy (OSTI)

Progress is reported from the University of Hawaii on: UHM rooftop solar energy laboratory; solar pond cleansing techniques; combustion properties of biomass pyrolysis products; high-temperature solar concentrator absorber; biological abatement of hydrogen sulfide during geothermal energy production; geothermal systems on submarine rift zones of the Hawaiian chain; nitrogenous products of OTEC chlorination; interaction of hydrogen and deuterium with transition metals and their alloys at high pressures; shallow magma chambers and geothermal potential of Haleakala, Maui; effects of OTEC waste water on phytoplankton; sodium-lithium geothermometer; breaking wave forces on OTEC pipes; seismic and thermal properties on basalts. (PSB)

Not Available

1984-01-01T23:59:59.000Z

180

Interim Report on SNP analysis and forensic microarray probe design for South American hemorrhagic fever viruses, tick-borne encephalitis virus, henipaviruses, Old World Arenaviruses, filoviruses, Crimean-Congo hemorrhagic fever viruses, Rift Valley fever  

SciTech Connect

The goal of this project is to develop forensic genotyping assays for select agent viruses, enhancing the current capabilities for the viral bioforensics and law enforcement community. We used a multipronged approach combining bioinformatics analysis, PCR-enriched samples, microarrays and TaqMan assays to develop high resolution and cost effective genotyping methods for strain level forensic discrimination of viruses. We have leveraged substantial experience and efficiency gained through year 1 on software development, SNP discovery, TaqMan signature design and phylogenetic signature mapping to scale up the development of forensics signatures in year 2. In this report, we have summarized the whole genome wide SNP analysis and microarray probe design for forensics characterization of South American hemorrhagic fever viruses, tick-borne encephalitis viruses and henipaviruses, Old World Arenaviruses, filoviruses, Crimean-Congo hemorrhagic fever virus, Rift Valley fever virus and Japanese encephalitis virus.

Jaing, C; Gardner, S

2012-06-05T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
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they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


181

Software Assurance (SwA) Automation  

Science Conference Proceedings (OSTI)

... Failure to Sanitize Directives in a Web Page (aka 'Cross-site scripting' (XSS)) (79) Failure to Sanitize Script-Related HTML Tags in a Web Page ...

2012-10-26T23:59:59.000Z

182

NETL: 2009 SW PA Science Bowl Information  

NLE Websites -- All DOE Office Websites (Extended Search)

second in the National Competition and traveled to France to visit Europe's largest nuclear power plant. 2009 Southwestern Pennsylvania Science Bowl Information Center DATE:...

183

PRE-SW EMF Workstation 2013  

Science Conference Proceedings (OSTI)

EMF Workstation 2013 allows a user to create a computer model of Transmission Lines, Distribution Lines, Buswork, and Substation Equipment. The software then calculates Electric and Magnetic Fields ...

2013-07-22T23:59:59.000Z

184

Mueller Streamline: Noncompliance Determination (2011-SW-2802...  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

to Mueller Streamline Co. finding that faucet model 120-003NL does not comport with the water conservation standards. DOE determined the product was noncompliant based on the...

185

Innovations in Nuclear Infrastructure and Education From the SW Consortium  

SciTech Connect

This report describes the final expenditures for the INIE project during FY 08/09. (There were no expenditures during FY09/10 or during FY10/11.) To see the list of accomplishments done using the INIE funds, please see the reports included here. The last of the FY 07/08 funds were brought forward and used to complete two distance education modules teaching reactor experiments. These modules and parts from the modules are still being used and are being disseminated off-campus as a part of our distance education effort. The second largest expenditure was sending students to the ANS to present student papers on work that they had done the previous year underwritten by INIE funds. The remaining expenditures were IDC charges and minor travel expenses to give students a tour of a medical facility. Once again we wish to express of sincere appreciation of the INIE program and hope that the return on investment is appreciated by the DOE. Although INIE has come to a close, looking back at all the Consortium has accomplished is astounding. And, as was hoped, these funds have proved to be a springboard for continuing work, particularly at Texas A&M. With the resurgence of nuclear power, the utilities have realized that the nuclear workforce in the near future will be too small for the task of bringing dozens of new plants on line and have turned their attention to the URRs to help feed the workforce pipeline. The distance education modules developed at the A&M are soon to be broadcast throughout the country to help train a new generation of nuclear workers. Our students at the Nuclear Science Center at being snapped up by the nuclear power plants after graduating. Our research projects at A&M have all ended with new data, new ways of looking at old problems, and produced a covey of good students. I want to say 'Thanks' with utmost sincerity because without the INIE funds our efforts would yield a small fraction of the accomplishments you see in this report.

Warren Reece

2011-03-22T23:59:59.000Z

186

U.S. Department of Energy 1000 Independence Ave, SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

of, of, ) Westinghouse Lighting Corporation ) Case Number: 2010-CE-09/1001 Issued : August 5, 2010 NOTICE OF ALLOWANCE TO RESUME DISTRIBUTION Manufacturers of certain covered products which have been determined by the Department of Energy (DOE) to be non-compliant with the applicable energy conservation standard may be allowed to resume distribution, per 10 CFR § 430.70 (a)(6)(v), if additional testing results supplied by the manufacturer results in a determination of compliance. On June 14, 2010, DOE issued a Notice of Non-Compliance Determination based on test results submitted by Westinghouse showing that certain models were noncompliant. Westinghouse later admitted that the original test results were based on testing that was not performed in accordance with

187

U.S. Department of Energy 1000 Independence Ave, SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

of: of: Aspen Manufacturing Case Number 2010-SE-0305 NOTICE OF NONCOMPLIANCE DETERMINATION CERTIFICATION Manufacturers of certain covered products are required to certify compliance with the applicable energy conservation standards through submission of a compliance statement and a certification report. 10 CFR § 430.62. See 42 U.S.C. 6296. The compliance statement is a legal statement by the manufacturer that the information provided in its certification reports is true, accurate and complete, that the basic models certified meet the applicable energy conservation standard, that the energy efficiency information report is the result of testing performed in conformance with the applicable test requirements in 10 CFR part 430, subpart B; and that the manufacturer is

188

U.S. Department of Energy 1000 Independence Ave, SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

of. of. Westinghouse Lighting Corporation Case Number : 2010-CE -09/ 1001 NOTICE OF NONCOMPLIANCE DETERMINATION CERTIFICATION Manufacturers of certain covered products are required to certify compliance with the applicable energy conservation standards through submission of a compliance statement and a certification report. 10 CFR § 430.62. See 42 U.S.C. 6296. As of April 19, 2010, Westinghouse Lighting Corporation (Westinghouse) had not filed these documents with DOE. Accordingly, DOE issued a Notice of Proposed Civil Penalty for apparent violations of the certification requirements. On June 4, 2010, Westinghouse provided to DOE a compliance statement for incandescent reflector lamps and copies of test reports for a variety of models of incandescent reflector lamps.

189

Microsoft PowerPoint - SW HydropowerCouncil-060910.pptx  

NLE Websites -- All DOE Office Websites (Extended Search)

we re headed * Does our Budget process represent our Mission? * One solution to future funding--Inland Waterways * The Problem * Study History and Results * Study History and...

190

Microsoft PowerPoint - Sadiki - SW Regional Hydropower Conference...  

NLE Websites -- All DOE Office Websites (Extended Search)

Southwestern Power Administration Western Power Administration Contracts Manitoba Hydro New Brunswick Power Corporation New York Power Authority Ontario Power...

191

Microsoft PowerPoint - Sadiki - SW Regional Hydropower Conference...  

NLE Websites -- All DOE Office Websites (Extended Search)

Operation Division Operation Division SOUTHWESTERN FEDERAL SOUTHWESTERN FEDERAL HYDROPOWER CONFERENCE HYDROPOWER CONFERENCE 12 June 2008 12 June 2008 USACE Cost Benchmarking...

192

Microsoft PowerPoint - MVD Hydrokinetics, SW Regional Hydropower...  

NLE Websites -- All DOE Office Websites (Extended Search)

Projects on the Mississippi River Mississippi River Southwestern Federal Hydropower Conference 10 June 2010 Jeff Artman, P.E. MVD Hydropower Business Line Manager Line Manager...

193

Zoe Industries: Notice of Allowance (2011-SW-2912) | Department...  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

showing that it had modified the model to be in compliance with the applicable water conservation standard. Zoe had ceased distribution of the model following DOE's...

194

Microsoft PowerPoint - SW Regional Hydropower Conference - June...  

NLE Websites -- All DOE Office Websites (Extended Search)

to Congress ( Feb ) Field Offices Develop Program Requirements ( Apr - May ) Appropriations Bills ( Jul - Sep ) Cong. Hearings ( Mar - Apr ) President Signs Approp. Bill (...

195

Microsoft PowerPoint - SW HydropowerCouncil-060910.pptx  

NLE Websites -- All DOE Office Websites (Extended Search)

STRONG 1 US Army Corps of Engineers BUILDING STRONG AGENDA * Budgets and Appropriations Trends * Where we are * Where we're headed Where we re headed * Does our Budget...

196

U.S. Department of Energy 1000 Independence Ave., SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

The problem is that it requires access to an accelerator. There are only 5 accelerators in the country providing proton therapy at U. S. medical centers, and they cost on...

197

PRE-SW Grid-IQ Harmonics Evaluation Module - Prototype  

Science Conference Proceedings (OSTI)

The application provides a user-friendly interface that would be used to perform harmonic analysis such as conducting frequency scans and harmonic distortion analysis by allowing user to select the ...

2012-09-04T23:59:59.000Z

198

Forrestal Building, 1000 Independence Avenue, S.W.,  

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

Conference Committee. Regional interest continues to focus on heating fuels, natural gas, heating oil and propane, and we are frequently briefing the Members of Congress and their...

199

District Energy SW 40th Street Thermal Plant Geothermal Project...  

Open Energy Info (EERE)

plant. In fact, although the geothermal system requires a higher initial investment, the energy savings results in an 8.7% total savings over a 25 year period. The energy savings...

200

U.S. Department of Energy 1000 Independence Ave, SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Advanced Distributor Products ) Case Number 2010-SE-0304 NOTICE OF NONCOMPLIANCE DETERMINATION CERTIFICATION Manufacturers of certain covered products are required to certify compliance with the applicable energy conservation standards through submission of a compliance statement and a certification report. 10 CFR § 430.62. See 42 U.S.C. 6296. The compliance statement is a legal statement by the manufacturer that the information provided in its certification reports is true, accurate and complete, that the basic models certified meet the applicable energy conservation standard, that the energy efficiency information report is the result of testing performed in conformance with the applicable test requirements in 10 CFR part 430, subpart B; and that the manufacturer is

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


201

U.S. Department of Energy 1000 Independence Ave, SW  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Case Number: 2010-SE-0103 Case Number: 2010-SE-0103 Whirlpool Corporation ) NOTICE OF COMPLIANCE DETERMINATION Issued on: July 08, 2010 On April 5, 2010, the Department of Energy (DOE) issued a Request for Data to Whirlpool Corporation (Whirlpool) in response to information received by DOE indicating that Whirlpool's Maytag refrigerator-freezer model "MSD2578VE" exceeds the applicable Federal energy conservation standard. On April 29, 2010, Whirlpool submitted to DOE a summary chart of its test data for the Maytag refrigerator-freezer model "MSD2578VE." In response to DOE's request for the underlying test data that formed the basis for the summary chart, Whirlpool submitted the raw test data to DOE on May 18, 2010. Whirlpool's Maytag refrigerator-freezer model "MSD2578VE" was selected for testing as part

202

Microsoft PowerPoint - MVD Hydrokinetics, SW Regional Hydropower...  

NLE Websites -- All DOE Office Websites (Extended Search)

* Free Flow Power Corporation (generators mounted on poles placed in the river bottom) * Hydro Green Energy (barge mounted generators) * MarMC Enterprises (generators submerged in...

203

FT-ICR `'u,SJ"-,t[OE",Z-- "OESw`Sw@HSwOEnOE<<@SBHSwU  

E-Print Network (OSTI)

/s),?,æ,Á,?·C"w^³3·~10-10 Torr ,?·,·^DFig. 3 ,?·¶·"·ª,?,ÍOE·[U·[·ö"-NX^·[OE¹,ª, ,é,ª

Maruyama, Shigeo

204

Electromagnetic exploration of the Exmouth and Vring rifted margins  

E-Print Network (OSTI)

Cox (1996) and patented by ExxonMobil (Lu and Srnka, 2005).to-peak output current. ExxonMobil have patented several

Myer, David Gerard

2012-01-01T23:59:59.000Z

205

Continental rifting across the Southern Gulf of California  

E-Print Network (OSTI)

earthquake in the Aleutian Islands . . . . . . . . . .from a 4.4 Ms event in the Aleutian Islands- both OSN1 and4.4 Ms shallow earthquake in the Aleutian Islands. Location

Sutherland, Fiona Helen

2006-01-01T23:59:59.000Z

206

Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical...  

Open Energy Info (EERE)

water as steam and produces a cooler saline shallow aquifer. The high partial pressure of carbon dioxide (about 30 bar in the reservoir) depresses the water table and restricts...

207

Mauna Loa Southwest Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Well Field Information Development Area: Number of Production Wells: Number of Injection Wells: Number of Replacement Wells: Average Temperature of Geofluid: Sanyal...

208

Data Acquisition-Manipulation At Rio Grande Rift Region (Morgan...  

Open Energy Info (EERE)

References Paul Morgan, Peter Barkmann, Charles Kluth, Matthew Sares (2010) Prospects For Electricity Generation In The San Luis Basin, Colorado, Usa Retrieved from "http:...

209

Static Temperature Survey At Rio Grande Rift Region (Morgan,...  

Open Energy Info (EERE)

References Paul Morgan, Peter Barkmann, Charles Kluth, Matthew Sares (2010) Prospects For Electricity Generation In The San Luis Basin, Colorado, Usa Retrieved from "http:...

210

Organic Geochemical and tectonic evolution of the Midcontinent Rift system  

SciTech Connect

The older assemblages stand in contrast with the ca. 1000 Ma old Hunting Formation, Arctic Canada, which contains what may be the oldest evidence for modem algae - red algal fossils that compare closely with members of the extant family Bangiophyceae (Butterfield et al., 1990). Taken together the Nonesuch, Shaler, Hunting and other assemblages support the hypothesis of a major episode of eukaryotic diversification ca. 1000 Ma ago. Prior to this time, eukaryotic primary producers must have been physiologically primitive (and now extinct) algae whose abundance in ecosystems is poorly constrained by analogies with the present oceans. Cyanobacteria were major primary producers in a wide range of marine environments. After 1000 Ma, diversifying red green and chromophyte algae contributed significantly to primary production in all save microbial mat communities in restricted environments. It bears mention that such mat communities remained significant potential sources of buried organic matter until the end of the Proterozoic, necessitating exploration strategies that differ from those commonly employed for younger rocks (Knoll, in press). As in Phanerozoic basins, petroleum exploration in Proterozoic rocks requires tools for stratigraphic correlation. In Neoproterozoic (<1000 Ma) rocks, biostratigraphy is possible, and it is aided significantly by C and Sr isotopic chemostratigraphy. New data from the Shaler Group contribute to the construction of C and Sr isotopic curves for Neoproterozoic time, making possible much improved chronostratigraphy for this time interval. (Asmerom et al., 1991; Hayes et al., ms. in preparation).

