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  1. South Texas Blending | Open Energy Information

    Open Energy Info (EERE)

    search Name: South Texas Blending Place: Laredo, Texas Zip: 78045 Product: Biodiesel producer based in Texas. References: South Texas Blending1 This article is a stub....

  2. Texas Nuclear Profile - South Texas Project

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

    South Texas Project" "Unit","Summer capacity (mw)","Net generation (thousand mwh)","Summer capacity factor (percent)","Type","Commercial operation date","License expiration date" 1,"1,280","11,304",100.8,"PWR","application/vnd.ms-excel","application/vnd.ms-excel"

  3. Texas-Louisiana- Mississippi Salt Basin Greater Green River Basin

    Gasoline and Diesel Fuel Update (EIA)

    Texas-Louisiana- Mississippi Salt Basin Greater Green River Basin W. Gulf Coast Basin ... Major Tight Gas Plays, Lower 48 States 0 200 400 100 300 Miles Source: Energy ...

  4. Texas

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

    Texas

  5. Geoscience/engineering characterization of the interwell environment in carbonate reservoirs based on outcrop analogs, Permian Basin, West Texas and New Mexico - petrophysical characterization of the South Cowden Grayburg Reservoir, Ector County, Texas. Final report

    SciTech Connect (OSTI)

    Lucia, F.J.

    1997-06-01

    Reservoir performance of the South Cowden Grayburg field suggests that only 21 percent of the original oil in place has been recovered. The purpose of this study is to construct a realistic reservoir model to be used to predict the location of the remaining mobile oil. Construction of reservoir models for fluid-flow simulation of carbonate reservoirs is difficult because they typically have complicated and unpredictable permeability patterns. Much of the difficulty results from the degree to which diagenetic overprinting masks depositional textures and patterns. For example, the task of constructing a reservoir model of a limestone reservoir that has undergone only cementation and compaction is easier than constructing a model of a karsted reservoir that has undergone cavern formation and collapse as well as cementation and compaction. The Permian-age carbonate-ramp reservoirs in the Permian Basin, West Texas and New Mexico, are typically anhydritic dolomitized limestone. Because the dolomitization occurred soon after deposition, depositional fabrics and patterns are often retained, and a reservoir model can be constructed using depositional concepts. Recent studies of the San Andres outcrop in the Guadalupe Mountains and the Seminole San Andres reservoir in the Permian Basin illustrate how depositional fabrics and patterns can be used to construct a reservoir model when depositional features are retained.

  6. Geoscience/engineering characterization of the interwell environment in carbonate reservoirs based on outcrop analogs, Permian Basin, West Texas and New Mexico--waterflood performance analysis for the South Cowden Grayburg Reservoir, Ector County, Texas. Final report

    SciTech Connect (OSTI)

    Jennings, J.W. Jr.

    1997-05-01

    A reservoir engineering study was conducted of waterflood performance in the South Cowden field, an Upper Permian Grayburg reservoir on the Central Basin Platform in West Texas. The study was undertaken to understand the historically poor waterflood performance, evaluate three techniques for incorporating petrophysical measurements and geological interpretation into heterogeneous reservoir models, and identify issues in heterogeneity modeling and fluid-flow scaleup that require further research. The approach included analysis of relative permeability data, analysis of injection and production data, heterogeneity modeling, and waterflood simulation. The poor South Cowden waterflood recovery is due, in part, to completion of wells in only the top half of the formation. Recompletion of wells through the entire formation is estimated to improve recovery in ten years by 6 percent of the original oil in place in some areas of the field. A direct three-dimensional stochastic approach to heterogeneity modeling produced the best fit to waterflood performance and injectivity, but a more conventional model based on smooth mapping of layer-averaged properties was almost as good. The results reaffirm the importance of large-scale heterogeneities in waterflood modeling but demonstrate only a slight advantage for stochastic modeling at this scale. All the flow simulations required a reduction to the measured whole-core k{sub v}/k{sub h} to explain waterflood behavior, suggesting the presence of barriers to vertical flow not explicitly accounted for in any of the heterogeneity models. They also required modifications to the measured steady-state relative permeabilities, suggesting the importance of small-scale heterogeneities and scaleup. Vertical flow barriers, small-scale heterogeneity modeling, and relative permeability scaleup require additional research for waterflood performance prediction in reservoirs like South Cowden.

  7. Ben South (Tannehill) oil field, Stonewall, County, Texas

    SciTech Connect (OSTI)

    Hillock, R.T.

    1984-01-01

    Ben South is one of 157 Tannehill oil fields on the northeastern shelf of the Permian basin. Texas Railroad Commission District 7B has 66 Tannehill oil fields while District 8A has 21. The discovery well for the Ben South field was the Ryder Scott Management (Sauder) 1 McMeans, completed in 1973. Ben South field production has totaled 749,340 bbl of oil through March 1983 from 13 wells. Oil production is from the lower Tannehill (lower Wolfcamp) sands underlying the Stockwether Limestone. These Tannehill sands were deposited in a fluvial environment. Channel-fill and point-bar deposits make up the pay sands. The trapping mechanism is both stratigraphic and structural.

  8. South Houston, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    article is a stub. You can help OpenEI by expanding it. South Houston is a city in Harris County, Texas. It falls under Texas's 29th congressional district.12 References...

  9. Homestead Meadows South, Texas: Energy Resources | Open Energy...

    Open Energy Info (EERE)

    help OpenEI by expanding it. Homestead Meadows South is a census-designated place in El Paso County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  10. Hidalgo County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas San Juan, Texas San Manuel-Linn, Texas Scissors, Texas South Alamo, Texas Sullivan City, Texas Villa Verde, Texas Weslaco, Texas West Sharyland, Texas Retrieved from...

  11. Willacy County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas Lasara, Texas Los Angeles Subdivision, Texas Lyford South, Texas Lyford, Texas Port Mansfield, Texas Ranchette Estates, Texas Raymondville, Texas San Perlita, Texas Santa...

  12. Structural evolution of Val Verde basin, west Texas

    SciTech Connect (OSTI)

    Sanders, D.E.; Petersen, N.

    1984-04-01

    The Val Verde basin is a northwest-southeast trending foreland basin contained within the southern portion of the Permian basin. The Val Verde basin has several large fields, e.g., Brown Bassett and JM, which have a combined ultimate recovery of over 1 tcf of gas. Structurally, the major fields are complexly faulted features related to differential uplift of basement blocks. Middle and Upper Permian strata are not present in the central and southern Val Verde basin. Appreciable amounts of Permian sediment were eroded prior to deposition of Cretaceous strata, thus, Cretaceous rocks unconformably overlie Wolfcamp sediments. Restored estimates for vitrinite reflectance data indicate a minimum of 8000-10,000 ft (2400-3000 m) of Permian rocks have been eroded. Therefore, in the central and southern portions of the basin, Paleozoic rocks are inferred to have occupied depths several miles deeper than present. Vitrinite reflectance values for Ellenburger (Ordovician) rocks at Brown Bassett are approximately 1.8 to 2.0% R/sub o/. Ellenburger reflectance values increase to the south and southeast to values greater than 4.5% R/sub o/. The most southerly wells also have reflectance depth trends which show a break in gradient within Wolfcamp sediments (9000-10,000 ft, 2700-3000 m). The change in gradient suggests a thermal event contemporaneous with the basin's rapid downwarping and Wolfcamp deposition. Any exploration in the basin, therefore, must recognize the unique relationships between structural timing, structural position, depth of burial, thermal pulses, and hydrocarbon mobility for a large portion of Val Verde basin.

  13. Ground-water hydraulics of the deep-basin brine aquifer, Palo Duro Basin, Texas panhandle

    SciTech Connect (OSTI)

    Smith, D.A.

    1985-01-01

    The Deep-Basin Brine aquifer of the Palo Duro Basin (Texas Panhandle) underlies thick Permian bedded evaporites that are being evaluated as a potential high-level nuclear waste isolation repository. Potentiometric surface maps of 5 units of the Deep-Basin Brine aquifer were drawn using drill-stem test (DST) pressure data, which were analyzed by a geostatistical technique (kriging) to smooth the large variation in the data. The potentiometric surface maps indicate that the Deep-Basin Brine aquifer could be conceptually modeled as 5 aquifer units; a Lower Permian (Wolfcamp) aquifer, upper and lower Pennsylvanian aquifers, a pre-Pennsylvanian aquifer, and a Pennsylvanian to Wolfcampian granite-wash aquifer. The hydraulic head maps indicate that ground-water flow in each of the units is west to east with a minor northerly component near the Amarillo Uplift, the northern structural boundary of the basin. The Wolfcamp potentiometric surface indicates the strongest component of northerly flow. Inferred flow direction in Pennsylvanian aquifers is easterly, and in the pre-Pennsylvanian aquifer near its pinch-out in the basin center, flow is inferred to be to the north. In the granite-wash aquifer the inferred flow direction is east across the northern edge of the basin and southeast along the Amarillo Uplift.

  14. Texas' lightly drilled Dalhart basin getting more oil exploration

    SciTech Connect (OSTI)

    Petzet, G.A.

    1991-06-24

    The Dalhart basin of the northwestern Texas Panhandle, the state's least drilled prospective area, is showing signs of another round of exploratory drilling. Horizon Oil and Gas Co., Dallas, opened ERT (Granite Wash) field in Potter County at 102 Bivins Ranch 9 miles north of Amarillo in early June. The discovery well pumped 105 b/d of 37.7{degrees} gravity oil and 48 b/d of water with gas too small to measure from perforations at 5,820-5,913 ft. Total depth is 7,516 ft in granite. In Hartley County, McKinney Operating Co., Amarillo, is pumped testing a second well in a field it discovered in 1990 that opened the first commercial Permian oil production in the Dalhart basin. The discovery well, McKinney's 1 Proctor, in section 63, block 22, CSL Survey, 19 miles west of Channing, pumped 12 b/d of oil and 15 b/d of water from Wolfcamp perforations at 4,038-50 ft. The well, which opened Proctor Ranch field, is producing about 35 b/d of oil.

  15. Crosswell seismic imaging in the Permian Basin, West Texas, USA

    SciTech Connect (OSTI)

    Langan, R.T.; Harris, J.M.; Jensen, T.L.

    1995-12-31

    Crosswell seismic imaging technology has advanced rapidly over the last three years as the processing methods have become more robust, the cost of data acquisition has fallen, and the interwell distances of operation have increased. The Permian Basin of west Texas, USA is proving to be an ideal environment in which to develop this technology because of the relatively low seismic attenuation of the carbonate-dominated lithology, the moderate well spacings in the large number of mature fields, and the unusually high number of reflecting horizons. Current technology permits us to operate in carbonates at well spacings on the order of 2000 ft (650 m) and to image P- and S-wave reflecting horizons on a scale of 8 to 25 ft (2.4 to 7.6 m). Crosswell technology is not limited to carbonates, although the majority of recent applications have been in this environment. We are involved in three separate crosswell experiments in the Permian Basin, each with unique objectives. The first experiment involves a CO{sub 2} pilot project in a Grayburg Formation reservoir on the eastern edge of the Central Basin Platform. Here we are attempting to characterize the reservoir at a scale unobtainable from 3-D surface seismic data and to image CO{sub 2} fronts directly. The second experiment deals with a waterflood in a Middle Clearfork Formation reservoir on the Eastern Shelf, where we are trying to explain the erratic response of adjacent wells to water injection. In the third project we are trying to image the structure and stratigraphy of subtle {open_quotes}anomalies{close_quotes} in 3-D surface seismic images of the Wolfcamp Formation.

  16. Lower Permian facies of the Palo Duro Basin, Texas: depositional systems, shelf-margin evolution, paleogeography, and petroleum potential

    SciTech Connect (OSTI)

    Handford, C.R.

    1980-01-01

    A Palo geological study suggests that potential hydrocarbon reservoirs occur in shelf-margin carbonates, delta-front sandstones, and fan-delta arkoses. Zones of porous (greater than 10 percent) dolomite are concentrated near shelf margins and have configurations similar to productive Lower Permian shelf-margin trends in New Mexico. Delta-front sandstones (log-computed porosity of 18 to 25 percent) are similar to producing deltaic sandstones of Morris Buie-Blaco Fields in North-Central Texas. Porous (18 percent) fan-delta sandstones along the south flank of the Amarillo Uplift may form reservoirs similiar to that of the Mobeetie Field on the north side of the Amarillo Uplife in Wheeler County, Texas. Potential hydrocarbon source beds occur in slope and basinal environments. Total organic carbon generally ranges from 1 to 2.3 percent by weight and averages 0.589 percent by weight.

  17. Playa basin development, southern High Plains, Texas and New Mexico

    SciTech Connect (OSTI)

    Gustavson, T.C. (Univ. of Texas, Austin, TX (United States)); Holliday, V.T. (Univ. of Wisconsin, Madison, WI (United States))

    1992-01-01

    More than 20,000 playa basins have formed on fine-grained eolian sediments of the Quaternary Blackwater Draw and Tertiary Ogallala Formations on the High Plains of TX and NM. Numerous hypotheses have been proposed for the development of playa basins: (1) subsidence due to dissolution of underlying Permian bedded salt, (2) dissolution of soil carbonate and piping of clastic sediment into the subsurface, (3) animal activity, and (4) deflation. Evidence of eolian processes includes lee dunes and straightened shorelines on the eastern and southern margins of many playas. Lee dunes, which occur on the eastern side of ca 15% of playa basins and contain sediment deflated from adjacent playas, are cresentic to oval in plain view and typically account for 15--40% of the volume of the playa basin. Quaternary fossil biotas and buried calcic soils indicate that grasslands and semi-arid to aid climatic conditions prevailed as these basins formed. Evidence of fluviolacustrine processes in playa basins includes centripetal drainage leading to fan deltas at playa margins and preserved deltaic and lacustrine sediments. Playa basins expanded as fluvial processes eroded basin slopes and carried sediment to the basin floor where, during periods of minimal vegetation cover, loose sediment was removed by deflation. Other processes that played secondary roles in the development of certain playa basins include subsidence induced by dissolution of deeply buried Permian salt, dissolution of soil carbonate and piping, and animal activity. Two small lake basins in Gray County, TX, occur above strata affected by dissolution-induced subsidence. Dissolution of soil carbonate was observed in exposures and cores of strata underlying playa basins. Cattle, and in the past vast numbers of migrating buffalo, destroy soil crusts in dry playas, making these sediments more susceptible to deflation, and carry sediment out of flooded playas on their hooves.

  18. Cameron County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Island, Texas South Point, Texas Tierra Bonita, Texas Villa Pancho, Texas Villa del Sol, Texas Yznaga, Texas Retrieved from "http:en.openei.orgwindex.php?titleCameronCou...

  19. Geology and geohydrology of the east Texas Basin. Report on the progress of nuclear waste isolation feasibility studies (1979)

    SciTech Connect (OSTI)

    Kreitler, C.W.; Agagu, O.K.; Basciano, J.M.

    1980-01-01

    The program to investigate the suitability of salt domes in the east Texas Basin for long-term nuclear waste repositories addresses the stability of specific domes for potential repositories and evaluates generically the geologic and hydrogeologic stability of all the domes in the region. Analysis during the second year was highlighted by a historical characterization of East Texas Basin infilling, the development of a model to explain the growth history of the domes, the continued studies of the Quaternary in East Texas, and a better understanding of the near-dome and regional hydrology of the basin. Each advancement represents a part of the larger integrated program addressing the critical problems of geologic and hydrologic stabilities of salt domes in the East Texas Basin.

  20. Feasibility study of heavy oil recovery in the Permian Basin (Texas and New Mexico)

    SciTech Connect (OSTI)

    Olsen, D.K.; Johnson, W.I.

    1993-05-01

    This report is one of a series of publications assessing the feasibility of increasing domestic heavy oil production. Each report covers select areas of the United States. The Permian Basin of West Texas and Southeastern New Mexico is made up of the Midland, Delaware, Val Verde, and Kerr Basins; the Northwestern, Eastern, and Southern shelves; the Central Basin Platform, and the Sheffield Channel. The present day Permian Basin was one sedimentary basin until uplift and subsidence occurred during Pennsylvanian and early Permian Age to create the configuration of the basins, shelves, and platform of today. The basin has been a major light oil producing area served by an extensive pipeline network connected to refineries designed to process light sweet and limited sour crude oil. Limited resources of heavy oil (10`` to 20`` API gravity) occurs in both carbonate and sandstone reservoirs of Permian and Cretaceous Age. The largest cumulative heavy oil production comes from fluvial sandstones of the Cretaceous Trinity Group. Permian heavy oil is principally paraffinic and thus commands a higher price than asphaltic California heavy oil. Heavy oil in deeper reservoirs has solution gas and low viscosity and thus can be produced by primary and by waterflooding. Because of the nature of the resource, the Permian Basin should not be considered a major heavy oil producing area.

  1. Feasibility study of heavy oil recovery in the Permian Basin (Texas and New Mexico)

    SciTech Connect (OSTI)

    Olsen, D.K.; Johnson, W.I.

    1993-05-01

    This report is one of a series of publications assessing the feasibility of increasing domestic heavy oil production. Each report covers select areas of the United States. The Permian Basin of West Texas and Southeastern New Mexico is made up of the Midland, Delaware, Val Verde, and Kerr Basins; the Northwestern, Eastern, and Southern shelves; the Central Basin Platform, and the Sheffield Channel. The present day Permian Basin was one sedimentary basin until uplift and subsidence occurred during Pennsylvanian and early Permian Age to create the configuration of the basins, shelves, and platform of today. The basin has been a major light oil producing area served by an extensive pipeline network connected to refineries designed to process light sweet and limited sour crude oil. Limited resources of heavy oil (10'' to 20'' API gravity) occurs in both carbonate and sandstone reservoirs of Permian and Cretaceous Age. The largest cumulative heavy oil production comes from fluvial sandstones of the Cretaceous Trinity Group. Permian heavy oil is principally paraffinic and thus commands a higher price than asphaltic California heavy oil. Heavy oil in deeper reservoirs has solution gas and low viscosity and thus can be produced by primary and by waterflooding. Because of the nature of the resource, the Permian Basin should not be considered a major heavy oil producing area.

  2. Wolfcampian sequence stratigraphy of eastern Central Basin platform, Texas

    SciTech Connect (OSTI)

    Candelaria, M.P.; Entzminger, D.J.; Behnken, F.H. ); Sarg, J.F. ); Wilde, G.L. )

    1992-04-01

    Integrated study of well logs, cores, high-resolution seismic data, and biostratigraphy has established the sequence framework of the Atokan (Early Pennsylvanian)-Wolfcampian (Early Permian) stratigraphic section along the eastern margin of the Central Basin platform in the Permian basin. Sequence interpretation of high-resolution, high-fold seismic data through this stratigraphic interval has revealed a complex progradational/retrogradational evolution of the platform margin that has demonstrated overall progradation of at least 12 km during early-middle Wolfcampian. Sequence stratigraphic study of the Wolfcamp interval has revealed details of the internal architecture and morphologic evolution of the contemporaneous platform margin. Two generalized seismic facies assemblages are recognized in the Wolfcampian. Platform interior facies are characterized by high-amplitude, laterally continuous parallel reflections; platform margin facies consist of progradational sigmoidal to oblique clinoforms and are characterized by discontinuous, low-amplitude reflections. Sequence interpretation of carbonate platform-to-basin strata geometries helps in predicting subtle stratigraphic trapping relationships and potential reservoir facies distribution. Moreover, this interpretive method assists in describing complex reservoir heterogeneities that can contribute to significant reserve additions from within existing fields.

  3. Controls on reservoir development in Devonian Chert: Permian Basin, Texas

    SciTech Connect (OSTI)

    Ruppel, S.C.; Hovorka, S.D.

    1995-12-01

    Chert reservoirs of the Lower Devonian Thirtyone Formation contain a significant portion of the hydrocarbon resource in the Permian basin. More than 700 million bbl of oil have been produced from these rocks, and an equivalent amount of mobile oil remains. Effective exploitation of this sizable remaining resource, however, demands a comprehensive appreciation of the complex factors that have contributed to reservoir development. Analysis of Thirtyone Formation chert deposits in Three Bar field and elsewhere in the Permian basin indicates that reservoirs display substantial heterogeneity resulting from depositional, diagenetic, and structural processes. Large-scale reservoir geometries and finer scale, intra-reservoir heterogeneity are primarily attributable to original depositional processes. Despite facies variations, porosity development in these cherts is principally a result of variations in rates and products of early silica diagenesis. Because this diagenesis was in part a function of depositional facies architecture, porosity development follows original depositional patterns. In reservoirs such as Three Bar field, where the Thirtyone Formation has been unroofed by Pennsylvanian deformation, meteoric diagenesis has created additional heterogeneity by causing dissolution of chert and carbonate, especially in areas of higher density fracturing and faulting and along truncated reservoir margins. Structural deformation also has exerted direct controls on heterogeneity that are particularly noteworthy in reservoirs under waterflood. High-density fracture zones create preferred flow paths that result in nonuniform sweep through the reservoir. Faulting locally creates compartments by offsetting reservoir flow units. As such, the processes and models defined here improve understanding of the causes of heterogeneity in all Thirtyone chert reservoirs in the Permian basin and aid recovery of the sizable hydrocarbon resource remaining in these rocks.

  4. Elemental mobility in sandstones during burial: Whole-rock chemical and isotopic data, Frio Formation, south Texas

    SciTech Connect (OSTI)

    Milliken, K.L.; Mack, L.E.; Land, L.S. . Dept. of Geological Sciences)

    1994-10-03

    The deepest (> 3.5 km) and most altered Oligocene Frio sandstones from south Texas typically contain authigenic minerals that exceed 30 volume percent of the rock. Elemental and isotopic analyses of whole rocks confirm conclusions based on petrography that authigenesis is accompanied by substantial material transfer involving both import to and export from the sandstone. Material transfer on the scale observed demonstrates that burial diagenesis is an open-system process for several major elements, and introduces a major obstacle to use of elemental data for provenance interpretation. Defining the sources of materials transported into sandstones, and the fate of materials exported, is key to documenting the scale of system closure in sedimentary basins and requires a better understanding of diagenetic processes in mudrocks.

  5. Phanerozoic tectono-stratigraphic evolution of the Trans-Pecos and Permian basin regions (Mexico, Texas, New Mexico) using Landsat imagery, subsurface and outcrop data

    SciTech Connect (OSTI)

    Markello, J.R.; Sarg, J.F.

    1996-08-01

    Integrating regional Landsat imagery, outcrop field studies, and subsurface data has resulted in a more comprehensive understanding and delineation of the tectono-stratigraphic evolution of the Trans-Pecos region. Landsat imagery were acquired and registered to the existing 1:25000 scale maps and mosaiced to create a regional view of the Trans-Pecos and Permian basin region. The imagery were used to extrapolate and map key stratigraphic and tectonic elements after calibration from documented outcrop and subsurface data. The interpretations aided in the extrapolation of scattered control information and were critical in the complete reconstruction of the geologic history of the area. The Trans-Pecos Phanerozoic history comprises five tectono-depositional phases, and these have controlled the shape of the modem landscape: (1) Late Proterozoic rifting (Gondwana from Laurentia), and development of the Early-Middle Paleozoic Tobosa basin; (2) Pennsylvanian collision (South and North Americas), and differentiation of the Tobosa basin into the Midland, Delaware, Orogrande, and Pedregosa basins separated by basement blocks: Central Basin Platform, Diablo Platform, Burro-Florida Platform; (3) Middle Mesozoic transtensional rifting (Mexico from North America), and Late Jurassic failed rifting of the Mexican Chihuahua and Coahuila Troughs west and south of the Diablo Platform; (4) Late Mesozoic Laramide collision (Mexico and Texas), and development of the Chihuahua fold/thrust belt limited by the western margin of the Diablo Platform; (5) Late Cenozoic North American basin and Range rifting, and development of Rio Grande grabens, block-faulted mountains, and volcanics. The Tobosa basin was a passive-margin interior sag; its continental margin was south of the Marathons.

  6. Jim Hogg County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Climate Zone Number 2 Climate Zone Subtype A. Places in Jim Hogg County, Texas Guerra, Texas Hebbronville, Texas Las Lomitas, Texas South Fork Estates, Texas Retrieved from...

  7. Measured Performance of Occupied, Side-by-Side, South Texas Homes

    SciTech Connect (OSTI)

    Chasar, Dave; vonSchramm, Valerie

    2012-09-01

    The performance of three homes in San Antonio, Texas with identical floor plans and orientation were evaluated through a partnership between the Florida Solar Energy Center (FSEC), CPS Energy, and Woodside Homes of South Texas. Measurements included whole house gas and electric use as well as heating, cooling, hot water, major appliances and indoor and outdoor conditions. One home built to builder standard practice served as the control, while the other homes demonstrated high performance features. Utility peak electric load comparisons of these dual-fuel homes provide an assessment of envelope and equipment improvements.

  8. ASSESSING AND FORECASTING, BY PLAY, NATURAL GAS ULTIMATE RECOVERY GROWTH AND QUANTIFYING THE ROLE OF TECHNOLOGY ADVANCEMENTS IN THE TEXAS GULF COAST BASIN AND EAST TEXAS

    SciTech Connect (OSTI)

    William L. Fisher; Eugene M. Kim

    2000-12-01

    A detailed natural gas ultimate recovery growth (URG) analysis of the Texas Gulf Coast Basin and East Texas has been undertaken. The key to such analysis was determined to be the disaggregation of the resource base to the play level. A play is defined as a conceptual geologic unit having one or more reservoirs that can be genetically related on the basis of depositional origin of the reservoir, structural or trap style, source rocks and hydrocarbon generation, migration mechanism, seals for entrapment, and type of hydrocarbon produced. Plays are the geologically homogeneous subdivision of the universe of petroleum pools within a basin. Therefore, individual plays have unique geological features that can be used as a conceptual model that incorporates geologic processes and depositional environments to explain the distribution of petroleum. Play disaggregation revealed important URG trends for the major natural gas fields in the Texas Gulf Coast Basin and East Texas. Although significant growth and future potential were observed for the major fields, important URG trends were masked by total, aggregated analysis based on a broad geological province. When disaggregated by plays, significant growth and future potential were displayed for plays that were associated with relatively recently discovered fields, deeper reservoir depths, high structural complexities due to fault compartmentalization, reservoirs designated as tight gas/low-permeability, and high initial reservoir pressures. Continued technology applications and advancements are crucial in achieving URG potential in these plays.

  9. Geostatistical analysis of potentiometric data in Wolfcamp aquifer of the Palo Duro Basin, Texas

    SciTech Connect (OSTI)

    Harper, W.V.; Furr, J.M.

    1986-04-01

    This report details a geostatistical analysis of potentiometric data from the Wolfcamp aquifer in the Palo Duro Basin, Texas. Such an analysis is a part of an overall uncertainty analysis for a high-level waste repository in salt. Both an expected potentiometric surface and the associated standard error surface are produced. The Wolfcamp data are found to be well explained by a linear trend with a superimposed spherical semivariogram. A cross-validation of the analysis confirms this. In addition, the cross-validation provides a point-by-point check to test for possible anomalous data.

  10. Tectonic mechanisms for formation of the Central Basin platform and adjacent basinal areas, Permian basin, Texas and New Mexico

    SciTech Connect (OSTI)

    Yang, Kennming; Dorobek, S.L. )

    1992-04-01

    Formation of the Central Basin platform (CBP), with the Delaware basin to its west and the Midland basin to its east, has been attributed to the crustal deformation in the foreland area of the Marathon Orogen during the late Paleozoic. Because of complexities in the areal distribution and magnitudes of uplift along the length of the CBP, its formative mechanisms are still controversial. Previous interpretations about the mechanisms for uplift of the CBP are based on the characteristics of the boundary faults between the CBP and adjacent basinal areas. Here, an integrated tectonic model is proposed for formation of the uplift and adjacent basins based on studies of the structure of sedimentary layers overlying Precambrian basement rocks of the uplift and restoration of the lower Paleozoic strata in the Delaware basin.

  11. Comparison of selected oil-field brines from fields in the Permian basin, West Texas-southeast New Mexico

    SciTech Connect (OSTI)

    White, H.G. III

    1992-04-01

    Stiff diagrams of oil-field brines from the west Texas Permian basin are identifiable within the geological framework. Plotted from a simple analysis of three cations and three anions, older Paleozoic waters can be categorized as either 'pristine' or modified, usually by a later influx of Permian or early Pennsylvanian water. These different plots can be segregated by geologic province. The Permian brines differ by age and also by environment (shelf, basin, etc.).

  12. South Atlantic sag basins: new petroleum system components

    SciTech Connect (OSTI)

    Henry, S.G. Mohriak, W.U.; Mello, M.R.

    1996-08-01

    Newly discovered pre-salt source rocks, reservoirs and seals need to be included as components to the petroleum systems of both sides of the South Atlantic. These new components lie between the pre-salt rift strata and the Aptian salt layers, forming large, post-rift, thermal subsidence sag basins. These are differentiated from the older rift basins by the lack of syn-rift faulting and a reflector geometry that is parallel to the base salt regional unconformity rather than to the Precambrian basement. These basins are observed in deep water regions overlying areas where both the mantle and the crust have been involved in the extension. This mantle involvement creates post-rift subsiding depocenters in which deposition is continuous while proximal rift-phase troughs with little or no mantle involvement are bypassed and failed to accumulate potential source rocks during anoxic times. These features have been recognized in both West African Kwanza Basin and in the East Brasil Rift systems. The pre-salt source rocks that are in the West African sag basins were deposited in lacustrine brackish to saline water environment and are geochemically distinct from the older, syn-rift fresh to brackish water lakes, as well as from younger, post-salt marine anoxic environments of the drift phase. Geochemical analyses of the source rocks and their oils have shown a developing source rock system evolving from isolated deep rift lakes to shallow saline lakes, and culminating with the infill of the sag basin by large saline lakes to a marginally marine restricted gulf. Sag basin source rocks may be important in the South Atlantic petroleum system by charging deep-water prospects where syn-rift source rocks are overmature and the post-salt sequences are immature.

  13. Evaporite replacement within the Permian strata of the Bighorn Basin, Wyoming and the Delaware Basin, west Texas and New Mexico

    SciTech Connect (OSTI)

    Ulmer, D.S.; Scholle, P.A. )

    1992-01-01

    The Park City and Goose Egg Formations of the Big Horn Basin, Wyoming and the Seven Rivers, Yates and Tansill Formations of west Texas and New Mexico contain numerous examples of silicified and calcitized evaporites. Both areas show significant preserved interstitial evaporite, but on outcrop the discrete crystals and nodular evaporites have been extensively replaced. These replacements appear to be a multistage phenomenon. Field and petrographic evidence (matted fabrics in nodules; evaporite inclusions) indicate that silicification involved direct replacement of evaporites and probably occurred during earlier stages of burial. Calcitization, however, appears to be a much later phenomenon and involved precipitation of coarse crystals within evaporite molds. The calcites are typically free of evaporite inclusions. Isotopic analyses of these calcites give a wide range of values from [minus]6.04 to [minus]25.02 [per thousand] [delta][sup 18]O and +6.40 to [minus]25.26 [per thousand] [delta][sup 13]C, reflecting their complex diagenetic histories. In both localities, silicification of evaporites was completed by the end of hydrocarbon migration and emplacement. The extremely broad isotopic range of the calcites indicates that the calcitization occurred during a long period of progressive uplift and increased groundwater circulation associated with mid-Tertiary block faulting. The very light oxygen values within the Bighorn Basin were produced by thermochemical sulfate reduction during deepest burial of the region. Evaporite diagenesis in both the Bighorn and Delaware Basins is an ongoing process that started prior to hydrocarbon migration, continued over millions of years, and has the potential to do significant porosity change.

  14. Boraflex panel degradation in spent-fuel storage racks at the South Texas Project

    SciTech Connect (OSTI)

    Hoppes, D.F.

