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Note: This page contains sample records for the topic "mt simon sandstone" 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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1

CO2 flood tests on whole core samples of the Mt. Simon sandstone, Illinois Basin  

SciTech Connect (OSTI)

Geological sequestration of CO2, whether by enhanced oil recovery (EOR), coal-bed methane (CBM) recovery, or saline aquifer injection is a promising near-term sequestration methodology. While tremendous experience exists for EOR, and CBM recovery has been demonstrated in existing fields, saline aquifer injection studies have only recently been initiated. Studies evaluating the availability of saline aquifers suitable for CO2 injection show great potential, however, the long-term fate of the CO2 injected into these ancient aqueous systems is still uncertain. For the subject study, a series of laboratory-scale CO2 flood tests were conducted on whole core samples of the Mt. Simon sandstone from the Illinois Basin. By conducting these tests on whole core samples rather than crushed core, an evaluation of the impact of the CO2 flood on the rock mechanics properties as well as the geochemistry of the core and brine solution has been possible. This empirical data could provide a valuable resource for the validation of reservoir models under development for these engineered CO2 systems.

O'Connor, William K.; Rush, Gilbert E.

2005-09-01T23:59:59.000Z

2

DOE Partnership Completes Successful CO2 Injection Test in the Mount Simon Sandstone  

Broader source: Energy.gov [DOE]

The Midwest Regional Carbon Sequestration Partnership, one of seven partnerships in the U.S. Department of Energy's Regional Carbon Sequestration Partnerships program, has successfully injected 1,000 metric tons of carbon dioxide (CO2) into the Mount Simon Sandstone, a deep saline formation that is widespread across much of the Midwest.

3

PowerPoint Presentation  

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

- 400sec 464 MMscfd - Minimum Pressure - 830 psi CAES Aquifer Storage System Geology of Iowa Mt. Simon Sandstone Jordan Sandstone St. Peter Sandstone Glenwood Fm....

4

Diagenesis of Miocene sandstones, South Louisiana  

E-Print Network [OSTI]

sandstones, expressed in relative terms using Hsu's (1977) method Microprobe data of carbonate cements 'n the sandstones 7B Average content of difterent authigenic clay minerals in sandstones Average oil saturation for each sand unit 121 :IST 0F... in nearby sandstones 84 20 Photographs illustrating presence of illite/smectite in sandstones 21 X-ray diffraction patterns of clay-size fraction of sandstone sample . . . . . . . . . . . ~ . ~ . ~ 22 Photographs illustrating presence of kaolinite...

Smith, Richard Lee

1983-01-01T23:59:59.000Z

5

Secondary porosity in sandstones  

SciTech Connect (OSTI)

Secondary porosity in sandstones is caused by dissolution and fracturing, and is common in the sedimentary record. Secondary porosity commonly develops in the deep subsurface and thus provides an opportunity to extend exploration to depths traditionally considered unsuitable for exploration. Two contrasting routes of diagenesis exist in nature: porosity reduction and porosity enhancement. Porosity reduction is commonly caused by compaction and cementation, whereas porosity enhancement is primarily caused by dissolution of carbonate minerals. Two basic types of primary pores (intergranular and intragranular) and four basic types of secondary pores (grain fractures, rock fractures, intergranular, and intragranular) can be differentiated on the basis of (1) position of pores, (2) timing of origin, and (3) processes of origin. The proposed classification system is useful in inferring reservoir quality. Various types of secondary porosity are recognized using a comprehensive set of 20 criteria. The various criteria are based on manner of breakage, pore geometry, grain geometry, products of dissolution, and sediment packing. New evidence suggests that silicate minerals, including quartz, dissolve more commonly than have been reported. The abundant occurrence of secondary porosity in reservoir sandstones emphasizes the importance of secondary porosity in evaluating deep reservoirs.

Shanmugam, G.

1983-03-01T23:59:59.000Z

6

CO{sub 2} Injectivity, Storage Capacity, Plume Size, and Reservoir and Seal Integrity of the Ordovician St. Peter Sandstone and the Cambrian Potosi Formation in the Illnois Basin  

SciTech Connect (OSTI)

The Cambro-Ordovician strata of the Illinois and Michigan Basins underlie most of the states of Illinois, Indiana, Kentucky, and Michigan. This interval also extends through much of the Midwest of the United States and, for some areas, may be the only available target for geological sequestration of CO{sub 2}. We evaluated the Cambro-Ordovician strata above the basal Mt. Simon Sandstone reservoir for sequestration potential. The two targets were the Cambrian carbonate intervals in the Knox and the Ordovician St. Peter Sandstone. The evaluation of these two formations was accomplished using wireline data, core data, pressure data, and seismic data from the USDOE-funded Illinois Basin â?? Decatur Project being conducted by the Midwest Geological Sequestration Consortium in Macon County, Illinois. Interpretations were completed using log analysis software, a reservoir flow simulator, and a finite element solver that determines rock stress and strain changes resulting from the pressure increase associated with CO{sub 2} injection. Results of this research suggest that both the St. Peter Sandstone and the Potosi Dolomite (a formation of the Knox) reservoirs may be capable of storing up to 2 million tonnes of CO{sub 2} per year for a 20-year period. Reservoir simulation results for the St. Peter indicate good injectivity and a relatively small CO{sub 2} plume. While a single St. Peter well is not likely to achieve the targeted injection rate of 2 million tonnes/year, results of this study indicate that development with three or four appropriately spaced wells may be sufficient. Reservoir simulation of the Potosi suggest that much of the CO{sub 2} flows into and through relatively thin, high permeability intervals, resulting in a large plume diameter compared with the St. Peter.

Hannes Leetaru; Alan Brown; Donald Lee; Ozgur Senel; Marcia Coueslan

2012-05-01T23:59:59.000Z

7

Simon Fraser University's  

E-Print Network [OSTI]

a happy second home in the Indigenous Student Centre. Simon Fraser University recognizes the value graduated from Fraser Valley College in 1980 with a diploma in Social Services. Theresa feels her strength

8

Mt Playfair Blair Athol  

E-Print Network [OSTI]

Norwich Park Epping Forest Yatton Outstation Injune Lockington Augathella Crystalbrook Bluff Dysart Saraji CALDERVALE BABBILOORA MT MOFFATT FRANKFIELD WETLANDS MT PLAYFAIR LOCHINVAR PENJOBE TM FOREST VALE TM/MAN DERBYSHIRE DOWNS BILLABOO AL CHESTERTON TM/MAN GLEN ROCK AL SPRINGSURE TM/(SYN) ECHO HILLS AL GREEN VALLEY AL

Greenslade, Diana

9

Student Awards Simon Fraser University  

E-Print Network [OSTI]

Student Awards Simon Fraser University #12;SIMON FRASER UNIVERSITY Simon Fraser University (SFU ­ gifts that will engage over 30,000 students and 6,500 researchers across three campuses, and strengthen our power to engage communities for the next 50 years. As part of this campaign, our goal for student

10

RESTRICTED GRASSMANNIANS SIMON SCOTT  

E-Print Network [OSTI]

Lie groups. Let {ei} i=1 be an orthonormal basis for H and let Hn be the subspace of H spanned by e1RESTRICTED GRASSMANNIANS SIMON SCOTT We begin by reviewing various facts about Grassmannians such p a regularised p- determinant detp : glp - C to be defined (4) det p (1 + T) = det F ((1 + T)e

Bushnell, Colin J.

11

IMPROVING SANDSTONE MATRIX STIMULATION OF OIL  

E-Print Network [OSTI]

IMPROVING SANDSTONE MATRIX STIMULATION OF OIL WELLS BY GAS PRECONDITIONING M. A. Aggour, M. Al, Dhahran, Saudi Arabia ABSTRACT Experience has shown that for sandstone formations, oil wells respond to matrix acidizing in a different manner as compared to gas wells. For oil wells, the improvement

Abu-Khamsin, Sidqi

12

Simon Gervais Professor of Finance  

E-Print Network [OSTI]

Simon Gervais Professor of Finance Faculty CoDirector of the Center for Financial Excellence Simon Gervais is a Full Professor of Finance at The Fuqua School of Business. Prior to joining Fuqua in 2003, he was an Assistant Professor of Finance at the Wharton School of the University of Pennsylvania

Reif, John H.

13

Porosity prediction in sandstones using erosional unconformities  

SciTech Connect (OSTI)

Erosional unconformities of subaerial origin are created by tectonic uplifts and eustatic sea level fall. Most erosional unconformities developed on sandstones are planes of increased porosity because uplifted sandstones are exposed to undersaturated CO/sub 2/-charged meteoric waters that result in dissolution of unstable framework grains and cements. The chemical weathering of sandstones is intensified in humid regions by heavy rainfall, lush vegetation, soil zones, and the voluminous production of inorganic and organic acids. Erosional unconformities are considered hydrologically open systems because of abundant supply of fresh meteoric water and relatively unrestricted transport of dissolved constituents away from the site of dissolution. Thus, porosity in sandstones commonly increases toward overlying unconformities. Empirical models have been developed on the basis of the observed relationship between erosional unconformities and porosity in the underlying sandstones in the North Sea (Middle Jurassic Brent Group) and in the Alaskan North Slope (Triassic Ivishak Formation). An important practical attribute of these models is that they allow for the prediction of porosity in frontier areas by recognizing erosional unconformities in seismic reflection profiles and by constructing subcrop maps for underlying sandstones. Hydrocarbon-bearing sandstone reservoirs in Alaska, Algeria, Australia, China, Libya, Netherlands, North Sea, Norwegian Sea, and Texas occur immediately beneath major erosional unconformities.

Shanmugam, G.

1988-02-01T23:59:59.000Z

14

Porosity prediction in sandstones using erosional unconformities  

SciTech Connect (OSTI)

Erosional unconformities of subaerial origin are created by tectonic uplifts and eustatic sea level fall. Most erosional unconformities developed on sandstones are planes of increased porosity because uplifted sandstones are exposed to undersaturated CO/sub 2/-charged meteoric waters that result in dissolution of unstable framework grains and cements. The chemical weathering of sandstones is intensified in humid regions by heavy rainfall, lush vegetation, soil zones, and the voluminous production of inorganic and organic acids. Erosional unconformities are considered hydrologically open systems because of abundant supply of fresh meteoric water and relatively unrestricted transport of dissolved constituents away from the site of dissolution. Thus, porosity in sandstones commonly increases toward overlying unconformities. Empirical models have been developed on the basis of the observed relationship between erosional unconformities and porosity in the underlying sandstones in the North Sea (Middle Jurassic Brent Group) and in the Alaskan North Slope (Triassic Ivishak Formation). An important practical attribute of these models is that they allow for the prediction of porosity in frontier areas by recognizing erosional unconformities in seismic reflection profiles and by constructing subcrop maps for underlying sandstones. Hydrocarbon-bearing sandstone reservoirs in Alaska, Algeria, Australia, China, Libya, Netherlands, North Sea, Norwegian Sea, and Texas occur immediately beneath major erosional unconformities.

Shanmugam, G.

1988-01-01T23:59:59.000Z

15

Composable Memory Transactions Tim Harris Simon Marlow Simon Peyton Jones Maurice Herlihy  

E-Print Network [OSTI]

Composable Memory Transactions Tim Harris Simon Marlow Simon Peyton Jones Maurice Herlihy Microsoft Research 7 J J Thomson Avenue, Cambridge, UK, CB3 0FB {tharris

Ramsey, Norman

16

Porosity prediction in sandstones using erosional unconformities  

SciTech Connect (OSTI)

Erosional unconformities of subaerial origin are created by tectonic uplifts and eustatic sea level fall. Most erosional unconformities developed on sandstones are planes of increased porosity because uplifted sandstones are exposed to undersaturated CO/sub 2/-charged meteoric waters that result in dissolution of unstable framework grains and cements. The chemical weathering of sandstones is intensified in humid regions by the heavy rainfall, soil zones, lush vegetation, and accompanying voluminous production of organic and inorganic acids. Erosional unconformities are considered hydrologically open systems because of abundant supply of fresh meteoric water and relatively unrestricted transport of dissolved constituents away from the site of dissolution, causing a net gain in porosity near unconformities. Thus, porosity in sandstones tends to increase toward overlying unconformities. Such porosity trends have been observed in hydrocarbon-bearing sandstone reservoirs in Alaska, Algeria, Australia, China, Libya, Netherlands, Norwegian North Sea, Norwegian Sea, and Texas. A common attribute of these reservoirs is that they were all subaerially exposed under heavy rainfall conditions. An empirical model has been developed for the Triassic and Jurassic sandstone reservoirs in the Norwegian North Sea on the basis of the observed relationship that shows an increase in porosity in these reservoirs with increasing proximity to the overlying base of Cretaceous unconformity. An important practical attribute of this model is that it allows for the prediction of porosity in the neighboring undrilled areas by recognizing the base of Cretaceous unconformity in seismic reflection profiles and by constructing subcrop maps.

Shanmugam, G.

1989-03-01T23:59:59.000Z

17

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

) by coordinating budget submissions, estimating and preparing cost projections, liaising with PurchasingHUMAN RESOURCES SIMON FRASER UNIVERSITY ADMINISTRATIVE & PROFESSIONAL JOB DESCRIPTION Position of the position in one or two sentences. Manages the Department's operating, capital, temporary instruction

18

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

funding priorities, budget consideration, application requirements, University policies and proceduresHUMAN RESOURCES SIMON FRASER UNIVERSITY ADMINISTRATIVE & PROFESSIONAL JOB DESCRIPTION Position to Canadian and international funding agencies. The incumbent will assist with the writing and reviewing

19

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

. The position is responsible for developing test scenarios, responding to system problems by investigating regarding the design of testing scenarios and scripts and how to evaluate outcomes. Makes decisions1 HUMAN RESOURCES SIMON FRASER UNIVERSITY TEMPORARY ADMINISTRATIVE & PROFESSIONAL STAFF POSITION

20

Human Resources Simon Fraser University  

E-Print Network [OSTI]

Human Resources Simon Fraser University Administrative and Professional Staff Job Description A. Identification Position Number: 31482 Position Title: Administrative Assistant (Human Resources Liaison) Name guidance, direction, coordination and effective management and implementation of SFU's Human Resources

Kavanagh, Karen L.

Note: This page contains sample records for the topic "mt simon sandstone" 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

Fire Clay coal and sandstone washouts  

SciTech Connect (OSTI)

The Fire Clay coal bed has been studied in a portion of southeastern Kentucky. This seam is easily recognizable by a distinctive flint clay parting. Mine maps, field descriptions, and laboratory investigations were used to investigate this coal bed. Several elongate sandstone bodies cut the seam in the study area. These sandstone bodies are subparallel roughly east-west, and are typically 10[sup 1] to 10[sup 2] m wide, and 10[sup 2] m to tens of kilometers long. These sandstone washouts occur in areas overlain by a larger channel sandstone, which usually is found associated with the thickest areas of the coal seam. In south-central Perry County, a cross section of one washout area was well exposed. North of the washout, a 4 to 7 cm thick cannel coal was present at the base of the sequence. The coal on the north side of the cutout gradually thins from 2 m to 1.5 m away from the washout. On the south side of the washout, the coal thins abruptly from over 1.5 m to 1.25 m within 30 m of the channel. An island of slumped and slickensided coal is present within the washout region. Postdepositional differential compaction of the peat is inferred to be the control on placement of the channel system. The areas of thickest peat compacted the most, creating topographic lows through which the stream moved. The regions of thick coal were probably the result of several controlling factors. Predepositional differential compaction and erosion may have produced relief which influenced peat development. Lithologic and geochemical continuity across the channel is good, supporting postdepositional emplacement of the sandstone bodies.

Andrews, W.M. Jr.; Hower, J.C. (Univ. of Kentucky, Lexington, KY (United States). Center for Applied Energy Research)

1992-01-01T23:59:59.000Z

22

Simon Kelly Postdoctoral Research Associate  

E-Print Network [OSTI]

Simon Kelly Postdoctoral Research Associate Imaging Functionality Group Center for Nanophase. Publications 1. Lakhani A. M.; Kelly S. J.; Pearl T.P., "Design and Operation of a Versatile, Ultrahigh Vacuum, Low Temperature Scanning Probe Microscope," Rev. Sci. Inst., 77 043709 (2006). 2. Kelly, S.; Galli, F

Pennycook, Steve

23

Radionuclide transport in sandstones with WIPP brine  

SciTech Connect (OSTI)

Retardation factors (R) have been measured for the transport of /sup 3/H, /sup 95m/Tc, and /sup 85/Sr in WIPP brine using St. Peter, Berea, Kayenta, and San Felipe sandstone cores. If tritium is assumed to have R=1, /sup 95m/Tc has R=1.0 to 1.3 and therefore is essentially not retarded. Strontium-85 has R = 1.0 to 1.3 on St. Peter, Berea, and Kayenta, but R=3 on San Felipe. This is attributed to sorption on the matrix material of San Felipe, which has 45 volume % matrix compared with 1 to 10 volume % for the others. Retardation factors (R/sub s/) for /sup 85/Sr calculated from static sorption measurements are unity for all the sandstones. Therefore, the static and transport results for /sup 85/Sr disagree in the case of San Felipe, but agree for St. Peter, Berea, and Kayenta.

Weed, H.C.; Bazan, F.; Fontanilla, J.; Garrison, J.; Rego, J.; Winslow, A.M.

1981-02-01T23:59:59.000Z

24

Imprecise reliability by evidential networks Christophe SIMON and Philippe WEBER  

E-Print Network [OSTI]

Imprecise reliability by evidential networks Christophe SIMON and Philippe WEBER October 3, 2008 to adequately tell variability from imprecision. Many representations exist C. Simon and Ph. Weber

Boyer, Edmond

25

Harmonic Cheeger-Simons characters with applications  

E-Print Network [OSTI]

We initiate the study of harmonic Cheeger-Simons characters, with applications to smooth versions of the Geometric Langlands program in the abelian case.

Richard Green; Varghese Mathai

2009-02-13T23:59:59.000Z

26

M.T. Thomas Recipient Named | EMSL  

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

M.T. Thomas Recipient Named M.T. Thomas Recipient Named EMSL Recognizes Patrick Roach for Postdoc Achievement Dr. Patrick Roach Patrick Roach, now an environmental scientist at...

27

Significance of Secondary Porosity in Interpreting Sandstone Composition  

SciTech Connect (OSTI)

Secondary porosity resulting from dissolution of unstable framework grains such as feldspar and rock fragments (including chert) is common in sandstones. Extensive dissolution of framework grains may result in misinterpreting the original composition of a sandstone and, hence, in misinterpreting its provenance. To avoid these problems, secondary porosity caused by grain dissolution must be recognized. Sandstone composition may be properly evaluated by including the dissolved portion of a framework grain as a grain, rather than as porosity, while point counting. This should be useful in interpreting original composition of sandstones and in paleogeographic reconstruction of prospect areas.

Shanmugam, G.

1985-03-01T23:59:59.000Z

28

Berea Sandstone reservoirs in Ashland and Medina Counties, Ohio  

SciTech Connect (OSTI)

The Berea Sandstone is one of the better known rock formations in Ohio. It occurs at shallow depths throughout a broad belt in central Ohio and crops out to the north and west of these counties. In Ashland and Medina Counties, the Berea may be divided into two separately identifiable units. The upper unit, called the blanket Berea in outcrop, is approximately equivalent to the cap Berea in the subsurface. The second unit, which lies below the cap Berea varies considerably in its thickness. The traditional, long-standing, and generally accepted view is that the Berea Sandstone was deposited in Ashland and Medina Counties in southward-flowing river channels. More recent drilling in these counties has demonstrated that these sand channels are not continuous, but are isolated sandstone bodies in which petroleum has accumulated. The reservoir capacity of the Berea is between 8 and 22% with an average porosity of 15%. The sandstone consists of loosely cemented, medium to fine-grained quartz with only rare shale breaks below the cap Berea. In Ashland and Medina Counties, Berea wells generally produce oil. Initial production in this area ranges between 1 or 2 bbl and to 40 BOPD after treatment. Reservoirs in the Berea Sandstone generally are productive where the sandstones are thick. They are also productive where the sandstone is thinner, but high on structure. Although a high structural position is preferred, the critical consideration is the thickness of the sandstone body and the reservoir geometry.

Hillebrand, L.B.; Coogan, A.H.

1984-12-01T23:59:59.000Z

29

Architecture of the upper Sego Sandstone, Book Cliffs, Utah  

E-Print Network [OSTI]

................................................................................................................... 22 SEDIMENTOLOGY.................................................................................................... 26 Marine Shale with Wavy Sandstones............................................................... 26 Highly... surfaces. The cross-section defines an 8.5 kilometer section that begins in Sego Canyon outside of Thompson Springs, Figure 12-Bedding diagram of major facies transitions with sedimentary logs overlain. SEDIMENTOLOGY Upper Sego Sandstone deposits can...

Birkhead, Stanley Scott

2006-04-12T23:59:59.000Z

30

Petrophysical rock classification in the Cotton Valley tight-gas sandstone reservoir with a clustering  

E-Print Network [OSTI]

Petrophysical rock classification in the Cotton Valley tight-gas sandstone reservoir classification method with field data acquired in the Cotton Valley tight-gas sandstone reservoir located

Torres-Verdín, Carlos

31

E-Print Network 3.0 - ahwaz sandstone member Sample Search Results  

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

ratios of Pb in Proterozoic sandstones from basins known to contain high-grade uranium deposits... in altered zones proximal to mineralization. Sandstones completely...

32

Sedimentology, diagenesis, and petrophysics of selected Cherokee group (Desmoinesian) sandstones in southeastern Kansas. Part 2  

SciTech Connect (OSTI)

Medium to very fine-grained sandstones of the Cherokee Group in S.E. Kansas were deposited by unidirectional currents in nearshore, continental channels resulting in sandstone deposits up to 35 m (116 ft) thick. Five lithofacies have been established: (1) conglomeratic sandstones subdivided into thin basal and thick sequence- capping conglomerates, (2) stacked sandstones, (3) crossbedded coarse sandstones, (4) rippled fine sandstones; and (5) interbedded sandstones, shales, and siltstones. The following diagenetic stages were established: Stage 1: rare, localized precipitation of concretionary calcite and siderite cements in both sandstones and shales; Stage 2: extensive chlorite coatings on grains and silica cementation; and Stage 3: patchy kaolinite, siderite, and dolomite-ankerite cements develop while feldspars, micas, and argillaceous rock fragments dissolve. A model is proposed for Cherokee Group sandstones which shows that coarser grain size, less cementation, and fewer argillaceous rock fragments are found in the coarse sandstone lithofacies in the lower portion of sandstone sequences. 96 references.

Woody, M.D.

1983-06-01T23:59:59.000Z

33

Microsoft Word - MtRichmond_CX  

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

Dorie Welch Project Manager - KEWM-4 Proposed Action: Mt. Richmond property funding Fish and Wildlife Project No.: 2011-003-00, BPA-007071 Categorical Exclusion Applied (from...

34

2-D discrete element modeling of unconsolidated sandstones  

E-Print Network [OSTI]

developed in this thesis is compared to the results of triaxial tests performed in cylindrical core samples of unconsolidated sandstones saturated with heavy oil. The discrete element model treats the sand as a two dimensional assembly of particles...

Franquet Barbara, Javier Alejandro

2012-06-07T23:59:59.000Z

35

Acidizing of Sandstone Reservoirs Using HF and Organic Acids  

E-Print Network [OSTI]

Mud acid, which is composed of HCl and HF, is commonly used to remove the formation damage in sandstone reservoirs. However, many problems are associated with HCl, especially at high temperatures. Formic-HF acids have served as an alternative...

Yang, Fei

2012-10-19T23:59:59.000Z

36

Feldspar diagenesis in the Yowlumne sandstone, Kern County, California  

E-Print Network [OSTI]

FELDSPAR DIAGENESIS IN THE YOWLUMNE SANDSTONE& KERN COUNTY& CALIFORNIA A Thesis by JOHN DAVID PIKE Submitted to the Graduate College of Texas A&M University in partial fulfillment of the requirement for the degree of MASTER OF SCIENCE... December 1981 Major Subject: Geology FELDSPAR DIAGENESIS IN THE YOWLUMNE SANDSTONE, KERN COUNTY, CALIFORNIA A Thesis by JOHN DAVID PIKE Approved as to style and content by: (Chairman of Committee) ( mber) (Me er) (He'a' of Dep rtment) December...

Pike, John David

1981-01-01T23:59:59.000Z

37

Leveraging Interpolant Strength in Model Simone Fulvio Rollini1  

E-Print Network [OSTI]

Leveraging Interpolant Strength in Model Checking Simone Fulvio Rollini1 , Ondrej Sery1,2 , and Natasha Sharygina1 1 Formal Verification Lab, University of Lugano, Switzerland {simone.fulvio

38

Daryl B. Simons--Hydraulic Engineer, Researcher, and Educator  

E-Print Network [OSTI]

FORUM Daryl B. Simons--Hydraulic Engineer, Researcher, and Educator Nani Bhowmik, P.E., M@engr.colostate.edu Introduction Daryl B. Simons is remembered for his hard work, dedication, and perseverance as an hydraulic

39

CURRICULUM VITAE Simon Kasif, Ph.D.  

E-Print Network [OSTI]

CURRICULUM VITAE Simon Kasif, Ph.D. Professor of Biomedical Engineering, Bioinformatics Mathematics M.S. University of Maryland May 1983 Computer Science Ph.D. University of Maryland May 1985+ Decision Tree Induction (OC1): 510+ Init. Sequence of the Human Genome (Public Consortium): 5900+ Numerous

40

Cornell Probability Summer School Simon Tavare  

E-Print Network [OSTI]

Cornell Probability Summer School 2006 Simon Tavar´e Lecture 6 Outline · We looked at evolution) Questions about Phylogenetic Trees · Topology of tree (the branching order) · Branch lengths (time of common Pleistocene 1 0.15 19 Middle Pleistocene 2 0.9 28 Early Pleistocene 3 1.8 22 Late Pliocene 4 3.6 47 Early

Durrett, Richard

Note: This page contains sample records for the topic "mt simon sandstone" 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

Oil Trading Simon Basey / November 28, 2013  

E-Print Network [OSTI]

. A hurricane develops in the Gulf of Mexico and threatens to shut in crude production. d. New data indicatesOil Trading Simon Basey / November 28, 2013 #12;2 What does IST do? Imports crude oil and other Markets BP's equity crude oil, NGLs and natural gas Generates entrepreneurial trading income Manages BP

Sheldon, Nathan D.

42

UNIVERSIDAD SIMON BOLIVAR VICE-RECTORADO ADMINISTRATIVO  

E-Print Network [OSTI]

DISEÃ?O, ARQUITECTURA Y ARTES PLASTICAS. OFICINA DE ORGANIZACION Y SISTEMAS #12;UNIVERSIDAD SIMON BOLIVAR de 77 L DEPARTAMENTO DE DISEÃ?O, ARQUITECTURA Y ARTES PLASTICAS INDICE DE CONTENIDO 1. ORGANIZACION. 1 DISEÃ?O, ARQUITECTURA Y ARTES PLASTICAS 3. DESCRIPCION DE CARGOS 3.1. Jefatura del Departamento. 3

Vásquez, Carlos

43

Depositional environment of downdip Yegua (Eocene) sandstones, Jackson County, Texas  

E-Print Network [OSTI]

as the geometry of the growth fault alters the reservoir morphology, The sandstones are fine to medium grained. Grain size within beds fines upward from 0. 40 mm at the base to 0. 13 mm at the top. The sandstones contain an average of 50% quartz... along the downthrown side of a growth fault that has 550 ft (167. 6 m) of throw. The channels form dip-trending bodies on the updip side of the growth fault, but form a strike trending, elongate body on the downthrown side of the fault...

Whitten, Christopher James

1988-01-01T23:59:59.000Z

44

Digital outcrop mapping of a reservoir-scale incised valley fill, Sego Sandstone, Book Cliffs, Utah  

E-Print Network [OSTI]

methodologies are demonstrated by mapping rock variations and stratal geometries within several kilometers-long, sub-parallel exposures of the Lower Sego Sandstone in San Arroyo Canyon, Book Cliffs, Utah. The digital outcrop model of the Lower Sego Sandstone...

Fey, Matthew F.

2009-06-02T23:59:59.000Z

45

Petrologic and petrophysical evaluation of the Dallas Center Structure, Iowa, for compressed air energy storage in the Mount Simon Sandstone.  

SciTech Connect (OSTI)

The Iowa Stored Energy Plant Agency selected a geologic structure at Dallas Center, Iowa, for evaluation of subsurface compressed air energy storage. The site was rejected due to lower-than-expected and heterogeneous permeability of the target reservoir, lower-than-desired porosity, and small reservoir volume. In an initial feasibility study, permeability and porosity distributions of flow units for the nearby Redfield gas storage field were applied as analogue values for numerical modeling of the Dallas Center Structure. These reservoir data, coupled with an optimistic reservoir volume, produced favorable results. However, it was determined that the Dallas Center Structure cannot be simplified to four zones of high, uniform permeabilities. Updated modeling using field and core data for the site provided unfavorable results for air fill-up. This report presents Sandia National Laboratories' petrologic and petrophysical analysis of the Dallas Center Structure that aids in understanding why the site was not suitable for gas storage.

Heath, Jason E.; Bauer, Stephen J.; Broome, Scott Thomas; Dewers, Thomas A.; Rodriguez, Mark Andrew

2013-03-01T23:59:59.000Z

46

Continuity and internal properties of Gulf Coast sandstones and their implications for geopressured fluid production  

SciTech Connect (OSTI)

The intrinsic properties of the genetic sandstone units that typify many geopressured geothermal aquifers and hydrocarbon reservoirs in the Gulf Coast region were systematically investigated classified, and differentiated. The following topics are coverd: structural and stratigraphic limits of sandstone reservoirs, characteristics and dimensions of Gulf Coast sandstones; fault-compartment areas; comparison of production and geologic estimates of aquifer fluid volume; geologic setting and reservoir characteristics, Wells of Opportunity; internal properties of sandstones; and implications for geopressured fluid production. (MHR)

Morton, R.A.; Ewing, T.E.; Tyler, N.

1983-01-01T23:59:59.000Z

47

Depositional environment of lower cretaceous Mitchell sandstone, St. Mary and Duty fields, Lafayette County, Arkansas  

E-Print Network [OSTI]

of the first facies are composed of stacked sandstone sets with a mean grain size of 0. 17 mm (fine grained) and a composition of 78% quartz, 11% rock fragments (predominantly polycrystalline quartz), and 9% matrix. The grain size and quartz : matrix ratio... sediments transported by the easterly-flowing long- shore currents. The thin, carbonaceous washover "A" and "B" sandstones of the second facies and the "A" sandstone of the third facies are finer grained and less quartzose than the barrier sandstones...

Mazzullo, Elsa Kapitan

1983-01-01T23:59:59.000Z

48

Depositional environment and reservoir morphology of the Upper Wilcox sandstones, Katy gas field, Waller County, Texas  

E-Print Network [OSTI]

overbank sandstones. Sandstones become thinner and less frequent upward in the section. Thin sand- stones 1n the predominantly shale section are widespread and exhibit sedimentary structures commonly observed in turbidity-current deposits (ABCDE, ABDE... feet of depth. Production in the Upper Wilcox section is from multiple sandstone units within a shale section on a local structural closure (Fig. 2). The properties of these sandstone units and the local stratigraphic variation determine...

DePaul, Gilbert John

1979-01-01T23:59:59.000Z

49

Z .Chemical Geology 152 1998 227256 The thermal and cementation histories of a sandstone petroleum  

E-Print Network [OSTI]

Z .Chemical Geology 152 1998 227­256 The thermal and cementation histories of a sandstone petroleum-feldspars recovered at various depths from a deep well drilled through a carbonate-cemented sandstone petroleum of a sandstone petroleum xreservoir, Elk Hills, California. Part 2: In situ oxygen and carbon isotopic results

50

Evaluating Berea Sandstone reservoirs in eastern Ashland County, Ohio  

SciTech Connect (OSTI)

The Berea Sandstone is a principal oil and gas reservoir in eastern Ashland County. It is stratigraphically situated above the red and gray Bedford shales and below the black Sunbury shale member of the Cuyahoga Formation, all of which are Late Devonian or Early Mississippian in age. In the study area, the Berea Sandstone is found at depths between 400 and 800 ft. It outcrops in an arcuate band to the north and west of the county. Geophysical logs indicate the reservoir capacity of the Berea is between 8 and 22%, with an average porosity of 15%. Generally, the Berea is a loosely cemented, gray to buff quartzose sandstone with few accessory minerals. The cement may be calcite, silica, or minor ferruginous materials. The reservoir geometry in eastern Ashland County is peculiar because these sands thin and thicken within relatively short distances. The long-standing explanation for this phenomenon is that these sands were deposited in incised river channels that had downcut through the Bedford shales as a result of isolated uplift in north-central Ohio. Recent subsurface mapping in this area shows that the continuity of these channels may be challenged. Also, well-ticket data indicate that red shale occurs above the Berea sands. This occurrence and the soft-sediment deformation between the Bedford Shale and Berea Sandstone indicate that these units were deposited contemporaneously rather than as two separate events.

Hillebrand, L.B.; Coogan, A.H.

1986-08-01T23:59:59.000Z

51

Mt. Baker Geothermal Project | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia: Energy Resources Jump to:46 -Energieprojekte3 ClimateSpurr GeothermalCarmel Public Utility Co JumpRanierMt StMt.

52

Forms and Determinant Lines Simon Scott  

E-Print Network [OSTI]

has discrete spectrum {(n + )2 , (n - )2 : n N}, where u = e2i satisfies u2 (1 + |z|2 ) + 2u(z + z Forms and Determinant Lines Simon Scott 1 Introduction The purpose here is to give a direct (M) Hi-2 (Y ) is integration over the fibres. That is, with = c1(T) ch(Ind (m)) = f em · 1 - e

Bushnell, Colin J.

53

Secondary porosity in sandstones: basic contributions of Chepikov and Savkevich  

SciTech Connect (OSTI)

The concept of secondary porosity in sandstones - porosity caused primarly by dissolution - has gained considerable attention recently. The basic contributions made by Chepikov and Savkevich, however, have been ignored completely in North American publications. Chepikov et al not only developed the first set of criteria for recognizing secondary porosity, but also attributed the dissolution of cements to the arrival of oil. Savkevich was the first to illustrate the trend of increasing porosity at considerable depths. 1 figure, 1 table.

Shanmugam, G.

1984-01-01T23:59:59.000Z

54

Secondary porosity in sandstones: basic contributions of Chepikov and Savkevich  

SciTech Connect (OSTI)

The concept of secondary porosity in sandstones-porosity caused primarily by dissolution--has gained considerable attention recently. The basic contributions made by Chepikov and Savkevich, however, have been ignored completely in North American publications. Chepikov et al not only developed the first set of criteria for recognizing secondary porosity, but also attributed the dissolution of cements to the arrival of oil. Savkevich was the first to illustrate the trend of increasing porosity at considerable depths.

Shanmugam, G.

1984-01-01T23:59:59.000Z

55

Permeability decrease in argillaceous sandstone; experiments and modelling  

SciTech Connect (OSTI)

Core flooding experiments on argillaceous sandstone are carried out showing that for high injection flow rates permeability reduction occurs. The decrease of permeability is a consequence of the migration of insitu particles. Two models are used to simulate the observed phenomena. The so-called network model is able to give insight in the physics behind the particle migration. The other model based on mass balance and constitutive laws is used for quantitative and qualitative comparison with the experiments.

Egberts, Paul; van Soest, Lennard; Vernoux, Jean-Francois

1996-01-24T23:59:59.000Z

56

Estimating sandstone permeability using network models with pore size distributions  

E-Print Network [OSTI]

in appearance to empirical data. A network model is developed to simulate the pore geometry of a clean, well-sorted sandstone. Pores were modeled as straight capillaries connected in various lattice configurations. Complex lattice configurations produce more... properties and can be closely monitored, allowing for study of their effects on flow in the network lattice. Various parameter variation techniques are introduced in the literature. These techniques induce flow property changes in the model allowing rock...

Mathews, Alan Ronald

1991-01-01T23:59:59.000Z

57

Office of Nuclear Physics Jehanne Simon-Gillo  

E-Print Network [OSTI]

Office of Nuclear Physics Jehanne Simon-Gillo Acquisition Executive (Acting) Office of Nuclear Physics Jehanne Simon-Gillo Program Manager BNL Site Office Nand Narain Federal Project Director NASA A. McNerney Physics Support D. Raparia E. Beebe A. Kponou M. Okamura A. Pikin #12;

58

Developing Mt. Hope: The megawatt line  

SciTech Connect (OSTI)

After facing numerous obstacles, including opposition and competition, the Mt. Hope pumped-storage project in New Jersey has been licensed by FERC. That license will allow a former iron ore mine site to be used in producing a new resource-hydroelectricity. In early August 1992, after more than seven years of effort, the 2,000-MW Mt. Hope Waterpower Project was licensed by the Federal Energy Regulatory Commission (FERC). Getting the $1.8 billion pumped-storage project licensed was not an easy task. It involved 54 submittals to FERC, six public meetings, and costs of more than $12 million. Along the way, the project has withstood competing applications, community opposition, and legal battles. Getting a project of this magnitude off the ground is a challenge for even the most experienced developer. The effort was especially challenging for the Halecrest Company, a local family-owned and operated firm with no previous experience in hydroelectric development. When financing became tight, creative ways were found to raise seed capital for the project. When hydroelectric experience was needed, the company developed a world-class corporate team that carried Mt. Hope through the complexities of the licensing process and beyond. With license now in hand, the project developers are ready to move forward with negotiating power sales contracts and securing construction financing. The resulting project will be the second largest pumped-storage facility in the country-second only to the 2,100-MW Bath County project in Virginia. Mt. Hope will take six years to construct and is scheduled to be phased into operation beginning in 1999.

Rodzianko, P.; Fisher, F.S.

1992-12-01T23:59:59.000Z

59

Marysville Mt Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia: Energy Resources Jump to:46 - 429Lacey,(MonasterLowellis a townLoading map...(Redirected from Marysville Mt

60

Simon Property Group | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExplorationUT-g Grant ofRichardton AbbeyARaftPadomaSierraSilver PeakWind FarmSimon

Note: This page contains sample records for the topic "mt simon sandstone" 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

Depositional environment of upper Wilcox sandstones, Northeast Thompsonville field, Jim Hogg and Webb Counties, Texas  

E-Print Network [OSTI]

in Shell Fulbright 1, Northeast Thompsonvi lie field. 38 Figure 13 Grain size, composition, and bedsets in the Hinnant 9 sandstone in ARCO McLean A3, Northeast Thompsonvi lie field. Page 39 14 15 16 17 Electric log character, textural..." facies in the Hinnant 1 sandstone in Standard of Texas Holbein 1, Northeast Thompsonville field. Electric log character, textural and compositional changes, and bedding characteristics of the "massive" facies in the Hinnant 1 sandstone in ARCO Mc...

Tedford, Fredrick John

1977-01-01T23:59:59.000Z

62

Facies Description and Interpretation of the Upper Lower Hickory Sandstone, Riley Formation, Central Texas  

E-Print Network [OSTI]

............................................................................................... viii INTRODUCTION ................................................................................................. 1 OVERVIEW OF WORLDWIDE PRE-SILURIAN SEDIMENTOLOGY.............. 4 HICKORY SANDSTONE.................................................................. 67 Pre-Silurian Sedimentology........................................................................ 68 CONCLUSIONS ................................................................................................... 69 REFERENCES...

Cook, Timothy D.

2010-01-16T23:59:59.000Z

63

Mt Wheeler Power, Inc | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home Page on Office of InspectorConcentrating Solar Powerstories onFocus Area EnergyMohawkaccrediation of NIE) Jump to:Open JumpMt

64

An Improved Model for Sandstone Acidizing and Study of the Effect of Mineralogy and Temperature on Sandstone Acidizing Treatments and Simulation  

E-Print Network [OSTI]

Sandstone acidizing is a complex operation because the acidizing fluid reacts with a variety of minerals present in the formation that results in a wide range of reaction products. The hydrofluoric acid (HF) reaction rate differs widely from mineral...