Hayes, J.M.; Pratt, L.M. (Indiana Univ., Bloomington, IN (United States)); Knoll, A.H. (Harvard Univ., Cambridge, MA (United States). Dept. of Organismal and Evolutionary Biology)

1992-01-01T23:59:59.000Z

211

Rio Grande Rift Geothermal Region | Open Energy Information  

Open Energy Info (EERE)

Buildings Clean Energy Economy Coordinated Low Emissions Assistance Network Geothermal Incentives and Policies International Clean Energy Analysis Low Emission Development...

212

Magnetotellurics At Rio Grande Rift Region (Aiken & Ander, 1981...  

Open Energy Info (EERE)

Mark E. Ander (1981) A Regional Strategy For Geothermal Exploration With Emphasis On Gravity And Magnetotellurics Retrieved from "http:en.openei.orgwindex.php?titleMagnetote...

213

Geologic Characterization of the South Georgia Rift Basin for...  

NLE Websites -- All DOE Office Websites (Extended Search)

Resources Institute University of South Carolina - Columbia Carbon Storage Program Infrastructure Annual Review Meeting Pittsburgh, PA November 15-17, 2011 Carbon Storage Program...

214

Assessing the extent of carbonate deposition in early rift settings  

E-Print Network (OSTI)

of trona, mirabolite and halite are present at the surface and can be as much as 3 m in thickness (Friedman

Purkis, Sam

215

Magnetotellurics At Kilauea Southwest Rift And South Flank Area...  

Open Energy Info (EERE)

the funds available to work at the Fort Bidwell Indian reservation where characterization work could be done at relatively low cost. We decided to perform a time lapse SP survey...

216

Microsoft PowerPoint - SW Regional Hydropower Conference - June 2007.ppt  

NLE Websites -- All DOE Office Websites (Extended Search)

of Engineers® of Engineers® Vision Statement Vision Statement Be the premier stewards of entrusted hydropower resources US Army Corps of Engineers® Mission Statement Mission Statement Provide reliable hydroelectric power services at the lowest possible cost, consistent with sound business principles, in partnership with other Federal hydropower generators, the Power Marketing Administrations, and Preference Customers, to benefit the Nation. US Army Corps of Engineers® Mission Statement Mission Statement Provide reliable hydroelectric power services at the lowest possible cost, consistent with sound business principles, in partnership with other Federal hydropower generators, the Power Marketing Administrations, and Preference Customers, to benefit the Nation. US Army Corps

217

PRE-SW Dynamic Mercury Cycling Model (D-MCM)Version 4.0, Beta  

Science Conference Proceedings (OSTI)

The Dynamic Mercury Cycling Model (D-MCM) is a Windows based simulation model for personal computers. It predicts mercury cycling and bioaccumulation in aquatic systems. Mercury forms include methylmercury, Hg(II), and elemental mercury. D-MCM is a time-dependent mechanistic model that can be applied deterministically or probabilistically. Version 4.0 is a major update to D-MCM. The model can be applied in 1,2, and 3 dimensional applications for lakes, rivers, estuaries, ...

2013-09-17T23:59:59.000Z

218

PRE-SW PTX Transformer Fleet Management Version 1.0, Beta  

Science Conference Proceedings (OSTI)

The PTX Transformer Fleet Management Software utilizes a Rule-Based MYCIN Expert System to assess the condition of a fleet of transformers using readily available condition and transformer description (nameplate) data. The end result is a series of indices for each transformer that provide insight into the condition of the cellulose insulation system and the potential for any abnormal incipient fault. These indices can be used to guide further diagnostic testing and maintenance actions ...

2012-09-12T23:59:59.000Z

219

OCEAN DRILLING PROGRAM CUMULATIVE INDEX GEOGRAPHIC AND SITE INDEX 1AABW Africa SW  

E-Print Network (OSTI)

with marine mam- mal research protocols. A second acoustic source north of the Hawaiian island of Kauai by a Russian group who have detected the Kauai Source transmissions using a receiver near Kamchatka. This Russian group is interested in continuing to receive the transmis- sions from the Kauai acoustic source

220

Microsoft PowerPoint - SW Fed Hydro Conference Jun 12 presentation Final [Compatibility Mode]  

NLE Websites -- All DOE Office Websites (Extended Search)

Projects Projects Impacting Federal Projects Impacting Federal Power Tulsa District Tulsa District Beau Biffle Beau Biffle 13 June 2012 BUILDING STRONG ® Topics Topics  Interior Least Tern Operations and Habitat Creation  Tulsa Vision 2025  Dam Safety Issues ► Keystone ► Pine Creek ► Tenkiller  Lake Eufaula Advisory Committee  Lake Eufaula Advisory Committee  Tenkiller Downstream Fishery Issues  Broken Bow Seasonal Pool Update - Cultural Broken Bow Seasonal Pool Update Cultural Resources Impacts  Arkansas River Navigation Improvement BUILDING STRONG ®  Oklahoma Comprehensive Water Plan Update Interior Least Tern Operations and H bit t C ti Habitat Creation  2011 Breeding Season Survey Results: - Arkansas River System: 517 adults, 358 fledglings. Season totals exceeded

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
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We encourage you to perform a real-time search of NLEBeta
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221

SILO LILLI SID NEY SW BIG SPRINGS SLOSS LITT LE H OOT SILO JUR  

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

BOE Reserve Class BOE Reserve Class No 2001 reserves 0.1 - 10 MBOE 10.1 - 100 MBOE 100.1 - 1,000 MBOE 1,000.1 - 10,000 MBOE 10,000.1- 100,000 MBOE > 100,000 MBOE Basin Outline The mapped oil and gas field boundary outlines were created by the Reserves and Production Division, Office of Oil and Gas, Energy Information Administration pursuant to studies required by Section 604 of the Energy Policy and Conservation Act Amendments of 2000 (P.L. 106-469). The boundaries are not informed by subsurface structural information. The data and methods used in their creation are detailed in a report, "Scientific Inventory of Onshore Federal Lands' Oil and Gas Resources and Reserves and the Extent and Nature of Restrictions to Their Development", prepared by the US Departments of Interior, Agriculture and Energy.

222

SILO LILLI SID NEY SW BIG SPRINGS SLOSS LITT LE H OOT SILO JUR  

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

Liquids Reserve Class Liquids Reserve Class No 2001 liquids reserves 0.1 - 10 Mbbl 10.1 - 100 Mbbl 100.1 - 1,000 Mbbl 1,000.1 - 10,000 Mbbl 10,000.1- 100,000 Mbbl Basin Outline The mapped oil and gas field boundary outlines were created by the Reserves and Production Division, Office of Oil and Gas, Energy Information Administration pursuant to studies required by Section 604 of the Energy Policy and Conservation Act Amendments of 2000 (P.L. 106-469). The boundaries are not informed by subsurface structural information. The data and methods used in their creation are detailed in a report, "Scientific Inventory of Onshore Federal Lands' Oil and Gas Resources and Reserves and the Extent and Nature of Restrictions to Their Development", prepared by the US Departments of Interior, Agriculture and Energy.

223

Reading Room 1E-190, Forrestal Building, 1000 Independence Ave., SW.,  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

239 / Thursday, December 14, 1989 / Notices 239 / Thursday, December 14, 1989 / Notices Public Participation: The meeting is open to the public. The Chairperson of the Panel is empowered to conduct the meeting in a fashion that will, in the Chairperson's judgment, facilitate the orderly conduct of business. Any member of the public who wishes to make oral statements pertaining to agenda items should contact the Executive Director at the address or telephone number listed above. Requests must be received at least 5 days prior to the meeting and reasonable provision will be made to include the presentation on the agenda. It is requested that oral presenters provide 15 copies of their statements at the time of their presentations. Minutes: Available for public review and copying approximately 30 days following the meeting at the Public

224

HW/SW for an intelligent transducer network based on IEEE 1451 standard  

Science Conference Proceedings (OSTI)

This work describes a hardware/software co-design system development, named IEEE 1451 platform, to be used in process automation. This platform intends to make easier the implementation of IEEE standards 1451.0, 1451.1, 1451.2 and 1451.5. The hardware ... Keywords: FPGA, IEEE 1451 standard, Intelligent transducers, NIOS II processor

E. A. Batista; L. Gonda; A. C. R. da Silva; S. R. Rossi; M. C. Pereira; A. A. de Carvalho; C. E. Cugnasca

2012-01-01T23:59:59.000Z

225

PRE-SW: Substation Condition Monitoring and Implementation Database Version 2.0  

Science Conference Proceedings (OSTI)

The Substation Sensor Database provides a searchable database of sensors available to substation engineers, categorized by Area, Component, Sub-Component, Parameter, and Technology. By specifying each category, the list can be filtered to a sub-set of sensors. By clicking on a sensors name, details can be viewed including a description, sensor maturity, and a link to the manufacturer. Through data-mining of this database substation engineers could work on the development of ...

2013-08-30T23:59:59.000Z

226

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive D  

E-Print Network (OSTI)

% Biomass 1% Petroleum & Pet Coke of conservation savings, far exceeding the Council's target of 200 average megawatts. The levelized cost for energy efficiency achievements. In addition, the achievements were low cost, at or below what

227

Independent Scientific Review Panel for the Northwest Power and Conservation Council, 851 SW 6th  

E-Print Network (OSTI)

programmatic goals. Another fundamental problem in other previous efforts was inadequate funding to implement actions. The document should describe how this plan would overcome these fundamental pitfalls to make & Management of Savanna Heterogeneity, Island Press, Washington, D.C. Handbook of Ecological Restoration

228

PRE-SW Crossarm Inspection and Evaluation Web-based Training (WBT)1.0, Beta  

Science Conference Proceedings (OSTI)

The EPRI Crossarm Inspection and Evaluation WBT provides interactive instruction on the identification, explanation for, and rating of the various conditions and factors that commonly affect wood, steel, and fiber-reinforced plastic (FRP) crossarms. Attention is given to identifying the types of structures (such as single-pole, double-pole, H-frame, and guyed) and conditions commonly observed in each. Visual examples of the degradation factors, the Maintenance Priority Rating, and ...

2013-09-01T23:59:59.000Z

229

UCRL-JC-116524 PREPRINT The Beaverhead Impact Structure, SW Montana...  

Office of Scientific and Technical Information (OSTI)

was originally Precambrian, the variable ages suggest varying degrees of thermal resetting. Preliminary paleomagnetic results from 11 samples from one body of...

230

Microsoft PowerPoint - SwRI CO2 Compressor Project-IGTI07.ppt  

NLE Websites -- All DOE Office Websites (Extended Search)

Concepts for the Compression of Large Volumes of CO 2 Dr. Jeffrey Moore Dr. Jeffrey Moore Dr. Klaus Brun Dr. Klaus Brun Ms. Marybeth Nored Ms. Marybeth Nored Mr. Ryan Gernentz Mr....

231

Coal resource estimation in the Bayir field, Yatagan-Mugla, SW Turkey  

SciTech Connect

This study focuses on some coal properties and calculation of coal resources with two classical (isopach and polygon) methods in the Bayir field, Yatagan-Mugla, which is located in southwestern Anatolia. This field has not been mined because it is still in the exploration stage. A productive coal seam of Early (?)-Middle Miocene age has a mineable coal thickness of 1.25 m to 18.01 m. Proximate analysis results indicated that this coal seam contains high moisture, ash, volatile matter, total sulphur content, and net calorific values. The weighted average mineable coal thickness calculated from the isopachs is 7.52 m and 7.82 m from polygonal methods. The in situ tonnages with isopach and polygonal methods were calculated to be 122.8 Mt and 130 Mt, respectively. The average value of the two methods shows 126.4 Mt in situ coal tonnages. Total amount of the in situ mineable coal resources is 77.7 Mt, which indicates an important coal potential in the Bayir field. The overburden thickness ranges from 72 m to 493 m in the Bayir field, averaging 257 m, indicating a deep coal mine. The overburden ratio averages 37 m{sup 3}/ton, indicating an underground coal mine to feed a power plant in near future.

Inaner, H.; Nakoman, E.; Karayigit, A.I. [Dokuz Eylul University, Buca Izmir (Turkey). Dept. of Geological Engineering

2008-07-01T23:59:59.000Z

232

An environmental control HW/SW framework for daily living of elderly and disabled people  

Science Conference Proceedings (OSTI)

A home control system is presented, based on standard IP LAN techniques. The system features large flexibility, dynamic reconfigurability, fault-tolerance and low costs. An integrated hardware/software framework has been conceived, which support device ... Keywords: electronic aids for daily living, remote services, smart homes

Guido Matrella; Ferdinando Grossi; Valentina Bianchi; Ilaria De Munari; Paolo Ciampolini

2008-04-01T23:59:59.000Z

233

PRE-SW Model Assisted Probability of Detection (MAPOD-R) Version 2.0, Beta  

Science Conference Proceedings (OSTI)

MAPOD-R, Version 1.0 was developed in 2009 using Crystal Ball statistical software. This software is expensive and has to be purchased and maintained by each utility. There is statistics software that is free and publically available called 8220R8221. The contractor will develop scripts using R to create the same output as MAPOD Version 1.0 creates. WindowsXP/Vista/7, Excel 2003 and 2007

2012-04-22T23:59:59.000Z

234

PRE-SW Insulator Calculation Engine (ICE) Version 2.0, Beta  

Science Conference Proceedings (OSTI)

ICE determines the electric field (E-field) distribution on transmission line polymer insulators (also called NCI or composite insulators) and aids in the selection of the appropriate corona ...

2013-09-08T23:59:59.000Z

235

PRE-SW Insulator Calculation Engine (ICE) Version 2.0, Beta  

Science Conference Proceedings (OSTI)

ICE determines the electric field (E-field) distribution on transmission line polymer insulators (also called NCI or composite insulators) and aids in the selection of the appropriate corona ring.Benefits & Value:Determine the appropriate application of corona rings on transmission line polymer insulators enabling life expectancy.Simple data entry of information selected from pre-populated structure, insulator and hardware ...

2013-09-08T23:59:59.000Z

236

PRE-SW Aging Chamber Report Tool (ACRT) Version 6.0, Beta  

Science Conference Proceedings (OSTI)

The 230kV Accelerated Aging Chamber is a multi-year test of more than 50 polymer and fiberglass components. Photographic inspections occur twice a year. Thousands of photographs accumulate making conventional reports difficult to read. This reporting tool enables the reader to jump from component to component and inspection to inspection. The reader can easily compare components at different levels of aging. This tool will make reviewing the important results of this ...

2013-08-11T23:59:59.000Z

237

PRE-SW Plug-in Electric Vehicle Load Estimator 0.81 BETA  

Science Conference Proceedings (OSTI)

The Plug-in Electric Vehicle Load Estimator generates forecasts of new plug-in vehicle sales in a specific geographical area and calculates relevant data including cumulative PEV market penetration, electricity demand of PEVs, and gasoline saved. The software calculates results for any time period from calendar year 2010 through 2050 based on a user-defined list of counties and a set of assumptions such as electricity and gasoline price forecasts. The county list may optionally include fractions that def...

2010-08-09T23:59:59.000Z

238

PRE-SW: Transformer Forensics Database Version 2.0, Beta  

Science Conference Proceedings (OSTI)

EPRI has been engaged in research on forensics related to transformer failures and decommissioning. There is a need to make this information available to EPRI members in an easily accessible ...