    1996-12-31

    Blackness (neutron absorption) testing was conducted in August 1994 on selected South Texas Project (STP) electric generating station spent-fuel pool (SFP) storage racks as required by the surveillance monitoring program. The tests were performed to determine if gaps had developed in the Boraflex neutron poison material and to determine size and location of any gaps identified. The testing was performed by HOLTEC International using a specially designed logging tool containing a {sup 252}Cf neutron source and four boron trifluoride (BF{sub 3}) thermal neutron detectors.

  15. Rare earth elements in chloride-rich groundwater, Palo Duro Basin, Texas, USA

    SciTech Connect (OSTI)

    Gosselin, D.C. ); Smith, M.R.; Lepel, E.A. ); Laul, J.C. )

    1992-04-01

    Rare earth element (REE) data for groundwater samples from the Deep-Basin Brine aquifer of the Palo Duro Basin, Texas, USA, illustrates the potential use of REE for inferring groundwater flow paths through different geologic materials. The REE content of the groundwaters range over 2.5 orders of magnitude and are depleted by 10{sup 2} to 10{sup 5} relative to aquifer materials. The shale-normalized REE patterns for groundwater that have primarily interacted with arkosic sandstones (granite wash) are flat with similar heavy REE (HREE) enrichments ((Lu/La){sub n} = 0.60 to 0.80). The samples with highest REE contents and REE patterns, which are enriched in the intermediate REEs (IREEs; Sm-Tb) reflect variable degrees of interaction with carbonate rocks. The IREE enrichment is the result of fluid interaction with Fe-Mn coatings on carbonate minerals and/or secondary minerals in fractures and vugs. The chloride complex. (LnCl{sup 2+}), and free-ions are the predominant REE species, accounting for over 95% of the REEs. Carbonate and sulfate species account for the other 5% and have very little influence on the behavior of the REEs. Although this study indicates a potentially important role for the REEs in understanding geochemical transport and groundwater movement, it also indicates the necessity for developing a better understanding of REE speciation in high ionic strength solutions.

  16. Application of Advanced Reservoir Characterization, Simulation, and Production Optimization Strategies to Maximize Recovery in Slope and Basin Clastic Reservoirs, West Texas (Delaware Basin), Class III

    SciTech Connect (OSTI)

    Dutton, Shirley P.; Flanders, William A.

    2001-11-04

    The objective of this Class III project was demonstrate that reservoir characterization and enhanced oil recovery (EOR) by CO2 flood can increase production from slope and basin clastic reservoirs in sandstones of the Delaware Mountain Group in the Delaware Basin of West Texas and New Mexico. Phase 1 of the project, reservoir characterization, focused on Geraldine Ford and East Ford fields, which are Delaware Mountain Group fields that produce from the upper Bell Canyon Formation (Ramsey sandstone). The demonstration phase of the project was a CO2 flood conducted in East Ford field, which is operated by Orla Petco, Inc., as the East Ford unit.

  17. Auxiliary feedwater system risk-based inspection guide for the South Texas Project nuclear power plant

    SciTech Connect (OSTI)

    Bumgardner, J.D.; Nickolaus, J.R.; Moffitt, N.E.; Gore, B.F.; Vo, T.V.

    1993-12-01

    In a study sponsored by the US Nuclear Regulatory Commission (NRC), Pacific Northwest Laboratory has developed and applied a methodology for deriving plant-specific risk-based inspection guidance for the auxiliary feedwater (AFW) system at pressurized water reactors that have not undergone probabilistic risk assessment (PRA). This methodology uses existing PRA results and plant operating experience information. Existing PRA-based inspection guidance information recently developed for the NRC for various plants was used to identify generic component failure modes. This information was then combined with plant-specific and industry-wide component information and failure data to identify failure modes and failure mechanisms for the AFW system at the selected plants. South Texas Project was selected as a plant for study. The product of this effort is a prioritized listing of AFW failures which have occurred at the plant and at other PWRs. This listing is intended for use by the NRC inspectors in preparation of inspection plans addressing AFW risk important components at the South Texas Project plant.

  18. Geochemistry of post-uplift calcite in the Permian Basin of Texas and New Mexico

    SciTech Connect (OSTI)

    Wiggins, W.D.; Harris, P.M. ); Burruss, R.C. )

    1993-06-01

    Integration whole-oil gas chromatography of produced oil and oil inclusions, formation-water chemistry, and stable isotopes has identified environment-diagnostic differences in calcite cements between oil field and outcrop environments in the Permian Basin of Texas and New Mexico. Calcite-[delta][sup 13]C and fluid-inclusion composition are the most diagnostic of pore-fluid evolution and can help interpret rock-fluid reactions. Late-stage calcite cement in the northwestern part of the basin formed in a meteoric aquifer that was emplaced by Neogene-age uplift and tilting of the Guadalupe Mountains. Where the confined aquifer intersects the Henderson oil field, the water, which is less saline than sea water, has 900-1,400 ppm bicarbonate alkalinity because of oil oxidation and contains 750 ppm H[sub 2]S as a result of anhydrite calcitization and sulfate reduction. The oil field has been severly damaged by biodegradation. Modeling of [delta][sup 13]C in pore-filling calcite from the field (mean [delta][sup 13]C = [minus]17% PDB) suggests oxidation of oil provided nearly 100% of the carbon in the cement. Comparison of gas chromatograms of produced oil and oil liberated from fluid inclusions in calcite shows that inclusion oil is older and more severely biodegraded (paraffin-free) than produced oil. This implies that oil in the reservoir was remobilized soon after Neogene-age meteoric invasion and carbonate cementation. The Algerita Escarpment in the Guadalupe Mountains is the site of active meteoric water recharge and growth of phreatic calcite cement. The phreatic cement contains single-phase, aqueous fluid inclusions. The cement is depleted in [sup 13]C to an extent that is diagnostic of a 1:1 mixture of soil-CO[sub 2] from decay of C[sub 4]-type plants (desert grasses) and carbon derived from dolomite matrix by ground-water dissolution. 64 refs., 12 figs., 3 tabs.

  19. Facies architecture of Spraberry submarine fan reservoirs (Permian), Midland basin, Texas

    SciTech Connect (OSTI)

    Guevara, E.H.; Tyler, N.

    1989-03-01

    Facies of mud-rich submarine fans of the Spraberry formation (Permian, Leonardian) form oil reservoirs in the central part of the Midland basin, west Texas. The principal reservoirs are submarine-channel and associated facies in the upper parts of generally upward-coarsening and upward-thickening sequences of the Jo Mill (lower Spraberry) and Driver and overlying Floyd (upper Spraberry) fans. They are naturally fractured, massive and laminated, very fine-grained, calcareous sandstones and siltstones usually occurring in beds 2 to approximately 12 ft thick. Two main subdivisions, inner and middle to outer fan, are recognized using isoliths, log motifs, and cores of predominantly terrigenous clastic, mostly basin-wide genetic intervals. The boundary between the subdivisions approximately coincides with the location of the subjacent Horseshoe atoll (Pennsylvanian). The narrow range in grain size of the fans results in limited basinward variations in texture and sedimentary structures and paucity of Bouma sequences. Facies architecture strongly influences hydrocarbon distribution and recovery. Wells having the best cumulative productions generally occur in sandstone depositional axes. Most accumulations in inner fan facies are scattered structural traps having relatively high recovery efficiencies (24%, Jo Mill field). The largest accumulations in mid to outer fan facies are stratigraphic traps in meandering to anastomosing channel sandstone belts 1-3 mi wide occurring in a widespread area. Recovery efficiencies range from 5% (Spraberry trend, stratigraphic trap) to 15% (Benedum field, combined stratigraphic-structural trap). Additional reserves can be recovered from partly drained and untapped reservoir compartments, especially in layered and compartmentalized middle to outer fan facies.

  20. Precambrian basement geology of the Permian basin region of west Texas and Eastern New Mexico: A geophysical perspective

    SciTech Connect (OSTI)

    Adams, D.C.; Keller, G.R.

    1996-03-01

    Because most of the Permian basin region of west Texas and southern New Mexico is covered by Phanerozoic rocks, other means must be found to examine the Precambrian upper crustal geology of the region. We have combined geologic information on the Precambrian from outcrops and wells with geophysical information from gravity and magnetic surveys in an integrated analysis of the history and structure of basement rocks in the region. Geophysical anomalies can be related to six Precambrian events: formation of the Early Proterozoic outer tectonic belt, igneous activity in the southern Granite-Rhyolite province, an episode of pre-Grenville extension, the Grenville orogeny, rifting to form the Delaware aulacogen, and Eocambrian rifting to form the early Paleozoic continental margin. Two geophysical features were studied in detail: the Abilene gravity minimum and the Central Basin platform gravity high. The Abilene gravity minimum is shown to extend from the Delaware basin across north-central Texas and is interpreted to be caused by a granitic batholith similar in size to the Sierra Nevada batholith in California and Nevada. This batholith appears to be related to formation of the southern Granite- Rhyolite province, possibly as a continental margin arc batholith. Because of this interpretation, we have located the Grenville tectonic front southward from its commonly quoted position, closer to the Llano uplift. Middle Proterozoic mafic intrusions are found to core the Central Basin platform and the Roosevelt uplift. These intrusions formed at about 1.1 Ga and are related in time to both the Mid-Continent rift system and the Grenville orogeny in Texas. Precambrian basement structures and changes in lithology have influenced the structure and stratigraphy in the overlying Permian basin, and thus have potential exploration significance.

  1. Cycle stratigraphy and porosity in Pennsylvanian and Lower Permian shelf limestones, eastern Central Basin Platform, Texas

    SciTech Connect (OSTI)

    Saller, A.H.; Dickson, J.A.D.; Boyd, S.A.

    1994-12-01

    Pennyslvanian and Lower Permian shelfal limestones were studied in core and wireline logs on the eastern side of the Central Basin platform in west Texas. Sixty-three (63) cycles were delineated in the study interval, which includes 200-250 m of Canyon (Missourian), Cisco (Virgilian), and Wolfcamp strata. Four general lithofacies are present: fossiliferous wackestones and packstones, grainstones, phylloid algal boundstones, and shales. These lithologies typically occur in 1-18-m-thick cycles bounded by subaerial exposure surfaces. Grainstones in the upper part of some cycles indicate a shallowing of environments prior to subaerial exposure. Many cycles have subaerial exposure surfaces developed on subtidal fossiliferous wackestones or packstones suggesting rapid falls in sea level. Long-term transgressive intervals (transgressive systems tracts or TST) are dominated by thick (>4 m) cycles, whereas long-term regressive intervals (highstand systems tract or HST) are dominated by thinner cycles. Stable carbon isotope data suggest that thick cycles in TSTs were subjected to short periods of subaerial exposure, whereas thin cycles in the HSTs were subjected to much longer subaerial exposure. Where present, reservoir-grade porosity occurs in the upper part of cycles, 0.3-5 m below subaerial exposure surfaces. Prolonged subaerial exposure apparently reduced matrix porosity by allowing more time for calcite precipitation, which was especially effective in reducing porosity in micritic strata below exposure surfaces.

  2. Cathodoluminescent textures and the origin of quartz silt in Oligocene mudrocks, south Texas

    SciTech Connect (OSTI)

    Milliken, K.L. . Dept. of Geological Sciences)

    1994-07-01

    In subsurface mudrocks of the Oligocene Frio Formation in South Texas, a substantial proportion of silt-size quartz (10--62 [mu]m) manifests cathodoluminescence (CL) that varies greatly in intensity within each particle, giving rise to textures that differ greatly from grain to grain. In contrast, most quartz grains of sand size ([ge] 62 [mu]m) have CL that is relatively homogeneous within individual grains. A substantial percentage of the quartz within silt grains is very weakly luminescent. No depth trend in the occurrence of luminescent textures in detrital quartz is observed, suggesting that the component of dark, possibly low-temperature silt-size quartz is not related to chemical processes in the present burial setting. Paleogene rhyolites of West Texas are a partial model for the source rocks that supplied sediment to the Frio Formation. Phenocrystic quartz in these volcanics has uniform CL similar to that observed in the Frio sand fraction, whereas complex CL structure seen in the associated groundmass bears many similarities to the CL textures observed in Frio silts. This observation further supports the idea that CL structure of detrital quartz in the Frio is most likely an inherited feature. If the quartz with dark CL is of low-temperature origin, it would help to elucidate the relatively [sup 18]O-enriched isotopic values reported for mudrock quartz in the Frio.

  3. Measured Performance of Occupied, Side-by-Side, South Texas Homes

    SciTech Connect (OSTI)

    Chasar, D.; vonSchramm, V.

    2012-09-01

    The performance of three homes in San Antonio, Texas with identical floor plans and orientation were evaluated through a partnership between the Florida Solar Energy Center (FSEC), CPS Energy, and Woodside Homes of South Texas. Measurements included whole house gas and electric use as well as heating, cooling, hot water, major appliances and indoor and outdoor conditions. One home built to builder standard practice served as the control, while the other homes demonstrated high performance features. Utility peak electric load comparisons of these dual-fuel homes provide an assessment of envelope and equipment improvements. The control home used natural gas for space and water heating only, while the improved homes had gas heating and major appliances with the exception of a high efficiency heat pump in one home. Data collection began in July of 2009 and continued through April of 2011. Energy ratings for the homes yielded E-Scales (aka HERS indices) of 86 for the control home, 54 for one improved home and 37 for the other home which has a 2.4kW photovoltaic array.

  4. Hydrogeologic investigations based on drill-stem test data: Palo Duro Basin Area, Texas and New Mexico

    SciTech Connect (OSTI)

    Bair, E.S.; O'Donnell, T.P.; Picking, L.W.

    1985-02-01

    Drill-stem test (DST) data were compiled from wildcat wells and DOE-sponsored wells in the Palo Duro Basin area of Texas and New Mexico. The data were used to construct pressure-depth diagrams and to map regional potentiometric surfaces, based on equivalent freshwater heads calculated from initial shut-in pressures of the Wolfcamp and Pennsylvanian brine aquifers, the two regionally important deep-basin aquifers downgradient of the proposed repository host rock. Eighty percent of the 5502 DSTs were screened from the data base containing DST data from various deep-basin geologic units because they did not comply with shut-in time and shut-in pressure agreement criteria. After screening, three sets of pressure-depth diagrams and potentiometric surfaces were constructed, corresponding to three levels of data refinement. These results indicate the possible need for more data from an areally extended study area.

  5. Diagenetic overprint of original depositional architecture in a shallow water carbonate reservoir, Permian Basin, Texas

    SciTech Connect (OSTI)

    Ruppel, S.C.; Lucia, F.J. )

    1996-01-01

    Permian shallow-water carbonate reservoirs are highly heterogeneous because of complex variations in depositional facies produced by high-frequency sea level rise and fall. Accordingly, establishment of a cycle stratigraphic framework is fundamental to defining reservoir heterogeneity. Because nearly all of these reservoirs have experienced multiple episodes of dolomitization and sulfate emplacement, however, permeability is a n of diagenetic overprint. The extent to which diagenesis can affect permeability development is dramatically displayed in the Grayburg Formation (middle Permian) at South Cowden field, Weit Texas. Three scales of cyclicity contribute to original depositional facies heterogeneity in the Grayburg; high-frequency cycles, averaging 3 meters in thickness, constitute the fundamental architectural element in the main reservoir interval. Despite original depositional heterogeneity due to this cyclicity, however, permeability development is substantially the result of two diagenetic events: (1) dolomite diagenesis in vertically burrowed wackestones and packstones and (2) late alteration and removal of anhydrite. Dolomite diagenesis in vertically burrowed wackestones and packstones has produced irregular vertical zones of higher permeability in mud-dominated bases of high-frequency cycles in leeward ramp-crest highstand successions. Because dolomite diagenesis is concentrated in burrowed highstand successions, the distribution of resultant permeability trends is partly constrained by patterns of longterm accommodation and high frequency cyclicity. Anhydrite diagenesis, which is characterized by conversion to gypsum or by complete removal of sulfate, is developed along basinward margins of the field and cross cuts original depositional framework.

  6. Diagenetic overprint of original depositional architecture in a shallow water carbonate reservoir, Permian Basin, Texas

    SciTech Connect (OSTI)

    Ruppel, S.C.; Lucia, F.J.

    1996-12-31

    Permian shallow-water carbonate reservoirs are highly heterogeneous because of complex variations in depositional facies produced by high-frequency sea level rise and fall. Accordingly, establishment of a cycle stratigraphic framework is fundamental to defining reservoir heterogeneity. Because nearly all of these reservoirs have experienced multiple episodes of dolomitization and sulfate emplacement, however, permeability is a n of diagenetic overprint. The extent to which diagenesis can affect permeability development is dramatically displayed in the Grayburg Formation (middle Permian) at South Cowden field, Weit Texas. Three scales of cyclicity contribute to original depositional facies heterogeneity in the Grayburg; high-frequency cycles, averaging 3 meters in thickness, constitute the fundamental architectural element in the main reservoir interval. Despite original depositional heterogeneity due to this cyclicity, however, permeability development is substantially the result of two diagenetic events: (1) dolomite diagenesis in vertically burrowed wackestones and packstones and (2) late alteration and removal of anhydrite. Dolomite diagenesis in vertically burrowed wackestones and packstones has produced irregular vertical zones of higher permeability in mud-dominated bases of high-frequency cycles in leeward ramp-crest highstand successions. Because dolomite diagenesis is concentrated in burrowed highstand successions, the distribution of resultant permeability trends is partly constrained by patterns of longterm accommodation and high frequency cyclicity. Anhydrite diagenesis, which is characterized by conversion to gypsum or by complete removal of sulfate, is developed along basinward margins of the field and cross cuts original depositional framework.

  7. The Spraberry trend, Midland basin, Texas: Development, innovation, and reserve growth potential in a mature giant

    SciTech Connect (OSTI)

    Guevara, E.H. ); Tyler, N. )

    1991-03-01

    The Spraberry trend area field is a stratigraphic trap about 60 mi long (N-S) and 40 mi wide (E-W) on a west-dipping monocline in the central Midland basin, west Texas. It contained 9,500 MMbls of in-place oil at discovery in 1949; recovery efficiency in these solution-gas-drive, originally underpressured reservoirs is projected to be 8%. There are more than 10,000 wells in the field, which, in the 1980s, was among the most intensely drilled areas in the nation. Wells are mostly at 160-ac and locally at 40-ac centers. Rapid production declines prompted local waterflooding. The Spraberry trend has been the experimental site of significant technological innovations, among them imbibition flooding, drilling using air, horizontal wells, and development of naturally fractured reservoirs. Main reservoirs occur in the Spraberry, Dean, and upper Wolfcamp formations (Lower Permian) at depths ranging from about 6,000 to 9,000 ft. They are naturally fractured, very fine-grained sandstones and siltstones in beds up to 14 ft thick, forming part of mid- to outer-fan, channel-fill and associated submarine-fan facies. Permeabilities average less than 1 md, and porosities are mostly less than 10%. Geochemical data suggest indigenous oils and short migration paths. Oils are paraffinic-naphthenic, light (36-40 API), and low in sulfur (0.17%). Entrapment is a product of reservoir pinch-out into slope and base-of-slope mud facies. Internal reservoir compartments result from channel-to-interchannel facies changes causing intrareservoir stratigraphic traps.

  8. Report of the South Texas Project Allegations Review Team. Docket Nos. 50-498 and 50-499, Houston Lighting and Power Company et al.

    SciTech Connect (OSTI)

    Kokajko, L.; Skay, D.; Wang, H.; Murphy, D.

    1995-03-01

    This report provides the results of the South Texas Project Allegations Review Team of the US Nuclear Regulatory Commission. This team was formed to obtain and review allegations from individuals represented by three attorneys who had contacted Congressional staff members. The allegers were employed in various capacities at South Texas Project Electric Generating Station, licensed by Houston Lighting and Power Company, et al.; therefore, the allegations are confined to this site. The South Texas Project Allegations Review Team reviewed, referred, and dispositioned concerns related to discriminatory issues (harassment and intimidation), falsification of records and omission of information, and various technical issues. The team was able to substantiate certain technical issues of minor safety significance or regulatory concern at the South Texas Project facility, but it did not find widespread discriminatory practices such as harassment and intimidation.

  9. Application of advanced reservoir characterization, simulation, and production optimization strategies to maximize recovery in slope and basin clastic reservoirs, West Texas (Delaware Basin), Class III

    SciTech Connect (OSTI)

    Dutton, Shirley P.; Flanders, William A.; Zirczy, Helena H.

    2000-05-24

    The objective of this Class 3 project was to demonstrate that detailed reservoir characterization of slope and basin clastic reservoirs in sandstones of the Delaware Mountain Group in the Delaware Basin of West Texas and New Mexico is a cost effective way to recover a higher percentage of the original oil in place through strategic placement of infill wells and geologically based field development. Phase 1 of the project, reservoir characterization, was completed this year, and Phase 2 began. The project is focused on East Ford field, a representative Delaware Mountain Group field that produces from the upper Bell Canyon Formation (Ramsey sandstone). The field, discovered in 1960, is operated by Oral Petco, Inc., as the East Ford unit. A CO{sub 2} flood is being conducted in the unit, and this flood is the Phase 2 demonstration for the project.

  10. South Belridge fields, Borderland basin, U. S. , San Joaquin Valley

    SciTech Connect (OSTI)

    Miller, D.D. ); McPherson, J.G. )

    1991-03-01

    South Belridge is a giant field in the west San Joaquin Valley, Kern County. Cumulative field production is approximately 700 MMBO and 220 BCFG, with remaining recoverable reserves of approximately 500 MMBO. The daily production is nearly 180 MBO from over 6100 active wells. The focus of current field development and production is the shallow Tulare reservoir. Additional probable diatomite reserves have been conservatively estimated at 550 MMBO and 550 BCFG. South Belridge field has two principal reservoir horizons; the Mio-Pliocene Belridge diatomite of the upper Monterey Formation, and the overlying Plio-Pleistocene Tulare Formation. The field lies on the crest of a large southeast-plunging anticline, sub-parallel to the nearby San Andreas fault system. The reservoir trap in both the Tulare and diatomite reservoir horizons is a combination of structure, stratigraphic factors, and tar seals; the presumed source for the oil is the deeper Monterey Formation. The diatomite reservoir produces light oil (20-32{degree} API gravity) form deep-marine diatomite and diatomaceous shales with extremely high porosity (average 60%) and low permeability (average 1 md). In contrast, the shallow ({lt}1000 ft (305 m) deep) overlying Tulare reservoir produces heavy oil (13-14{degree} API gravity) from unconsolidated, arkosic, fluviodeltaic sands of high porosity (average 35%) and permeability (average 3000 md). The depositional model is that of a generally prograding fluviodeltaic system sourced in the nearby basin-margin highlands. More than 6000 closely spaced, shallow wells are the key to steamflood production from hundreds of layered and laterally discontinuous reservoir sands which create laterally and vertically discontinuous reservoir flow units.

  11. Texas - Compare - U.S. Energy Information Administration (EIA)

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

    Texas Texas

  12. Texas - Rankings - U.S. Energy Information Administration (EIA)

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

    Texas Texas

  13. Texas - Search - U.S. Energy Information Administration (EIA)

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

    Texas Texas

  14. The tectonic mechanism for uplift and rotation of crustal blocks in the Central basin platform, Permian basin, Texas and New Mexico

    SciTech Connect (OSTI)

    Yang Kennming; Dorobek, S.L. )

    1991-03-01

    The Central basin platform is a positive tectonic element in the subsurface of the Permian basin. This enigmatic platform strikes north-northwest-south-southeast and at a high angle to the Marathon fold-and-thrust belt to the south. Although the uplift of the platform was related temporally to major overthrusting in the orogenic belt to the south and east, its formative mechanisms are still poorly understood. Previously compiled tectonic maps and cross sections were analyzed to identify the significant characteristics of this complicated structure. (1) Much of the platform is bounded by laterally discontinuous, high-angle faults with large vertical displacements. (2) The bounding faults suggest that the platform is composed of several discrete blocks that are arranged in a dextral en echelon pattern. (3) The southwest and northeast corners of each block typically are bounded by major faults; block uplift is greatest at the southwest and northeast corners. (4) Blocks are separated by west-northwest-east-southeast-trending transfer zones. These characteristics suggest that the Central Basin platform was subjected to a north-northwest-south-southeast-trending dextral couple that caused the platform to split into several blocks. Individual blocks rotated in the same clockwise sense and produced the maximum uplift observed at the southwest and northeast corners of blocks. In addition to the above characteristics, the amount of uplift an the width of individual blocks progressively decrease toward the north; block boundaries also become less defined northward. However, these additional complexities are not fully understood yet.

  15. Depositional environments, sequence stratigraphy, and trap configuration of lower Wolfcampian clastics along eastern edge of Midland basin, west Texas

    SciTech Connect (OSTI)

    Stewart, N.R.; Reuter, S.G.

    1989-03-01

    The Lower Permian (lower Wolfcampian) along the eastern edge of the Midland basin, west Texas, is characterized by ramp-type shelf margins. During eustatic lowstand, nearshore sedimentation shifted drastically to the west into a basinal setting below the Pennsylvanian (Canyon) shelf margin. Core descriptions demonstrate that lowstand systems tract (LST) and transgressive systems tract (TST) siliciclastics were deposited in deltaic and coastal-plain environments. Prodelta, delta-front, and stream-mouth bar facies are associated with the LST. Coastal-plain and distributary channels are preserved in the TST. The sequence stratigraphic framework indicates type 1 sequence boundaries at 287 Ma, 282 Ma, and 280 Ma in the lower Wolfcampian clastics. This lower Wolfcampian package of sedimentary rocks overlies the Pennsylvanian and is capped by the 279-Ma middle Wolfcampian unconformity. All three sequence boundaries and associated systems tract deposits exhibit a prograding stacking pattern within the sequence stratigraphic framework. Basinally restricted prograding LST deltaic rocks are overlain by backstepping TST deltaics and highstand systems tract (HST) outer marine shales. Production in lower Wolfcampian clastic fields is associated with fine-grained quartzarenites up to 45 ft thick which were deposited in stream-mouth bars. Delta-front and prodelta low-permeability shales encase the reservoir facies, forming lateral permeability barriers. HST outer marine shales deposited over the stream-mouth-bar sandstones act as a top seal, creating a stratigraphic trap and providing source for the high-BTU gas and oil produced from these basinally restricted LST deltaics.

  16. 1,"W A Parish","Coal","NRG Texas Power LLC",3675 2,"South Texas Project","Nuclear","STP Nuclear Operating Co",2560

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

    Texas" ,"Plant","Primary energy source","Operating company","Net summer capacity (MW)" 1,"W A Parish","Coal","NRG Texas Power LLC",3675 2,"South Texas Project","Nuclear","STP Nuclear Operating Co",2560 3,"Martin Lake","Coal","Luminant Generation Company LLC",2410 4,"Comanche Peak","Nuclear","Luminant Generation Company LLC",2400

  17. Regional basinal sandstone depositional patterns during the Guadalupian (Late Permian), Delaware basin, west Texas-New Mexico

    SciTech Connect (OSTI)

    Geisen, J.H.; Scholle, P.A. )

    1990-05-01

    Examination of well logs from more than 300 Delaware basin wells penetrating the Bell Canyon and Brushy Canyon formations has allowed definition of regional depositional patterns during the Late Permian (Guadalupian). Characteristic gamma-ray hot-kicks mark thin but widespread calcareous shales or limestones representing starved basin sedimentation during sea level highstands. Correlation of such markers along three strike and ten dip lines permitted isopaching of intervening lowstand clastic wedges. The low-stand wedges typically thin significantly from basin margin to basin center and are marked by a prominent linearity oriented perpendicular to the margin. These lineations probably represent channelized turbidite and grain-flow deposits. Most intervals show dozens of such lineations indicating multiple input points for terrigenous detritus rather than just a few major point sources of debris. The resulting deposits appear to be more apron-like than fan-like and coalesce into broad, sheetlike deposits toward the basin center. Isopach thicks vary in position through time, but terrigenous sediment transport is predominantly from northerly directions throughout the analyzed interval. Thus, the filling of the Midland basin at the close of Cherry Canyon deposition did not result in a major new source of terrigenous debris from the east (Central Basin platform). The well-sorted nature of the basinal sands, their widely distributed input points, apron-like geometry, and other factors argue for migration of eolian dunes to the shelf margin during sea level lowstands. Transport of these well-sorted, unconsolidated sands into the basin was not however, mainly by direct eolian processes as has been proposed recently, but must have involved submarine current mechanisms.

  18. Geology and geohydrology of the Palo Duro Basin, Texas Panhandle. Report on the progress of nuclear waste isolation feasibility studies, 1979

    SciTech Connect (OSTI)

    Gustavson, T.C.; Presley, M.W.; Handford, C.R.; Finley, R.J.; Dutton, S.P.; Baumgardner, R.W. Jr.; McGillis, K.A.; Simpkins, W.W.

    1980-01-01

    Since early 1977, the Bureau of Economic Geology has been evaluating several salt-bearing basins within the State of Texas as part of the national nuclear repository program. The Bureau, a research unit of The University of Texas at Austin and the State of Texas, is carrying out a long-term program to gather and interpret all geologic and hydrologic information necessary for description, delineation, and evaluation of salt-bearing strata in the Palo Duro and Dalhart Basins of the Texas Panhandle. The program in FY 79 has been subdivided into four broad research tasks, which are addressed by a basin analysis group, a surface studies group, a geohydrology group, and a host-rock analysis group. The basin analysis group has delineated the structural and stratigraphic framework of the basins, initiated natural resource assessment, and integrated data from 8000 ft (2400 m) of core material into salt-stratigraphy models. Salt depth and thickness have been delineated for seven salt-bearing stratigraphic units. Concurrently, the surface studies group has collected ground and remotely sensed data to describe surficial processes, including salt solution, slope retreat/erosion mechanisms, geomorphic evolution, and fracture system development. The basin geohydrology group has begun evaluating both shallow and deep fluid circulation within the basins. The newly formed host-rock analysis group has initiated study of cores from two drilling sites for analysis of salt and the various lithologies overlying and interbedded with salt units. This paper, a summary report of progress in FY 79, presents principal conclusions and reviews methods used and types of data and maps generated.

  19. Porosity distribution in Wolfcamp strata, Palo Duro basin, Texas panhandle: implications for deep-basin ground-water flow

    SciTech Connect (OSTI)

    Conti, R.D.; Wirojanagud, P.

    1984-04-01

    Average-porosity distributions in the Wolfcamp deep-basin aquifer are critical to discernment of the geographic trends in effective-porosity in the Palo Duro basin. Precise data are used to improved resolution of porosity values for computer-simulated areal ground-water modeling. Assessing vertical distributions of lithology and porosity in each well studied involves analysis of crossplotted neutron- and density-porosity log responses. This method more accurately identifies lithology and porosity than does the commonly employed crossplotted neutron-porosity and sonic (interval travel time) responses. Log-derived average-porosity distributions yield information about effective pore volume (i.e., movable water) in the Wolfcamp aquifer and enhance the accuracy of estimated of travel times and velocities of brines in basinwide traverses. Mathematical analysis of average travel time and total effective pore volume yield estimates of the rates of annual discharge from the Wolfcamp aquifer in the Palo Duro basin. Based on average flush rates between 2.2 and 1.5 m.y., annual discharge rates from the Wolfcamp aquifer across the northern and eastern basin boundaries, are about 3.6 x 10/sup 5/ m/sup 3/ year/sup -1/ to 5.3 x 10/sup 5/m/sup 3/ year/sup -1/.

  20. Petroleum source rock potential and thermal maturity, Palo Duro Basin, Texas

    SciTech Connect (OSTI)

    Dutton, S.P.