Agarwal, Amit Kumar

2013-01-14T23:59:59.000Z

65

SCALING RANDOM WALKS ON ARBITRARY SETS Simon C. Harris  

E-Print Network [OSTI]

SCALING RANDOM WALKS ON ARBITRARY SETS by Simon C. Harris , Robin Sibson and David Williams School deterministic sets I. In the 1-dimensional case discussed here and in the following paper by Harris, much

Harris, Simon Colin

66

SIMON FRASER UNIVERSITY SENIOR ADMINISTRATIVE/ACADEMIC PERSONNEL  

E-Print Network [OSTI]

Sept.1/09-Aug.31/15 #12;FACULTY OF ARTS & SOCIAL SCIENCES, (Cont'd.) Philosophy, Chair Dr. M. Hahn Sept Financial Risk Management, Program Director Dr. Jan Simon

67

Red Fork sandstone of Oklahoma: depositional history and reservoir distribution  

SciTech Connect (OSTI)

The Middle Pennsylvanian Red Fork sandstone formed as a result of progradation across eastern Kansas and most of Oklahoma. The Red Fork is one of several transgressive-regressive sequences (cyclothems) developed within the Desmoinesian Cherokee Group. Sea level changes, together with varying subsidence, were dominant factors controlling the general stratigraphic (correlative) characteristics of the Red Fork interval. Progradation was episodic, with sand deposition in the more active part of the basin during lower sea level stands and valley-fill deposition in the more stable areas during sea level rises. A map of Red Fork sand trends reveals an alluvial-deltaic complex covering most of Oklahoma. The Red Fork consists primarily of alluvial-valley and plain (fluvial) bodies in the northernmost part of northeastern Oklahoma, alluvial-deltaic bodies in most of the remaining parts of the shelf area, and off-shelf submarine-fan and slope basinal-floor complexes within the deeper part of the Anadarko basin. Determination of reservoir trend and genesis requires integration of rock and log data. Logs need to be calibrated to cores in order to estimate depositional environments accurately and to make a reasonable assessment of diagenetic overprints. Much of the oil and gas has been trapped in stratigraphic traps, and a significant amount of oil is in channel sandstones with trends at high angles to the structural grain. In some areas, secondary clay, in particular chloritic clay, has resulted in microporosity, high water saturation, and correspondingly low resistivities in oil reserves.

Shelton, J.W.; Fritz, R.D.; Johnson, C.

1989-03-01T23:59:59.000Z

68

Pore water evolution in oilfield sandstones: constraints from oxygen isotope microanalyses of quartz cement  

E-Print Network [OSTI]

of quartz cement Ann M.E. Marchanda,*, Calum I. Macaulayb , R. Stuart Haszeldinea , Anthony E. Fallickc--direct measurements were not possible) precipitated in the sandstones at temperatures jC; (2) the second zone B in the sandstones most likely between 70 and 90 jC; (3) the third zone C (homogeneous CL pattern and directly

Haszeldine, Stuart

69

Evalutaion of Multi-Stage Sandstone Acidizing Uging an Organic Mud Acid and a Clay Stabalizer  

E-Print Network [OSTI]

and clay particles. The purpose of this study is to present and evaluate multi-stage acid injection into the Bandera sandstone cores to remove formation damage. In this study, coreflood experiments were conducted on Bandera sandstone cores (1.5 in. x 6 in...

Sakipour, Armin

2013-05-29T23:59:59.000Z

70

Mineral paragenesis and textures associated with sandstone-hosted roll-front uranium deposits, NW China  

E-Print Network [OSTI]

, People's Republic of China c Northwest Institute of Uranium Geology, China National Nuclear CorporationMineral paragenesis and textures associated with sandstone-hosted roll-front uranium deposits, NW, Wuyiyi and Shihongtan sandstone-hosted roll-front uranium deposits, northwest China. The mineralization

Fayek, Mostafa

71

,"Sweetgrass, MT Natural Gas Pipeline Imports From Canada (MMcf...  

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

Sweetgrass, MT Natural Gas Pipeline Imports From Canada (MMcf)" ,"Click worksheet name or tab at bottom for data" ,"Worksheet Name","Description"," Of Series","Frequency","Latest...

72

,"Whitlash, MT Natural Gas Pipeline Imports From Canada (MMcf...  

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

Whitlash, MT Natural Gas Pipeline Imports From Canada (MMcf)" ,"Click worksheet name or tab at bottom for data" ,"Worksheet Name","Description"," Of Series","Frequency","Latest...

73

,"Babb, MT Natural Gas Pipeline Imports From Canada (MMcf)"  

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

Imports From Canada (MMcf)" ,"Click worksheet name or tab at bottom for data" ,"Worksheet Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Babb, MT...

74

,"Havre, MT Natural Gas Pipeline Imports From Canada (MMcf)"  

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

Imports From Canada (MMcf)" ,"Click worksheet name or tab at bottom for data" ,"Worksheet Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Havre, MT...

75

Water Sampling At Mt Princeton Hot Springs Geothermal Area (Olson...  

Open Energy Info (EERE)

Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Water Sampling At Mt Princeton Hot Springs Geothermal Area (Olson & Dellechaie, 1976)...

76

Ground Gravity Survey At Mt Princeton Hot Springs Geothermal...  

Open Energy Info (EERE)

to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Ground Gravity Survey At Mt Princeton Hot Springs Geothermal Area (Case, Et Al., 1984) Exploration...

77

Vertical Electrical Sounding Configurations At Mt Princeton Hot...  

Open Energy Info (EERE)

navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Vertical Electrical Sounding Configurations At Mt Princeton Hot Springs Geothermal Area (Zohdy, Et Al.,...

78

Anomalous spin of the Chern-Simons-Georgi-Glashow model  

E-Print Network [OSTI]

With the Coulomb gauge, the Chern-Simons-Georgi-Glashow (CSGG) model is quantized in the Dirac formalism for the constrained system. Combining the Gauss law and Coulomb gauge consistency condition, the difference between the Schwinger angular momentum and canonical angular momentum of the system is found to be an anomalous spin. The reason for this result lies in that the Schwinger energy momentum tensor and the canonical one have different symmetry properties in presence of the Chern-Simons term.

Huo Qiu-Hong; Jiang Yunguo

2012-05-08T23:59:59.000Z

79

WPA Omnibus Award MT Wind Power Outreach  

SciTech Connect (OSTI)

The objective of this grant was to further the development of Montanaâ??s vast wind resources for small, medium, and large scale benefits to Montana and the nation. This was accomplished through collaborative work with wind industry representatives, state and local governments, the agricultural community, and interested citizens. Through these efforts MT Dept Environmental Quality (DEQ) was able to identify development barriers, educate and inform citizens, as well as to participate in regional and national dialogue that will spur the development of wind resources. The scope of DEQâ??s wind outreach effort evolved over the course of this agreement from the development of the Montana Wind Working Group and traditional outreach efforts, to the current focus on working with the stateâ??s university system to deliver a workforce trained to enter the wind industry.

Brian Spangler, Manager Energy Planning and Renewables

2012-01-30T23:59:59.000Z

80

Data Update for Mt. Tom, Holyoke, MA August 2006  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA August 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Elkinton Monthly Data Summary for August 2006 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

Note: This page contains sample records for the topic "mt simon sandstone" 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

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA June 2005 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for June 2005 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59.2" N, 72

Massachusetts at Amherst, University of

82

Data Update for Mt. Tom, Holyoke, MA January 2006  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA January 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for December 2005 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

83

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA May 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for May 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

84

Data Update for Mt. Tom, Holyoke, MA October 2006  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA October 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Elkinton Monthly Data Summary for October 2006 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

85

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA July 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for July 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

86

Data Update for Mt. Tom, Holyoke, MA December 2005  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA December 2005 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for December 2005 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

87

Data Update for Mt. Tom, Holyoke, MA October 2005  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA October 2005 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for October 2005 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

88

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA July 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Elkinton Monthly Data Summary for July 2006 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

89

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA July 2005 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for July 2005 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59.2" N, 72

Massachusetts at Amherst, University of

90

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA March 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for March 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

91

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA May 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for May 2006 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59.2" N, 72

Massachusetts at Amherst, University of

92

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA April 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for April 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

93

Data Update for Mt. Tom, Holyoke, MA October 2007  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA October 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for October 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

94

Data Update for Mt. Tom, Holyoke, MA November 2005  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA November 2005 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for November 2005 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

95

Data Update for Mt. Tom, Holyoke, MA January 2008  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA January 2008 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for January 2008 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

96

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA June 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for June 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

97

Data Update for Mt. Tom, Holyoke, MA January 2007  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA January 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for January 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

98

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA April 2008 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for April 2008 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

99

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA March 2008 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for March 2008 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

100

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA June 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Elkinton Monthly Data Summary for June 2006 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

Note: This page contains sample records for the topic "mt simon sandstone" 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.


101

Data Update for Mt. Tom, Holyoke, MA November 2006  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA November 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Elkinton Monthly Data Summary for November 2006 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

102

Data Update for Mt. Tom, Holyoke, MA February 2007  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA February 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for February 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

103

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA April 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for April 2006 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59.2" N, 72

Massachusetts at Amherst, University of

104

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA March 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for March 2006 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59.2" N, 72

Massachusetts at Amherst, University of

105

Data Update for Mt. Tom, Holyoke, MA August 2005  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA August 2005 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for August 2005 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

106

Data Update for Mt. Tom, Holyoke, MA Prepared for  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA May 2008 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for May 2008 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

107

Data Update for Mt. Tom, Holyoke, MA August 2007  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA August 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for August 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

108

Data Update for Mt. Tom, Holyoke, MA February 2006  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA February 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for February 2005 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

109

Data Update for Mt. Tom, Holyoke, MA February 2008  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA February 2008 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for February 2008 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

110

Data Update for Mt. Tom, Holyoke, MA November 2007  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA November 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for November 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

111

Data Update for Mt. Tom, Holyoke, MA September 2007  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA September 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Puneet Malhotra Monthly Data Summary for September 2007 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

112

Data Update for Mt. Tom, Holyoke, MA September 2006  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA September 2006 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Elkinton Monthly Data Summary for September 2006 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

113

Data Update for Mt. Tom, Holyoke, MA September 2005  

E-Print Network [OSTI]

Data Update for Mt. Tom, Holyoke, MA September 2005 Prepared for Massachusetts Technology Collaborative 75 North Drive, Westborough, MA 01581 By Melissa Ray Monthly Data Summary for September 2005 This update summarizes the monthly data results for the Mt. Tom monitoring site in Holyoke, MA, at 42° 14' 59

Massachusetts at Amherst, University of

114

Effect of confining pressure on pore volume in tight sandstones  

SciTech Connect (OSTI)

The effect of confining pressure on the pore volume of some tight sandstones from the Uinta Basin, Utah, was investigated. A new method based on the pressure-volume relationships of a gas was developed and used to measure pore volume reduction. The results were compared with the results obtained using the more common method that involves the measurement of liquid expelled from a saturated core and were found to be in good agreement. Pore volume compressibility of the samples studies is in the range of values reported by other investigators and ranges from 2.0 x 10/sup -6/ to 1.3 x 10/sup -5/ pv/pv/psi at a confining pressure of 5,000 psi.

Sampath, K.

1982-05-01T23:59:59.000Z

115

The influence of pore fluids on the frictional properties of quartzose sandstone  

E-Print Network [OSTI]

the influence of pore fluids on the frictional properties of Tennessee and Coconino Sandstones, a series of triaxial compression tests have been performed. Specimens tested have been dry or they have contained kerosene, distilled water, or solutions of FeC1... Sandstone at different effective confining pressure. 19 Stress-shortening curves of four experiments performed with Tennessee Sandstone at 1 kb effective pressure: dry, saturated with kerosene, water, or 5x10 4 FeC13 solution. 21 Stress-shortening curves...

Blackwell, Michael Lloyd

1973-01-01T23:59:59.000Z

116

Facies architecture of the Bluejacket Sandstone in the Eufaula Lake area, Oklahoma: Implications for the reservoir characterization of the Bartlesville Sandstone  

SciTech Connect (OSTI)

Outcrop studies of the Bluejacket Sandstone (Middle Pennsylvanian) provide significant insights to reservoir architecture of the subsurface equivalent Bartlesville Sandstone. Quarry walls and road cuts in the Lake Eufaula area offer excellent exposures for detailed facies architectural investigations using high-precision surveying, photo mosaics. Directional minipermeameter measurements are being conducted. Subsurface studies include conventional logs, borehole image log, and core data. Reservoir architectures are reconstructed in four hierarchical levels: multi-storey sandstone, i.e. discrete genetic intervals; individual discrete genetic interval; facies within a discrete genetic interval; and lateral accretion bar deposits. In both outcrop and subsurface, the Bluejacket (Bartlesville) Sandstone comprises two distinctive architectures: a lower braided fluvial and an upper meandering fluvial. Braided fluvial deposits are typically 30 to 80 ft thick, and are laterally persistent filling an incised valley wider than the largest producing fields. The lower contact is irregular with local relief of 50 ft. The braided-fluvial deposits consist of 100-400-ft wide, 5-15-ft thick channel-fill elements. Each channel-fill interval is limited laterally by an erosional contact or overbank deposits, and is separated vertically by discontinuous mudstones or highly concentrated mudstone interclast lag conglomerates. Low-angle parallel-stratified or trough cross-stratified medium- to coarse-grained sandstones volumetrically dominate. This section has a blocky well log profile. Meandering fluvial deposits are typically 100 to 150 ft thick and comprise multiple discrete genetic intervals.

Ye, Liangmiao; Yang, Kexian [Univ. of Tulsa, OK (United States)

1997-08-01T23:59:59.000Z

117

Refined Chern-Simons Theory and Knot Homology  

E-Print Network [OSTI]

The refined Chern-Simons theory is a one-parameter deformation of the ordinary Chern-Simons theory on Seifert manifolds. It is defined via an index of the theory on N M5 branes, where the corresponding one-parameter deformation is a natural deformation of the geometric background. Analogously with the unrefined case, the solution of refined Chern-Simons theory is given in terms of S and T matrices, which are the proper Macdonald deformations of the usual ones. This provides a direct way to compute refined Chern-Simons invariants of a wide class of three-manifolds and knots. The knot invariants of refined Chern-Simons theory are conjectured to coincide with the knot superpolynomials -- Poincare polynomials of the triply graded knot homology theory. This conjecture is checked for a large number of torus knots in S^3, colored by the fundamental representation. This is a short, expository version of arXiv:1105.5117, with some new results included.

Mina Aganagic; Shamil Shakirov

2012-02-12T23:59:59.000Z

118

Interactive Arts and Technology Student Union Room 245, Simon Fraser University Surrey  

E-Print Network [OSTI]

Society). Page 1 #12;Interactive Arts and Technology Student Union Room 245, Simon Fraser UniversityInteractive Arts and Technology Student Union Room 245, Simon Fraser University Surrey 2400 Central City Surrey BC V3T 2W1 604-268-7542 The Board of Directors Simon Fraser Student Society Maggie Bentson

119

Geophysical Fault Mapping Using the Magnetic Method at Hickory Sandstone Aquifer, Llano Uplift, Texas  

E-Print Network [OSTI]

A magnetic study over a 95 m x 150 m area of the Hickory sandstone aquifer in central Texas was carried out as part of multitechnique geophysical investigation that included ground penetrating radar (GPR), electromagnetic (EM), seismic...

Pereira, Antonio Do Nascimento

2013-04-05T23:59:59.000Z

120

Investigating the Use of Chelating Agents for Clay Dissolution and Sandstone Acidizing Purposes  

E-Print Network [OSTI]

Mud acid, a mixture of HCl and HF, has been frequently used for stimulating sandstone reservoirs. However, using HCl in such environments can be problematic, especially at higher temperatures. Some of the most common problems are the following: clay...

Andotra, Gautam

2014-08-06T23:59:59.000Z

Note: This page contains sample records for the topic "mt simon sandstone" 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

Sedimentology, diagenesis, and petrophysics of selected Cherokee group (Desmoinesian) sandstones in Southeastern Kansas. Part 1  

SciTech Connect (OSTI)

Pennsylvanian deposits of the Cherokee Group in S.E. Kansas and N.E. Oklahoma contain petroleum bearing sandstones that currently are being considered for the application of enhanced oil recovery processes. The objectives of this research are to determine pertinent geologic and petrophysical properties of Cherokee Group sandstones and to establish relationships among these properties to aid in understanding fluid movement in reservoirs during enhanced recovery operations. The area of study is the portion of the Cherokee Basin in S.E. Kansas. Eighteen cores containing a total of 27 individual sandstone bodies from the Cherokee Group were selected from the core library of the Kansas Geological Survey. Depths at which cores were taken range from 9 m on the eastern side of the study area to over 1050 m on the western side of the study area. These sandstones are representative of the numerous narrow, elongate, lenticular, discontinuous sand bodies characteristic of the Pennsylvanian deposits of this area.

Woody, M.D.

1983-05-01T23:59:59.000Z

122

An In-depth Investigation of an Aluminum Chloride Retarded Mud Acid System on Sandstone Reservoirs  

E-Print Network [OSTI]

Sandstone acidizing using mud acid is a quick and complex process where dissolution and precipitation occur simultaneously. Retarded mud acids are less reactive with the rock reducing the reaction rate hence increased penetration into the formation...

Aneto, Nnenna

2012-07-16T23:59:59.000Z

123

Pore-scale modeling of electrical and fluid transport in Berea sandstone  

E-Print Network [OSTI]

The purpose of this paper is to test how well numerical calculations can predict transport properties of porous permeable rock, given its 3D digital microtomography (?CT) image. For this study, a Berea 500 sandstone sample ...

Zhan, Xin

124

Altering Wettability in Gas Condensate Sandstone Reservoirs for Gas Mobillity Improvement  

E-Print Network [OSTI]

study on Berea sandstone rocks treated with a fluorinated polymer. Various concentrations of the polymer are investigated to obtain the optimum alteration in wettability to intermediate gas-wet. This wetting condition is achieved with an 8% polymer...

Fernandez Martinez, Ruth Gabriela

2012-07-16T23:59:59.000Z

125

Depositional environment and facies relationships of the Canyon sandstone, Val Verde Basin, Texas  

E-Print Network [OSTI]

units of the Bouma turbi- dit. e sequence. The sequence of sedimentary structures and change in grain size indicate that the Canyon sandstone was deposited from a turbidity current flow. Complete bed sets are present within the cored interval...

Mitchell, Michael Harold

1975-01-01T23:59:59.000Z

126

The effects of composition and bedding on log response, Yowlumne sandstone, Kern County, California  

E-Print Network [OSTI]

southwest of Bakersfield (Figures 3 and 4). Stratigraphy The Yowlumne sandstone is Upper Miocene (Mohnian) in age and is found as an isolated, lenticular body of sand within the Antelope Shale member of the Monterey Formation (Table 1) . Upper Miocene...THE EFFECTS OF COMPOSITION AND BEDDING ON LOG RESPONSE, YOWLUMNE SANDSTONE, KERN COUNTY, CALIFORNIA A Thesis by DAVID WILLIAM FORTNER Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment...

Fortner, David William

1988-01-01T23:59:59.000Z

127

Diagenesis of the Dakota sandstone, West Lindrith Field, Rio Arriba County, New Mexico  

E-Print Network [OSTI]

Christian University Chairman of Advisory Commiuee: Dr, Thomas T. Tieh The Cretaceous Dakota sandstone at West Lindrith Field, Rio Arriba County, New Mexico consists of lenticular sand bodies interstratified with marine shales. The sandstones... rocks which were deposited under diverse marine and non-marine conditions near the southwestern margin of an epicontinental sea that covered much of the western interior (Owen, 1969) (Fig. 3). Local subsidence and major uplifts in the Cordillera...

Franklin, Stanley Powell

1987-01-01T23:59:59.000Z

128

The environment of deposition of the Oligocene Burbank sandstone, Tulare Lake field, Kings County, California  

E-Print Network [OSTI]

THE ENVIRONMENT OF DEPOSITION OF THE OLIGOCENE BURBANK SANDSTONE, TULARE LAKE FIELD, KINGS COUNTY, CALIFORNIA A Thesis by WILLIAM HAACK GOULET Submitted to the Graduate College of Texas A&M University in partial fulfillment... of the requirements for the degree of MASTER OF SCIENCE DECEMBER 1986 Major Subject: Geology THE ENVIRONMENT OF DEPOSITION OF THE OLIGOCENE BURBANK SANDSTONE, TULARE LAKE PIELD, KINGS COUNTY, CALIFORNIA A Thesis by WILLIAM HAACK GODLET Approved as to style...

Goulet, William Haack

1986-01-01T23:59:59.000Z

129

Diagenesis of the Upper Devonian sandstones in Westmoreland County, southwestern Pennsylvania  

E-Print Network [OSTI]

and proximal turbidites were created as a result of different topography at the time of deposition. McCandless (1981) studied the subsurface Bradford sandstones in Indiana, Clearfieid, and Jefferson Counties adjacent to the study area. These sandstones were... are a function of mineralogy, temperature, fluid composition and amount of reactive surface area (Bruton, 1985). Mineral dissolution which releases cations into solution is attributed to a decrease in pH of the pore fluids. For the dissolution...

Zverina, Walter Charles

1989-01-01T23:59:59.000Z

130

Depositional environment of the Bartlesville sandstone, La Harpe field, Allen County, Kansas  

E-Print Network [OSTI]

), and Johnson (1973). These . ,tudies centered on the environment of deposition of the Bartlesville sandstone in central and eastern Oklahoma and central I ansas. Johnson (1973), however, worked in southeast l ansas, south of the La Narpe area... sandstone established by Visher and others (1 971 ) for Oklahoma and extended by Johnson (1 97/) into south Kansas can now be placed in a more regional per- spective. Regional Geology The midcontinental United States changed from ". 'table positive...

Schumacher, Madelyn

2012-06-07T23:59:59.000Z

131

Deposition of the Woodbine-Eagleford sandstones, Aggieland field, Brazos County, Texas  

E-Print Network [OSTI]

. , University of Montana Chair of Advisory Committee: Dr. Robert R. Berg Sandstones of the Upper Cretaceous Woodbine-Eagleford interval produce oil and gas from a stratigraphic trap at Aggieland field . The reservoir has an overall north-south trending... . 110 LIST OF FIGURES Figure Index map of northeast Texas showing major structural features, the location of Aggie- land field and other oil and gas fields which produce from the Woodbine-Eagleford sandstones. Modified from Berg and Leethem (1985...

DeDominic, Joseph Robert

1988-01-01T23:59:59.000Z

132

The geology of the basal sandstone-mudstone unit of the Blackhawk Landslide, Lucerne Valley, California  

E-Print Network [OSTI]

THE GEOLOGY OF THE BASAL SANDSTONE-MUDSTONE UNIT OF THE BLACKHAWK LANDSLIDE, LUCERNE VALLEY, CALIFORNIA A Thesis by JERRY LINN KUZIOR Submitted to the Graduate College of Texas AAM University in partial fulfillment of the requirements... for the degree of MASTER OF SCIENCE December 1983 Major Subject: Geology THE GEOLOGY OF THE BASAL SANDSTONE-MUDSTONE UNIT OF THE BLACKHANK LANDSLIDE, LUCERNE VALLEY, CALIFORNIA A Thesis by JERRY LINN KUZIOR Approved as to style and content by: Brann Jo...

Kuzior, Jerry Linn

1983-01-01T23:59:59.000Z

133

Environment of deposition of the Permian Lyons Sandstone at Black Hollow Field, Weld County, Colorado  

E-Print Network [OSTI]

ENVIRONMENT OF DEPOSITION OF THE PERMIAN LYONS SANDSTONE AT BLACK HOLLOW FIELD, WELD COUNTY, COLORADO A Thesis by DAVID MICHAEL FRANK Submitted to the Graduate College of Texas A&M University in partial fulfillment of the requirement... for the degree of MASTER QF SCIENCE August 1984 Major Subject: Geology ENVIRONMENT OF DEPOSITION OF THE PERMIAN LYONS SANDSTONE AT BLACK HOLLOW FIELD, WELD COUNTY, COLORADO A Thesis by DAVID MICHAEL FRANK Approved as to style and content by: R. R. Berg...

Frank, David Michael

1984-01-01T23:59:59.000Z

134

Depositional environment and reservoir morphology of Canyon sandstones, Central Midland Basin, Texas  

E-Print Network [OSTI]

-1, Burnt Rock field. Letters at right of center column indicate turbi dite divisions . . . . . . . . . . 35 14. Grain size, compostion, and bedding types in Canyon sandstones, 7296-7299 feet, Phillips Petroleum Munn 1-A, Jameson field. Letters at right... divisions. . . . . . . . . . . 37 16. Grain size, composition, and bedding types in Canyon sandstones, 7377-7381 feet, Phillips Petroleum Munn 1-A, Jameson field. Letters at right of center column indicate turbi dite divisions...

Jones, James Winston

1980-01-01T23:59:59.000Z

135

The Chern-Simons diffusion rate from higher curvature gravity  

E-Print Network [OSTI]

An important transport coefficient in the study of non-Abelian plasmas is the Chern-Simons diffusion rate, which parameterizes the rate of transition among the degenerate vacua of a gauge theory. We compute this quantity at strong coupling, via holography, using two theories of gravity with higher curvature corrections, namely Gauss-Bonnet gravity and quasi-topological gravity. We find that these corrections may either increase or decrease the result obtained from Einstein's gravity, depending on the value of the couplings. The Chern-Simons diffusion rate for Gauss-Bonnet gravity decreases as the shear viscosity over entropy ratio is increased.

Viktor Jahnke; Anderson Seigo Misobuchi; Diego Trancanelli

2014-03-13T23:59:59.000Z

136

Even-dimensional topological gravity from Chern-Simons gravity  

E-Print Network [OSTI]

It is shown that the topological action for gravity in 2n-dimensions can be obtained from the 2n+1-dimensional Chern-Simons gravity genuinely invariant under the Poincare group. The 2n-dimensional topological gravity is described by the dynamics of the boundary of a 2n+1-dimensional Chern-Simons gravity theory with suitable boundary conditions. The field $\\phi^{a}$, which is necessary to construct this type of topological gravity in even dimensions, is identified with the coset field associated with the non-linear realizations of the Poincare group ISO(d-1,1).

Nelson Merino; Alfredo Perez; Patricio Salgado

2009-10-08T23:59:59.000Z

137

Chern-Simons terms and cocycles in physics and mathematics  

SciTech Connect (OSTI)

Contemporary topological research in Yang-Mills theory is reviewed, emphasizing the Chern-Simons terms and their relatives. Three applications of the Chern-Simons terms in physical theory are described: to help understanding gauge theories in even dimensional space-time; gauge field dynamics in odd dimensional space-time; and mathematically coherent description of even-dimensional gauge theories with chiral fermions that are apparently inconsistent due to chiral anomalies. Discussion of these applications is preceded by explanation of the mathematical preliminaries and examples in simple quantum mechanical settings. 24 refs. (LEW)

Jackiw, R.

1984-12-01T23:59:59.000Z

138

Dirac matrices for Chern-Simons gravity  

SciTech Connect (OSTI)

A genuine gauge theory for the Poincare, de Sitter or anti-de Sitter algebras can be constructed in (2n- 1)-dimensional spacetime by means of the Chern-Simons form, yielding a gravitational theory that differs from General Relativity but shares many of its properties, such as second order field equations for the metric. The particular form of the Lagrangian is determined by a rank n, symmetric tensor invariant under the relevant algebra. In practice, the calculation of this invariant tensor can be reduced to the computation of the trace of the symmetrized product of n Dirac Gamma matrices {Gamma}{sub ab} in 2n-dimensional spacetime. While straightforward in principle, this calculation can become extremely cumbersome in practice. For large enough n, existing computer algebra packages take an inordinate long time to produce the answer or plainly fail having used up all available memory. In this talk we show that the general formula for the trace of the symmetrized product of 2n Gamma matrices {Gamma}{sub ab} can be written as a certain sum over the integer partitions s of n, with every term being multiplied by a numerical cofficient {alpha}{sub s}. We then give a general algorithm that computes the {alpha}-coefficients as the solution of a linear system of equations generated by evaluating the general formula for different sets of tensors B{sup ab} with random numerical entries. A recurrence relation between different coefficients is shown to hold and is used in a second, 'minimal' algorithm to greatly speed up the computations. Runtime of the minimal algorithm stays below 1 min on a typical desktop computer for up to n = 25, which easily covers all foreseeable applications of the trace formula.

Izaurieta, Fernando; Ramirez, Ricardo; Rodriguez, Eduardo [Departamento de Matematica y Fisica Aplicadas, Universidad Catolica de la Santisima Concepcion, Alonso de Ribera 2850, 4090541 Concepcion (Chile)

2012-10-06T23:59:59.000Z

139

Factors controlling reservoir quality in tertiary sandstones and their significance to geopressured geothermal production  

SciTech Connect (OSTI)

Variable intensity of diagenesis is the factor primarily responsible for contrasting regional reservoir quality of Tertiary sandstones from the upper and lower Texas coast. Detailed comparison of Frio sandstone from the Chocolate Bayou/Danbury Dome area, Brazoria County, and Vicksburg sandstones from the McAllen Ranch Field area, Hidalgo County, reveals that extent of diagenetic modification is most strongly influenced by (1) detrital mineralogy and (2) regional geothermal gradients. The regional reservoir quality of Frio sandstones from Brazoria County is far better than that characterizing Vicksburg sandstones from Hidalgo County, especially at depths suitable for geopressured geothermal energy production. However, in predicting reservoir quality on a site-specific basis, locally variable factors such as relative proportions for porosity types, pore geometry as related to permeability, and local depositional environment must also be considered. Even in an area of regionally favorable reservoir quality, such local factors can significantly affect reservoir quality and, hence, the geothermal production potential of a specific sandstone unit.

Loucks, R.G.; Richmann, D.L.; Milliken, K.L.

1981-01-01T23:59:59.000Z

140

Analysis of borehole temperature data from the Mt. Princeton...  

Open Energy Info (EERE)

Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Paper: Analysis of borehole temperature data from the Mt. Princeton Hot Springs area, Chaffee County,...

Note: This page contains sample records for the topic "mt simon sandstone" 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

Doing political ecology inside and outside the academy Simon Batterbury  

E-Print Network [OSTI]

Doing political ecology inside and outside the academy Simon Batterbury University of Melbourne www.simonbatterbury.net For: Bryant R, ed. 2015. International Handbook of Political Ecology. Edward Elgar. Abstract The chapter presents a survey of political ecology (PE) scholarship in, and beyond, academic institutions

Batterbury, Simon

142

Broadband Photodetector Based on Carbon Nanotube Fibers Simon Lee,1  

E-Print Network [OSTI]

UG-30 Broadband Photodetector Based on Carbon Nanotube Fibers Simon Lee,1 Xuan Wang absorption properties of the carbon nanotube fibers generate a thermal distribution across the length of applications of carbon nanotubes has been constantly expanding since its inception. From being a copper wire

143

University of Applied Sciences Georg-Simon-Ohm Fachhochschule Nurnberg  

E-Print Network [OSTI]

) an der Georg-Simon-Ohm Fachhochschule N¨urnberg C++-Programmiertechniken f¨ur High Performance Computing Access), aber auch manche Multi-Core-Systeme geh¨oren, sind im High Performance Computing (HPC) weit-Optimierung von C++-Code f¨ur High Performance Computing 26 3.1 C

Fiebig, Peter

144

Personal energy metering Simon Hay, Andrew Rice and Andy Hopper  

E-Print Network [OSTI]

based on energy and usage data collected over the course of a year. We also studied the addi- tionalPersonal energy metering Simon Hay, Andrew Rice and Andy Hopper {sjeh3,acr31,ah12}@cam.ac.uk Computer Laboratory, University of Cambridge 1 Introduction Every day each of us consumes a significant

Cambridge, University of

145

DHV water pumping optimization Simon van Mourik1  

E-Print Network [OSTI]

Chapter 6 DHV water pumping optimization Simon van Mourik1 Joris Bierkens2 Hans Stigter1 Martijn for optimizing a drinking water network over a horizon of 48 hours, given variable water demands, energy prices and constraints on the pumping strategy and water levels in the reservoirs. Both the dynamic model and goal

Rottschäfer, Vivi

146

Rainwater-Simons-type convergence theorems for generalized convergence methods  

E-Print Network [OSTI]

We extend the well-known Rainwater-Simons convergence theorem to various generalized convergence methods such as strong matrix summability, statistical convergence and almost convergence. In fact we prove these theorems not only for boundaries but for the more general notion of (I)-generating sets introduced by Fonf and Lindenstrauss.

Hardtke, Jan-David

2010-01-01T23:59:59.000Z

147

Factors controlling reservoir quality in tertiary sandstones and their significance to geopressured geothermal production. Annual report, May 1, 1979-May 31, 1980  

SciTech Connect (OSTI)

Differing extents of diagenetic modification is the factor primarily responsible for contrasting regional reservoir quality of Tertiary sandstones from the Upper and Lower Texas Gulf Coast. Detailed comparison of Frio sandstones from the Chocolate Bayou/Danbury Dome area, Brazoria County, and Vicksburg sandstones from the McAllen Ranch Field area, Hidalgo County, reveals that extent of diagenetic modification is most strongly influenced by (1) detrital mineralogy and (2) regional geothermal gradients. Vicksburg sandstones from the McAllen Ranch Field area are less stable, chemically and mechanically, than Frio sandstones from the Chocolate Bayou/Danbury dome area. Vicksburg sandstones are mineralogically immature and contain greater proportions of feldspars and rock fragments than do Frio sandstones. Thr reactive detrital assemblage of Vicksubrg sandstones is highly susceptible to diagenetic modification. Susceptibility is enhanced by higher than normal geothermal gradients in the McAllen Ranch Field area. Thus, consolidation of Vicksburg sandstones began at shallower depth of burial and precipitation of authigenic phases (especially calcite) was more pervasive than in Frio sandstones. Moreover, the late-stage episode of ferroan calcite precipitation that occluded most secondary porosity in Vicksburg sandstones did not occur significantly in Frio sandstones. Therefore, regional reservoir quality of Frio sandstones from Brazoria County is far better than that characterizing Vicksburg sandstones from Hidalgo County, especially at depths suitable for geopressured geothermal energy production.

Loucks, R.G.; Richmann, D.L.; Milliken, K.L.

1980-07-01T23:59:59.000Z

148

Depositional environment of Woodbine and Eagleford sandstones at OSR-Halliday field, Leon and Madison counties, Texas  

E-Print Network [OSTI]

-3" sandstones were cores approximate'y 230 feet bel w "69-3" sandstones. These thin sandstone units have a ahern bas, 1 contact, are massive at the bottom and rippled or intcrl minated with shales at the top. B'otuzbation is restricted to the tcp o... represents the distributary channel. Fossillferous shales of an irdistributary bay were deposited on top of these sandstones follow- ing abandonment of the channel. A second delta front/distributary channel sequence overlies the interdistributary Lay...

Bukowski, Charles Thomas

1984-01-01T23:59:59.000Z

149

Preliminary statistical analysis and provenance trends in Desmoinesian sandstones from central and eastern Oklahoma  

SciTech Connect (OSTI)

Desmoinesian sandstones from the northeast Oklahoma platform and from the Anadarko and McAlester basins record a complex interaction between mid-Pennsylvanian source-area tectonism and cyclic sedimentation patterns associated with transgressions and regressions. Framework grain summaries for 67 thin sections from sandstones of the Cherokee Group (Bartlesville, Red Fork, Skinner, and Prue) were subjected to multivariate statistical analysis to establish regional compositional trends for provenance analysis. R-mode cluster and correspondence analyses were used to determine the contributing effect (total variance) of key framework grains. Fragments of monocrystalline and polycrystalline quartz, chert, metamorphic rock, and limestone contribute most to the variation in the grain population. Q-mode cluster and correspondence analyses were used to identify three distinct petrofacies. Petrofacies I is rich in monocrystalline quartz (86 to 98%) and contains rare mica and rock fragments. Petrofacies II is also rich in monocrystalline quartz (66 to 86%) and contains as much as 15% metamorphic and sedimentary rock fragments. Petrofacies III is compositionally heterogeneous and contains fragments of polycrystalline and monocrystalline quartz, mica, chert, and metamorphic and sedimentary rocks. Quantitative analyses indicate that Desmoinesian sandstones were derived from complex sedimentary and metamorphic source areas. Petrofacies I sandstones are restricted to the southwestern part of the Anadarko basin and the northeast Oklahoma platform, whereas petrofacies II and III sandstones are distributed throughout the study area. The distribution of petrofacies within the region suggests a model of source-area interaction and cratonic sediment recycling.

Dyman, T.S.

1987-05-01T23:59:59.000Z

150

RAPID/Roadmap/3-MT-e | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExploration JumpSanyalTempWellheadWahkiakumNV-a20-AK-a WellAK-g UtilityHI-dMT-c3-MT-e

151

RAPID/Roadmap/17-MT-c | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, search RAPIDColorado <17-HI-a < RAPID‎ | Roadmap Jump to:7-MT-a7-MT-c

152

Depositional environment of Upper Cretaceous deep Tuscaloosa Sandstones, Profit Island field, east Baton Rouge Parish, Louisiana  

E-Print Network [OSTI]

in thickness from 12 ft to 17 ft (4 m to 5 m). Finally, thin-bedded, distinctly parallel-laminated and ripple-laminated sandstones represent overbank deposits which range in thickness from 4 ft to 9 ft (1 m to 3 m) ~ Black marine shales with thinly... Island field is in the lower Tuscaloosa sandstones. The exact age of the Tuscaloosa has recently been the subj ect of many stratigraphic studies. It has generally been assumed that the 11 deep Tuscaloosa of Louisiana and the Woodbine of East Texas...

Roth, Susan Viola

1981-01-01T23:59:59.000Z

153

Depositional environment and reservoir morphology of Spraberry sandstones, Parks field, Midland County, Texas  

E-Print Network [OSTI]

, structureless sand- stones, very thinly laminated and bioturbated siltstones, and thin black shales. Sandstones are either thick or thin bedded, and vary in thickness from 0. 05 ft (0. 02 m) to 14. 5 ft (4. 4 m). Sandstones average 2. 7 ft (0. 8 m... of a reservoir study at Parks; and Mr. F. E. Hill in Dallas, for providing me with rewarding summer jobs. Mrs. Nina Ronalder, who as the Mobil employee in-charge of the field has been my primary source of data on the Parks field. Finally, I cannot...

Yale, Mark William

1986-01-01T23:59:59.000Z

154

Effect of core length on laboratory displacement of oil by CO? in sandstone  

E-Print Network [OSTI]

EXPECT OP CORE LENGTH ON LABORATORY DISPLACEMENT OP OIL BY C02 IN SANDSTONE A Thesis by KENNETH YUN KWONG CHAN Submitted to the Graduate College of Texas khM University in partial fulfillment of the requirement for the degree of MASTER OP... SCIENCE August 1974 Major Subject: Petroleum Engineering EPACT OP CORE LENGTH ON LABORATORY DISPLACEMENT Oy OIL BY COR IN SANDSTONE A Thesis by KENNETH YUN KWONG CHAN Approved as to style and content by: a an o omm ee ea o Department ember Mem...

Chan, Kenneth Yun-Kwong

1974-01-01T23:59:59.000Z

155

Stratigraphic relationships in Woodbine-Eagleford and Sub-Clarksville sandstones, IDS field, Brazos County, Texas  

E-Print Network [OSTI]

-Clarksville Sandstones, IDS Field, Brazos County, Texas. (August 1990) Ron Lee Brogdon, B. A. , Harvard University Chair of Advisory Committee: Dr. Robert R. Berg Sandstones of the Upper-Cretaceous Woodbine-Eagleford interval produce oil and gas from a small... no influence as a hydrocarbon trap. Production from IDS field, like the extent of the reservoir, is small. Nine years of production from 13 wells have yielded only 584 MBBLS of oil. Production is not uniform across the field, but defines a trend which...