2013-09-21T23:59:59.000Z

239

PRE-SW Utility Energy Efficiency Potential Calculator v2.0, Beta  

Science Conference Proceedings (OSTI)

With the promulgation of energy efficiency savings mandates in many states and other jurisdictions, utilities and policy makers have a keen interest in understanding the potential for energy efficiency at the national, regional, subregional, state, and service-territory levels. Many load serving entities are required by their regulatory commissions to submit energy efficiency potential filings on a periodic basis; these undertakings typically require significant investment in consultants. ...

2013-09-01T23:59:59.000Z

240

GTOP for Siemens-Westinghouse (SW) 501F Version 1.0  

Science Conference Proceedings (OSTI)

The GTOPSIEMENS-WESTINGHOUSE 501F software enables users to plan, manage, and document major overhauls of Siemens Energy Model SGT6-5000F simple cycle gas turbines and electric generators. The GTOPSIEMENS-WESTINGHOUSE 501F software has been developed to aid the power industry with economic and efficient planning, scheduling and execution of major overhauls of Siemens Energy Model SGT6-5000F simple cycle gas turbine generator units using computer-based techniques. This Gas Turbine Overhaul Plan (GTOPis p...

2010-12-02T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


241

Microsoft Word - 4.2 AH FINAL Remarkable Rocks SW.docx  

NLE Websites -- All DOE Office Websites (Extended Search)

Claire Roybal of Claire Roybal & Associates Ltd. Pajarito Plateau Field Science Curriculum 4 th Grade Lesson 2 Page 9 OVERVIEW OF LESSON In this activity, students will...

242

A NUMERICAL ANALYSIS OF THE SINGLE-WELL STEAM ASSISTED GRAVITY DRAINAGE (SW-SAGD) PROCESS  

E-Print Network (OSTI)

commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does and surrounding rock. Hot oil and condensed water drain though the force of gravity to a production well condenses as heat is transferred to the oil. Condensed water and hot oil flow along the steam chamber

243

Hopper OS upgrade and new SW set to default next Wed, Feb 27  

NLE Websites -- All DOE Office Websites (Extended Search)

parallel-netcdf1.3.1 -- perftools6.0.1 -- papi5.0.1 -- atp1.6.0 -- stat1.2.1.3 -- javajdk1.7.007 -- xt-asyncpe5.16 The availability of the above software versions were...

244

PRE-SW Inspection Technology and Sensor Database v3.0, Beta  

Science Conference Proceedings (OSTI)

The Inspection Technology and Sensor Database provides a searchable database of sensors available to overhead transmission engineers, categorized by Area, Component, Sub-Component, Parameter, and Technology. By specifying each category, the list can be filtered to a sub-set of sensors. By clicking on a sensors name, details can be viewed including a description, sensor maturity, and a link to the manufacturer. Through data-mining of this database substation engineers could work on ...

2013-09-02T23:59:59.000Z

245

PRE-SW Energy Storage Valuation Tool (ESVT) Version 4.0, Beta  

Science Conference Proceedings (OSTI)

The Energy Storage Valuation Tool (ESVT) Version 4.0 is an energy storage cost-benefit analysis simulation tool, based on ...

2013-10-07T23:59:59.000Z

246

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network (OSTI)

of natural gas electricity generation for coal, increased use of natural gas vehicles, increased demand. In contrast the low forecast would be consistent with conditions that limit the demand for natural gas affect the plan or the region. Last August, Council updated its long-term outlook for natural gas

247

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network (OSTI)

/province updates September Power Committee Meeting 1. Reviewed updates to the demand and natural gas price assumptions § Cases with high and low demand as well as high and low natural gas prices § Finalize update and natural gas price forecasts 2 #12;9/27/2012 2 Seasonal Patterns of Electricity Price at Mid-C 3 0 10 20 30

248

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network (OSTI)

percent today. n The share of single family homes with dishwashers has grown from about two-thirds in 1992 to nearly 90 percent today. n The average single family household does about 170 dishwasher loads of per 2010 2030 Clothes Washer Other Non-Subs Freezer Dishwasher Air Condition Refrigeration Clothes Dryer

249

PRE-SW Transmission Line Workstation - Generation 2, Version 1.2, Beta  

Science Conference Proceedings (OSTI)

This is a complete rewrite of the platform supporting the Transmission Line Workstation. The aim is to provide a common platform to share data and support tools between existing and future T&S software. This release adds Vibration and OpenDSS Fault calculations to the initial TFlash and ACDC line calculations.Benefits & Value:Simplified data input by sharing between applicationsCreate common look and feel between ...

2013-08-20T23:59:59.000Z

250

Estimation of methane flux offshore SW Taiwan and the influence of tectonics on gas hydrate accumulation  

E-Print Network (OSTI)

­510 INTRODUCTION Gas hydrates are naturally occurring solids, nonstoichio- metric clathrates, stable at relatively and in sedimentary strata of continen- tal deep sea areas and are typically composed of natural gas, mainly methane have suggested that methane concentra- tions play an important role in gas hydrate investigations. Very

Lin, Andrew Tien-Shun

251

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network (OSTI)

is becoming more important. action item ANLYS-8. ANLYS-8: Improve natural gas demand forecasting. demand important. This was identified in the Action Plan at Improve natural gas demand forecasting. Work TO: Power Committee FROM: Massoud Jourabchi SUBJECT: Enhancing Natural Gas Demand Forecasting

252

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network (OSTI)

to estimate future natural gas consumption, future CO2 production, and future export/import markets. 2 #12 at natural gas consumption, CO2 production, export/import results, runs with & without system wide CO2 § Updates to the model inputs include: ­ Demand Forecast ­ Natural Gas Price Forecast ­ A comprehensive

253

PRE-SW Strategic Capacity Axial Compressor Maintenance Program (SCAMP) Version 3.0, Beta  

Science Conference Proceedings (OSTI)

The Strategic Capacity Axial-Compressor Maintenance Program (SCAMP) spreadsheet provides combustion turbine operators with a low-cost, easy-to-install, easy-to-use program for monitoring combustion turbine axial compressor and overall turbine performance. It can be used to diagnose the condition of axial compressors and to determine the benefits of maintenance actions such as an off-line compressor wash.Benefits & ...

2012-09-23T23:59:59.000Z

254

PRE-SW EPRI Overhead Transmission Line Inspection - Online Training (OTLOT) Version 9.0, Beta  

Science Conference Proceedings (OSTI)

The EPRI Overhead Transmission Line Inspection - Online Training is a CD-based application for training on how to complete overhead transmission line inspections.Itcontains fourteen modules of instruction on overhead transmission line inspections. A browser interface helps the user navigate through the interactive training. As the user moves through the module, it provides instruction, application practice, and review questions.Benefits ...

2013-08-25T23:59:59.000Z

255

Preliminary Analysis of ARM SGP Area Sky Cover and Downwelling SW Irradiance  

NLE Websites -- All DOE Office Websites (Extended Search)

Clarifying and Implementing a Stricter DOD Definition Across Datastreams Clarifying and Implementing a Stricter DOD Definition Across Datastreams C. Sivaraman, B. Ermold, M. Macduff Pacific Northwest National Laboratory Definition of DOD: All dimension, attribute and variable types and names are considered part of a DOD. A change in any part of the DOD is considered a version change. Outcomes: ACRF enforces greater consistency in data Downstream users benefit (DQ, VAPs, scientists) Identify inconsistencies across datastreams Datastream development is more efficient BODS interface, updated libraries Improved data analysis tools for ACRF and ARM Visual Datastream history tool (below) Issues with current DOD history: The DOD History page: http://science.arm.gov/tool/dod/showdod.php * Tracks both content and structure. * Needs Custom Configuration

256

SILO LILLI SID NEY SW BIG SPRINGS SLOSS LITT LE H OOT SILO JUR  

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

Gas Reserve Class Gas Reserve Class No 2001 gas reserves 0.1 - 10 MMCF 10.1 - 100 MMCF 100.1 - 1,000 MMCF 1,000.1 - 10,000 MMCF 10,000.1- 100,000 MMCF > 100,000 MMCF Basin Outline The mapped oil and gas field boundary outlines were created by the Reserves and Production Division, Office of Oil and Gas, Energy Information Administration pursuant to studies required by Section 604 of the Energy Policy and Conservation Act Amendments of 2000 (P.L. 106-469). The boundaries are not informed by subsurface structural information. The data and methods used in their creation are detailed in a report, "Scientific Inventory of Onshore Federal Lands' Oil and Gas Resources and Reserves and the Extent and Nature of Restrictions to Their Development", prepared by the US Departments of Interior, Agriculture and Energy.

257

Influence of a Tropical Island Mountain on Solar Radiation, Air Temperature and Vapor Pressure  

Science Conference Proceedings (OSTI)

Measured solar radiation, air temperature, and water vapor pressure at 17 stations on the northwest flank of Haleakala, Maui, Hawaii are compared with modeled clear day solar radiation and free atmosphere air temperature and water vapor pressure. ...

Dennis Nullet

1989-03-01T23:59:59.000Z

258

Model for trace metal exposure in filter-feeding flamingos at alkaline Rift Valley Lake, Kenya  

SciTech Connect

Toxic trace metals have been implicated as a potential cause of recent flamingo kills at Lake Nakuru, Kenya. Chromium (Cr), copper (Cu), lead (Pb), and zinc (Zn) have accumulated in the lake sediments as a result of unregulated discharges and because this alkaline lake has no natural outlet. Lesser flamingos (Phoeniconaias minor) at Lake Nakuru feed predominantly on the cyanobacterium Spirulina platensis, and because of their filter-feeding mechanism, they are susceptible to exposure to particle-bound metals. Trace metal adsorption isotherms to lake sediments and S. platensis were obtained under simulated lake conditions, and a mathematical model was developed to predict metal exposure via filter feeding based on predicted trace metal phase distribution. Metal adsorption to suspended solids followed the trend Pb {much_gt} Zn > Cr > Cu, and isotherms were linear up to 60 {micro}g/L. Adsorption to S. platensis cells followed the trend Pb {much_gt} Zn > Cu > Cr and fit Langmuir isotherms for Cr, Cu and Zn and a linear isotherm for Pb. Predicted phase distributions indicated that Cr and Pb in Lake Nakuru are predominantly associated with suspended solids, whereas Cu and Zn are distributed more evenly between the dissolved phase and particulate phases of both S. platensis and suspended solids. Based on established flamingo feeding rates and particle size selection, predicted Cr and Pb exposure occurs predominantly through ingestion of suspended solids, whereas Cu and Zn exposure occurs through ingestion of both suspended solids and S. platensis. For the lake conditions at the time of sampling, predicted ingestion rates based on measured metal concentrations in lake suspended solids were 0.71, 6.2, 0.81, and 13 mg/kg-d for Cr, Cu, Pb, and Zn, respectively.

Nelson, Y.M.; DiSante, C.J.; Lion, L.W. [Cornell Univ., Ithaca, NY (United States). School of Civil and Environmental Engineering; Thampy, R.J.; Raini, J.A. [Worldwide Fund for Nature, Nakuru (Kenya). Lake Nakuru Conservation and Development Project; Motelin, G.K. [Egerton Univ., Njoro (Kenya). Dept. of Animal Health

1998-11-01T23:59:59.000Z

259

A NEW SPECIES OF BOUBOU (MALACONOTIDAE: LANIARIUS) FROM THE ALBERTINE RIFT  

E-Print Network (OSTI)

.pone.0002502. #12;N. Rajakaruna and R.S. Boyd2009 7 Mittermeier, R.A., P.R. Gil, M. Hoffman, J. Pilgrim, T

Kelly, John J.

260

Late Jurassic rifting along the Australian North West Shelf: margin geometry and spreading ridge  

E-Print Network (OSTI)

and extends over 2400 km from the Arafura Sea between northern Australian and Irian Jaya in the east, up

Müller, Dietmar

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


261

Outside influences and ruling Iran : the emergence of the rift with the West.  

E-Print Network (OSTI)

??Since the establishment of a united, Shia Persian empire in 1501 through to the overthrow of the last Shah in the Islamic Revolution, Iran and (more)

Campbell, Alana

2009-01-01T23:59:59.000Z

262

Organic Geochemical and tectonic evolution of the Midcontinent Rift system. Final report  

SciTech Connect

The older assemblages stand in contrast with the ca. 1000 Ma old Hunting Formation, Arctic Canada, which contains what may be the oldest evidence for modem algae - red algal fossils that compare closely with members of the extant family Bangiophyceae (Butterfield et al., 1990). Taken together the Nonesuch, Shaler, Hunting and other assemblages support the hypothesis of a major episode of eukaryotic diversification ca. 1000 Ma ago. Prior to this time, eukaryotic primary producers must have been physiologically primitive (and now extinct) algae whose abundance in ecosystems is poorly constrained by analogies with the present oceans. Cyanobacteria were major primary producers in a wide range of marine environments. After 1000 Ma, diversifying red green and chromophyte algae contributed significantly to primary production in all save microbial mat communities in restricted environments. It bears mention that such mat communities remained significant potential sources of buried organic matter until the end of the Proterozoic, necessitating exploration strategies that differ from those commonly employed for younger rocks (Knoll, in press). As in Phanerozoic basins, petroleum exploration in Proterozoic rocks requires tools for stratigraphic correlation. In Neoproterozoic (<1000 Ma) rocks, biostratigraphy is possible, and it is aided significantly by C and Sr isotopic chemostratigraphy. New data from the Shaler Group contribute to the construction of C and Sr isotopic curves for Neoproterozoic time, making possible much improved chronostratigraphy for this time interval. (Asmerom et al., 1991; Hayes et al., ms. in preparation).

Hayes, J.M.; Pratt, L.M. [Indiana Univ., Bloomington, IN (United States); Knoll, A.H. [Harvard Univ., Cambridge, MA (United States). Dept. of Organismal and Evolutionary Biology

1992-12-31T23:59:59.000Z

263

Drilling investigations of crustal rifting processes in the Salton Trough, California  

DOE Green Energy (OSTI)

The paper describes the results of CSDP activities in the Salton Sea Geothermal Field (SSGF), concentrating on a shallow heat-flow survey, but also considering preliminary results from the Salton Sea Scientific Drilling Program (SSSDP). Whether the heat input rate to localized systems is high enough to account for the overall thermal budget of the Salton Trough is examined. (ACR)

Kasameyer, P.W.; Younker, L.W.; Newmark, R.L.; Duba, A.G.

1986-01-01T23:59:59.000Z

264

Dynamics of ice shelf rift propagation and iceberg calving inferred from geodetic and seismic observations  

E-Print Network (OSTI)

2. Ice Shelves . . . . . . . . . . . . . . . . .5. Ice Rheology . . . . . . . . . . . . . 6.vi Calving Glaciers and Ice

Bassis, Jeremy N.

2007-01-01T23:59:59.000Z

265

Isotopic Geochemistry and Hydrology of Geothermal Waters in the Ethiopian Rift Valley  

E-Print Network (OSTI)

evidence subsurface water-rock source for a reaction in thissuch source water undergoes isotopic exchange with rocks totype source waters are modified by interaction with rocks to

Isotope Laboratory, Scripps Institution of Oceanography

1977-01-01T23:59:59.000Z

266

Flow and Mixing in the Rift Valley of the Mid-Atlantic Ridge  

Science Conference Proceedings (OSTI)

High levels of diapycnal mixing and geothermal heating near midocean ridges contribute to the buoyancy fluxes that are required to close the global circulation. In topographically confined areas, such as the deep median valleys of slow-spreading ...