    1980-01-01

    Samples collected from 20 geographically widespread wells in the sparsely drilled Palo Duro Basin were analyzed for total organic carbon content (TOC). Highest values of TOC, up to 6.9%, occur in Upper Permian San Andres dolomite in the southern part of the basin. Pennsylvanian and Lower Permian (Wolfcampian) basinal shales contain up to 2.4% TOC and are fair to very good source rocks. Kerogen color and vitrinite reflectance, which indicate maximum paleotemperatures, were analyzed in all samples containing greater than 0.5% TOC. Pennsylvanian and Wolfcampian kerogen is yellow orange to orange, an indication that temperatures were sufficiently high to begin to generate hydrocarbons from lipid-rich organic material. Palo Duro Basin samples have a broad range of vitrinite reflectance values, but populations with the lowest reflectance probably indicate the true temperatures that were reached in the basin. Average reflectance in representative Pennsylvanian vitrinite is 0.52%; in Wolfcampian samples the average reflectance is 0.48%. These values are consistent with kerogen color and suggest that basinal source rocks may have begun to generate hydrocarbons.

  1. Wolfcampian and early Leonardian fore-shelf carbonate debris production, Permian basin, west Texas

    SciTech Connect (OSTI)

    Becher, J.W.; Von Der Hoya, H.A. )

    1990-05-01

    Since 1980, a number of Wolfcampian and early Leonardian oil fields have been discovered in a previously unexplored carbonate environment of the Permian basin i.e. basinal fore-shelf debris. These fields range up to 25 MMBOE in size. The Permian basin formed during the Early Pennsylvanian through the earliest Leonardian. Carbonate buildups dominated shelf-edge deposition and a syntectonic wedge of shelf debris was shed into the basins during both high and low sea level stands. Combined eustatic and tectonic sea level fluctuations of over 300 ft have been documented. The geometry, texture, and seismic expression of the debris changes with depositional slope, which ranges from very steep fault-block edges on the Central Basin platform to gentle ramps on the eastern shelf. Productive, low-stand deposits derived from steep shelf edges, consist of turbidite grainstones; clean, very coarse, lithoclastic, debris flaws; and allochthonous slide blocks. These deposits were derived from point sources on the eroded shelf and have a single-lobe or multi-lobe fan geometry. Debris clasts commonly display subaerial lithification and leaching. Lowstand fans extend 4-8 mi into the basin. Productive, lowstand deposits derived from ramp settings have a submarine channel geometry and consist dominantly of grainstone and packstone. Porosity has been enhanced by late subsurface solution. Nonproductive, highstand deposits were derived from a line source and have an apron geometry. These deposits consist of thinly bedded shaly, bioclastic turbidites with no evidence of lithification before final transport.

  2. Evolution of Permian carbonate shelf and foreshelf detrital systems, Midland basin, Texas

    SciTech Connect (OSTI)

    Mazzullo, S.J.; Reid, A.M. II; Reid, S.T.

    1986-03-01

    A major phase of shelf progradation and consequent filling of the Midland basin began in the Early Permian. Prior to this time, shelf carbonate systems were mostly ineffective in generating coarse detritus in quantities sufficient to infill adjoining basins. Beginning in the Early Permian (Wolfcampian), however, the character of shelf and basin deposition was abruptly modified, in part because of faunal changes - proliferation of rock-forming biotic communities and the consequent potential for rapid shelf-marginal oversteepening - and the effects of sea level fluctuations and periods of shale influx. Shelf systems in the northern Midland basin and Eastern shelf evolved from ramps in the lowermost Wolfcamp to steep rimmed platforms by the lower Leonard. Shelf progradation into the Midland basin was cyclic, with extensive carbonate shelves having developed during sea level highstands and massive shale wedges deposited during alternate lowstands. Coarse megabreccia with markedly little sand dominates in the lower to middle Wolfcamp systems, despite the occurrence of ramps in this section. Such an anomaly can be explained by invoking widespread shelf wastage caused by the inherent instability and failure of the shale slopes on which these ramps were deposited. In certain middle Wolfcamp zones, thin shelf-ramp sections may be recognized only because any thick shelf-marginal buildups that may have been present have been displaced into adjoining basinal tracts. The evolution to rimmed-platform shelves by the lower Leonard strata, foreshelf debris occurs mostly as complexes of megabreccia wedges and aprons, anastomosing megabreccia, and sand-channel and lobe deposits derived from adjoining rimmed-platforms. Major variations exist in the gross geometries of foreshelf units and component reservoirs even laterally within rocks of the same age.

  3. Sedimentary basins on the connugate margins of South America and Africa

    SciTech Connect (OSTI)

    Moore, G.T. )

    1990-05-01

    An Early Cretaceous spreading system formed the South Atlantic by separating South America from Africa along two subparallel major transform fault systems. The distribution of major sedimentary depocenters is controlled by the complex interplay of two factors: the late Mesozoic-Cenozoic cycle of sea-floor spreading and the legacy of a Precambrian collage of ancient cores that comprised western Gondwana. Three spreading modes created this configuration: rift, transform, and subduction. Each produces a different geometry and tectonic framework for the accumulation of sediment. Rifted margins (60%) contain basins that are elongate, form with their depocenter axes inboard of the ocean-continent transition, and rest on a tectonically complex, foundered basement. Transform margins have abrupt ocean-continent transitions. Such margins (30%) may be sediment starved or contain a thick sedimentary section controlled by the volcanic ridges of transform faults. Off Tierra del Fuego, Burdwood Bank is bounded on the north by a fossil (aseismic) subduction zone. The associated basin is an elongate, deformed accretionary prism of sediments on a gently dipping, faulted oceanic plate. The South Atlantic margins are divisible into 68 basins or segments that collectively contain over 33 {times} 106 km{sup 3} of syn- and postbreakup sediments. The South American margin contains 22 {times} 10{sup 6} km{sup 3} in 46 basins, and the African margin, 11 {times} 10{sup 6} km{sup 3} in 22 basins. Over 65% of the basins have a sediment column greater than 5 km with some depocenters that locally exceed 10 km. The source rock quality and character vary along both margins. The top of the oil generation window averages about 3.3 km; however, due to differing thermal histories, individual basins can depart significantly from this average.

  4. Radioactive waste isolation in salt: peer review of the Office of Nuclear Waste Isolation's report on the Organic Geochemistry of Deep Groundwaters from the Palo Duro Basin, Texas

    SciTech Connect (OSTI)

    Fenster, D.F.; Brookins, D.G.; Harrison, W.; Seitz, M.G.; Lerman, A.; Stamoudis, V.C.

    1984-08-01

    This report summarizes Argonne's review of the Office of Nuclear Waste Isolation's (ONWI's) final report entitled The Organic Geochemistry of Deep Ground Waters from the Palo Duro Basin, Texas, dated September 1983. Recommendations are made for improving the ONWI report. The main recommendation is to make the text consistent with the title and with the objective of the project as stated in the introduction. Three alternatives are suggested to accomplish this.

  5. Characterization of bedded salt for storage caverns -- A case study from the Midland Basin, Texas

    SciTech Connect (OSTI)

    Hovorka, Susan D.; Nava, Robin

    2000-06-13

    The geometry of Permian bedding salt in the Midland Basin is a product of interaction between depositional facies and postdepositional modification by salt dissolution. Mapping high-frequency cycle patterns in cross section and map view using wireline logs documents the salt geometry. Geologically based interpretation of depositional and dissolution processes provides a powerful tool for mapping and geometry of salt to assess the suitability of sites for development of solution-mined storage caverns. In addition, this process-based description of salt geometry complements existing data about the evolution of one of the best-known sedimentary basins in the world, and can serve as a genetic model to assist in interpreting other salts.

  6. First status report on regional groundwater flow modeling for the Palo Duro Basin, Texas

    SciTech Connect (OSTI)

    Andrews, R.W.

    1984-12-01

    Regional groundwater flow within the principal hydrogeological units of the Palo Duro Basin is evaluated by developing a conceptual model of the flow regime in the shallow aquifers and the deep-basin brine aquifers and testing these models using a three-dimensional, finite-difference flow code. Semiquantitative sensitivity analysis (a limited parametric study) is conducted to define the system response to changes in hydrologic properties or boundary conditions. Adjoint sensitivity analysis is applied to the conceptualized flow regime in the Wolfcamp carbonate aquifer. All steps leading to the final results and conclusions are incorporated in this report. The available data utilized in this study are summarized. The specific conceptual models, defining the areal and vertical averaging of lithologic units, aquifer properties, fluid properties, and hydrologic boundary conditions, are described in detail. The results are delineated by the simulated potentiometric surfaces and tables summarizing areal and vertical boundary fluxes, Darcy velocities at specific points, and groundwater travel paths. Results from the adjoint sensitivity analysis included importance functions and sensitivity coefficients, using heads or the average Darcy velocities as the performance measures. The reported work is the first stage of an ongoing evaluation of two areas within the Palo Duro Basin as potantial repositories for high-level radioactive wastes. The results and conclusions should thus be considered preliminary and subject to modification with the collection of additional data. However, this report does provide a useful basis for describing the sensitivity and, to a lesser extent, the uncertainty of the present conceptualization of groundwater flow within the Palo Duro Basin.

  7. Geochemistry of Ca, Sr, Ba and Ra sulfates in some deep brines from the Palo Duro basin, Texas

    SciTech Connect (OSTI)

    Langmuir, D.; Melchior, D.

    1985-11-01

    The geochemistry of Ca, Sr, Ba and Ra sulfates in some deep brines from the Palo Duro Basin of north Texas, was studied to define geochemical controls on radionuclides such as /sup 90/Sr and /sup 226/Ra. Published solubility data for gypsum, anhydrite, celestite, barite and RaSO/sub 4/ were first reevaluated, in most cases using the ion interaction approach of Pitzer, to determine solubility products of the sulfates as a function of temperature and pressure. Ionic strengths of the brines were from 2.9 to 4.8 m, their temperatures and pressures up to 40/sup 0/C and 130 bars. Saturation indices of the sulfates were computed with the ion-interaction approach in one brine from the arkosic granite wash facies and four from the carbonate Wolfcamp Formation. All five brines are saturated with respect to gypsum, anhydrite and celestite, and three of the five with respect to barite. All are undersaturated by from 5 to 6 orders of magnitude with respect to pure RaSO/sub 4/. /sup 226/Ra concentrations in the brines, which ranged from 10/sup -11.3/ to 10/sup -12.7/ m, are not controlled by RaSO/sub 4/ solubility or adsorption, but possibly by the solubility of trace Ra solid solutions in sulfates including celestite and barite.

  8. Geological characterization of permian submarine fan reservoirs of the driver waterflood unit, Spraberry Trend, Midland Basin, Texas

    SciTech Connect (OSTI)

    Guevara, E.H.

    1989-01-01

    This book discusses the geological characterization and assessment of the relationship between reservoir stratigraphy and oil recovery of the Driver waterflood unit of the Spraberry Trend, Midland Basin, West Texas. In this study , the author focuses on the Driver waterflood unit, which is located in Midland, Glasscock, Upton, and Reagan Counties and is part of the giant Spraberry Trend currently being studied by the Bureau. Gamma-ray logs and scout cards from more than 350 wells and slabbed cores from 2 wells, along with core analyses and production data, provided the main sources of information for the study. Fifteen log-defined genetic-stratigraphic operational units were delineated in the Spraberry Formation and were correlated throughout the study area to define the stratigraphic framework. The text presents net sandstone and siltstone maps, cross sections, depth plots of core analyses, and maps of production data. The author describes the depositional systems and hydrocarbon distribution in the Driver unit (currently operated by Standard Oil), details the influence of reservoir stratigraphy on oil recovery, and outlines opportunities for additional recovery. He notes that reservoir management strategies must take into account the stratigraphic heterogeneities of accumulations in the unit. He concludes that a program of selective recompletions and infill drilling based on knowledge of both reservoir stratigraphy and natural fractures is the key to improving oil recovery from the Driver unit in particular and from the Spraberry Trend in general.

  9. Recurrent motion on Precambrian-age basement faults, Palo Duro basin, Texas Panhandle

    SciTech Connect (OSTI)

    Budnik, R.T.

    1983-03-01

    The distribution of Late Precambrian through Quaternary strata in the Palo Duro basin and surrounding uplifts documents recurrent motion on Precambrian-age basement faults. Basement blocks have been uplifted with little tilting or folding of overlying strata along a system of northwest-southeast oriented faults, part of a regional trend extending from central Colorado to southwestern Oklahoma. The orientation of basement terranes in Colorado and that of a 50-mi (80-km) long mylonite zone in east-central New Mexico suggest a Precambrian age for the faults. An Arkosic sandstone overlies basement and underlies a Cambrian(.) quartzose sandstone in a few Palo Duro basin wells. It may represent debris shed from active fault blocks during the opening of the southern Oklahoma aulocogen in the Late Precambrian or Early Cambrian. Ordovician carbonates thin or are missing beneath Mississippian carbonates on some fault blocks, indicating a post-Ordovician-pre-Mississippian period of faulting. The greatest amount of deformation occurred during the Pennsylvanian. Thickness, distribution, and facies of sediments were controlled by the location of active faults. Lower Pennsylvanian strata thin by up to 50% across some structures. Fault blocks provided sources of arkosic debris and loci for carbonate buildups throughout the Pennsylvanian and Early Permian. Around the periphery of the basin, Late Pennsylvanian or Early Permian faulting caused a wedging out of older units beneath the Wolfcamp. Permian, Triassic, and Neogene units, along with present topography, all have been subtly affected by basement structures. The entire section thins over basement highs. Middle and Upper Permian evaporites are thicker in structural lows. The overlying Dockum Group (Triassic) and Ogallala Formation (Neogene), both nonmarine clastic units, become finer grained over basement highs. Present topographic highs coincide with some basement highs.

  10. Regional elemental abundances within South Pole-Aitken basin as measured with lunar prospector gamma-ray spectrometer data.

    SciTech Connect (OSTI)

    Lawrence, David J. ,; Pieters, Carlé M.; Elphic, R. C.; Gasnault, O. M.; Prettyman, T. H.; Feldman, W. C.

    2003-01-01

    South Pole-Aitken (SPA) basin has been a target of intense study since it is one of the largest impact basins in the solar system. It is thought that SPA basin excavated deep into the lunar crust and possibly even the mantle. Such conclusions have been supported by the observed mafic and thorium composition anomalies seen across the entire basin. One of the major goals of lunar and planetary science has been to measure and understand the composition of the non-mare materials within SPA basin. It is expected that this information will help to increase our understanding of the formation and differentiation processes that occurred early on the Moon.

  11. Extent of water-rock interactions in Lower Permian Wolfcamp carbonates, Palo Duro Basin, Texas

    SciTech Connect (OSTI)

    Fisher, R.S.; Posey, H.H.

    1985-01-01

    A laterally-extensive permeable zone in upper Wolfcampian carbonate strata constitutes the first important transmissive unit below a thick evaporite sequence that is being considered for nuclear waste isolation. The extent of water-rock interaction was evaluated by comparing the chemical and isotopic composition of formation water and core collected at four DOE test wells. Wolfcamp mineralogy is dominantly calcite and dolomite with minor anhydrite at each of the four sites despite minor variations in depositional environment, diagenetic alteration, and abundance of clastic material. Isotopic compositions of calcite and dolomite and of anhydrite are within the ranges expected for Permian marine sediments altered by early diagenesis. Wolfcamp formation water compositions are more variable than host rock compositions, and are not completely controlled by local water-rock equilibria. Wolfcamp brines from two wells in the western part of the basin have depleted isotopic compositions relative to the two eastern wells and have not equilibrated with Wolfcamp carbonates, whereas the eastern fluids have. Strontium in the western samples is more radiogenic than that of the eastern samples, indicating a greater influence of clays or feldspars on the western fluids. Comparison of water and rock compositions suggests: (1) the western brines have interacted less with the carbonate host than the eastern brines due to shorter residence times or greater water: rock ratios, and (2) the minerals encountered along flow paths prior to entering the Wolfcamp are different for the western and eastern Wolfcamp brines.

  12. Radionuclides in plankton from the South Pacific Basin

    SciTech Connect (OSTI)

    Marsh, K.V.; Buddemeier, R.W.

    1984-03-23

    We have initiated an investigation of the utility of marine plankton as bioconcentrating samplers of low-level marine radioactivity in the southern hemisphere. A literature review has shown that both freshwater and marine plankton have trace element and radionuclide concentration factors (relative to water) of up to 10/sup 4/. We participated in Operations Deepfreeze 1981 and 1982, collecting a total of 48 plankton samples from the USCGC Glacier on its Antarctic cruises. Battelle Pacific Northwest Laboratories sampled air, water, rain, and fallout. We were able to measure concentrations in plankton of the naturally-occurring radionuclides /sup 7/Be, /sup 40/K, and the U and Th series, and we believe that we have detected low levels of /sup 144/Ce and /sup 95/Nb in seven samples ranging as far south as 68/sup 0/. Biological identification of the plankton suggests a possible correlation between radionuclide concentration and the protozoa content of the samples. 7 references, 5 figures.

  13. Diagenesis of early Permian evaporites and carbonates, Palo Duro Basin, Texas

    SciTech Connect (OSTI)

    Posey, H.H.; Fisher, R.S.; Hovorka, S.D.; Elliott, L.A.

    1985-01-01

    Anhydrite nodules within dolomite grainstone constitute a characteristic facies marking the transition from open marine deposits of the Lower Permian Wolfcamp Formation into hypersaline dolomite and evaporite deposits of the overlying Wichita Formation. Accompanying this transition is a shift from nodular to bedded anhydrite, a decrease in faunal diversity, finer carbonate grain size, a greater abundance of algae and a decrease in calcite abundance. Anhydrite nodules in the Upper Wolfcamp probably displaced carbonate muds before Wichita deposition. Other diagenetic features include dolomitization, and anhydrite recrystallization and replacement by silica. Sr, C, O and S isotopes help account for many of the primary and diagenetic features. Values for delta/sup 34/S and /sup 87/Sr//sup 86/Sr from unaltered Wichita anhydrite beds (approx.13.5 per thousands and 0.7078) indicate equilibrium with Early Permian seawater. Unaltered Upper Wolfcamp nodules, most abundant in the northeastern Palo Dura Basin, have lighter delta/sup 34/S (approx.12.7 per thousands) but probably record the seawater delta/sup 34/S composition of Early Permian, pre-Wichita Formation seawater. delta/sup 34/S of altered anhydrite nodules, cements and anhydrite veins are 1 to 4 per thousands heavier, probably due to anhydrite reduction during silicification. Dolomite ranges from -1 to +5.5 (delta/sup 13/C, PDB) and -1 to +3(delta/sup 18/O, PDB) whereas limestone ranges from -1 to +7 (delta/sup 13/C) and -4.5 to -2.5 (delta/sup 18/O). Dolomite delta/sup 13/C and delta/sup 18/O values are 2 to 4 thousands heavier than adjacent limestone, suggesting that dolomite and calcite are locally in equilibrium.

  14. Strontium and sulfur isotope study of well-preserved Permian anhydrite, Palo Duro basin, Texas

    SciTech Connect (OSTI)

    Leary, D.A. )

    1990-05-01

    The {delta}{sup 34}S, {sup 87}Sr/{sup 86}Sr ratio, and strontium concentrations for 50 well-preserved samples of Permian marine anhydrite have been determined. The samples were collected from two continuous cores drilled through cyclic Permian evaporites, The Department of Energy drilled the samples in its search for a permanent storage facility for high-level nuclear waste. Primary depositional fabrics (selenite pseudomorphs) and high strontium concentrations (average 1,850 ppm), in association with published bromide and fluid inclusion data from associated halite, suggest primary seawater {sup 87}Sr/{sup 86}Sr ratios may be recorded in many of the samples. The general shape of the {sup 87}Sr/{sup 86}Sr ratio curve through the Permian is in accord with previously published observations. However, the increased stratigraphic detail from this unique set of cores constrains the abrupt charge in {sup 87}Sr/{sup 86}Sr during the Permian at a precision previously available only in Deep Sea Drilling Project material. Interpretation of the more complex portions of the curve is limited by poor biostratigraphic control, the specter of provincial early diagenetic effects, and interpretation of the time significance of hiatal surfaces in cyclic strata. Age relationships are constrained by a K-Ar date on an interbedded volcanic ash in the Ochoan strata, and fusulinid age determinations of a well-documented regional transgression during the earliest Guadalupe. Sulfur isotopes yield typical Permian values of 12{per thousand} during the marine portion of the basin fill phase, and abruptly shift to 10{per thousand} in those cycles with a significant component of siliciclastic sediment.

  15. Dolomitization of coeval shelf and fore-shelf carbonates, Lower Permian, Midland basin, Texas

    SciTech Connect (OSTI)

    Mazzullo, S.J.; Qiuchang, Ye )

    1991-03-01

    Coeval shelf and fore-shelf carbonates in Lower Permian (Leonardian) rocks in the Midland basin are pervasively dolomitized. Shelf strata consist of a regional mosaic of shelf margin reef, lagoon, and peritidal facies associated with contemporaneous evaporite deposition; fore-shelf facies consist of resedimented shelf margin deposits. Numerous relative sea-level fluctuations that resulted in the formation of Type 1 and 2 unconformities are recognized throughout this section. Mean stable oxygen and carbon isotopic compositions of the shelf strate suggest that dolomitization occurred essentially syndepositionally, likely by interaction with normal marine( ) and hypersaline fluids. In fore-shelf strata petrographic evidence, in combination with paleotemperature estimates from isotopic data and the burial depth-temperature history of these rocks, suggest relatively early (late Permian) dolomitization in rock-dominated systems. Three possible modes of dolomitization could have affected these fore-shelf beds: (1) dolomitization by reflux of normal-marine and/or hypersaline fluids during sea level highstands or lowstands; (2) dolomitization by mixed meteoric-marine fluids during lowstands; and (3) replacement by calcic dolomites via reaction with circulating marine fluids during deposition and early, shallow burial without organic matter influences. The latter mode of origin, however, is favored for most of the rocks examined on the basis of the slightly positive carbon isotopic compositions, Sr versus MgCO{sub 3} compositions (mean Sr 61 ppm, mean MgCO{sub 3} 49.5), and low Mn contents (mean 61 ppm) of the dolomites, although later burial recrystallization is indicated by their relatively depleted isotopic compositions.

  16. Haynes Wave Basin | Open Energy Information

    Open Energy Info (EERE)

    Wave Basin Jump to: navigation, search Basic Specifications Facility Name Haynes Wave Basin Overseeing Organization Texas A&M (Haynes) Hydrodynamic Testing Facility Type Wave Basin...

  17. Calculation and interpretation of crustal shortening along the Central Basin Platform, West Texas: A method to calculate basement motion for modeling input

    SciTech Connect (OSTI)

    Hoak, T.E. |; Sundberg, K.R.; Ortoleva, P.

    1998-12-31

    The analysis carried out in the Chemical Interaction of Rocks and Fluids Basin (CIRFB) model describes the chemical and physical evolution of the entire system. One aspect of this is the deformation of the rocks, and its treatment with a rigorous flow and rheological model. This type of analysis depends on knowing the state of the model domain`s boundaries as functions of time. In the Andrews and Ector County areas of the Central Basin Platform of West Texas, the authors calculate this shortening with a simple interpretation of the basic motion and a restoration of the Ellenburger formation. Despite its simplicity, this calculation reveals two distinct periods of shortening/extension, a relatively uniform directionality to all the deformation, and the localization of deformation effects to the immediate vicinities of the major faults in the area. Conclusions are drawn regarding the appropriate expressions of these boundary conditions in the CIRFB model and possible implications for exploration.

  18. Sequence stratigraphic model of the Rio Grande Delta, south west Texas: Potential analog for the Niger Delta

    SciTech Connect (OSTI)

    Banfield, L.A.; Anderson, J.B.; Vail, P.R.

    1996-12-31

    A sequence stratigraphic model developed from the ancient Rio Grande Delta in South West Texas is suggested as an analog for the Niger Delta. The two delta systems are characterized by high sand bedloads, shale diapirism with associated listric normal faulting, and large amounts of tidal and wave influence forming lower coastal plains characterized by swamps and estuaries. The sequence stratigraphic model of the ancient Rio Grande delta is based on approximately 1200 kilometers of single channel, 15 cubic inch water gun data, lithologic descriptions from approximately 25 long cores (28-30 m) located in 17-94 meters water depth, three gamma ray logs, paleontologic data from two cores, and oxygen isotopic data from one core (152 meters in length and located in 94 meters water depth). The combined data indicate that considerable quantities of sand are sequestered on the continental shelf and point sourcing the slope. The Rio Grande sequence stratigraphic model provides an improved understanding of sand deposits on the shelf, of the role of sediment bypass during lowstands, and of the base of slope deposits formed by headward eroding canyons (?) or channels (?) located at the shelf break. This information regarding the distribution of sand in the Rio Grande system can provide valuable insight into the reservoir distribution in the Niger system, improving existing reservoir predictions.

  19. AIR QUALITY IMPACTS OF LIQUEFIED NATURAL GAS IN THE SOUTH COAST AIR BASIN OF CALIFORNIA

    SciTech Connect (OSTI)

    Carerras-Sospedra, Marc; Brouwer, Jack; Dabdub, Donald; Lunden, Melissa; Singer, Brett

    2011-07-01

    The effects of liquefied natural gas (LNG) on pollutant emission inventories and air quality in the South Coast Air Basin of California were evaluated using recent LNG emission measurements by Lawrence Berkeley National Laboratory and the Southern California Gas Company (SoCalGas), and with a state-of-the-art air quality model. Pollutant emissions can be affected by LNG owing to differences in composition and physical properties, including the Wobbe index, a measure of energy delivery rate. This analysis uses LNG distribution scenarios developed by modeling Southern California gas flows, including supplies from the LNG receiving terminal in Baja California, Mexico. Based on these scenarios, the projected penetratino of LNG in the South Coast Air Basin is expected to be limited. In addition, the increased Wobbe index of delivered gas (resulting from mixtures of LNG and conventional gas supplies) is expected to cause increases smaller than 0.05 percent in overall (area-wide) emissions of nitrogen oxides (NOx). BAsed on the photochemical state of the South Coast Air Basin, any increase in NOx is expected to cause an increase in the highest local ozone concentrations, and this is reflected in model results. However, the magnitude of the increase is well below the generally accepted accuracy of the model and would not be discernible with the existing monitoring network. Modeling of hypothetical scenarios indicates that discernible changes to ambient ozone and particulate matter concentrations would occur only at LNG distribution rates that are not achievable with current or planned infrastructure and with Wobbe index vlaues that exceed current gas quality tariffs. Results of these hypothetical scenarios are presented for consideration of any proposed substantial expansion of LNG supply infrastructure in Southern California.

  20. Pennsylvanian and Permian paleogeography of south-central Idaho: The Wood River basin

    SciTech Connect (OSTI)

    Mahoney, J.B. ); Burton, B.R. ); O'Brien, J.P.; Link, P.K. )

    1991-02-01

    The Sun Valley Assemblage (Wood River, Dollarhide, and Grand Prize formations) was deposited in the Wood Rover basin in what is now south-central Idaho, north of the Snake River Plain, from the Atokan to Wolfcampian and Leonardian( ). Atokan and Des Moinesian deposition occurred in braided deltas and overlying clear water carbonate shoals. The rocks of this depositional system vary in thickness from tens to several hundreds of meters reflecting irregularities in the erosional surface on the underlying foundered Antler highland. This basal unconformity has been sheared during Mesozoic and Paleogene deformation. Significant regional subsidence of the Wood River basin began in the Des Moinesian, was most rapid in the Virgilian, and slowed in the Wolfcampian, resulting in total thickness of over 2,000 m for each of the three formations. In the central part of the basin (Wood River Formation) a sub-wave-base ramp system with southeastern paleoslope was fed by turbidite flows of mixed carbonate-siliciclastic fine-grained sediment that had been thoroughly mixed on a shelf area to the north and east. The carbonate fraction may have been derived from the Snaky Canyon Formation carbonate platform to the east. To the north, a siliciclastic fan or ramp system (Grand Prize Formation) was present. Virgilian and Wolfcampian strata represent highstand systems tracts and a lowstand tract is present in strata deposited near the Virgilian-Wolfcampian boundary.

  1. Water-quality data for aquifers, streams, and lakes in the vicinity of Keechi, Mount Sylvan, Oakwood, and Palestine salt domes, northeast Texas salt-dome basin

    SciTech Connect (OSTI)

    Carr, J.E.; Halasz, S.J.; Liscum, F.

    1980-11-01

    This report contains water-quality data for aquifers, streams, and lakes in the vicinity of Keechi, Mount Sylvan, Oakwood, and Palestine Salt Domes in the northeast Texas salt-dome basin. Water-quality data were compiled for aquifers in the Wilcox Group, the Carrizo Sand, and the Queen City Sand. The data include analyses for dissolved solids, pH, temperature, hardness, calcium, magnesium, sodium, bicarbonate, chloride, and sulfate. Water-quality and streamflow data were obtained from 63 surface-water sites in the vicinity of the domes. These data include water discharge, specific conductance, pH, water temperature, and dissolved oxygen. Samples were collected at selected sites for analysis of principal and selected minor dissolved constituents.

  2. Secondary natural gas recovery: Targeted applications for infield reserve growth in midcontinent reservoirs, Boonsville Field, Fort Worth Basin, Texas. Topical report, May 1993--June 1995

    SciTech Connect (OSTI)

    Hardage, B.A.; Carr, D.L.; Finley, R.J.; Tyler, N.; Lancaster, D.E.; Elphick, R.Y.; Ballard, J.R.

    1995-07-01

    The objectives of this project are to define undrained or incompletely drained reservoir compartments controlled primarily by depositional heterogeneity in a low-accommodation, cratonic Midcontinent depositional setting, and, afterwards, to develop and transfer to producers strategies for infield reserve growth of natural gas. Integrated geologic, geophysical, reservoir engineering, and petrophysical evaluations are described in complex difficult-to-characterize fluvial and deltaic reservoirs in Boonsville (Bend Conglomerate Gas) field, a large, mature gas field located in the Fort Worth Basin of North Texas. The purpose of this project is to demonstrate approaches to overcoming the reservoir complexity, targeting the gas resource, and doing so using state-of-the-art technologies being applied by a large cross section of Midcontinent operators.

  3. Meteorite search in the deflation basins in Lea County, New Mexico and Winkler County, Texas, USA: Discovery of Lea County 003 (H4)

    SciTech Connect (OSTI)

    Mikouchi, T; Buchanan, P C; Zolensky, M E; Welten, K C; Hutchison, R; Hutchison, M

    2000-01-14

    During the past few decades great numbers of meteorites have been recovered from the ice accumulation zones of Antarctica and from the vast Sahara. Although these two great deserts are the two most productive areas, the Southern High Plains in USA (New Mexico and Texas) and Nullarbor Plain, Western Australia have great potential for meteorite recovery. The number of meteorite finds from Roosevelt County, New Mexico alone exceeds 100 in only approximately 11 km{sup 2} area. Most meteorites from this area have been found on the floors of active deflation basins (blowouts) that have been excavated from a mantle of sand dunes. This area has no apparent fluvial or permafrost activity within the last 50,000 years, suggesting that only prevailing winds and natural aridity aid in the concentration and preservation of meteorites. The authors investigated these deflation surfaces in Lea County (the SE corner of New Mexico) and neighboring Winkler County, Texas following a prior search in this area which found two chondrites. They found a tiny H4 chondrite in this search and here they report its mineralogy and petrology along with preliminary data on its exposure history.

  4. Deep-water density current deposits of Delaware Mountain Group (Permian), Delaware basin, Texas and New Mexico

    SciTech Connect (OSTI)

    Harms, J.C.; Williamson, C.R.