Brogdon, Ron Lee

1990-01-01T23:59:59.000Z

156

Environment of deposition of the upper Jurassic "Gray" sandstones, Terryville field, Lincoln Parish, Louisiana  

E-Print Network [OSTI]

polycrystalline quartz, 0th = other minerals, Nx = matrix. c Sil = silica as grain overgrowths, Cal = calcite. 35 in decreasing amounts from cores S18-1, D20-1, and D19-1. Oolite nucleii are frequently composed of monocrystalline quartz grains and rock... as feldspathic subli- tharenites (Folk, 1974). Sandstones occur in a section of dominant dark shale that has a total thickness of 600 ft (182 m) . Cores exhibit thin sandstone beds with repetit'ous sequences of sedimentary structures and textural grading...

Mani, Philip Charles

1983-01-01T23:59:59.000Z

157

Frictional properties between fine grained limestone, dolomite and sandstone along precut surfaces  

E-Print Network [OSTI]

properties of all the combinations of rocks in contact. Th following are the experimental variables: (1) Angle between cut surface and load axis: 45 0 (2) Confining pressure: 350, 700, 1, 000, 1, 400 bars. -4 (3) Strain-rate: 10 / sec. (4) Temperature... 13 4. 0 P =1 c gl, 00 400 (bars) 700 4. 0 3. 0 700 350 A 350 2. 0 eLO A 2. 0 4. 0 6. 0 Strain (X) Figure 1-a. Stress-strain curves of Tennessee Sandstone against Tennessee Sandstone. 4. 0 2. 0 4. 0 6. 0 Strain (%%d) Figure 1-b...

Iwasaki, Takeshi

1970-01-01T23:59:59.000Z

158

Detrital zircon geochronology from the Cambrian-Ordovician Bliss Sandstone, New Mexico: Evidence for contrasting Grenville-age and  

E-Print Network [OSTI]

Detrital zircon geochronology from the Cambrian-Ordovician Bliss Sandstone, New Mexico: Evidence and Greg H. Mack Department of Geological Sciences, New Mexico State University, Las Cruces, New Mexico-Ordovician Bliss Sandstone in southern New Mexico are used to test models for the influence and signifi- cance

Amato, Jeff

159

Discriminant Analysis of XRF Data from Sandstones of Like Facies and Appearance: A Method for Identifying a Regional Unconformity, Paleotopography,  

E-Print Network [OSTI]

Discriminant Analysis of XRF Data from Sandstones of Like Facies and Appearance: A Method Reserved #12;ABSTRACT Discriminant Analysis of XRF Data from Sandstones of Like Facies and Appearance candidate surfaces. Using statistical discriminant analysis of XRF data, formations bounding an unconformity

Seamons, Kent E.

160

A Remote Controlled Vehicle with Omnidirectional Sensors Simon Lok, Shree K. Nayar  

E-Print Network [OSTI]

PARAROVER A Remote Controlled Vehicle with Omnidirectional Sensors Simon Lok, Shree K. Nayar.8 DC Power System . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 10 2 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 3.2 Electrical

Note: This page contains sample records for the topic "mt simon sandstone" 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

Existence and uniqueness of domain wall solitons in a Maxwell–Chern–Simons model  

SciTech Connect (OSTI)

We present some sharp existence and uniqueness theorems for the domain wall solutions of the basic governing equations of a self-dual Maxwell–Chern–Simons model.

Zhang, Ruifeng [Institute of Contemporary Mathematics, Henan University, Kaifeng 475001 (China) [Institute of Contemporary Mathematics, Henan University, Kaifeng 475001 (China); College of Mathematics and Information Science, Henan University, Kaifeng 475001 (China); Li, Fangfang [College of Mathematics and Information Science, Henan University, Kaifeng 475001 (China)] [College of Mathematics and Information Science, Henan University, Kaifeng 475001 (China)

2014-02-15T23:59:59.000Z

162

Origin of Lower Cretaceous (`Nubian') sandstones of North-east Africa and Arabia from detrital zircon U-Pb SHRIMP dating  

E-Print Network [OSTI]

as widespread sandstone sheets, typically are mineralogically and texturally mature. Previous petrographic contain aerially extensive siliciclastic rock units typically dominated by quartz-rich sandstone older sources (Kolodner et al., 2006). Petrogra- phical examination and detrital zircon geochro- nology

Dov, Avigad

163

Chern-Simons Reduction and non-Abelian Fluid Mechanics  

E-Print Network [OSTI]

We propose a non-Abelian generalization of the Clebsch parameterization for a vector in three dimensions. The construction is based on a group-theoretical reduction of the Chern-Simons form on a symmetric space. The formalism is then used to give a canonical (symplectic) discussion of non-Abelian fluid mechanics, analogous to the way the Abelian Clebsch parameterization allows a canonical description of conventional fluid mechanics.

R. Jackiw; V. P. Nair; So-Young Pi

2000-07-17T23:59:59.000Z

164

Refined Chern-Simons Theory and Topological String  

E-Print Network [OSTI]

We show that refined Chern-Simons theory and large N duality can be used to study the refined topological string with and without branes. We derive the refined topological vertex of hep-th/0701156 and hep-th/0502061 from a link invariant of the refined SU(N) Chern-Simons theory on S^3, at infinite N. Quiver-like Chern-Simons theories, arising from Calabi-Yau manifolds with branes wrapped on several minimal S^3's, give a dual description of a large class of toric Calabi-Yau. We use this to derive the refined topological string amplitudes on a toric Calabi-Yau containing a shrinking P^2 surface. The result is suggestive of the refined topological vertex formalism for arbitrary toric Calabi-Yau manifolds in terms of a pair of vertices and a choice of a Morse flow on the toric graph, determining the vertex decomposition. The dependence on the flow is reminiscent of the approach to the refined topological string in upcoming work of Nekrasov and Okounkov. As a byproduct, we show that large N duality of the refined topological string explains the ``mirror symmetry`` of the refined colored HOMFLY invariants of knots.

Mina Aganagic; Shamil Shakirov

2012-10-09T23:59:59.000Z

165

Continuity and internal properties of Gulf Coast sandstones and their implications for geopressured energy development. Annual report, November 1, 1980-October 31, 1981  

SciTech Connect (OSTI)

Systematic investigation, classification, and differentiation of the intrinsic properties of genetic sandstone units that typify many geopressured geothermal aquifers and hydrocarbon reservoirs of the Gulf Coast region are provided. The following are included: structural and stratigraphic limits of sandstone reservoirs; characteristics and dimensions of Gulf Coast Sandstones; fault compartment areas; comparison of production and geologic estimates of aquifer volume; geologic setting and reservoir characteristics, wells of opportunity; internal properties of sandstones and implications for geopressured energy development. (MHR)

Morton, R.A.; Ewing, T.E.; Tyler, N.

1982-06-01T23:59:59.000Z

166

Strategic Planning Notes MT AHEC/MORH Advisory Board  

E-Print Network [OSTI]

big, complex issues ­ Montana Healthcare Workforce Advisory Committee, HC Workforce Strategic PlanStrategic Planning Notes MT AHEC/MORH Advisory Board February 7, 2014 Strategic Priorities 1. Healthcare Workforce Training and educating the workforce Montana needs o Educational infrastructure o

Dyer, Bill

167

Rock doughnut and pothole structures of the Clarens Fm. Sandstone in the Karoo Basin, South Africa: Possible links to Lower Jurassic fluid seepage  

E-Print Network [OSTI]

Rock doughnut and pothole structures of the Clarens Fm. Sandstone in the Karoo Basin, South Africa, Archaeology & Environmental Studies, University of the Witwatersrand, P/Bag 3, WITS 2050, South Africa b Morphology Process origins Clarens Fm. Sandstone South Africa has a wealth of sandstone landforms, yet many

Svensen, Henrik

168

SEISMIC ANISOTROPY IN TIGHT GAS SANDSTONES, RULISON FIELD, PICEANCE BASIN, COLORADO  

E-Print Network [OSTI]

a quarter of the proven natural gas reserves in the United States. Rulison Field, located in the PiceanceSEISMIC ANISOTROPY IN TIGHT GAS SANDSTONES, RULISON FIELD, PICEANCE BASIN, COLORADO by Gerardo J-based rock physics to estimate the seismic anisotropy of the tight gas reservoir at Rulison Field. Seismic

169

Permeability characterization of shear zones in the Hickory sandstone member, Riley Formation, Texas  

E-Print Network [OSTI]

. The main objectives of this work are to (1) characterize the geometry and permeability of deformation elements within shear zones; (2) determine permeability anisotropy in shear zones according to fault characteristics and host lithology; and (3) develop... I INTRODUCTION .............................................................................................1 II HICKORY SHEAR ZONES AND DEFORMATION ELEMENTS..............11 2.1 Shear Zones in Hickory Sandstone Member...

Nieto Camargo, Jorge Enrique

2005-02-17T23:59:59.000Z

170

Three-dimensional seismic stratigraphic study of downdip Yegua sandstones, Edna Field, Jackson County, Texas  

E-Print Network [OSTI]

This study reports an investigation of the structure and stratigraphy of the downdip Yegua sandstones at Edna Field, Jackson County, South Texas. The study is based on 22.9 square miles of three dimensional (3-D) seismic data, well-logs from 15...

Trikania, Andra

1996-01-01T23:59:59.000Z

171

Further Investigation of Fluoboric Acid in Sandstone Acidizing Using ^(11)B and ^(19)F NMR  

E-Print Network [OSTI]

Although fluoboric acid (HBF_(4)) has long been known as one of the low-damaging acid treatments for clayey sandstone formations, little is known of its chemistry which could explain the mixed results of fluoboric acid in actual field application. A...

Pituckchon, Arpajit

2014-05-01T23:59:59.000Z

172

Effect of fluid rheology on enhanced oil recovery in a microfluidic sandstone device  

E-Print Network [OSTI]

recovery with that secondary fluid alone. These results clearly demonstrate that the microfluidic sandstone oil in the field will have been recov- ered [1]. The secondary stage of oil recovery is characterized of the oil being recovered [1]. After primary and secondary oil recovery techniques have been exhausted

Rothstein, Jonathan

173

Reservoir heterogeneity in Carter Sandstone, North Blowhorn Creek oil unit and vicinity, Black Warrior Basin, Alabama  

SciTech Connect (OSTI)

This report presents accomplishments made in completing Task 3 of this project which involves development of criteria for recognizing reservoir heterogeneity in the Black Warrior basin. The report focuses on characterization of the Upper Mississippian Carter sandstone reservoir in North Blowhorn Creek and adjacent oil units in Lamar County, Alabama. This oil unit has produced more than 60 percent of total oil extracted from the Black Warrior basin of Alabama. The Carter sandstone in North Blowhorn Creek oil unit is typical of the most productive Carter oil reservoirs in the Black Warrior basin of Alabama. The first part of the report synthesizes data derived from geophysical well logs and cores from North Blowhorn Creek oil unit to develop a depositional model for the Carter sandstone reservoir. The second part of the report describes the detrital and diagenetic character of Carter sandstone utilizing data from petrographic and scanning electron microscopes and the electron microprobe. The third part synthesizes porosity and pore-throat-size-distribution data determined by high-pressure mercury porosimetry and commercial core analyses with results of the sedimentologic and petrographic studies. The final section of the report discusses reservoir heterogeneity within the context of the five-fold classification of Moore and Kugler (1990).

Kugler, R.L.; Pashin, J.C.

1992-05-01T23:59:59.000Z

174

Z .Chemical Geology 152 1998 257271 The thermal and cementation histories of a sandstone petroleum  

E-Print Network [OSTI]

Z .Chemical Geology 152 1998 257­271 The thermal and cementation histories of a sandstone petroleum of the cement formed, the maturation of petroleum in the interbedded shales likely postdates cementation. q 1998 of partially cemented petroleum reservoirs may help in constraining the physical character of a reservoir

175

Mineral Sequestration of Carbon Dixoide in a Sandstone-Shale System  

SciTech Connect (OSTI)

A conceptual model of CO2 injection in bedded sandstone-shale sequences has been developed using hydrogeologic properties and mineral compositions commonly encountered in Gulf Coast sediments. Numerical simulations were performed with the reactive fluid flow and geochemical transport code TOUGHREACT to analyze mass transfer between sandstone and shale layers and CO2 immobilization through carbonate precipitation. Results indicate that most CO2 sequestration occurs in the sandstone. The major CO2 trapping minerals are dawsonite and ankerite. The CO2 mineral-trapping capacity after 100,000 years reaches about 90 kg per cubic meter of the medium. The CO2 trapping capacity depends on primary mineral composition. Precipitation of siderite and ankerite requires Fe+2 supplied mainly by chlorite and some by hematite dissolution and reduction. Precipitation of dawsonite requires Na+ provided by oligoclase dissolution. The initial abundance of chlorite and oligoclase therefore affects the CO2 mineral trapping capacity. The sequestration time required depends on the kinetic rate of mineral dissolution and precipitation. Dawsonite reaction kinetics is not well understood, and sensitivity regarding the precipitation rate was examined. The addition of CO2 as secondary carbonates results in decreased porosity. The leaching of chemical constituents from the interior of the shale causes slightly increased porosity. The limited information currently available for the mineralogy of natural high-pressure CO2 gas reservoirs is also generally consistent with our simulation. The ''numerical experiments'' give a detailed understanding of the dynamic evolution of a sandstone-shale geochemical system.

Xu, Tianfu; Apps, John A.; Pruess, Karsten

2004-07-09T23:59:59.000Z

176

Depositional environment of Oligocene Hackberry sandstones, Hilde brandt Bayou area, Jefferson County, Texas  

E-Print Network [OSTI]

km) from the Hilde- brandt Bayou area, and the Hartburg flexure may have represented the Oligocene shelf-edge as proposed for other flexures in the Gulf Coast. It is possible that all Hackberry sandstones have a turbi di ty- flow origin...

Powers, Brian Kennett

1980-01-01T23:59:59.000Z

177

Geochemical anomalies in soil and sandstone overlying the Phoenix uranium deposit, Athabasca Basin Natural Resources  

E-Print Network [OSTI]

Co Mo Ni UU Geochemical anomalies in soil and sandstone overlying the Phoenix uranium deposit, Athabasca Basin Natural Resources Canada Geological Survey of Canada with Provincial and Territorial Collaboration Introduction The Wheeler River Property, host of Denison Mine's Phoenix uranium deposit

178

Evidence of uranium biomineralization in sandstone-hosted roll-front uranium deposits, northwestern China  

E-Print Network [OSTI]

Evidence of uranium biomineralization in sandstone-hosted roll-front uranium deposits, northwestern Available online 25 January 2005 Abstract We show evidence that the primary uranium minerals, uraninite-front uranium deposits, Xinjiang, northwestern China were biogenically precipitated and psuedomorphically

Fayek, Mostafa

179

Broadband marine MT exploration of the East Pacific Rise at 9500 Kerry Key and Steven Constable  

E-Print Network [OSTI]

Broadband marine MT exploration of the East Pacific Rise at 9°°500 N Kerry Key and Steven Constable., and S. Constable, Broadband marine MT exploration of the East Pacific Rise at 9°500 N, Geophys. Res

Key, Kerry

180

Hydrodynamic flow in lower cretaceous muddy sandstone, Gas Draw field, Powder River basin, Wyoming  

SciTech Connect (OSTI)

Lower Cretaceous Muddy sandstones form a simple stratigraphic trap at Gas Draw field, northeast Power River Basin. The Muddy at Gas Draw can be subdivided into six zones. The lowest, sixth Muddy sandstone is fluvial in origin, and the overlying fifth sandstone is a transgressive marine deposit. The fourth zone represents a fluvial origin below to shallow marine above. The third zone is interpreted to be of fluvial-overbank origin with possibly a bay-lagoonal association. The second sandstone is suggested to be a deposit of a fluvial or deltaic environment. The first zone was deposited in a lagoonal and poorly-drained marsh environment. At Gas Draw, the second Muddy sandstone is the major producing zone and has the highest average porosity and permeability of 22.6% and 209 md. It had high initial production rates of up to 1200 BOPD (191 m/sup 3//day). From correlation of well logs, the Muddy reservoirs appear to be separated by thin shales, but analysis of drill stem tests show that these reservoirs are connected at some points within the area. Analysis of drill-stem test pressures provides the basis for interpreting fluid potential relationships. The average potentiometric gradient of 32 ft/mi across the field results in a hydrodynamic oil column of 210 feet, whereas capillary-pressure differences due to permeability changes can account for only 38 feet of oil column. The observed oil column over most of the field has a height somewhat greater than 250 feet which agrees well with total calculated oil column of about 248 feet. Furthermore, local decrease in permeability to oil may be responsible for water production at any place within the field, even updip from the producing area.

Lin, J.T.C.

1981-10-01T23:59:59.000Z

Note: This page contains sample records for the topic "mt simon sandstone" 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.


181

Page 1 of 4 Policy R50.03 SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

of Simon Fraser University. They are valued members of the community, who may be funded through fellowships of designation by others or their source of funding. This Policy does not apply to University Research AssociatesPage 1 of 4 Policy R50.03 SIMON FRASER UNIVERSITY Policies and Procedures Date October 26, 2000

182

Constitution of the Interactive Arts and Technology Student Union of the Simon Fraser Student Society  

E-Print Network [OSTI]

Society May 12, 2010 Article 1 ­ Name The name of the Union shall be the "Interactive Arts and Technology of Interactive Arts and Technology, the University, the Simon Fraser Student Society (hereinafter referredConstitution of the Interactive Arts and Technology Student Union of the Simon Fraser Student

183

Industrial Research Chair in Energy Systems for Smart Cities SIMON FRASER UNIVERSITY, CANADA  

E-Print Network [OSTI]

Industrial Research Chair in Energy Systems for Smart Cities SIMON FRASER UNIVERSITY, CANADA energy, as well as any other renewable energy sources and related technology in alignment The Faculty of Applied Sciences at Simon Fraser University, British Columbia, Canada, invites applications

184

Going-to-the-Sun Road, Glacier National Park, MT, USA  

E-Print Network [OSTI]

Going-to-the-Sun Road, Glacier National Park, MT, USA Avalanche Path Atlas Erich H. Peitzsch Daniel..................................................................................................................................... 2 Overview of Red Rock Group avalanche paths, Going-to-the-Sun Road, Glacier National Park, MT................................................................................................................................................... 3 Overview of Lower GTSR group avalanche paths, Going-to-the-Sun Road, Glacier National Park, MT

185

Depositional environment and hydrodynamic flow in Guadalupian Cherry Canyon sandstone, West Ford and West Geraldine fields, Delaware Basin, Texas  

E-Print Network [OSTI]

. Composition, texture and sedimentary structur es in the B1 and B2 sandstones, Conoco G. E. Ramsey 46-16, 3479-3537 ft, Geraldine field. Letters at the right of center column indicate turbidite divisions 31 12. Burial diagenesis of Cherry Canyon sandstones..., permeability and fluid saturations in the 81 and 82 intervals, Conoco G. E. Ramsey 46-16, Geraldine field 58 25. Secondary porosity in Cherry Canyon sandstones, Conoco G. E. Ramsey 14-3, Conoco G. E. Ramsey 22-3, and Conoco G. E. Ramsey 46-1 6, West For d...

Linn, Anne Marie

1985-01-01T23:59:59.000Z

186

Origin of upper Bell Canyon Reservoir Sandstones (Guadalupian), El Mar and Paduca Fields, Southeast New Mexico and West Texas  

E-Print Network [OSTI]

210 ft at El Mar and 120 ft at Paduca. Core examination shows that oil production comes primarily from massive sandstones having a gross thickness of over 70 ft. Single beds have a maximum thickness of 6 ft. These massive sandstones are interbedded... with organic-rich shales only 1/8 to 1 in. thick. Within non-producing sections, lithology is dominated by interlaminated siltstones and shales which are commonly bioturbated. The distribution of sandstones is in channel-like trends per- pendicular...

Weinmeister, Marcus Paul

1978-01-01T23:59:59.000Z

187

Static Length Scales of N=6 Chern-Simons Plasma  

E-Print Network [OSTI]

Using gravity description, we compute various static length scales of N=6 Chern Simons plasma in a strongly coupled regime. For this, we consider the CP3 compactification of the type IIA supergravity down to four dimensions, and identify all the low-lying bosonic modes up to masses corresponding to the operator dimension 3 together with all the remaining CP3 invariant modes. We find the true mass gap, the Debye screening mass and the corresponding dual operators to be probed in the field theory side.

Dongsu Bak; Kazem Bitaghsir Fadafan; Hyunsoo Min

2010-04-19T23:59:59.000Z

188

The effects of chemical environment on the frictional properties of a quartzose sandstone  

E-Print Network [OSTI]

=0. 2 M pH=7 0 1 3 4 5 6 7 6 9 10 11 12 13 PERCENT AXtAL STRAlN Figure 9. Stress-strain curves for Tennessee Sandstone deformed nominally dry and in Na, SO4 solutions of pH 7 with ionic strengths of 0. 2 M. 1. 0 M, and 4. 3 M. 70 60 50 8 4Q I... for Tennessee Sandstone deformed nominally dry and in CaCI, solutions of pH 7 with ionic strengths of 0. 2 M. 1. 0 M, and 5. 0 M. 70 60 50 40 30 z 20 Q 10 I/ -"-- Nominally Dry ? NaCI I=5. 0 N ? --- CaCl. 1=5. 0 N ? ? Na, SO4 1=4. 3 N 0 1 2 3 4 5...

Feucht, Lynn Janet

2012-06-07T23:59:59.000Z

189

Core analysis in a low permeability sandstone reservoir: Results from the Multiwell Experiment  

SciTech Connect (OSTI)

Over 4100 ft (1100 ft oriented) of Mesaverde core was taken during the drilling of the three Multiwell Experiment (MWX) wells, for study in a comprehensive core analysis program. This core traversed five separate depositional environments (shoreline/marine, coastal, paludal, fluvial, and paralic), and almost every major sand in the Mesaverde at the site was sampled. This paper summarizes MWX core analysis and describes the petrophysical properties at the MWX site; reservoir parameters, including permeabilities of naturally fractured core; and mechanical rock properties including stress-related measurements. Some correlations are made between reservoir properties and mineralogy/petrology data. Comparisons are made between the properties of lenticular and blanket sandstone morphologies existing at the site. This paper provides an overview of a complete core analysis in a low-permeability sandstone reservoir. 66 refs., 17 figs. , 9 tabs.

Sattler, A.R.

1989-04-01T23:59:59.000Z

190

Variations in permeability and fine particle migrations in unconsolidated sandstones submitted to saline circulations  

SciTech Connect (OSTI)

Samples of unconsolidated clayey sandstone were submitted to percolations with NaCl and CaCl{sub 2} solutions with ionic strengths I = 0.01 and I = 2 at 20, 60 and 90{degrees}C. The permeability decreased as a function of time for all the samples examined. When the temperature rose from 20 to 90{degrees}C, permeability decreased for the I = 0.01 solutions, but it increased for the I = 2 solutions. The fluid circulations were accompanied by an entrainment of fine particles that was all the greater as the solutions became more diluted and fluid. This behavior, explained by the phenomenon of clay flocculation-deflocculation, is governed by the values of the attraction and repulsion potentials between particles. The calculation of the forces present shows that the electrokinetic phenomena govern flocculation and migration of fine particles in sandstone.

Baudracco, J. (Univ. Paul Sabatier, Lab. de Mineralogie, U.A. 67, 39 Allees Jules Guesde, F-31400 Toulouse (FR))

1990-01-01T23:59:59.000Z

191

Hydrogeologic characterization of the Hickory Sandstone Aquifer near Camp Air in northern Mason and southern McCulloch counties, Texas  

E-Print Network [OSTI]

Hickory Sandstone is the primary source of ground water for the Western Uano Region of Central Texas. Irrigation from the Hickory Aquifer has been intensive for the past 15 years. Available hydrogeologic data for development of a management model... are very limited. Localized detailed studies of the spatial and temporal variations within the aquifer were conducted to provide data for characterization of the ground-water flow system. Field investigations of the Hickory Sandstone included geologic...

Delaney, Cynthia Daphine

1990-01-01T23:59:59.000Z

192

Authigenic clay minerals in sandstones of the Delaware Mountain Group: Bell Canyon and Cherry Canyon Formations, Waha Field, West Texas  

E-Print Network [OSTI]

AUTHIGENIC CLAY MINERALS IN SANDSTONES OF THE DELAWARE MOUNTAIN GROUP: BELL CANYON AND CHERRY CANYON FORMATIONS, WAHA FIELD, WEST TEXAS A Thesis by SUZETTE DENISE WALLING Submitted to the Office of Graduate Studies of Texas A&M University... in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 1992 Major Subject: Geology AUTHIGENIC CLAY MINERALS IN SANDSTONES OF THE DELAWARE MOUNTAIN GROUP: BELL CANYON AND CHERRY CANYON FORMATIONS, WAHA FIELD, WEST TEXAS...

Walling, Suzette Denise

1992-01-01T23:59:59.000Z

193

Geometry and continuity of fine-grained reservoir sandstones deformed within an accretionary prism - Basal Unit, West Woodbourne  

E-Print Network [OSTI]

be difficult to distinguish reservoir from non-reservoir intervals in successions of thinly interbedded sandstones and shales using conventional well logs; (3) There is limited outcrop analogue data that could be used to estimate the geometry and lateral... the depositional geometry and continuity of deep-water reservoir sandstones within the Basal Unit of the Scotland Formation in Woodbourne Trough, beneath Barbados. Observations in the study area were combined with observations of local outcrops of the Scotland...

Blackman, Ingrid Maria

2004-09-30T23:59:59.000Z

194

Diagenesis of Woodbine and Sub-Clarksville sandstones at the Kurten and Iola field areas, Brazos and Grimes Counties, Texas  

E-Print Network [OSTI]

Diagenesis of Woodbine' and Sub-Clarksville Sandstones at the Kurten and Iola Field Areas, Brazos and Grimes Counties, Texas A Thesis by MICHAEL LOUIS FROSSARD Submitted to the Graduate College of Texas A&M University in partial fulfillment... of the requirement for the degree of MASTER OF SCIENCE December 1982 Major Subject: Geology DIAGENESIS OF WOODBINE AND SUB-CLARKSVILLE SANDSTONES AT THE KURTEN AND IOLA FIELD AREAS, BRAZOS AND GRIMES COUNTIES, TEXAS A Thesis by MICHAEL LOUIS FROSSARD...

Frossard, Michael Louis

1982-01-01T23:59:59.000Z

195

Facies, depositional environments, and reservoir properties of the Shattuck sandstone, Mesa Queen Field and surrounding areas, southeastern New Mexico  

E-Print Network [OSTI]

iii FACIES, DEPOSITIONAL ENVIRONMENTS, AND RESERVOIR PROPERTIES OF THE SHATTUCK SANDSTONE, MESA QUEEN FIELD AND SURROUNDING AREAS, SOUTHEASTERN NEW MEXICO A Thesis by JARED BRANDON HAIGHT Submitted to the Office... PROPERTIES OF THE SHATTUCK SANDSTONE, MESA QUEEN FIELD AND SURROUNDING AREAS, SOUTHEASTERN NEW MEXICO A Thesis by JARED BRANDON HAIGHT Submitted to Texas A&M University in partial fulfillment of the requirements for the degree...

Haight, Jared

2004-09-30T23:59:59.000Z

196

Depositional environment of lower Green River Formation sandstones (Eocene), Red Wash field (Uinta Basin), Uintah County, Utah  

E-Print Network [OSTI]

DFPOSITIONAL FNVIRONMENT OF LOWER GREEN RIVER FORMATION SANDSTONES (EOCENE), RED WASH FIELD (UINTA BASIN), UINTAH COUNTY, UTAH A Thesis by ANTHONY SCOTT MCCLAIN Submitted to the Graduate College of Texas AAM University in partial fulfillment... of the requirements for the degree of MASTER OF SCIENCE May 1985 Major Subject: Geology OPPOSITIONAL ENVIRONMENT OF LOWFR BPEEN RIVER FORMATION SANDSTONES (EOCFNE. ), RED WASH FIELD (UINTA BASIN), UINTAH COUNTY, UTAH A Thesis by ANTHONY SCOTT MCCLAIN Approved...

McClain, Anthony Scott

1985-01-01T23:59:59.000Z

197

Depositional environment and reservoir characteristics of the upper Frio sandstones, Willamar field, Willacy County, Texas  

E-Print Network [OSTI]

that are fine to very fine grained. Grain size within bedsets fines upward from 0. 12 mm at the hase to 0. 04 mm at the top. The sandstones contain ~pal ~ of monocrystalline quartz, feldspars and rock fza~ encl are classified as lithic arkoses...~cos ichnofacies, and exhibits intense churning of the sediment ~ rapid, intermittent turbidite deposition. Turbidity currents, initiated by tropical storms, brought fine to very fine grained sediment from an up-dip deltaic source, down topographic laws across...

Caram, Hector Luis

1988-01-01T23:59:59.000Z

198

Environment of deposition of the Pennsylvanian Bartlesville Sandstone, Labette County, Kansas  

E-Print Network [OSTI]

were available for study. Published reports on the Bartlesville Sandstone in Kansas, Missouri, and Oklahoma (Bass, 1936, Howe, 1956j Weirich, 1953; Hayes, 1963; Pharos, 1969; Visher, Saitta B. and Phares, 1971) provided additional information..., with the Chautauqua Arch forming a connection between the two uplifts (Figure 2). By Late Devonian time the Chautaugua Arch was no longer active, Eastern Kansas was divided by the Bourbon Arch into the Forest City and Cherokee Basins in Late Mississippian time...

Johnson, Charles Truman Lars

1973-01-01T23:59:59.000Z

199

Depositional setting, structural style, and sandstone distribution in three geopressured geothermal areas, Texas Gulf Coast  

SciTech Connect (OSTI)

Three areas in the Texas Gulf Coast region with different depositional settings, structural styles, and sandstone distribution were studied with well log and seismic data to evaluate some of the controls on subsurface conditions in geopressured aquifers. Structural and stratigraphic interpretations were made primarily on the basis of well log correlations. Seismic data confirm the log interpretations but also are useful in structure mapping at depths below well control.

Winker, C.D.; Morton, R.A.; Ewing, T.E.; Garcia, D.D.

1981-10-01T23:59:59.000Z

200

Identification of Pore Structure and Clay Content from Seismic Data within an Argillaceous Sandstone Reservoir  

E-Print Network [OSTI]

IDENTIFICATION OF PORE STRUCTURE AND CLAY CONTENT FROM SEISMIC DATA WITHIN AN ARGILLACEOUS SANDSTONE RESERVOIR A Thesis by ROBERT LELAND SCHELSTRATE Submitted to the Office of Graduate and Professional Studies of Texas A&M University... Ds Compressibility of the rock matrix Dd Compressibility of the dry rock frame Df Compressibility of the pore-filling fluid F, FK Frame flexibility factors kd Bulk modulus of dry rock Ks Bulk modulus of the rock...

Schelstrate, Robert

2014-08-11T23:59:59.000Z

Note: This page contains sample records for the topic "mt simon sandstone" 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

Hydrodynamic flow in Lower Cretaceous Muddy Sandstones, Rozet Field, Powder River Basin, Wyoming  

E-Print Network [OSTI]

/km) across the field yields a hydrodynamic oil column of 420 ft (128 m). Capillary pressure differences due to permeability changes account for a oil column of 72 ft (42 m). The combined capillary and hydrodynamic oil columns of 492 ft (150 m) compares... and other Muddy Formation oil fields. Contour interval 1000 ft (305 m). . . Regional east-west cross section showing variable sandstone development in the Muddy interval from Kitty to Rozet Fields. . . . . . . . . Diagrammatic environments the northern...

Smith, David Arthur

1984-01-01T23:59:59.000Z

202

The effect of various mud filtrates on the permeability of sandstone cores  

E-Print Network [OSTI]

' or the Degree of MASTER OF SCIENCE August, 1954 MAJOR SUBJECT: PETROLEUM ENGINEERING THE EFFECT OF VARIOUS MUD FILTRATES ON THE PERMEABILITY OF SANDSTONE CORES A Thesis By Robert A. Pfile Appr ved as to styIe and content by: (Chairman of mmittee... kind and amount of clay contained in the different cores. INTRODUCTION There is general agreement among members of the petroleum industry that the productive capacity of a well penetrating a clay- containing oil sand may be seriously impaired due...

Pfile, Robert Ambrose

1954-01-01T23:59:59.000Z

203

Depositional environment and reservoir morphology of the Frio sandstones, Nine Mile Point Field, Aransas County, Texas  

E-Print Network [OSTI]

of Department (M August 1976 Depositional Environment and Reservoir Norphology of the Frio Sandstones, N1ne Nile Point Field, Aransas County~ Texas (August 1975) ~ Rains Rae Powell~ B, S? ~ Stephen F Austin State University Ch~ of Advisory Caamitteee Dr...), massive and laminated (AB) ~ and laminated only (B) divisions characterize the Frio, Bedsets are of'ten separated by middle-neritic, h1oturbated shales (E), and occasionally a rippled (C) and finely laminated (D) division are present A and AB bedsets...

Powell, Raina Rae

1976-01-01T23:59:59.000Z

204

Properties of natural gas reservoirs in Cotton Valley sandstones, northwest Louisiana  

E-Print Network [OSTI]

th) n sections using luminescence petrography (Sippel, 196R ), and in small fractured specimens under the scanning elec- tron microscope. Luminescence petrography was used to distinguish authigenic quartz from detrital quartz and to determine... of Davis sandstone, Tenneco Osby, illustrating a quartz surface possibly etched by calcite cement. The calcite was removed by HCl before viewing (9203). Bar represents 10 micr ometers. 53 54 results in triangular pore shapes (Figure 20C). Under...

Sonnenberg, Stephen Arnold

1975-01-01T23:59:59.000Z

205

Texture and mineralogy of the Upper Gambrian Welge sandstone, Central Mineral region, Texas  

E-Print Network [OSTI]

region of Texas. Textural and mineralogical characteristics were determined f'rom outcrop samples collected at, ten sections throughout the Central Mineral region. These were combined with f'ield observations to provide a means of interpreting... the environmental conditions and the direction of the source area with respect to the location of the ten sections during the time of Welge deposition. The Welge sandstone fs characterised by both areal and vertical homofeneity of sedimentary parameters, grain...

Hooks, James Edward

1961-01-01T23:59:59.000Z

206

Depositional environment of jurassic smackover sandstones, Thomasville field, Rankin County, Mississippi  

E-Print Network [OSTI]

of an ancient oil pool. Heat and burial cracked the oil, releasing the lighter, more volatile fractions and leaving a residue of pyrobitumen and heavy oil. On the basis of log character, it is possible to dis- tinguish between most sandstones, limestones... in the grammatical and quantitative editing of the manuscript. Hunt Energy Corporation provided funding, cores, and valuable information on Thomasville field. Hunt's aid to this study is greatly appreciated. Alan Thomson's (Shell Oil Co. ) comments on various...

Olsen, Rebecca Sarah Penfield

1980-01-01T23:59:59.000Z

207

Depositional environment of Upper Devonian sandstones in Westmoreland County, southwestern Pennsylvania  

E-Print Network [OSTI]

standard microscopic techniques. Composition was determined for each thin section by using 100 point counts. Mean size was determined from long axis measurement of 100 monocrystalline quartz grains in each thin section. The rock properties as determined... quartz to monocrystalline quartz to increase with increasing grain size. This relationship is demonstrated by a sample from the Bayard Sandstone (2544. 6) in which the amount of polycrystalline quartz is 41% of the total quartz and the mean grain...

McGee, Patricia Ann

1985-01-01T23:59:59.000Z

208

Petrography and prediction of reservoir rock properties in the Sussex Sandstone, Powder River Basin, Wyoming  

E-Print Network [OSTI]

to determine rock composition and texture. Composition was established by point count of 100 grains. Framework grains were identified and counted as monocrystalline quartz, polycrystalline quartz, volcanic rock fragments, potassium feldspar, plagioclase... and quiet water deposition of shale was resumed. The sandstone is classified as a volcanic aronite based on a det: ital composition averaging 59 percent quartz, including both monccrystalline and polycrystalline varieties, 18 percent rock frag- ments...

Shirley, Richard Hoyt

1977-01-01T23:59:59.000Z

209

Depositional environments of Lower Cretaceous Muddy Sandstones, Recluse area, Campbell County, Wyoming  

E-Print Network [OSTI]

log plotted in conjunction with compositional and textural analysis 17 18 Pan American Norfolk No. A-2 electrical log plotted in conjunction with compositional and textural analysis Arco Heard Federal No. 6 electric log plotted in conjunction... structures and bedding. A core from the Arco Bow and Arrow No. 3 well (NW SE Sec. 25, T. 75N. , R. 75W. ) illustrates the characteristics of two reser- voirs, the fifth and sixth Muddy sandstones. The sixth Muddy is characterized by cross laminations...

Stoudt, David Luther

1974-01-01T23:59:59.000Z

210

Depositional environment of woodbine sandstones, Polk, Tyler and San Jacinto Counties, Texas  

E-Print Network [OSTI]

. . . . . . . . . . . . . . . . . . . . . . . . . 73 INTRODUCTION Prior to 1969, oil and gas production from Woodbine sandstones in Texas was restricted to updip areas well north of San Jacinto, Polk, and Tyler Counties (Figure 1). These older Woodbine reservoirs have been interpreted as fluvial... of oil in degrees API c. SITP = shut-in tubing pressure (pounds per square in. ) BHSIP = bottom hole shut-in pressure (pounds per square in. ) 22 while wells in the Seven Oaks field are normally pressured. Accord- ing to Kiatta (1974), Hortense...

Foss, Deane Campbell

1978-01-01T23:59:59.000Z

211

Geological characterization of a sandstone reservoir in Eastern Kansas: Savonburg NE field, Allen County, Kansas  

SciTech Connect (OSTI)

Production on the Nelson leases of the Savonburg NE oil field in eastern Kansas is from sandstone that is part of the fill of a paleovalley that was eroded after deposition of the Tebo coal but before deposition of the Scammon coal. Sandstone in this interval is called the Chelsea Sandstone; the interval is referred to as the Skinner interval. (That interval is part of the Cabaniss Formation, Cherokee Group, and assigned to the Desmoinesian stage of the Middle Pennsylvanian). In addition to determining the stratigraphic relationships of the reservoir, geological characterization helped to understand the distribution of the most productive areas of the field and led to specific recommendations for abandonment of wells, workovers, well treatments, well conversions from producers to injectors, and drilling of new wells, all with the aim of increasing productivity and decreasing costs for the operator. The reservoir characterization used information routinely gathered in the course of oil field operations in eastern Kansas. Gamma-neutron logs indicated lithology as well as stratigraphy, while core descriptions provided insight into stratigraphic distinctions and depositional processes. Core analysis of porosity, permeability, and fluid saturations permitted depiction of the distribution of such attributes throughout the productive region. Key geological concepts of regional marker intervals and incised valley fills provided the theoretical framework for analyzing the reservoir.

Walton, A.W.; Beaty, D.S.

1995-12-31T23:59:59.000Z

212

Depositional framework and reservoir distribution of Red Fork sandstone in Oklahoma  

SciTech Connect (OSTI)

The Middle Pennsylvanian Red Fork sandstone formed as a result of southward progradation across most of Oklahoma. The Red Fork is one of several cyclothemic (transgressive-regressive) sequences developed within the Desmoinesian Cherokee Group. Sea level changes and stability of the depositional area were dominant factors in determining the general stratigraphic characteristics of the Red Fork interval. Progradation was episodic, with sand deposition in the distal, more subsident part of the basin during lower sea level stands, and valley-fill deposition in the more stable areas during sea level rises. Red Fork sandstone trends depict an alluvial-deltaic complex covering most of Oklahoma. The Red Fork consists primarily of alluvial-valley and plain (fluvial) bodies in the northern part of northeastern Oklahoma, alluvial-deltaic bodies in most of the remaining parts of the shelf area, and off-shelf submarine-fan and slope/basin-floor complexes within the deeper part of the Anadarko basin. Determination of reservoir trend and genesis requires integration of rock data and log data, with logs calibrated to cores for estimating depositional environments and assessing diagenetic overprints. Much of the oil and gas has been trapped in stratigraphic traps, some of which represent channelized sandstones with trends at high angles to the structural grain. Secondary chlorite, in particular, is associated locally with development of productive reservoirs showing microporosity, high water saturation, and correspondingly low resistivities.