A. M. Thurnherr; K. J. Richards; C. R. German; G. F. Lane-Serff; K. G. Speer

2002-06-01T23:59:59.000Z

267

Pre-SW - Steam Generator Management Program: Flaw Handbook Calculator for Excel 2010, Version 2.0  

Science Conference Proceedings (OSTI)

The EPRI Steam Generator Management Program: Steam Generator Degradation Specific Flaw Handbook (1019037) defines burst pressure equations for steam generator tubes with various degradation morphologies, and the EPRI Steam Generator Management Program: Steam Generator Integrity Assessment Guidelines (1019038) describes a probabilistic evaluation process which can be used to account for key input parameter uncertainties. The Flaw Handbook Calculator software is an automated ...

2013-11-20T23:59:59.000Z

268

Molecular Dynamics of Formation Process of Fullerene "`@@SZRvi"OE`Hj <@Sw@@ZROEN--i"OE`H@j  

E-Print Network (OSTI)

,µ·Ct·[OE"·\\`¢,ðOE`·¬,·,é?"\\·«,?,?,¢,? OEY"¢,µ,½·DFig. 1 ,?·"x,ð3000K ,?·§OEä,µ,½OEn,?,?OEvZZOE

Maruyama, Shigeo

269

GEOCHEMICAL PHASE DIAGRAMS AND GALE P.H. EDELMAN, S.W. PETERSON, V. REINER, AND J.H. STOUT  

E-Print Network (OSTI)

ater steam Steam 100 1 Pressure(bar) steam ice Figure 1. The phase diagram for the simple chemical system with phases ice, water, and steam. 1. Introduction A central problem in geochemistry has been illustrates the familiar phase diagram for a simple chemi- cal system that involves three phases (ice, water

Reiner, Victor

270

GEOCHEMICAL PHASE DIAGRAMS AND GALE P.H. EDELMAN, S.W. PETERSON, V. REINER, AND J.H. STOUT  

E-Print Network (OSTI)

water steam Steam 100 1 Pressure (bar) steam ice Figure 1. The phase diagram for the simple chemical system with phases ice, water, and steam. 1. Introduction A central problem in geochemistry has been illustrates the familiar phase diagram for a simple chemi­ cal system that involves three phases (ice, water

Reiner, Victor

271

PRE-SW DNP3 Head-end for DER Version 0.1.8.1 - BETA  

Science Conference Proceedings (OSTI)

This software provides a human interface through which smart inverter-based systems, such as photovoltaic and battery storage, may be managed and monitored. The software achieves this through the use of standards-based smart inverter functions as described in the IEC 61850-90-7 and using the DNP3 communication standard for smart PV/storage (DNP3 AN2011-001). One or many end devices may be managed, either locally or distributed, and connected via any IP network. A mechanism is provided by which data from ...

2012-04-02T23:59:59.000Z

272

MORB that have formed in conjunction with continental rifting and where EM-1 component signatures occur. A  

E-Print Network (OSTI)

there is a relationship between the property and the logs. Similar opinions have been emphasised in Wendt et al. (1986

273

COUPLED SEISMIC STRATIGRAPHY AND PALEOCLIMATE RECONSTRUCTION OF A SEDIMENT STARVED, SYN-RIFT BASIN: SEARLES VALLEY, CALIFORNIA  

E-Print Network (OSTI)

of compact materials have been built between evaporation ponds used to extract trona from brines derived from

Heller, Paul

274

Impact of lake-level changes on the formation of thermogene travertine in continental rifts: Evidence from Lake Bogoria,  

E-Print Network (OSTI)

pool. The spring has thin subaerial opaline silica­ trona­thermonatrite crusts around the vent. Thin white efflorescent crusts of thermonatrite, trona, nahcolite, halite and opaline silica com- monly- nated with calcite. Euhedral acicular and bladed trona, thermonatrite, nahcolite and halite crys- tals

Konhauser, Kurt

275

Structural Control of Hydrology, Hydrogeology and Hydrochemistry along the Eastern Escarpment of the Jordan Rift Valley, JORDAN.  

E-Print Network (OSTI)

??The relationship of structural geology and hydrogeological characteristics NW Jordan. Superior 3 phase tectonic model was derived from re-evaluation of structural elements which are strongly (more)

Sahawneh, Julia

2011-01-01T23:59:59.000Z

276

Geological and geometrical constraints on reconstructions of Gondwana: implications for the derivation of Gondwanan fragments in Asia  

Science Conference Proceedings (OSTI)

The relative positions of east (India, Madagascar, Antarctica, Australia, etc.) and west (Africa, S. America, Arabia) Gondwana remains controversial. The authors present a new reconstruction based on (1) tight fit of Madagascar within the Somalian embayment which satisfies both sea-floor spreading data, and Karoo and older geology: (2) a tight fit of India against a reconstructed Africa-Arabian margin, such that the east stepping margin south of Socotra is matched with the east stepping re-entrant of the Suliaman Range east of Quetta; (3) a two-phase motion history of east and west Gondwana characterized by initial NW-SE spreading, followed by essentially N-S motion parallel with the Davies Ridge. Although rifting occurred episodically within Gondwana from the Carboniferous onwards, sea floor spreading did not occur until early late Jurassic and was characterized by long right lateral transform-short ridge geometry. Break-up of E and W Gondwana succeeded early Middle Jurassic spreading along the northern margin of Gondwana from at least Oman to New Guinea. Spreading directions preserved off northwest Australia suggest that motions of the rifted fragments was directed toward the northwest into Tethys. This suggests that the Lhasa, central Pamir, Sistan, Lut (.), and Central Iranian Plateau blocks which collided with Asia after the Jurassic were derived from the southeast, as opposed to the SW as generally portrayed.

Rowley, D.B.; Ziegler, A.M.; Sahagian, D.; Nie, S.Y.; Lottes, A.L.; Jacobs, D.; Hulver, M.

1985-01-01T23:59:59.000Z

277

The Heavy Rain Event of 29 October 2000 in Hana, Maui  

Science Conference Proceedings (OSTI)

On 29 October 2000, the Hana region of Maui received 700 mm of rain in 7 h. Radar analyses revealed that the storm consisted of seven cells that were initiated along the southeast slope of Haleakala volcano. One of these cells survived for nearly ...

Ryan E. Lyman; Thomas A. Schroeder; Gary M. Barnes

2005-08-01T23:59:59.000Z

278

A Coordinated Exploration Program for Geothermal Sources on the...  

Open Energy Info (EERE)

east rift of Kilauea. The surveys carried out over the east rift included magnetic, gravity, and electrical surveys by various methods: microearthquake, surveillance,...

279

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

SUBJECT: Briefing on Puget Sound Energy's Integrated Resource Plan On May 31, 2013, Puget Sound Energy aMW Annual Energy Position #12;-- 500 1,000 1,500 2,000 2,500 3,000 3,500 4,000 4,500 5,000 2012 2033 RECs'000 Minimum amounts of produced and banked RECs Hydro REC Need:2013 IRP Base Demand less Base

280

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

and steelhead run forecasts. Brian will also explain how NOAA is working with the ocean indicator data salmon and steelhead returns post season and develops preseason forecasts. TAC works to review salmon,500 Chin, 7,400 coho Below Bonneville ­ 130,000 angler trips, 24,000 Chin, 1,000 coho Hanford Reach ­ 21

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
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We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


281

PRE-SW Industry-wide Database: Power Transformers - Populated Data-Sets (Failure Analysis Tool) v1.0, Beta  

Science Conference Proceedings (OSTI)

Improves reliability and availability via reduced reliance on time-based maintenance by using analytics based on asset health and condition analysis to determine maintenance actions.Enables more effective use of existing infrastructure and data as well as efficient use of maintenance personnel to manage operational ...

2012-09-15T23:59:59.000Z

282

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

only) No Yes No Demand Response Dispatchable Load (e.g., water heaters) Yes No Yes Yes * Note%Hydro, 70% *Simulated results from GENESYS over all water, temperature, forced outage and wind No Yes Yes Nuclear Yes Yes No No Wind No Yes No No Solar ­ Photovoltaic No Yes

283

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

. For example, a cellphone-type chip could be required that allows recharging only during off-peak hours

284

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Power Strips Commercial Street Lighting Industrial Motors Residential Appliances ­ Refrigerators compliance · 1 year to bring research plan to RTF for review De-activated · Inadequate data exists to bring Compressor Systems 8 Appliances - Refrigerator/Freezer Decommissioning 25 Lighting - CFLs 9 Cooking Equipment

285

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

, the Western Electricity Coordinating Council (WECC) develops a transmission expansion plan, a reliability SUBJECT: Briefing on Coordination of Regional Power and Transmission Planning The Council is a primary the regional transmission system. Similarly, regional transmission planning entities must accurately represent

286

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

and purchase of transmission capacity of the power grid that delivers electricity to customers in the Northwest. Northern Tier Transmission Group members include: Deseret Power Electric Cooperative; Idaho Power; North, Power Planning Division Director SUBJECT: Briefing on Regional Transmission Organization Activities

287

DESCRIPTION: DC/DC converter 20050 SW 112th Ave. Tualatin, Oregon 97062 phonephone 503.612.2300 faxfax 503.612.2382  

E-Print Network (OSTI)

weight 40 grams (1.41) (ounces) MTBF MIL-HDBK-217F 580k hours operating temperature regular models - see

Berns, Hans-Gerd

288

DESCRIPTION: point of load converter 20050 SW 112th Ave. Tualatin, Oregon 97062 phonephone 503.612.2300 faxfax 503.612.2382  

E-Print Network (OSTI)

recueil RDF 93), la spécification militaire américaine MIL-HDBK 217F, le modèle de prédiction Telcordia MIL-HDBK 217F le taux de défaillance constant d'un composant (partie II de la figure 1-4) s'écrit : 0 partir des spécifications militaires américaine MIL-HDBK 217F. 1.3.2.1.1 Calcul pour un condensateur Les

Berns, Hans-Gerd

289

Miller, K.G., and Snyder, S.W. (Eds.), 1997 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 150X  

E-Print Network (OSTI)

COVIDIEN ­ RALEIGH, NC 2. THOMAS BAIADA DUPONT-TYVEK ­ RICHMOND, VA 3. JASON BAKER EXXON MOBIL ­ BEAUMONT ­ CHAPEL HILL, NC 9. ROBERT DEEDRICK MWV ­ RALEIGH, NC 10. AARON FRYE EXXON MOBIL - BEAUMONT, TX 11. MATTHEW LEE GRAY O'BRIEN & GERE ENGINEERS, INC. ­ RALEIGH, NC 12. JAMI GUTHRIE (HALL) EXXON MOBIL

290

Miller, K.G., and Snyder, S.W. (Eds.), 1997 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 150X  

E-Print Network (OSTI)

2. CHRISTOPHER AUSTIN ROVISYS ­ APEX, NC 3. JEFFREY BASEY MWV ­ COVINGTON, VA 4. ERIC BLAKE EXXON. DEREK FRICK COVIDIEN ­ RALEIGH, NC 12. AARON FRYE EXXON MOBIL ­ BEAUMONT, TX 13. KATHRYN GAITHER MWV SMITH KLINE ­ MORRISVILLE, NC 25. KYLE LESLIE DOMTAR ­ BENNETSVILLE, SC 26. JORDAN LEWIS EXXON MOBIL

291

Miller, K.G., and Snyder, S.W. (Eds.), 1997 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 150X  

E-Print Network (OSTI)

1950; Vaillancourt 1973).This recommendationwas emphasizedwith regard to contingent valuation (CV the natural re- sourcesin Prince William Sound,Alaska, thatwere injured by the 1989Exxon Valdez oil spill detailed sce- nario describing the condition of Prince William Soundbefore and after the Exxon Valdez spill

292

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

that these preliminary costs are a planning baseline from which to refine costs as the project progresses through members FROM: Mark Fritsch, project implementation manager SUBJECT: Step 2 review of the Kootenai River White Sturgeon Aquaculture Conservation Facility, Project #1988-064-00, a BiOp project. PROPOSED ACTION

293

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

, the role of Columbia Grid in facilitating the project, and how the parties settled on a cost deficiencies · Utilities then determined cost allocation 5 #12;Joint Project · New 230kV line from Rapids are responsible for all costs on their associated individual projects 7 #12;Joint Project Benefits · Mitigates

294

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Power Includes microgrid and solar sites at local public schools Inland Power & Light Co Includes of ancillary services, ranging from contingency reserves to intra-hour regulation and balancing. The label DR for balancing services (DR 2.0) ­ Load increase as well as decrease ­ Many times per year, all

295

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

% Energy Efficiency 16% Geothermal Petroleum & Pet Coke of regulation and carbon cost in the Council's Plan, the Council is also required to consider environmental costs more broadly. This presentation is intended to provide a foundation of facts from which discussion

296

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

and chair a forum to focus regional attention on the need to update end use load profile data. The purpose SUBJECT: End Use Load Forum Status Report In January, the Power Committee gave the go ahead to convene

297

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

develop large amounts of solar power; if so, its generation profile will affect the wholesale power market response We agree that changing paradigms for energy efficiency, such as utilities with little or no load

298

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Thermal 100 3 4,979 0.00 66.09 261.5 Solar PV 150 2 3,805 0.00 21.37 144.3 Power Plant Fuel Efficiency its thermal efficiency Thus, a power plant with a heat rate of 6,824 Btu/kWh has a fuel efficiency SGT5-8000HTM MW Langley Gulch Power Plant Idaho Power Co ­ 570 MW output ­ 60 % thermal efficiency

299

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

partners and citizen groups, working together to make rooftop solar electricity more cost-effective for all. The ESSP was one of 22 teams working under the U.S. Department of Energy's Rooftop Solar Challenge program, a nationwide effort to reduce the "soft costs" associated with installing rooftop solar electricity

300

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

topics, role of the GRAC, focus on preliminary solar photovoltaic resource assessment (utility scale and rooftop).assessment (utility scale and rooftop). Good attendance and participation - 29 in person, 19 Woody residues Offshore Wind Solar PV Conventional hydrothermal Geothermal Modular Nuclear Units

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
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301

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

a schematic of the project, and Figure 10 shows the main site. This water treatment plant contains the biogas digestor with waste-wood-fired heat, the biogas engines, and a battery bank. Under an agreement

302

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

is investigating biogas- powered grid-independent data centres [43], the synergistic effects from using data

303

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

renewable energy arenas: ­ Wind Power ­ Biomass (Biogas, Biofuels, ...) ­ Hydro power ­ Water purification ­ Familysized biogas plants ­ Solar cookers ­ Home lighting ­ Solar lantern ­ Solar water Heating #12;Biomass, Energy Efficiency, Fuels, Renewable Electricity, Renewable Electricity, Clean Coal, Biogas Clean Coal

304

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

to the management and maintenance of the property and maintenance of habitat units. This also should be explained integrated invasive-species management system. The ISRP recommended that wildlife projects take a more elements of a project or management plan in the interim period between category reviews based on staff

305

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

elements within projects that contribute to the development, maintenance, and/or management of databases Information System and CRITFC's Tribal Data Network). (3) Individual Project Data Management: Occurs within entities' database systems. During the current category review of regional data management, sub