    1988-03-01

    The Guadalupian Delaware Mountain Group is a 1000-1600-m (3281-5250-ft) thick section of siltstone and sandstone deposited in a deep-water density-stratified basin surrounded by carbonate banks or reefs and broad shallow evaporite-clastic shelves. The most prevalent style of basinal deposition was suspension settling of silt. Laminated siltstone beds are laterally extensive and cover basin-floor topographic irregularities and flat-floored channels as much as 30 m (99 ft) deep and 1 km or more wide. Channels can be observed in outcrop at the basin margin and can be inferred from closely spaced wells in the basin. The channels are straight to slightly sinuous, trend at high angles to the basin margin, and extend at least 70 km (43 mi) into the basin. Sandstone beds, confined to channels, form numerous stratigraphic traps. Hydrocarbon sealing beds are provided by laminated organic siltstone, which laterally can form the erosional margin where channels are cut into siltstone beds. Thick beds of very fine-grained sandstones fill the channels. These sandstones contain abundant large and small-scale traction-current-produced stratification. These sandy channel deposits generally lack texturally graded sedimentation units and show no regular vertical sequence of stratification types or bed thickness. Exploration predictions based on submarine fan models formed by turbidity currents would anticipate very different proximal-distal changes in sandstone geometry and facies. 16 figures.

  5. Application of advanced reservoir characterization, simulation, and production optimization strategies to maximize recovery in slope and basin clastic reservoirs, west Texas (Delaware Basin). Annual progress report, March 31, 1995--March 31, 1996

    SciTech Connect (OSTI)

    Dutton, S.P.; Hovorka, S.D.; Cole, A.G.

    1996-08-01

    The objective of this Class III project is to demonstrate that detailed reservoir characterization of clastic reservoirs in basinal sandstones of the Delaware Mountain Group in the Delaware Basin of West Texas and New Mexico is a cost-effective way to recover more of the original oil in place by strategic infill-well placement and geologically based field development. Reservoirs in the Delaware Mountain Group have low producibility (average recovery <14 percent of the original oil in place) because of a high degree of vertical and lateral heterogeneity caused by depositional processes and post-depositional diagenetic modification. Detailed correlations of the Ramsey sandstone reservoirs in Geraldine Ford field suggest that lateral sandstone continuity is less than interpreted by previous studies. The degree of lateral heterogeneity in the reservoir sandstones suggests that they were deposited by eolian-derived turbidites. According to the eolian-derived turbidite model, sand dunes migrated across the exposed shelf to the shelf break during sea-level lowstands and provided well sorted sand for turbidity currents or grain flows into the deep basin.

  6. Numerical modeling of regional ground-water flow in the deep-basin brine aquifer of the Palo Duro Basin, Texas Panhandle

    SciTech Connect (OSTI)

    Wirojanagud, P.; Kreitler, C.W.; Smith, D.A.

    1986-01-01

    Bedded Permian-age evaporite sequences in the Palo Duro Basin are being considered for a permanent nuclear waste repository by the U.S. Department of Energy. The purpose of this modeling study is to provide an understanding of regional ground-water flow in the formations beneath the Permian evaporite section. From this understanding, more detailed, smaller scale studies can be designed. This study is also intended to provide a better understanding of the boundary conditions and permeabilities of the aquifer and aquitard system as well as provide estimates of ground-water travel times across the basin. Numerical simulations were made of the Wolfcamp aquifer modeled as a single layer and of the entire Deep-Basin Brine aquifer system, including the Wolfcamp aquifer, modeled as a single layer.

  7. Risk assessment of drain valve failure in the K-West basin south loadout pit

    SciTech Connect (OSTI)

    MORGAN, R.G.

    1999-06-23

    The drain valve located in the bottom of the K-West Basin South Loadout Pit (SLOP) could provide an additional leak path from the K Basins if the drain valve were damaged during construction, installation, or operation of the cask loading system. For the K-West Basin SLOP the immersion pail support structure (IPSS) has already been installed, but the immersion pail has not been installed in the IPSS. The objective of this analysis is to evaluate the risk of damaging the drain valve during the remaining installation activities or operation of the cask loading system. Valve damage, as used in this analysis, does not necessarily imply large amounts of the water will be released quickly from the basin, rather valve damage implies that the valve's integrity has been compromised. The analysis process is a risk-based uncertainty analysis where best engineering judgement is used to represent each variable in the analysis. The uncertainty associated with each variable is represented by a probability distribution. The uncertainty is propagated through the analysis by Monte Carlo convolution techniques. The corresponding results are developed as a probability distribution and the risk is expressed in terms of the corresponding complementary cumulative distribution function (''risk curve''). The total risk is the area under the ''risk curve''. The risk of potentially dropping a cask into or on the IPSS and damaging the drain valve is approximately 1 x 10{sup -4} to 2 x 10{sup -5} per year. The risk of objects falling behind the IPSS and damaging the valve is 3 x 10{sup -2} to 6 x 10{sup -3} per year. Both risks are expressed as drain value failure frequencies. The risk of objects falling behind the IPSS and damaging the valve can be significantly reduced by an impact limiter and/or installing a gating or plate over the area bounded by the back of the IPSS and the wall of the SLOP. With either of these actions there is a 90 percent confidence that the frequency of drain valve

  8. Renewed petroleum generation related to Tertiary intrusions and increased heat flow, western Permian basin, Texas and New Mexico

    SciTech Connect (OSTI)

    Barker, C.E.; Pawlewicz, M.J.

    1989-03-01

    Higher paleogeothermal gradients, commencing in the Tertiary after maximum burial, have caused renewed petroleum generation in the western Permian basin. Evidence for this reheating is two distinct trends in the mean random vitrinite reflectance (R/sub m/) and depth data compiled from over 40 wells. One group, with a 0.7% R/sub m//km gradient, is from the western edge of the basin; the other, with a 0.5% R/sub m//km gradient, is from the central and eastern portions. Post-Mississippian tilting produced greater subsidence and a thicker, mostly uneroded sedimentary section in the eastern portion of the Permian basin. Continued tilting prior to the Cretaceous caused uplift and erosion that exposed the Upper Permian section in the western part. Potassium-argon ages of igneous intrusions along the western edge of the basin show they were emplaced about 35 Ma, followed by Miocene to Holocene basin-and-range-type block faulting and associated high heat flow. Isopach-reflectance contours confirm this renewed heating is post-tectonic - that is, it occurred after eastward tilting and erosion had reduced burial depth. Maximum temperatures computed from R/sub m/-depth relationships infer that paleogeothermal gradients exceeded 40/degrees/C/km (2.2/degrees/F/100 ft) in the Tertiary. This reheating thermally matured rocks as young as Guadalupian in the western Permian basin and apparently caused a second episode of petroleum generation. By this time, however, the potential reservoir rocks and evaporite seals had been deeply eroded, resulting in poor conditions for trapping the renewed pulse of petroleum.

  9. Sequence stratigraphic framework and exploration potential of lower Permian (Wolfcampian) gravity-flow deposits, eastern Midland Basin, Texas

    SciTech Connect (OSTI)

    Morgan, W.A.; Clopine, W.W. ); Kokkoros, G.F.; Wiley, B.H. )

    1996-01-01

    Eight major Wolfcampian sequences (W1-W8) have been identified on seismic data and well logs in a 1500 square mile study area along the Eastern Shelf of the Midland Basin. These sequences compose two lower frequency sequences (W1-W5 W6-W8) which are separated by a major erosional surface associated with a sea-level fall near the time of the early-middle Wolfcampian boundary. Sea-level falls associated with sequences W5 and W6 resulted in significant erosion of platform-margin deposits, incision of a submarine canyon several miles into the Eastern Shelf, and deposition of carbonate gravity flows in the Midland Basin. Gravity flows entered the basin via the submarine canyon and fed basin-floor fan systems which extend up to 25 miles basinward of the toe-of-slope. Within the study area, production from carbonate gravity-flow deposits is mostly from three submarine fan systems within sequences W5 and W6 - the Credo (10 MMBOER) fan (oldest) , the Triple M (5 MMBOER)-Howard Glasscock (7 MMBOER) fan, and the Hutto (5 MMBOER) fan (youngest). The maximum gross thickness of the fans ranges from 100 to 200 feet. Regional isolith and seismic amplitude data were used to high-grade a 70 square mile area in the vicinity of Triple M and Howard Glasscock fields. Model-based velocity inversions, constrained by sonic and density data from 52 wells, were performed utilizing a grid of 2-D seismic data and a 3-D survey. Both Triple M and Howard Glasscock fields are clearly defined by high-velocity anomalies within the productive basin-floor fan interval of sequence W6. An untested high-velocity anomaly with a velocity signature and stratal geometry similar to the two fields, and estimated reserves of 5 MMBOER, is scheduled to be drilled in 1995.

  10. Sequence stratigraphic framework and exploration potential of lower Permian (Wolfcampian) gravity-flow deposits, eastern Midland Basin, Texas

    SciTech Connect (OSTI)

    Morgan, W.A.; Clopine, W.W.; Kokkoros, G.F.; Wiley, B.H.

    1996-12-31

    Eight major Wolfcampian sequences (W1-W8) have been identified on seismic data and well logs in a 1500 square mile study area along the Eastern Shelf of the Midland Basin. These sequences compose two lower frequency sequences (W1-W5 & W6-W8) which are separated by a major erosional surface associated with a sea-level fall near the time of the early-middle Wolfcampian boundary. Sea-level falls associated with sequences W5 and W6 resulted in significant erosion of platform-margin deposits, incision of a submarine canyon several miles into the Eastern Shelf, and deposition of carbonate gravity flows in the Midland Basin. Gravity flows entered the basin via the submarine canyon and fed basin-floor fan systems which extend up to 25 miles basinward of the toe-of-slope. Within the study area, production from carbonate gravity-flow deposits is mostly from three submarine fan systems within sequences W5 and W6 - the Credo (10 MMBOER) fan (oldest) , the Triple M (5 MMBOER)-Howard Glasscock (7 MMBOER) fan, and the Hutto (5 MMBOER) fan (youngest). The maximum gross thickness of the fans ranges from 100 to 200 feet. Regional isolith and seismic amplitude data were used to high-grade a 70 square mile area in the vicinity of Triple M and Howard Glasscock fields. Model-based velocity inversions, constrained by sonic and density data from 52 wells, were performed utilizing a grid of 2-D seismic data and a 3-D survey. Both Triple M and Howard Glasscock fields are clearly defined by high-velocity anomalies within the productive basin-floor fan interval of sequence W6. An untested high-velocity anomaly with a velocity signature and stratal geometry similar to the two fields, and estimated reserves of 5 MMBOER, is scheduled to be drilled in 1995.

  11. Early-to-late-diagenetic dolomitization of platform carbonates: Lower Ordovician Ellenburger Group, Permian basin, west Texas and southeastern New Mexico

    SciTech Connect (OSTI)

    Amthor, J.E. ); Friedman, G.M. Northeastern Science Foundation, Troy, NY )

    1991-03-01

    Pervasive early- to late-diagenetic dolomitization of Lower Ordovician Ellenburger carbonates in the deep Permian basin is recorded in core samples having present-day burial depths of 1.5 to 7.0 km. Fine-crystalline planar replacement dolomite formed during early diagenesis in a subtidal to peritidal setting under near-surface, low-temperature conditions, with Mg{sup 2+} for dolomitization of precursor lime mud supplied by diffusion from overlying seawater. During intermediate burial (500-2,000 m), medium- to coarse-crystalline planar-s dolomite replaced allochems and matrix, or occurred as void-filling. Burial-history and thermal maturation calculations suggest that deep-burial dolomite cementation occurred during the Late Pennsylvanian/Early Permian. Inter- and intracrystalline dissolution surfaces are observed within the paragenetic sequence. Major truncation surfaces between early replacement dolomites and later void-filling dolomites, and between planar and nonplanar dolomite cements are evidence for dolomite dissolution. Deep-discharge of meteoric fluids as a result of frequent periods of karsting in overlying strata, and long-distance fluid migration during the Ouachita orogeny from foreland basins to the south are invoked for sources of undersaturated fluids causing dolomite dissolution and creating matrix-porosity in the deep subsurface. Similar diagenetic relationships have been described from other deeply buried carbonate rocks elsewhere, indicating that trends and timing of dolomitization, dissolution and porosity formation, and cementation by late dolomite and calcite are intimately related to the evolution of sedimentary basins. The origin of massive dolostones such as the Ellenburger is best explained in the context of basin evolution, rather than by a single model of dolomite formation.

  12. Advanced Reservoir Characterization and Development through High-Resolution 3C3D Seismic and Horizontal Drilling: Eva South Marrow Sand Unit, Texas County, Oklahoma

    SciTech Connect (OSTI)

    Wheeler,David M.; Miller, William A.; Wilson, Travis C.

    2002-03-11

    The Eva South Morrow Sand Unit is located in western Texas County, Oklahoma. The field produces from an upper Morrow sandstone, termed the Eva sandstone, deposited in a transgressive valley-fill sequence. The field is defined as a combination structural stratigraphic trap; the reservoir lies in a convex up -dip bend in the valley and is truncated on the west side by the Teepee Creek fault. Although the field has been a successful waterflood since 1993, reservoir heterogeneity and compartmentalization has impeded overall sweep efficiency. A 4.25 square mile high-resolution, three component three-dimensional (3C3D) seismic survey was acquired in order to improve reservoir characterization and pinpoint the optimal location of a new horizontal producing well, the ESU 13-H.

  13. Socioeconomic impact of infill drilling recovery from carbonate reservoirs in the Permian basin, west Texas. Master's thesis

    SciTech Connect (OSTI)

    Jagoe, B.K.

    1994-05-01

    This investigative study presents results on the socioeconomic impact of infill drilling recovery from carbonate reservoirs in the Permian Basin. The amount of incremental oil and gas production from infill drilling in 37 carbonate reservoir units is established using decline curve analysis. The increase in incremental recovery is used to compute the amount of increased revenue and taxes (local, state and federal). A job market analysis is performed to determine the impact of these increased revenues on primary jobs in the oil industry and secondary jobs in the community. Secondary jobs are generated by oil industry workers spending money in the community. The appropriation of the estimated taxes is analyzed to determine which government agencies benefit most from the infill drilling. The observations from this research are that most of the San Andres and Clearfork carbonate reservoir units in the Permian Basin are potentially profitable to infill drill. The incremental oil and gas production from infill drilling could maintain or create many primary jobs within the local oil industry and also secondary jobs in the community. The incremental production could generate taxes which would greatly benefit certain local, state, and federal government agencies.

  14. The Need to Reduce Mobile Source Emissions in the South Coast Air Basin

    Office of Energy Efficiency and Renewable Energy (EERE)

    2004 Diesel Engine Emissions Reduction (DEER) Conference Presentation: South Coast Air Quality Management District

  15. Reservoir characterization of a Permian Slope Fan/basin-floor fan complex: Cherry Canyon Formation, Ward County, Texas

    SciTech Connect (OSTI)

    Spain, D.R. )

    1990-05-01

    The Cherry Canyon Formation consists of a 925-ft- (280-m) thick section of up to 25 different sandstone and siltstone units that were deposited in a deep-water environment in the Delaware basin. Lowstand sedimentation by fluid density currents with periodic turbidity currents resulted in a broad-migrating channelized slope fan/basin-floor fan complex interpreted to exhibit an intricate reservoir geometry. Thirteen lithofacies are identified. Primary reservoirs are found in massive channel sandstones, and beds of lesser reservoir quality are present in laminated overbank/interchannel sandstones. Original depositional fabric modified by diagenetic cements and authigenic clays created three petrophysical rock types. Type I reservoirs contain intergranular macroporosity relatively free of carbonate cement and authigenic clay. Types II and III reservoirs contain mesoporosity and abundant microporosity created by moderate to abundant carbonate cementation and plugging of pore throats by authigenic grain-coating chlorite and pore-bridging fibrous illite. Depositional and diagenetic factors combine with insufficient oil column height to yield low initial oil saturations that decrease with depth in a hydrocarbon-water transition zone. Mercury injection capillary pressure measurements illustrate the vertical stratification of petrophysical rock types that exist in the section; reservoirs which contain all water are interbedded with reservoirs containing mostly oil. Subsequently, a slight change in height above free water can drive production from all water to all oil. Hydrocarbon column heights greater than 60 ft are required to establish water-free oil production. Accurate reservoir water saturations can be derived using Archie's equation; when combined with a movable oil analysis and drainage relative permeability/fractional flow curves, initial water cuts can be predicted to maximize deliverability.

  16. Geoscience/Engineering Characterization of the Interwell Environment in Carbonate Reservoirs Based on Outcrop Analogs, Permian Basin, West Texas and New Mexico.

    SciTech Connect (OSTI)

    Lucia, Jerry F.; Kerans, Charles

    1997-05-29

    The objective of this project is to investigate styles of reservoir heterogeneity found in low permeability pelleted wackestone/packstone facies and mixed carbonate/clastic facies found in Permian Basin reservoirs by studying similar facies exposed in the Guadalupe Mountains. Specific objectives for the outcrop study include construction of a stratigraphic framework, petrophysical quantification of the framework, and testing the outcrop reservoir model for effects of reservoir heterogeneity on production performance. Specific objectives for the subsurface study parallel objectives for the outcrop study. Subsurface Activities - We continue to prepare two final reports that summarize research results of the South Cowden Field study. One report summarizes results of the petrophysical characterization research, and one summarizes results of the fluid-flow modeling research. Outcrop Activities - We also continue to prepare the final report, which summarizes the research results of the Grayburg outcrop reservoir study.

  17. Geoscience/Engineering Characterization of the Interwell Environment in Carbonate Reservoirs Based on Outcrop Analogs, Permian Basin, West Texas and New Mexico.

    SciTech Connect (OSTI)

    Lucia, Jerry F.; Kerans, Charles

    1997-05-19

    The objective of this project is to investigate styles of reservoir heterogeneity found in low permeability pelleted wackestone/packstone facies and mixed carbonate/clastic facies found in Permian Basin reservoirs by studying similar facies exposed in the Guadalupe Mountains. Specific objectives for the outcrop study include construction of a stratigraphic framework, petrophysical quantification of the framework, and testing the outcrop reservoir model for effects of reservoir heterogeneity on production performance. Specific objectives for the subsurface study parallel objectives for the outcrop study. Subsurface Activities - We continue to prepare two final reports that summarize research results of the South Cowden Field study. One report summarizes results of the petrophysical characterization research, and one summarizes results of the fluid-flow modeling research. Outcrop Activities - We also continue to prepare the final report, which summarizes the research results of the Grayburg outcrop reservoir study.

  18. Geohydrology of the Keechi, Mount Sylvan, Oakwood, and Palestine salt domes in the northeast Texas salt-dome basin

    SciTech Connect (OSTI)

    Carr, J.E.; Halasz, S.J.; Peters, H.B.

    1980-01-01

    The salt within these domes has penetrated as much as 20,000 feet of Mesozoic and Cenozoic strata, and presently extends to within 120 to 800 feet of the land surface. The salt penetrates or closely underlies major freshwater and salinewater aquifers within the basin. To provide a safe repository for radioactive wastes within one or more of these domes, a thorough understanding of the geohydrology needs to be obtained, and the hydrologic stability of the domes needs to be established for the expected life of the storage facility. Dissolution may exist at all four candidate salt domes, possibly through contact with Cretaceous or Tertiary aquifers, or through fault systems in the vicinity of the domes. Strata overlying and surrounding Palestine and Keechi Salt Domes have been arched into steeply-dipping folds that are complexly faulted. Similar conditions exist at Oakwood and Mount Sylvan Domes, except that the Tertiary strata have been only moderately disturbed. Additional problems concerning the hydrologic stability of Oakwood and Palestine Salt Domes have resulted from the disposal of oil-field salinewater in the cap rock at the Oakwood Dome and previous solution mining of salt at the Palestine Dome.

  19. sRecovery Act: Geologic Characterization of the South Georgia Rift Basin for Source Proximal CO2 Storage

    SciTech Connect (OSTI)

    Waddell, Michael

    2014-09-30

    This study focuses on evaluating the feasibility and suitability of using the Jurassic/Triassic (J/TR) sediments of the South Georgia Rift basin (SGR) for CO2 storage in southern South Carolina and southern Georgia The SGR basin in South Carolina (SC), prior to this project, was one of the least understood rift basin along the east coast of the U.S. In the SC part of the basin there was only one well (Norris Lightsey #1) the penetrated into J/TR. Because of the scarcity of data, a scaled approach used to evaluate the feasibility of storing CO2 in the SGR basin. In the SGR basin, 240 km (~149 mi) of 2-D seismic and 2.6 km2 3-D (1 mi2) seismic data was collected, process, and interpreted in SC. In southern Georgia 81.3 km (~50.5 mi) consisting of two 2-D seismic lines were acquired, process, and interpreted. Seismic analysis revealed that the SGR basin in SC has had a very complex structural history resulting the J/TR section being highly faulted. The seismic data is southern Georgia suggest SGR basin has not gone through a complex structural history as the study area in SC. The project drilled one characterization borehole (Rizer # 1) in SC. The Rizer #1 was drilled but due to geologic problems, the project team was only able to drill to 1890 meters (6200 feet) instead of the proposed final depth 2744 meters (9002 feet). The drilling goals outlined in the original scope of work were not met. The project was only able to obtain 18 meters (59 feet) of conventional core and 106 rotary sidewall cores. All the conventional core and sidewall cores were in sandstone. We were unable to core any potential igneous caprock. Petrographic analysis of the conventional core and sidewall cores determined that the average porosity of the sedimentary material was 3.4% and the average permeability was 0.065 millidarcy. Compaction and diagenetic studies of the samples determined there would not be any porosity or permeability at depth in SC. In Georgia there appears to be porosity in

  20. Bowie County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas De Kalb, Texas Hooks, Texas Leary, Texas Maud, Texas Nash, Texas New Boston, Texas Red Lick, Texas Redwater, Texas Texarkana, Texas Wake Village, Texas Retrieved from "http:...

  1. Navarro County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Navarro County, Texas Angus, Texas Barry, Texas Blooming Grove, Texas Corsicana, Texas Dawson, Texas Emhouse, Texas Eureka, Texas Frost, Texas Goodlow, Texas Kerens, Texas Mildred,...

  2. McLennan County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Lorena, Texas Mart, Texas McGregor, Texas Moody, Texas Riesel, Texas Robinson, Texas Ross, Texas Valley Mills, Texas Waco, Texas West, Texas Woodway, Texas Retrieved from...

  3. Disequilibrium study of natural radionuclides of uranium and thorium series in cores and briny groundwaters from Palo Duro Basin, Texas

    SciTech Connect (OSTI)

    Laul, J.C.; Smith, M.R.

    1988-05-01

    The concentrations of natural radionuclides of the /sup 238/U and /232/Th series are reported in several cores and in ten deep and five shallow briny groundwaters from various formations in the Palo Duro Basin. The formations include Granite Wash, Pennsylvanian Granite Wash, Wolfcamp Carbonate, Pennsylvanian Carbonate, Seven River, Queen Grayburg, San Andres, Yates and Salado. The natural radionuclide data in cores suggest that the radionuclides have not migrated or been leached for at least a period of about 1 million years. Relative to the U and Th concentrations in cores, the brines are depleted by a factor of 10/sup 4/ to 10/sup 5/, indicating extremely low solubility of U and Th in brines. The natural radionuclide data in brines suggest that radium is not sorbed significantly and thus not retarded in nine deep brines. Radium is somewhat sorbed in one deep brine of Wolfcamp Carbonate and significantly sorbed in shallow brines. Relative to radium, the U, Th, Pb, Bi, and Po radionuclides are highly retarded by sorption. The retardation factors for /sup 228/Th range from 10/sup 2/ to 10/sup 3/, whereas those for /sup 230/Th and /sup 234/U range from 10/sup 3/ to 10/sup 5/, depending on the formation. The /sup 234/U//sup 238/U ratios in these brines are constant at about 1.5. The magnitude of the /sup 234/U//sup 230/Th ratio appears to reflect the degree of redox state of the aquifer's environment. The /sup 234/U//sup 230/Th ratio in nine deep brines is about unity, suggesting that U, like Th/sup +4/, is in the +4 state, which in turn suggests a reduced environment. 49 refs., 23 figs., 18 tabs.

  4. Pyrolysis and hydrocarbon source bed potential of the Upper Devonian Woodford Shale, Hovey Channel, southern Permian basin, west Texas

    SciTech Connect (OSTI)

    Hussain, M.; Bloom, M.A. )

    1991-03-01

    The Upper Devonian Woodford Shale in the Hovey Channel area, southern Permian basin, is 50 m thick and composed largely of brown to black, pyritic, spore-bearing, organic-rich, fissile shale an chert. Total organic carbon, distillable hydrocarbons, genetic potential, organic carbon index, hydrogen index, temperature of maximum hydrocarbon generation, and kerogen transformation index of the Woodford Shale suggest a matured to overmatured, gas-generating source bed. The total organic carbon content of the formation ranged from a low of 0.77% in the cherty samples to a high of 4.59% in a shaley sample, averaging 2.18%. Distillable hydrocarbon content of the samples is fairly high (averaging 1.72 mg HC/gm{degree} rock), varying from 0.90 mg HC/gm{degree} rock to 3.22 mg HC/gm{degree} rock. Genetic potential evaluated in terms of both residual and total generative potential showed above average potential, averaging 3.25 mg HC/gm{degree} rock for the residual and 4.90 mg HC/gm{degree} rock for the total, respectively. Live organic carbon index values ranged from 11-28%, characterizing the formation as a moderate to good source bed. Hydrogen index values ranged from 73 mg HC/gm{degree} C org to 155 mg HC/gm{degree} C org, suggesting overmaturity and gas-generation potential of the source bed. Temperature of maximum hydrocarbon generation values and kerogen transformation ratio values (averaging 0.34) also indicate overmatured nature of the Woodford Shale.

  5. An integrated study of the Grayburg/San Andres reservoir, Foster and South Cowden fields, Ector County, Texas, Class II

    SciTech Connect (OSTI)

    Trentham, DGS, Robert C.; Robinson, M.S., William C.; Wider, Kevin; Weinbrandt, Ph.D.,PE, Richard

    2000-04-14

    A project to recover economic amounts of oil from a very mature oil field is being conducted by Laguna Petroleum Corporation of Midland, Texas, with partial funding from a U. S. Department of Energy (DOE) grant to study shallow carbonate rock reservoirs. The objectives of the project are to use modern engineering methods to optimize oil field management and to use geological and geophysical data to recover untapped potential within the petroleum reservoirs. The integration of data and techniques from these disciplines has yielded results greater than those achievable without their cooperation. The cost of successfully accomplishing these goals is to be low enough for even small independent operators to afford. This article is a report describing accomplishments for the fiscal year 1998-1999.

  6. Late Paleozoic structural evolution of Permian basin

    SciTech Connect (OSTI)

    Ewing, T.E.

    1984-04-01

    The southern Permian basin is underlain by the NNW-trending Central Basin disturbed belt of Wolfcamp age (Lower Permian), the deep Delaware basin to its west, and the shallower Midland basin to its eat. The disturbed belt is highly segmented with zones of left-lateral offset. Major segments from south to north are: the Puckett-Grey Ranch zone; the Fort Stockton uplift; the Monahans transverse zone; the Andector ridges and the Eunice ridge; the Hobbs transverse zone; and the Tatum ridges, which abut the broad Roosevelt uplift to the north. The disturbed belt may have originated along rift zones of either Precambrian or Cambrian age. The extent of Lower and Middle Pennsylvanian deformation is unclear; much of the Val Verde basin-Ozona arch structure may have formed then. The main Wolfcamp deformation over thrust the West Texas crustal block against the Delaware block, with local denudation of the uplifted edge and eastward-directed backthrusting into the Midland basin. Latter in the Permian, the area was the center of a subcontinental bowl of subsidence - the Permian basin proper. The disturbed belt formed a pedestal for the carbonate accumulations which created the Central Basin platform. The major pre-Permian reservoirs of the Permian basin lie in large structural and unconformity-bounded traps on uplift ridges and domes. Further work on the regional structural style may help to predict fracture trends, to assess the timing of oil migration, and to evaluate intrareservoir variations in the overlying Permian giant oil fields.

  7. Brazoria County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas Hillcrest, Texas Holiday Lakes, Texas Iowa Colony, Texas Jones Creek, Texas Lake Jackson, Texas Liverpool, Texas Manvel, Texas Oyster Creek, Texas Pearland, Texas Quintana,...

  8. Henderson County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Eustace, Texas Gun Barrel City, Texas Log Cabin, Texas Mabank, Texas Malakoff, Texas Moore Station, Texas Murchison, Texas Payne Springs, Texas Poynor, Texas Seven Points, Texas...

  9. Fannin County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    in Fannin County, Texas Bailey, Texas Bonham, Texas Dodd City, Texas Ector, Texas Honey Grove, Texas Ladonia, Texas Leonard, Texas Pecan Gap, Texas Ravenna, Texas Savoy,...

  10. Galveston County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas Clear Lake Shores, Texas Dickinson, Texas Friendswood, Texas Galveston, Texas Hitchcock, Texas Jamaica Beach, Texas Kemah, Texas La Marque, Texas League City, Texas San...

  11. Early Pennsylvanian wrenching along the Red River-Matador Arch: Formation of a pull-apart basin, Depocenter for Atokan to Lower Des Moines (bend) clastics, Cottle County, Texas

    SciTech Connect (OSTI)

    Stephens, W.C. Jr.; Gunn, R.D.

    1995-06-01

    Early Pennsylvanian wrenching along the Red River-Matador Arch (Tectonic Zone) created a braided series of en echelon faults and folds with associated pop-up structures and pull-apart basins. Local extension, or overstepping, in Southeast Cottle County, Texas, has produced the deepest pull-apart basin along the arch with over 10,000` of structural relief. The emerging Wichita-Amarillo Uplift, to the north, provided an abundant sediment source, which prograded rapidly southward as an alluvial fan-braided river complex. Exposure of basement rocks and lower Paleozoic sediments along the Red River-Matador Arch, also contributed to the basin fill. Syntectonic sedimentation led to the accumulation of over 6000` of Bend (Atoka-lower Des Moines) sediments within the basin. Deposition was dominated initially by alluvial fan to fluvial siliciclastics. As basin subsidence was further amplified by sediment loading, accommodation exceeded sedimentation capturing a large segment of the southward prograding Wichita-Amarillo derived clastic wedge. Encroachment of the late Atoka to lower Des Moines epeiric sea promoted further evolution of depositional environments to fan deltas, marine dominated clastics and, later, localized carbonate development. Type III kerogen rich organic shales produced abundant gas prone source rocks. The extreme depth of the basin combined with the local geothermal gradient provided for significant hydrocarbon generation. By early 1988 new well control helped revise previous stratigraphic correlation demonstrating a rapidly expanding lower Des Moines to Atokan section. The drilling of the Gunn Oil Company-Brothers No. 1 to a total depth of 10,301` in the Mississippian Chappel Limestone, encountered 2025` of Bend sediments, with 279` of gross Bend Conglomerate (162` of net pay). The Brothers No. 1 was potentialled on 11/19/89 with a CAOF of 6.0 MMCFD and filed as the field discovery for the Broken Bone (Bend Conglomerate) field.

  12. Open system diagenesis and the los of provenance signatures: isotopic and elemental data from sandstones, Frio Formation, south Texas

    SciTech Connect (OSTI)

    Land, L.S.; Mack, L.E.; Milliken, K.L. ); MacPherson, G.L. )

    1990-05-01

    Oligocene Frio sandstones in which detrital feldspars are completely altered typically contain authigenic minerals that exceed 30% of the rock volume. Elemental and isotopic analyses of whole rocks show that authigenesis is accompanied by both gain and loss of material. Subsurface sandstones for elemental and isotopic analysis were sampled from approximately 3,000-14,000 ft (0.9-4.3 km). Over this depth range, dissolution and minor albitization of detrital K-feldspar is accompanied by loss of 2 to 3 wt.% of K{sub 2}O from the whole rock. Loss of about 50% of the initial strontium also correlates with alteration of detrital feldspars. {sup 87}Sr/{sup 86}Sr for whole-rock and silicate fractions change with depth as strontium characteristic of the detrital fraction is replaced by more radiogenic strontium derived from deeper in the basin. Aluminum, titanium, phosphorous, manganese, and barium also exhibit trends compatible with net export, but uncertainties about initial variation remain. Trends for silicon, sodium, iron, boron, and lithium are equivocal. Magnesium gain accompanies precipitation of authigenic chlorite. Whole-rock calcium values are dominated by calcite that includes both detrital and authigenic components. Significant dissolution of the detrital carbonate component does not occur, and calcium in authigenic carbonate exceeds by about five times the calcium released during destruction of detrital silicates, thus requiring considerable calcium and CO{sub 2} import. Material transfer on the scale observed suggests that simple burial diagenesis is not a closed-system process for several major elements and introduces a major obstacle to the use of elemental data for provenance interpretation.