Shelton, J.W.; Fritz, R.D.; Johnson, C. (Masera Corp., Tulsa, OK (USA))

1989-08-01T23:59:59.000Z

213

Mt St Helens Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia: Energy Resources Jump to:46 -Energieprojekte3 ClimateSpurr GeothermalCarmel Public Utility Co JumpRanierMt St

214

RAPID/Roadmap/11-MT-c | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExploration JumpSanyalTempWellheadWahkiakum CountyPzero-FD-b BLM Land1-MT-c Cultural

215

RAPID/Roadmap/14-MT-c | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExploration JumpSanyalTempWellheadWahkiakum CountyPzero-FD-b34-HI-b4-MT-c Underground

216

RAPID/Roadmap/14-MT-d | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExploration JumpSanyalTempWellheadWahkiakum CountyPzero-FD-b34-HI-b4-MT-c

217

RAPID/Roadmap/17-MT-b | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExploration JumpSanyalTempWellheadWahkiakumNV-a Nonpoint7-FD-a Wild & Scenic7-MT-b

218

RAPID/Roadmap/3-MT-c | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExploration JumpSanyalTempWellheadWahkiakumNV-a20-AK-a WellAK-g UtilityHI-dMT-c State

219

RAPID/Roadmap/3-MT-d | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExploration JumpSanyalTempWellheadWahkiakumNV-a20-AK-a WellAK-g UtilityHI-dMT-c

220

RAPID/Roadmap/5-MT-a | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExplorationUT-g Grant of Access Permit5-ID-a Drilling and Well Development5-MT-a

Note: This page contains sample records for the topic "mt simon sandstone" 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.


221

RAPID/Roadmap/9-MT-a | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExplorationUT-g Grant of Access Permit5-ID-a Drilling7-HI-ce <9-FD-e9-MT-a State

222

M.T. Thomas Award for Outstanding Postdoctoral Achievement | EMSL  

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

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcalgovInstrumentsrucLas Conchas recovery challenge fund Las ConchasTrail of a martian20085816M.T. Thomas Award

223

RAPID/Roadmap/11-MT-a | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, search RAPIDColorado < RAPID‎ | Geothermal‎-CA-a) <11-FD-c1-MT-a

224

RAPID/Roadmap/14-MT-a | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, search RAPIDColorado < RAPID‎ |1-TX-a13-ID-a State14-FD-c4-MT-a Nonpoint

225

RAPID/Roadmap/14-MT-e | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, search RAPIDColorado < RAPID‎ |1-TX-a13-ID-a State14-FD-c4-MT-a

226

RAPID/Roadmap/17-MT-a | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, search RAPIDColorado <17-HI-a < RAPID‎ | Roadmap Jump to:7-MT-a

227

RAPID/Roadmap/18-MT-b | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, search RAPIDColorado <17-HI-a < RAPID‎ |18-MT-b Hazardous Waste

228

RAPID/Roadmap/3-MT-b | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, search RAPIDColorado <17-HI-a <3-FD-d Foresto <Roadmap/3-ID-e3-MT-b

229

RAPID/Roadmap/4-MT-a | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, search RAPIDColorado <17-HI-a <3-FD-d3-WA-b Land4-FD-b4-HI-a4-MT-a

230

RAPID/Roadmap/6-MT-a | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, search RAPIDColorado <17-HI-a4-WA-a State6-CO-b ConstructionRoadmap/6-MT-a

231

National uranium resource evaluation. Geology and recognition criteria for sandstone uranium deposits of the salt wash type, Colorado Plateau Province. Final report  

SciTech Connect (OSTI)

The uranium-vanadium deposits of the Salt Wash Member of the Morrison Formation in the Colorado Plateau are similar to sandstone uranium deposits elsewhere in the USA. The differences between Salt Wash deposits and other sandstone uranium deposits are also significant. The Salt Wash deposits are unique among sandstone deposits in that they are dominantly vanadium deposits with accessory uranium. The Salt Wash ores generally occur entirely within reduced sandstone, without adjacent tongues of oxidized sandstone. They are more like the deposits of Grants, which similarly occur in reduced sandstones. Recent studies of the Grants deposits have identified alteration assemblages which are asymmetrically distributed about the deposits and provide a basis for a genetic model for those deposits. The alteration types recognized by Shawe in the Slick Rock district may provide similar constraints on ore formation when expanded to broader areas and more complete chemical analyses.

Thamm, J.K.; Kovschak, A.A. Jr.; Adams, S.S.

1981-01-01T23:59:59.000Z

232

The effects of Chern-Simons gravity on bodies orbiting the Earth  

E-Print Network [OSTI]

One of the possible low-energy consequences of string theory is the addition of a Chern-Simons term to the standard Einstein-Hilbert action of general relativity. It can be argued that the quintessence field should couple to this Chern-Simons term, and if so, it drives in the linearized theory a parity-violating interaction between the gravito-electric and gravitomagnetic fields. In this paper, the linearized spacetime for Chern-Simons gravity around a massive spinning body is found to include new modifications to the gravitomagnetic field that have not appeared in previous work. The orbits of test bodies and the precession of gyroscopes in this spacetime are calculated, leading to new constraints on the Chern-Simons parameter space due to current satellite experiments.

Tristan L. Smith; Adrienne L. Erickcek; Robert R. Caldwell; Marc Kamionkowski

2008-01-08T23:59:59.000Z

233

E-Print Network 3.0 - abelian chern-simons gauge Sample Search...  

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

<< < 1 2 3 4 5 > >> 1 Entanglement Entropy at 2D quantum critical points, topological fluids and quantum Hall fluids Summary: is Abelian Chern-Simons gauge theory U(1)m for the...

234

Simon Fraser University | Sustainability Communications Designer | August 13, 2014 Sustainability Communications Coordinator  

E-Print Network [OSTI]

Simon Fraser University | Sustainability Communications Designer | August 13, 2014 Sustainability Communications Coordinator JOB DESCRIPTION Position Title: Sustainability Communications Coordinator Position, 2014-March, 2016 (extension possible) Reports to: Director, SFU Sustainability Office Posting Date

235

Interactive Translucent Volume Rendering and Procedural Modeling Joe Kniss Simon Premoze Charles Hansen David Ebert  

E-Print Network [OSTI]

Interactive Translucent Volume Rendering and Procedural Modeling Joe Kniss Simon Premoze¶ Charles School of Electrical and Computer Engineering Purdue University Figure 1: A translucent fish rendered. Abstract Direct volume rendering is a commonly used technique in visual- ization applications. Many

Kniss, Joe Michael

236

Cancer Systems Biology Dana Faratian, James L. Bown, V. Anne Smith, Simon P. Langdon,  

E-Print Network [OSTI]

245 Chapter 12 Cancer Systems Biology Dana Faratian, James L. Bown, V. Anne Smith, Simon P. Langdon+Business Media, LLC 2010 #12;246 Faratian et al. While cancer can arise from any cell in the body, the commonest

Smith, V Anne

237

Multiple-scattering in radar systems: A review Alessandro Battaglia a,b,, Simone Tanelli c  

E-Print Network [OSTI]

Review Multiple-scattering in radar systems: A review Alessandro Battaglia a,b,Ã, Simone Tanelli c. Tel.: +44 116 2709859. E-mail address: a.battaglia@le.ac.uk (A. Battaglia). Journal of Quantitative Spectroscopy & Radiative Transfer ] (

Hogan, Robin

238

Monitoring and Targeting (M&T): A Low Investment, Low Risk Approach to Energy Cost Savings  

E-Print Network [OSTI]

Monitoring and Targeting (M&T): A Low Investment, Low Risk Approach to Energy Cost Savings Andrew McMullan Mike Rutkowski Alan Karp Vice President President Manager Bus. Development VERITECH, INC. Sterling, VA ABSTRACT Monitoring... and Targeting (M&T) is a disciplined approach to energy management that ensures that energy resources are used to their maximmn economic advantage. M&T serves two principal functions: ? Ongoing, day-to-day control of energy use ? Planned improvements...

McMullan, A.; Rutkowski, M.; Karp, A.

239

Adiabatic Pumping of Chern-Simons Axion Coupling  

E-Print Network [OSTI]

We study the adiabatic pumping of the Chern-Simons axion (CSA) coupling along a parametric loop characterized by a non-zero second Chern number $C^{(2)}$ from the viewpoint of the hybrid Wannier representation, in which the Wannier charge centers (WCCs) are visualized as sheets defined over a projected 2D Brillouin zone. We derive a new formula for the CSA coupling, expressing it as an integral involving Berry curvatures and potentials defined on the WCC sheets. We show that a loop characterized by a non-zero $C^{(2)}$ requires a series of sheet-touching events at which $2\\pi$ quanta of Berry curvature are passed from sheet to sheet, in such a way that $e^2/h$ units of CSA coupling are pumped by a lattice vector by the end of the cycle. We illustrate these behaviors via explicit calculations on a model tight-binding Hamiltonian and discuss their implications.

Maryam Taherinejad; David Vanderbilt

2014-11-06T23:59:59.000Z

240

,"Port of Del Bonita, MT Natural Gas Pipeline Imports From Canada...  

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

Del Bonita, MT Natural Gas Pipeline Imports From Canada (MMcf)" ,"Click worksheet name or tab at bottom for data" ,"Worksheet Name","Description"," Of Series","Frequency","Latest...

Note: This page contains sample records for the topic "mt simon sandstone" 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

Depositional setting, structural style, and sandstone distribution in three geopressured geothermal areas, Texas Gulf Coast  

SciTech Connect (OSTI)

Three areas in the Texas Gulf Coastal Plain were studied using electric logs and seismic-reflection data to interpret their depositional and structural history and to compare their potential as geopressured-geothermal reservoirs. The Cuero study area, on the lower Wilcox (upper Paleocene) growth-fault trend, is characterized by closely and evenly spaced, subparallel, down-to-the-basin growth faults, relatively small expansion ratios, and minor block rotation. Distributary-channel sandstones in the geopressured lower Wilcox Group of the South Cook fault block appear to be the best geothermal aquifers in the Cuero area. The Blessing study area, on the lower Frio (Oligocene) growth-fault trend, shows wider and more variable fault spacing and much greater expansion ratios and block rotation, particularly during early Frio time. Thick geopressured sandstone aquifers are laterally more extensive in the Blessing area than in the Cuero area. The Pleasant Bayou study area, like the Blessing area, is on the Frio growth-fault trand, and its early structural development was similar rapid movement of widely spaced faults resulted in large expansion ratios and major block rotation. However, a late-stage pattern of salt uplift and withdrawal complicated the structural style. Thick geopressured lower Frio sandstone aquifers are highly permeable and laterally extensive, as in the Blessing area. In all three areas, geopressured aquifers were created where early, rapid movement along down-to-the-basin growth faults juxtaposed shallow-water sands against older shales, probably deposited in slope environments. Major transgressions followed the deposition of reservoir sands and probably also influenced the hydraulic isolation that allowed the build up of abnormal pressures. 26 refs., 49 figs., 8 tabs.

Winker, C.D.; Morton, R.A.; Ewing, T.E.; Garcia, D.D.

1983-01-01T23:59:59.000Z

242

Sedimentology, diagenesis, and trapping style, Chesterian Tar Springs sandstone at Inman Field, Gallatin County, Illinois  

SciTech Connect (OSTI)

The Tar Springs Sandstone in southern Illinois is often over-looked as a pay, yet it can be a prolific producer. The Inman Field, discovered in 1940, produces from several cyclic Chesterian sandstones from structural-stratigraphic traps in the Wabash Valley Fault System of southeastern Illinois. The oil was sourced from the Devonian New Albany Shale and apparently migrated vertically along the Wabash Valley faults to its present location, thus charging many of the Chesterian and lower Pennsylvanian sands in the field. The Tar Springs Sandstone produces from stacked distributary channel sand reservoirs up to 125 feet thick which have cut up to 40 feet into laterally equivalent non-reservoir, delta-fringe facies and the underlying Glen Dean Limestone. The reservoir sands are well-sorted, fine- to medium-grained quartz arenites with less than 5% feldspar and chert. Quartz grains have quartz overgrowths. Feldspar grains are clouded in thin-section and show pronounced etching and dissolution in SEM. Diagenetic kaolinite and small amounts of illite and magnesium-rich chlorite occur in intergranular pores. Sparry, iron-rich dolomite or ankerite that fills pores in irregular millimeter-size patches, occupies up to 10% of the reservoir rock. Typical reservoir porosity ranges from 16 to 19 percent and permeability ranges from 60 to 700 md. By contrast non-reservoir delta-fringe sands typically have porosities of 6 to 12 percent and permeabilities of 1 to 20 md. Delta-fringe Tar Springs shales act as impermeable lateral and vertical seals, aiding in stratigraphic trapping.

Morse, D.G. [Illinois State Geological Survey, Champaign, IL (United States)

1996-09-01T23:59:59.000Z

243

SIMON FRASER The Applied Research in Ichnology and Sedimentology (ARISE) Group (www.sfu.ca/arise) in the Department of  

E-Print Network [OSTI]

SIMON FRASER UNIVERSITY The Applied Research in Ichnology and Sedimentology (ARISE) Group (www at conferences and consortium workshops. Preferred applicants should have strong sedimentological

Dashtgard, Shahin

244

Depositional environment of upper Cretaceous woodbine sandstones, Kurten field, Brazos County, Texas  

E-Print Network [OSTI]

" sand- stone showing a broad, channel-like morphology 34 17 Seismic section showing the location of Kur ten field in relation to the Hi11 Ranch salt dome. Points A, B, and C correspond to the downdip limits of the "A", "B" and "C" sandstones... at Madisonvil le, this trend extends southwest through Grimes, Brazos and Washington counties with the occur r ence of Ferguson Crossing, Mil1ican and Brenham salt domes, Drilling History The Kurten Field was di scovered in August, 1976, with the compl e...

Watkins, John Mark

1982-01-01T23:59:59.000Z

245

Facies distribution of upper cretaceous Woodbine Sandstones, southern Kurten Field, Brazos County, Texas  

E-Print Network [OSTI]

CI EAST TEXAS TYLER FIELD I SABINE - UPLlFT I' 7 ~ Z 1 . '~+ KURTEN'-, g' ?qS+ +POLK TYLER N TEXAS SEVEN OAKS 0 50 mi SUGAR CREEK 0 80 km Figure 1. Nap of northeast Texas showing major structural features and Woodbine oil production..., anticlines and salt domes were the targets of early exploration in east Texas. The Woodbine sandstones are prolific oil and gas producers in the East Texas basin. Although this mature petroleum province has been productive for more than 50 years, new...

Leethem, John Thomas

1984-01-01T23:59:59.000Z

246

Characterization of a sandstone reservoir using seismic methods: Yowlumne Field, Kern County, California  

E-Print Network [OSTI]

shale, and 2) the high V;-sones identifled for regions outside these boundaries may contain reservoir-quality rocks. To My Parents ACKNOWLEDGMENTS I wish to express my gratitude to Dr. Anthony Gangi. chairman of my com- mittee, for discussing... ft/s per ft (0. 464 m/s per m) to a maximum depth of 13, 500 ft (4114. 8 m). Rapid lateral variations in lithology prevented him from identifying shales or sandstones using velocities. The variation of velocity with respect to depth was considered...

Proust, Rodrigo Diez

1988-01-01T23:59:59.000Z

247

Contrasting depositional processes of Sub-Clarksville and Woodbine reservoir sandstones, Grimes County, Texas  

E-Print Network [OSTI]

time allowed, I would liked to have drawn more upon his expertise for this study. I would also like to thank Dr. Tieh, of Geology, for his willingness to look at any "troublesome" thin sections. His good-heartedness, as well as Dr. Stanton... showing the Sub-Clarksville thinning to the east and west in a structure low. . . . 81 21. Isopach of the Sub-Clarksville Sandstone. Contour interval is 5 ft 82 22. Se' mic line that extends northwest- southeast across Hill field showing salt...

Barton, Robert Andrew

1982-01-01T23:59:59.000Z

248

Depositional environment of Upper Devonian gas producing sandstones, Westmoreland County, southwestern Pennsylvania  

E-Print Network [OSTI]

for each sandstone; for each thin section, 100 monocrystalline quartz grains were counted. 37 LLOYDSVILLE SPORTSMAN ASSOCIATION I GRAIN SIZE mm 2. 0 I. O 0. 5 0. 25 O. I2 COMPOSITION /o CEM % 0 50 100 0 30 I 3I95 C Ep I I I I 3I97 FIRS T BRA... or polycrystalline as determined by the number of crystals within the quartz grain. Monocrystalline quartz is composed of a single crystal, and has simple or wavy extinction. Polycrystalline quartz contains more than one crystal within the grain. If crystals...

Work, Rebecca Miller

1988-01-01T23:59:59.000Z

249

Depositional environment of Canyon (Cisco) sandstones, North Jameson field Mitchell County, Texas  

E-Print Network [OSTI]

deposits are dominated by "CE" and "CDE" bedsets that form sequences 0. 1 to 5. 0 ft (0. 0$ to 1. 5 m) thick. Together, these three kinds of deposits form an interbedded sand and shale wedge approximately 150 ft (46 m) thick, thinning basinward. iv... Basins. The sand. stones are part of the Cisco Group and form thin, narrow, dip-trending petroleum reservoirs. These reservoirs form stratigraphic traps in and around older carbonate reefs. Jameson (North) Strawn field is a typical basinal sandstone...

Dally, David Jesse

1983-01-01T23:59:59.000Z

250

A study of uranium distribution in an upper Jackson lignite-sandstone ore body, South Texas  

E-Print Network [OSTI]

-central Wyoming (Denson, 1959). Since then similar discoveries have been made in North and South Dakota, Montana, Idaho, New Mexico, and most recently, in Texas. Porous, organic-r1ch sediments have repeatedly been proven to be favorable sites for uranium...A STUDY OF URANIUM DISTRIBUTION IN AN UPPER JACKSON LIGNITE-SANDSTONE ORE BODY, SOUTH TEXAS A Thesis James Randall Chatham Subnitted to the Graduate College of Texas A8M University in Partial fulfillment of the requirement for the degree...

Chatham, James Randall

1979-01-01T23:59:59.000Z

251

An assessment of regional climate trends and changes to the Mt. Jaya glaciers of Irian Jaya  

E-Print Network [OSTI]

on the Mt. Jaya glaciers has been lacking since the early 1970s. Using IKONOS satellite images, the ice extents of the Mt. Jaya glaciers in 2000, 2002, 2003, 2004, and 2005 were mapped. The mapping indicates that the recessional trend which began in the mid...

Kincaid, Joni L.

2007-09-17T23:59:59.000Z

252

MT-SDF: Scheduled Dataflow Architecture with mini-threads Domenico Pace  

E-Print Network [OSTI]

MT-SDF: Scheduled Dataflow Architecture with mini-threads Domenico Pace University of Pisa Pisa Dataflow (SDF) architecture. We call the new architecture MT-SDF. We introduce mini-threads to execute and quantitative comparison of the mini-threads with the original SDF architecture, and out-of-order superscalar

Kavi, Krishna

253

Mixed fluvial systems of Messak Sandstone, a deposit of Nubian lithofacies, southwestern Libya  

SciTech Connect (OSTI)

The Messak Sandstone is a coarse to pebbly, tabular cross-bedded, Lower Cretaceous deposit of the widespread Nubian lithofacies. It was deposited at the northern edge of the Murzuq basin in southwestern Libya. Although the sedimentary record is predominantly one of braided fluvial systems, a common subfacies within the formation is interpreted to record the passage of straight-crested sand waves across laterally migrating point bars in sinuous rivers, similar to the pattern documented by Singh and Kumar on the modern Ganga and Yamuna Rivers. Because the sand waves were larger on the lower parts of the point bars, lateral migration created diagnostic thinning-upward, unidirectional cosets of tabular cross-beds as well as fining-upward, grain-size trends. Common, thick, interbedded claystones, deposited in associated paludal and lacustrine environments, and high variance in cross-bed dispersion patterns also suggest the local presence of sinuous fluvial systems within the overall braided regime. The Messak Sandstone contains some of the features that led Harms et al to propose an unconventional low-sinuosity fluvial environment for the Nubian lithofacies in Egypt, and the continuously high water levels of this model may explain channel-scale clay drapes and overturned cross-beds in the Messak. However, most of the Messak characteristics are incompatible with the low-sinuosity model, suggesting instead that the fluvial channels in the Murzuq basin alternated between braided and high-sinuosity patterns.

Lorenz, J.C.

1987-05-01T23:59:59.000Z

254

Reservoir heterogeneity in Carboniferous sandstone of the Black Warrior basin. Final report  

SciTech Connect (OSTI)

Although oil production in the Black Warrior basin of Alabama is declining, additional oil may be produced through improved recovery strategies, such as waterflooding, chemical injection, strategic well placement, and infill drilling. High-quality characterization of reservoirs in the Black Warrior basin is necessary to utilize advanced technology to recover additional oil and to avoid premature abandonment of fields. This report documents controls on the distribution and producibility of oil from heterogeneous Carboniferous reservoirs in the Black Warrior basin of Alabama. The first part of the report summarizes the structural and depositional evolution of the Black Warrior basin and establishes the geochemical characteristics of hydrocarbon source rocks and oil in the basin. This second part characterizes facies heterogeneity and petrologic and petrophysical properties of Carter and Millerella sandstone reservoirs. This is followed by a summary of oil production in the Black Warrior basin and an evaluation of seven improved-recovery projects in Alabama. In the final part, controls on the producibility of oil from sandstone reservoirs are discussed in terms of a scale-dependent heterogeneity classification.

Kugler, R.L.; Pashin, J.C.; Carroll, R.E.; Irvin, G.D.; Moore, H.E.

1994-04-01T23:59:59.000Z

255

Reservoir heterogeneity in carboniferous sandstone of the Black Warrior basin. Final report  

SciTech Connect (OSTI)

Although oil production in the Black Warrior basin of Alabama is declining, additional oil may be produced through improved recovery strategies, such as waterflooding, chemical injection, strategic well placement, and infill drilling. High-quality characterization of reservoirs in the Black Warrior basin is necessary to utilize advanced technology to recover additional oil and to avoid premature abandonment of fields. This report documents controls on the distribution and producibility of oil from heterogeneous Carboniferous reservoirs in the Black Warrior basin of Alabama. The first part of the report summarizes the structural and depositional evolution of the Black Warrior basin and establishes the geochemical characteristics of hydrocarbon source rocks and oil in the basin. This second part characterizes facies heterogeneity and petrologic and petrophysical properties of Carter and Millerella sandstone reservoirs. This is followed by a summary of oil production in the Black Warrior basin and an evaluation of seven improved-recovery projects in Alabama. In the final part, controls on the producibility of oil from sandstone reservoirs are discussed in terms of a scale-dependent heterogeneity classification.

Kugler, R.L.; Pashin, J.C.; Carroll, R.E.; Irvin, G.D.; Moore, H.E.

1994-06-01T23:59:59.000Z

256

Depositional environment and reservoir characteristics of the lower Vicksburg sandstones, west McAllen Ranch Field, Hidalgo County, Texas  

E-Print Network [OSTI]

. 5 ft in thickness. This sequence represents AB turbidites probably of channel origin and con- tains minor amounts of shale. Thin-bedded sandstones are dominated by laminated and rippled sandstones of BCD turbidites with bedsets aver- aging 2. 5... at the base to 0. 09 mm at the top. Aver- age detrital compositional is 16 percent monocrystalline quartz, 35 percent feldspar, 39 percent rock fragments, 9 percent matrix and 1 percent other grains. Common cement is calcite as pore fillings and some grain...

Marshall, William Dustin

1978-01-01T23:59:59.000Z

257

Determination of capillary displacement pressure and representative average capillary pressure vs. depth in shally sandstones from well logs  

SciTech Connect (OSTI)

This research presents a method whereby the capillary displacement pressure Pcd and the representative average capillary pressure in shaly sandstone reservoirs exhibits continuous information vs. depth from well logs. By the aid of special core analysis, correlation functions were obtained that relate the capillary characteristics of the reservoir rock to its lithologic development. Since the lithologic influence factor is a well log-derived parameter the correlations then were used to determine by means of well logs the capillary displacement and average capillary pressures for borehole sections where special core analysis is not available. This technique has been developed and applied to the shaly sandstone reservoir of the Sarir oil field in Libya.

Barlai, Z.; Berruin, N.A.; Mawla, R.A.

1981-01-01T23:59:59.000Z

258

Contrasting processes of deposition for the Eagleford "B" sandstone, Bryan, IDS, and Kurten fields, Brazos County, Texas  

E-Print Network [OSTI]

of Meridian Oil for production data and Sandra Phillips of Arco Alaska for the loan of a most valuable reference. Thanks go to the many friends I have made while attending A&M but especially to Jack Sanford, Ron Brogdon, Andy Davidoff, and Budi...) Figure Page Index map of Brazos County showing location of major oil and gas fields productive from Eagleford sandstones. 18 Type log for the Kurten field, Amal- gamated Bonanza Lloyd 1, showing log character of the five Woodbine- Eagleford sandstones...

Golding, Robert Martin

1990-01-01T23:59:59.000Z

259

Action Principles for Transgression and Chern-Simons AdS Gravities  

E-Print Network [OSTI]

Chern-Simons gravities are theories with a lagrangian given by a Chern-Simons form constructed from a space-time gauge group. In previous investigations we showed that, for some special field configurations that are solutions of the field equations, the extension from Chern-Simons to Transgression forms as lagrangians, motivated by gauge invariance, automatically yields the boundary terms required to regularize the theory, giving finite conserved charges and black hole thermodynamics. Further work by other researchers showed that one of the action functionals considered in the above mentioned work yields a well defined action principle in the metric (zero torsion) case and for asymptotically Anti de Sitter (AdS) space-times. In the present work we consider several action functionals for Chern-Simons AdS gravity constructed from Transgression forms, and show the action principles to be well defined and the Noether charges and Euclidean action to be finite for field configurations satisfying only that the gauge field curvature (field strength) for the AdS gauge group is asymptotically finite. For that purpose we consider an asymptotic expansion of the vielbein and spin connection that may be regarded as a perturbation of an AdS space-time, but allowing a non zero torsion. Our results are of potential interest for Lovelock gravity theories, as it has been shown that the boundary terms dictated by the transgressions for Chern-Simons gravities are also suitable to regularize Lovelock theories.

Pablo Mora

2014-08-06T23:59:59.000Z

260

The Chern-Simons term in a dual Josephson junction  

E-Print Network [OSTI]

A dual Josephson junction corresponding to a (2+1)-dimensional non-superconducting layer sandwiched between two (3+1)-dimensional dual superconducting regions constitutes a model of localization of a U(1) gauge field within the layer. Monopole tunneling currents flow from one dual superconducting region to another due to a phase difference between the wave functions of the monopole condensate below and above the non-superconducting layer when there is an electromagnetic field within the layer. These magnetic currents appear within the (2+1)-dimensional layer as a gas of magnetic instanton events and a weak electric charge confinement is expected to take place at very long distances within the layer. In the present work, we consider what happens when one introduces fermions in this physical scenario. Due to the dual Meissner effect featured in the dual superconducting bulk, it is argued that unconfined fermions would be localized within the (2+1)-dimensional layer, where their quantum fluctuations radiatively induce a Chern-Simons term, which is known to destroy the electric charge confinement and to promote the confinement of the magnetic instantons.

L. S. Grigorio; M. S. Guimaraes; R. Rougemont; C. Wotzasek; C. A. D. Zarro

2013-08-27T23:59:59.000Z

Note: This page contains sample records for the topic "mt simon sandstone" 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

Optical Properties Chern-Simons (3+1)D $?$-systems  

E-Print Network [OSTI]

Chern-Simons (CS) $\\theta$-systems are described by a $\\theta \\int F\\wedge F$ term in the action ($\\theta$ is an adimensional parameter), which does not change field equations in the bulk, but affects the system behaviour when it is bounded. When two of those $\\theta$-systems, each one characterized by a different value of $\\theta$ (even zero), share a common boundary, surface effects are then induced by a CS $\\theta$ term. Here, we study the consequences of the above in the propagation of electromagnetic radiation in $\\theta$-systems. In a previous paper, electromagnetic radiation properties traversing a $\\theta$-vacuum were analyzed where a number of interesting features arise related to polarization and energy distribution. Now, we investigate how electric and magnetic properties of the $\\theta$-system affect the optical response. Apart from the well-known Kerr polarization rotation found for the particular case of topological insulators, we examine in detail the issue and the results could be applied in other contexts where $\\theta$-term accounts for the system dynamics. In particular, we find two different Brewster angles, for $s$ and $p$ polarization of reflected radiation, respectively, with peculiar features derived from the $\\theta$ term influence. Possible applications of these results are discussed.

Luis Huerta

2014-12-17T23:59:59.000Z

262

The Chern-Simons term in a dual Josephson junction  

E-Print Network [OSTI]

A dual Josephson junction corresponding to a (2+1)-dimensional non-superconducting layer sandwiched between two (3+1)-dimensional dual superconducting regions constitutes a model of localization of a U(1) gauge field within the layer. Monopole tunneling currents flow from one dual superconducting region to another due to a phase difference between the wave functions of the monopole condensate below and above the non-superconducting layer. These magnetic currents appear within the (2+1)-dimensional layer as a gas of magnetic instanton events and a weak electric charge confinement is expected to take place at very long distances within the layer. In the present work, we consider what happens when one introduces fermions in this physical scenario. Due to the dual Meissner effect featured in the dual superconducting bulk, it is argued that unconfined fermions would be localized within the (2+1)-dimensional layer, where their quantum fluctuations radiatively induce a Chern-Simons term, which is known to destroy th...

Grigorio, L S; Rougemont, R; Wotzasek, C; Zarro, C A D

2013-01-01T23:59:59.000Z

263

To: SIMON FRASER UNIVERSITY NON-DISCLOSURE AGREEMENT REQUEST Office of Research Services (Fax: 778-782-3477)  

E-Print Network [OSTI]

To: SIMON FRASER UNIVERSITY NON-DISCLOSURE AGREEMENT REQUEST Office of Research Services (Fax: 778-782-3477) Party 1 to Agreement: Simon Fraser University funding (including student/post-docs funding sources) used in creating Information? Yes No. If yes

264

The Implementation of a FirstOrder Logic AGM Belief Revision System Simon Dixon and Wayne Wobcke  

E-Print Network [OSTI]

The Implementation of a First­Order Logic AGM Belief Revision System Simon Dixon and Wayne Wobcke­mail: simon@cs.su.oz.au, wobcke@cs.su.oz.au Abstract Belief revision is increasingly being seen as central belief revision system. The system is based on classical first­ order logic, and for any finitely

Dixon, Simon

265

Impact of monsoons, temperature, and CO2 on the rainfall and ecosystems of Mt. Kenya during the Common Era  

E-Print Network [OSTI]

Impact of monsoons, temperature, and CO2 on the rainfall and ecosystems of Mt. Kenya during Leaf waxes Glacial and early Holocene-age sediments from lakes on Mt. Kenya have documented strong and atmospheric CO2 concentra- tions. However, little is known about climate and ecosystem variations on Mt. Kenya

Vuille, Mathias

266

Testing Chern-Simons modified gravity with orbiting superconductive gravity gradiometers --- The non-dynamical formulation  

E-Print Network [OSTI]

High precision Superconductivity Gravity Gradiometers (SGG) are powerful tools for relativistic experiments. In this paper, we work out the tidal signals in non-dynamical Chern-Simons modified gravity, which could be measured by orbiting SGGs around Earth. We find that, with proper orientations of multi-axes SGGs, the tidal signals from the Chern-Simons modification can be isolated in the combined data of different axes. Furthermore, for three-axes SGGs, such combined data is the trace of the total tidal matrix, which is invariant under the rotations of SGG axes and thus free from axis pointing errors. Following nearly circular orbits, the tests of the parity-violating Chern-Simons modification and the measurements of the gravitomagnetic sector in parity-conserving metric theories can be carried out independently in the same time. A first step analysis on noise sources is also included.

Qiang, Li-E

2015-01-01T23:59:59.000Z

267

Testing Chern-Simons modified gravity with orbiting superconductive gravity gradiometers --- The non-dynamical formulation  

E-Print Network [OSTI]

High precision Superconductivity Gravity Gradiometers (SGG) are powerful tools for relativistic experiments. In this paper, we work out the tidal signals in non-dynamical Chern-Simons modified gravity, which could be measured by orbiting SGGs around Earth. We find that, with proper orientations of multi-axes SGGs, the tidal signals from the Chern-Simons modification can be isolated in the combined data of different axes. Furthermore, for three-axes SGGs, such combined data is the trace of the total tidal matrix, which is invariant under the rotations of SGG axes and thus free from axis pointing errors. Following nearly circular orbits, the tests of the parity-violating Chern-Simons modification and the measurements of the gravitomagnetic sector in parity-conserving metric theories can be carried out independently in the same time. A first step analysis on noise sources is also included.

Li-E Qiang; Peng Xu

2015-02-16T23:59:59.000Z

268

Level-Rank Duality in Chern-Simons Theory from a Non-Supersymmetric Brane Configuration  

E-Print Network [OSTI]

We derive level-rank duality in pure Chern-Simons gauge theories from a non-supersymmetric Seiberg duality by using a non-supersymmetric brane configuration in type IIB string theory. The brane configuration consists of fivebranes, N D3 antibranes and an O3 plane. By swapping the fivebranes we derive a 3d non-supersymmetric Seiberg duality. After level shifts from loop effects, this identifies the IR of Sp(2N)_{2k-2N+2} and Sp(2k-2N+2)_{-2N} pure Chern-Simons theories, which is a level-rank pair. We also derive level-rank duality in a Chern-Simons theory based on a unitary group.

Adi Armoni; Edwin Ireson

2014-08-20T23:59:59.000Z

269

Interpretation of Pennsylvania Bartlesville sandstone in southeastern Kansas and northeastern Oklahoma from continuous dipmeter and gamma-ray logs  

E-Print Network [OSTI]

of the stream current, w111 enable a more precise determination of the paleogeography and morphology of the reservoir sandstones in each f1eld. However, an environmental The c1tat1ons of this thesis follow the format and style of the Amefic o A tocietio f P...

Kranz, Dwight Stanley

1981-01-01T23:59:59.000Z

270

Frio sandstone reservoirs in the deep subsurface along the Texas Gulf Coast: their potential for production of geopressured geothermal energy  

SciTech Connect (OSTI)

Detailed geological, geophysical, and engineering studies conducted on the Frio Formation have delineated a geothermal test well site in the Austin Bayou Prospect which extends over an area of 60 square miles. A total of 800 to 900 feet of sandstone will occur between the depths of 13,500 and 16,500 feet. At leat 30 percent of the sand will have core permeabilities of 20 to 60 millidarcys. Temperature at the top of the sandstone section will be 300/sup 0/F. Water, produced at a rate of 20,000 to 40,000 barrels per day, will probably have to be disposed of by injection into shallower sandstone reservoirs. More than 10 billion barrels of water are in place in these sandstone reservoirs of the Austin Bayou Prospect; there should be approximately 400 billion cubic feet of methane in solution in this water. Only 10 percent of the water and methane (1 billion barrels of water and 40 billion cubic feet of methane) will be produced without reinjection of the waste water into the producing formation. Reservoir simulation studies indicate that 90 percent of the methane can be produced with reinjection. 106 figures.

Bebout, D.G.; Loucks, R.G.; Gregory, A.R.

1983-01-01T23:59:59.000Z

271

CO2 percolation experiment through chlorite/zeolite-rich sandstone (Pretty Hill Formation Otway BasinAustralia)  

E-Print Network [OSTI]

CO2 percolation experiment through chlorite/zeolite-rich sandstone (Pretty Hill Formation ­ Otway November 2011 Editor: D.B. Dingwell Keywords: CO2 storage Clay precipitation Carbon Permeability Reactive transport Underground CO2 sequestration is highly recommended as an effective means of significantly

Demouchy, Sylvie

272

Effect of Temperature and Solution Composition on the Permeability of St. Peters Sandstone: Role of Iron (III)  

SciTech Connect (OSTI)

The purpose of this study was to systematically investigate effects of temperature and fluid composition on the permeability of quartz sandstones. We have concentrated our initial efforts on the time and flow dependence at 2 elevated temperatures (100°C, 200°C).

Potter, J.M.; Nur, A.; Dibble, W.E. Jr.

1980-12-16T23:59:59.000Z

273

MT3D: a 3 dimensional magnetotelluric modeling program (user's guide and documentation for Rev. 1)  

SciTech Connect (OSTI)

MT3D.REV1 is a non-interactive computer program written in FORTRAN to do 3-dimensional magnetotelluric modeling. A 3-D volume integral equation has been adapted to simulate the MT response of a 3D body in the earth. An integro-difference scheme has been incorporated to increase the accuracy. This is a user's guide for MT3D.REV1 on the University of Utah Research Institute's (UURI) PRIME 400 computer operating under PRIMOS IV, Rev. 17.

Nutter, C.; Wannamaker, P.E.

1980-11-01T23:59:59.000Z

274

Photoproduction through Chern-Simons term induced interactions in holographic QCD  

SciTech Connect (OSTI)

We employ both top-down and bottom-up holographic dual models of QCD to calculate vertex functions and couplings that are induced by the five-dimensional Chern-Simons term. We use these couplings to study the photoproduction of f{sub 1} mesons. The Chern-Simons-term-induced interaction leads to a simple relation between the polarization of the incoming photon and the final state f{sub 1} meson which should allow a clear separation of this interaction from competing processes.

Domokos, Sophia K.; Harvey, Jeffrey A. [Enrico Fermi Institute and Department of Physics, University of Chicago, Chicago Illinois 60637 (United States); Grigoryan, Hovhannes R. [Physics Division, Argonne National Laboratory, Argonne, Illinois 60439-4843 (United States)

2009-12-01T23:59:59.000Z

275

Numerical modelling of sandstone uniaxial compression test using a mix-mode cohesive fracture model  

E-Print Network [OSTI]

A mix-mode cohesive fracture model considering tension, compression and shear material behaviour is presented, which has wide applications to geotechnical problems. The model considers both elastic and inelastic displacements. Inelastic displacement comprises fracture and plastic displacements. The norm of inelastic displacement is used to control the fracture behaviour. Meantime, a failure function describing the fracture strength is proposed. Using the internal programming FISH, the cohesive fracture model is programmed into a hybrid distinct element algorithm as encoded in Universal Distinct Element Code (UDEC). The model is verified through uniaxial tension and direct shear tests. The developed model is then applied to model the behaviour of a uniaxial compression test on Gosford sandstone. The modelling results indicate that the proposed cohesive fracture model is capable of simulating combined failure behaviour applicable to rock.

Gui, Yilin; Kodikara, Jayantha

2015-01-01T23:59:59.000Z

276

Methane Hydrate Dissociation by Depressurization in a Mount Elbert Sandstone Sample: Experimental Observations and Numerical Simulations  

SciTech Connect (OSTI)

A preserved sample of hydrate-bearing sandstone from the Mount Elbert Test Well was dissociated by depressurization while monitoring the internal temperature of the sample in two locations and the density changes at high spatial resolution using x-ray CT scanning. The sample contained two distinct regions having different porosity and grain size distributions. The hydrate dissociation occurred initially throughout the sample as a result of depressing the pressure below the stability pressure. This initial stage reduced the temperature to the equilibrium point, which was maintained above the ice point. After that, dissociation occurred from the outside in as a result of heat transfer from the controlled temperature bath surrounding the pressure vessel. Numerical modeling of the test using TOUGH+HYDRATE yielded a gas production curve that closely matches the experimentally measured curve.

Kneafsey, T.; Moridis, G.J.