306

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

, PUC regulations Technical Manufacturer data Reliability/power quality Fuel availability Purchase Power the past 20 years from both stationary sources and motor vehicles. However, PM-10 emissions in the SJV have Deployment 6 between PG&E (the distribution company), several small scale generator manufacturers, and Edison

307

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Chair Montana Henry Lorenzen Oregon W. Bill Booth Idaho James A. Yost Idaho Pat Smith Montana Tom Karier Lindstrom SUBJECT: Briefing on renewable resource development in Idaho Mark Stokes, Power Supply Planning, Idaho Power Company will make a presentation on renewable resources in the Idaho Power service territory

308

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Chair Montana Henry Lorenzen Oregon W. Bill Booth Idaho James A. Yost Idaho Pat Smith Montana Tom Karier Lindstrom SUBJECT: Briefing on Idaho Power Company and Integrated Design Lab projects Idaho Power Co. (IPC) and the University of Idaho ­ Integrated Design Lab (UI-IDL) have been working together since 2004

309

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Chair Montana Henry Lorenzen Oregon W. Bill Booth Idaho James A. Yost Idaho Pat Smith Montana Tom Karier Lindstrom SUBJECT: Briefing on the University of Idaho - Integrated Design Lab Kevin Van Den Wymelenberg is an Associate Professor at the University of Idaho, Director of the University of Idaho - Integrated Design Lab

310

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

-Chair Oregon Bruce A. Measure Montana James A. Yost Idaho W. Bill Booth Idaho Henry Lorenzen Oregon Tom Karier Coop Ken Baker, Idaho Industrial Consultant Theresa Drake, Idaho Power Company Stacy Donohue, Idaho PUC

311

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Chair Montana Henry Lorenzen Oregon W. Bill Booth Idaho James A. Yost Idaho Pat Smith Montana Tom Karier Lindstrom, Idaho Council Staff SUBJECT: Presentation by five North Idaho Cooperatives The Idaho Council Members invited five of the North Idaho Electric Cooperatives to come before the Council and tell you

312

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

generating and demand-management resources to satisfy maximum system demands for electricity at a specific about having sufficient resources to provide for anticipated long-term growth in demand. Operators rely on operating reserves to maintain power flow. These reserves are surplus resources and demand-side actions

313

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

to the substation at Anaconda. #12;·200 feet high ·381 feet long ·Generation Capacity of 196 MW ·On average

314

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

tightened up. Natural gas rig count has decreased.g g Price competition between coal and natural gas forecast of natural gas prices in the near-term The oil prices has been increased Coal prices are within SUBJECT: Natural gas price forecast update At the June Council meeting we presented a draft update

315

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

for the revised natural gas price forecasts as well as refiners acquisition cost of oil and minemouth coal prices for power river basin coal. The natural gas prices are shown for the wellhead as well as at various hubs with the Natural Gas Advisory Committee (NGAC) we have proposed a downward revision of our range of fuel price

316

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

, the average wellhead price of natural gas averaged $12.60. Even Powder River Basin coal prices, which have. Natural gas prices at the wellhead averaged $2.37 per million Btu in January 2000. In June 2008. With the higher natural gas prices of recent years and technological improvements in drilling, nonconventional

317

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

forecasts to provide information about its current views on future natural gas, oil, and coal prices. I have is very low compared to recent prices and forecasts. Natural gas prices are low also, but by a smaller Committee. Very roughly, the proposed revision of the natural gas price forecast range would move the prices

318

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

monitoring regional markets we look at Regional Economy, Natural Gas Prices as well as electric utility sales of Residential Rates Since 2007 § Recent PNUCC survey of residential rates indicated increase in rates

319

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

MeasureReview · Acted upon over 80 measures ­ 42 Residential Industrial 42 Residential ­ 29 Commercial ­ 10 Agricultural ­ 2 Industrial ­ 2 new measures added to RTF library Residential/31/2013y p p / / / / Commercial Cooking Equipment Combination Ovens Small Saver Under Review 4/16/2013 7

320

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

that is consistent with our Charter's requirement to assess lifecycle tracking. The diagrams are populated with example content for: a) data collection and management information across the lifecycle; and b) flow or more organizations (e.g., Idaho Fish and Wildlife Information System, CRITFC's Tribal Data Network

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
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321

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Changes timing of discharge-related lifecycle, changes food availability, alters sediment and organic 3 0 2 3 Blackfoot (BFT) 2 3 3 2 3 3 Goose (GSE) 3 3 3 0 3 3 Idaho Falls (IFA) 3 3 3 0 3 3 Lower was restricted to Idaho, so the watersheds that cross state boundaries are assessed only for the Idaho portion

322

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Formulation. Collaboration between PNNL, Idaho National Laboratory, Savannah River National Laboratory at Hanford by roughly 45% and saves billions of dollars in lifecycle costs. · Integrated Scaled Testing. PNNL River, Oak Ridge and Idaho. Researchers at these laboratories have advanced the science and processes

323

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

-Chair Oregon Bruce A. Measure Montana James A. Yost Idaho W. Bill Booth Idaho Henry Lorenzen Oregon Tom Karier - October X X X X X Lifecycle Chart - Diagram life cycle use of tagging technology to help clarify relevance-Chair Oregon Rhonda Whiting Montana W. Bill Booth Idaho James A. Yost Idaho Bill Bradbury Oregon Tom Karier

324

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

and Idaho National Engineering Laboratories (INEL) on various DOE electric vehicle and battery programs the lifecycle of passenger and freight transport, materials, electricity, and heating and cooking; iii) detailed fuels and electricity, and lifecycle analysis. He received a Master's degree in Transportation

325

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

................................................................................ 19 10.6 Fuel Cards for: · Superannuation Contributions Surcharge · H.E.C.S repayments · Medicare Levy Surcharge · Child Support obligations · Terminations Payments Surcharge #12;FLEXIBLE REMUNERATION PACKAGING MANUAL Version 2

326

PRE-SW Computer Based Training (CBT) - American Society of Mechanical Engineers (ASME) CBT for Service Water System Engineers v1.0  

Science Conference Proceedings (OSTI)

American Society of Mechanical Engineers (ASME) requirements for Service Water System Engineers, Version 1.0 is a computer-based training module that allows users to access training when desired and review it at their own pace.This computer-based training (CBT) course's objective is to introduce students to ASME requirements associated with service water systems, and in particular, service water piping systems. The student will first learn about the design criteria used to ...

2013-06-30T23:59:59.000Z

327

Saunders, A.D., Larsen, H.C., and Wise, S.W., Jr. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 152  

E-Print Network (OSTI)

of ash fallout from large explosive eruptions. The tephra are bimodal (colorless km elevation in midsummer, followed by fallout in southern Greenland and in the Irminger Basin

328

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

to the region's Indian tribes and state and federal fish and wildlife agencies for recommendations for: #12 to be submitted by federal and state water management agencies, by the region's electric power producing agencies this Act and other laws, and other federal agencies to protect, mitigate, and enhance fish and wildlife

329

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Geothermal X X X Hydroelectric X X X Hydrogen X Landfill Gas X X X Municipal Solid Waste X O Th l X XOcean

330

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

on the following topics: 1. Regional Economic Conditions 2. Electricity Demand 3. Natural Gas Markets and Prices 4 supplies or increasing demand. Increasingly, natural gas-fired generation is displacing coal Efficiency Achievements and Issues 23 IV. Renewable Resources 30 V. Natural Gas-Fired Generating Resources 34

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851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Conditions B. Electricity Demand C. Natural Gas Markets and Prices D. Emissions Regulations and Impacts E, upward movements in natural gas prices have been triggered by reductions in supply or increases in demand. This is the result of several factors at the national level, including increasing demand from natural gas

332

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

Forecast Base Case includes Medium Demand Forecast Medium Natural Gas Price Forecast Federal CO2 has continued, with refinements to input parameters pertaining to resource capacities, natural gas emissions, generation, and natural gas fuel consumption for the region. #12;Update On The Wholesale

333

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

;Schedule July: framework; electric demand forecast; natural gas price forecast August: Sixth Power Plan · Conservation · Renewable generation · Natural gas-fired generation Action plan 8 #12;2. Situation Scan and Narratives Strong conservation acquisition during 2010-2011 Soft regional economy Low natural gas prices

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851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

& Demographic Forecasts Fuel Price Forecasts Conservation Supply Curves Generating Resources and Costs Wholesale: Progress Report on Electricity Price Forecast As part of the Mid Term Assessment, staff is preparing a long-term wholesale electricity market price forecast. Staff will review how the forecasts are made and some

335

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

plan for the Crystal Springs Fish hatchery and Programs for Snake River Chinook Salmon and Yellowstone for the proposed Crystal Springs Fish Hatchery (Project #2008-906-00, Crystal Springs Planning and Operations sponsor of the final costs associated with the entire Crystal Springs Fish Hatchery and associated support

336

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

" dealt with issue of how utilities can claim credit for codes and standards that were adopted after of smallscale solar photovoltaic (PV) applications in response to state and federal tax incentives developments, environmental conflicts, and system integration needs. Some progress is being made with respect

337

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

. The general opinion of those in the industry is that the political support exists to extend the credit. #12 projects is in the range of $72 to 98/MWh6 . Factors including increased commodity (steel, copper, resin

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851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

gas storage ­ 7.7 Bcf natural gas proven reserves · Total owned generation ­ MT ­ 372 MW ­ regulated Storage 18.0 - 18 Electric 337,600 60,800 398,400 Natural gas 181,300 85,300 266,600 System (miles) MT SD ­ 400,500 electric ­ 267,800 natural gas · Approximately 123,000 123,000 square mile Service Service

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851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

, but also on storage capability and other natural gas peaking resources like line pack, LNG storage 2008 it averaged $127, even approaching $150 some days. Natural gas prices at the wellhead averaged $2.37 per million Btu in January 2000. In June 2008, the average wellhead price of natural gas averaged $12

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851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

algorithm, load forecast, microgrid, neural networks. I. INTRODUCTION DISTRIBUTED generation of electricity and Forecasting Electricity Loads and Prices: A Statistical Approach. Chichester, U.K.: Wiley, 2006. [8] M286 IEEE TRANSACTIONS ON SMART GRID, VOL. 1, NO. 3, DECEMBER 2010 Short-Term Load Forecast

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


341

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

privatized and deregulated, the issue of accurately forecasting electricity load has received more attention in recent years. The error of electricity load forecasting increases operational costs [2­4]. Overestimation for load prediction and electricity price forecasting, and have achieved good performances [20],[21]. SVM

342

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

for electricity demand. The demand forecast looks at energy use by sector to predict monthly load for electricity in forecasting wholesale electricity prices. Northwest load is used in the Council's Regional Portfolio Model assumptions or demand forecast for electricity. Many things determine the load forecast, and energy demand

343

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

following these developments and are working to incorporate them into the Council's load forecast and its in forecasting future demand for electricity and in estimating conservation potential of data centers. BACKGROUND. Data centers represent relatively large electrical loads at each site, reducing the transactions costs

344

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

. Both Energy Star [23] and non-Energy Star versions of the following loads are included: · dishwasher

345

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

not break out its specific assumptions for clothes washers and dishwashers, but it did indicate that between Efficiency 1983 Plan Base Use Figures 6 and 7 show AHAM's sales weighted average energy use for dishwashers's implied achievable potential savings for new dishwashers and clothes washers. As was the case

346

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

's Fifth Power Plan, in the form of light-emitting diode (LED) traffic lights. In the Sixth Power Plan, LED Snap Shot July 2013 Higher US Saturation for LED Reflector Lamps Source: DOE/EERE Adoption of LightEmitting Diodes in Common Lighting Applications, April 2013, Revised May 2013 #12;9/4/2013 11 Bulb Cost Trends

347

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

of supplemental wood heat in homes with electric heating systems. The reduction in supplemental wood use has two their homes with electricity, they reduced their wood use. The reduction in wood use results in lower wood for incorporating environmental (e.g., air emissions) benefits of reduced wood heat usage in its cost

348

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

consistent with adequate and reliable electricity service. Natural gas plays an important role in both Washington Phil Rockefeller Washington NORTHWEST POWER AND CONSERVATION COUNCIL CHARTER OF THE NATURAL GAS and Conservation Council's Natural Gas Advisory Committee. 2. Background: The Pacific Northwest Electric Power

349

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

consistent with adequate and reliable electricity service. Natural gas plays an important role in both Manager, Economic Analysis SUBJECT: Renewal of Natural Gas Advisory Committee Staff will ask the Council to authorize the renewal of the Natural Gas Advisory Committee charter that is about to expire in June 2013

350

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

's important to note the market's volatility. Recently, forward market for natural gas prices have tightened up of shale gas has created a glut of natural gas that is likely to last for several years and depress prices. The price of natural gas in 2011 and first two quarters of 2012 were the lowest since 2002. However, it

351

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

sources and liquified natural gas (LNG) imports. With the higher natural gas prices of recent years and it is projected that imports from that area to the U.S. are unlikely to be able to meet growing natural gas demand of future natural gas supplies. There are currently three proposed LNG import terminals in the region

352

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

intake form Submit intake form and maps/aerial photo of the property Sponsor 2 Conduct intake call if there are eligible tenants on the property BPA 6 Determine if boundary survey is needed Review legal description and determine if boundary survey is needed BPA 7 Conduct boundary survey If legal description is not adequate

353

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

installationssend AC power to the grid. Can range from small installations around 1 MW to large units nearly 300 MW SUBJECT: Primer on Solar Power Staff has prepared another in a series of primers designed to build up. At the Power Committee meeting on August 6, Steve Simmons and Gillian Charles will present a primer on solar

354

Saunders, A.D., Larsen, H.C., and Wise, S.W., Jr. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 152  

E-Print Network (OSTI)

. Furthermore, inspection of published tephra geochemistry, as highlighted by Hunt and Hill (1993; 1994 of the interlaboratory comparison of electron micro- probe data (see Jarosewich et al., 1979). Such a program can serve

355

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

conservation savings are "weather normalized", i.e., based on 30-year average temperature and solar conditions SUBJECT: Follow Up on Weather and Energy Efficiency Impacts on Loads At the Power Committee meeting on year-to-year upward and downward impacts of weather on regional loads, as well as the more lasting load

356

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

recovery and other biogas facilities. Second, for each hour, any unit that did not generate electricityCost(nominal$/MWh) Hydro Nuclear Wind Coal/Biomass NG CCCT/Biogas NG SCCT/Fuel Oil/Demand Response Demand The regionCost(nominal$/MWh) Hydro Nuclear Wind Biomass/Biogas Coal/NG CCCT Coal/NG SCCT/Fuel Oil/Demand Response Demand With high CO

357

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

are provided for the model to draw upon for this purpose. Resources, such as biogas, available in relatively

358

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

4498 Solar Thermal 2475 Wind 2718 Biogas/mass 164 Geothermal 80 9935 In Development and Approved2011

359

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network (OSTI)

. 7 http://www1.eere.energy.gov/buildings/appliance_standards/pdfs/epact2005_appliance_stds.pdf 5 ENERGY INDEPENDENCE AND SECURITY ACT OF 2007 (EISA), pg. 86 http://www1.eere. 4. http://www1.eere.energy.gov/buildings/appliance_standards/pdfs/74fr34080.pdf 7 Announcement from

360

Predictability of the Normalized Difference Vegetation Index in Kenya and Potential Applications as an Indicator of Rift Valley Fever Outbreaks in the Greater Horn of Africa  

Science Conference Proceedings (OSTI)

In this paper the progress made in producing predictions of the Normalized Difference Vegetation Index (NDVI) over Kenya in the Greater Horn of Africa (GHA) for the OctoberDecember (OND) season is discussed. Several studies have identified a ...