  13. An integrated study of the Grayburg/San Andres Reservoir, Foster and South Cowden Fields, Ector County, Texas. Annual report, August 1, 1996--July 31, 1997

    SciTech Connect (OSTI)

    Trentham, R.C.; Weinbrandt, R.; Robinson, W.

    1997-12-01

    The objective of this two-phase study is to demonstrate an integrated methodology for reservoir characterization of shallow shelf carbonate reservoir that is feasible, and cost effective for the independent operator. Furthermore, it will provide one of the first public demonstrations of the enhancement of reservoir characterization using high-resolution three dimensional (3D) seismic data. This particular project is evaluating the Grayburg and San Andres reservoirs in the Foster and South Cowden Fields, Ector County, Texas. This 68 year old field was approaching its economic limit and the leases evaluated would have been abandoned in 10 years. A multidisciplinary approach to waterflood design and implementation, along with the addition of reserves by selective infill drilling and deepening, is being applied to this field. This approach in reservoir development will be applicable to a wide range of shallow shelf carbonate reservoirs throughout the US. The first phase of the project included the design, acquisition, and interpretation of the 3D seismic survey, the collection and evaluation of geologic (core and log) data, and engineering (historical production, well test, injection) data from a variety of sources. From this work, a geologically based production history model was simulated. Based on the recommendations made at the end of Phase One, three new wells were drilled, one existing well was deepened, two wells were worked over, one TA`d well was re-entered, and one well was converted to injection. In addition, the quality of the injection water was greatly improved, a step necessary prior to increasing injection in the project area. The realignment of the waterflood and all additional well work await the completion of the seismic based history match and engineering simulation.

  14. Characterization of oil and gas reservoirs and recovery technology deployment on Texas State Lands

    SciTech Connect (OSTI)

    Tyler, R.; Major, R.P.; Holtz, M.H.

    1997-08-01

    Texas State Lands oil and gas resources are estimated at 1.6 BSTB of remaining mobile oil, 2.1 BSTB, or residual oil, and nearly 10 Tcf of remaining gas. An integrated, detailed geologic and engineering characterization of Texas State Lands has created quantitative descriptions of the oil and gas reservoirs, resulting in delineation of untapped, bypassed compartments and zones of remaining oil and gas. On Texas State Lands, the knowledge gained from such interpretative, quantitative reservoir descriptions has been the basis for designing optimized recovery strategies, including well deepening, recompletions, workovers, targeted infill drilling, injection profile modification, and waterflood optimization. The State of Texas Advanced Resource Recovery program is currently evaluating oil and gas fields along the Gulf Coast (South Copano Bay and Umbrella Point fields) and in the Permian Basin (Keystone East, Ozona, Geraldine Ford and Ford West fields). The program is grounded in advanced reservoir characterization techniques that define the residence of unrecovered oil and gas remaining in select State Land reservoirs. Integral to the program is collaboration with operators in order to deploy advanced reservoir exploitation and management plans. These plans are made on the basis of a thorough understanding of internal reservoir architecture and its controls on remaining oil and gas distribution. Continued accurate, detailed Texas State Lands reservoir description and characterization will ensure deployment of the most current and economically viable recovery technologies and strategies available.

  15. Lithospheric flexure and composite tectonic loads in the foreland of the Marathon orogenic belt: Permian Basin, west Texas and southern New Mexico

    SciTech Connect (OSTI)

    Yang, Kenn Ming; Dorobek, S. . Dept. of Geology)

    1992-01-01

    Lithospheric flexure caused by loading of orogenic belts is regarded as the main process that produces subsidence in foreland basins. However in some foreland areas, subsidence may be affected by synorogenic foreland uplifts that act as additional loads. The Permian Basin is located in the foreland area of the late Paleozoic Marathon orogenic belt (Mob). The Permian Basin consists of several sub-basins that are separated by several structurally complex uplifts. Uplift of the Central Basin Platform (CBP) and subsidence in adjacent basins were coeval with final stages of deformation in the Marathon orogen. The CBP is oriented at high angles to the Marathon orogen and consists of several blocks arranged in an en echelon pattern. Data suggest that uplift of the CBP was affected by clockwise rotation of crustal blocks between NNW-SSE trending boundary faults. Although both the Delaware Basin (DB) and Val Verde Basin (VVB) are adjacent to the Mob, the synorogenic geometries of these basins are different. The VVB has a typical flexural profile that apparently is due to loading of the Marathon orogen. However, the flexural profile becomes narrower and deeper toward the western end of the VVB where the basin is bordered by the southernmost block of the CBP. In contrast, synorogenic DB profiles have composite wavelengths which show maximum deflection next to the Mob and toward the uplifted blocks of the CBP. This suggests that synorogenic subsidence of the DB was affected by loading of the CBP. In addition, the loading geometry across the uplifted CBP is asymmetric, with greater uplift and basement shortening on the western side of the CBP and less uplift and basement shortening on the eastern side. This may explain greater synorogenic subsidence in the DB than the Midland Basin.

  16. Ellis County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas Milford, Texas Oak Leaf, Texas Ovilla, Texas Palmer, Texas Pecan Hill, Texas Red Oak, Texas Venus, Texas Waxahachie, Texas Retrieved from "http:en.openei.orgw...

  17. Starr County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Los Alvarez, Texas Los Villareales, Texas North Escobares, Texas Rio Grande City, Texas Roma Creek, Texas Roma, Texas Salineno, Texas San Isidro, Texas Santa Cruz, Texas Retrieved...

  18. Guadalupe County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Places in Guadalupe County, Texas Cibolo, Texas Geronimo, Texas Kingsbury, Texas Marion, Texas McQueeney, Texas New Berlin, Texas New Braunfels, Texas Redwood, Texas San...

  19. Cass County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Subtype A. Places in Cass County, Texas Atlanta, Texas Avinger, Texas Bloomburg, Texas Domino, Texas Douglassville, Texas Hughes Springs, Texas Linden, Texas Marietta, Texas Queen...

  20. Tarrant County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Benbrook, Texas Blue Mound, Texas Briar, Texas Burleson, Texas Colleyville, Texas Crowley, Texas Dalworthington Gardens, Texas Edgecliff Village, Texas Euless, Texas Everman,...

  1. Orange County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    City, Texas Mauriceville, Texas Orange, Texas Pine Forest, Texas Pinehurst, Texas Port Arthur, Texas Rose City, Texas Vidor, Texas West Orange, Texas Retrieved from "http:...

  2. Jefferson County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas Central Gardens, Texas China, Texas Groves, Texas Nederland, Texas Nome, Texas Port Arthur, Texas Port Neches, Texas Taylor Landing, Texas Retrieved from "http:...

  3. Bexar County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas Converse, Texas Cross Mountain, Texas Elmendorf, Texas Fair Oaks Ranch, Texas Grey Forest, Texas Helotes, Texas Hill Country Village, Texas Hollywood Park, Texas Kirby,...

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

    SciTech Connect (OSTI)

    Blount, G.; Millings, M.

    2011-08-01

    A reconnaissance assessment of the carbon dioxide (CO{sub 2}) sequestration potential within the Triassic age rift trend sediments of South Carolina, Georgia and the northern Florida Rift trend was performed for the Office of Fossil Energy, National Energy Technology Laboratory (NETL). This rift trend also extends into eastern Alabama, and has been termed the South Georgia Rift by previous authors, but is termed the South Carolina, Georgia, northern Florida, and eastern Alabama Rift (SGFAR) trend in this report to better describe the extent of the trend. The objectives of the study were to: (1) integrate all pertinent geologic information (literature reviews, drilling logs, seismic data, etc.) to create an understanding of the structural aspects of the basin trend (basin trend location and configuration, and the thickness of the sedimentary rock fill), (2) estimate the rough CO{sub 2} storage capacity (using conservative inputs), and (3) assess the general viability of the basins as sites of large-scale CO{sub 2} sequestration (determine if additional studies are appropriate). The CO{sub 2} estimates for the trend include South Carolina, Georgia, and northern Florida only. The study determined that the basins within the SGFAR trend have sufficient sedimentary fill to have a large potential storage capacity for CO{sub 2}. The deeper basins appear to have sedimentary fill of over 15,000 feet. Much of this fill is likely to be alluvial and fluvial sedimentary rock with higher porosity and permeability. This report estimates an order of magnitude potential capacity of approximately 137 billion metric tons for supercritical CO{sub 2}. The pore space within the basins represent hundreds of years of potential storage for supercritical CO{sub 2} and CO{sub 2} stored in aqueous form. There are many sources of CO{sub 2} within the region that could use the trend for geologic storage. Thirty one coal fired power plants are located within 100 miles of the deepest portions of

  5. EIS-0520: Texas LNG Project; Cameron County, Texas | Department...

    Office of Environmental Management (EM)

    20: Texas LNG Project; Cameron County, Texas EIS-0520: Texas LNG Project; Cameron County, Texas Summary The Federal Energy Regulatory Commission (FERC) announced its intent to ...

  6. Integrated geological and engineering characterization of an Upper Permian, carbonate reservoir, South Cowden unit, Ector County Texas -- a work in progress

    SciTech Connect (OSTI)

    Gerard, M.G.; Johnson, J.V.; Snow, S.C.

    1995-09-01

    South Cowden Unit, located on the eastern margin of the Central Basin Platform, has produced 35 million barrels of oil since initial development in the late 1940`s. The Unit, under waterflood since 1965, has been proposed for a CO{sub 2} flood using horizontal injection wells. A team of geologists and engineers was formed to characterize the reservoir. The early and complete integration of geologic and engineering work has resulted in a detailed reservoir description to be used in reservoir simulation. Regional mapping and 3D seismic data indicate that sediments within the reservoir interval were draped over a paleohigh resulting in an unfaulted, anticlinal-like structure. A field-wide stratigraphic framework was developed using two to four-foot thick, gamma-ray log markers which correspond to low permeability, sandy dolomite layers recognized in core. These log correlations indicate fairly simple and uniform structure and stratigraphy. The gamma-ray markers delineate four zones within the 150 foot reservoir interval. Rocks composing these zones are extensively dolomitized and display a complex color mottling. This mottling is related most likely to bioturbation of carbonate sediments in a shallow, subtidal marine environment. Extensive and interconnected bioturbated areas have core analysis porosities averaging approximately 20% and permeabilities generally ranging from 2 to 350 md. The intervening, nonburrowed and unstained areas have porosities averaging 5% and permeabilities typically ranging form 0.01 to 2 md. Variations in the quality and thickness of the mottled facies are major parameters controlling oil recovery. A belt of better reservoir-quality rock runs roughly parallel to structure and results in an area of higher cumulative oil production. Good waterflood response and uniform pressure distribution indicate continuity of the pay zones within this belt.

  7. Geoscience/Engineering Characterization of the Interwell Environment in Carbonate Reservoirs Based on Outcrop Analogs, Permian Basin, West Texas and New Mexico.

    SciTech Connect (OSTI)

    Lucia, F.J.; Kerans, C.

    1997-05-29

    The objective of this project is to investigate styles of reservoir heterogeneity found in low permeability pelleted wackestone/packstone facies and mixed carbonate/clastic facies found in Permian Basin reservoirs by studying similar facies found in Permian Basin reservoirs by studying similar facies exposed in the Guadalupe Mountains. Specific objectives for the outcrop study include construction of a stratigraphic framework, petrophysical quantification of the framework, and testing the outcrop reservoir model for effects of reservoir heterogeneity on production performance. Specific objectives for the subsurface study parallel objectives for the outcrop study.

  8. Austin County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    in Austin County, Texas Ag Fuels Ltd Places in Austin County, Texas Bellville, Texas Brazos Country, Texas Industry, Texas San Felipe, Texas Sealy, Texas Wallis, Texas Retrieved...

  9. Caldwell County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Places in Caldwell County, Texas Lockhart, Texas Luling, Texas Martindale, Texas Mustang Ridge, Texas Niederwald, Texas San Marcos, Texas Uhland, Texas Retrieved from "http:...

  10. Comal County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas Canyon Lake, Texas Fair Oaks Ranch, Texas Garden Ridge, Texas New Braunfels, Texas San Antonio, Texas Schertz, Texas Selma, Texas Retrieved from "http:en.openei.orgw...

  11. Travis County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    in Travis County, Texas Texas General Land Office Places in Travis County, Texas Anderson Mill, Texas Austin, Texas Barton Creek, Texas Bee Cave, Texas Briarcliff, Texas Cedar...

  12. Williamson County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Williamson County, Texas Texas General Land Office Places in Williamson County, Texas Anderson Mill, Texas Austin, Texas Bartlett, Texas Brushy Creek, Texas Cedar Park, Texas...

  13. Bee County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Number 2 Climate Zone Subtype A. Places in Bee County, Texas Beeville, Texas Blue Berry Hill, Texas Normanna, Texas Pawnee, Texas Pettus, Texas Skidmore, Texas Tuleta, Texas...

  14. Petrographic report on clay-rich samples from Permian Unit 4 salt, G. Friemel No. 1 well, Palo Duro Basin, Deaf Smith County, Texas: unanalyzed data

    SciTech Connect (OSTI)

    Fukui, L M

    1983-09-01

    This report presents the results of mineralogic and petrographic analyses performed on five samples of clay-rich rock from salt-bearing Permian strata sampled by drill core from G. Friemel No. 1 Well, Deaf Smith County, Texas. Five samples of clay-rich rock from depths of about 2457, 2458, 2521, 2548, and 2568 feet were analyzed to determine the amounts of soluble phase (halite) and the amounts and mineralogy of the insoluble phases. The amounts of halite found were 59, 79, 47, 40, and 4 weight percent, respectively, for the samples. The insoluble minerals are predominately clay (20 to 60 volume percent) and anhydrite (up to 17 volume percent), with minor (about 1.0%) and trace amounts of quartz, dolomite, muscovite, and gypsum. The clays include illite, chlorite, and interstratified chlorite-smectite. The results presented in this petrographic report are descriptive, uninterpreted data. 2 references, 7 tables.

  15. Top-down estimate of methane emissions in California using a mesoscale inverse modeling technique: The South Coast Air Basin

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

    Cui, Yu Yan; Brioude, Jerome; McKeen, Stuart A.; Angevine, Wayne M.; Kim, Si -Wan; Frost, Gregory J.; Ahmadov, Ravan; Peischl, Jeff; Bousserez, Nicolas; Liu, Zhen; et al

    2015-07-28

    Methane (CH4) is the primary component of natural gas and has a larger global warming potential than CO2. Some recent top-down studies based on observations showed CH4 emissions in California's South Coast Air Basin (SoCAB) were greater than those expected from population-apportioned bottom-up state inventories. In this study, we quantify CH4 emissions with an advanced mesoscale inverse modeling system at a resolution of 8 km × 8 km, using aircraft measurements in the SoCAB during the 2010 Nexus of Air Quality and Climate Change campaign to constrain the inversion. To simulate atmospheric transport, we use the FLEXible PARTicle-Weather Research andmore » Forecasting (FLEXPART-WRF) Lagrangian particle dispersion model driven by three configurations of the Weather Research and Forecasting (WRF) mesoscale model. We determine surface fluxes of CH4 using a Bayesian least squares method in a four-dimensional inversion. Simulated CH4 concentrations with the posterior emission inventory achieve much better correlations with the measurements (R2 = 0.7) than using the prior inventory (U.S. Environmental Protection Agency's National Emission Inventory 2005, R2 = 0.5). The emission estimates for CH4 in the posterior, 46.3 ± 9.2 Mg CH4/h, are consistent with published observation-based estimates. Changes in the spatial distribution of CH4 emissions in the SoCAB between the prior and posterior inventories are discussed. Missing or underestimated emissions from dairies, the oil/gas system, and landfills in the SoCAB seem to explain the differences between the prior and posterior inventories. Furthermore, we estimate that dairies contributed 5.9 ± 1.7 Mg CH4/h and the two sectors of oil and gas industries (production and downstream) and landfills together contributed 39.6 ± 8.1 Mg CH4/h in the SoCAB.« less

  16. Case studies of the legal and institutional obstacles and incentives to the development of small-scale hydroelectric power: South Columbia Basin Irrigation District, Pasco, Washington

    SciTech Connect (OSTI)

    Schwartz, L.

    1980-05-01

    The case study concerns two modern human uses of the Columbia River - irrigation aimed at agricultural land reclamation and hydroelectric power. The Grand Coulee Dam has become synonomous with large-scale generation of hydroelectric power providing the Pacific Northwest with some of the least-expensive electricity in the United States. The Columbia Basin Project has created a half-million acres of farmland in Washington out of a spectacular and vast desert. The South Columbia River Basin Irrigation District is seeking to harness the energy present in the water which already runs through its canals, drains, and wasteways. The South District's development strategy is aimed toward reducing the costs its farmers pay for irrigation and raising the capital required to serve the remaining 550,000 acres originally planned as part of the Columbia Basin Project. The economic, institutional, and regulatory problems of harnessing the energy at site PEC 22.7, one of six sites proposed for development, are examined in this case study.

  17. Tectonic and eustatic controls on the carbonate stratigraphy of the Leonardian-Guadalupin (Permian) section, northwestern Delaware basin, New Mexico and Texas

    SciTech Connect (OSTI)

    Glaser, K.S.; Vail, P.R. ); Jordan, J.E. )

    1990-05-01

    The effects of tectonics and eustasy on carbonate sedimentation have been determined using seismic, well logs, and outcrop data for the middle Permian of the Delaware basin. Sequence and chronostratigraphic analyses indicate the section contains a broad, tectonically controlled aggradational/progradational cycle overprinted by eustatic sea level cycles. Early Leonardian deposition of the Abo Formation and the third Bone Spring sand occurred during a period of rapid subsidence, producing the aggradational geometry observed on seismic and well logs. This followed a time of uplift to the northwest of the study area, which caused enhanced shelf erosion during the late Wolfcampian. The aggradational style of deposition continued through the middle Leonardian. Late Leonardian time is characterized by progradational geometry, due to a slower subsidence rate. This resulted in a 15-km progradation of the Bone Spring shelf margin in the northwestern part of the Delaware basin. A second period of uplift to the northwest followed, leading to the deposition of the sands of the Brushy Canyon Formation (Guadalupian). This aggradational/progradational cycle is followed by a similar cycle which ends after the deposition of the Capitan Formation. Within the carbonate-dominated Leonardian aggradational/progradational cycle, nine sea level cycles are recognized. The lowstand systems tracts within this package are of two types. The lowstands within the aggradational part of the section consist primarily of slope fans, while those associated with progradation contain large lowstand prograding wedges. Steep margins are associated with aggradation, while progradation is characterized by a ramplike geometry. Highstands are widespread on the shelf and prograde into the basin throughout this interval.

  18. Geoscience/Engineering Characterization of the Interwell Environment in Carbonate Reservoirs Based on Outcrop Analogs, Permian Basin, West Texas and New Mexico.

    SciTech Connect (OSTI)

    Lucia, F.J.; Kerans, C.

    1996-12-31

    The objective of this project is to investigate styles of reservoir heterogeneity found in low permeability pelleted wackestone/packstone facies and mixed carbonate/clastic facies found in Permian Basin reservoirs by studying similar facies exposed in the Guadalupe Mountains. Specific objectives for the outcrop study include construction of a stratigraphic framework, petrophysical quantification of the framework, and testing the outcrop reservoir model for effects of reservoir heterogeneity on production performance. Specific objectives for the subsurface study parallel objectives for the outcrop study.

  19. Top-down estimate of methane emissions in California using a mesoscale inverse modeling technique: The South Coast Air Basin

    SciTech Connect (OSTI)

    Cui, Yu Yan; Brioude, Jerome; McKeen, Stuart A.; Angevine, Wayne M.; Kim, Si -Wan; Frost, Gregory J.; Ahmadov, Ravan; Peischl, Jeff; Bousserez, Nicolas; Liu, Zhen; Ryerson, Thomas B.; Wofsy, Steve C.; Santoni, Gregory W.; Kort, Eric A.; Fischer, Marc L.; Trainer, Michael

    2015-07-28

    Methane (CH4) is the primary component of natural gas and has a larger global warming potential than CO2. Some recent top-down studies based on observations showed CH4 emissions in California's South Coast Air Basin (SoCAB) were greater than those expected from population-apportioned bottom-up state inventories. In this study, we quantify CH4 emissions with an advanced mesoscale inverse modeling system at a resolution of 8 km × 8 km, using aircraft measurements in the SoCAB during the 2010 Nexus of Air Quality and Climate Change campaign to constrain the inversion. To simulate atmospheric transport, we use the FLEXible PARTicle-Weather Research and Forecasting (FLEXPART-WRF) Lagrangian particle dispersion model driven by three configurations of the Weather Research and Forecasting (WRF) mesoscale model. We determine surface fluxes of CH4 using a Bayesian least squares method in a four-dimensional inversion. Simulated CH4 concentrations with the posterior emission inventory achieve much better correlations with the measurements (R2 = 0.7) than using the prior inventory (U.S. Environmental Protection Agency's National Emission Inventory 2005, R2 = 0.5). The emission estimates for CH4 in the posterior, 46.3 ± 9.2 Mg CH4/h, are consistent with published observation-based estimates. Changes in the spatial distribution of CH4 emissions in the SoCAB between the prior and posterior inventories are discussed. Missing or underestimated emissions from dairies, the oil/gas system, and landfills in the SoCAB seem to explain the differences between the prior and posterior inventories. Furthermore, we estimate that dairies contributed 5.9 ± 1.7 Mg CH4/h and the two sectors of oil and gas industries (production and downstream) and landfills together contributed 39.6 ± 8.1 Mg CH4/h in the SoCAB.

  20. Top-down estimate of methane emissions in California using a mesoscale inverse modeling technique: The South Coast Air Basin

    SciTech Connect (OSTI)

    Cui, Yu Yan; Brioude, Jerome; McKeen, Stuart A.; Angevine, Wayne M.; Kim, Si -Wan; Frost, Gregory J.; Ahmadov, Ravan; Peischl, Jeff; Bousserez, Nicolas; Liu, Zhen; Ryerson, Thomas B.; Wofsy, Steve C.; Santoni, Gregory W.; Kort, Eric A.; Fischer, Marc L.; Trainer, Michael

    2015-07-28

    Methane (CH4) is the primary component of natural gas and has a larger global warming potential than CO2. Some recent top-down studies based on observations showed CH4 emissions in California's South Coast Air Basin (SoCAB) were greater than those expected from population-apportioned bottom-up state inventories. In this study, we quantify CH4 emissions with an advanced mesoscale inverse modeling system at a resolution of 8 km 8 km, using aircraft measurements in the SoCAB during the 2010 Nexus of Air Quality and Climate Change campaign to constrain the inversion. To simulate atmospheric transport, we use the FLEXible PARTicle-Weather Research and Forecasting (FLEXPART-WRF) Lagrangian particle dispersion model driven by three configurations of the Weather Research and Forecasting (WRF) mesoscale model. We determine surface fluxes of CH4 using a Bayesian least squares method in a four-dimensional inversion. Simulated CH4 concentrations with the posterior emission inventory achieve much better correlations with the measurements (R2 = 0.7) than using the prior inventory (U.S. Environmental Protection Agency's National Emission Inventory 2005, R2 = 0.5). The emission estimates for CH4 in the posterior, 46.3 9.2 Mg CH4/h, are consistent with published observation-based estimates. Changes in the spatial distribution of CH4 emissions in the SoCAB between the prior and posterior inventories are discussed. Missing or underestimated emissions from dairies, the oil/gas system, and landfills in the SoCAB seem to explain the differences between the prior and posterior inventories. Furthermore, we estimate that dairies contributed 5.9 1.7 Mg CH4/h and the two sectors of oil and gas industries (production and downstream) and landfills together contributed 39.6 8.1 Mg CH4/h in the SoCAB.

  1. Hale County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Texas Edmonson, Texas Hale Center, Texas Petersburg, Texas Plainview, Texas Seth Ward, Texas Retrieved from "http:en.openei.orgwindex.php?titleHaleCounty,Texas&oldid...

  2. Hunt County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Number 3 Climate Zone Subtype A. Places in Hunt County, Texas Caddo Mills, Texas Campbell, Texas Celeste, Texas Commerce, Texas Greenville, Texas Hawk Cove, Texas Josephine,...

  3. Frio County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Subtype B. Places in Frio County, Texas Bigfoot, Texas Dilley, Texas Hilltop, Texas Moore, Texas North Pearsall, Texas Pearsall, Texas Retrieved from "http:en.openei.orgw...

  4. Hardin County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Places in Hardin County, Texas Kountze, Texas Lumberton, Texas Pinewood Estates, Texas Rose Hill Acres, Texas Silsbee, Texas Sour Lake, Texas Retrieved from "http:en.openei.org...

  5. Angelina County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Subtype A. Places in Angelina County, Texas Burke, Texas Diboll, Texas Hudson, Texas Huntington, Texas Lufkin, Texas Zavalla, Texas Retrieved from "http:en.openei.orgw...

  6. Chambers County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    County, Texas Reliant Baytown Biomass Facility Places in Chambers County, Texas Anahuac, Texas Baytown, Texas Beach City, Texas Cove, Texas Mont Belvieu, Texas Old...

  7. Geoscience/engineering characterization of the interwell environment in carbonate reservoirs based on outcrop analogs, Permian basin, west Texas and New Mexico. Quarterly technical progress report, July 1--September 30, 1995

    SciTech Connect (OSTI)

    Lucia, F.J.; Kerans, C.

    1995-12-01

    The objective of this project is to investigate styles of reservoir heterogeneity found in low-permeability pelleted wackestone/packstone facies and mixed carbonate/clastic facies found in Permian Basin reservoirs by studying similar facies exposed in the Guadalupe Mountains. Specific objectives for the outcrop study include construction of a stratigraphic framework, petrophysical quantification of the framework, and testing the outcrop reservoir model for effects of reservoir heterogeneity on production performance. Specific objectives for the subsurface study parallel objectives for the outcrop study. Mapping and documenting ooid channel deposits continued through the third quarter. A report on the geological characterization of the South Cowden field has been completed and submitted as the 1995 annual report. An initial simulation model of part of the Moss Unit has been prepared using a simple layering scheme and geostatistical techniques.

  8. The Convergence of Heat, Groundwater & Fracture Permeability. Innovative Play Fairway Modelling Applied to the Tularosa Basin Phase 1 Project Report

    SciTech Connect (OSTI)

    Bennett, Carlon R.; Nash, Gregory D.; Sorkhabi, Rasoul; Moore, Joseph; Simmons, Stuart; Brandt, Adam; Barker, Benjamin; Swanson, Brigitte

    2015-10-16

    This report summarizes the activities and key findings of the project team occurring during Phase 1 (August 2014-October 2015) of the Tularosa Basin Geothermal Play Fairway Analysis Project. The Tularosa Basin Play Fairway Analysis (PFA) project tested two distinct geothermal exploration methodologies covering the entire basin within South Central New Mexico and Far West Texas. Throughout the initial phase of the project, the underexplored basin proved to be a challenging, yet ideal test bed to evaluate effectiveness of the team’s data collection techniques as well as the effectiveness of our innovative PFA. Phase 1 of the effort employed a low-cost, pragmatic approach using two methods to identify potential geothermal plays within the study area and then compared and contrasted the results of each method to rank and evaluate potential plays. Both methods appear to be very effective and highly transferable to other areas.

  9. Radioactive waste isolation in salt: peer review of the Office of Nuclear Waste Isolation's reports on preferred repository sites within the Palo Duro Basin, Texas

    SciTech Connect (OSTI)

    Fenster, D.; Edgar, D.; Gonzales, S.; Domenico, P.; Harrison, W.; Engelder, T.; Tisue, M.

    1984-04-01

    Documents are being submitted to the Salt Repository Project Office (SRPO) of the US Department of Energy (DOE) by Battelle Memorial Institute's Office of Nuclear Waste Isolation (ONWI) to satisfy milestones of the Salt Repository Project of the Civilian Radioactive Waste Management Program. Some of these documents are being reviewed by multidisciplinary groups of peers to ensure DOE of their adequacy and credibility. Adequacy of documents refers to their ability to meet the standards of the US Nuclear Regulatory Commission, as enunciated in 10 CFR 60, and the requirements of the National Environmental Policy Act and the Nuclear Waste Policy Act of 1982. Credibility of documents refers to the validity of the assumptions, methods, and conclusions, as well as to the completeness of coverage. This report summarizes Argonne's review of ONWI's two-volume draft report entitled Identification of Preferred Sites within the Palo Duro Basin: Vol. 1 - Palo Duro Location A, and Vol. 2 - Palo Duro Location B, dated January 1984. Argonne was requested by DOE to review these documents on January 17 and 24, 1984 (see App. A). The review procedure involved obtaining written comments on the reports from three members of Argonne's core peer review staff and three extramural experts in related research areas. The peer review panel met at Argonne on February 6, 1984, and reviewer comments were integrated into this report by the review session chairman, with the assistance of Argonne's core peer review staff. All of the peer review panelists concurred in the way in which their comments were represented in this report (see App. B). A letter report and a draft of this report were sent to SRPO on February 10, 1984, and April 17, 1984, respectively. 5 references.

  10. Fluvial and deltaic facies and environments of the late permian back-reef shelves of the Permian Basin of Texas and New Mexico

    SciTech Connect (OSTI)

    Mazzullo, J. )

    1993-02-01

    The Artesia Group is a sequence of carbonates, evaporites, and clastics that was deposited across the back-reef shelves of the Permian Basin during late Permian time. There has been some controversy over the depositional environments of the clastic members of the Artesia Group and the role of sea level fluctuations in their accumulation. However, the results of a regional core study of the Queen Formation of the Artesia Group indicate that they were largely deposited in desert fluvial and deltaic environments during low-stands of sea level. Three fluvial-deltaic facies are recognized within the clastic members of the Queen. The first consists of medium to very find sandstones and silty sandstones with cross-beds, ripple cross-laminae, and planar and wavy laminae. This facies forms wavy sheets that thicken and thin along linear trends, and was deposited in sandy braided streams. The second facies consists of very find to fine sandstones, silty sandstones, and siltstones with ripple cross-laminae, planar and wavy laminae, cross-beds, clay drapes and pedogenetic cutans, as well as siltstones and silty mudstones with haloturbation structures and evaporite nodules. This facies forms thick planar sheets, and was deposited in fluvial sandflats and adjacent fluvial-dominated continental sabkhas. The third facies consists of cyclic deposits of haloturbated silty mudstones that grade into siltstones and very fine sandstones with crossbeds, planar and wavy laminae, haloturbation structures and evaporite nodules. Each cycle forms a lobate body that is bounded by carbonates or evaporites and which was deposited in sheet deltas that formed along the landward margins of a back-reef lagoon.

  11. ,"Texas Natural Gas Prices"

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

    Data for" ,"Data 1","Texas Natural Gas Prices",8,"Monthly","2... 6:46:23 AM" "Back to Contents","Data 1: Texas Natural Gas Prices" "Sourcekey","N3050TX3"...

  12. Parana basin

    SciTech Connect (OSTI)

    Zalan, P.V.; Wolff, S.; Conceicao, J.C.J.; Vieira, I.S.; Astolfi, M.A.; Appi, V.T.; Zanotto, O.; Neto, E.V.S.; Cerqueira, J.R.