2011-01-15T23:59:59.000Z

277

Reservoir condition special core analyses and relative permeability measurements on Almond formation and Fontainebleu sandstone rocks  

SciTech Connect (OSTI)

This report describes the results from special core analyses and relative permeability measurements conducted on Almond formation and Fontainebleu sandstone plugs. Almond formation plug tests were performed to evaluate multiphase, steady-state,reservoir-condition relative permeability measurement techniques and to examine the effect of temperature on relative permeability characteristics. Some conclusions from this project are as follows: An increase in temperature appeared to cause an increase in brine relative permeability results for an Almond formation plug compared to room temperature results. The plug was tested using steady-state oil/brine methods. The oil was a low-viscosity, isoparaffinic refined oil. Fontainebleu sandstone rock and fluid flow characteristics were measured and are reported. Most of the relative permeability versus saturation results could be represented by one of two trends -- either a k{sub rx} versus S{sub x} or k{sub rx} versus Sy trend where x and y are fluid phases (gas, oil, or brine). An oil/surfactant-brine steady-state relative permeability test was performed to examine changes in oil/brine relative permeability characteristics from changes in fluid IFTS. It appeared that, while low interfacial tension increased the aqueous phase relative permeability, it had no effect on the oil relative permeability. The BOAST simulator was modified for coreflood simulation. The simulator was useful for examining effects of variations in relative permeability and capillary pressure functions. Coreflood production monitoring and separator interface level measurement techniques were developed using X-ray absorption, weight methods, and RF admittance technologies. The three types of separators should be useful for routine and specialized core analysis applications.

Maloney, D.

1993-11-01T23:59:59.000Z

278

Hawaiian hot-spot swell structure from seafloor MT sounding Steven Constablea,*, Graham Heinsonb,1  

E-Print Network [OSTI]

Hawaiian hot-spot swell structure from seafloor MT sounding Steven Constablea,*, Graham Heinsonb,1 5348090. E-mail addresses: sconstable@ucsd.edu (S. Constable)8 Graham.Heinson@adelaide.edu.au (G. Heinson

Constable, Steve

279

E-Print Network 3.0 - area mt evidence Sample Search Results  

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

search results for: area mt evidence Page: << < 1 2 3 4 5 > >> 1 University of St Andrews School of Mathematics and Statistics Summary: ;1 HONOURS PROGRAMME IN MATHEMATICS AND...

280

Environment of deposition and reservoir facies of the Taylor "B" Sandstone, Cotton Valley group (Upper Jurassic), Kildare Field, Cass County, Texas  

E-Print Network [OSTI]

amounts of calcite cementation in the sandstones may account for this. Consequently, drill stem tests are used to deter- mine the reservoir quality in the field. Cotton Valley sandstones have been described and interpreted as barrier-bar deposits... Sandstone e absolute open flow rate from drill stem tests in the "B" is 3318 MCFG/0 ( 1019 m /day). Average bottom hole shut-in 3 pressure in the "B" is 4338 psi. A gas-water transition in the Tavlor "8" Kildare Field Kildare field is located...

Black, Cynthia England

1983-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "mt simon sandstone" 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.


281

New anionic states of the lithium trimer Maciej Gutowski') and Jack Simons  

E-Print Network [OSTI]

to the high temperatures necessary to heat the metal and the corrosive properties of lithium.' PhotoelectronNew anionic states of the lithium trimer Maciej Gutowski') and Jack Simons Chemistry Department interaction with single, double, and approximate triple excitations calculations to more accurately determine

Simons, Jack

282

Branching Random Walk in inhomogeneous breeding Sergey Bocharov, Simon C. Harris  

E-Print Network [OSTI]

Branching Random Walk in inhomogeneous breeding potential Sergey Bocharov, Simon C. Harris) If p > 2 then Texplo Harris and S. Harris [7]. Theorem 1.4 (J. Harris and S. Harris). Consider a BBM model. a) If p [0, 2) then lim t Rt t

Harris, Simon Colin

283

Some path large deviation results for a branching diffusion Robert Hardy and Simon C. Harris  

E-Print Network [OSTI]

in Git, J.Harris and S.C.Harris [4]. Our approach involves an application of a change of measureSome path large deviation results for a branching diffusion Robert Hardy and Simon C. Harris of Hardy and Harris [5, 7, 6]. Our proof combines simple martingale ideas with applications of Varadhan

Harris, Simon Colin

284

A new formulation of the spine approach to branching Robert Hardy and Simon C. Harris  

E-Print Network [OSTI]

deviations for a continuous­typed branching di#usion in Git, J.W.Harris and S.C.Harris [8] and HardyA new formulation of the spine approach to branching di#usions Robert Hardy and Simon C. Harris in branching di#usions: see, for example, the L p convergence of additive martingales in Hardy and Harris [12

Harris, Simon Colin

285

Large deviations and martingales for a typed branching diffusion, 1 Simon C Harris and David Williams  

E-Print Network [OSTI]

Large deviations and martingales for a typed branching diffusion, 1 by Simon C Harris and David are rather complicated; and these are only sketched here ­ see Harris (1995) and Harris and Williams (1995 for a simpler problem in Champneys, Harris, Toland, Warren and Williams (1995); in the present context

Harris, Simon Colin

286

A new formulation of the spine approach to branching Robert Hardy and Simon C. Harris  

E-Print Network [OSTI]

deviations for a continuous-typed branching diffusion in Git, J.W.Harris and S.C.Harris [8] and HardyA new formulation of the spine approach to branching diffusions Robert Hardy and Simon C. Harris in branching diffusions: see, for example, the Lp convergence of additive martingales in Hardy and Harris [12

Harris, Simon Colin

287

Random Walk on an Arbitrary Set By Simon C. Harris, Robin Sibson, and  

E-Print Network [OSTI]

Random Walk on an Arbitrary Set By Simon C. Harris, Robin Sibson, and David Williams School be a countably infinite set of points in R, and suppose that I has no points of accumulation and that its convex hull is the whole of R. It will be convenient to index I as {ui : i Z}, with ui

Harris, Simon Colin

288

Branching Brownian Motion with branching at the origin Sergey Bocharov, Simon C. Harris  

E-Print Network [OSTI]

Branching Brownian Motion with branching at the origin Sergey Bocharov, Simon C. Harris University. Dawson and K. Fleischmann [4], K. Fleischmann and J.F. Le Gall [9] or J. Engl¨ander and D. Turaev [7 result is the Strong Law of Large Numbers for the branching system. Theorem 1.7 (SLLN). Let f : R R

Harris, Simon Colin

289

Toward Harnessing User Feedback For Machine Learning Simone Stumpf, Vidya Rajaram, Lida Li, Margaret Burnett,  

E-Print Network [OSTI]

Toward Harnessing User Feedback For Machine Learning Simone Stumpf, Vidya Rajaram, Lida Li University School of Electrical Engineering and Computer Science Corvallis, OR 97331 USA 1 to the learning algorithm. The results show that user feedback has the potential to significantly improve machine

290

RED: a Rich Epinions Dataset for Recommender Systems Simon Meyffret1,2  

E-Print Network [OSTI]

RED: a Rich Epinions Dataset for Recommender Systems Simon Meyffret1,2 , Emmanuel Guillot1}@liris.cnrs.fr ABSTRACT Recommender Systems require specific datasets to evaluate their approach. They do not require is not gathered in today datasets. In this paper, we provide a dataset containing reviews from users on items

Paris-Sud XI, Université de

291

9. Forza e debolezza del governo locale di Tommaso Vitale e Simone Tosi  

E-Print Network [OSTI]

227 9. Forza e debolezza del governo locale di Tommaso Vitale e Simone Tosi 9.1 Quasi un di governo dei soggetti sul territorio. L'inserimento nell'Obbiettivo 2 dei Fondi Strutturali è stato sue successive evoluzioni ­ non hanno pressoché mai rag- giunto posizioni di governo. Anche sul lato

Paris-Sud XI, Université de

292

Action Investment Energy Games Kim G. Larsen, Simon Laursen, and Jiri Srba  

E-Print Network [OSTI]

of action investment energy games where we study the trade-off between investments limited by given budgets energy games where we study the trade-off between investments limited by given budgets and resourceAction Investment Energy Games Kim G. Larsen, Simon Laursen, and Jir´i Srba Aalborg University

Srba, Jiri

293

Exact beta-functions in softly-broken N=2 Chern-Simons matter theories  

E-Print Network [OSTI]

We present exact results for the beta-functions for the soft-breaking parameters in softly-broken N=2 Chern-Simons matter theories in terms of the anomalous dimension in the unbroken theory. We check our results explicitly up to the two loop level.

I. Jack; C. Luckhurst

2011-01-21T23:59:59.000Z

294

Wind power bidding in a soft penalty market Antonio Giannitrapani, Simone Paoletti, Antonio Vicino, Donato Zarrilli  

E-Print Network [OSTI]

Wind power bidding in a soft penalty market Antonio Giannitrapani, Simone Paoletti, Antonio Vicino, Donato Zarrilli Abstract-- In this paper we consider the problem of offering wind power in a market of the prior wind power statistics, is derived analytically by maximizing the expected profit of the wind power

Giannitrapani, Antonello

295

The Limits of ESS Methodology Simon M. Huttegger Kevin J. S. Zollman  

E-Print Network [OSTI]

The Limits of ESS Methodology Simon M. Huttegger Kevin J. S. Zollman December 31, 2010 Abstract of evolutionarily stable strategy (ESS) can tell us about evolutionary processes. We shall argue that ESS is very on refinements of Nash equilibrium. In the first place, ESS can also be viewed as a Nash equilibrium refinement

Zollman, Kevin

296

A Short Cut to Deforestation Andrew Gill John Launchbury Simon L Peyton Jones  

E-Print Network [OSTI]

A Short Cut to Deforestation Andrew Gill John Launchbury Simon L Peyton Jones Department example of just such a transformation is deforestation (Wadler 1990]). Deforestation removes arbitrary]), we know of no mature com- piler that uses deforestation as part of its regular optimisa- tions

Jones, Simon Peyton

297

SIMON FRASER UNIVERSITY Campus Directory General Telephone Information (2/8/13) i  

E-Print Network [OSTI]

SIMON FRASER UNIVERSITY Campus Directory General Telephone Information (2/8/13) i TABLE OF CONTENTS.......................................................................................................................... 5 · Trouble/Repair Calls · Name Changes · Voice Mail Queries · Campus Telephone Directory · Telus...................................................................................................................................... 8 · Long Distance Directory Assistance · Direct Distance Dialing (DDD) · Difficulties Placing Long

298

Hamilton's rule in multi-level selection Burton Simon, Jeffrey A. Fletcher & Michael Doebeli  

E-Print Network [OSTI]

Hamilton's rule in multi-level selection models Burton Simon, Jeffrey A. Fletcher & Michael Doebeli is determined (statistically) by the composi- tion of the parent group. We derive Hamilton-like inequalities ways due to both individual-level and group level processes. Hamilton's rules only contain first

Simon, Burt

299

Hamilton's rule in multi-level selection models Burton Simon a  

E-Print Network [OSTI]

Hamilton's rule in multi-level selection models Burton Simon a , Jeffrey A. Fletcher b , Michael Group selection Partial differential equation a b s t r a c t Hamilton's rule is regarded as a useful. Here we model more realistic situations, in which the traditional Hamilton's rule generally fails

Doebeli, Michael

300

Security Investigations on an Asynchronous PLA Configuration Petros Oikonomakos, Simon Moore  

E-Print Network [OSTI]

Security Investigations on an Asynchronous PLA Configuration Petros Oikonomakos, Simon Moore the potential of using asynchronous PLAs in security applications. For this purpose, we borrow a promising PLA to random logic in VLSI systems [1, 2]. The regularity of a PLA layout makes its timing predictable

Moore, Simon

Note: This page contains sample records for the topic "mt simon sandstone" 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.


301

An Asynchronous PLA with Improved Security Characteristics Petros Oikonomakos, Simon Moore  

E-Print Network [OSTI]

An Asynchronous PLA with Improved Security Characteristics Petros Oikonomakos, Simon Moore to logic-gate based design. We propose the transistor level structure of a PLA for single-rail asynchronous fine-tune the PLA to enhance its resistance to side-channel attacks, while par- ity prediction

Moore, Simon

302

BEaST: Brain Extraction based on nonlocal Segmentation Technique Simon F. Eskildsena,b,  

E-Print Network [OSTI]

BEaST: Brain Extraction based on nonlocal Segmentation Technique Simon F. Eskildsena,b, , PierrickConnell Brain Imaging Centre, Montreal Neurological Institute, McGill University, 3801 University Street Research Centre (DRC), UCL Institute of Neurology, Queens Square, London, WC1N 3BG, UK Abstract ­ Brain

Paris-Sud XI, Université de

303

Bitter to Better --How to Make Bitcoin a Better Currency Simon Barber 1  

E-Print Network [OSTI]

Bitter to Better -- How to Make Bitcoin a Better Currency Simon Barber 1 , Xavier Boyen 1 , Elaine. Bitcoin is a distributed digital currency which has attracted a substan- tial number of users. We perform an in-depth investigation to understand what made Bitcoin so successful, while decades of research

Shi, Elaine

304

Hollywood 3D: Recognizing Actions in 3D Natural Scenes Simon Hadfield Richard Bowden  

E-Print Network [OSTI]

Hollywood 3D: Recognizing Actions in 3D Natural Scenes Simon Hadfield Richard Bowden Centre-class variations. It is made even more challenging when complex 3D actions are projected down to the image plane, losing a great deal of information. The recent emergence of 3D data, both in broadcast content

Bowden, Richard

305

Interactive Translucent Volume Rendering and Procedural Modeling Simon Premoze Charles Hansen  

E-Print Network [OSTI]

Interactive Translucent Volume Rendering and Procedural Modeling Joe Kniss Simon Premoze¡ Charles rendered from a CT scan of a carp. Left: Blinn-Phong shading. Center and right: translucent volume shading. Abstract Direct volume rendering is a commonly used technique in visual- ization applications. Many

Kniss, Joe Michael

306

Interferometric velocity analysis using physical and nonphysical energy Simon King1  

E-Print Network [OSTI]

Interferometric velocity analysis using physical and nonphysical energy Simon King1 , Andrew Curtis as apparent energy that could not have propagated between receiver locations -- so-called nonphysical energy. We have developed a novel method of velocity analysis that uses both the physical and nonphysical

307

Robust control/scheduling co-design: application to robot control Daniel Simon  

E-Print Network [OSTI]

Robust control/scheduling co-design: application to robot control Daniel Simon INRIA Rh of robust closed-loop control can also be ap- plied to the real-time scheduler to provide on-line adap- tion of some scheduling parameters, with the objective of controlling the computing resource allocation

Paris-Sud XI, Université de

308

Pictures: A simple structured graphics model Sigbjorn Finne and Simon Peyton Jones,  

E-Print Network [OSTI]

Pictures: A simple structured graphics model Sigbjorn Finne and Simon Peyton Jones, Department­independent model for de­ scribing two­dimensional graphics using a functional language. Graphical scenes the geometric composition of arbitrary pictures. The structured graphics model presented has been implemented

Jones, Simon Peyton

309

Computational Paradigms and Protection Simon N. Foley and John P. Morrison,  

E-Print Network [OSTI]

Computational Paradigms and Protection Simon N. Foley and John P. Morrison, Department of Computer Science, University College, Cork, Ireland. fs.foley,j.morrisong@cs.ucc.ie Categories and Subject Descriptors D.4.6 [Security and Protection]: Access Controls; D.1 [Programming Techniques]: General; F.1

Foley, Simon

310

DAMAGE DETECTION IN A WIND TURBINE BLADE BASED ON TIME SERIES Simon Hoell, Piotr Omenzetter  

E-Print Network [OSTI]

DAMAGE DETECTION IN A WIND TURBINE BLADE BASED ON TIME SERIES METHODS Simon Hoell, Piotr Omenzetter, the consequences are growing sizes of wind turbines (WTs) and erections in remote places, such as off in the past years, thus efficient energy harvesting becomes more important. For the sector of wind energy

Boyer, Edmond

311

Simon Fraser University's School for International Studies invites you to a free public lecture  

E-Print Network [OSTI]

, and opinions on the questions above, and more generally on the course of economic policy reform in India since to a free public lecture India at the Crossroads: The Meaning of Modi's Victory By Dr. Vivek Dehejia Tuesday, September 23, 2014 17:00 Policy Room 4400 Simon Fraser University, Segal Building 500 Granville Street

312

Evaluating the options for carbon sequestration Clair Gough and Simon Shackley  

E-Print Network [OSTI]

Evaluating the options for carbon sequestration Clair Gough and Simon Shackley Tyndall Centre for carbon sequestration Tyndall Centre Technical Report No. 2 November 2002 This is the final report from Tyndall research project IT1.22 (Carbon sequestration: a pilot stage multi-criteria evaluation

Watson, Andrew

313

Telehealth using ECG Sensor and Accelerometer Hristijan Gjoreski*, Aleksandra Rashkovska**, Simon Kozina*, Mitja Lustrek*, Matjaz Gams*,  

E-Print Network [OSTI]

Telehealth using ECG Sensor and Accelerometer Hristijan Gjoreski*, Aleksandra Rashkovska**, Simon are important components of such systems. Moreover, the monitoring of vital signs, like the ECG, has a key role by combining an ECG sensor and two accelerometers. Our system recognizes the user's activities and detects

LuÂ?trek, Mitja

314

Detectable Changes in the Frequency of Temperature Extremes SIMONE MORAK AND GABRIELE C. HEGERL  

E-Print Network [OSTI]

Detectable Changes in the Frequency of Temperature Extremes SIMONE MORAK AND GABRIELE C. HEGERL of hot and cold extremes over land can be explained by climate variability or whether they show a detectable response to external influences. The authors analyze changes in the frequency of moderate-to-extreme

Hegerl, Gabriele Clarissa "Gabi"

315

Depositional patterns and reservoir morphology of Guadalupian Cherry Canyon sandstones, Indian Draw Field, Eddy County, New Mexico  

E-Print Network [OSTI]

shown in Fig. 29 119 Isopach of final channel-fill showing the highly sinuous geometry of the thinly interbedded sandstones siltstones and shales. Contour interval 5 ft (1. 5 m). . 121 44 Diagrammatic cross section illustrating the size, shape... at depths ranging from. 3200 to 3350 ft (975 to 1020 m). These reservoir sand- stones occur interbedded with limestones, siltstones and thin shales, and were deposited approximately 10 mi (16 km) downdip from the Guadalupian reef front in the Delaware...

Phillips, Sandra

1981-01-01T23:59:59.000Z

316

Determination of foraminiferal criteria for environmental interpretation using Upper Cretaceous sandstones, Brazos, Frio, Walker, and Zavala counties, Texas  

E-Print Network [OSTI]

of the Amalga- mated Bonanza Smith 2 and a basinal depositional en- vironment for the shale of the Morgan Central Coal and Coke, G-4 Wildcat 7) Few tests were recovered from the sediments of the Amalgamated Bonanza Smith 2 and the Norgan Central Coal... Johnson 3-Sand Niguel Sandstone Amalgamated Bonanza Smith 2-Woodbine Sand- stone ~ ~ ~ ~ Morgan Central Coal & Coke, G-4 Wildcat- Woodbine Shale Norgan Central Coal & Coke, G-4 wildcat- Georgetown Limestone Morgan Central Coal & Coke, G-4 Wildcat...

Nufer, Janet Ann

2012-06-07T23:59:59.000Z

317

Environment of deposition and reservoir properties of Teapot sandstones (Upper Cretaceous), Well Draw field, Converse County, Wyoming  

E-Print Network [OSTI]

= monocrystalline quartz, F = feldspar, Rx = rock fragments including chert, micas, and polycrystalline quartz, Mx = maxtrix, and 0th = other minerals. c Sil = silica as grain overgrowths including minor chert, Cal = calcite including minor dolomite and siderite... fossils, and reservoir morphology. Three distinct sandstone facies produce oil and gas at Well Draw field. The main producing zone consists of thicker, channel turbidites. The lower two zones are thinly interbedded with shale and have limited reservoir...

Sullivan, John Joseph

1982-01-01T23:59:59.000Z

318

Environment of deposition and reservoir characteristics of Lower Pennsylvanian Morrowan sandstones, South Empire field area, Eddy County, New Mexico  

E-Print Network [OSTI]

New Mexico. The Lower and Middle Morrow intervals in the South Empire field area consist of stacked, fluvial to deltaic sandstones that are interbedded with thin limestones. An understanding of the complex, interfingering relation- ships... of the Tobosa basin, the thinning of Ordovician sediments suggests the initiation of uplift on the Diablo Platform. A period of quiescence punctuated by episodes of regional uplift existed from the late Ordovician to the late Devonian-early Mississ- ippian...

Lambert, Rebecca Bailey

1986-01-01T23:59:59.000Z

319

Evaluation of the Berea sandstone formation in eastern Pike County, Kentucky  

SciTech Connect (OSTI)

The Gas Research Institute (GRI) has been sponsoring a cooperative well program with Ashland Exploration, Inc., (AEI) during the past two years targeting the Devonian Shale and Berea sandstone formations in Pike County of eastern Kentucky. Operators typically complete both the shales and Berea in one well bore in this area. This presentation summarizes the research results of the Berea cooperative well, the COOP 2 (Ashland FMC 80). The specific objectives of the Berea evaluation in the COOP 2 were to develop an integrated reservoir description for stimulation design and predicting long-term well performance, identify geologic production controls, determine the in-situ stress profile, and develop Berea log interpretation models for gas porosity and stress. To satisfy these objectives, data were collected and analyzed from 146 ft of whole core, open-hole geophysical logs, including formation microscanner and digital sonic, in-situ stress measurements, and prefracture production and pressure transient tests. In addition, data from a minifracture, a fracture stimulation treatment, and postfracture performance tests were analyzed. The authors determined the integrated reservoir/hydraulic fracture descriptions from analyzing the data collected in the open- and cased-hole, in addition to the log interpretation models developed to accurately predict gas porosity and stress profiles. Results can be applied by operators to better understand the Berea reservoir in the study area, predict well performance, and design completion procedures and stimulation treatments. The methodology can also be applied to other tight-gas sand formations.

Frantz, J.H. Jr. (S.A. Holditch Associates, Inc., Pittsburgh, PA (United States)); Luffel, D. (ResTech Houston, Inc., Houston, TX (United States)); Kubik, W. (K A Energy Consultants, Tulsa, OK (United States))

1993-08-01T23:59:59.000Z

320

Using X-Ray Computed Tomography in Pore Structure Characterization for a Berea Sandstone: Resolution Effect  

SciTech Connect (OSTI)

X-raycomputedtomography (XCT) is a powerful tool for detecting the micro-scale porestructure and has been applied to many natural and synthetic porous media. However, due to the resolution limitations, either non-representative view of the sample or inaccurate results can be produced from the XCT image processing. In this paper, two XCT (micro-CT and CT with synchrotron radiation) with different resolutions of 12.7 ?m and 0.35 ?m, as well as mercury intrusion porosimetry (MIP) with a minimum detection limit of 3 nm, were used for Berea sandstone to investigate the effect of detecting resolution on the porestructure. Several key porestructure parameters, including porosity, pore size distribution, pore connectivity, surface area, hydraulic radius, and aspect ratio were analyzed in a manner of quantitative comparison between different resolutions of XCT and MIP. The low resolution XCT can capture the large-pore porosity, while overestimates the pore size and pore connectivity. The high resolution XCT is more accurate in describing the pore shape, porosity, pore size; however, it is not representative since narrower detecting pore size range and small volume represented. A representative element volume related to large-pore porosity and probably large-pore connectivity with diameter and height of 2.8 mm is obtained through scale effect analysis. Therefore, selecting an appropriate resolution should be a compromise between the pore size and the representative element volume for the specific property or process of interest.

Peng, Sheng; Hu, Qinhong; Dultz, Stefan; Zhang, Ming

2012-11-23T23:59:59.000Z

Note: This page contains sample records for the topic "mt simon sandstone" 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.


321

Geologic reservoir characterization of Humphreys sandstone (Pennsylvanian), east Velma field, Oklahoma  

SciTech Connect (OSTI)

East Velma field is located in the Ardmore basin, Stephens County, Oklahoma, on the north flank of a truncated anticline with dips that range from 30/degrees/-60/degrees/. The discovery well of the Humphreys sand unit was drilled in April 1951 and an original oil in place of 32.7 million bbl was calculated. Primary depletion was by solution gas drive with gas reinjection and gravity drainage which was enhanced by the steep structural dip of the field. A waterflood that was initiated in 1983 and a proposed CO/sub 2/ miscible displacement program to further enhance field recovery prompted the need to develop a detailed geologic description of the reservoir. Core studies indicate that the Humphreys sandstone was deposited in a shallow marine, tidally dominated environment. Subfacies include sand-rich tidal flat and tidal channel deposits. The unit is primarily composed of very fine to fine-grained, moderately to well-sorted quartzarenites. Dominant sedimentary structures include bidirectional and unidirectional current ripples, cross-laminations, common slump structures, and zones abundant and scattered burrows.

McGowen, M.K.

1988-02-01T23:59:59.000Z

322

Simone GilardoniNufact03 7/06/2003 Horn R&D for 2002-2003  

E-Print Network [OSTI]

-like: ­ Normally 1-2 interaction lengths · Order 20-30 cm for heavy targets (Hg) · Particle produced with large · Power supply for Test One: 30 kA and 1 Hz, pulse 100 µs long First mechanical measurements Test and water connections #12;Simone GilardoniNufact03 7/06/2003 Inside the neck 5.6 cm #12;Simone Gilardoni

McDonald, Kirk

323

Injection of CO2 with H2S and SO2 and Subsequent Mineral Trapping in Sandstone-Shale Formation  

SciTech Connect (OSTI)

Carbon dioxide (CO{sub 2}) injection into deep geologic formations can potentially reduce atmospheric emissions of greenhouse gases. Sequestering less-pure CO{sub 2} waste streams (containing H{sub 2}S and/or SO{sub 2}) would be less expensive or would require less energy than separating CO{sub 2} from flue gas or a coal gasification process. The long-term interaction of these injected acid gases with shale-confining layers of a sandstone injection zone has not been well investigated. We therefore have developed a conceptual model of injection of CO{sub 2} with H{sub 2}S and/or SO{sub 2} into a sandstone-shale sequence, using hydrogeologic properties and mineral compositions commonly encountered in Gulf Coast sediments of the United States. We have performed numerical simulations of a 1-D radial well region considering sandstone alone and a 2-D model using a sandstone-shale sequence under acid-gas injection conditions. Results indicate that shale plays a limited role in mineral alteration and sequestration of gases within a sandstone horizon for short time periods (10,000 years in present simulations). The co-injection of SO{sub 2} results in different pH distribution, mineral alteration patterns, and CO{sub 2} mineral sequestration than the co-injection of H{sub 2}S or injection of CO{sub 2} alone. Simulations generate a zonal distribution of mineral alteration and formation of carbon and sulfur trapping minerals that depends on the pH distribution. The co-injection of SO{sub 2} results in a larger and stronger acidified zone close to the well. Precipitation of carbon trapping minerals occurs within the higher pH regions beyond the acidified zones. In contrast, sulfur trapping minerals are stable at low pH ranges (below 5) within the front of the acidified zone. Corrosion and well abandonment due to the co-injection of SO{sub 2} could be important issues. Significant CO{sub 2} is sequestered in ankerite and dawsonite, and some in siderite. The CO{sub 2} mineral-trapping capability can reach 80 kg per cubic meter of medium. Most sulfur is trapped through alunite precipitation, although some is trapped by anhydrite precipitation and minor amount of pyrite. The addition of the acid gases and induced mineral alteration result in changes in porosity. The limited information currently available on the mineralogy of natural high-pressure acid-gas reservoirs is generally consistent with our simulations.

Xu, Tianfu; Apps, John A.; Pruess, Karsten; Yamamoto, Hajime

2004-09-07T23:59:59.000Z

324

Null geodesics and shadow of a rotating black hole in extended Chern-Simons modified gravity  

SciTech Connect (OSTI)

The Chern-Simons modification to general relativity in four dimensions consists of adding to the Einstein-Hilbert term a scalar field that couples to the first-class Pontryagin density. In this theory, which has attracted considerable attention recently, the Schwarzschild metric persists as an exact solution, and this is why this model resists several observational constraints. In contrast, the spinning black hole solution of the theory is not given by the Kerr metric but by a modification of it, so far only known for slow rotation and small coupling constant. In the present paper, we show that, in this approximation, the null geodesic equation can be integrated, and this allows us to investigate the shadow cast by a black hole. We discuss how, in addition to the angular momentum of the solution, the coupling to the Chern-Simons term deforms the shape of the shadow.

Amarilla, Leonardo [Facultad de Ciencias Astronomicas y Geofisicas, Universidad Nacional de La Plata, Paseo del Bosque, 1900, La Plata (Argentina); Departamento de Fisica, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellon 1, 1428, Buenos Aires (Argentina); Eiroa, Ernesto F. [Instituto de Astronomia y Fisica del Espacio, C.C. 67 Suc. 28, 1428, Buenos Aires (Argentina); Departamento de Fisica, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellon 1, 1428, Buenos Aires (Argentina); Giribet, Gaston [Departamento de Fisica, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellon 1, 1428, Buenos Aires (Argentina)

2010-06-15T23:59:59.000Z

325

Random Walk on an Arbitrary Set By Simon C. Harris, Robin Sibson, and  

E-Print Network [OSTI]

j 6=i q i;j (u j u i ) = 0 for every i: (1:1) Write ` i and r i for the gaps to the leftRandom Walk on an Arbitrary Set By Simon C. Harris, Robin Sibson, and David Williams School be a countably in#12;nite set of points in R, and suppose that I has no points of accumulation and that its

Harris, Simon Colin

326

Study on fine geological modelling of the fluvial sandstone reservoir in Daqing oilfield  

SciTech Connect (OSTI)

These paper aims at developing a method for fine reservoir description in maturing oilfields by using close spaced well logging data. The main productive reservoirs in Daqing oilfield is a set of large fluvial-deltaic deposits in the Songliao Lake Basin, characterized by multi-layers and serious heterogeneities. Various fluvial channel sandstone reservoirs cover a fairly important proportion of reserves. After a long period of water flooding, most of them have turned into high water cut layers, but there are considerable residual reserves within them, which are difficult to find and tap. Making fine reservoir description and developing sound a geological model is essential for tapping residual oil and enhancing oil recovery. The principal reason for relative lower precision of predicting model developed by using geostatistics is incomplete recognition of complex distribution of fluvial reservoirs and their internal architecture`s. Tasking advantage of limited outcrop data from other regions (suppose no outcrop data available in oilfield) can only provide the knowledge of subtle changing of reservoir parameters and internal architecture. For the specific geometry distribution and internal architecture of subsurface reservoirs (such as in produced regions) can be gained only from continuous infilling logging well data available from studied areas. For developing a geological model, we think the first important thing is to characterize sandbodies geometries and their general architecture`s, which are the framework of models, and then the slight changing of interwell parameters and internal architecture`s, which are the contents and cells of the model. An excellent model should possess both of them, but the geometry is the key to model, because it controls the contents and cells distribution within a model.

Zhoa Han-Qing [Daqing Research Institute, Helongjiang (China)

1997-08-01T23:59:59.000Z

327

Protected qubits and Chern-Simons theories in Josephson junction arrays  

SciTech Connect (OSTI)

We present general symmetry arguments that show the appearance of doubly degenerate states protected from external perturbations in a wide class of Hamiltonians. We construct the simplest spin Hamiltonian belonging to this class and study its properties both analytically and numerically. We find that this model generally has a number of low energy modes which might destroy the protection in the thermodynamic limit. These modes are qualitatively different from the usual gapless excitations as their number scales as the linear size (instead of volume) of the system. We show that the Hamiltonians with this symmetry can be physically implemented in Josephson junction arrays and that in these arrays one can eliminate the low energy modes with a proper boundary condition. We argue that these arrays provide fault tolerant quantum bits. Further we show that the simplest spin model with this symmetry can be mapped to a very special Z{sub 2} Chern-Simons model on the square lattice. We argue that appearance of the low energy modes and the protected degeneracy is a natural property of lattice Chern-Simons theories. Finally, we discuss a general formalism for the construction of discrete Chern-Simons theories on a lattice.

Doucot, B. [Laboratoire de Physique Theorique et Hautes Energies, CNRS UMR 7589, Universites Paris 6 et 7, 4, place Jussieu, 75252 Paris Cedex 05 (France); Feigel'man, M.V.; Ioselevich, A.S. [Landau Institute for Theoretical Physics, Kosygina 2, Moscow, 117940 (Russian Federation); Ioffe, L.B. [Department of Physics and Astronomy, Center for Materials Theory, Rutgers University, 136 Frelinghuysen Road, Piscataway, New Jersey 08854 (United States)

2005-01-01T23:59:59.000Z

328

Sequence and annotation of the 314-kb MT325 and the 321-kb FR483 viruses that infect Chlorella Pbi  

E-Print Network [OSTI]

Sequence and annotation of the 314-kb MT325 and the 321-kb FR483 viruses that infect Chlorella Pbi of the family Phycodnaviridae, genus Chlorovirus, infect the fresh water, unicellular, eukaryotic, chlorella-like green alga, Chlorella Pbi. The 314,335-bp genome of MT325 and the 321,240-bp genome of FR483

Graves, Michael V.

329

PARTICLE FILTER WITH EFFICIENT IMPORTANCE SAMPLING AND MODE TRACKING (PF-EIS-MT) AND ITS APPLICATION TO LANDMARK SHAPE TRACKING  

E-Print Network [OSTI]

PARTICLE FILTER WITH EFFICIENT IMPORTANCE SAMPLING AND MODE TRACKING (PF-EIS-MT) AND ITS a practically implementable particle filtering (PF) method called "PF-EIS-MT" for tracking on large dimensional dimensions and (b) direct application of PF requires an impractically large number of particles. PF-EIS

Vaswani, Namrata

330

Altered Mitochondrial Retrograde Signaling in Response to mtDNA Depletion or a Ketogenic Diet  

E-Print Network [OSTI]

kinase kinase MCI Mild cognitive impairment MCT Monocarboxylate transporter Mfn Mitofusin mtDNA Mitochondrial DNA mTOR Mammalian target of rapamycin mTORC1 mTOR complex 1 MRC Mitochondrial Respiratory Complex NAD(H) Nicotinamide adenine...

Selfridge, Jennifer Eva

2012-12-31T23:59:59.000Z

331

Behavioral/Systems/Cognitive Receptive Field Positions in Area MT during Slow Eye  

E-Print Network [OSTI]

Behavioral/Systems/Cognitive Receptive Field Positions in Area MT during Slow Eye Movements Till S across eye movements. We first tested the hypothesis that motion signals are integrated by neurons whose receptive fields (RFs) do not move with the eye but stay fixed in the world. Specifically, we measured

Krekelberg, Bart

332

M.-T. DO, P. MARSAC, Y. DELANNE Prediction of Tire/Wet Road Friction from  

E-Print Network [OSTI]

M.-T. DO, P. MARSAC, Y. DELANNE 1 Prediction of Tire/Wet Road Friction from Road Surface, validation of a contact model for the prediction of low-speed friction from road surface microtexture the friction ­ speed curve from road- and tire measurable parameters. The model development is briefly

Paris-Sud XI, Université de

333

Going Beyond AER: An Extensive Analysis of Word Alignments and Their Impact on MT  

E-Print Network [OSTI]

Going Beyond AER: An Extensive Analysis of Word Alignments and Their Impact on MT Necip Fazil Ayan (AER)--attempts to balance the precision and recall scores at the level of alignment links (Och and Ney et al., 2002) or METEOR (Banerjee and Lavie, 2005)). However, these studies showed that AER and BLEU

Ayan, Necip Fazil

334

Abrupt contraction flow of magnetorheological fluids , M.T. Lpez-Lpez1,2  

E-Print Network [OSTI]

engineering interest, the MR fluids are very attractive from a purely scientific point of view. The coupling1 Abrupt contraction flow of magnetorheological fluids P. Kuzhir1 , M.T. López-López1,2 and G Granada, 18071 Granada, Spain Abstract Contraction and expansion flows of magnetorheological fluids occur

Boyer, Edmond

335

MSU Human Resources 19 Montana Hall ~ PO Box 172520 ~ Bozeman, MT 59717-2520  

E-Print Network [OSTI]

MSU Human Resources 19 Montana Hall ~ PO Box 172520 ~ Bozeman, MT 59717-2520 Tel (406) 994 with the Social Security Administration and State policies, the Human Resources procedure for Name and Address changes has been modified. The Human Resources Department uses two separate forms ­ one for name changes

Dyer, Bill

336

Analysis of Critical Permeabilty, Capillary Pressure and Electrical Properties for Mesaverde Tight Gas Sandstones from Western U.S. Basins  

SciTech Connect (OSTI)

Although prediction of future natural gas supply is complicated by uncertainty in such variables as demand, liquefied natural gas supply price and availability, coalbed methane and gas shale development rate, and pipeline availability, all U.S. Energy Information Administration gas supply estimates to date have predicted that Unconventional gas sources will be the dominant source of U.S. natural gas supply for at least the next two decades (Fig. 1.1; the period of estimation). Among the Unconventional gas supply sources, Tight Gas Sandstones (TGS) will represent 50-70% of the Unconventional gas supply in this time period (Fig. 1.2). Rocky Mountain TGS are estimated to be approximately 70% of the total TGS resource base (USEIA, 2005) and the Mesaverde Group (Mesaverde) sandstones represent the principal gas productive sandstone unit in the largest Western U.S. TGS basins including the basins that are the focus of this study (Washakie, Uinta, Piceance, northern Greater Green River, Wind River, Powder River). Industry assessment of the regional gas resource, projection of future gas supply, and exploration programs require an understanding of reservoir properties and accurate tools for formation evaluation. The goal of this study is to provide petrophysical formation evaluation tools related to relative permeability, capillary pressure, electrical properties and algorithms for wireline log analysis. Detailed and accurate moveable gas-in-place resource assessment is most critical in marginal gas plays and there is need for quantitative tools for definition of limits on gas producibility due to technology and rock physics and for defining water saturation. The results of this study address fundamental questions concerning: (1) gas storage; (2) gas flow; (3) capillary pressure; (4) electrical properties; (5) facies and upscaling issues; (6) wireline log interpretation algorithms; and (7) providing a web-accessible database of advanced rock properties. The following text briefly discusses the nature of these questions. Section I.2 briefly discusses the objective of the study with respect to the problems reviewed.

Alan Byrnes; Robert Cluff; John Webb; John Victorine; Ken Stalder; Daniel Osburn; Andrew Knoderer; Owen Metheny; Troy Hommertzheim; Joshua Byrnes; Daniel Krygowski; Stefani Whittaker

2008-06-30T23:59:59.000Z

337

Measuring and predicting reservoir heterogeneity in complex deposystems: The fluvial-deltaic Big Injun sandstone in West Virginia  

SciTech Connect (OSTI)

The purpose of this research is to develop techniques to measure and predict heterogeneities in oil reservoirs that are the products of complex deposystems. The unit chosen for study is the Lower Mississippian Big Injun sandstone, a prolific oil producer (nearly 60 fields) in West Virginia. This research effort has been designed and is being implemented as an integrated effort involving stratigraphy, structural geology, petrology, seismic study, petroleum engineering, modeling and geostatistics. Sandstone bodies are being mapped within their regional depositional systems, and then sandstone bodies are being classified in a scheme of relative heterogeneity to determine heterogeneity across depositional systems. Facies changes are being mapped within given reservoirs, and the environments of deposition responsible for each facies are being interpreted to predict the inherent relative heterogeneity of each facies. Structural variations will be correlated both with production, where the availability of production data will permit, and with variations in geologic and engineering parameters that affect production. A reliable seismic model of the Big Injun reservoirs in Granny Creek field is being developed to help interpret physical heterogeneity in that field. Pore types are being described and related to permeability, fluid flow and diagenesis, and petrographic data are being integrated with facies and depositional environments to develop a technique to use diagenesis as a predictive tool in future reservoir development. Another objective in the Big Injun study is to determine the effect of heterogeneity on fluid flow and efficient hydrocarbon recovery in order to improve reservoir management. Graphical methods will be applied to Big Injun production data and new geostatistical methods will be developed to detect regional trends in heterogeneity.