Matayo Indeje; M. Neil Ward; Laban J. Ogallo; Glyn Davies; Maxx Dilley; Assaf Anyamba

2006-05-01T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


361

Complete genome sequence of the halophilic bacterium Spirochaeta africana type strain (Z-7692T) from the alkaline Lake Magadi in the East African Rift  

SciTech Connect

Spirochaeta africana Zhilina et al. 1996 is an anaerobic, aerotolerant, spiral-shaped bacte- rium that is motile via periplasmic flagella. The type strain of the species, Z-7692T, was iso- lated in 1993 or earlier from a bacterial bloom in the brine under the trona layer in a shallow lagoon of the alkaline equatorial Lake Magadi in Kenya. Here we describe the features of this organism, together with the complete genome sequence, and annotation. Considering the pending reclassification of S. caldaria to the genus Treponema, S. africana is only the second 'true' member of the genus Spirochaeta with a genome-sequenced type strain to be pub- lished. The 3,285,855 bp long genome of strain Z-7692T with its 2,817 protein-coding and 57 RNA genes is a part of the Genomic Encyclopedia of Bacteria and Archaea project.

Liolios, Konstantinos [U.S. Department of Energy, Joint Genome Institute; Abt, Birte [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Scheuner, Carmen [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Teshima, Hazuki [Los Alamos National Laboratory (LANL); Held, Brittany [Los Alamos National Laboratory (LANL); Lapidus, Alla L. [U.S. Department of Energy, Joint Genome Institute; Nolan, Matt [U.S. Department of Energy, Joint Genome Institute; Lucas, Susan [U.S. Department of Energy, Joint Genome Institute; Deshpande, Shweta [U.S. Department of Energy, Joint Genome Institute; Cheng, Jan-Fang [U.S. Department of Energy, Joint Genome Institute; Tapia, Roxanne [Los Alamos National Laboratory (LANL); Goodwin, Lynne A. [Los Alamos National Laboratory (LANL); Pitluck, Sam [U.S. Department of Energy, Joint Genome Institute; Pagani, Ioanna [U.S. Department of Energy, Joint Genome Institute; Ivanova, N [U.S. Department of Energy, Joint Genome Institute; Mavromatis, K [U.S. Department of Energy, Joint Genome Institute; Mikhailova, Natalia [U.S. Department of Energy, Joint Genome Institute; Huntemann, Marcel [U.S. Department of Energy, Joint Genome Institute; Pati, Amrita [U.S. Department of Energy, Joint Genome Institute; Chen, Amy [U.S. Department of Energy, Joint Genome Institute; Palaniappan, Krishna [U.S. Department of Energy, Joint Genome Institute; Land, Miriam L [ORNL; Rohde, Manfred [HZI - Helmholtz Centre for Infection Research, Braunschweig, Germany; Tindall, Brian [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Detter, J. Chris [U.S. Department of Energy, Joint Genome Institute; Goker, Markus [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Bristow, James [U.S. Department of Energy, Joint Genome Institute; Eisen, Jonathan [U.S. Department of Energy, Joint Genome Institute; Markowitz, Victor [U.S. Department of Energy, Joint Genome Institute; Hugenholtz, Philip [U.S. Department of Energy, Joint Genome Institute; Woyke, Tanja [U.S. Department of Energy, Joint Genome Institute; Klenk, Hans-Peter [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Kyrpides, Nikos C [U.S. Department of Energy, Joint Genome Institute

2013-01-01T23:59:59.000Z

362

Detrital zircon provenance link of the Chinle Formation and the Auld Lang Syne Group in Nevada  

Science Conference Proceedings (OSTI)

Previous workers have interpreted the Upper Triassic Auld Lang Syne Group of northwest Nevada as (a) part of a suspect terrane displaced with respect to the craton, or (b) the deltaic terminus of the Chinle depositional system of the Colorado Plateau. U-Pb ages for detrital zircons (air-abraded and analyzed as individual crystals), from sandstones in basal Chinle Fm near Currie and the Osobb Fm (basal Auld Lang Syne Gp) in Dixie Valley, set constraints on the provenance of the two units as follows: (a) Chinle grains (n = 40): 225--235 (n = 2), 505--525 (n = 19), 1,410--1,440 (n = 9), 1,700--1,740 (n = 4); (b) Osobb grains (n = 40): [approximately]235 (n = 1), [approximately]265 (n = 1), 355--415 (n = 3), 510--530 (n = 5), 1,010--1,080 (n = 11), [approximately]1,160 (n = 1), 1,430--1,450 (n = 7), 1,705--1,730 (n = 3). Proterozoic grains were likely shed from basement rocks in the SW US, whereas Triassic grains in both samples and Silurian-Devonian and Permian grains in the Osobb sample may have come from arc terranes to the south (Chinle) or west (Osobb). The Chinle sand is quartzose with only rare chert-quartzite grains, whereas the Osobb sand is subarkosic with chert-argillite and feldspar grains that presumably reflect the admixture of Grenville-age detritus (1,010--1,160 Ma) of uncertain provenance. The most likely source for Cambrian grains (505--530 Ma) is the rift-related igneous province stretching from southern Colorado to SW Oklahoma (Wichita Mtns). Regardless of origin, the unexpected occurrence of Cambrian grains in both Nevada samples supports the suggestion of Lupe and Silberling (1985) that the Auld Lang Syne Gp was deposited as a linked facies equivalent of the Chinle Fm.

Gehrels, G.E.; Dickinson, W.R. (Univ. of Arizona, Tucson, AZ (United States). Dept of Geosciences); Riggs, N. (Northern Arizona Univ., Flagstaff, AZ (United States). Dept of Geology)

1993-04-01T23:59:59.000Z

363

Near-Source Modeling of Transportation Emissions in Built Environments Surrounding Major Arterials  

E-Print Network (OSTI)

6 th St. 6/30/08 6 th St. Pasadena 7/23/08 Colorado Blvd.7/25/08 Colorado Blvd.7/29/08 Colorado Blvd. (W) (W) (SW) (S) (SW) (SW) (SE) (

2009-01-01T23:59:59.000Z

364

Geophys. J. Int. (2010) 183, 11191133 doi: 10.1111/j.1365-246X.2010.04813.x GJIGeodynamicsandtectonics  

E-Print Network (OSTI)

subduction is associated with the backarc rifting of the Okinawa trough (Letouzey & Kimura 1986; Sibuet et al

Demouchy, Sylvie

365

ELSEVIER Tectonophysics 274 (1997) 171-190 TECTONOPHYSICS  

E-Print Network (OSTI)

to the southwest. Back-arc rifting may thus occur in the westernmost section of the Okinawa trough above

Demouchy, Sylvie

366

New insights on 3-D plates interaction near Taiwan from tomography and tectonic implications  

E-Print Network (OSTI)

the South China Sea prior to Pliocene. (5) The Southern Okinawa Trough rifted during the last 2 ^ 1 Ma

Demouchy, Sylvie

367

CRS Report for Congress Prepared for Members and Committees of Congress  

E-Print Network (OSTI)

. Nearby Lake Magadi, a playa in the sump of the Kenyan rift valley is also promising. Earlier trona

368

Quaternary Science Reviews 23 (2004) 561580 Recent environmental change and prehistoric human activity in  

E-Print Network (OSTI)

. Nearby Lake Magadi, a playa in the sump of the Kenyan rift valley is also promising. Earlier trona

Nicoll, Kathleen

369

P2JW323012-0-A01900-1--------XA AZ,EE,MW,NE,NY,SC,SW,WB,WE P2JW323012-0-A01900-1--------XA  

E-Print Network (OSTI)

/11 Status after 9/11 CTBT Comprehensive Test Ban Treaty Not supported by administration. No change. NPT Non-ProliferationPutting the Genie Back in the Bottle: Nuclear Non-Proliferation in the New Millennium G by an adversary could have a devastating influence on US security and non-proliferation. One of the highest

Deutch, John

370

P2JW340011-0-A01800-1--------XA AZ,EE,MW,SC,SW,WE P2JW340011-0-A01800-1--------XA  

E-Print Network (OSTI)

. With or without the NIE's opinion of Iran's nuclear program, that world is still a dangerous place. Let's assume's a remarkably big one. North Korea in July 2006 tested the long- range Taepodong-2, a nuclear payload-capable ballistic missile. North Korea has exported its missile technology to Iran and Pakistan. And of course

Rhoads, James

371

Modeling views for semantic web using extensible semantic (XSemantic) nets  

Science Conference Proceedings (OSTI)

The emergence of Semantic Web (SW) and the related technologies promise to make the web a meaningful experience. Yet, high level modeling, design and querying techniques proves to be a challenging task for organizations that are hoping utilize the SW ...

R. Rajugan; Elizabeth Chang; Ling Feng; Tharam S. Dillon

2005-10-01T23:59:59.000Z

372

JESSICA GUREVITCH CURRICULUM VITAE Department of Ecology and Evolution  

E-Print Network (OSTI)

, Petersham MA Species Diameter (cm) SW depth (cm) SW age (rings) Mean Range Acer rubrum 33.1 2.1 8.3 1.1 43 4

373

A Flexible Nonparametric Test for Conditional Independence  

E-Print Network (OSTI)

Model Specication Tests,Journal of Econometrics, [4]A Consistent Conditional Moment Test of Functional Form,the 5% standardized GCR test, SW2007 test, and SW2008 test

Huang, Meng; Sun, Yixiao; White, Hal

2013-01-01T23:59:59.000Z

374

An Integrated Geophysical Analysis Of The Upper Crust Of The Southern Kenya  

Open Energy Info (EERE)

Upper Crust Of The Southern Kenya Upper Crust Of The Southern Kenya Rift Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: An Integrated Geophysical Analysis Of The Upper Crust Of The Southern Kenya Rift Details Activities (0) Areas (0) Regions (0) Abstract: Previous interpretations of seismic data collected by the Kenya Rift International Seismic Project (KRISP) experiments indicate the presence of crustal thickening within the rift valley area beneath the Kenya dome, an uplift centred on the southern part of the Kenya rift. North of the dome, these interpretations show thinning of the crust and an increase in crustal extension. To the south near the Kenya/Tanzania border, crustal thinning associated with the rift is modest. Our study was aimed at further investigating crustal structure from this dome southwards via a

375

Today in Energy - U.S. Energy Information Administration (EIA)  

U.S. Energy Information Administration (EIA)

Lower railroad energy consumption reflects improved ... Central Appalachian ... 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press ...

376

Small Business Cyber Security Workshop for Portland, Oregon ...  

Science Conference Proceedings (OSTI)

Page 1. Portland District Office Small Business Cyber Security Workshop Portland District Office 601 SW Second Ave. Suite ...

2013-07-24T23:59:59.000Z

377

Natural Gas - Pub - U.S. Energy Information Administration (EIA)  

U.S. Energy Information Administration (EIA)

U.S. Department of Energy Headquarters (Forrestal Building) 1000 Independence Avenue, SW Washington, DC 20585 Room ... Organization: Phone: Email:

378

DEGAS 2 Neutral Transport Modeling of High Density, Low Temperature Plasmas  

E-Print Network (OSTI)

of Atomic Energy 1 Kurchatov Sq., Moscow 123098, Russia # Presently at McKinsey & Company, Inc., London SW1Y

379

Building and Fire Publications  

Science Conference Proceedings (OSTI)

... Kwon, SW; Liapi, KA; Haas, CT; Sreenivasan, SV; McLaughlin, JT; Human Behavior and Fire Emergencies: An Annotated Bibliography. ...

380

Building and Fire Publications  

Science Conference Proceedings (OSTI)

... Automation. (212 K) Kwon, SW; Liapi, KA; Haas, CT; Sreenivasan, SV; McLaughlin, JT. NIST SP 989; September 2002. ...

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


381

Interactions between Electric-drive Vehicles and the Power Sector in California  

E-Print Network (OSTI)

NGST = Natural gas steam turbine; NW = Northwest, SW =generation, and steam and combustion turbines (NGST+NGCT)

McCarthy, Ryan; Yang, Christopher; Ogden, Joan M.

2009-01-01T23:59:59.000Z

382

1  

NLE Websites -- All DOE Office Websites (Extended Search)

... 4 7 Diffuse disagreement as a percentage of the SIROS diffuse for October 14, 1995... 5 8 Total SW...

383

Self-reported Impacts of LED Lighting Technology Compared to Fuel-based Lighting on Night Market Business Prosperity in Kenya  

E-Print Network (OSTI)

Market Business Prosperity in Kenya Peter Johnstone * , Arnemany people and businesses in Kenya who participated in thismarket testing field work in Kenyas Rift Valley Province,

Johnstone, Peter

2009-01-01T23:59:59.000Z

384

#Itano 2.EPS  

Science Conference Proceedings (OSTI)

... grounded on a submarine bed contained in an extensional rift basin coated with thick marine sediments and is subject to high geothermal heat flow ...

1998-01-30T23:59:59.000Z

385

Project Title  

NLE Websites -- All DOE Office Websites (Extended Search)

Rift basin in SC * Results of petrographic and core analysis from the Rizer 1 * Future investigations in the SGR * Summary 3 Benefit to the Program Program Goals: * Develop...

386

An Integrated Mapping And Remote Sensing Investigation Of The...  

Open Energy Info (EERE)

And Remote Sensing Investigation Of The Structural Control For Fumarole Location In The Eburru Volcanic Complex, Kenya Rift Jump to: navigation, search GEOTHERMAL ENERGYGeothermal...

387

Uganda - U.S. Energy Information Administration (EIA)  

U.S. Energy Information Administration (EIA)

Country Analysis Note. The first commercial oil discovery was made in the Lake Albert Rift Basin in 2006. Since then, successful well appraisals have boosted Uganda's ...

388

The Lillehammer Submarine Fan Complex.  

E-Print Network (OSTI)

??Abstract The Lillehammer Submarine Fan Complex is a mixed mud/sand rich turbidite fan system. The fan complex was deposited in the Neoproterozoic Hedmark rift basin (more)

Skaten, Maren Kristin Mllerup

2006-01-01T23:59:59.000Z

389

Coarse-clastic turbidite sedimentation : the neoproterozoic Imsdalen submarine fan complex, Hedmark Basin, South Norway.  

E-Print Network (OSTI)

??The Imsdalen Submarine Fan Complex is a gravel and coarse sand dominated turbidite fan system. The fan complex was deposited in the Neoproterozoic Hedmark rift (more)

Stalsberg, Martin

2004-01-01T23:59:59.000Z

390

Location of Cobalts Kwanza Basin Blocks to Campos Basin ...  

U.S. Energy Information Administration (EIA)

Brazil B21 B20 B9 Cachalote Caxareu Itaipu Wahoo Azul Pirambu Franca Cobalt Cameia-1 Discovery Well Lontra Atlantic Rift Baleia-1A (1996)

391

Anomalously High B-Values In The South Flank Of Kilauea Volcano...  

Open Energy Info (EERE)

High B-Values In The South Flank Of Kilauea Volcano, Hawaii- Evidence For The Distribution Of Magma Below Kilauea'S East Rift Zone Jump to: navigation, search GEOTHERMAL...

392

Conduction Models Of The Temperature Distribution In The East...  