    1987-05-01

    The Parana basin is a large intracratonic basin in South America, developed entirely on continental crust and filled with sedimentary and volcanic rocks ranging in age from Silurian to Cretaceous. It occupies the southern portion of Brazil (1,100,000 km/sup 2/ or 425,000 mi/sup 2/) and the eastern half of Paraguay (100,000 km/sup 2/ or 39,000 mi/sup 2/); its extension into Argentina and Uruguay is known as the Chaco-Parana basin. Five major depositional sequences (Silurian, Devonian, Permo-Carboniferous, Triassic, Juro-Cretaceous) constitute the stratigraphic framework of the basin. The first four are predominantly siliciclastic in nature, and the fifth contains the most voluminous basaltic lava flows of the planet. Maximum thicknesses are in the order of 6000 m (19,646 ft). The sequences are separated by basin wide unconformities related in the Paleozoic to Andean orogenic events and in the Mesozoic to the continental breakup and sea floor spreading between South America and Africa. The structural framework of the Parana basin consists of a remarkable pattern of criss-crossing linear features (faults, fault zones, arches) clustered into three major groups (N45/sup 0/-65/sup 0/W, N50/sup 0/-70/sup 0/E, E-W). The northwest- and northeast-trending faults are long-lived tectonic elements inherited from the Precambrian basement whose recurrent activity throughout the Phanerozoic strongly influenced sedimentation, facies distribution, and development of structures in the basin. Thermomechanical analyses indicate three main phases of subsidence (Silurian-Devonian, late Carboniferous-Permian, Late Jurassic-Early Cretaceous) and low geothermal gradients until the beginning of the Late Jurassic Permian oil-prone source rocks attained maturation due to extra heat originated from Juro-Cretaceous igneous intrusions. The third phase of subsidence also coincided with strong tectonic reactivation and creation of a third structural trend (east-west).

  13. Revitalizing a mature oil play: Strategies for finding and producing unrecovered oil in Frio Fluvial-Deltaic reservoirs of South Texas. Technical progress report, April 1, 1994--June 30, 1994

    SciTech Connect (OSTI)

    Tyler, N.; Dutton, S.

    1994-06-30

    Advanced reservoir characterization techniques are being applied to selected reservoirs in the Frio Fluvial-Deltaic Sandstone (Vicksburg Fault Zone) trend of South Texas in order to maximize the economic producibility of resources in this mature oil play. More than half of the reservoirs in this depositionally complex play have already been abandoned, and large volumes of oil may remain unproduced unless advanced characterization techniques are applied to define untapped, incompletely drained, and new pool reservoirs as suitable targets for near-term recovery methods. This project is developing interwell-scale geological facies models and assessing engineering attributes of Frio fluvial-deltaic reservoirs in selected fields in order to characterize reservoir architecture, flow unit boundaries, and the controls that these characteristics exert on the location and volume of unrecovered mobile and residual oil. The results of these studies will lead directly to the identification of specific opportunities to exploit these heterogeneous reservoirs for incremental recovery by recompletion and strategic infill drilling. Work during the second project quarter of 1994 focused on continuation of Phase 2 tasks associated with characterizing stratigraphic heterogeneity in selected Frio fluvial-deltaic sandstone reservoirs. Playwide reservoir assessment continued as reservoir engineering data from fields throughout the Frio Fluvial-Deltaic Sandstone trend were grouped within stratigraphic sub-intervals in order to characterize general reservoir heterogeneity, evaluate production behavior, and assess remaining resource potential in middle Frio, lower Frio, and upper Vicksburg reservoir sandstones.

  14. Milam County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Number 2 Climate Zone Subtype A. Places in Milam County, Texas Buckholts, Texas Cameron, Texas Milano, Texas Rockdale, Texas Thorndale, Texas Retrieved from "http:...

  15. Duval County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Number 2 Climate Zone Subtype A. Places in Duval County, Texas Benavides, Texas Concepcion, Texas Freer, Texas Realitos, Texas San Diego, Texas Retrieved from "http:...

  16. Uvalde County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    2 Climate Zone Subtype B. Places in Uvalde County, Texas Knippa, Texas Sabinal, Texas Utopia, Texas Uvalde Estates, Texas Uvalde, Texas Retrieved from "http:en.openei.orgw...

  17. Hall County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    B. Places in Hall County, Texas Estelline, Texas Lakeview, Texas Memphis, Texas Turkey, Texas Retrieved from "http:en.openei.orgwindex.php?titleHallCounty,Texas&oldid...

  18. Nacogdoches County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    A. Places in Nacogdoches County, Texas Appleby, Texas Chireno, Texas Cushing, Texas Garrison, Texas Nacogdoches, Texas Retrieved from "http:en.openei.orgw...

  19. Texas Nuclear Profile - Power Plants

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

    nuclear power plants, summer capacity and net generation, 2010" "Plant name/total reactors","Summer capacity (mw)","Net generation (thousand mwh)","Share of State nuclear net generation (percent)","Owner" "Comanche Peak Unit 1, Unit 2","2,406","20,208",48.9,"Luminant Generation Company LLC" "South Texas Project Unit 1, Unit 2","2,560","21,127",51.1,"STP Nuclear

  20. Texas Solar Energy Society | Open Energy Information

    Open Energy Info (EERE)

    Society Jump to: navigation, search Logo: Texas Solar Energy Society Name: Texas Solar Energy Society Address: P. O. Box 1447 Place: Austin, Texas Zip: 78767 Region: Texas Area...

  1. Biodiesel Coalition of Texas | Open Energy Information

    Open Energy Info (EERE)

    Coalition of Texas Jump to: navigation, search Logo: Biodiesel Coalition of Texas Name: Biodiesel Coalition of Texas Address: 100 Congress Avenue Place: Austin, Texas Zip: 78701...

  2. Central Texas Biofuels LLC | Open Energy Information

    Open Energy Info (EERE)

    Texas Biofuels LLC Jump to: navigation, search Name: Central Texas Biofuels LLC Place: Giddings, Texas Zip: 78942 Product: Biodiesel producer in Giddings, Texas. References:...

  3. Texas Retail Energy, LLC (Texas) | Open Energy Information

    Open Energy Info (EERE)

    Texas Retail Energy, LLC (Texas) Jump to: navigation, search Name: Texas Retail Energy, LLC Address: 2001 SE 10th St Place: Bentonville, AR Zip: 72712 Phone Number: (479) 204-0845...

  4. Texas City, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Texas City is a city in Chambers County and Galveston County, Texas. It falls under Texas's 14th congressional...

  5. DOE-Sponsored IGCC Project in Texas Takes Important Step Forward...

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

    The captured CO2 will be used for enhanced oil recovery (EOR) in the West Texas Permian Basin, a process that both prevents the greenhouse gas from entering the atmosphere and ...

  6. Enernoc (Texas) | Open Energy Information

    Open Energy Info (EERE)

    Lamar Place: Houston, Texas Zip: 77002 Region: Texas Area Sector: Efficiency Product: Demand response provider serving commercial and industrial customers Website:...

  7. Geoscience/engineering characterization of the interwell environment in carbonate reservoirs based on outcrop analogs, Permian Basin, West Texas and New Mexico-stratigraphic hierarchy and cycle stacking facies distribution, and interwell-scale heterogeneity: Grayburg Formation, New Mexico. Final report

    SciTech Connect (OSTI)

    Barnaby, R.J.; Ward, W.B.; Jennings, J.W. Jr.

    1997-06-01

    The Grayburg Formation (middle Guadalupian) is a major producing interval in the Permian Basin and has yielded more than 2.5 billion barrels of oil in West Texas. Grayburg reservoirs have produced, on average, less than 30 percent of their original oil in place and are undergoing secondary and tertiary recovery. Efficient design of such enhanced recovery programs dictates improved geological models to better understand and predict reservoir heterogeneity imposed by depositional and diagenetic controls. The Grayburg records mixed carbonate-siliciclastic sedimentation on shallow-water platforms that rimmed the Delaware and Midland Basins. Grayburg outcrops in the Guadalupe and Brokeoff Mountains region on the northwest margin of the Delaware Basin present an opportunity to construct a detailed, three-dimensional image of the stratigraphic and facies architecture. This model can be applied towards improved description and characterization of heterogeneity in analogous Grayburg reservoirs. Four orders of stratigraphic hierarchy are recognized in the Grayburg Formation. The Grayburg represents a long-term composite sequence composed of four high-frequency sequences (HFS 1-4). Each HFS contains several composite cycles comprising two or more cycles that define intermediate-scale transgressive-regressive successions. Cycles are the smallest scale upward-shoaling vertical facies successions that can be recognized and correlated across various facies tracts. Cycles thus form the basis for establishing the detailed chronostratigraphic correlations needed to delineate facies heterogeneity.

  8. Platform, Delaware Basin, and Midland Basin, West Texas and New...

    Office of Scientific and Technical Information (OSTI)

    The two primary emphases were on: (1) delineating the temporal and spatial evolution of the regional stress state; and (2) calculating the amount of regional shortening...

  9. South Trent Wind Farm LLC | Open Energy Information

    Open Energy Info (EERE)

    South Trent Wind Farm LLC Jump to: navigation, search Name: South Trent Wind Farm, LLC Place: Texas Sector: Wind energy Product: US-based wind project developer and special purpose...

  10. Collingsworth County, Texas: Energy Resources | Open Energy Informatio...

    Open Energy Info (EERE)

    Places in Collingsworth County, Texas Dodson, Texas Quail, Texas Samnorwood, Texas Wellington, Texas Retrieved from "http:en.openei.orgwindex.php?titleCollingsworthCounty,...

  11. Ector County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Number 3 Climate Zone Subtype B. Places in Ector County, Texas Gardendale, Texas Goldsmith, Texas Odessa, Texas West Odessa, Texas Retrieved from "http:en.openei.orgw...

  12. Brooks County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    169-2006 Climate Zone Number 2 Climate Zone Subtype A. Places in Brooks County, Texas Airport Road Addition, Texas Cantu Addition, Texas Encino, Texas Falfurrias, Texas Flowella,...

  13. Matagorda County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Subtype A. Registered Energy Companies in Matagorda County, Texas Gulf Coast Green Energy Places in Matagorda County, Texas Bay City, Texas Blessing, Texas Markham, Texas...

  14. Callahan County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    169-2006 Climate Zone Number 3 Climate Zone Subtype B. Places in Callahan County, Texas Baird, Texas Clyde, Texas Cross Plains, Texas Putnam, Texas Retrieved from "http:...

  15. Coke County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Subtype B. Places in Coke County, Texas Blackwell, Texas Bronte, Texas Robert Lee, Texas Retrieved from "http:en.openei.orgwindex.php?titleCokeCounty,Texas&oldid...

  16. Parmer County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    County, Texas Scandia Wind Southwest LLC Places in Parmer County, Texas Bovina, Texas Farwell, Texas Friona, Texas Retrieved from "http:en.openei.orgwindex.php?titleParmerCo...

  17. Grimes County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    169-2006 Climate Zone Number 2 Climate Zone Subtype A. Places in Grimes County, Texas Anderson, Texas Bedias, Texas Navasota, Texas Todd Mission, Texas Retrieved from "http:...

  18. San Patricio County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    A. Places in San Patricio County, Texas Aransas Pass, Texas Corpus Christi, Texas Del Sol-Loma Linda, Texas Doyle, Texas Edgewater-Paisano, Texas Edroy, Texas Falman-County...

  19. Bastrop County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Number 2 Climate Zone Subtype A. Places in Bastrop County, Texas Bastrop, Texas Camp Swift, Texas Circle D-KC Estates, Texas Elgin, Texas Mustang Ridge, Texas Smithville, Texas...

  20. Medina County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Castroville, Texas Devine, Texas Hondo, Texas LaCoste, Texas Lytle, Texas Natalia, Texas San Antonio, Texas Retrieved from "http:en.openei.orgwindex.php?titleMedinaCounty,T...

  1. Lamar County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    A. Places in Lamar County, Texas Blossom, Texas Deport, Texas Paris, Texas Roxton, Texas Sun Valley, Texas Toco, Texas Retrieved from "http:en.openei.orgwindex.php?titleLamar...

  2. Texas Power, LP | Open Energy Information

    Open Energy Info (EERE)

    search Name: Texas Power, LP Place: Texas Website: www.texaspoweronline.com Facebook: https:www.facebook.compagesTexas-Power-LP110752578951516 References: EIA Form...

  3. Third Planet Windpower (Texas) | Open Energy Information

    Open Energy Info (EERE)

    Windpower (Texas) Jump to: navigation, search Name: Third Planet Windpower Address: 909 Fannin Place: Houston, Texas Zip: 77010 Region: Texas Area Sector: Wind energy Product:...

  4. Fermilab Today | University of Texas at Arlington

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

    Texas at Arlington Aug. 22, 2012 NAME: University of Texas at Arlington HOME TOWN: Arlington, Texas MASCOT: Blaze the Mustang SCHOOL COLORS: Orange and blue COLLABORATING AT...

  5. Texas Department of Transportation | Open Energy Information

    Open Energy Info (EERE)

    Texas Department of Transportation Jump to: navigation, search Logo: Texas Department of Transportation Name: Texas Department of Transportation Abbreviation: TxDOT Place: Austin,...

  6. Texas Emerging Technology Fund | Open Energy Information

    Open Energy Info (EERE)

    Emerging Technology Fund Jump to: navigation, search Name: Texas Emerging Technology Fund Place: Texas Product: String representation "The Texas Emerg ... hnology fields." is too...

  7. Corsicana, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    County, Texas. It falls under Texas's 6th congressional district.12 Registered Energy Companies in Corsicana, Texas Corsicana Chemical Company References US Census...

  8. Austin, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Entrepreneurs Network Austin Technology Incubator Biodiesel Coalition of Texas Texas Renewable Energy Industries Association Texas Solar Energy Society The Wind Coalition...

  9. Texas General Land Office | Open Energy Information

    Open Energy Info (EERE)

    Land Office Jump to: navigation, search Logo: Texas General Land Office Name: Texas General Land Office Address: 1700 Congress Ave Place: Austin, Texas Zip: 78701 Website:...

  10. Basin development, petrology, and paleogeography - Early Permian carbonates, northwestern Bolivia

    SciTech Connect (OSTI)

    Canter, K.L.; Isaacson, P.E. )

    1990-05-01

    Early Permian carbonate rocks of the Yaurichambi Formation in northwestern Bolivia demonstrate in-situ, low-paleolatitude development within a complexly interbedded sequence punctuated by siliciclastics apparently derived from a western source. The Yaurichambi Formation (Copacabana Group) occurs above a regional caliche surface that caps Upper Carboniferous quartzarenites. Lower beds of the formation are characterized by interbedded carbonate and quartz-rich lithologies. This interval is gradationally overlain by a shallowing-upward, carbonate-dominated sequence. Mud-rich wackestones and packstones grade upward to bioclastic packstones and grainstones. Common allochems in bioclastic-rich lithologies include echinoderms, brachiopods, fenestrate bryozoans, intraclasts, and less common corals. Uppermost beds contain abundant siliciclastic interbeds. Where exposed, this carbonate sequence is terminated by the Tiquina Sandstone. Permian rocks were deposited in a northwest-southeast-oriented basin. Siliciclastic flooding from the western and southwestern margin of the basin dominated throughout the Carboniferous and occurred intermittently during the Permian, with apparent shallowing to the south. A low-latitude paleogeographic setting for these rocks is indicated by the carbonate lithologies dominating the Lower Permian sequence. Sedimentary and diagenetic features diagnostic of semi-arid warm-water deposition include penecontemporaneous dolomites, fenestral fabric, and calcretes. Furthermore, the faunas are similar to those found in equivalent strata of the Permian basin area of west Texas, indicating that deposition occurred at relatively low latitudes.

  11. INTEGRATED OUTCROP AND SUBSURFACE STUDIES OF THE INTERWELL ENVIRONMENT OF CARBONATE RESERVOIRS: CLEAR FORK (LEONARDIAN-AGE) RESERVOIRS, WEST TEXAS AND NEW MEXICO

    SciTech Connect (OSTI)

    F. Jerry Lucia

    2002-01-31

    This is the final report of the project ''Integrated Outcrop and Subsurface Studies of the Interwell Environment of Carbonate Reservoirs: Clear Fork (Leonardian-Age) Reservoirs, West Texas and New Mexico'', Department of Energy contract no. DE-AC26-98BC15105 and is the third in a series of similar projects funded jointly by the U.S. Department of Energy and The University of Texas at Austin, Bureau of Economic Geology, Reservoir Characterization Research Laboratory for Carbonates. All three projects focus on the integration of outcrop and subsurface data for the purpose of developing improved methods for modeling petrophysical properties in the interwell environment. The first project, funded by contract no. DE-AC22-89BC14470, was a study of San Andres outcrops in the Algerita Escarpment, Guadalupe Mountains, Texas and New Mexico, and the Seminole San Andres reservoir, Permian Basin. This study established the basic concepts for constructing a reservoir model using sequence-stratigraphic principles and rock-fabric, petrophysical relationships. The second project, funded by contract no. DE-AC22-93BC14895, was a study of Grayburg outcrops in the Brokeoff Mountains, New Mexico, and the South Cowden Grayburg reservoir, Permian Basin. This study developed a sequence-stratigraphic succession for the Grayburg and improved methods for locating remaining hydrocarbons in carbonate ramp reservoirs. The current study is of the Clear Fork Group in Apache Canyon, Sierra Diablo Mountains, West Texas, and the South Wasson Clear Fork reservoir, Permian Basin. The focus was on scales of heterogeneity, imaging high- and low-permeability layers, and the impact of fractures on reservoir performance. In this study (1) the Clear Fork cycle stratigraphy is defined, (2) important scales of petrophysical variability are confirmed, (3) a unique rock-fabric, petrophysical relationship is defined, (4) a porosity method for correlating high-frequency cycles and defining rock-fabric flow layers

  12. Texas | OpenEI Community

    Open Energy Info (EERE)

    Submitted by Alevine(5) Member 29 July, 2013 - 14:46 Texas Legal Review BHFS flora and fauna leasing Legal review permitting roadmap Texas The NREL roadmap team recently met with...

  13. Texas Area | Open Energy Information

    Open Energy Info (EERE)

    Area Jump to: navigation, search Contents 1 Clean Energy Clusters in the Texas Area 1.1 Products and Services in the Texas Area 1.2 Research and Development Institutions in the...

  14. Texas Workshop Program V01

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

    Workshop on Studies of Super-Heavy Nuclei at the SHE Factory and Super-Heavy Element Collaboration Meeting Texas A&M University College Station, Texas March 12-13, 2013 Tuesday, ...

  15. Zavala County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Number 2 Climate Zone Subtype B. Places in Zavala County, Texas Batesville, Texas Chula Vista-River Spur, Texas Crystal City, Texas La Pryor, Texas Las Colonias, Texas Retrieved...

  16. Hood County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    169-2006 Climate Zone Number 3 Climate Zone Subtype A. Places in Hood County, Texas Brazos Bend, Texas Cresson, Texas DeCordova, Texas Granbury, Texas Lipan, Texas Oak Trail...

  17. Nueces County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    169-2006 Climate Zone Number 2 Climate Zone Subtype A. Places in Nueces County, Texas Agua Dulce, Texas Aransas Pass, Texas Bishop, Texas Corpus Christi, Texas Driscoll, Texas...

  18. Texas Onshore Natural Gas Plant Liquids Production Extracted in Texas

    Gasoline and Diesel Fuel Update (EIA)

    (Million Cubic Feet) Texas (Million Cubic Feet) Texas Onshore Natural Gas Plant Liquids Production Extracted in Texas (Million Cubic Feet) Decade Year-0 Year-1 Year-2 Year-3 Year-4 Year-5 Year-6 Year-7 Year-8 Year-9 2010's 790,721 - = No Data Reported; -- = Not Applicable; NA = Not Available; W = Withheld to avoid disclosure of individual company data. Release Date: 08/31/2016 Next Release Date: 09/30/2016 Referring Pages: NGPL Production, Gaseous Equivalent Texas Onshore-Texas

  19. Texas Onshore Natural Gas Processed in Texas (Million Cubic Feet)

    Gasoline and Diesel Fuel Update (EIA)

    Texas (Million Cubic Feet) Texas Onshore Natural Gas Processed in Texas (Million Cubic Feet) Decade Year-0 Year-1 Year-2 Year-3 Year-4 Year-5 Year-6 Year-7 Year-8 Year-9 2010's 4,763,732 5,274,730 5,854,956 6,636,937 - = No Data Reported; -- = Not Applicable; NA = Not Available; W = Withheld to avoid disclosure of individual company data. Release Date: 08/31/2016 Next Release Date: 09/30/2016 Referring Pages: Natural Gas Processed Texas Onshore-Texas

  20. Blanco County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Number 3 Climate Zone Subtype A. Places in Blanco County, Texas Blanco, Texas Johnson City, Texas Round Mountain, Texas Retrieved from "http:en.openei.orgw...

  1. Crosby County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Number 3 Climate Zone Subtype B. Registered Energy Companies in Crosby County, Texas Brownfield Biodiesel LLC Places in Crosby County, Texas Crosbyton, Texas Lorenzo, Texas Ralls,...

  2. Renewable Energy Systems Inc (RES Americas) (Texas) | Open Energy...

    Open Energy Info (EERE)

    (Texas) Jump to: navigation, search Name: Renewable Energy Systems Inc (RES Americas) Address: 9050 Capital of Texas Hwy Place: Austin, Texas Zip: 78759 Region: Texas Area Sector:...

  3. Calhoun County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Number 2 Climate Zone Subtype A. Places in Calhoun County, Texas Point Comfort, Texas Port Lavaca, Texas Seadrift, Texas Retrieved from "http:en.openei.orgw...

  4. Gillespie County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    3 Climate Zone Subtype A. Places in Gillespie County, Texas Fredericksburg, Texas Harper, Texas Stonewall, Texas Retrieved from "http:en.openei.orgwindex.php?titleGillesp...

  5. SEMI-ANNUAL REPORTS FOR TEXAS LNG - TEXAS LNG - FTA - FE DKT...

    Office of Environmental Management (EM)

    TEXAS LNG - TEXAS LNG - FTA - FE DKT. NO. 13-160-LNG - 3443 SEMI-ANNUAL REPORTS FOR TEXAS LNG - TEXAS LNG - FTA - FE DKT. NO. 13-160-LNG - 3443 October 2014 April 2015 More...

  6. SEMI-ANNUAL REPORTS FOR TEXAS LNG - TEXAS LNG - FTA - FE DKT...

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

    TEXAS LNG - TEXAS LNG - FTA - FE DKT. NO. 13-160-LNG - 3443 SEMI-ANNUAL REPORTS FOR TEXAS LNG - TEXAS LNG - FTA - FE DKT. NO. 13-160-LNG - 3443 PDF icon October 2014 PDF icon April ...

  7. Geoscience/engineering characterization of the interwell environment in carbonate reservoirs based on outcrop analogs, Permian Basin, West Texas and New Mexico. Quarterly report, January 1--April 30, 1996

    SciTech Connect (OSTI)

    Lucia, F.J.; Kerans, C.

    1996-04-30

    The objective of this project is to investigate styles of reservoir heterogeneity found in low-permeability pelleted wackestone/packstone facies and mixed carbonate/clastic facies found in Permian Basin reservoirs by studying similar facies exposed in the Guadalupe Mountains. Specific objectives for the outcrop study include construction of a stratigraphic framework, petrophysical quantification of the framework, and testing the outcrop reservoir model for effects of reservoir heterogeneity on production performance. Specific objectives for the subsurface study parallel objectives for the outcrop study.

  8. Geoscience/engineering characterization of the interwell environment in carbonate reservoirs based on outcrop analogs, Permian Basin, West Texas and New Mexico. Quarterly technical progress report, April 1, 1995--June 1, 1995

    SciTech Connect (OSTI)

    Lucia, F.J.; Kerans, C.

    1995-09-01

    The objective of this project is to investigate styles of reservoir heterogeneity that occur in low permeability pelleted wackestone/packstone facies and mixed carbonate/clastic facies found in Permian Basin reservoirs by studying similar facies exposed in the Guadalupe mountains. Specific objectives for the outcrop study include construction of a stratigraphic framework, petrophysical quantification of the framework, and testing the outcrop reservoir model for effects of reservoir heterogeneity on production performance. Specific objectives for the subsurface study parallel objectives for the outcrop study. Technical progress is reported for outcrop activities and subsurface activities.

  9. Abandoned Texas oil fields

    SciTech Connect (OSTI)

    Not Available

    1980-12-01

    Data for Texas abandoned oil fields were primarily derived from two sources: (1) Texas Railroad Commission (TRRC), and (2) Dwight's ENERGYDATA. For purposes of this report, abandoned oil fields are defined as those fields that had no production during 1977. The TRRC OILMASTER computer tapes were used to identify these abandoned oil fields. The tapes also provided data on formation depth, gravity of oil production, location (both district and county), discovery date, and the cumulative production of the field since its discovery. In all, the computer tapes identified 9211 abandoned fields, most of which had less than 250,000 barrel cumulative production. This report focuses on the 676 abandoned onshore Texas oil fields that had cumulative production of over 250,000 barrels. The Dwight's ENERGYDATA computer tapes provided production histories for approximately two-thirds of the larger fields abandoned in 1966 and thereafter. Fields which ceased production prior to 1966 will show no production history nor abandonment date in this report. The Department of Energy hopes the general availability of these data will catalyze the private sector recovery of this unproduced resource.

  10. Ferris, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    is a stub. You can help OpenEI by expanding it. Ferris is a city in Dallas County and Ellis County, Texas. It falls under Texas's 30th congressional district and Texas's 6th...

  11. Texas Municipal Power Agency | Open Energy Information

    Open Energy Info (EERE)

    Texas Municipal Power Agency Jump to: navigation, search Name: Texas Municipal Power Agency Place: Texas Sector: Wind energy Phone Number: (936) 873-1100 Website: www.texasmpa.org...

  12. WKN Texas LLC | Open Energy Information

    Open Energy Info (EERE)

    Product: A wind farm developer based in Texas. Originally a subsidiary of Windkraft Nord USA, WKN Texas LLC is currently owned by Enel North America. References: WKN Texas LLC1...

  13. Friendswood, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    You can help OpenEI by expanding it. Friendswood is a city in Galveston County and Harris County, Texas. It falls under Texas's 14th congressional district and Texas's 22nd...

  14. Tomball, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Tomball is a city in Harris County, Texas. It falls under Texas's 10th congressional district and Texas's 8th...

  15. Seabrook, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    OpenEI by expanding it. Seabrook is a city in Chambers County and Galveston County and Harris County, Texas. It falls under Texas's 14th congressional district and Texas's 22nd...

  16. Shoreacres, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    stub. You can help OpenEI by expanding it. Shoreacres is a city in Chambers County and Harris County, Texas. It falls under Texas's 14th congressional district and Texas's 22nd...

  17. Pearland, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    OpenEI by expanding it. Pearland is a city in Brazoria County and Fort Bend County and Harris County, Texas. It falls under Texas's 14th congressional district and Texas's 22nd...

  18. Humble, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Humble is a city in Harris County, Texas. It falls under Texas's 2nd congressional district and Texas's 18th...

  19. Stafford, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    stub. You can help OpenEI by expanding it. Stafford is a city in Fort Bend County and Harris County, Texas. It falls under Texas's 9th congressional district and Texas's 22nd...

  20. Baytown, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    a stub. You can help OpenEI by expanding it. Baytown is a city in Chambers County and Harris County, Texas. It falls under Texas's 14th congressional district and Texas's 2nd...

  1. Pasadena, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Pasadena is a city in Harris County, Texas. It falls under Texas's 22nd congressional district and Texas's 29th...

  2. Abilene, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    is a stub. You can help OpenEI by expanding it. Abilene is a city in Jones County and Taylor County, Texas. It falls under Texas's 13th congressional district and Texas's 19th...

  3. ,"Texas Underground Natural Gas Storage - All Operators"

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

    ...010TX2","N5020TX2","N5070TX2","N5050TX2","N5060TX2" "Date","Texas Natural Gas Underground Storage Volume (MMcf)","Texas Natural Gas in Underground Storage (Base Gas) (MMcf)","Texas ...

  4. Texas A&M University

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

    from women, minorities, individuals with disabilities, and veterans. In addition, Texas A&M University strives to be responsive to the particular needs of dual career...

  5. OpenEI Community - Texas

    Open Energy Info (EERE)

    Texas Legal Review http:en.openei.orgcommunityblogtexas-legal-review

    The NREL roadmap team recently met with our legal team Brownstein Hyatt Farber and Schreck...

  6. CPower (Texas) | Open Energy Information

    Open Energy Info (EERE)

    Texas Area Sector: Efficiency Product: Provides various energy efficiencymanagement services Website: www.cpowered.com Coordinates: 30.264043, -97.744762 Show Map...

  7. Fermilab Today | Texas Tech University

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

    and to increasing public awareness of physics research. FUNDING AGENCIES: DOE, NSF Texas Tech University High-Energy Physics Group: (Left) From left: Kittikul Kovitanggoon, Nural...

  8. RAPID/Geothermal/Land Access/Texas | Open Energy Information

    Open Energy Info (EERE)

    Texas GLO Coastal Forms Texas GLO Highway Right of Way Leasing Forms Texas GLO Oil and Gas Sealed Bid Forms Texas GLO Rights of Way Forms Texas General Land Office - Rights of...

  9. Geothermal resource assessment for the state of Texas: status of progress, November 1980. Final report

    SciTech Connect (OSTI)

    Woodruff, C.M. Jr.; Caran, S.C.; Gever, C.; Henry, C.D.; Macpherson, G.L.; McBride, M.W.

    1982-03-01

    Data pertaining to wells and thermal aquifers and data interpretation methods are presented. Findings from a program of field measurements of water temperatures (mainly in South-Central Texas) and an assessment of hydrologic properties of three Cretaceous aquifers (in North-Central Texas) are included. Landsat lineaments and their pertinance to the localization of low-temperature geothermal resources are emphasized. Lineament data were compared to structural and stratigraphic features along the Balcones/Ouachita trend in Central Texas to test for correlations. (MHR)

  10. Waco, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Registered Research Institutions in Waco, Texas Baylor University - Renewable Aviation Fuels Development Center Registered Energy Companies in Waco, Texas McDowell Research...

  11. Texas Solar Power Company | Open Energy Information

    Open Energy Info (EERE)

    1703 W Koenig Ln Place: Austin, Texas Zip: 78756 Region: Texas Area Sector: Solar Product: Design, sales and installation of renewable energy equipment and systems Website:...

  12. SVTC Technologies (Texas) | Open Energy Information

    Open Energy Info (EERE)

    Austin, Texas Zip: 78741 Region: Texas Area Sector: Solar Product: Provides emiconductor process tools for new silicon developers Website: www.svtc.com Coordinates: 30.218411,...

  13. Texas/Wind Resources | Open Energy Information

    Open Energy Info (EERE)

    TexasWind Resources < Texas Jump to: navigation, search Print PDF Print Full Version WIND ENERGY STAKEHOLDER ENGAGEMENT & OUTREACHSmall Wind Guidebook OpenEI Home >> Wind >> Small...

  14. Element Labs (Texas) | Open Energy Information

    Open Energy Info (EERE)

    Blvd Place: Austin, Texas Zip: 78758 Region: Texas Area Sector: Efficiency Product: LED Producer Website: www.elementlabs.com Coordinates: 30.376797, -97.715649 Show Map...

  15. Texas Beachfront Construction Webpage | Open Energy Information

    Open Energy Info (EERE)

    Construction Webpage Jump to: navigation, search OpenEI Reference LibraryAdd to library Web Site: Texas Beachfront Construction Webpage Author Texas General Land Office Published...

  16. Texas Water Development Board | Open Energy Information

    Open Energy Info (EERE)

    Development Board Jump to: navigation, search Logo: Texas Water Development Board Name: Texas Water Development Board Abbreviation: TWDB Address: 1700 North Congress Avenue Place:...