Patchen, D.G.; Hohn, M.E.; Aminian, K.; Donaldson, A.; Shumaker, R.; Wilson, T.

1993-04-01T23:59:59.000Z

338

Evaluating impacts of CO2 gas intrusion into a confined sandstone aquifer: Experimental results  

SciTech Connect (OSTI)

Deep subsurface storage and sequestration of CO2 has been identified as a potential mitigation technique for rising atmospheric CO2 concentrations. Sequestered CO2 represents a potential risk to overlying aquifers if the CO2 leaks from the deep storage reservoir. Experimental and modeling work is required to evaluate potential risks to groundwater quality and develop a systematic understanding of how CO2 leakage may cause important changes in aquifer chemistry and mineralogy by promoting dissolution/precipitation, adsorption/desorption, and redox reactions. Sediments from the High Plains aquifer in Kansas, United States, were used in this investigation, which is part of the National Risk Assessment Partnership Program sponsored by the US Department of Energy. This aquifer was selected to be representative of consolidated sand and gravel/sandstone aquifers overlying potential CO2 sequestration repositories within the continental US. In this paper, we present results from batch experiments conducted at room temperature and atmospheric pressure with four High Plains aquifer sediments. Batch experiments simulate sudden, fast, and short-lived releases of the CO2 gas as would occur in the case of well failure during injection. Time-dependent release of major, minor, and trace elements were determined by analyzing the contacting solutions. Characterization studies demonstrated that the High Plains aquifer sediments were abundant in quartz and feldspars, and contained about 15 to 20 wt% montmorillonite and up to 5 wt% micas. Some of the High Plains aquifer sediments contained no calcite, while others had up to about 7 wt% calcite. The strong acid extraction tests confirmed that in addition to the usual elements present in most soils, rocks, and sediments, the High Plains aquifer sediments had appreciable amounts of As, Cd, Pb, Cu, and occasionally Zn, which potentially may be mobilized from the solid to the aqueous phase during or after exposure to CO2. However, the results from the batch experiments showed that the High Plains sediments mobilized only low concentrations of trace elements (potential contaminants), which were detected occasionally in the aqueous phase during these experiments. Importantly, these occurrences were more frequent in the calcite-free sediment. Results from these investigations provide useful information to support site selection, risk assessment, and public education efforts associated with geological CO2 storage and sequestration.

Qafoku, Nikolla; Lawter, Amanda R.; Shao, Hongbo; Wang, Guohui; Brown, Christopher F.

2014-12-31T23:59:59.000Z

339

Anisotropy and Spatial Variation of Relative Permeability and Lithologic Character of Tensleep Sandstone Reservoirs in the Bighorn and Wind River Basins, Wyoming  

SciTech Connect (OSTI)

This multidisciplinary study is designed to provide improvements in advanced reservoir characterization techniques. This goal is to be accomplished through: (1) an examination of the spatial variation and anisotropy of relative permeability in the Tensleep Sandstone reservoirs of Wyoming; (2) the placement of that variation and anisotropy into paleogeographic, depositional, and diagenetic frameworks; (3) the development of pore-system imagery techniques for the calculation of relative permeability; (4) reservoir simulations testing the impact of relative permeability anisotropy and spatial variation on Tensleep Sandstone reservoir enhanced oil recovery; and (5) a geochemical investigation of the spatial and dynamic alteration in sandstone reservoirs that is caused by rock-fluid interaction during CO{sub 2}-enhanced oil recovery processes.

Dunn, Thomas L.

1996-10-01T23:59:59.000Z

340

SIMON FRASER UNIVERSITY Campus Directory Unless otherwise indicated use 778-782 and the last four digits listed when calling from off campus  

E-Print Network [OSTI]

SIMON FRASER UNIVERSITY Campus Directory Unless otherwise indicated use 778-782 and the last four the bottom of the page click on "Contact Us" under the DIRECTORIES heading click on "Campus Email Directory & Administrative Assistant 27029 #12;SIMON FRASER UNIVERSITY Campus Directory Unless otherwise indicated use 778

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341

PHYS 390 Lecture 20 -Reactions III -Thermonuclear processes 20 -1 2001 by David Boal, Simon Fraser University. All rights reserved; further resale or copying is strictly prohibited.  

E-Print Network [OSTI]

PHYS 390 Lecture 20 - Reactions III - Thermonuclear processes 20 - 1 © 2001 by David Boal, Simon - Reactions III - Thermonuclear processes What's Important: · energy-dependent cross sections · complete rate 20 - Reactions III - Thermonuclear processes 20 - 2 © 2001 by David Boal, Simon Fraser University

Boal, David

342

A Review of "The Emblem in Scandinavia and the Baltic" by Simon McKeown, and "Emblematic Paintings from Sweden's Age of Greatness. Nils Bielke and the Neo-Stoic Gallery at Skokloster" by Simon McKeown  

E-Print Network [OSTI]

reviews 185 The Emblem in Scandinavia and the Baltic. Ed. Simon McKeown and Mara R. Wade. Glasgow: Glasgow Emblem Studies 11, 2006. xxvi + 340 pp. + illus. ? 21.99. Simon McKeown, Emblematic Paintings from Sweden?s Age of Greatness. Nils...- and early eighteenth centuries, but the Danish and Swedish realms were geographically vast, and the rise of Sweden as a European great power extraordinary. The cultural influx in Scandinavia was strong and quick, and it is interesting to reflect on how...

Burman, Lars

2009-01-01T23:59:59.000Z

343

Predictive modeling of CO{sub 2} sequestration in deep saline sandstone reservoirs: Impacts of geochemical kinetics  

SciTech Connect (OSTI)

One idea for mitigating the increase in fossil-fuel generated CO{sub 2} in the atmosphere is to inject CO{sub 2} into subsurface saline sandstone reservoirs. To decide whether to try such sequestration at a globally significant scale will require the ability to predict the fate of injected CO{sub 2}. Thus, models are needed to predict the rates and extents of subsurface rock-water-gas interactions. Several reactive transport models for CO{sub 2} sequestration created in the last decade predicted sequestration in sandstone reservoirs of ~17 to ~90 kg CO{sub 2} m{sup -3|. To build confidence in such models, a baseline problem including rock + water chemistry is proposed as the basis for future modeling so that both the models and the parameterizations can be compared systematically. In addition, a reactive diffusion model is used to investigate the fate of injected supercritical CO{sub 2} fluid in the proposed baseline reservoir + brine system. In the baseline problem, injected CO{sub 2} is redistributed from the supercritical (SC) free phase by dissolution into pore brine and by formation of carbonates in the sandstone. The numerical transport model incorporates a full kinetic description of mineral-water reactions under the assumption that transport is by diffusion only. Sensitivity tests were also run to understand which mineral kinetics reactions are important for CO{sub 2} trapping. The diffusion transport model shows that for the first ~20 years after CO{sub 2} diffusion initiates, CO{sub 2} is mostly consumed by dissolution into the brine to form CO{sub 2,aq} (solubility trapping). From 20-200 years, both solubility and mineral trapping are important as calcite precipitation is driven by dissolution of oligoclase. From 200 to 1000 years, mineral trapping is the most important sequestration mechanism, as smectite dissolves and calcite precipitates. Beyond 2000 years, most trapping is due to formation of aqueous HCO{sub 3}{sup -}. Ninety-seven percent of the maximum CO{sub 2} sequestration, 34.5 kg CO{sub 2} per m{sup 3} of sandstone, is attained by 4000 years even though the system does not achieve chemical equilibrium until ~25,000 years. This maximum represents about 20% CO{sub 2} dissolved as CO{sub 2},aq, 50% dissolved as HCO{sub 3}{sup -}{sub ,aq}, and 30% precipitated as calcite. The extent of sequestration as HCO{sub 3}{sup -} at equilibrium can be calculated from equilibrium thermodynamics and is roughly equivalent to the amount of Na+ in the initial sandstone in a soluble mineral (here, oligoclase). Similarly, the extent of trapping in calcite is determined by the amount of Ca2+ in the initial oligoclase and smectite. Sensitivity analyses show that the rate of CO{sub 2} sequestration is sensitive to the mineral-water reaction kinetic constants between approximately 10 and 4000 years. The sensitivity of CO{sub 2} sequestration to the rate constants decreases in magnitude respectively from oligoclase to albite to smectite.

Balashov, Victor N.; Guthrie, George D.; Hakala, J. Alexandra; Lopano, Christina L. J.; Rimstidt, Donald; Brantley, Susan L.

2013-03-01T23:59:59.000Z

344

From Doubled Chern-Simons-Maxwell Lattice Gauge Theory to Extensions of the Toric Code  

E-Print Network [OSTI]

We regularize compact and non-compact Abelian Chern-Simons-Maxwell theories on a spatial lattice using the Hamiltonian formulation. We consider a doubled theory with gauge fields living on a lattice and its dual lattice. The Hilbert space of the theory is a product of local Hilbert spaces, each associated with a link and the corresponding dual link. The two electric field operators associated with the link-pair do not commute. In the non-compact case with gauge group $\\mathbb{R}$, each local Hilbert space is analogous to the one of a charged "particle" moving in the link-pair group space $\\mathbb{R}^2$ in a constant "magnetic" background field. In the compact case, the link-pair group space is a torus $U(1)^2$ threaded by $k$ units of quantized "magnetic" flux, with $k$ being the level of the Chern-Simons theory. The holonomies of the torus $U(1)^2$ give rise to two self-adjoint extension parameters, which form two non-dynamical background lattice gauge fields that explicitly break the manifest gauge symmetry from $U(1)$ to $\\mathbb{Z}(k)$. The local Hilbert space of a link-pair then decomposes into representations of a magnetic translation group. In the pure Chern-Simons limit of a large "photon" mass, this results in a $\\mathbb{Z}(k)$-symmetric variant of Kitaev's toric code, self-adjointly extended by the two non-dynamical background lattice gauge fields. Electric charges on the original lattice and on the dual lattice obey mutually anyonic statistics with the statistics angle $\\frac{2 \\pi}{k}$. Non-Abelian $U(k)$ Berry gauge fields that arise from the self-adjoint extension parameters may be interesting in the context of quantum information processing.

T. Z. Olesen; N. D. Vlasii; U. -J. Wiese

2015-03-24T23:59:59.000Z

345

Induced Spin from the $ISO(2,1)$ Gauge Theory with the Gravitational Chern-Simons Term  

E-Print Network [OSTI]

In the context of $ISO(2,1)$ gauge theory, we consider $(2+1)$-dimensional gravity with the gravitational Chern-Simons term (CST). This formulation allows the `exact' solution for the system coupled to a massive point particle (which is not the case in the conventional Chern-Simons gravity). The solution exhibits locally trivial structure even with the CST, although still shows globally nontrivialness such as the conical space and the helical time structure. Since the solution is exact, we can say the CST induces spin even for noncritical case of $\\s+\\al m\

Jin-Ho Cho; Hyuk-jae Lee

1995-06-07T23:59:59.000Z

346

Holographic Dark Energy Models and Higher Order Generalizations in Dynamical Chern-Simons Modified Gravity  

E-Print Network [OSTI]

Dark Energy models are here investigated and studied in the framework of the Chern-Simons modified gravity model. We bring into focus the Holographic Dark Energy (HDE) model with Granda-Oliveros cut-off, the Modified Holographic Ricci Dark Energy (MHRDE) model and, moreover, a model with higher derivatives of the Hubble parameter as well. The relevant expressions of the scale factor a(t) for a Friedmann-Robertson-Walker Universe are derived and studied, and in this context, the evolution of the scale factor is shown to be similar to that one displayed by the modified Chaplygin gas in two of the above models.

Antonio Pasqua; Roldao da Rocha; Surajit Chattopadhyay

2014-12-29T23:59:59.000Z

347

Wilcox sandstone reservoirs in the deep subsurface along the Texas Gulf Coast: their potential for production of geopressured geothermal energy. Report of Investigations No. 117  

SciTech Connect (OSTI)

Regional studies of the lower Eocene Wilcox Group in Texas were conducted to assess the potential for producing heat energy and solution methane from geopressured fluids in the deep-subsurface growth-faulted zone. However, in addition to assembling the necessary data for the geopressured geothermal project, this study has provided regional information of significance to exploration for other resources such as lignite, uranium, oil, and gas. Because the focus of this study was on the geopressured section, emphasis was placed on correlating and mapping those sandstones and shales occurring deeper than about 10,000 ft. The Wilcox and Midway Groups comprise the oldest thick sandstone/shale sequence of the Tertiary of the Gulf Coast. The Wilcox crops out in a band 10 to 20 mi wide located 100 to 200 mi inland from the present-day coastline. The Wilcox sandstones and shales in the outcrop and updip shallow subsurface were deposited primarily in fluvial environments; downdip in the deep subsurface, on the other hand, the Wilcox sediments were deposited in large deltaic systems, some of which were reworked into barrier-bar and strandplain systems. Growth faults developed within the deltaic systems, where they prograded basinward beyond the older, stable Lower Cretaceous shelf margin onto the less stable basinal muds. Continued displacement along these faults during burial resulted in: (1) entrapment of pore fluids within isolated sandstone and shale sequences, and (2) buildup of pore pressure greater than hydrostatic pressure and development of geopressure.

Debout, D.G.; Weise, B.R.; Gregory, A.R.; Edwards, M.B.

1982-01-01T23:59:59.000Z

348

Electric Chern-Simons term, enlarged exotic Galilei symmetry and noncommutative plane  

E-Print Network [OSTI]

The extended exotic planar model for a charged particle is constructed. It includes a Chern-Simons-like term for a dynamical electric field, but produces usual equations of motion for the particle in background constant uniform electric and magnetic fields. The electric Chern-Simons term is responsible for the non-commutativity of the boost generators in the ten-dimensional enlarged exotic Galilei symmetry algebra of the extended system. The model admits two reduction schemes by the integrals of motion, one of which reproduces the usual formulation for the charged particle in external constant electric and magnetic fields with associated field-deformed Galilei symmetry, whose commuting boost generators are identified with the nonlocal in time Noether charges reduced on-shell. Another reduction scheme, in which electric field transmutes into the commuting space translation generators, extracts from the model a free particle on the noncommutative plane described by the two-fold centrally extended Galilei group of the non-relativistic anyons.

Mariano A. del Olmo; Mikhail S. Plyushchay

2005-11-13T23:59:59.000Z

349

Partition Functions of Superconformal Chern-Simons Theories from Fermi Gas Approach  

E-Print Network [OSTI]

We study the partition function of three-dimensional ${\\mathcal N}=4$ superconformal Chern-Simons theories of the circular quiver type, which are natural generalizations of the ABJM theory, the worldvolume theory of M2-branes. In the ABJM case, it was known that the perturbative part of the partition function sums up to the Airy function as $Z(N)=e^{A}C^{-1/3}\\mathrm{Ai}[C^{-1/3}(N-B)]$ with coefficients $C$, $B$ and $A$ and that for the non-perturbative part the divergences coming from the coefficients of worldsheet instantons and membrane instantons cancel among themselves. We find that many of the interesting properties in the ABJM theory are extended to the general superconformal Chern-Simons theories. Especially, we find an explicit expression of $B$ for general ${\\mathcal N}=4$ theories, a conjectural form of $A$ for a special class of theories, and cancellation in the non-perturbative coefficients for the simplest theory next to the ABJM theory.

Sanefumi Moriyama; Tomoki Nosaka

2014-08-14T23:59:59.000Z

350

From Doubled Chern-Simons-Maxwell Lattice Gauge Theory to Extensions of the Toric Code  

E-Print Network [OSTI]

We regularize compact and non-compact Abelian Chern-Simons-Maxwell theories on a spatial lattice using the Hamiltonian formulation. We consider a doubled theory with gauge fields living on a lattice and its dual lattice. The Hilbert space of the theory is a product of local Hilbert spaces, each associated with a link and the corresponding dual link. The two electric field operators associated with the link-pair do not commute. In the non-compact case with gauge group $\\mathbb{R}$, each local Hilbert space is analogous to the one of a charged "particle" moving in the link-pair group space $\\mathbb{R}^2$ in a constant "magnetic" background field. In the compact case, the link-pair group space is a torus $U(1)^2$ threaded by $k$ units of quantized "magnetic" flux, with $k$ being the level of the Chern-Simons theory. The holonomies of the torus $U(1)^2$ give rise to two self-adjoint extension parameters, which form two non-dynamical background lattice gauge fields that explicitly break the manifest gauge symmetry...

Olesen, T Z; Wiese, U -J

2015-01-01T23:59:59.000Z

351

Review of potential technologies for the treatment of Methyl tertiary butyl Ether (MtBE) in drinking water  

SciTech Connect (OSTI)

At present, the state of knowledge on effective treatment technologies for MtBE in drinking water, and groundwater in general, is limited. Research by others is focusing on the remediation of MtBE close to the point of release. The City of Santa Monica, MWD, Komex and USC are currently conducting research into different technologies that could be used to remove MtBE from drinking water supplies. The objectives of the research are to evaluate different treatment technologies to identify cost-effective and technically feasible alternatives for the removal of MtBE from drinking water. The evaluation is considering moderate to high water flow rates (100 to 2,000+ gpm) and low to moderate MtBE concentrations (<2,000 {mu}g/l). The research program includes four phases: (1) Literature Review; (2) Bench Scale Study; (3) Field Scale Pre-pilot Study; and (4) Summary Evaluation. This paper presents some preliminary information and findings from the first phase of this research - the literature review. The review discusses the chemical properties of MtBE and how they affect remediation and thus, an evaluation of alternative treatment technologies. The review of available literature, and the applicability and limitations of the following technologies are presented in detail.

Brown, A.; Browne, T.E. [Komex H2O Science, Huntington Beach, CA (United States); Devinny, J.S. [Univ. of Southern California, Los Angeles, CA (United States)] [and others

1997-12-31T23:59:59.000Z

352

Depositional setting and sandstone diagenesis of the Upper Pennsylvanian (Missourian) Hepler Formation, Cherokee Shelf of the midcontinent  

SciTech Connect (OSTI)

The Hepler Formation marks the base of the Pleasanton Group which is recognized as the base of the Upper Pennsylvanian in southeastern Kansas. This formation consists of interstratified units of shales, siltstones, and sandstones, as well as a localized coal bed. These lithologies are interpreted as having formed in a prograting, fluvially-dominated deltaic sequence that was deposited as the Late Pennsylvanian sea temporarily withdrew from the Cherokee shelf. Hepler sandstone bodies in the study area are predominantly quartz arenites and sublitharenites. The diagenetic history of the Hepler consisted of alternating periods of authigenic mineral precipitation and dissolution of both detrital grains and cements. Petrographic observations indicate that silica cementation, in the form of quartz overgrowths, took place early in the paragenetic sequence. Changes in the meteoric water chemistry, resulted in partial quartz and feldspar dissolution, and alteration of feldspars to clays. Precipitation of carbonate into dissolution features was initiated by acidic surface waters (fluvial) followed by a sea level rise allowing carbonate-saturated marine waters to flush these sediments. Further burial and compaction destroyed much of remaining porosity and left concavo-convex contacts and sutured quartz grains. This was followed by anoxic conditions which allowed pyrite crystallization to take place. A subsequent fall in sea level exposed Hepler deposits once again to meteoric, low pH waters, resulting in carbonate dissolution. All observed porosity is secondary, formed by carbonate dissolution. Surface samples were subjected to weathering of iron-bearing components to iron-oxide, a product not observable in subsurface core samples.

Gilmer, M.H.; Brenner, R.L. (Univ. of Iowa, Iowa City, IA (United States). Dept. of Geology)

1992-01-01T23:59:59.000Z

353

Towards a Situated, Multimodal Interface for Multiple UAV Control Geraint Jones, Nadia Berthouze, Roman Bielski, Simon Julier  

E-Print Network [OSTI]

Towards a Situated, Multimodal Interface for Multiple UAV Control Geraint Jones, Nadia Berthouze, Roman Bielski, Simon Julier Abstract-- Multiple autonomous Unmanned Aerial Vehicles (UAVs) can be used perspective, Unmanned Aerial Ve- hicles (UAVs) can aid the activities of human teams in a number of situations

Jones, Peter JS

354

Synthesis of Polyfluorenes with Pendant Silylcarboranes Yoan C. Simon, Joseph J. Peterson, Christine Mangold, Kenneth R. Carter,* and  

E-Print Network [OSTI]

Synthesis of Polyfluorenes with Pendant Silylcarboranes Yoan C. Simon, Joseph J. Peterson ReceiVed NoVember 3, 2008 ABSTRACT: The synthesis of a novel silylcarborane-containing fluorene monomer-workers on pyrroles and thiophene has underlined the advantage of introducing carboranes as a way to reinforce

355

Large deviations and martingales for a typed branching di usion, 1 Simon C Harris and David Williams  

E-Print Network [OSTI]

Large deviations and martingales for a typed branching di#11;usion, 1 by Simon C Harris and David are rather complicated; and these are only sketched here { see Harris (1995) and Harris and Williams (1995 for a simpler problem in Champneys, Harris, Toland, Warren and Williams (1995); in the present context

Harris, Simon Colin

356

A spine proof of a lower bound for a typed branching Robert Hardy and Simon C. Harris  

E-Print Network [OSTI]

of an important and difficult path large-deviations lower bound for a typed branching diffusion as found in Git, J.HarrisA spine proof of a lower bound for a typed branching diffusion Robert Hardy and Simon C. Harris March 8, 2004 Abstract We follow the spine approach as found in Hardy and Harris [6, 8, 7] to define new

Harris, Simon Colin

357

EXPERIMENTAL TESTS OF COMPETITIVE MARKETS FOR ELECTRIC POWER Simon Ede, Timothy Mount, William Schulze, Robert Thomas, Ray Zimmerman  

E-Print Network [OSTI]

when there are capacity shortfalls, and the following four market structures: 1. Load is responsiveCSMAE06 EXPERIMENTAL TESTS OF COMPETITIVE MARKETS FOR ELECTRIC POWER Simon Ede, Timothy Mount@cornell.edu, rjt1@cornell.edu, rz10@cornell.edu Abstract Testing the performance of electricity markets

358

Bayesian networks Applications on Dependability, Risk Analysis and Maintenance G. Medina Oliva, P. Weber, C. Simon, B. Iung  

E-Print Network [OSTI]

. Weber, C. Simon, B. Iung CRAN, Nancy-Université, CNRS, Boulevard des Aiguillettes B.P. 70239 F-54506 Vandoeuvre lès Nancy (e-mail: {gabriela.medina-oliva, benoit.iung}@cran.uhp-nancy.fr,{philippe.weber

Boyer, Edmond

359

Knowledge-based recognition of utility map sub-diagrams Simon J. Hickinbotham and Anthony G. Cohn  

E-Print Network [OSTI]

are represented as Figure 1. sub-diagrams in a typical utility map dotted lines on the map. The layout of cables to find visual objects in utility maps. The literature for extracting line primitives from raster mapsKnowledge-based recognition of utility map sub-diagrams Simon J. Hickinbotham and Anthony G. Cohn

Leeds, University of

360

Rfam: annotating non-coding RNAs in complete genomes Sam Griffiths-Jones*, Simon Moxon, Mhairi Marshall, Ajay Khanna1  

E-Print Network [OSTI]

Rfam: annotating non-coding RNAs in complete genomes Sam Griffiths-Jones*, Simon Moxon, Mhairi-coding RNA families, represented by multiple sequence alignments and profile stochastic context free grammars profile stochastic context free grammars (SCFGs), analogous to profile hidden Markov models (HMMs

Eddy, Sean

Note: This page contains sample records for the topic "mt simon sandstone" 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

Rfam: annotating non-coding RNAs in complete Sam Griffiths-Jones*, Simon Moxon, Mhairi Marshall, Ajay Khanna1  

E-Print Network [OSTI]

Rfam: annotating non-coding RNAs in complete genomes Sam Griffiths-Jones*, Simon Moxon, MhairiRNA) families, represented by multiple sequence alignments and profile stochastic context- free grammars. Rfam profile stochastic context-free grammars (SCFGs), analogous to profile hidden Markov models (HMMs

Eddy, Sean

362

An Economic Analysis of the Self Commitment of Thermal Units Simon Ede, Ray Zimmerman, Timothy Mount, Robert Thomas, William Schulze  

E-Print Network [OSTI]

An Economic Analysis of the Self Commitment of Thermal Units Simon Ede, Ray Zimmerman, Timothy a series of economic experiments conducted at Cornell University's Laboratory for Experimental Economics Commitment In the most conventional form of economic dispatch, the problem facing the system operator

363

Methyl tertiary butyl ether (MtBE) contamination of the City of Santa Monica drinking water supply  

SciTech Connect (OSTI)

In the summer of 1996, the City of Santa Monica ceased pumping groundwater from two Well Fields (Charnock and Arcadia) used for public drinking water supply due to persistent and increasing concentrations of MtBE in all seven municipal water supply wells. This lost production accounted for 50% of the City`s total drinking water supply. In late 1996, the City, in cooperation with State and Federal agencies, initiated an investigation of MtBE contamination at the two well fields. The objectives of the investigation were as follows: (1) Review available data on the production, use, chemical characteristics, fate and transport, toxicology, and remediation of MtBE; (2) Identify locations of potential sources of MtBE groundwater contamination at the well fields; (3) Develop an understanding of the hydrologic pathways from the potential sources to the drinking water wells; and (4) Evaluate alternative treatment technologies for the removal of MtBE from drinking water. In addition to a review of available information about MtBE, the investigation included an extensive review of literature and available data relevant to the well fields, including well field production histories, site and regional hydrogeology, all well logs and production in the groundwater basins, general groundwater quality, and the record of MtBE detection. Based upon the review of background information, conceptual hydrogeologic models were developed. A detailed review of agency files for over 45 potential source sites was conducted. The information from this review was summarized, and source site screening and ranking criteria were developed. A field program was conducted at the major well field (Charnock), including soil gas surveys, CPTs, soil borings and well installations, geophysics, and aquifer testing. The field program provided site data which allowed the conceptual hydrogeologic model to be refitted to actual site conditions.

Brown, A.; Farrow, J.R.C. [Komex H2O Science, Huntington Beach, CA (United States); Rodriguez, R.A. [City of Santa Monica, CA (United States)] [and others

1997-12-31T23:59:59.000Z

364

3-D Density Model Of Mt Etna Volcano (Southern Italy) | Open Energy  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 NoPublic Utilities Address: 160 East 300 South Place:ReferenceEditWisconsin:YBR14InformationInformation Of Mt

365

Rock Sampling At Mt Ranier Area (Frank, 1995) | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia:FAQ < RAPID Jump to: navigation, searchVirginia BlueRiverwoods, Illinois:239178°,isWind Farm is)EnergyMt

366

Study of Yang–Mills–Chern–Simons theory in presence of the Gribov horizon  

SciTech Connect (OSTI)

The two-point gauge correlation function in Yang–Mills–Chern–Simons theory in three dimensional Euclidean space is analysed by taking into account the non-perturbative effects of the Gribov horizon. In this way, we are able to describe the confinement and de-confinement regimes, which naturally depend on the topological mass and on the gauge coupling constant of the theory. -- Highlights: •We implement the Gribov quantization to the Topologically massive Yang–Mills theory. •We find a modified propagator at strong coupling by the Gribov horizon. •The gauge propagator depends on the topological mass and the coupling constant. •By studying the gauge propagator we describe the confined–deconfined regimes.

Canfora, Fabrizio, E-mail: canfora@cecs.cl [Centro de Estudios Cientificos (CECs), Valdivia (Chile); Universidad Andres Bello, Av. Republica 440, Santiago (Chile); Gomez, Arturo, E-mail: arturo.gomez@proyectos.uai.cl [Departamento de Ciencias, Facultad de Artes Liberales y Facultad de Ingeniería y Ciencias, Universidad Adolfo Ibáñez, Viña del Mar. (Chile); Sorella, Silvio Paolo, E-mail: sorella@uerj.br [UERJ, Universidade do Estado do Rio de Janeiro (UERJ), Instituto de Física Teórica, Rua São Francisco Xavier 524, 20550-013, Maracaná, Rio de Janeiro (Brazil); Vercauteren, David, E-mail: vercauteren.uerj@gmail.com [UERJ, Universidade do Estado do Rio de Janeiro (UERJ), Instituto de Física Teórica, Rua São Francisco Xavier 524, 20550-013, Maracaná, Rio de Janeiro (Brazil)

2014-06-15T23:59:59.000Z

367

Free Energy of D_n Quiver Chern-Simons Theories  

E-Print Network [OSTI]

We apply the matrix model of Kapustin, Willett and Yaakov to compute the free energy of N=3 Chern-Simons matter theories with D_n quivers in the large N limit. We conjecture a general expression for the free energy that is explicitly invariant under Seiberg duality and show that it can be interpreted as a sum over certain graphs known as signed graphs. Through the AdS/CFT correspondence, this leads to a prediction for the volume of certain tri-Sasaki Einstein manifolds. We also study the unfolding procedure, which relates these D_n quivers to A_{2n-5} quivers. Furthermore, we consider the addition of massive fundamental flavor fields, verifying that integrating these out decreases the free energy in accordance with the F-theorem.

P. Marcos Crichigno; Christopher P. Herzog; Dharmesh Jain

2012-11-06T23:59:59.000Z

368

Maxwell-Chern-Simons vortices in a CPT-odd Lorentz-violating Higgs Electrodynamics  

E-Print Network [OSTI]

We have studied BPS vortices in a CPT-odd and Lorentz-violating Maxwell-Chern-Simons-Higgs (MCSH) electrodynamics attained from the dimensional reduction of the Carroll-Field-Jackiw-Higgs model. The Lorentz-violating parameter induces a pronounced behavior at origin (for the magnetic/electric fields and energy density) which is absent in the MCSH vortices. For some combination of the Lorentz-violating coefficients there always exist a sufficiently large winding number $n_{0}$ such that for all $% |n|\\geq |n_{0}|$ the magnetic field flips its signal, yielding two well defined regions with opposite magnetic flux. However, the total magnetic flux remains quantized and proportional to the winding number.

R. Casana; M. M. Ferreira Jr.; E. da Hora; A. B. F. Neves

2014-04-18T23:59:59.000Z

369

Comments on absorption cross section for Chern-Simons black holes in five dimensions  

E-Print Network [OSTI]

In this paper we study the effects of black hole mass on the absorption cross section for a massive scalar field propagating in a 5-dimensional topological Chern-Simons black hole at the low-frequency limit. We consider the two branches of black hole solutions $(\\alpha=\\pm 1)$ and we show that, if the mass of black hole increase the absorption cross section decreases at the zero-frequency limit for the branch $\\alpha=-1$ and for the other branch, $\\alpha=1$, the behavior is opposite, if the black hole mass increase the absorption cross section increases. Also we find that beyond a certain frequency value, the mass black hole does not affect the absorption cross section.

P. A. González; Joel Saavedra

2011-05-12T23:59:59.000Z

370

Conceptual Model Summary Report Simulation Framework for Regional Geologic CO{sub 2} Storage Along Arches Province of Midwestern United States  

SciTech Connect (OSTI)

A conceptual model was developed for the Arches Province that integrates geologic and hydrologic information on the Eau Claire and Mt. Simon formations into a geocellular model. The conceptual model describes the geologic setting, stratigraphy, geologic structures, hydrologic features, and distribution of key hydraulic parameters. The conceptual model is focused on the Mt. Simon sandstone and Eau Claire formations. The geocellular model depicts the parameters and conditions in a numerical array that may be imported into the numerical simulations of carbon dioxide (CO{sub 2}) storage. Geophysical well logs, rock samples, drilling logs, geotechnical test results, and reservoir tests were evaluated for a 500,000 km{sup 2} study area centered on the Arches Province. The geologic and hydraulic data were integrated into a three-dimensional (3D) grid of porosity and permeability, which are key parameters regarding fluid flow and pressure buildup due to CO{sub 2} injection. Permeability data were corrected in locations where reservoir tests have been performed in Mt. Simon injection wells. The final geocellular model covers an area of 600 km by 600 km centered on the Arches Province. The geocellular model includes a total of 24,500,000 cells representing estimated porosity and permeability distribution. CO{sub 2} injection scenarios were developed for on-site and regional injection fields at rates of 70 to 140 million metric tons per year.

None

2011-06-30T23:59:59.000Z

371

Structural and functional studies of a phosphatidic acid-binding antifungal plant defensin MtDef4: Identification of an RGFRRR motif governing fungal cell entry  

SciTech Connect (OSTI)

A highly conserved plant defensin MtDef4 potently inhibits the growth of a filamentous fungus Fusarium graminearum. MtDef4 is internalized by cells of F. graminearum. To determine its mechanism of fungal cell entry and antifungal action, NMR solution structure of MtDef4 has been determined. The analysis of its structure has revealed a positively charged patch on the surface of the protein consisting of arginine residues in its ?-core signature, a major determinant of the antifungal activity of MtDef4. Here, we report functional analysis of the RGFRRR motif of the ?-core signature of MtDef4. The replacement of RGFRRR to AAAARR or to RGFRAA not only abolishes fungal cell entry but also results in loss of the antifungal activity of MtDef4. MtDef4 binds strongly to phosphatidic acid (PA), a precursor for the biosynthesis of membrane phospholipids and a signaling lipid known to recruit cytosolic proteins to membranes. Mutations of RGFRRR which abolish fungal cell entry of MtDef4 also impair its binding to PA. Our results suggest that RGFRRR motif is a translocation signal for entry of MtDef4 into fungal cells and that this positively charged motif likely mediates interaction of this defensin with PA as part of its antifungal action.

Sagaram, Uma S.; El-Mounadi, Kaoutar; Buchko, Garry W.; Berg, Howard R.; Kaur, Jagdeep; Pandurangi, Raghoottama; Smith, Thomas J.; Shah, Dilip

2013-12-04T23:59:59.000Z

372

Measuring and predicting reservoir heterogeneity in complex deposystems. The fluvial-deltaic Big Injun Sandstone in West Virginia. Final report, September 20, 1991--October 31, 1993  

SciTech Connect (OSTI)

Non-uniform composition and permeability of a reservoir, commonly referred to as reservoir heterogeneity, is recognized as a major factor in the efficient recovery of oil during primary production and enhanced recovery operations. Heterogeneities are present at various scales and are caused by various factors, including folding and faulting, fractures, diagenesis and depositional environments. Thus, a reservoir consists of a complex flow system, or series of flow systems, dependent on lithology, sandstone genesis, and structural and thermal history. Ultimately, however, fundamental flow units are controlled by the distribution and type of depositional environments. Reservoir heterogeneity is difficult to measure and predict, especially in more complex reservoirs such as fluvial-deltaic sandstones. The Appalachian Oil and Natural Gas Research Consortium (AONGRC), a partnership of Appalachian basin state geological surveys in Kentucky, Ohio, Pennsylvania, and West Virginia, and West Virginia University, studied the Lower Mississippian Big Injun sandstone in West Virginia. The Big Injun research was multidisciplinary and designed to measure and map heterogeneity in existing fields and undrilled areas. The main goal was to develop an understanding of the reservoir sufficient to predict, in a given reservoir, optimum drilling locations versus high-risk locations for infill, outpost, or deeper-pool tests.

Hohn, M.E.; Patchen, D.G.; Heald, M.; Aminian, K.; Donaldson, A.; Shumaker, R.; Wilson, T.

1994-05-01T23:59:59.000Z

374

Reservoir Characterization of Bridgeport and Cypress Sandstones in Lawrence Field Illinois to Improve Petroleum Recovery by Alkaline-Surfactant-Polymer Flood  

SciTech Connect (OSTI)

Within the Illinois Basin, most of the oilfields are mature and have been extensively waterflooded with water cuts that range up to 99% in many of the larger fields. In order to maximize production of significant remaining mobile oil from these fields, new recovery techniques need to be researched and applied. The purpose of this project was to conduct reservoir characterization studies supporting Alkaline-Surfactant-Polymer Floods in two distinct sandstone reservoirs in Lawrence Field, Lawrence County, Illinois. A project using alkaline-surfactantpolymer (ASP) has been established in the century old Lawrence Field in southeastern Illinois where original oil in place (OOIP) is estimated at over a billion barrels and 400 million barrels have been recovered leaving more than 600 million barrels as an EOR target. Radial core flood analysis using core from the field demonstrated recoveries greater than 20% of OOIP. While the lab results are likely optimistic to actual field performance, the ASP tests indicate that substantial reserves could be recovered even if the field results are 5 to 10% of OOIP. Reservoir characterization is a key factor in the success of any EOR application. Reservoirs within the Illinois Basin are frequently characterized as being highly compartmentalized resulting in multiple flow unit configurations. The research conducted on Lawrence Field focused on characteristics that define reservoir compartmentalization in order to delineate preferred target areas so that the chemical flood can be designed and implemented for the greatest recovery potential. Along with traditional facies mapping, core analyses and petrographic analyses, conceptual geological models were constructed and used to develop 3D geocellular models, a valuable tool for visualizing reservoir architecture and also a prerequisite for reservoir simulation modeling. Cores were described and potential permeability barriers were correlated using geophysical logs. Petrographic analyses were used to better understand porosity and permeability trends in the region and to characterize barriers and define flow units. Diagenetic alterations that impact porosity and permeability include development of quartz overgrowths, sutured quartz grains, dissolution of feldspar grains, formation of clay mineral coatings on grains, and calcite cementation. Many of these alterations are controlled by facies. Mapping efforts identified distinct flow units in the northern part of the field showing that the Pennsylvanian Bridgeport consists of a series of thick incised channel fill sequences. The sandstones are about 75-150 feet thick and typically consist of medium grained and poorly sorted fluvial to distributary channel fill deposits at the base. The sandstones become indistinctly bedded distributary channel deposits in the main part of the reservoir before fining upwards and becoming more tidally influenced near their top. These channel deposits have core permeabilities ranging from 20 md to well over 1000 md. The tidally influenced deposits are more compartmentalized compared to the thicker and more continuous basal fluvial deposits. Fine grained sandstones that are laterally equivalent to the thicker channel type deposits have permeabilities rarely reaching above 250 md. Most of the unrecovered oil in Lawrence Field is contained in Pennsylvanian Age Bridgeport sandstones and Mississippian Age Cypress sandstones. These reservoirs are highly complex and compartmentalized. Detailed reservoir characterization including the development of 3-D geologic and geocellular models of target areas in the field were completed to identify areas with the best potential to recover remaining reserves including unswept and by-passed oil. This project consisted of tasks designed to compile, interpret, and analyze the data required to conduct reservoir characterization for the Bridgeport and Cypress sandstones in pilot areas in anticipation of expanded implementation of ASP flooding in Lawrence Field. Geologic and geocellular modeling needed for reservoir characterization and res

Seyler, Beverly; Grube, John; Huff, Bryan; Webb, Nathan; Damico, James; Blakley, Curt; Madhavan, Vineeth; Johanek, Philip; Frailey, Scott

2012-12-21T23:59:59.000Z

375

II: MOTION in ONE SPACE DIMENSION -Pt IIb 1st year CLASSICAL MECHANICS MT06 PLR from RCED  

E-Print Network [OSTI]

that this happens for x >> 1/a, then the velocity approaches a limiting value of v0. Why is this ­ no resistance to motion has been included. Indeed what difference would the addition of a resistance term of the form R. To assess the relative importance of the terms one needs the model for M(t) or equivalent data. A linear

Read, Peter L.

376

EIS-0092: Conversion to Coal, Holyoke Water Power Company, Mt. Tom Generating Station Unit 1 Holyoke, Hampden County, Massachusetts  

Broader source: Energy.gov [DOE]

The Economic Regulatory Administration prepared this statement to assess the environmental impacts of prohibiting Unit 1 of the Mt. Tom Generation Station Unit 1 from using either natural gas or petroleum products as a primary energy source, which would result in the utility burning low-sulfur coal.