Open Energy Info (EERE)

Conduction Models Of The Temperature Distribution In The East Rift Zone Of Kilauea Volcano Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Conduction...

393

Structure and phase behavior of colloidal dumbbells with tunable attractive interactions  

E-Print Network (OSTI)

We investigate thermodynamic and structural properties of colloidal dumbbells in the framework provided by the Reference Interaction Site Model (RISM) theory of molecular fluids and Monte Carlo simulations. We consider two different models: in the first one we set identical square-well attractions on the two tangent spheres composing the molecule (SW-SW model); in the second scheme, one of square-well interactions is switched off (HS-SW model). Appreciable differences emerge between the physical properties of the two models. Specifically, the $k \\to 0$ behavior of SW-SW structure factors $S(k)$ points to the presence of a gas-liquid coexistence, as confirmed by subsequent fluid phase equilibria calculations. Conversely, the HS-SW $S(k)$ develops a low-$k$ peak, signaling the presence of aggregates; such a process destabilizes the gas-liquid phase separation, promoting at low temperatures the formation of a cluster phase, whose structure depends on the system density. We further investigate such differences by studying the phase behavior of a series of intermediate models, obtained from the original SW-SW by progressively reducing the depth of one square-well interaction. RISM structural predictions positively reproduce the simulation data, including the rise of $S(k \\to 0$) in the SW-SW model and the low-$k$ peak in the HS-SW structure factor. As for the phase behavior, RISM agrees with Monte Carlo simulations in predicting a gas-liquid coexistence for the SW-SW model (though the critical parameters appears overestimated by the theory) and its progressive disappearance moving toward the HS-SW model.

Gianmarco Muna; Dino Costa; Achille Giacometti; Carlo Caccamo; Francesco Sciortino

2013-10-16T23:59:59.000Z

394

Seismic exploration for shallow magma bodies in the vicinity of Socorro, New Mexico. Final report, January 1, 1977-December 31, 1977  

DOE Green Energy (OSTI)

This report contains the following articles: Characteristics of Rio Grande rift in vicinity of Socorro, New Mexico, from geophysical studies; Exploration framework of the Socorro Geothermal Area, New Mexico; a study of Poisson's ratio in the upper crust in the Socorro, New Mexico, Area; and Microearthquake frequency attenuation of S phases in the Rio Grande rift near Socorro. (ACR)

Sanford, A.R.; Schlue, J.

1980-11-01T23:59:59.000Z

395

African sedimentary basins - Tectonic controls on prospectivity  

Science Conference Proceedings (OSTI)

An important prerequisite for the evaluation of any sedimentary basin is the understanding of its regional tectonic setting. This is especially so in the underexplored regions of Africa. The majority of African sedimentary basins developed in an extensional setting although some have undergone subsequent compressional or transpressional deformation. The geometry and evolution of these basins is often influenced by basement structure. The extensional phase of basin development controls not only the distribution of syn-rift sediments but also the magnitude of post-rift regional subsidence and the preservation or removal of pre-rift sediments. This has important consequences for exploration models of syn-rift and pre-rift source rocks and reservoirs. Post-rift basin inversion and uplift provide crucial controls on the preservation of mature source rocks and quality of reservoirs. The distribution, nature, timing, and possible mechanisms of this uplift in Africa will be addressed. The hydrocarbon prospectivity of African basis appears to be highly variable although the limited exploration of some regions makes the exact extent of this variability unclear. Basins considered potentially prospective range from late Precambrian to Tertiary in age. The various tectonic controls outlined above, and criteria for the evaluation of underexplored areas, will be demonstrated by reference to basins studied by The Robertson Group. Examples described include basins from Bagon, Angola, Namibia, East Africa, Tertiary Rift and Karoo Rifts, and North Africa (Sudan, Egypt, Algeria, and Morocco).

Bunter, M.A.G.; Crossley, R.; Hammill, M.; Jones, P.W.; Morgan, R.K.; Needham, D.T.; Spaargaren, F.A. (Robertson Group plc, Gwynedd (England))

1991-03-01T23:59:59.000Z

396

Workbook Contents  

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

capwork_a_(na)_8sw0_mbbl_a.xls" capwork_a_(na)_8sw0_mbbl_a.xls" ,"Available from Web Page:","http://www.eia.gov/dnav/pet/pet_pnp_capwork_a_(na)_8sw0_mbbl_a.htm" ,"Source:","Energy Information Administration" ,"For Help, Contact:","infoctr@eia.gov" ,,"(202) 586-8800",,,"6/20/2013 4:20:16 PM" "Back to Contents","Data 1: Total " "Sourcekey","8_NA_8SW0_NUS_MBBL","8_NA_8SW0_R10_MBBL","8_NA_8SW0_R20_MBBL","8_NA_8SW0_R30_MBBL","8_NA_8SW0_R40_MBBL","8_NA_8SW0_R50_MBBL" "Date","U.S. Refinery Working Storage Capacity as of January 1 (Thousand Barrels)","East Coast (PADD 1) Refinery Working Storage Capacity as of January 1 (Thousand Barrels)","Midwest (PADD 2) Refinery Working Storage Capacity as of January 1 (Thousand Barrels)","Gulf Coast (PADD 3) Refinery Working Storage Capacity as of January 1 (Thousand Barrels)","Rocky Mountain (PADD 4) Refinery Working Storage Capacity as of January 1 (Thousand Barrels)","West Coast (PADD 5) Refinery Working Storage Capacity as of January 1 (Thousand Barrels)"

397

How Does a Poplar Tree Make its Wood? | U.S. DOE Office of Science...  

Office of Science (SC) Website

Contact Information Biological & Environmental Research (BER) U.S. Department of Energy SC-23Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

398

Coal - U.S. Energy Information Administration (EIA)  

U.S. Energy Information Administration (EIA)

The amount of U.S. railroad ... Coal-fired electric generators continue to dominate electric supply in the central ... 1000 Independence Avenue, SW, W ...

399

Microsoft PowerPoint - Proceedings Cover Sheets  

NLE Websites -- All DOE Office Websites (Extended Search)

& Aerospace Engineering Arizona State University; Tempe, Arizona 85287 USA o National Energy Technology Laboratory - Albany 1450 Queen Avenue SW; Albany, Oregon 97321-2152 This...

400

Buildings News  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Independence Avenue, SW Washington, DC 20585 en New Energy Dept., Berkeley Lab Report on Energy Service Company Industry Growth http:energy.govarticlesnew-energy-dept-berkeley...

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401

The Role of Materials in Sustainable Mobility  

Science Conference Proceedings (OSTI)

Source: S.C. Davis and S.W. Diegel, Transportation Energy Data Book, v23, DOE, .... Analysis was based on ... Impact of changes in market / technology.

402

James L. Smith, 1986 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

403

Other Participants 2006 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P: (202)...

404

John Nuckolls, 1969 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

405

Gregory W. Swift, 2004 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

406

Industrial SPP Partner Teaming Profile Relight Depot Navistar...  

NLE Websites -- All DOE Office Websites (Extended Search)

Navistar International 1341 SW 5 th Ave 6025 Urbana Street Boca Raton, FL 33432 Springfield, OH 45502 Business: Energy Efficient Lighting Business: Truck and Engine Manufacturer...

407

Chloride Ion Diffusion in Cement-Based Materials ...  

Science Conference Proceedings (OSTI)

... into Hardened Cement Paste , Fly Ash, Silica Fume ... Diffusion Cell: Effects of Material and Test ... LJ, and Yu, SW, Diffusion in Cementitious Materials: II ...

2012-02-23T23:59:59.000Z

408

United States - Rankings - U.S. Energy Information ...  

U.S. Energy Information Administration (EIA)

Carbon Dioxide Emissions: State CO 2 Emissions; Thank You. We welcome your comments or suggestions (optional). EIA - 1000 Independence Avenue, SW, ...

409

December 22, 1998, Board letter forwarding staff issue report...  

NLE Websites -- All DOE Office Websites (Extended Search)

(202) 208-6400 December 22, 1998 Mr. James M. Owendoff Acting Assistant Secretaq for Environmental Management Department of Energy 1000 Independence Avenue, SW Washington,...

410

October 16, 1996, Board letter forwarding staff trip report on...  

NLE Websites -- All DOE Office Websites (Extended Search)

DNFSB LETTERHEAD October 16, 1996 The Honorable Alvin L. Alm Assistant Secretary for Environmental Management Department of Energy 1000 Independence Avenue, SW Washington, DC...

411

The Death of a Massive Star Holds Key to Early Universe | U.S...  

Office of Science (SC) Website

2010 2009 2008 2007 2006 2005 Presentations & Testimony Recovery Act Contact Information Office of Science U.S. Department of Energy 1000 Independence Ave., SW Washington, DC...

412

Storing Industry's Carbon Dioxide in Real Time | U.S. DOE Office...  

Office of Science (SC) Website

Laboratories Contact Information Laboratory Policy and Evaluation U.S. Department of Energy SC-32Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P: (202)...

413

recycling.tex - CECM  

E-Print Network (OSTI)

Vor A. Voros, Nuclear Physics, B165 (1980) 209-236 . SW S. Wolfram and D. Hillman, private communication (1998). WW E. T. Whittaker, G. N. Watson,...

414

Short-Term Energy Outlook - U.S. Energy Information Administration ...  

U.S. Energy Information Administration (EIA)

Annual Energy Outlook; International Energy Outlook; Thank You. We welcome your comments or suggestions (optional). EIA - 1000 Independence Avenue, SW, Washington, DC ...

415

Interactions between Electric-drive Vehicles and the Power Sector in California  

E-Print Network (OSTI)

average natural gas combustion turbine (peaking plant) plantcombined-cycle; NGCT = Natural gas combustion turbine; NGST= Natural gas steam turbine; NW = Northwest, SW = Southwest

McCarthy, Ryan; Yang, Christopher; Ogden, Joan M.

2009-01-01T23:59:59.000Z

416

Table 6. Fields Not Currently Recognized by State Regulatory Agencies  

U.S. Energy Information Administration (EIA)

alabama beaverton ne lamar beaverton 050317 beaverton nw lamar beaverton 050317 beaverton se lamar beaverton 050317 beaverton sw lamar beaverton 050317

417

WEA-201101  

NLE Websites -- All DOE Office Websites (Extended Search)

October 3, 2011 RETURN RECEIPT REQUESTED Mr. David A. Pethick Group General Manager URS-Washington Division Global Management & Operations Services 106 Newberry Street SW...

418

Other Participants 1997 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P:...

419

Greater Cincinnati Regional High School Science Bowl | U.S. DOE...  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P:...

420

Texas A&M Regional High School Science Bowl | U.S. DOE Office...  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P:...

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421

SWPA Regional Middle School Science Bowl | U.S. DOE Office of...  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P:...

422

SWPA Regional High School Science Bowl | U.S. DOE Office of Science...  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P:...

423

Other Participants 1995 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P:...

424

Understanding Nature's Choreography in Batteries | U.S. DOE Office...  

Office of Science (SC) Website

& Resources Contact Information Advanced Scientific Computing Research U.S. Department of Energy SC-21Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

425

Joan F. Brennecke, 2009 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

426

Texas A&M Regional Middle School Science Bowl | U.S. DOE Office...  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P:...

427

U.S. States - U.S. Energy Information Administration (EIA)  

U.S. Energy Information Administration (EIA)

Play a short video to learn how to use this tool. Thank You. We welcome your comments or suggestions (optional). EIA - 1000 Independence Avenue, SW, Washington, DC 20585

428

Understanding the cost of power interruptions to U.S. electricity consumers  

E-Print Network (OSTI)

PUD #1 (Washington) Tacoma Power (Washington) Xcel (SouthDakota) Xcel Sioux Falls (South Dakota) Xcel SW Sioux Falls (South Dakota) Western

LaCommare, Kristina Hamachi; Eto, Joseph H.

2004-01-01T23:59:59.000Z

429

Enerdat - Energy Information Administration  

U.S. Energy Information Administration (EIA)

Electricity Data Browser. Thank You. We welcome your comments or suggestions (optional). EIA - 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press Room

430

FOIA Contacts | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Independence Avenue, SW Washington, DC 20585 Phone: 202-586-5955 Fax: 202-586-0575 FOIA Web Page: http:energy.govmanagementoffice-managementoperational-management...

431

Fusion Links | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Advisory Committee (FESAC) News & Resources Contact Information Fusion Energy Sciences U.S. Department of Energy SC-24Germantown Building 1000 Independence Ave., SW Washington,...

432

University Research & National Labs | U.S. DOE Office of Science...  

Office of Science (SC) Website

Advisory Committees News & Resources Contact Information High Energy Physics U.S. Department of Energy SC-25Germantown Building 1000 Independence Ave., SW Washington,...

433

Competition Opens for Time on DOE Supercomputers | U.S. DOE Office...  

Office of Science (SC) Website

In Focus Presentations & Testimony Recovery Act Contact Information Office of Science U.S. Department of Energy 1000 Independence Ave., SW Washington, DC 20585 P: (202)...

434

Simulating Complex Sea Ice-Salt Water Interactions | U.S. DOE...  

Office of Science (SC) Website

& Resources Contact Information Biological and Environmental Research U.S. Department of Energy SC-23Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

435

Energy Savings Assessment Training Manual  

NLE Websites -- All DOE Office Websites (Extended Search)

Table of Contents U.S. Department of Energy Federal Energy Management Program 1000 Independence Avenue, S.W. Washington, DC 20585 For more information contact: EERE Information...

436

Making a Better Hydrogen Producing Bacterium | U.S. DOE Office...  

Office of Science (SC) Website

Contact Information Biological & Environmental Research (BER) U.S. Department of Energy SC-23Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

437

EIA - State Electricity Profiles - Energy Information Administration  

U.S. Energy Information Administration (EIA)

Energy Information Administration, Form EIA-923 ... 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses

438

Contact | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

& Information Resources Contact Contact Information Office of Science U.S. Department of Energy 1000 Independence Ave., SW Washington, DC 20585 P: (202) 586-5430 Contact Print...

439

Washington - U.S. Energy Information Administration (EIA) - U.S ...  

U.S. Energy Information Administration (EIA)

EIA - 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses Petroleum Coal Natural Gas Renewable Nuclear

440

Today in Energy - U.S. Energy Information Administration (EIA)  

U.S. Energy Information Administration (EIA)

Washington November 15, 2012 ... EIA - 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses Petroleum Coal

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


441

Washington - SEDS - U.S. Energy Information Administration (EIA)  

U.S. Energy Information Administration (EIA)

Washington. State Profile and Energy Estimates. ... SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses Petroleum Coal Natural Gas

442

Environment - Data - U.S. Energy Information Administration (EIA)  

U.S. Energy Information Administration (EIA)

EIA - 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses Petroleum Coal Natural Gas Renewable Nuclear

443

Washington - U.S. Energy Information Administration (EIA) - U.S ...  

U.S. Energy Information Administration (EIA)

Washington State Energy Office; ... EIA - 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses Petroleum

444

Contact Us | National Nuclear Security Administration  

National Nuclear Security Administration (NNSA)

> Contact Us Contact Us National Nuclear Security Administration Office of Test Capabilities and Evaluation, NA-115 1000 Independence Avenue, SW Washington, DC 20585 (202) 586-0812...

445

U.S. Energy Information Administration - EIA - Independent ...  