  17. PEPCO Energy Services (Texas) | Open Energy Information

    Open Energy Info (EERE)

    PEPCO Energy Services (Texas) Jump to: navigation, search Name: PEPCO Energy Services Place: Texas Website: www.pepcoenergy.com References: EIA Form EIA-861 Final Data File for...

  18. REC Generator Certification Application - Texas | Open Energy...

    Open Energy Info (EERE)

    REC Generator Certification Application - Texas Jump to: navigation, search OpenEI Reference LibraryAdd to library Reference: REC Generator Certification Application - Texas...

  19. Geopower Texas Co | Open Energy Information

    Open Energy Info (EERE)

    Product: Oregon-based Geo Texas was founded in January 2009 by former Vulcan Power CEO Steve Munson to develop geothermal projects in Texas. Coordinates: 44.05766,...

  20. Amarillo, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Act Smart Grid Projects in Amarillo, Texas Golden Spread Electric Cooperative, Inc. Smart Grid Project Utility Companies in Amarillo, Texas Golden Spread Electric...

  1. Fermilab Today | University of Texas at Austin

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

    Austin March 13, 2013 NAME: University of Texas at Austin HOME TOWN: Austin, Texas MASCOT: Bevo the Longhorn COLORS: Burnt orange COLLABORATING AT FERMILAB SINCE: Mid-1990s...

  2. Texas/Incentives | Open Energy Information

    Open Energy Info (EERE)

    137) Incentive Incentive Type Active AEP Texas North Company - CitySmart Program (Texas) Utility Rebate Program Yes AEP (Central and North) - Residential Energy Efficiency...

  3. ,"Texas Natural Gas Underground Storage Capacity (MMcf)"

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

    Data for" ,"Data 1","Texas Natural Gas Underground Storage Capacity ... 7:01:01 AM" "Back to Contents","Data 1: Texas Natural Gas Underground Storage Capacity ...

  4. ,"Texas Natural Gas Consumption by End Use"

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

    Data for" ,"Data 1","Texas Natural Gas Consumption by End ... 6:36:11 AM" "Back to Contents","Data 1: Texas Natural Gas Consumption by End Use" ...

  5. ,"Texas Natural Gas Vehicle Fuel Consumption (MMcf)"

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

    Data for" ,"Data 1","Texas Natural Gas Vehicle Fuel Consumption ... 7:09:53 AM" "Back to Contents","Data 1: Texas Natural Gas Vehicle Fuel Consumption ...

  6. ,"Texas Natural Gas Underground Storage Withdrawals (MMcf)"

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

    Data for" ,"Data 1","Texas Natural Gas Underground Storage ... 7:00:40 AM" "Back to Contents","Data 1: Texas Natural Gas Underground Storage ...

  7. Environmental assessment: Deaf Smith County site, Texas

    SciTech Connect (OSTI)

    Not Available

    1986-05-01

    In February 1983, the US Department of Energy (DOE) identified a location in Deaf Smith County, Texas, as one of the nine potentially acceptable sites for mined geologic repository for spent nuclear fuel and high-level radioactive waste. To determine their suitability, the Deaf Smith County site and eight other potentially acceptable sites have been evaluated in accordance with the DOE's General Guidelines for the Recommendation of Sites for the Nuclear Waste Repositories. The Deaf Smith County site is in the Permian Basin, which is one of five distinct geohydrologic settings considered for the first repository. On the basis of the evaluations reported in this EA, the DOE has found that the Deaf Smith County site is not disqualified under the guidelines.

  8. Environmental assessment: Deaf Smith County site, Texas

    SciTech Connect (OSTI)

    Not Available

    1986-05-01

    In February 1983, the US Department of Energy (DOE) identified a location in Deaf Smith County, Texas, as one of nine potentially acceptable sites for a mined geologic repository for spent nuclear fuel and high-level radioactive waste. To determine their suitability, the Deaf Smith County site and the eight other potentially sites have been evaluated in accordance with the DOE's General Guidelines for the Recommendation of Sites for the Nuclear Waste Repositories. The Deaf Smith County site is in the Permian Basin, which is one of five distinct geohydrologic settings considered for the first repository. On the basis of the evaluations reported in this EA, the DOE has found that the Deaf Smith County site is not disqualified under the guidelines. On the basis of these findings, the DOE is nominating the Deaf Smith County site as one of the five sites suitable for characterization. 591 refs., 147 figs., 173 tabs.

  9. Coastal land loss in Texas - An overview

    SciTech Connect (OSTI)

    Morton, R.A.; Paine, J.G. )

    1990-09-01

    Each year in Texas more than 1,500 acres of prime real estate and productive wetlands are destroyed along the Gulf shoreline and near the bay margins primarily as a result of coastal erosion and submergence. Wetland losses constitute about half of the total land losses. Historical analyses of maps and aerial photographs since the mid-1800s indicate that land losses are accelerating and that human activities are either directly or indirectly responsible for the increased losses, Natural decreases in sediment supply since the modern sea-level stillstand have been exacerbated by (1) river basin projects that reduce the volume of sediment transported to the coast and (2) coastal structures and navigation projects that prevent redistribution of littoral sediments along the coast. Erosion is primarily caused by high wave and current energy combined with an inadequate supply of sediment. Erosion is responsible for higher local rates of land loss than submergence, and the erosion losses are more perceptible, especially after major storms when the greatest losses occur. The principal components of submergence are subsidence and the eustatic rise in sea level. Together these components are recorded by tide gauges as a relative rise in sea level. Submergence converts uplands to wetlands and wetlands to open water. These surficial changes occur mostly on the coastal plain but are also observed on barrier islands and bayhead deltas and within entrenched valleys. Although compactional subsidence is a natural process operating in the Gulf Coast basin, most of the accelerated land-surface subsidence in Texas is attributed to extraction of shallow ground water or production of hydrocarbons at moderate depths. Faults activated by the withdrawal of these fluids concentrate the subsidence near the fault planes. Coastal land losses caused by dredging are less than those caused by erosion and submergence, but they constitute a growing percentage of total land losses.

  10. Reduction of Risk in Exploration and Prospect Generation through a Multidisciplinary Basin-Analysis Program in the South-Central Mid-Continent Region

    SciTech Connect (OSTI)

    Banerjee, S.; Barker, C.; Fite, J.; George, S.; Guo, Genliang; Johnson, W.; Jordan, J., Szpakiewicz, M.; Person, M.; Reeves, T.K.; Safley, E.; Swenson, J.B.; Volk, L.; and Erickson, R.

    1999-04-02

    This report will discuss a series of regional studies that were undertaken within the South-Central Mid-Continent region of the U.S. Coverage is also provided about a series of innovative techniques that were used for this assessment.

  11. Hydrogeologic subdivision of the Wolfcamp series and Pennsylvanian system of eastern Texas Panhandle, north-central Texas, and southwestern Oklahoma

    SciTech Connect (OSTI)

    Kayal, R.R.; Kistner, D.J.; Kranes, R.; Verock, F.P.

    1987-03-01

    The Pennsylvanian-Wolfcamp section in the Palo Duro Basin includes brine aquifers that are considered to be the most important ground-water flow paths in the deep-basin system. This report is the fifth in a series providing summary documentation of studies that subdivide the section into hydrogeologic units based on their judged relative capacities for transmitting water. This report extends the hydrogeologic study area to the eastern Texas Panhandle, north-central Texas, and southwestern Oklahoma. It includes 37 counties in Texas and Oklahoma. Underground patterns of rock distribution are delineated from a hydrologic perspective and at a level of detail appropriate for numerical modeling of regional ground-water flow. Hydrogeologic units are defined and characterized so that appropriate porosity and permeability values can be assigned to each unit during construction of the numerical models (not part of this study), and so that modelers can combine units where necessary. In this study, hydrogeologic units have been defined as mappable, physically continuous rock bodies that function in bulk as water-transmitting or water-retarding units relative to adjacent rocks. Interpretations are made primarily from geophysical logs. Hydrologic characteristics are assessed on the basis of properties typically associated with certain lithologies (e.g., sandstones are more pervious than shales) and on the basis of gross variations in effective porosity (particularly in carbonate sequences). 44 refs., 32 figs., 1 tab.

  12. Depositional architecture of lacustrine-delta and fluvial systems of the Permian Epsilon and Toolachee Formations at Dullingari field, southeastern Cooper basin, south Australia

    SciTech Connect (OSTI)

    Ambrose, W.A.; Hamilton, D.S.; Holtz, M.H. )

    1996-01-01

    The Epsilon and Toolachee Formations record a transition from lacustrine deltas to fluvial depositional systems in the southeastern part of the Cooper Basin. Gas reservoirs in these formations occur mainly in narrow (typically less than 2 mi [3.2 km] wide) belts of distributary- and fluvial-channel sandstones in structurally high areas in Dullingari field and neighboring areas. In a study by the Bureau of Economic Geology and Santos to document distribution of Epsilon and Toolachee lithotacies, we mapped multiple depositional axes and projected them into undeveloped areas in the field. We performed a high-resolution sequence-stratigraphic study, defining four operational Epsilon subunits bounded by lacustrine mudstones recording periods of delta-platform abandonment and subsidence. In contrast, six genetic Toolachee subunits are bounded by regionally extensive coal seams recording pervasive sediment-supply shutoff and peat-swamp development over broad areas. Epsilon lacustrine deltas prograded northwestward over a muddy substrate on a broad, shallow basin floor. Distributary-channel axes, defined by narrow, northwest-trending belts of upward-fining sandstones less than 20 ft (6 m) thick, are projected across the field area. However, the younger Toolachee Formation contains northeast-trending sandstones in structural troughs, suggesting tectonic control on deposition. Detailed lithofacies maps of these formations provide a framework for assessing potential development targets at Dullingari field.

  13. Depositional architecture of lacustrine-delta and fluvial systems of the Permian Epsilon and Toolachee Formations at Dullingari field, southeastern Cooper basin, south Australia

    SciTech Connect (OSTI)

    Ambrose, W.A.; Hamilton, D.S.; Holtz, M.H.

    1996-12-31

    The Epsilon and Toolachee Formations record a transition from lacustrine deltas to fluvial depositional systems in the southeastern part of the Cooper Basin. Gas reservoirs in these formations occur mainly in narrow (typically less than 2 mi [3.2 km] wide) belts of distributary- and fluvial-channel sandstones in structurally high areas in Dullingari field and neighboring areas. In a study by the Bureau of Economic Geology and Santos to document distribution of Epsilon and Toolachee lithotacies, we mapped multiple depositional axes and projected them into undeveloped areas in the field. We performed a high-resolution sequence-stratigraphic study, defining four operational Epsilon subunits bounded by lacustrine mudstones recording periods of delta-platform abandonment and subsidence. In contrast, six genetic Toolachee subunits are bounded by regionally extensive coal seams recording pervasive sediment-supply shutoff and peat-swamp development over broad areas. Epsilon lacustrine deltas prograded northwestward over a muddy substrate on a broad, shallow basin floor. Distributary-channel axes, defined by narrow, northwest-trending belts of upward-fining sandstones less than 20 ft (6 m) thick, are projected across the field area. However, the younger Toolachee Formation contains northeast-trending sandstones in structural troughs, suggesting tectonic control on deposition. Detailed lithofacies maps of these formations provide a framework for assessing potential development targets at Dullingari field.

  14. Blast rips Texas LPG storage site

    SciTech Connect (OSTI)

    Not Available

    1992-04-13

    This paper reports that Seminole Pipeline Co. at presstime last week had planned to reopen its 775 mile liquefied petroleum gas pipeline in South Texas by Apr. 12 after a huge explosion devastated the area around a Seminole LPG storage salt dome near Brenham, Tex., forcing the pipeline shutdown. A large fire was still burning at the storage site at presstime last week. The blast - shortly after 7 a.m. Apr. 7 - occurred at a pipeline connecting the main Seminole line with the storage facility and caused shock waves felt 130 miles away. A 5 year old boy who lived in a trailer near Seminole's LPG storage dome was killed, and 20 persons were injured.

  15. EIS-0444: Texas Clean Energy Project (TCEP), Ector County, Texas

    Broader source: Energy.gov [DOE]

    DOE has prepared a draft Supplement Analysis to the Texas Clean Energy Project due to changes made to the project after the issuance of the record of decision. See the draft SA for more detailed information on these changes.

  16. EIS-0520: Texas LNG Project; Cameron County, Texas | Department...

    Energy Savers [EERE]

    proposal to construct and operate a natural gas liquefaction and export terminal at the Port of Brownsville Ship Channel in Cameron County, Texas. DOE, Office of Fossil Energy, has...

  17. National Uranium Resource Evaluation: Marfa Quadrangle, Texas

    SciTech Connect (OSTI)

    Henry, C D; Duex, T W; Wilbert, W P

    1982-09-01

    The uranium favorability of the Marfa 1/sup 0/ by 2/sup 0/ Quadrangle, Texas, was evaluated in accordance with criteria established for the National Uranium Resource Evaluation. Surface and subsurface studies, to a 1500 m (5000 ft) depth, and chemical, petrologic, hydrogeochemical, and airborne radiometric data were employed. The entire quadrangle is in the Basin and Range Province and is characterized by Tertiary silicic volcanic rocks overlying mainly Cretaceous carbonate rocks and sandstones. Strand-plain sandstones of the Upper Cretaceous San Carlos Formation and El Picacho Formation possess many favorable characteristics and are tentatively judged as favorable for sandstone-type deposits. The Tertiary Buckshot Ignimbrite contains uranium mineralization at the Mammoth Mine. This deposit may be an example of the hydroauthigenic class; alternatively, it may have formed by reduction of uranium-bearing ground water produced during diagenesis of tuffaceous sediments of the Vieja Group. Although the presence of the deposit indicates favorability, the uncertainty in the process that formed the mineralization makes delineation of a favorable environment or area difficult. The Allen intrusions are favorable for authigenic deposits. Basin fill in several bolsons possesses characteristics that suggest favorability but which are classified as unevaluated because of insufficient data. All Precambrian, Paleozoic, other Mesozoic, and other Cenozoic environments are unfavorable.

  18. Public Utility Commission of Texas | Open Energy Information

    Open Energy Info (EERE)

    Public Utility Commission of Texas Name: Public Utility Commission of Texas Address: 1701 N. Congress Avenue Place: Austin, Texas Zip: 78701 Year Founded: 1975 Website:...

  19. Texas's 21st congressional district: Energy Resources | Open...

    Open Energy Info (EERE)

    Companies in Texas's 21st congressional district Texas General Land Office Retrieved from "http:en.openei.orgwindex.php?titleTexas%27s21stcongressionaldistrict&oldid204390...

  20. Texas's 25th congressional district: Energy Resources | Open...

    Open Energy Info (EERE)

    Companies in Texas's 25th congressional district Texas General Land Office Retrieved from "http:en.openei.orgwindex.php?titleTexas%27s25thcongressionaldistrict&oldid204394...

  1. Sevin Rosen Funds (Texas - Dallas) | Open Energy Information

    Open Energy Info (EERE)

    Dallas) Jump to: navigation, search Name: Sevin Rosen Funds (Texas - Dallas) Address: 13455 Noel Road, Suite 1670 Place: Dallas, Texas Zip: 75240 Region: Texas Area Product:...

  2. Sevin Rosen Funds (Texas - Austin) | Open Energy Information

    Open Energy Info (EERE)

    Austin) Jump to: navigation, search Name: Sevin Rosen Funds (Texas - Austin) Address: 6300 Bridgepoint Parkway, Building 1, Suite 500 Place: Austin, Texas Zip: 78730 Region: Texas...

  3. Texas State Technical College Wind Farm | Open Energy Information

    Open Energy Info (EERE)

    In Service Owner Texas State Technical College Developer Texas State Technical College Energy Purchaser Texas State Technical College Location Sweetwater TX Coordinates...

  4. Midland County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Subtype B. Registered Energy Companies in Midland County, Texas Hilliard Energy Renovar Energy Corp Skyward Energy LLC Places in Midland County, Texas Midland, Texas Odessa,...

  5. Martin County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Subtype B. Registered Energy Companies in Martin County, Texas Hilliard Energy Renovar Energy Corp Skyward Energy LLC Places in Martin County, Texas Ackerly, Texas Midland,...

  6. Electricity Reliability Council of Texas | Open Energy Information

    Open Energy Info (EERE)

    Reliability Council of Texas Jump to: navigation, search Logo: Electricity Reliability Council of Texas Name: Electricity Reliability Council of Texas Abbreviation: ERCOT Address:...

  7. New Mexico Natural Gas Processed in Texas (Million Cubic Feet...

    Gasoline and Diesel Fuel Update (EIA)

    Texas (Million Cubic Feet) New Mexico Natural Gas Processed in Texas (Million Cubic Feet) ...2016 Next Release Date: 8312016 Referring Pages: Natural Gas Processed New Mexico-Texas

  8. Railroad Commission of Texas, Oil and Gas Division | Open Energy...

    Open Energy Info (EERE)

    Texas, Oil and Gas Division Jump to: navigation, search Name: Texas Railroad Commission, Oil and Gas Division Address: 1701 N. Congress Place: Texas Zip: 78711-2967 Website:...

  9. Topic A and B Awardee: Electric Reliability Council of Texas...

    Office of Environmental Management (EM)

    and B Awardee: Electric Reliability Council of Texas Topic A and B Awardee: Electric Reliability Council of Texas The Electric Reliability Council of Texas (ERCOT) manages the flow ...

  10. Texas Department of State Health Services - WIPP Program | Department...

    Office of Environmental Management (EM)

    Texas Department of State Health Services - WIPP Program Texas Department of State Health Services - WIPP Program PDF icon Texas Department of State Health Services - WIPP Program ...

  11. First Amendment to the Texas Programmatic Agreement | Department...

    Energy Savers [EERE]

    the Texas Programmatic Agreement First Amendment to the Texas Programmatic Agreement First Amendment to the Programmatic Agreement among the U.S. Department of Energy, the Texas ...

  12. Texas | National Nuclear Security Administration

    National Nuclear Security Administration (NNSA)

    Wind farm generating more renewable energy than expected for Pantex The Texas Panhandle has some of the world's best winds for creating renewable energy, and the Wind Farm at the ...

  13. Castro County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Number 4 Climate Zone Subtype B. Places in Castro County, Texas Dimmitt, Texas Hart, Texas Nazareth, Texas Retrieved from "http:en.openei.orgwindex.php?titleCastroCo...

  14. Terry County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    169-2006 Climate Zone Number 3 Climate Zone Subtype B. Places in Terry County, Texas Brownfield, Texas Meadow, Texas Wellman, Texas Retrieved from "http:en.openei.orgw...

  15. Concho County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Zone Number 3 Climate Zone Subtype B. Places in Concho County, Texas Eden, Texas Paint Rock, Texas Retrieved from "http:en.openei.orgwindex.php?titleConchoCounty,Texa...

  16. San Antonio, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    city in Bexar County and Comal County and Medina County, Texas. It falls under Texas's 20th congressional district and Texas's 21st congressional district and Texas's 23rd...

  17. Texas-New Mexico Power Co | Open Energy Information

    Open Energy Info (EERE)

    Texas-New Mexico Power Co Jump to: navigation, search Name: Texas-New Mexico Power Co Place: Texas Service Territory: Texas Website: www.tnmp.com Twitter: @TNMP Facebook: https:...

  18. EA-377 DC Energy Texas LLC | Department of Energy

    Energy Savers [EERE]

    7 DC Energy Texas LLC EA-377 DC Energy Texas LLC Order authorizing DC Energy Texas LLC to export electric energy to Mexico. PDF icon EA-377 DC Energy Texas LLC More Documents & ...

  19. RAPID/Overview/Geothermal/Exploration/Texas | Open Energy Information

    Open Energy Info (EERE)

    Texas < RAPID | Overview | Geothermal | Exploration(Redirected from RAPIDAtlasGeothermalExplorationTexas) Redirect page Jump to: navigation, search REDIRECT...

  20. Richmond, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Hide Map This article is a stub. You can help OpenEI by expanding it. Richmond is a city in Fort Bend County, Texas. It falls under Texas's 22nd congressional...

  1. Clint, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Clint is a town in El Paso County, Texas. It falls under Texas's 23rd congressional district.12 References...

  2. Vinton, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Vinton is a village in El Paso County, Texas. It falls under Texas's 16th congressional district.12 References...

  3. Socorro, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Socorro is a city in El Paso County, Texas. It falls under Texas's 16th congressional district.12 References...

  4. Anthony, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Anthony is a town in El Paso County, Texas. It falls under Texas's 16th congressional district.12 References...

  5. Seagoville, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    a stub. You can help OpenEI by expanding it. Seagoville is a city in Dallas County and Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  6. Combine, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    is a stub. You can help OpenEI by expanding it. Combine is a city in Dallas County and Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  7. Terrell, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Terrell is a city in Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  8. Mesquite, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    a stub. You can help OpenEI by expanding it. Mesquite is a city in Dallas County and Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  9. Mabank, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    a stub. You can help OpenEI by expanding it. Mabank is a town in Henderson County and Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  10. Rosser, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Rosser is a village in Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  11. Forney, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Forney is a city in Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  12. Cottonwood, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Cottonwood is a city in Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  13. Talty, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Talty is a town in Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  14. Crandall, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Crandall is a city in Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  15. Kemp, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Kemp is a town in Kaufman County, Texas. It falls under Texas's 5th congressional district.12 References...

  16. Tyler, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Tyler is a city in Smith County, Texas. It falls under Texas's 1st congressional district.12 Registered...

  17. Hydrogen Education in Texas | Department of Energy

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

    9_hitchcock.pdf (347.23 KB) More Documents & Publications Texas Recovery Act State Memo Texas Hydrogen Highway - Fuel Cell Hybrid Bus and Fueling Infrastructure Technology Showcase Clean Cities Education & Outreach Activities

  18. Texas GLO Coastal Forms | Open Energy Information

    Open Energy Info (EERE)

    Coastal Forms Jump to: navigation, search OpenEI Reference LibraryAdd to library Legal Document- OtherOther: Texas GLO Coastal FormsLegal Abstract The Texas General Land Office...

  19. Magnolia, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Magnolia is a city in Montgomery County, Texas. It falls under Texas's 8th congressional district.12 References...

  20. Stagecoach, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Stagecoach is a town in Montgomery County, Texas. It falls under Texas's 8th congressional district.12 References...

  1. Montgomery, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Hide Map This article is a stub. You can help OpenEI by expanding it. Montgomery is a city in Montgomery County, Texas. It falls under Texas's 8th congressional...

  2. Conroe, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Conroe is a city in Montgomery County, Texas. It falls under Texas's 8th congressional district.12 References...

  3. Willis, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Willis is a city in Montgomery County, Texas. It falls under Texas's 8th congressional district.12 References...

  4. Woodbranch, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Woodbranch is a city in Montgomery County, Texas. It falls under Texas's 8th congressional district.12 References...

  5. Splendora, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Splendora is a city in Montgomery County, Texas. It falls under Texas's 8th congressional district.12 References...

  6. Shenandoah, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Shenandoah is a city in Montgomery County, Texas. It falls under Texas's 8th congressional district.12 References...

  7. Ackerly, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Ackerly is a city in Dawson County and Martin County, Texas. It falls under Texas's 11st congressional...

  8. Katy, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    is a stub. You can help OpenEI by expanding it. Katy is a city in Fort Bend County and Harris County and Waller County, Texas. It falls under Texas's 14th congressional district...

  9. Waller, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Waller is a city in Harris County and Waller County, Texas. It falls under Texas's 10th congressional...

  10. Taylor, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Hide Map This article is a stub. You can help OpenEI by expanding it. Taylor is a city in Williamson County, Texas. It falls under Texas's 31st congressional...

  11. ,"Texas Heat Content of Natural Gas Consumed"

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

    Data for" ,"Data 1","Texas Heat Content of Natural Gas ...2016 6:34:00 AM" "Back to Contents","Data 1: Texas Heat Content of Natural Gas Consumed

  12. The WCI report and Texas Town Meeting

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

    WCI report and Texas Town Meeting * Chapter format to be defined in Texas * In parentheses are listed the the people proposed to take responsibility for each chapter. One of them ...

  13. Cyclotron Institute - Texas A&M

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

    Research", is now available. May 14, 2015 Texas A&M Physics Undergrad Finds Home in ... May 24th, 3:45 PM Professor Klaus Blaum >full listing< Cyclotron Institute Texas A&M ...

  14. Texas Offshore Natural Gas Plant Liquids Production Extracted in Texas

    Gasoline and Diesel Fuel Update (EIA)

    7 (Million Cubic Feet)

    Offshore Natural Gas Plant Liquids Production Extracted in Texas (Million Cubic Feet) Decade Year-0 Year-1 Year-2 Year-3 Year-4 Year-5 Year-6 Year-7 Year-8 Year-9 2010's 0 - = No Data Reported; -- = Not Applicable; NA = Not Available; W = Withheld to avoid disclosure of individual company data. Release Date: 08/31/2016 Next Release Date: 09/30/2016 Referring Pages: NGPL Production, Gaseous Equivalent Texas Offshore Natural Gas Plant Processing

  15. Texas Clean Energy Project | Department of Energy

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

    Texas Clean Energy Project Texas Clean Energy Project On March 12, 2010, DOE announced the award of a Cooperative Agreement to Summit Texas Clean Energy, LLC to construct the Texas Clean Energy Project (TCEP), an integrated gasification combined cycle (IGCC) poly-generation facility with fully integrated CO2 capture. Under Round 3 of the Clean Coal Power Initiative (CCPI), DOE is providing up to $450 million in financial assistance, including funding from the Recovery Act of 2009. Due to the

  16. Evaluation of solitary waves as a mechanism for oil transport in poroelastic media: A case study of the South Eugene Island field, Gulf of Mexico basin

    SciTech Connect (OSTI)

    Joshi, Ajit; Appold, Martin S.; Nunn, Jeffrey A.

    2012-11-01

    Hydrocarbons in shallow reservoirs of the Eugene Island 330 field in the Gulf of Mexico basin are thought to have migrated rapidly along low permeability sediments of the Red fault zone as discrete pressure pulses from source rocks at depths of about 4.5 km. The aim of this research was to evaluate the hypothesis that these pressure pulses represent solitary waves by investigating the mechanics of solitary wave formation and motion and wave oil transport capability. A two-dimensional numerical model of Eugene Island minibasin formation predicted overpressures at the hydrocarbon source depth to increase at an average rate of 30 Pa/yr, reaching 52 MPa by the present day and oil velocities of 1E?¢????12 m/yr, far too low for kilometer scale oil transport to fill shallow Plio-Pleistocene reservoirs within the 3.6 million year minibasin history. Calculations from a separate one-dimensional model that used the pressure generation rate from the two-dimensional model showed that solitary waves could only form and migrate within sediments that have very low permeabilities between 1E?¢????25 to 1E?¢????24 m2 and that are highly overpressured to 91-93% of lithostatic pressure. Solitary waves were found to have a maximum pore volume of 105 m3, to travel a maximum distance of 1-2 km, and to have a maximum velocity of 1E?¢????3 m/yr. Based on these results, solitary waves are unlikely to have transported oil to the shallowest reservoirs in the Eugene Island field in a poroelastic fault gouge rheology at the pressure generation rates likely to have been caused by disequilibrium compaction and hydrocarbon generation. However, solitary waves could perhaps be important agents for oil transport in other locations where reservoirs are closer to the source rocks, where the pore space is occupied by more than one fluid, or where sudden fracturing of overpressured hydrocarbon source sediments would allow the solitary waves to propagate as shock waves. Hydrocarbons

  17. Yates field, west Texas: Geology of a Permian basin giant

    SciTech Connect (OSTI)

    Heymans, M.J. ); Craig, D.H.

    1991-03-01

    Yates field, which produces oil largely from Late Permian San Andres dolomites, was discovered in 1926 and logged its billionth barrel in 1985. It is remarkable for the size of its original oil in place (four billion barrels estimated) and for its early ability to produce hundreds to thousands of barrels per hour from individual wells at depths of less than 2,000 ft. The high quality of the reservoir has been related to the following geologic characteristics: (1) a broad anticline with significant closure located at the apex of regional structure which formed a trap for large volumes of primary and secondary oil; (2) a vast integrated system of porosity (ranging from intergrain/intercrystal pores to joints, fractures, and small caves) that imparts high storage capacity and transmissivity to the reservoir dolomites; (3) a thick, efficient seal of anhydrite capping the reservoir sequence; and (4) high flowing pressures during much of the history of the field. The western area of the Yates field reservoir is dominated by peritidal to lagoonal mudstones and wackestones; the eastern area, by shallow subtidal packstones and grainstones. These depositional facies reflect both aggradation and eastward progradation of upper San Andres carbonates. Effective engineering management of the field has followed from a recognition of the quite different reservoir qualities in the two areas of the field and from adapting secondary and tertiary recovery techniques to constraints imposed by the geologic factors listed above.

  18. New tools attack Permian basin stimulation problems

    SciTech Connect (OSTI)

    Ely, J.W.; Schubarth, S.K.; Wolters, B.C.; Kromer, C. )

    1992-06-08

    This paper reports that profitable stimulation treatments in the Permian basin of the southwestern U.S. combine new tools with technology and fluids previously available. This paper reports that a wide selection of fracturing fluids and techniques needs to be considered to solve the varied problems associated with stimulating hydrocarbon reservoirs that are at diverse depths, temperatures, pressures, and lithologies. The Permian basin of West Texas and New Mexico is the most fertile ground in the U.S. for some of the newer stimulation technologies. In this basin, these new tools and techniques have been applied in many older producing areas that previously were treated with more conventional stimulation techniques, including acidizing and conventional fracturing procedures.

  19. Sequence stratigraphic analysis of the Lower Permian Hueco Group, northern Sierra Diablo, west Texas

    SciTech Connect (OSTI)

    Starcher, M.A. )

    1992-04-01

    The upper Wolfcamp Hueco Group in the northern Sierra Diablo of west Texas was deposited in a shelf setting on the western margin of the Delaware basin. This outcrop study subdivides the Hueco Group, including the Powwow Formation, into a sequence stratigraphic framework. Two depositional sequences and component system tracts within the Hueco have been defined on the basis of cycle stacking patterns and the recognition of unconformities. This study serves as a framework for cycle and sequence recognition in the remainder of the Delaware basin for the upper Wolfcamp.

  20. Delaware basin/Central basin platform margin: The development of a subthrust deep-gas province in the Permian Basin

    SciTech Connect (OSTI)

    Purves, W.J. ); Ting, S.C. )

    1990-05-01

    A deep-gas-prone province was identified along the Delaware basin/Central Basin platform margin, a margin conventionally interpreted to be bounded by high-angle normal or high-angle reverse structures. Redefinition of the tectonic style between the Delaware basin and the adjacent platform resulted in the identification of this Delaware basin/Central Basin platform subthrust province and a giant prospect within it. Definition of a giant-sized gas prospect in northern Pecos County, Texas, revealed that portions of this margin may be characterized by shingled, low-angle, eastward-dipping, basement involved thrust faults. Interpretations suggest that hidden, subthrust footwall structures may trend discontinuously for greater than 100 mi along this structural margin. Subthrust footwall structures formed as basinal buttress points for the Central Basin platform to climb over the Delaware basin. In this area, structural relief of over 19,000 ft over a 10-mi width is believed due to stacking of low-angle thrust sheets. Seismic resolution of this subthrust margin has been complexed by allochtonous hanging-wall gravity-glide blocks and folds and by velocity changes in overlying syn- and posttectonic sediments associated with basin-to-shelf lithofacies changes. Statistical studies indicate that this deep-gas province has a play potential of greater than 10 tcf of gas, with individual prospect sizes exceeding 1 tcfg. The prospects defined along this trend are deep (approximately 20,000 ft) subthrust structural traps that are indigenously sourced and reservoired by dual-matrix porosity. Vitrinite supported maturation modeling suggests that these subthrust structures formed prior to catagenic conversion of the oldest source rocks to oil and later to gas. Tectonically fractured Ordovician Ellenburger and Devonian sediments are considered the principal reservoirs. Shales overlying reservoir intervals form vertical seals.