377

Index theorem, spin Chern Simons theory and fractional magnetoelectric effect in strongly correlated topological insulators  

E-Print Network [OSTI]

Making use of index theorem and spin Chern Simons theory, we construct an effective topological field theory of strongly correlated topological insulators coupling to a nonabelian gauge field $ SU(N) $ with an interaction constant $ g $ in the absence of the time-reversal symmetry breaking. If $ N $ and $ g $ allow us to define a t'Hooft parameter $ \\lambda $ of effective coupling as $ \\lambda = N g^{2} $, then our construction leads to the fractional quantum Hall effect on the surface with Hall conductance $ \\sigma_{H}^{s} = \\frac{1}{4\\lambda} \\frac{e^{2}}{h} $. For the magnetoelectric response described by a bulk axion angle $ \\theta $, we propose that the fractional magnetoelectric effect can be realized in gapped time reversal invariant topological insulators of strongly correlated bosons or fermions with an effective axion angle $ \\theta_{eff} = \\frac{\\pi}{2 \\lambda} $ if they can have fractional excitations and degenerate ground states on topologically nontrivial and oriented spaces. Provided that an effective charge is given by $ e_{eff} = \\frac{e}{\\sqrt{2 \\lambda}} $, it is shown that $ \\sigma_{H}^{s} = \\frac{e_{eff}^{2}}{2h} $, resulting in a surface Hall conductance of gapless fermions with $ e_{eff} $ and a pure axion angle $ \\theta = \\pi $.

K. -S. Park; H. Han

2011-05-31T23:59:59.000Z

378

Dark energy and Chern-Simons like gravity from a dynamical four-form  

E-Print Network [OSTI]

We consider the dynamics of a four-form field $\\tilde {w} $, treating it as a distinct physical degree of freedom, independent of the metric. The equations of motion are derived from an action which, besides having the standard Hilbert-Einstein term and the matter part, consists of a new action for $\\tilde {w} $. The evolution of $\\tilde {w} $ in a flat FRW universe is studied, and it is shown that the parameters of the theory admit solutions wherein it is possible to have an equation of state $p_\\phi \\approx -\\epsilon_\\phi $, so that it leads to an accelerating universe. We also put forward electromagnetic as well as gravitational `Chern-Simons' like terms that arise naturally in 4D, entailing a modified Einstein-Maxwell equation and an enlarged system of Einstein equation involving a Cotton tensor. We demonstrate that the scalar-density associated with $\\tilde {w} $ can be employed to construct a generalized exterior derivative that converts a p-form density to a (p+1)-form density of identical weight.

Patrick Das Gupta

2011-12-02T23:59:59.000Z

379

Geological and petrophysical characterization of the Ferron Sandstone for 3-D simulation of a fluvial-deltaic reservoir. Annual report, October 1, 1995--September 30, 1996  

SciTech Connect (OSTI)

The objective of the Ferron Sandstone project is to develop a comprehensive, interdisciplinary, quantitative characterization of a fluvial-deltaic reservoir to allow realistic inter-well and reservoir-scale models to be developed for improved oil-field development in similar reservoirs world-wide. Quantitative geological and petrophysical information on the Cretaceous Ferron Sandstone in east-central Utah was collected. Both new and existing data is being integrated into a three-dimensional model of spatial variations in porosity, storativity, and tensorial rock permeability at a scale appropriate for inter-well to regional-scale reservoir simulation. Simulation results could improve reservoir management through proper infill and extension drilling strategies, reduction of economic risks, increased recovery from existing oil fields, and more reliable reserve calculations. Transfer of the project results to the petroleum industry is an integral component of the project. This report covers research activities for fiscal year 1995-96, the third year of the project. Most work consisted of interpreting the large quantity of data collected over two field seasons. The project is divided into four tasks: (1) regional stratigraphic analysis, (2) case studies, (3) reservoirs models, and (4) field-scale evaluation of exploration strategies. The primary objective of the regional stratigraphic analysis is to provide a more detailed interpretation of the stratigraphy and gross reservoir characteristics of the Ferron Sandstone as exposed in outcrop. The primary objective of the case-studies work is to develop a detailed geological and petrophysical characterization, at well-sweep scale or smaller, of the primary reservoir lithofacies typically found in a fluvial-dominated deltaic reservoir.

Chidsey, T.C. Jr.

1997-05-01T23:59:59.000Z

380

Level-rank duality of the U(N) WZW model, Chern-Simons theory, and 2d qYM theory  

E-Print Network [OSTI]

We study the WZW, Chern-Simons, and 2d qYM theories with gauge group U(N). The U(N) WZW model is only well-defined for odd level K, and this model is shown to exhibit level-rank duality in a much simpler form than that for SU(N). The U(N) Chern-Simons theory on Seifert manifolds exhibits a similar duality, distinct from the level-rank duality of SU(N) Chern-Simons theory on S^3. When q = e^{2 pi i/(N+K)}, the observables of the 2d U(N) qYM theory can be expressed as a sum over a finite subset of U(N) representations. When N and K are odd, the qYM theory exhibits N K duality, provided q = e^{2 pi i/(N+K)} and theta = 0 mod 2 pi /(N+K).

Stephen G. Naculich; Howard J. Schnitzer

2007-06-11T23:59:59.000Z

Note: This page contains sample records for the topic "mt simon sandstone" 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

Sequence-Stratigraphic Analysis of the Rollins and the Cozzette Sandstone Members, the Upper Cretaceous Mount Garfield Formation of the Piceance Basin, Colorado.  

E-Print Network [OSTI]

at the top. Both siltstone and mudstone are locally bioturbated. Siltstone beds (~20 cm) are sharp-based, light brown to gray in color, and are interbeded with mudstone beds. Coal with siltstone Trough-cross bedding Laminae/flaser beddin g/burrows 10 m10... it occurs at the top of the Rollins Sandstone Member. It is laterally continuous, distinctively white colored, and 22 capped with a coal bed (Figure 9). This unit is composed of six subunits arranged in an upward-coarsening trend and is described...

Ouaichouche, Fatma Zahra

2011-08-31T23:59:59.000Z

382

Four-year prospective study of the respiratory effects of volcanic ash from Mt. St. Helens  

SciTech Connect (OSTI)

This report describes the 4-yr follow-up of 712 loggers exposed over an extended period to varying levels of fresh volcanic ash from the 1980 eruptions of Mt. St. Helens. Concerns related to the irritant effect the ash might have on the airways and also to its fibrogenic potential if exposures were intense and continued over many years. Our subjects were divided into 3 groups: high, low, and no exposure. Baseline testing was begun in June 1980, 1 month after the major eruption, and follow-up testing continued on an annual basis through 1984; 88% of the loggers have been tested at least 3 times. Analysis of lung function data showed that a significant, exposure-related decline in FEV1 occurred during the first year after the eruption. The decline was short-lived, however, and by 1984 the differences between exposure groups were no longer significant. Self-reported symptoms of cough, phlegm, and wheeze showed a similar pattern. No ash-related changes were seen in chest roentgenograms taken in 1980 and in 1984. Our findings are consistent with the hypothesis that the inhaled ash caused mucus hypersecretion and/or airway inflammation that reversed when the exposure levels decreased. The ash levels to which the loggers were exposed were low compared with permissible occupational levels for nuisance dusts, but generally higher than the total suspended particulate levels permissible in ambient air.

Buist, A.S.; Vollmer, W.M.; Johnson, L.R.; Bernstein, R.S.; McCamant, L.E.

1986-04-01T23:59:59.000Z

383

Silurian "Clinton" Sandstone Reservoir Characterization for Evaluation of CO2-EOR Potential in the East Canton Oil Field, Ohio  

SciTech Connect (OSTI)

The purpose of this study was to evaluate the efficacy of using CO2-enhanced oil recovery (EOR) in the East Canton oil field (ECOF). Discovered in 1947, the ECOF in northeastern Ohio has produced approximately 95 million barrels (MMbbl) of oil from the Silurian “Clinton” sandstone. The original oil-in-place (OOIP) for this field was approximately 1.5 billion bbl and this study estimates by modeling known reservoir parameters, that between 76 and 279 MMbbl of additional oil could be produced through secondary recovery in this field, depending on the fluid and formation response to CO2 injection. A CO2 cyclic test (“Huff-n-Puff”) was conducted on a well in Stark County to test the injectivity in a “Clinton”-producing oil well in the ECOF and estimate the dispersion or potential breakthrough of the CO2 to surrounding wells. Eighty-one tons of CO2 (1.39 MMCF) were injected over a 20-hour period, after which the well was shut in for a 32-day “soak” period before production was resumed. Results demonstrated injection rates of 1.67 MMCF of gas per day, which was much higher than anticipated and no CO2 was detected in gas samples taken from eight immediately offsetting observation wells. All data collected during this test was analyzed, interpreted, and incorporated into the reservoir characterization study and used to develop the geologic model. The geologic model was used as input into a reservoir simulation performed by Fekete Associates, Inc., to estimate the behavior of reservoir fluids when large quantities of CO2 are injected into the “Clinton” sandstone. Results strongly suggest that the majority of the injected CO2 entered the matrix porosity of the reservoir pay zones, where it diffused into the oil. Evidence includes: (A) the volume of injected CO2 greatly exceeded the estimated capacity of the hydraulic fracture and natural fractures; (B) there was a gradual injection and pressure rate build-up during the test; (C) there was a subsequent, gradual flashout of the CO2 within the reservoir during the ensuing monitored production period; and (D) a large amount of CO2 continually off-gassed from wellhead oil samples collected as late as 3½ months after injection. After the test well was returned to production, it produced 174 bbl of oil during a 60-day period (September 22 to November 21, 2008), which represents an estimated 58 percent increase in incremental oil production over preinjection estimates of production under normal, conditions. The geologic model was used in a reservoir simulation model for a 700-acre model area and to design a pilot to test the model. The model was designed to achieve a 1-year response time and a five-year simulation period. The reservoir simulation modeling indicated that the injection wells could enhance oil production and lead to an additional 20 percent recovery in the pilot area over a five-year period. The base case estimated that by injecting 500 MCF per day of CO2 into each of the four corner wells, 26,000 STBO would be produced by the central producer over the five-year period. This would compare to 3,000 STBO if a new well were drilled without the benefit of CO2 injection. This study has added significant knowledge to the reservoir characterization of the “Clinton” in the ECOF and succeeded in identifying a range on CO2-EOR potential. However, additional data on fluid properties (PVT and swelling test), fractures (oriented core and microseis), and reservoir characteristics (relative permeability, capillary pressure, and wet ability) are needed to further narrow the uncertainties and refine the reservoir model and simulation. After collection of this data and refinement of the model and simulation, it is recommended that a larger scale cyclic- CO2 injection test be conducted to better determine the efficacy of CO2-EOR in the “Clinton” reservoir in the ECOF.

Riley, Ronald; Wicks, John; Perry, Christopher

2009-12-30T23:59:59.000Z

384

Investigation of exfoliation joints in Navajo sandstone at the Zion National Park and in granite at the Yosemite National Park by tectonofractographic techniques  

SciTech Connect (OSTI)

Tectonofractographic techniques have been applied to the study of joint exfoliation in the Navajo sandstone at Zion National Park and in the granite at Yosemite National Park. New types of fracture surface morphologies have been observed which enabled the discerning of incipient joints and consequent fracture growth in these rocks. Incipient jointing in the sandstone is mostly manifested by elliptical and circular fractures (meters to tens meters across) initiating from independent origins. They interfere with each other and grow to larger circular fractures producing exfoliation surfaces up to hundreds of meters across. Less frequently, series of large concentric undulations demonstrate the propagation of a large fracture front producing exfoliation from an individual origin. One such fracture front reveals refraction of undulations at a layer boundary. Certain en echelon fringes surround the joint mirror plane with well defined rims of en echelons and hackles which enable the determination of the tensile fracture stress, {sigma}f. Arches in Zion National Park are ubiquitous in shape and size, revealing stages in their evolution by a mechanical process, which was associated with exfoliation, but independent of local faulting. Exfoliation and arching mostly occurred on vertical surfaces of N-NNW and NE sets of prominent joints, but there are also deviations from this general trend. In Yosemite National Park large exfoliations (hundreds of meters in size) developed on the El Capitan cliff by the interaction and merging of many previous smaller incipient joints that vary in size from meters to tens of meter.

Bahat, D.; Grossenbacher, K.; Karasaki, K.

1995-04-01T23:59:59.000Z

385

Geological and petrophysical characterization of the ferron sandstone for 3-D simulation of a fluvial-deltaic reservoir. Annual report, October 1, 1994--September 30, 1995  

SciTech Connect (OSTI)

The objective of the Ferron Sandstone project is to develop a comprehensive, interdisciplinary, quantitative characterization of a fluvial-deltaic reservoir to allow realistic interwell and reservoir-scale models to be developed for improved oil-field development in similar reservoirs world-wide. Quantitative geological and petrophysical information on the Cretaceous Ferron Sandstone in east-central Utah was collected. Both new and existing data is being integrated into a three-dimensional model of spatial variations in porosity, storativity, and tensorial rock permeability at a scale appropriate for inter-well to regional-scale reservoir simulation. Simulation results could improve reservoir management through proper infill and extension drilling strategies, reduction of economic risks, increased recovery from existing oil fields, and more reliable reserve calculations. Transfer of the project results to the petroleum industry is an integral component of the project. This report covers research activities for fiscal year 1994-95, the second year of the project. Most work consisted of developing field methods and collecting large quantities of existing and new data. We also continued to develop preliminary regional and case-study area interpretations. The project is divided into four tasks: (1) regional stratigraphic analysis, (2) case studies, (3) reservoirs models, and (4) field-scale evaluation of exploration strategies.

Chidsey, T.C. Jr.; Allison, M.L.

1996-05-01T23:59:59.000Z

386

Digenetic Changes in Macro- to Nano-Scale Porosity in the St. Peter Sandstone:L An (Ultra) Small Angle Neutron Scattering and Backscattered Electron Imagining Analysis  

SciTech Connect (OSTI)

Small- and Ultra-Small Angle Neutron Scattering (SANS and USANS) provide powerful tools for quantitative analysis of porous rocks, yielding bulk statistical information over a wide range of length scales. This study utilized (U)SANS to characterize shallowly buried quartz arenites from the St. Peter Sandstone. Backscattered electron imaging was also used to extend the data to larger scales. These samples contain significant volumes of large-scale porosity, modified by quartz overgrowths, and neutron scattering results show significant sub-micron porosity. While previous scattering data from sandstones suggest scattering is dominated by surface fractal behavior over many orders of magnitude, careful analysis of our data shows both fractal and pseudo-fractal behavior. The scattering curves are composed of subtle steps, modeled as polydispersed assemblages of pores with log-normal distributions. However, in some samples an additional surface-fractal overprint is present, while in others there is no such structure, and scattering can be explained by summation of non-fractal structures. Combined with our work on other rock-types, these data suggest that microporosity is more prevalent, and may play a much more important role than previously thought in fluid/rock interactions.

Anovitz, Lawrence {Larry} M [ORNL; Cole, David [Ohio State University; Rother, Gernot [ORNL; Allard Jr, Lawrence Frederick [ORNL; Jackson, Andrew [NIST Center for Neutron Research (NCRN), Gaithersburg, MD; Littrell, Ken [ORNL

2013-01-01T23:59:59.000Z

387

The lithology, environment of deposition, and reservoir evaluation of sandstones in the Upper Queen Formation (Guadalupian, Permian) at Concho Bluff North and Jennifer Fields, Upton and Ector Counties, Texas  

E-Print Network [OSTI]

THE LI THOLOGY g ENVIRONMENT OF DEPOS ITION g AND RESERVOIR EVALUATION OF SANDSTONES IN THE UPPER QUEEN FORMATION (GUADALUPIAN, PERMIAN) AT CONCHO BLUFF NORTH AND JENNIFER F I ELDS g UPTON AND ECTOR COUNT I ES ~ TEXAS A Thesis by JAMES BROOX... EVALUATION OF SANDSTONES IN THE UPPER QUEEN FORMATION (GUADALUPIAN, PERMIAN) AT CONCHO BLUFF NORTH AND JENNIFER F IELDS ~ UPTON AND ECTOR COUNT I ES g TEXAS A Thesis by JAMES BROOX HARPER Approved as to style and content by: Jame (Chair Mazzullo...

Harper, James Broox

1990-01-01T23:59:59.000Z

388

Probing the effects of Lorentz-symmetry violating Chern-Simons and Ricci-Cotton terms in higher derivative gravity  

SciTech Connect (OSTI)

The combined effects of the Lorentz-symmetry violating Chern-Simons and Ricci-Cotton actions are investigated for the Einstein-Hilbert gravity in the second-order formalism modified by higher derivative terms, and their consequences on the spectrum of excitations are analyzed. We follow the lines of previous works and build up an orthonormal basis of projector-like operators for the degrees of freedom, rather than for the spin modes of the fields. With this new basis, the attainment of the propagators is remarkably simplified and the identification of the physical and unphysical modes becomes more immediate. Our conclusion is that the only tachyon- and ghost-free model is the Einstein-Hilbert action added up by the Chern-Simons term with a timelike vector of the type v{sup {mu}=}({mu},0-vector). Spectral consistency imposes that the Ricci-Cotton term must be switched off. We then infer that gravity with Lorentz-symmetry violation imposes a drastically different constraint on the background if compared to ordinary gauge theories whenever conditions for the suppression of tachyons and ghosts are imposed.

Pereira-Dias, B.; Hernaski, C. A.; Helayeel-Neto, J. A. [Centro Brasileiro de Pesquisas Fisicas, Rua Dr. Xavier Sigaud 150, Urca, Rio de Janeiro, Brazil, CEP 22290-180 (Brazil)

2011-04-15T23:59:59.000Z

389

Uranium hydrogeochemical and stream-sediment reconnaissance of the Mt. Michelson NTMS quadrangle, Alaska  

SciTech Connect (OSTI)

This report presents results of a Hydrogeochemical and Stream Sediment Reconnaissance (HSSR) of the Mt. Michelson NTMS quadrangle, Alaska. In addition to this abbreviated data release, more complete data are available to the public in machine-readable form. These machine-readable data, as well as quarterly or semiannual program progress reports containing further information on the HSSR program in general, or on the Los Alamos National Laboratory (LANL) portion of the program in particular, are available from DOE's Technical Library at its Grand Junction Area Office. Presented in this data release are location data, field analyses, and laboratory analyses of several different sample media. For the sake of brevity, many field site observations have not been included in this volume; these data are, however, available on the magnetic tape. Appendices A and B describe the sample media and summarize the analytical results for each medium. The data have been subdivided by one of the Los Alamos National Laboratory sorting programs of Zinkl and others (1981a) into groups of stream-sediment and lake-sediment samples. For each group which contains a sufficient number of observations, statistical tables, tables of raw data, and 1:1,000,000 scale maps of pertinent elements have been included in this report. Also included are maps showing results of multivariate statistical analyses. Information on the field and analytical procedures used by the Los Alamos National Laboratory during sample collection and analysis may be found in any HSSR data release prepared by the Laboratory and will not be included in this report.

Zinkl, R.J.; Shettel, D.L. Jr.; Langfeldt, S.L.; Hardy, L.C.; D'Andrea, R.F. Jr. (comps.) [comps.

1982-04-01T23:59:59.000Z

390

Dark Matter Particle Spectroscopy at the LHC: Generalizing M(T2) to Asymmetric Event Topologies  

SciTech Connect (OSTI)

We consider SUSY-like missing energy events at hadron colliders and critically examine the common assumption that the missing energy is the result of two identical missing particles. In order to experimentally test this hypothesis, we generalize the subsystem M{sub T2} variable to the case of asymmetric event topologies, where the two SUSY decay chains terminate in different 'children' particles. In this more general approach, the endpoint M{sub T2(max)} of the M{sub T2} distribution now gives the mass {tilde M}p({tilde M}{sub c}{sup (a)}, {tilde M}{sub c}{sup (b)}) of the parent particles as a function of two input children masses {tilde M}{sub c}{sup (a)} and {tilde M}{sub c}{sup (b)}. We propose two methods for an independent determination of the individual children masses M{sub c}{sup (a)} and M{sub c}{sup (b)}. First, in the presence of upstream transverse momentum PUTM the corresponding function {tilde M}p({tilde M}{sub c}{sup (a)}, {tilde M}{sub c}{sup (b)}, P{sub UTM}) is independent of P{sub UTM} at precisely the right values of the children masses. Second, the previously discussed MT2 'kink' is now generalized to a 'ridge' on the 2-dimensional surface {tilde M}p({tilde M}{sub c}{sup (a)}, {tilde M}{sub c}{sup (b)}). As we show in several examples, quite often there is a special point along that ridge which marks the true values of the children masses. Our results allow collider experiments to probe a multi-component dark matter sector directly and without any theoretical prejudice.

Konar, Partha; /Florida U.; Kong, Kyoungchul; /SLAC; Matchev, Konstantin T.; Park, Myeonghun; /Florida U.; ,

2012-04-03T23:59:59.000Z

391

A fast, simple, and naturally machine-precision algorithm for calculating both symmetric and asymmetric MT2, for any physical inputs  

E-Print Network [OSTI]

This document describes a stransverse-mass calculation algorithm that has better numerical stability, and therefore accuracy, than the fastest existing implementations. The new algorithm naturally permits computation of MT2 to machine-precision for any valid set of inputs. In addition to being more accurate than existing fast calculators, the new implementation is arguably simpler to understand, comprises fewer lines of active code, and provides the first fast machine-precision asymmetric-MT2 calculator known to the authors.

Christopher G. Lester; Benjamin Nachman

2014-11-16T23:59:59.000Z

392

PHYS 211 Lecture 15 -Kepler's Laws 15 -1 2001 by David Boal, Simon Fraser University. All rights reserved; further copying or resale is strictly prohibited.  

E-Print Network [OSTI]

: Fowles and Cessiday, Chap. 6 One of the major successes of Newton's law of universal gravitation of the planet's orbit. We now use Newton's laws of mechanics and gravitation to explain (or derive) eachPHYS 211 Lecture 15 - Kepler's Laws 15 - 1 © 2001 by David Boal, Simon Fraser University. All

Boal, David

393

PHYS 390 Lecture 23 -Photon gas 23 -1 2001 by David Boal, Simon Fraser University. All rights reserved; further resale or copying is strictly prohibited.  

E-Print Network [OSTI]

reserved; further resale or copying is strictly prohibited. Lecture 23 - Photon gas What's Important University. All rights reserved; further resale or copying is strictly prohibited. Assuming the gas 390 Lecture 23 - Photon gas 23 - 3 © 2001 by David Boal, Simon Fraser University. All rights reserved

Boal, David

394

PHYS 390 Lecture 22 -Energy production in stars 22 -1 2001 by David Boal, Simon Fraser University. All rights reserved; further resale or copying is strictly prohibited.  

E-Print Network [OSTI]

PHYS 390 Lecture 22 - Energy production in stars 22 - 1 © 2001 by David Boal, Simon Fraser, Sec. 5.3 Energy production in PP I Because 3 He production from D is a relatively fast step at T = 15 � 106 K and #12;PHYS 390 Lecture 22 - Energy production in stars 22 - 2 © 2001 by David Boal

Boal, David

395

Mineral hints at bright blue rocks deep in the Earth 12 March 2014 Last updated at 21:16 ET | By Simon Redfern Science writer  

E-Print Network [OSTI]

Mineral hints at bright blue rocks deep in the Earth 12 March 2014 Last updated at 21:16 ET | By Simon Redfern Science writer Minerals preserved in diamond have revealed hints of the bright blue and back, which it has." Blue planet Prof Joseph Smyth of the University of Colorado has spent many

Machel, Hans

396

PHYS 390 Lecture 12 -Energy and temperature 12 -1 2001 by David Boal, Simon Fraser University. All rights reserved; further copying or resale is strictly prohibited.  

E-Print Network [OSTI]

· it has a contribution from a mass energy mc 2 . Where does kinetic energy fit into this? By definition: E, thus releasing energy to the system. This definition can be applied to decays as well: QPHYS 390 Lecture 12 - Energy and temperature 12 - 1 © 2001 by David Boal, Simon Fraser University

Boal, David

397

SEQUENCE STRATIGRAPHY AND FACIES ANALYSIS OF THE ROLLINS SANDSTONE MEMBER (MOUNT GARFIELD FORMATION) AND RE-EXAMINATION OF THE CONTACT BETWEEN THE MOUNT GARFIELD AND WILLIAMS FORK FORMATIONS (LATE CRETACEOUS)  

E-Print Network [OSTI]

there is no upward-climbing geometry at the top of the Mount Garfield Formation, and the Rollins Sandstone Member and the Cameo Wheeler coal zone (of the Williams Fork Formation) are not time-equivalent units. The marine- shoreface deposits within the Rollins...

Thompson, Jesse David

2011-08-31T23:59:59.000Z

398

Geology and petrophysical characterization of the Ferron Sandstone for 3-D simulation of a fluvial-deltaic reservoir. Annual report, October 1, 1996--September 30, 1997  

SciTech Connect (OSTI)

The objective of the Ferron Sandstone (Utah) project is to develop a comprehensive, interdisciplinary, quantitative characterization of a fluvial-deltaic reservoir to allow realistic interwell and reservoir-scale models to be developed for improved oil-field development in similar reservoirs world-wide. Both new and existing data is being integrated into a 3-D model of spatial variations in porosity, storativity, and tensorial rock permeability at a scale appropriate for inter-well to regional-scale reservoir simulation. Simulation results could improve reservoir management through proper infill and extension drilling strategies, reduction of economic risks, increased recovery from existing oil fields, and more reliable reserve calculations. The project is divided into four tasks: (1) regional stratigraphic analysis, (2) case studies, (3) reservoirs models, and (4) field-scale evaluation of exploration strategies. The primary objective of the regional stratigraphic analysis is to provide a more detailed interpretation of the stratigraphy and gross reservoir characteristics of the Ferron Sandstone as exposed in outcrop. The primary objective of the case-studies work is to develop a detailed geological and petrophysical characterization, at well-sweep scale or smaller, of the primary reservoir lithofacies typically found in a fluvial-dominated deltaic reservoir. Work on tasks 3 and 4 consisted of developing two- and three-dimensional reservoir models at various scales. The bulk of the work on these tasks is being completed primarily during the last year of the project, and is incorporating the data and results of the regional stratigraphic analysis and case-studies tasks.

Chidsey, T.C. Jr.; Anderson, P.B.; Morris, T.H.; Dewey, J.A. Jr.; Mattson, A.; Foster, C.B.; Snelgrove, S.H.; Ryer, T.A.

1998-05-01T23:59:59.000Z

399

The massive fermion phase for the U(N) Chern-Simons gauge theory in D=3 at large N  

SciTech Connect (OSTI)

We explore the phase structure of fermions in the U(N) Chern-Simons Gauge theory in three dimensions using the large N limit where N is the number of colors and the fermions are taken to be in the fundamental representation of the U(N) gauge group. In the large N limit, the theory retains its classical conformal behavior and considerable attention has been paid to possible AdS/CFT dualities of the theory in the conformal phase. In this paper we present a solution for the massive phase of the fermion theory that is exact to the leading order of ‘t Hooft’s large N expansion. We present evidence for the spontaneous breaking of the exact scale symmetry and analyze the properties of the dilaton that appears as the Goldstone boson of scale symmetry breaking.

Bardeen, William A. [Fermilab

2014-10-01T23:59:59.000Z

400

A polymorphism in metallothionein 1A (MT1A) is associated with cadmium-related excretion of urinary beta 2?microglobulin  

SciTech Connect (OSTI)

Objectives: Cadmium (Cd) toxicity of the kidney varies between individuals despite similar exposure levels. In humans Cd is mainly bound to metallothioneins (MT), which scavenge its toxic effects. Here we analyzed whether polymorphisms in MT genes MT1A and MT2A influence Cd-related kidney damage. Methods: In a cross-sectional study N = 512 volunteers were selected from three areas in South-Eastern China, which to varying degree were Cd-polluted from a smelter (control area [median Cd in urine U-Cd = 2.67 ?g/L], moderately [U-Cd = 4.23 ?g/L] and highly [U-Cd = 9.13 ?g/L] polluted areas). U-Cd and blood Cd (B-Cd) concentrations were measured by graphite-furnace atomic absorption spectrometry. MT1A rs11076161 (G/A), MT2A rs10636 (G/C) and MT2A rs28366003 (A/G) were determined by Taqman assays; urinary N-Acetyl-beta-(D)-Glucosaminidase (UNAG) by spectrometry, and urinary ?2-microglobulin (UB2M) by ELISA. Results: Higher B-Cd (natural log-transformed) with increasing number of MT1A rs11076161 A-alleles was found in the highly polluted group (p-value trend = 0.033; all p-values adjusted for age, sex, and smoking). In a linear model a significant interaction between rs11076161 genotype and B-Cd was found for UNAG (p = 0.001) and UB2M concentrations (p = 0.001). Carriers of the rs11076161 AA genotype showed steeper slopes for the associations between Cd in blood and natural log-transformed UB2M (? = 1.2, 95% CI 0.72–1.6) compared to GG carriers (? = 0.30, 95% CI 0.15–0.45). Also for UNAG (natural log-transformed) carriers of the AA genotype had steeper slopes (? = 0.55, 95% CI 0.27–0.84) compared to GG carriers (? = 0.018, 95% CI ? 0.79–0.11). Conclusions: MT1A rs11076161 was associated with B-Cd concentrations and Cd-induced kidney toxicity at high exposure levels. -- Highlights: ? Cadmium is toxic to the kidney but the susceptibility differs between individuals. ? The toxic effect of cadmium is scavenged by metallothioneins. ? A common variant of metallothionein 1A was genotyped in 512 cadmium exposed humans. ? Variant carriers of this polymorphism showed more kidney damage from cadmium. ? The frequency of these variants needs to be taken into account in risk assessment.

Lei, Lijian [Department of Occupational Health, School of Public Health, Fudan University, Shanghai (China) [Department of Occupational Health, School of Public Health, Fudan University, Shanghai (China); Department of Epidemiology, School of Public Health, Shanxi Medical University, Shanxi (China); Chang, Xiuli [Department of Occupational Health, School of Public Health, Fudan University, Shanghai (China)] [Department of Occupational Health, School of Public Health, Fudan University, Shanghai (China); Rentschler, Gerda [Department of Occupational and Environmental Medicine, Lund University, SE-22185, Lund (Sweden)] [Department of Occupational and Environmental Medicine, Lund University, SE-22185, Lund (Sweden); Tian, Liting [Department of Occupational Health, School of Public Health, Fudan University, Shanghai (China)] [Department of Occupational Health, School of Public Health, Fudan University, Shanghai (China); Zhu, Guoying; Chen, Xiao [Department of Bone Metabolism, Institute of Radiation Medicine, Fudan University, Shanghai (China)] [Department of Bone Metabolism, Institute of Radiation Medicine, Fudan University, Shanghai (China); Jin, Taiyi, E-mail: tyjinster@gmail.com [Department of Occupational Health, School of Public Health, Fudan University, Shanghai (China)] [Department of Occupational Health, School of Public Health, Fudan University, Shanghai (China); Broberg, Karin, E-mail: karin.broberg_palmgren@med.lu.se [Department of Occupational and Environmental Medicine, Lund University, SE-22185, Lund (Sweden)] [Department of Occupational and Environmental Medicine, Lund University, SE-22185, Lund (Sweden)

2012-12-15T23:59:59.000Z

Note: This page contains sample records for the topic "mt simon sandstone" 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.


401

Reservoir description of a sand-rich submarine fan complex for a steamflood project: upper Miocene Potter sandstone, North Midway Sunset field, California  

SciTech Connect (OSTI)

Nearly 650 m of cores from the upper Miocene Potter sandstone in Mobil's Alberta/Shale property, North Midway Sunset field, California, were examined to determine depositional facies, sand-body geometry, and reservoir quality for a proposed steamflood project. The Potter represents a sand-rich submarine fan complex with braided-channel, meandering-channel, levee, and crevasse-splay facies. The braided-channel facies (gravel and coarse sand) is thick (up to 100 m), sheetlike (> 500 m wide), and highly permeable (10,000 + md). The meandering-channel facies (coarse to medium sand) is up to 20 m thick, over 400 m long, lenticular in geometry, and exhibits an upward decrease in permeability (e.g., 9000 to 500 md) related to grain size that fines upward. The levee facies (in bioturbated sand) is up to 21 m thick, shows variable geometry, and is generally low in permeability (100-1500 md). The crevasse splay (medium sand) is up to 12 m thick, sheetlike (> 300 m wide), and shows moderately high permeability (2000-8000 md). The braided-channel facies was a product of density-modified grain flows, and the remaining three facies were deposited by turbidity currents. Steam flooding of the Potter reservoir should perform extremely well because the entire reservoir is composed of relatively clean sand and the reservoir lacks both horizontal and vertical permeability barriers.

Shanmugam, G.; Clayton, C.A.

1989-03-01T23:59:59.000Z

402

Comment on ``A modified leapfrog scheme for shallow water equations'' by Wen-Yih Sun and Oliver M.T. Sun  

E-Print Network [OSTI]

Commentary Comment on ``A modified leapfrog scheme for shallow water equations'' by Wen-Yih Sun and Oliver M.T. Sun Paul D. Williams Department of Meteorology, University of Reading, UK a r t i c l e i n f integration of the shallow-water equa- tions using the leapfrog time-stepping scheme [Sun Wen-Yih, Sun Oliver

Williams, Paul

403

Gauge fixing and classical dynamical r-matrices in ISO(2,1)-Chern-Simons theory  

E-Print Network [OSTI]

We apply Dirac's gauge fixing procedure to Chern-Simons theory with gauge group ISO(2,1) on manifolds RxS, where S is a punctured oriented surface of general genus. For all gauge fixing conditions that satisfy certain structural requirements, this yields an explicit description of the Poisson structure on the moduli space of flat ISO(2,1)-connections on S via the resulting Dirac bracket. The Dirac bracket is determined by classical dynamical r-matrices for ISO(2,1). We show that the Poisson structures and classical dynamical r-matrices arising from different gauge fixing conditions are related by dynamical ISO(2,1)-valued transformations that generalise the usual gauge transformations of classical dynamical r-matrices. By means of these transformations, it is possible to classify all Poisson structures and classical dynamical r-matrices obtained from such gauge fixings. Generically these Poisson structures combine classical dynamical r-matrices for non-conjugate Cartan subalgebras of iso(2,1).

Catherine Meusburger; Torsten Schönfeld

2012-05-31T23:59:59.000Z

404

Simon Fraser University Simon Fraser University  

E-Print Network [OSTI]

and UniverCity residents). When implemented, the district heating system will support SFU's progress towards

405

Geologic controls on transgressive-regressive cycles in the upper Pictured Cliffs sandstone and coal geometry in the lower Fruitland Formation, Northern San Juan Basin, New Mexico and Colorado  

SciTech Connect (OSTI)

Three upper Pictured Cliffs Sandstone tongues in the northern part of the San Juan Basin record high-frequency transgressive episodes during the Late Cretaceous and are inferred to have been caused by eustatic sea level rise coincident with differential subsidence. Outcrop and subsurface studies show that each tongue is an amalgamated barrier strand-plain unit up to 100 ft (30 m) thick. Upper Pictured Cliffs barrier strand-plain sandstones underlie and bound thickest Fruitland coal seams on the seaward side. Controls on Fruitland coal-seam thickness and continuity are a function of local facies distribution in a coastal-plain setting, shoreline positions related to transgressive-regressive cycles, and basin subsidence. During periods of relative sea level rise, the Pictured Cliffs shoreline was temporarily stabilized, allowing thick, coastal-plain peats to accumulate. Although some coal seams in the lower Fruitland tongue override abandoned Pictured Cliffs shoreline deposits, many pinch out against them. Differences in the degree of continuity of these coal seams relative to coeval shoreline sandstones are attributed to either differential subsidence in the northern part of the basin, multiple episodes of sea level rise, local variations in accommodation and progradation, stabilization of the shoreline by aggrading peat deposits, or a combination of these factors. Fruitland coalbed methane resources and productivity are partly controlled by coal-seam thickness; other important factors include thermal maturity, fracturing, and overpressuring. The dominant production trend occurs in the northern part of the basin and is oriented northwestward, coinciding with the greatest Fruitland net coal thickness.

Ambrose, W.A.; Ayers, W.B. [University of Texas, Austin, TX (United States)

2007-08-15T23:59:59.000Z

406

Electrically charged finite energy solutions of an $SO(5)$ and an $SU(3)$ Higgs-Chern-Simons--Yang-Mills-Higgs systems in $3+1$ dimensions  

E-Print Network [OSTI]

We study spherically symmetric finite energy solutions of two Higgs-Chern-Simons--Yang-Mills-Higgs (HCS-YMH) models in $3+1$ dimensions, one with gauge group $SO(5)$ and the other with $SU(3)$. The Chern-Simons (CS) densities are defined in terms of both the Yang-Mills (YM) and Higgs fields and the choice of the two gauge groups is made so they do not vanish. The solutions of the $SO(5)$ model carry only electric charge and zero magnetic charge, while the solutions of the $SU(3)$ model are dyons carrying both electric and magnetic charges like the Julia-Zee (JZ) dyon. Unlike the latter however, the electric charge in both models receives an important contribution from the CS dynamics. We pay special attention to the relation between the energies and charges of these solutions. In contrast with the electrically charged JZ dyon of the Yang-Mills-Higgs (YMH) system, whose mass is larger than that of the electrically neutral (magnetic monopole) solutions, the masses of the electrically charged solutions of our HCS-YMH models can be smaller than their electrically neutral counterparts in some parts of the parameter space. To establish this is the main task of this work, which is performed by constructing the HCS-YMH solutions numerically. In the case of the $SU(3)$ HCS-YMH, we have considered the question of angular momentum, and it turns out that it vanishes.

Francisco Navarro-Lerida; D. H. Tchrakian

2014-12-15T23:59:59.000Z

407

Abundance of fin whales in West Greenland in 2007 M.P. HEIDE-JRGENSEN*, K.L. LAIDRE*+, M. SIMON*, M.L. BURT$, D.L. BORCHERS$ AND M. RASMUSSEN#  

E-Print Network [OSTI]

Abundance of fin whales in West Greenland in 2007 M.P. HEIDE-JØRGENSEN*, K.L. LAIDRE*+, M. SIMON transect survey of fin whales (Balaenoptera physalus) conducted off West Greenland in 2007 was used of the survey plane. The abundance estimate furthermore only represents the coastal areas of West Greenland

Laidre, Kristin L.

408

Log interpretation of shaly sandstones  

E-Print Network [OSTI]

and Gas, Arco Oil and Gas, and Sun Oil Companies for their contributions of cores, logs, and other valuable data. Their contributions were an immense help in formulating and supporting the ideas developed in my study. I also wish to express gratitute... of Water Saturation page . . 78 79 . . 81 . 87 91 93 VI CONCLUSIONS . 104 REFERENCES CITED APPENDIX I REESE INTRACOASTAL LAND ?2 DATA . 107 . . 111 APPENDIX II ARCO HANKAMER 630 ? 1 DATA 133 APPENDIX III SUN SMITH JR. ?8 DATA VITA 152 163...

Baker, Joel Foster

1987-01-01T23:59:59.000Z

409

Simon Fraser University Annual Report Fiscal Year 1998/99 At the heart of the University, the SFU LAt the heart of the University, the SFU LAt the heart of the University, the SFU LAt the heart of the University, the SFU Library is dedicated toibrary is d  

E-Print Network [OSTI]

SFU Simon Fraser University Annual Report Fiscal Year 1998/99 At the heart of the University, the SFU LAt the heart of the University, the SFU LAt the heart of the University, the SFU LAt the heart

410

Faddeev-Senjanovic Quantization of SU(n) N=2 Supersymmetric Gauge Field System with Non-Abelian Chern-Simons Topological Term and Its Fractional Spin  

E-Print Network [OSTI]

Using Faddeev-Senjanovic path integral quantization for constrained Hamilton system, we quantize SU(n) N=2 supersymmetric gauge field system with non-abelian Chern-Simons topological term in 2+1 dimensions, and use consistency of a gauge condition naturally to deduce another gauge condition. Further, we get the generating functional of Green function in phase space, deduce the angular momentum based on the global canonical Noether theorem at quantum level, obtain the fractional spin of this supersymmetric system, and show that the total angular momentum has the orbital angular momentum and spin angular momentum of the non-abelian gauge field. Finally, we find out the anomalous fractional spin and discover that the fractional spin has the contributions of both the group superscript components and the A_0^s (x) charge.