U.S. Energy Information Administration (EIA)

Washington. State Profile and Energy Estimates. ... SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses Petroleum Coal Natural Gas

446

U.S. Energy Information Administration (EIA) - Map  

U.S. Energy Information Administration (EIA)

EIA - 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses Petroleum Coal Natural Gas Renewable Nuclear

447

Careers - Jobs - U.S. Energy Information Administration (EIA)  

U.S. Energy Information Administration (EIA)

EIA - 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses Petroleum Coal Natural Gas Renewable Nuclear

448

EIA-Voluntary Reporting of Greenhouse Gases Program - Contact  

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

U.S. Mail: Voluntary Reporting of Greenhouse Gases Program Energy Information Administration, EI-81 U.S. Department of Energy 1000 Independence Ave, SW Washington, DC 20585...

449

United States - U.S. Energy Information Administration (EIA ...  

U.S. Energy Information Administration (EIA)

Where shown, R = Revised data. Thank You. We welcome your comments or suggestions (optional). EIA - 1000 Independence Avenue, SW, Washington, DC 20585 About EIA

450

Carl Wieman, 1993 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

451

Exploring the Texture of Ocean-Atmosphere Redox Evolution on the Early Earth  

E-Print Network (OSTI)

Bakken Fm. Williston Basin, S.W. Manitoba sub-greenschistWilliston Basin, S. Manitoba sub-greenschist epicontinentaltheir foraminifera in the Manitoba Escarpment. Geol Assoc

Reinhard, Christopher Thomas

2012-01-01T23:59:59.000Z

452

Microsoft Word - 271C2C7B.doc  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Anderson, Recovery Act Program Manager phone: (202) 586-2083 email: Cynthia.anderson@em.doe.gov address: 1000 Independence Ave., SW Washington, DC 20585 1. Objectives Program...

453

EM News Flashes  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

flashes Office of Environmental Management 1000 Independence Ave., SW Washington, DC 20585 202-586-7709 en Waste Isolation Pilot Plant's Excavated Salt Agreement Supports...

454

EM News  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

archive Office of Environmental Management 1000 Independence Ave., SW Washington, DC 20585 202-586-7709 en Waste Isolation Pilot Plant's Excavated Salt Agreement Supports...

455

SYNTHESIS OF LIGHT-WEIGHT METALLIC MATERIALS II: VI ...  

Science Conference Proceedings (OSTI)

Session Chairpersons: L. Christodulou, Imperial College, Prince Consort Rd., London SW7 2BP; O. Senkov, University of Idaho, Moscow, ID 83844-3026...

456

Building and Fire Publications  

Science Conference Proceedings (OSTI)

... Kwon, SW; Liapi, KA; Haas, CT; Sreenivasan, SV; McLaughlin, JT; Rapid Human-Assisted Creation of Bounding Models for Obstacle Avoidance in ...

457

Building and Fire Publications  

Science Conference Proceedings (OSTI)

... 2002. Kwon, SW; Liapi, KA; Haas, CT; Sreenivasan, SV; McLaughlin, JT; In-Situ Gas Concentration Measurements for Fires. ...

458

Building and Fire Publications  

Science Conference Proceedings (OSTI)

... Kwon, SW; Liapi, KA; Haas, CT; Sreenivasan, SV; McLaughlin, JT; Immersive Virtual Reality for Steel Structures. Referenced Paper No. ...

459

Microseismicity and 3-D Mapping of an Active Geothermal Field...  

Open Energy Info (EERE)

Shear wave polarization indicates that the active,fluid-filled fracture system trends SW-NE, consistent with the orientation of the LERZ. Double difference relocation...

460

Robert J. Hanrahan  

Science Conference Proceedings (OSTI)

... Security Administration 1000 Indpendence Ave Sw Washington, DC 20585. USA Telephone: (202) 586-4606. Fax: E-Mail: robert.hanrahan@nnsa.doe.gov.

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


461

Deputy Director for Resource Management Homepage | U.S. DOE Office...  

Office of Science (SC) Website

Deputy Director Biography Organization Contact Information Deputy Director for Resource Management U.S. Department of Energy SC-4Forrestal Building 1000 Independence Ave., SW...

462

Encyclopedic Search for New Cellulases | U.S. DOE Office of Science...  

Office of Science (SC) Website

Contact Information Biological & Environmental Research (BER) U.S. Department of Energy SC-23Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

463

Silicon Photomultiplier Arrays at TJNAF| U.S. DOE Office of Science...  

Office of Science (SC) Website

(NSAC) NP News & Resources Contact Information Nuclear Physics (NP) U.S. Department of Energy SC-26Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

464

Proton Radiography at LANL | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

(NSAC) NP News & Resources Contact Information Nuclear Physics (NP) U.S. Department of Energy SC-26Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

465

741 Transaction  

National Nuclear Security Administration (NNSA)

Director, Office of Nuclear Materials Integration NMMSS Program, NA-73, Germantown Building U.S. Department of Energy 1000 Independence Avenue, SW Washington, DC 20585-1290...

466

Charles A. McDonald, 1974 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

467

Modeling of Exascale Applications Summit | U.S. DOE Office of...  

Office of Science (SC) Website

Contact Information Advanced Scientific Computing Research (ASCR) U.S. Department of Energy SC-21Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

468

2010 DOE National Science Bowl Photos - Gale Range Middle School...  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P:...

469

2010 DOE National Science Bowl Photos - Albuquerque Academy...  

Office of Science (SC) Website

News Media WDTS Home Contact Information National Science Bowl U.S. Department of Energy SC-27 Forrestal Building 1000 Independence Ave., SW Washington, DC 20585 P:...

470

Brief Science Highlights | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Highlights SBIRSTTR Highlights Contact Information Office of Science U.S. Department of Energy 1000 Independence Ave., SW Washington, DC 20585 P: (202) 586-5430 Brief Science...

471

Improvement of snowpack simulations in a regional climate model  

E-Print Network (OSTI)

that intensifies the solar radiation absorption on the landulate and predict the solar radiation budget at the sur-SW # the downward solar radiation, LWNET the net longwave

Jin, J.

2012-01-01T23:59:59.000Z

472

Ecological Footprint Budgeting: Environmental Analysis of the Generic American Car  

E-Print Network (OSTI)

Running, S.W. and Gower, S.T. Biome-BGC Model Description.dioxide absorption rates BIOME-BGC 18 MRS 19 Atjay 20 Hart

Zhang, Teresa

2005-01-01T23:59:59.000Z

473

Quantum state manipulation of trapped atomic ions  

Science Conference Proceedings (OSTI)

... Jones, RR, Raman, CS, Schumacher, SW & Bucksbaum, PH 1993 Phys. ... Turchette, QA, Hood, C., Lange, W., Mabushi, H. & Kimble, HJ 1995 Phys. ...

2002-08-13T23:59:59.000Z

474

Charles Roger Alcock, 1996 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

475

Contact Us | Department of Energy  

NLE Websites -- All DOE Office Websites (Extended Search)

Contact Us Contact Us Leadership Organization Contact Us Office of Economic Impact & Diversity US Department of Energy 1000 Independence Ave., SW Washington, DC 20585 Phone: (202)...

476

Aluminum 2002 TABLE OF CONTENTS  

Science Conference Proceedings (OSTI)

Development of Strain Induced Surface Topography of 6XXX Series Aluminum Sheet Under Balanced Biaxial Tension [pp. 83-90] S.W. Banovic and T. Foecke.

477

FORMERLY UTILIZED SITES REMEDIAL ACTION PROGRAM ELIMINATION REPORT  

Office of Legacy Management (LM)

BUILDING 7 BLOOMFIELD, NEW JERSEY SW 30 1985 Department of Energy Office of Nuclear Energy Office of Remedial Action and Waste Technology Division of Facility and Site...

478

Natural Gas Monthly (NGM) - Energy Information Administration ...  

U.S. Energy Information Administration (EIA)

Natural Gas Storage Report; Natural Gas Weekly Update; Thank You. We welcome your comments or suggestions (optional). EIA - 1000 Independence Avenue, SW, Washington ...

479

WORLD OIL REFINING LOGISTICS DEMAND MODEL  

U.S. Energy Information Administration (EIA)

Energy Information Administration 1000 Independence Avenue, S.W., Washington, DC 20585. ... OB1 Optimization with Barriers 1 OSL Optimization Subroutine Library

480

Applied Mathematics Conferences and Workshops | U.S. DOE Office...  

Office of Science (SC) Website

& Resources Contact Information Advanced Scientific Computing Research U.S. Department of Energy SC-21Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

Note: This page contains sample records for the topic "haleakala sw rift" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


481

http://www.hss.doe.gov/deprep/1996-2/bm96y10a.htm  

NLE Websites -- All DOE Office Websites (Extended Search)

DNFSB LETTERHEAD May 10, 1996 Mr. Mark B. Whitaker, Jr. Department of Energy 1000 Independence Avenue, SW Washington, DC 20585-0119 Dear Mr. Whitaker: Enclosed for your...

482

http://www.hss.doe.gov/deprep/1996-2/bm96f08a.htm  

NLE Websites -- All DOE Office Websites (Extended Search)

DNFSB LETTERHEAD February 8, 1996 Mr. Mark Whitaker Department of Energy 1000 Independence Avenue, SW Washington, DC 20585-0119 Dear Mr. Whitaker: Enclosed for your information...

483

jcliD1200119 3159..3172  

NLE Websites -- All DOE Office Websites (Extended Search)

FU** * LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China 1 LaSW, Chinese Academy of Meteorological Sciences, China Meteorological...

484

A Conduit-Related Genesis Of The Lengshuiqing Intrusive Assemblage...  

Open Energy Info (EERE)

icon A Conduit-Related Genesis Of The Lengshuiqing Intrusive Assemblage (Sichuan, Sw China) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A...

485

Oil and Gas Field Code Index  

U.S. Energy Information Administration (EIA)

000478 TX Cat 000479 TX Cattail Hollow 000480 TX Catto 000481 TX Cavallo West 000482 TX Cayman 000483 TX Cecile South 000484 TX Celery 000485 OK Centerpoint SW

486

News & Resources | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Links Contact Information Advanced Scientific Computing Research U.S. Department of Energy SC-21Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301)...

487

Office of Used Nuclear Fuel Disposition International Program...  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

1000 Independence Avenue, S.W. Washington, D.C. 20585 UFD INTERNATIONAL PROGRAM STRATEGIC PLAN Foreword Message from the Deputy Assistant Secretary for Fuel Cycle...

488

Keep in mind, that with formality, often comes more of a standing...  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

INDIAN COUNTRY ENERGY AND INFRASTRUCTURE WORKING GROUP ICEIWG Sunday, October 30, 2011 HILTON PORTLAND & EXECUTIVE TOWER 921 SW Sixth Avenue Portland, Oregon 503-226-1611 AGENDA...

489

Heating and cooling no longer majority of U.S. home energy use ...  

U.S. Energy Information Administration (EIA)

... more efficient windows, ... EIA - 1000 Independence Avenue, SW, Washington, DC 20585 About EIA Press Room Careers Feedback Contact Us. Sources & Uses Petroleum

490

U.S. Department of Energy OMB No. 1905-0160 U.S. Energy ...  

U.S. Energy Information Administration (EIA)

to protect information against unauthorized access during transmission. ... Mail Stop: BG-076 (Form EIA-858), 1000 Independence Avenue, S.W ... price related. Item 1 ...

491

Research Highlight  

NLE Websites -- All DOE Office Websites (Extended Search)

K-Distribution Method for a SW Radiative Transfer Model Submitter: Ackerman, T. P., University of Washington Area of Research: General Circulation and Single Column Models...

492

Final_Tech_Session_Schedule_and_Location.xls  

NLE Websites -- All DOE Office Websites (Extended Search)

US) * West Pearl Queen (SW US) * Sleipner (North Sea) 1M tonnesyr (1996) * Weyburn (Canada): 2M tonnesyr (2000) Sleipner Sleipner Time Time - - Lapse Seismic Lapse Seismic top...

493

Table 3. Top Five Retailers of Electricity, with End Use Sectors...  

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

c","Investor-Owned",1439002,513084,720009,205909,"-" "4. Sioux Valley SW Elec Coop","Cooperative",543948,273406,37503,233039,"-" "5. Southeastern Electric Coop...

494

International Natural Gas Workshop  

U.S. Energy Information Administration (EIA)

International Natural Gas Workshop U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585 and a member of ...

495

Overview of Geothermal Energy Development  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

Geothermal Energy Geothermal Energy Development Kermit Witherbee Geothermal Geologist/Analyst DOE Office of Indian Energy Webcast: Overview of Geothermal Energy Development Tuesday, January 10, 2012 Geothermal Geology and Resources Environmental Impacts Geothermal Technology - Energy Conversion Geothermal Leasing and Development 2 PRESENTATION OUTLINE GEOTHERMAL GEOLOGY AND RESOURCES 3 Geology - Plate Tectonics 4 Plate Tectonic Processes Schematic Cross-Section "Extensional" Systems- "Rifting" Basin and Range Rio Grand Rift Imperial Valley East Africa Rift Valley "Magmatic" Systems Cascade Range 6 Geothermal Resources(USGS Fact Sheet 2008-3062) 7 State Systems

496

Solid-State Lighting on a Shoestring Budget: The Economics of Off-Grid Lighting for Small Businesses in Kenya  

E-Print Network (OSTI)

for Small Businesses in Kenya Kristen Radecsky*, Petermany people and businesses in Kenya who participated in thisin two small towns in Kenyas Rift Valley Province. The work

Radecsky, Kristen

2009-01-01T23:59:59.000Z

497

An Integrated Mapping And Remote Sensing Investigation Of The Structural  

Open Energy Info (EERE)

Mapping And Remote Sensing Investigation Of The Structural Mapping And Remote Sensing Investigation Of The Structural Control For Fumarole Location In The Eburru Volcanic Complex, Kenya Rift Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Conference Paper: An Integrated Mapping And Remote Sensing Investigation Of The Structural Control For Fumarole Location In The Eburru Volcanic Complex, Kenya Rift Details Activities (0) Areas (0) Regions (0) Abstract: The Eburru volcanic complex is located in the central portion of the Kenya Rift. It belongs to the complex of volcanoes - Suswa, Longonot, Olkaria, Eburru, and Menengai - that. form the Kenya Dome. These volcanoes are geothermal fields, and Olkaria is the site for the first geothermal power plant commissioned in 1981 in the East African Rift System (EARS).

498

CX-007612: Categorical Exclusion Determination  

Energy.gov (U.S. Department of Energy (DOE))

Geological Characterization of the South Georgia Rift Basin for Source Proximal Carbon Dioxide Storage CX(s) Applied: B3.6 Date: 01/10/2012 Location(s): Texas Offices(s): National Energy Technology Laboratory

499

Arabian Journal of Geosciences ISSN 1866-7511  

E-Print Network (OSTI)

, Binna, Nogal and the northwest of Madagascar Karoo rifting was active during the Permo­Triassic (Karoo the Karoo (Permo­Triassic) to the Burdigalian. Drawn up after the literature cited in this article and using

Demouchy, Sylvie

500

South Atlantic continental margins of Africa: A comparison of the tectonic vs climate interplay on the evolution  

E-Print Network (OSTI)

(Gladczenko et al., 1998), interpreted as Permian to Triassic in age (Karoo Rift, Clemson et al., 1999). Post al., 1993). This phase allowed deposition of the extensive Permian­Jurassic Karoo conti- nental

Demouchy, Sylvie