Yong-Chang Huang; Qiu-Hong Huo

2009-01-13T23:59:59.000Z

411

Interview of Simon Schaffer  

E-Print Network [OSTI]

museum of the Nobel Prize which opened just a few years ago; Svante is an impressive technology historian who wrote on the introduction of the steam engine into Sweden and an article on glass-blowing as the key technology of the modern world...

Schaffer, Simon

2008-11-17T23:59:59.000Z

412

Hyperbelfunktionen Simone kopp  

E-Print Network [OSTI]

.1 Spinnennetz . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 1.2 Golden Gate Bridge Seilkonstruktion der Golden Gate Bridge beispielsweise bildet, wie in der Abbildung 1.2 zu sehen, die sogenannten Kettenlinie. Abbildung 1.2 ­ Golden Gate Bridge Zudem wurden auch in der Antike schon griechische Säulen

Thäter, Gudrun

413

Simon Monard Cell Sorting  

E-Print Network [OSTI]

Hz Amplitude Variables #12;The number of particles per second that the sorter is able to process Sort Speed #12 are indispensable for biological research. They are expensive and complicated. Generally run by dedicated operators;The limiting factor is the number of droplets generated/sec =DDF A high DDF needs high pressure

414

Presupposing Mandy Simons  

E-Print Network [OSTI]

-cleft construction, illustrated in (3): (3) It was (wasn't) President Obama who went to Afghanistan. The speaker of this sentence appears to take for granted that some salient individual went to Afghanistan, and to be making

Spirtes, Peter

415

Molecular Anions Jack Simons  

E-Print Network [OSTI]

-Plesset perturbation (MPPT) method D. The Coupled-Cluster (CC) method E. Density Functional Theory (DFT) VI University of Utah Opening remarks: This web-based text book offers many web links to researchers who have

Simons, Jack

416

SIMON FRASER FISCAL YEAR  

E-Print Network [OSTI]

......................................................................... 4 Media Services ......................................................................................... 5 TECHNOLOGICAL AND DIGITAL SERVICES ............................................................................... 5 Digital Services

417

Experiment Safety Assurance Package for the 40- to 50-GWd/MT Burnup Phase of Mixed Oxide Fuel Irradiation in Small I-Hole Positions in the Advanced Test Reactor  

SciTech Connect (OSTI)

This experiment safety assurance package (ESAP) is a revision of the last MOX ESAP issued in February 2001(Khericha 2001). The purpose of this revision is to identify the changes in the loading pattern and to provide a basis to continue irradiation up to {approx}42 GWd/MT burnup (+ 2.5%) as predicted by MCNP (Monte Carlo N-Particle) transport code before the preliminary postirradiation examination (PIE) results for 40 GWd/MT burnup are available. Note that the safety analysis performed for the last ESAP is still applicable and no additional analysis is required (Khericha 2001). In July 2001, it was decided to reconfigure the test assembly using the loading pattern for Phase IV, Part 3, at the end of Phase IV, Part 1, as the loading pattern for Phase IV, Parts 2 and 3. Three capsule assemblies will be irradiated until the highest burnup capsule assembly accumulates: {approx}50 GWd/MT burnup, based on the MCNP code predictions. The last ESAP suggests that at the end of Phase IV, Part 1, we remove the two highest burnup capsule assemblies ({at} {approx}40 GWd/MT burnup) and send them to ORNL for PIE. Then, irradiate the test assembly using the loading pattern for Phase IV, Part 2, until the highest burnup capsule reaches {approx}40 GWd/MT burnup per MCNP-predicted values.

Khericha, S.T.

2002-06-30T23:59:59.000Z

418

Experiment Safety Assurance Package for the 40- to 50-GWd/MT Burnup Phase of Mixed Oxide Fuel Irradiation in Small I-Hole Positions in the Advanced Test Reactor  

SciTech Connect (OSTI)

This experiment safety assurance package (ESAP) is a revision of the last MOX ESAP issued in February 2001(Khericha 2001). The purpose of this revision is to identify the changes in the loading pattern and to provide a basis to continue irradiation up to ~42 GWd/MT burnup (+ 2.5% as predicted by MCNP (Monte Carlo N-Particle) transport code before the preliminary postirradiation examination (PIE) results for 40 GWd/MT burnup are available. Note that the safety analysis performed for the last ESAP is still applicable and no additional analysis is required (Khericha 2001). In July 2001, it was decided to reconfigure the test assembly using the loading pattern for Phase IV, Part 3, at the end of Phase IV, Part 1, as the loading pattern for Phase IV, Parts 2 and 3. Three capsule assemblies will be irradiated until the highest burnup capsule assembly accumulates: ~50 GWd/MT burnup, based on the MCNP code predictions. The last ESAP suggests that at the end of Phase IV, Part 1, we remove the two highest burnup capsule assemblies (@ ~40 GWd/MT burnup) and send them to ORNL for PIE. Then, irradiate the test assembly using the loading pattern for Phase IV, Part 2, until the highest burnup capsule reaches ~40 GWd/MT burnup per MCNP-predicted values.

Khericha, Soli T

2002-06-01T23:59:59.000Z

419

Experiment Safety Assurance Package for the 40- to 52-GWd/MT Burnup Phase of Mixed Oxide Fuel Irradiation in Small I-hole Positions in the Advanced Test Reactor  

SciTech Connect (OSTI)

This experiment safety assurance package (ESAP) is a revision of the last mixed uranium and plutonium oxide (MOX) ESAP issued in June 2002). The purpose of this revision is to provide a basis to continue irradiation up to 52 GWd/MT burnup [as predicted by MCNP (Monte Carlo N-Particle) transport code The last ESAP provided basis for irradiation, at a linear heat generation rate (LHGR) no greater than 9 kW/ft, of the highest burnup capsule assembly to 50 GWd/MT. This ESAP extends the basis for irradiation, at a LHGR no greater than 5 kW/ft, of the highest burnup capsule assembly from 50 to 52 GWd/MT.

S. T. Khericha; R. C. Pedersen

2003-09-01T23:59:59.000Z

420

EXPERIMENTAL EVALUATION OF CHEMICAL SEQUESTRATION OF CARBON DIOXIDE IN DEEP AQUIFER MEDIA - PHASE II  

SciTech Connect (OSTI)

In 1998 Battelle was selected by the U.S. Department of Energy's (DOE) National Energy Technology Laboratory (NETL) under a Novel Concepts project grant to continue Phase II research on the feasibility of carbon dioxide (CO{sub 2}) sequestration in deep saline formations. The focus of this investigation is to conduct detailed laboratory experiments to examine factors that may affect chemical sequestration of CO{sub 2} in deep saline formations. Reactions between sandstone and other geologic media from potential host reservoirs, brine solutions, and CO{sub 2} are being investigated under high-pressure conditions. Some experiments also include sulfur dioxide (SO{sub 2}) gases to evaluate the potential for co-injection of CO{sub 2} and SO{sub 2} related gases in the deep formations. In addition, an assessment of engineering and economic aspects is being conducted. This current Technical Progress Report describes the status of the project as of September 2000. The major activities undertaken during the quarter included several experiments conducted to investigate the effects of pressure, temperature, time, and brine composition on rock samples from potential host reservoirs. Samples (both powder and slab) were taken from the Mt. Simon Sandstone, a potential CO{sub 2} host formation in the Ohio, the Eau Claire Shale, and Rome Dolomite samples that form the caprock for Mt. Simon Sandstone. Also, a sample with high calcium plagioclase content from Frio Formation in Texas was used. In addition, mineral samples for relatively pure Anorthite and glauconite were experimented on with and without the presence of additional clay minerals such as kaolinite and montmorillonite. The experiments were run for one to two months at pressures similar to deep reservoirs and temperatures set at 50 C or 150 C. Several enhancements were made to the experimental equipment to allow for mixing of reactants and to improve sample collection methods. The resulting fluids (gases and liquids) as well as the rock samples were characterized to evaluate the geochemical changes over the experimental period. Preliminary results from the analysis are presented in the report. More detailed interpretation of the results will be presented in the technical report at the end of Phase II.

Neeraj Gupta; Bruce Sass; Jennifer Ickes

2000-11-28T23:59:59.000Z

Note: This page contains sample records for the topic "mt simon sandstone" 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.


421

A variable for measuring masses at hadron colliders when missing energy is expected; mT2: the truth behind the glamour  

E-Print Network [OSTI]

AMSB-like points discussed in section 4.2. The hadronic branching ratios can be found in [10]. m?+1 #7;M?˜1 Point (GeV) (MeV) ?+1 ? ?01 e+?e ?+1 ? ?01 µ+?µ SPS-300 165 886 17.0% 15.9% SPS-250 159 1798 21.9% 21.5% A-250 101 766 15.4% 13.9% A-200 97 1603... ‘natural’ way. Readers who would prefer a ‘top down’ description of mT 2, i.e. a description which starts with a definition and then works towards its consequences, are directed to skip to section 3 where this approach is taken. The concrete example which...

Barr, Alan; Lester, Christopher G; Stephens, Phil

422

Arnaud Rykner, L'incomprhensible dans le tapis (Sur Henry James) , in L'Incomprhensible. Littrature, rel, visuel, sous la dir. de M.-T. Mathet, Paris, L'Harmattan,  

E-Print Network [OSTI]

'Incompréhensible. Littérature, réel, visuel, sous la dir. de M.-T. Mathet, Paris, L'Harmattan, coll. Champs visuels, 2003, p.-T. Mathet, Paris, L'Harmattan, coll. Champs visuels, 2003, p. 137-165. 2 Georges Didi-Huberman et dans un

Boyer, Edmond

423

Visualizing the Surface Infrastructure Used to Move 2 MtCO2/year from the Dakota Gasification Company to the Weyburn CO2 Enhanced Oil Recovery Project: Version of July 1, 2009  

SciTech Connect (OSTI)

Google Earth Pro has been employed to create an interactive flyover of the world’s largest operational carbon dioxide capture and storage project. The visualization focuses on the transport and storage of 2 MtCO2/year which is captured from the Dakota Gasification Facility (Beula, North Dakota) and transported 205 miles and injected into the Weyburn oil field in Southeastern Saskatchewan.

Dooley, James J.

2009-07-09T23:59:59.000Z

424

Investigation and evaluation of geopressured-geothermal wells. Final report: Beulah Simon No. 2 Well, Vermilion Parish, Louisiana. Volume I. Completion and testing  

SciTech Connect (OSTI)

Geopressured-geothermal (Geo{sup 2}) test operations were conducted at the Beulah Simon No. 2 well site during the period from September through December 1979. The well provided the second geopressured-geothermal test to be completed under the DOE-Gruy Well of Opportunity program. The completion in a geopressured aquifer of Oligocene age at approximately 14,700 feet and the testing of hot salt water from this zone were accomplished without significant difficulty. Some problems were encountered with the wireline and wireline high-pressure lubricator associated with the running of bottomhole instruments. The objectives of the project were all accomplished, and good test data were obtained on the flow rates of gas and water. The gas content was 24 standard cubic feet per stock tank barrel of water. The disposal well accepted the full wellhead stream at temperatures as high as 255{sup 0}F (124{sup 0}C). Over the 10-day flow period the hot brine did not appear to adversely affect the clay minerals in the disposal aquifer. A conclusion from this operation is that presently available wirelines and pressure lubricators are not adaptable for use with uninhibited well fluids under flowing conditions. In addition, this test demonstrated that injection of scale inhibitor down the annulus eliminated scale buildup within the flow string and surface facilities. (MHR)

Dobson, R.J.; Hartsock, J.H.; McCoy, R.L.; Rodgers, J.A.

1980-07-01T23:59:59.000Z

425

Variable Density Flow Modeling for Simulation Framework for Regional Geologic CO{sub 2} Storage Along Arches Province of Midwestern United States  

SciTech Connect (OSTI)

The Arches Province in the Midwestern U.S. has been identified as a major area for carbon dioxide (CO{sub 2}) storage applications because of the intersection of Mt. Simon sandstone reservoir thickness and permeability. To better understand large-scale CO{sub 2} storage infrastructure requirements in the Arches Province, variable density scoping level modeling was completed. Three main tasks were completed for the variable density modeling: Single-phase, variable density groundwater flow modeling; Scoping level multi-phase simulations; and Preliminary basin-scale multi-phase simulations. The variable density modeling task was successful in evaluating appropriate input data for the Arches Province numerical simulations. Data from the geocellular model developed earlier in the project were translated into preliminary numerical models. These models were calibrated to observed conditions in the Mt. Simon, suggesting a suitable geologic depiction of the system. The initial models were used to assess boundary conditions, calibrate to reservoir conditions, examine grid dimensions, evaluate upscaling items, and develop regional storage field scenarios. The task also provided practical information on items related to CO{sub 2} storage applications in the Arches Province such as pressure buildup estimates, well spacing limitations, and injection field arrangements. The Arches Simulation project is a three-year effort and part of the United States Department of Energy (U.S. DOE)/National Energy Technology Laboratory (NETL) program on innovative and advanced technologies and protocols for monitoring/verification/accounting (MVA), simulation, and risk assessment of CO{sub 2} sequestration in geologic formations. The overall objective of the project is to develop a simulation framework for regional geologic CO{sub 2} storage infrastructure along the Arches Province of the Midwestern U.S.

Joel Sminchak

2011-09-30T23:59:59.000Z

426

Simon Fraser University Annual Report Fiscal Year 1999/2000 At the heart of the University, the SFU Library is dedicated toAt the heart of the University, the SFU Library is dedicated toAt the heart of the University, the SFU Library is dedicated toAt the  

E-Print Network [OSTI]

SFU Simon Fraser University Annual Report Fiscal Year 1999/2000 At the heart of the University, the SFU Library is dedicated toAt the heart of the University, the SFU Library is dedicated toAt the heart of the University, the SFU Library is dedicated toAt the heart of the University, the SFU Library is dedicated

427

Mitochondrial Variants in Schizophrenia, Bipolar Disorder, and Major Depressive Disorder  

E-Print Network [OSTI]

Genomics 29: 26. Coskun PE, Beal MF, Wallace DC (2004)MT, Simon DK, Ahn CH, Kim LM, Beal MF (2002) High aggregate92. Gibson GE, Ratan RR, Beal MF (2008) Mitochondria and

2009-01-01T23:59:59.000Z

428

Recovery Act: Understanding the Impact of CO{sub 2} Injection on the Subsurface Microbial Community in an Illinois Basin CCS Reservoir: Integrated Student Training in Geoscience and Geomicrobiology  

SciTech Connect (OSTI)

An integrated research and teaching program was developed to provide cross-­?disciplinary training opportunities in the emerging field of carbon capture and storage (CCS) for geobiology students attending the University of Illinois Urbana-­?Champaign (UIUC). Students from across the UIUC campus participated, including those from the departments of Geology, Microbiology, Biochemistry, Civil and Environmental Engineering, Animal Sciences and the Institute for Genomic Biology. The project took advantage of the unique opportunity provided by the drilling and sampling of the large-­?scale Phase III CCS demonstration Illinois Basin -­? Decatur Project (IBDP) in the central Illinois Basin at nearby Decatur, Illinois. The IBPD is under the direction of the Illinois State Geological Survey (ISGS, located on the UIUC campus) and the Midwest Geological Sequestration Consortium (MGSC). The research component of this project focused on the subsurface sampling and identification of microbes inhabiting the subsurface Cambrian-­?age Mt. Simon Sandstone. In addition to formation water collected from the injection and monitoring wells, sidewall rock cores were collected and analyzed to characterize the cements and diagenetic features of the host Mt. Simon Sandstone. This established a dynamic geobiological framework, as well as a comparative baseline, for future studies of how CO2 injection might affect the deep microbial biosphere at other CCS sites. Three manuscripts have been prepared as a result of these activities, which are now being finalized for submission to top-­?tier international peer-­?reviewed research journals. The training component of this project was structured to ensure that a broad group of UIUC students, faculty and staff gained insight into CCS issues. An essential part of this training was that the UIUC faculty mentored and involved undergraduate and graduate students, as well as postdocs and research scientists, at all stages of the project in order to develop CCS-­?focused classroom and field courses, as well as seminars. This program provided an excellent opportunity for participants to develop the background necessary to establish longer-­?term research in CCS-­?related geology and microbial ecology. Further, the program provided an ongoing dynamic platform to foster long-­?term collaboration with the regional ISGS and MGSC sequestration partnership, while offering hands-­?on, applied learning experiences.

Fouke, Bruce

2013-03-31T23:59:59.000Z

429

Miniature MT optical assembly (MMTOA)  

DOE Patents [OSTI]

An optical assembly (10) includes a rigid mount (12) with a recess (26) proximate a first side thereof, a substrate (14), and an optical die (16) flip-chip bonded to the substrate (14). The substrate (14) is secured to the first side of the mount and includes a plurality of die bonding elements (40), a plurality of optical apertures (32), and a plurality of external bonding elements (42). A plurality of traces (44) interconnect the die bonding elements (40) and the external bonding elements (42). The optical die (16) includes a plurality of optical elements, each element including an optical signal interface (48), the die being bonded to the plurality of die bonding elements (40) such that the optical signal interface (48) of each element is in registry with an optical aperture (32) of the substrate (14) and the die (16) is at least partially enclosed by the recess (26).

Laughlin, Daric (Overland Park, KS); Abel, Phillip (Overland Park, KS)

2008-04-01T23:59:59.000Z

430

Stress corrosion crack growth in porous sandstones  

E-Print Network [OSTI]

Stress corrosion crack growth occurs when the chemical weakening of strained crack tip bonds facilitates crack propagation. I have examined the effect of chemical processes on the growth of a creack population by carrying out triaxial compression...

Ojala, Ira O

431

Trace fossil assemblages in selected shelf sandstones  

E-Print Network [OSTI]

Harris. Thank you, good luck in the future, and may God bless you all. vi TABLE OF CONTENTS INTRODUCTION Background Objectives Methods . TRACE FOSSIL IDENTIFICATION IN CORES Introduction Description of Selected Trace Fossils TRACE FOSSILS..., the trace foss11 distributions agreed with those of the ichnofacies described by Seilacher (1978) and with the known environmental distributions compiled by Chamberlain (1978), but many trace fossils have widespread occurrences that limit...

Locke, Kathleen Ann

1983-01-01T23:59:59.000Z

432

Numerical simulation of sandstone reservoir models  

E-Print Network [OSTI]

. Case 3 - Alternatin h1 h and low ermeabilities Waterflood performance of the Case 3 reservoir is shown in Figures 19 and 20. The process 1s practically rate insensitive for both the high and low viscosity ratio cases because of the ex istence... The results of the water flood study indicate that lower rates result i n higher waterflood oil recoveries from heterogeneous reservoirs, particularly where high oil-water viscosity ratios exist. These results support the conclusions of Jordan et. al...

Gross, Stephen Joseph

1983-01-01T23:59:59.000Z

433

Alkali solution treatment on sandstone cores  

E-Print Network [OSTI]

was used for filtering the solution before the injection into the core. Hassler-t e Core Holder A stainless steel core holder was used to hold the core for treatment with the solutions. The core sample was positioned in the center of the core holder... and heat the water in the flask. Electric Heatin Ta e A silicone rubber embedded flexible heating tape was used to wrap the core holder to heat the core sample to the desired temperature. The maximum 0 continuous operating temperature of the tape...

Lee, Suk Jin

2012-06-07T23:59:59.000Z

434

Bernie Simon 9 October 96  

E-Print Network [OSTI]

followed by three arguments. The rst argument is the input load le, the second argument is the output load and the action. Rules are applied in the following way. The task reads a row from the input load le the new rows are written to the output load le. For example, suppose the rules le contained the following

Sirianni, Marco

435

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

an effective preventive maintenance program, and assists Superintendents in organizing and performing scheduled, and coordinating Preventive Maintenance Programs for all critical equipment in facilities at the SFU Burnaby campus the effectiveness of scheduled maintenance. Identifies preventive maintenance backlogs within trades shops

436

NEWCDBS Installation Instructions Bernie Simon  

E-Print Network [OSTI]

OS (.sparc), VAX VMS (.vax), and Alpha VMS (.alpha). Since the name of the make le is nonstandard, the make the Solaris version of the make le and the command mms /descrip=makefile.vax runs the Vax version. The top

Sirianni, Marco

437

Geography 213 Simon Fraser University  

E-Print Network [OSTI]

of life. Nature, 439, 411-418. Field trip report due November 14, 2014 @ 10:30 FINAL EXAM: December 14, and topics Review of basic geological concepts Historical conceptions of the landscape (Davis, Gilbert, Leopold, Wolman, modern era) Readings: Review geological concepts from GEOG 111 and/or EASC 101 textbooks

Venditti, Jeremy G.

438

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

requirements for software testing and operations; the design of testing scenarios and scripts and ho Position Number: 112049 A. IDENTIFICATION Position Title: Business Analyst NameofEmployee: Department: Career Management Centre Position Reports To (Title): Associate Director, EmployerRelations Description

Delgrande, James P.

439

Engagement Indicators Simon Fraser University  

E-Print Network [OSTI]

Faculty Interaction Effective Teaching Practices Quality of Interactions Supportive Environment Report sections medium, and .8 large. Comparisons with an effect size of at least .3 in magnitude (before rounding institutions. Academic Challenge Learning with Peers Experiences with Faculty Campus Environment Engagement

440

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

with proficiency in all phases of the systems development life cycle; researches, evaluates and recommends basic of professional and technical staff working in any phase of the software systems development life cycle involving of Information Technology: Application Software Development & Systems Integration) Name of Employee: Department

Note: This page contains sample records for the topic "mt simon sandstone" 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

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

, and administration activities of the faculty. Participates in all phases of the systems development life cycle

442

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

of the systems development life cycle; conducts research for feasibility studies and cost benefit analyses

443

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

development life cycle; conducts research for feasibility studies and cost benefit analyses; reviews of time spent on each particular task. Description % of Time Participates in most phases of the systems

444

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

Position Number: 115669 A. IDENTIFICATION B. POSITION SUMMARY Briefly describe the primary function information, conducting research, profiling best practices, preparing materials and reports and 40% Position and purpose of the position in one or two sentences. As a member of the Applied Sciences Student Affairs Unit

445

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

lifecycle including: design criteria, development of specifications, and programming; acquisition and support. Responsible for all aspects of the web development lifecycle including: design criteria

446

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

DESCRIPTION A. IDENTIFICATION Position Number: 100993 Position Title: Student Recruiter, French Cohort Program, the Student Recruiter is responsible for recruiting prospective students to the French Cohort Program of educational, community and professional settings. The Student Recruiter presents information to a broad

447

An interview with Simon Blackburn  

E-Print Network [OSTI]

that - then it becomes a mystery why we actually express ourselves in ways which make it look like ethics are much more a question of fact - e.g. its wrong to torture people; one possible response is to say we just deceive ourselves, a popular position in the 1970s; I...

Blackburn, Simon

2010-01-01T23:59:59.000Z

448

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

the visual identity and brand image expression of all communications materials ensuring that web of campus and university communications and brand marketing strategies. The incumbent of the position and brand management. The Communications Officer also plays a role in the coordination and marketing

449

UNIVERSIDAD SIMON BOLIVAR Consejo Directivo  

E-Print Network [OSTI]

Comisión Permanente sobre contrataciones, renovaciones de contratos, ingresos y ascensos al escalafón del Proceso de Admisión 2012 X. Informes Académico y Administrativo - Cursos Intensivos 2012 XI. Designación

Vásquez, Carlos

450

UNIVERSIDAD SIMON BOLIVAR Consejo Directivo  

E-Print Network [OSTI]

contrataciones, renovaciones de contratos, ingresos y ascensos al escalafón del personal académico b. Informe de conferimiento de distinción honorífica "Profesor Emérito" (*) XIII. Informe sobre el proceso de admisión de la

Vásquez, Carlos

451

UNIVERSIDAD SIMON BOLIVAR Consejo Directivo  

E-Print Network [OSTI]

Comisión Permanente sobre contrataciones, renovaciones de contratos, ingresos y ascensos al escalafón del proceso de inscripción de los bachilleres asignados a la USB por el proceso CNU-OPSU 2012 XIII. Convenio

Vásquez, Carlos

452

UNIVERSIDAD SIMON BOLIVAR Consejo Directivo  

E-Print Network [OSTI]

Comisión Permanente sobre contrataciones, renovaciones de contratos, ingresos y ascensos al escalafón del año 2013 X. Informe General de Año Sabático 2014-2015 XI. Informe del proceso de inscripción de los bachilleres asignados a la USB por el proceso CNU-OPSU 2013 XII. Informe sobre los procesos de admisión de la

Vásquez, Carlos

453

UNIVERSIDAD SIMON BOLIVAR Consejo Directivo  

E-Print Network [OSTI]

Comisiones Permanentes: a. Informe de la Comisión Permanente sobre contrataciones, renovaciones de contratos estudiantes con discapacidad X. Informe del proceso de inscripción de los bachilleres asignados a la USB por el proceso CNU-OPSU 2013 (*) XI. Reestructuracón de la comisión sobre derechos de autor y patente

Vásquez, Carlos

454

UNIVERSIDAD SIMON BOLIVAR Consejo Directivo  

E-Print Network [OSTI]

Permanentes: a. Informe de la Comisión Permanente sobre contrataciones, renovaciones de contratos, ingresos y FONJUSIBO XIV. Manual de Organización del Decanato de Estudios Tecnológicos XV. Informe sobre el proceso de

Vásquez, Carlos

455

UNIVERSIDAD SIMON BOLIVAR Consejo Directivo  

E-Print Network [OSTI]

la Comisión de Convenios b. Informe de la Comisión Permanente sobre contrataciones, renovaciones de VIII. Resultado de la averiguación administrativa sobre los hechos irregulares incurridos en el proceso

Vásquez, Carlos

456

Xinming (Simon) Ou Curriculum Vitae  

E-Print Network [OSTI]

2012. · Idaho National Laboratory, Research Associate, May 2006 ­ Aug 2006. · Purdue University, Post Research Instrumentation Program (DURIP), Air Force Office of Scientific Research (AFOSR). $605,650, 9 Office of Scientific Research. $1,000,311, 4/1/2012-3/31/2017. 6. An Innovative Cybersecurity Curriculum

Ou, Xinming "Simon"

457

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

and digital assets programs; develops and administers a media and digital assets training program; provides professional support for the ongoing assessment of digital and media resources; develops and establishes file media and digital assets. Develops and administers a media and digital assets training program

458

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

and inventories; identification and interviewing of internal resource persons; analysis and synthesis of data

459

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

and distributes information and updates regarding spaces and other activities in the Education Building. Gives Projects Administrator will manage a special project underway to review, audit, and renovate the Education particular task. Description % of Time 1. Education Building ­ Operations and Guidelines Implementation

460

UNIVERSIDAD SIMON BOLIVAR VICERRECTORADO ADMINISTRATIVO  

E-Print Network [OSTI]

emergencia, arquitectura y obras civiles Coordinadora Prof. Myriam Araujo Sartenejas, Mayo 2012 #12 emergencia, arquitectura y obras civiles N°CD/2012-046-2-2 Objeto del Concurso Cerrado: El objeto del, Sistema contra incendios y emergencia, arquitectura y obras civiles, de la Universidad Simón Bolívar, Sede

Vásquez, Carlos

Note: This page contains sample records for the topic "mt simon sandstone" 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

HUMAN RESOURCES SIMON FRASER UNIVERSITY  

E-Print Network [OSTI]

staff in the delivery of a comprehensive residence life program. The position responds and manages properties that promotes and supports the academic and personal endeavors of residents. Through collaboration-learning environment for residence students that promotes academic and personal development. The position collaborates

462

Announcements Pick up old homework & MT  

E-Print Network [OSTI]

-REPLICATING, ENCAPSULATED, CHEMICAL SYSTEM THAT UNDERGOES DARWINIAN EVOLUTION" Important points to examine: -What/Archean transition 4.0 ­ 3.5 billion years ago #12;At this time the solar system was bombarded with comets

Mojzsis, Stephen J.

463

Wind speed vertical distribution at Mt. Graham  

E-Print Network [OSTI]

The characterization of the wind speed vertical distribution V(h) is fundamental for an astronomical site for many different reasons: (1) the wind speed shear contributes to trigger optical turbulence in the whole troposphere, (2) a few of the astroclimatic parameters such as the wavefront coherence time (tau_0) depends directly on V(h), (3) the equivalent velocity V_0, controlling the frequency at which the adaptive optics systems have to run to work properly, depends on the vertical distribution of the wind speed and optical turbulence. Also, a too strong wind speed near the ground can introduce vibrations in the telescope structures. The wind speed at a precise pressure (200 hPa) has frequently been used to retrieve indications concerning the tau_0 and the frequency limits imposed to all instrumentation based on adaptive optics systems, but more recently it has been proved that V_200 (wind speed at 200 hPa) alone is not sufficient to provide exhaustive elements concerning this topic and that the vertical d...

Hagelin, S; Lascaux, F

2010-01-01T23:59:59.000Z

464

Controlled Source Audio MT | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 NoPublic Utilities Address: 160Benin:EnergyWisconsin:2003) | OpenMinor Permit ApplicationsSaskatchewan,Controlled

465

Havre, MT Natural Gas Exports to Canada  

Gasoline and Diesel Fuel Update (EIA)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May Jun Jul(Summary) " ,"ClickPipelines About U.S.30Natural Gas Glossary529 6330 0 1 0 058.588,219 719,435

466

Category:Billings, MT | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home Page on Office of InspectorConcentrating SolarElectricEnergyCTBarreis aCallahanWind Farm JumpBLM) Lease. Add.png Add a new

467

Mt Rainier Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia: Energy Resources Jump to:46 -Energieprojekte3 ClimateSpurr GeothermalCarmel Public Utility Co Jump to:Rainier

468

Mt Rainier Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia: Energy Resources Jump to:46 -Energieprojekte3 ClimateSpurr GeothermalCarmel Public Utility Co Jump

469

Mt Ranier Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data CenterFranconia, Virginia: Energy Resources Jump to:46 -Energieprojekte3 ClimateSpurr GeothermalCarmel Public Utility Co JumpRanier

470

Marysville Mt Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revision hasInformation Earth's Heat JumpIncMAKGalway Bay(HeldManhattan,andMarsInformationWind

471

Mt Peak Utility | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revision hasInformation Earth's HeatMexico: EnergyMithun Jump to:Moe WindMontMoraineAbbeyIMozart Jump

472

Mt Poso Cogeneration | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revision hasInformation Earth's HeatMexico: EnergyMithun Jump to:Moe WindMontMoraineAbbeyIMozart JumpPoso

473

Mt Signal Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revision hasInformation Earth's HeatMexico: EnergyMithun Jump to:Moe WindMontMoraineAbbeyIMozart

474

Babb, MT Natural Gas Export to Canada  

Gasoline and Diesel Fuel Update (EIA)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May Jun Jul(Summary) " ,"ClickPipelines About U.S.30Natural Gas Glossary529 633 622 566 8021 1 2 22008662 564 1,1460 0 20 0 0 122

475

Rethinking Newton's Principia Simon Saunders1  

E-Print Network [OSTI]

That is not the strategy taken here. My objective is to give a consistent reading of Newton's Principia ­ discarding of mass of the solar system), wrongly identi...ed by Newton as inertial, is exemplary: it is a local total energy and angular momentum zero can be de...ned. No such constraint ­ and no such prediction

Saunders, Simon

476

UNIVERSIDAD SIMON BOUVAR VICE-RECTORADO ADMINISTRATIVO  

E-Print Network [OSTI]

) y el de Recursos Naturales Renovables (IRNR) como órganos especializados en áreas específicas; el recursos humanos y económicos requeridos por el área de Ciencias Biológicas. 2.t2, Funciones. a) Manejar

Vásquez, Carlos

477

Simon Fraser University Campus Sustainability Assessment  

E-Print Network [OSTI]

from the generic Campus Sustainability Framework to the SFU context. Linkages among the environmental

478

CSRI Senior Fellows Simon Zadek and Salil  

E-Print Network [OSTI]

billion people lack access to drinking water, nearly 2.6 billion people lack access to sanitation to Water and Sanitation Program Through research, publications, and dialogue among practitioners and academics, the Carr Center's Human Rights to Water and Sanitation Program seeks to provide critical

Heller, Eric

479

Updated 2-09 Simon Chang  

E-Print Network [OSTI]

and atmospheric effects on naval weapon systems, and to develop numerical analysis and prediction systems. Dr

480

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Turismo, Hotelería y Hospitalidad), María Fátima Pinho (Coordinadora Encargada de Comercio Exterior y Lic. en Comercio Internacional), Oranys Marín (Coordinador de Lic. Biología). Invitados Permanentes-2013, 08-2013 y 09-2013 fue diferida para próximas sesiones del Consejo Asesor. 3.- Informe de la Decana La

Vásquez, Carlos

Note: This page contains sample records for the topic "mt simon sandstone" 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

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Ingeniería de Mantenimiento) y Enio Ortiz (Coordinador encargado de Comercio Exterior y Lic. Comercio Acta 10.2012 3.- Informe de la Decana La Decana dio inicio a la sesión, dando la bienvenida a los Consejo Directivo, quien estará acompañando al Cuerpo durante un año. Prosiguió su informe notificando

Vásquez, Carlos

482

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Encargado de Turismo, Hotelería y Hospitalidad), María Fátima Pinho (Coordinadora Encargada de Comercio Exterior y Lic. en Comercio Internacional), René Escalante (Coordinador de Lic. Matemáticas), Ana María.- Informe de la Decana La Decana dio la bienvenida a la sesión a la Profa. María Elena Ludeña, Coordinadora

Vásquez, Carlos

483

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

. Comercio Internacional) Invitados Permanentes: Profesores: Kenyer Domínguez (Coordinador de Cooperación/2011 Aprobadas. 3.- Informe de la Decana La Decana dio inicio a su informe dando la bienvenida al Prof. Henry Vicente quien asiste en representación de la Coordinación de Arquitectura. Continuó su informe

Vásquez, Carlos

484

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Ing. de Telecomunicaciones), María Fátima Pinho (en representación de la Coordinación de Comercio Exterior y Lic. en Comercio Internacional), María Bouzas (Representante Estudiantil). Invitados Permanentes 01-2013 y 02-2013 Fueron diferidas las actas, al considerar el orden del día. 3.- Informe de la

Vásquez, Carlos

485

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Turismo, Hotelería y Hospitalidad), María Fátima Pinho (Coordinadora de Comercio Exterior y Lic. en Comercio Internacional), René Escalante (Coordinador de Lic. Matemáticas). Invitados Permanentes: Lic. Lucy-2013 y 05-2013 3.- Informe de la Decana La Decana, Prof. Gómez, le dio la bienvenida a la sesión, a los

Vásquez, Carlos

486

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

), María Fátima Pinho (Coordinadora Encargada de Comercio Exterior y Lic. en Comercio Internacional), René 06-2013, 07-2013 y 08-2013 Fueron aprobadas las actas 06-2013, 07-2013 y 08-2013 3.- Informe de la la presentación de su informe, comunicando lo acontecido y acordado en los Consejos Directivos del 25

Vásquez, Carlos

487

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Jiménez (Coordinador de Lic. Comercio Internacional) Invitados Permanentes: Profesores: Kenyer Domínguez, derivado que fue enviada tardíamente para la revisión de los consejeros. 3.- Informe de la Decana La Decana dio inicio a su informe refiriéndose a los siguientes aspectos discutidos en: Consejos Directivos del

Vásquez, Carlos

488

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Encargado de Turismo, Hotelería y Hospitalidad), María Fátima Pinho (Coordinadora Encargada de Comercio Exterior y Licenciatura en Comercio Internacional), René Escalante (Coordinador de Lic. Matemáticas aprobadas las actas 09-2013 y 10-2013. 3.- Informe de la Decana La Decana le dio la bienvenida a la Profa

Vásquez, Carlos

489

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

.- Informe de la Decana La decana dio inicio a su informe dando la bienvenida al Prof. Jorge Ramírez, quien), continuó el informe refiriéndose a los siguientes aspectos discutidos en: Consejos Académicos del 05 y 19 2010. En esta reunión fue aprobado el proyecto de carrera de la Licenciatura en Comercio #12;cont

Vásquez, Carlos

490

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Decana dio inicio a su informe dando la bienvenida al Prof Enio Ortiz (Coordinación Encargado de Comercio Turismo, Hotelería y Hospitalidad), Enio Ortiz (Coordinador Encargado de Comercio Exterior y Lic. Comercio del Acta 01/2012 Fueron aprobadas las actas N° 02.2012, 03.12, 04.12. 3.- Informe de la Decana La

Vásquez, Carlos

491

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Lic. Comercio Internacional),Omar Pérez (Director de Desarrollo Estudiantil), la representación del aprobada sin modificaciones. 2.- Consideración del Acta 05/2011 Aprobada sin modificaciones. 3.- Informe de la Decana La Decana dio inicio a su informe refiriéndose a los siguientes aspectos discutidos en

Vásquez, Carlos

492

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

(Coordinador de Cooperación Técnica y Desarrollo Social), representación de la Coordinación de Comercio Exterior y Lic. Comercio Internacional, Omar Pérez (Director de Desarrollo Estudiantil) y Br. Esay Boscán Acta 01.12 3. Informe de la Decana 4. Talleres de Reflexión del Ciclo Básico en las Carreras Largas 5

Vásquez, Carlos

493

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Hospitalidad), María Fátima Pinho (Coordinadora Encargada de Comercio Exterior y Licenciatura en Comercio lista a tiempo para el consejo plenario. 3.- Informe del Decano El Decano le dio la bienvenida al Prof informe, comunicando lo acontecido y acordado en las sesiones de los Consejos Directivos del 15 de enero

Vásquez, Carlos

494

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Hospitalidad), María Fátima Pinho (Coordinadora Encargada de Comercio Exterior y Lic. en Comercio Internacional del acta. 2.- Aprobación del Acta 04-2013 La aprobación del Acta 04-2013 quedó diferida. 3.- Informe informe notificando sobre los siguientes aspectos discutidos en las sesiones correspondientes a los

Vásquez, Carlos

495

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Coordinador de Comercio Exterior y Lic. en Comercio Internacional), Luis Urbano (Coordinador de Ing. de.- Informe de la Decana La Decana dio inicio a su informe agradeciendo a la Profa. Jeanette González (quien

Vásquez, Carlos

496

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

, Hotelería y Hospitalidad), Enio Ortiz (Coordinador encargado de Comercio Exterior y Lic. en Comercio del punto 2. 2.- Informe de la Decana La Decana dio inicio a su informe dando la bienvenida a los

Vásquez, Carlos

497

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

encargado de Comercio Exterior y Lic. Comercio Internacional), Representante Estudiantil, quienes referida para la próxima sesión al someter el orden del día. 3.- Informe de la Decana La Decana dio inicio a su informe con la siguiente información correspondiente a los aspectos informados, tratados y

Vásquez, Carlos

498

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Comercio Exterior y Licenciatura en Comercio Internacional), René Escalante (Coordinador de Lic.- Informe de la Decana La Decana María Gabriela Gómez inició su informe, dando la bienvenida a los de su informe, comunicando lo acontecido y acordado en las sesiones de los Consejos Directivos del 04

Vásquez, Carlos

499

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Técnica y Desarrollo Social), representación de la Coordinación de Comercio Exterior y Lic. En Comercio consejeros la agenda del día, la cual fue aprobada sin modificaciones 2.- Informe de la Decana La Decana dio

Vásquez, Carlos

500

UNIVERSIDAD SIMON BOLIVAR Decanato de Estudios Profesionales  

E-Print Network [OSTI]

Jiménez (Coordinador de Lic. en Comercio Internacional) Invitados Permanentes: Profesores: Kenyer consideración de los consejeros la agenda del día, la cual fue aprobada con el diferimiento del punto 8: Informe Medina en relación a su voto salvado en el punto del informe de la Decana, relacionado a la información

Vásquez, Carlos