  1. Ground-water in Texas

    SciTech Connect (OSTI)

    Ward-McLemore, E.

    1985-01-01

    Amount 61% of the water used by Texans is ground-water. Some areas, both municipal and rural, depend entirely on ground-water. In many areas long term withdrawal is lowering the water levels, causing surface land subsidence, salt-water encroachment, and reducing future reservoir availability. The increasing probability of seepage from radioactive and toxic wastes, herbicide residues, septic systems, and oilfield brines is threatening dangerous contamination of fresh ground-water reservoirs. The Texas Department of Water Resources, the Texas Department of Health, State and private colleges and universities, the US Geological Survey, the Environmental Protection Agency, various underground water districts, among others, are cooperating with concerned hydrologists in a concentrated program to increase the efficiency of ground-water use and development, preserve the aquifer reservoirs, and decrease the pollution potential. 88 references.

  2. Origin, distribution, and movement of brine in the Permian Basin (U. S. A. ). A model for displacement of connate brine

    SciTech Connect (OSTI)

    Bein, A.; Dutton, A.R. )

    1993-06-01

    Na-Cl, halite Ca-Cl, and gypsum Ca-Cl brines with salinities from 45 to >300 g/L are identified and mapped in four hydrostratigraphic units in the Permian Basin area beneath western Texas and Oklahoma and eastern New Mexico, providing spatial and lithologic constraints on the interpretation of the origin and movement of brine. Na-Cl brine is derived from meteoric water as young as 5-10 Ma that dissolved anhydrite and halite, whereas Ca-Cl brine is interpreted to be ancient, modified-connate Permian brine that now is mixing with, and being displaced by, the Na-Cl brine. Displacement fronts appear as broad mixing zones with no significant salinity gradients. Evolution of Ca-Cl brine composition from ideal evaporated sea water is attributed to dolomitization and syndepositional recycling of halite and bittern salts by intermittent influx of fresh water and sea water. Halite Ca-Cl brine in the evaporite section in the northern part of the basin differs from gypsum Ca-Cl brine in the south-central part in salinity and Na/Cl ratio and reflects segregation between halite- and gypsum-precipitating lagoons during the Permian. Ca-Cl brine moved downward through the evaporite section into the underlying Lower Permian and Pennsylvanian marine section that is now the deep-basin brine aquifer, mixing there with pre-existing sea water. Buoyancy-driven convection of brine dominated local flow for most of basin history, with regional advection governed by topographically related forces dominant only for the past 5 to 10 Ma. 71 refs., 11 figs.

  3. Energy Incentive Programs, Texas | Department of Energy

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

    Texas Energy Incentive Programs, Texas Updated September 2015 What public-purpose-funded energy efficiency programs are available in my state? The Public Utility Commission of Texas (PUCT) oversees a set of statewide "standard offer" and market transformation programs that are available to customers in each of the investor-owned utilities' service territories. The programs are funded through a systems benefits charge on transmission and distribution services and are administered by the

  4. McCulloch County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Climate Zone Number 3 Climate Zone Subtype B. Places in McCulloch County, Texas Brady, Texas Melvin, Texas Retrieved from "http:en.openei.orgwindex.php?titleMcCulloch...

  5. Delta County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    169-2006 Climate Zone Number 3 Climate Zone Subtype A. Places in Delta County, Texas Cooper, Texas Pecan Gap, Texas Retrieved from "http:en.openei.orgwindex.php?titleDeltaC...

  6. Sutton County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    169-2006 Climate Zone Number 3 Climate Zone Subtype B. Places in Sutton County, Texas Sonora, Texas Retrieved from "http:en.openei.orgwindex.php?titleSuttonCounty,Texas&old...

  7. Somervell County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Climate Zone Number 3 Climate Zone Subtype A. Places in Somervell County, Texas Glen Rose, Texas Retrieved from "http:en.openei.orgwindex.php?titleSomervellCounty,Texas&o...

  8. Deep East Texas Elec Coop Inc | Open Energy Information

    Open Energy Info (EERE)

    Deep East Texas Elec Coop Inc Jump to: navigation, search Name: Deep East Texas Elec Coop Inc Place: Texas Phone Number: 1-800-392-5986 Website: www.deepeast.com Facebook: https:...

  9. Horizon City, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    This article is a stub. You can help OpenEI by expanding it. Horizon City is a city in El Paso County, Texas. It falls under Texas's 16th congressional district and Texas's 23rd...

  10. Baylor County, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    169-2006 Climate Zone Number 3 Climate Zone Subtype B. Places in Baylor County, Texas Seymour, Texas Retrieved from "http:en.openei.orgwindex.php?titleBaylorCounty,Texas&ol...

  11. Heart of Texas Electric Coop | Open Energy Information

    Open Energy Info (EERE)

    of Texas Electric Coop Jump to: navigation, search Name: Heart of Texas Electric Coop Place: Texas Website: www.hotec.coop Twitter: @HOTECcoop Facebook: https:www.facebook.com...

  12. Missouri City, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    You can help OpenEI by expanding it. Missouri City is a city in Fort Bend County and Harris County, Texas. It falls under Texas's 9th congressional district and Texas's 22nd...

  13. League City, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    You can help OpenEI by expanding it. League City is a city in Galveston County and Harris County, Texas. It falls under Texas's 14th congressional district and Texas's 22nd...

  14. Texas Renewable Electric Power Industry Statistics

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

    Texas" "Primary Renewable Energy Capacity Source","Wind" "Primary Renewable Energy ... " Hydro Conventional",689,0.6 " Solar",14,"*" " Wind",9952,9.2 " WoodWood ...

  15. Hudson Energy Services (Texas) | Open Energy Information

    Open Energy Info (EERE)

    Energy Services Place: Texas Website: www.hudsonenergy.net Twitter: @HudsonEnergy Facebook: https:www.facebook.comHudsonEnergyServices Outage Hotline: 866-552-5551...

  16. Texas Instruments Incorporated | Open Energy Information

    Open Energy Info (EERE)

    Place: Texas Zip: 75243-4136 Sector: Solar Product: Manufactures devices for digital signal processing and analogue technologies, including a DCDC boost converter which could...

  17. ,"Texas Natural Gas LNG Storage Additions (MMcf)"

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

    Of Series","Frequency","Latest Data for" ,"Data 1","Texas Natural Gas LNG Storage Additions (MMcf)",1,"Annual",2014 ,"Release Date:","9302015" ,"Next Release...

  18. Lewisville, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    district.12 Registered Energy Companies in Lewisville, Texas Caprock Roofing Uranium Resources Inc URI References US Census Bureau Incorporated place and minor civil...

  19. Richardson, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Richardson, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 32.9481789, -96.7297205 Show Map Loading map... "minzoom":false,"mappingserv...

  20. ,"Texas Natural Gas Gross Withdrawals and Production"

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

    Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Texas Natural Gas Gross Withdrawals and Production",10,"Monthly","42016","01151989" ,"Release ...

  1. Irving, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    congressional district.12 Registered Energy Companies in Irving, Texas ExxonMobil Fluor Corp Shermco Industries Inc References US Census Bureau Incorporated place and...

  2. Adjusted Estimates of Texas Natural Gas Production

    Reports and Publications (EIA)

    2005-01-01

    The Energy Information Administration (EIA) is adjusting its estimates of natural gas production in Texas for 2004 and 2005 to correctly account for carbon dioxide (CO2) production.

  3. Grapevine, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Apps Datasets Community Login | Sign Up Search Page Edit with form History Grapevine, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates...

  4. Daniel Yates Advisor: Dr. Rogachev Texas...

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

    gas mixtures for active target detector application Daniel Yates Advisor: Dr. Rogachev Texas Active Target (TexAT) New active target detector under development by Rogachev...

  5. Plano, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Help Apps Datasets Community Login | Sign Up Search Page Edit with form History Plano, Texas: Energy Resources (Redirected from Plano, TX) Jump to: navigation, search Equivalent...

  6. Arlington, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Apps Datasets Community Login | Sign Up Search Page Edit with form History Arlington, Texas: Energy Resources (Redirected from Arlington, TX) Jump to: navigation, search...

  7. Frisco, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Help Apps Datasets Community Login | Sign Up Search Page Edit with form History Frisco, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates...

  8. ,"Texas Natural Gas Vehicle Fuel Consumption (MMcf)"

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

    ,"Worksheet Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Texas Natural Gas Vehicle Fuel Consumption (MMcf)",1,"Annual",2014 ,"Release Date:","930...

  9. Plano, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Help Apps Datasets Community Login | Sign Up Search Page Edit with form History Plano, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates...

  10. ,"Texas Natural Gas Lease Fuel Consumption (MMcf)"

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

    ,"Worksheet Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Texas Natural Gas Lease Fuel Consumption (MMcf)",1,"Annual",2014 ,"Release Date:","930...

  11. Carrollton, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Apps Datasets Community Login | Sign Up Search Page Edit with form History Carrollton, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates...

  12. ,"Texas Natural Gas Underground Storage Capacity (MMcf)"

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

    ,"Worksheet Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Texas Natural Gas Underground Storage Capacity (MMcf)",1,"Annual",2014 ,"Release Date:","9...

  13. Garland, Texas: Energy Resources | Open Energy Information

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    Apps Datasets Community Login | Sign Up Search Page Edit with form History Garland, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates...

  14. ,"Texas Natural Gas Processed (Million Cubic Feet)"

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

    ,"Worksheet Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Texas Natural Gas Processed (Million Cubic Feet)",1,"Annual",2014 ,"Release Date:","930...

  15. ,"Texas Natural Gas Input Supplemental Fuels (MMcf)"

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

    ,"Worksheet Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Texas Natural Gas Input Supplemental Fuels (MMcf)",1,"Annual",2014 ,"Release Date:","0930...

  16. ,"Texas Natural Gas Plant Fuel Consumption (MMcf)"

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

    ,"Worksheet Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Texas Natural Gas Plant Fuel Consumption (MMcf)",1,"Annual",2014 ,"Release Date:","930...

  17. Sheldon, Texas: Energy Resources | Open Energy Information

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    Sheldon, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 29.8680014, -95.1282643 Show Map Loading map... "minzoom":false,"mappingservice...

  18. ,"Texas Natural Gas Gross Withdrawals and Production"

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

    Name","Description"," Of Series","Frequency","Latest Data for" ,"Data 1","Texas Natural Gas Gross Withdrawals and Production",10,"Annual",2014,"06301967" ,"Release...

  19. Bellaire, Texas: Energy Resources | Open Energy Information

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    Bellaire, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 29.7057858, -95.4588299 Show Map Loading map... "minzoom":false,"mappingservic...

  20. Midland, Texas: Energy Resources | Open Energy Information

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    district.12 Registered Energy Companies in Midland, Texas Hilliard Energy Renovar Energy Corp Skyward Energy LLC References US Census Bureau Incorporated place and...

  1. Tessera Solar (Texas) | Open Energy Information

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    77002 Region: Texas Area Sector: Solar Product: Developer of utility scale solar power plants based on dish-Stirling engine designs Website: www.tesserasolar.com Coordinates:...

  2. Alamo, Texas: Energy Resources | Open Energy Information

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    Alamo, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 26.1836854, -98.1230638 Show Map Loading map... "minzoom":false,"mappingservice":...

  3. Hitchcock, Texas: Energy Resources | Open Energy Information

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    Hitchcock, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 29.3482905, -95.0160368 Show Map Loading map... "minzoom":false,"mappingservi...

  4. Texas Natural Resources Code | Open Energy Information

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    Resources CodeLegal Abstract This regulation governs the law pertaining to natural resources management in Texas. Published NA Year Signed or Took Effect 2014 Legal...

  5. Texas Railroad Commission - Pollution Discharge Regulations ...

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    Not Provided DOI Not Provided Check for DOI availability: http:crossref.org Online Internet link for Texas Railroad Commission - Pollution Discharge Regulations Citation...

  6. Jolly, Texas: Energy Resources | Open Energy Information

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    Jolly, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 33.8639877, -98.3494937 Show Map Loading map... "minzoom":false,"mappingservice":...

  7. Windthorst, Texas: Energy Resources | Open Energy Information

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    Windthorst, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 33.5762163, -98.4367186 Show Map Loading map... "minzoom":false,"mappingserv...

  8. Petrolia, Texas: Energy Resources | Open Energy Information

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    Petrolia, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 34.0131515, -98.2322669 Show Map Loading map... "minzoom":false,"mappingservic...

  9. Dean, Texas: Energy Resources | Open Energy Information

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    Dean, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 33.9503748, -98.34616 Show Map Loading map... "minzoom":false,"mappingservice":"go...

  10. Byers, Texas: Energy Resources | Open Energy Information

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    Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 34.0681503, -98.1905989 Show Map Loading map... "minzoom":false,"mappingservice":"google...

  11. Bellevue, Texas: Energy Resources | Open Energy Information

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    Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 33.6364933, -98.0139278 Show Map Loading map... "minzoom":false,"mappingservice":"google...

  12. Henrietta, Texas: Energy Resources | Open Energy Information

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    Henrietta, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 33.8173224, -98.1953221 Show Map Loading map... "minzoom":false,"mappingservi...

  13. Webster, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Webster, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 29.5377315, -95.1182645 Show Map Loading map... "minzoom":false,"mappingservice...

  14. Farwell, Texas: Energy Resources | Open Energy Information

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    Farwell, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 34.383409, -103.0380016 Show Map Loading map... "minzoom":false,"mappingservice...

  15. Dickinson, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Dickinson, Texas: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 29.4607876, -95.0513172 Show Map Loading map... "minzoom":false,"mappingservi...

  16. 2008 Texas State Energy Plan | Department of Energy

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

    8 Texas State Energy Plan 2008 Texas State Energy Plan 2008 Texas State Energy Plan. Governor's Competitiveness Council. July 2008 2008 Texas State Energy Plan (4.37 MB) More Documents & Publications Dispatchable Distributed Generation: Manufacturing's Role in Support of Grid Modernization, FEBRUARY 10-11 A Look Behind the Texas Renewable Portfolio Standard Impacts of Increasing Natural Gas Fueled CHP from 20 to 35 Percent of Total Electricity Production in Texas, April 2011

  17. Texas Offshore Pilot Research Project | Open Energy Information

    Open Energy Info (EERE)

    Offshore Pilot Research Project Jump to: navigation, search Name Texas Offshore Pilot Research Project Facility Texas Offshore Pilot Research Project Sector Wind energy Facility...

  18. File:Texas Construction General Permit (TXR150000).pdf | Open...

    Open Energy Info (EERE)

    Texas Construction General Permit (TXR150000).pdf Jump to: navigation, search File File history File usage Metadata File:Texas Construction General Permit (TXR150000).pdf Size of...

  19. Texas Large Construction Site Notice for Secondary Operators...

    Open Energy Info (EERE)

    navigation, search OpenEI Reference LibraryAdd to library Reference: Texas Large Construction Site Notice for Secondary Operators Published Texas Commission on Environmental...

  20. Texas Large Construction Site Notice for Primary Operators |...

    Open Energy Info (EERE)

    navigation, search OpenEI Reference LibraryAdd to library Reference: Texas Large Construction Site Notice for Primary Operators Published Texas Commission on Environmental...

  1. Texas Small Construction Site Notice | Open Energy Information

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    Small Construction Site Notice Jump to: navigation, search OpenEI Reference LibraryAdd to library Reference: Texas Small Construction Site Notice Published Texas Commission on...

  2. Texas's 17th congressional district: Energy Resources | Open...

    Open Energy Info (EERE)

    Institutions in Texas's 17th congressional district Baylor University - Renewable Aviation Fuels Development Center Registered Energy Companies in Texas's 17th congressional...

  3. Texas Department of Motor Vehicles | Open Energy Information

    Open Energy Info (EERE)

    Vehicles Name: Texas Department of Motor Vehicles Abbreviation: TxDMV Address: 4000 Jackson Ave. Place: Austin, Texas Zip: 78731 Phone Number: 1-888-368-4689 Website:...

  4. Texas's 19th congressional district: Energy Resources | Open...

    Open Energy Info (EERE)

    district in Texas. Registered Energy Companies in Texas's 19th congressional district Big Daddy s Biodiesel Inc Cratech Inc Horn Wind Lauren Engineers amp Constructors Levelland...

  5. TCEQ - Texas Nonpoint Source Management Program Manual | Open...

    Open Energy Info (EERE)

    Texas Nonpoint Source Management Program Manual Jump to: navigation, search OpenEI Reference LibraryAdd to library PermittingRegulatory Guidance - GuideHandbook: TCEQ - Texas...

  6. Overcoming Multifamily Sector Barriers in Austin, Texas | Department...

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

    Overcoming Multifamily Sector Barriers in Austin, Texas Overcoming Multifamily Sector Barriers in Austin, Texas Presents techniques on overcoming the barriers of multifamily energy...

  7. Texas's 12th congressional district: Energy Resources | Open...

    Open Energy Info (EERE)

    You can help OpenEI by expanding it. This page represents a congressional district in Texas. Registered Energy Companies in Texas's 12th congressional district Aecom Government...

  8. Clean Cities: Lone Star Clean Fuels Alliance (Central Texas)...

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

    Lone Star Clean Fuels Alliance (Central Texas) Coalition The Lone Star Clean Fuels Alliance (Central Texas) coalition works with vehicle fleets, fuel providers, community leaders,...

  9. City of Hallettsville, Texas (Utility Company) | Open Energy...

    Open Energy Info (EERE)

    Hallettsville, Texas (Utility Company) Jump to: navigation, search Name: City of Hallettsville Place: Texas Phone Number: (361) 798-3681 Website: www.cityofhallettsville.orgut...

  10. City of Sanger, Texas (Utility Company) | Open Energy Information

    Open Energy Info (EERE)

    Texas (Utility Company) Jump to: navigation, search Name: City of Sanger Place: Texas Website: sangertexas.org?pageid289 Twitter: @cityofsanger Facebook: https:...

  11. City of Greenville,, Texas (Utility Company) | Open Energy Information

    Open Energy Info (EERE)

    Greenville,, Texas (Utility Company) Jump to: navigation, search Name: Greenville, City of Place: Texas Website: www.geus.org Twitter: @GEUSsocialmedia Facebook: https:...

  12. Texas's 1st congressional district: Energy Resources | Open Energy...

    Open Energy Info (EERE)

    Energy Companies in Texas's 1st congressional district Eisenbach Consulting NM Invest Retrieved from "http:en.openei.orgwindex.php?titleTexas%27s1stcongressionaldis...

  13. City of Gonzales, Texas (Utility Company) | Open Energy Information

    Open Energy Info (EERE)

    Gonzales, Texas (Utility Company) Jump to: navigation, search Name: City of Gonzales Place: Texas Phone Number: (830) 672-2815 Website: www.cityofgonzales.orgDepartm Outage...

  14. Texas's 6th congressional district: Energy Resources | Open Energy...

    Open Energy Info (EERE)

    by expanding it. This page represents a congressional district in Texas. Registered Energy Companies in Texas's 6th congressional district Corsicana Chemical Company Demilec...

  15. Texas Petroleum Storage Tanks Webpage | Open Energy Information

    Open Energy Info (EERE)

    Petroleum Storage Tanks Webpage Jump to: navigation, search OpenEI Reference LibraryAdd to library Web Site: Texas Petroleum Storage Tanks Webpage Author Texas Commission on...

  16. RAPID/BulkTransmission/Texas | Open Energy Information

    Open Energy Info (EERE)

    information about BulkTransmission in Texas. Use the Edit with form button to editupdate. Planning Organizations not provided Texas Owners not provided Current Projects not...

  17. EIS-0501: Golden Pass LNG Export and Pipeline Project, Texas...

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

    1: Golden Pass LNG Export and Pipeline Project, Texas and Louisiana EIS-0501: Golden Pass LNG Export and Pipeline Project, Texas and Louisiana Summary The Federal Energy Regulatory ...

  18. City of Georgetown, Texas (Utility Company) | Open Energy Information

    Open Energy Info (EERE)

    Georgetown, Texas (Utility Company) Jump to: navigation, search Name: Georgetown City of Place: Texas Website: electric.georgetown.org Twitter: @georgetowntx Facebook: https:...

  19. Spotlight on Austin, Texas: Best Offer Ever Produces 564 Upgrades...

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

    Spotlight on Austin, Texas: Best Offer Ever Produces 564 Upgrades in Record Time Spotlight on Austin, Texas: Best Offer Ever Produces 564 Upgrades in Record Time This Better ...

  20. Spotlight on Austin, Texas: Best Offer Ever Produces Upgrades...

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

    Best Offer Ever Produces Upgrades in Record Time Spotlight on Austin, Texas: Best Offer Ever Produces Upgrades in Record Time Spotlight on Austin, Texas: Best Offer Ever Produces ...

  1. Houston, Texas: Solar in Action (Brochure), Solar America Cities...

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

    Houston, Texas: Solar in Action (Brochure), Solar America Cities, Energy Efficiency & Renewable Energy (EERE) Houston, Texas: Solar in Action (Brochure), Solar America Cities, ...

  2. Electricity Reliability Council of Texas (ERCOT) | Open Energy...

    Open Energy Info (EERE)

    Electricity Reliability Council of Texas (ERCOT) Jump to: navigation, search The Electric Reliability Council of Texas (ERCOT) manages the flow of electric power to 22 million...

  3. Texas A&M (OTRC) | Open Energy Information

    Open Energy Info (EERE)

    Texas A&M (OTRC) Jump to: navigation, search Hydro | Hydrodynamic Testing Facilities Name Texas A&M (OTRC) Address Offshore Technology Research Center, 1200 Mariner Drive Place...

  4. City of Floydada, Texas (Utility Company) | Open Energy Information

    Open Energy Info (EERE)

    Name: City of Floydada Place: Texas Phone Number: (806) 983-2834 Facebook: https:www.facebook.compagesFloydada-Texas103874716318301 Outage Hotline: (806) 983-2834...

  5. Texas Renewable Energy Industries Association | Open Energy Informatio...

    Open Energy Info (EERE)

    Renewable Energy Industries Association Jump to: navigation, search Logo: Texas Renewable Energy Industries Association Name: Texas Renewable Energy Industries Association Address:...

  6. Texas CO2 Capture Demonstration Project Hits Three Million Metric...

    Office of Environmental Management (EM)

    Texas CO2 Capture Demonstration Project Hits Three Million Metric Ton Milestone Texas CO2 Capture Demonstration Project Hits Three Million Metric Ton Milestone June 30, 2016 - ...

  7. Texas Surface Water Quality Standards Webpage | Open Energy Informatio...

    Open Energy Info (EERE)

    Not Provided DOI Not Provided Check for DOI availability: http:crossref.org Online Internet link for Texas Surface Water Quality Standards Webpage Citation Texas Commission on...

  8. Federal Offshore--Texas Natural Gas Marketed Production (Million...

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

    Marketed Production (Million Cubic Feet) Federal Offshore--Texas Natural Gas Marketed ... Referring Pages: Natural Gas Marketed Production Federal Offshore Texas Natural Gas Gross ...

  9. ,"Texas--State Offshore Natural Gas Gross Withdrawals (MMcf)...

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

    Data for" ,"Data 1","Texas--State Offshore Natural Gas Gross Withdrawals ... "Back to Contents","Data 1: Texas--State Offshore Natural Gas Gross Withdrawals (MMcf)" ...

  10. ,"Federal Offshore--Texas Natural Gas Liquids Lease Condensate...

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

    Data for" ,"Data 1","Federal Offshore--Texas Natural Gas Liquids Lease ... AM" "Back to Contents","Data 1: Federal Offshore--Texas Natural Gas Liquids Lease ...

  11. ,"Texas--State Offshore Crude Oil Reserves in Nonproducing Reservoirs...

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

    Data for" ,"Data 1","Texas--State Offshore Crude Oil Reserves in Nonproducing ... "Back to Contents","Data 1: Texas--State Offshore Crude Oil Reserves in Nonproducing ...

  12. ,"Texas (with State Offshore) Coalbed Methane Proved Reserves...

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

    Data for" ,"Data 1","Texas (with State Offshore) Coalbed Methane Proved Reserves ... to Contents","Data 1: Texas (with State Offshore) Coalbed Methane Proved Reserves ...

  13. ,"Federal Offshore--Texas Natural Gas Gross Withdrawals (MMcf...

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

    Data for" ,"Data 1","Federal Offshore--Texas Natural Gas Gross Withdrawals ... AM" "Back to Contents","Data 1: Federal Offshore--Texas Natural Gas Gross Withdrawals ...

  14. ,"Texas--State Offshore Natural Gas Marketed Production (MMcf...

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

    Data for" ,"Data 1","Texas--State Offshore Natural Gas Marketed Production ... "Back to Contents","Data 1: Texas--State Offshore Natural Gas Marketed Production (MMcf)" ...

  15. ,"Texas--State Offshore Natural Gas Liquids Lease Condensate...

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

    Data for" ,"Data 1","Texas--State Offshore Natural Gas Liquids Lease Condensate, ... "Back to Contents","Data 1: Texas--State Offshore Natural Gas Liquids Lease Condensate, ...

  16. ,"Texas State Offshore Crude Oil + Lease Condensate Proved Reserves...

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

    Data for" ,"Data 1","Texas State Offshore Crude Oil + Lease Condensate Proved ... "Back to Contents","Data 1: Texas State Offshore Crude Oil + Lease Condensate Proved ...

  17. ,"Federal Offshore--Texas Coalbed Methane Proved Reserves (Billion...

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

    Data for" ,"Data 1","Federal Offshore--Texas Coalbed Methane Proved Reserves ... AM" "Back to Contents","Data 1: Federal Offshore--Texas Coalbed Methane Proved Reserves ...

  18. ,"Texas State Offshore Natural Gas, Wet After Lease Separation...

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

    Data for" ,"Data 1","Texas State Offshore Natural Gas, Wet After Lease Separation ... "Back to Contents","Data 1: Texas State Offshore Natural Gas, Wet After Lease Separation ...

  19. ,"Texas (with State Offshore) Natural Gas Plant Liquids, Expected...

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

    Data for" ,"Data 1","Texas (with State Offshore) Natural Gas Plant Liquids, Expected ... to Contents","Data 1: Texas (with State Offshore) Natural Gas Plant Liquids, Expected ...

  20. ,"Texas (with State Offshore) Shale Proved Reserves (Billion...

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

    Data for" ,"Data 1","Texas (with State Offshore) Shale Proved Reserves (Billion Cubic ... to Contents","Data 1: Texas (with State Offshore) Shale Proved Reserves (Billion Cubic ...

  1. Texas--State Offshore Natural Gas Marketed Production (Million...

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

    Marketed Production (Million Cubic Feet) Texas--State Offshore Natural Gas Marketed ... Referring Pages: Natural Gas Marketed Production Texas State Offshore Natural Gas Gross ...

  2. Federal Offshore--Texas Natural Gas Liquids Lease Condensate...

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

    Liquids Lease Condensate, Proved Reserves (Million Barrels) Federal Offshore--Texas ... Lease Condensate Proved Reserves as of Dec. 31 Federal Offshore, Gulf of Mexico, Texas ...

  3. ,"Texas State Offshore Dry Natural Gas Expected Future Production...

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

    Data for" ,"Data 1","Texas State Offshore Dry Natural Gas Expected Future ... "Back to Contents","Data 1: Texas State Offshore Dry Natural Gas Expected Future ...

  4. ,"Texas--State Offshore Shale Proved Reserves (Billion Cubic...

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

    Data for" ,"Data 1","Texas--State Offshore Shale Proved Reserves (Billion Cubic ... "Back to Contents","Data 1: Texas--State Offshore Shale Proved Reserves (Billion Cubic ...

  5. ,"Texas (with State Offshore) Natural Gas Liquids Lease Condensate...

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

    Data for" ,"Data 1","Texas (with State Offshore) Natural Gas Liquids Lease Condensate, ... to Contents","Data 1: Texas (with State Offshore) Natural Gas Liquids Lease Condensate, ...

  6. ,"Federal Offshore--Texas Natural Gas Marketed Production (MMcf...

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

    Data for" ,"Data 1","Federal Offshore--Texas Natural Gas Marketed Production ... AM" "Back to Contents","Data 1: Federal Offshore--Texas Natural Gas Marketed Production ...

  7. ,"Texas State Offshore Nonassociated Natural Gas, Wet After Lease...

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

    Data for" ,"Data 1","Texas State Offshore Nonassociated Natural Gas, Wet After ... "Back to Contents","Data 1: Texas State Offshore Nonassociated Natural Gas, Wet After ...

  8. ,"Texas State Offshore Associated-Dissolved Natural Gas, Wet...

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

    Data for" ,"Data 1","Texas State Offshore Associated-Dissolved Natural Gas, Wet ... "Back to Contents","Data 1: Texas State Offshore Associated-Dissolved Natural Gas, Wet ...

  9. ,"Texas--State Offshore Coalbed Methane Proved Reserves (Billion...

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

    Data for" ,"Data 1","Texas--State Offshore Coalbed Methane Proved Reserves (Billion ... "Back to Contents","Data 1: Texas--State Offshore Coalbed Methane Proved Reserves (Billion ...

  10. Texas Recovery Act State Memo | Department of Energy

    Energy Savers [EERE]

    Texas Recovery Act State Memo Texas has substantial natural resources, including oil, gas, solar, biomass, and wind power. The American Recovery & Reinvestment Act (ARRA) is making ...

  11. Preliminary Analysis of Texas Instrument Hercules Flash-based...

    Office of Scientific and Technical Information (OSTI)

    Technical Report: Preliminary Analysis of Texas Instrument Hercules Flash-based Microcontroller Citation Details In-Document Search Title: Preliminary Analysis of Texas Instrument ...

  12. Gulf of Mexico Federal Offshore - Texas Crude Oil + Lease Condensate...

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

    Gulf of Mexico Federal Offshore - Texas Crude Oil + Lease Condensate Proved Reserves ... as of Dec. 31 Federal Offshore, Gulf of Mexico, Texas Crude Oil plus Lease Condensate ...

  13. ,"Gulf of Mexico Federal Offshore - Texas Nonassociated Natural...

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

    Data for" ,"Data 1","Gulf of Mexico Federal Offshore - Texas Nonassociated ... AM" "Back to Contents","Data 1: Gulf of Mexico Federal Offshore - Texas Nonassociated ...

  14. ,"Gulf of Mexico Federal Offshore - Texas Associated-Dissolved...

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

    Data for" ,"Data 1","Gulf of Mexico Federal Offshore - Texas ... AM" "Back to Contents","Data 1: Gulf of Mexico Federal Offshore - Texas ...

  15. Gulf of Mexico Federal Offshore - Texas Nonassociated Natural...

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

    Gulf of Mexico Federal Offshore - Texas Nonassociated Natural Gas, Wet After Lease ... as of Dec. 31 Federal Offshore, Gulf of Mexico, Texas Nonassociated Natural Gas Proved ...

  16. San Antonio, Texas Data Dashboard | Department of Energy

    Energy Savers [EERE]

    Data Dashboard San Antonio, Texas Data Dashboard The data dashboard for San Antonio, Texas, a partner in the Better Buildings Neighborhood Program. San Antonio Data Dashboard ...

  17. ,"Texas - RRC District 3 Onshore Associated-Dissolved Natural...

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

    Data for" ,"Data 1","Texas - RRC District 3 Onshore ... 7:20:49 AM" "Back to Contents","Data 1: Texas - RRC District 3 Onshore ...

  18. ,"Texas - RRC District 8 Nonassociated Natural Gas, Wet After...

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

    Data for" ,"Data 1","Texas - RRC District 8 Nonassociated Natural ... 7:20:00 AM" "Back to Contents","Data 1: Texas - RRC District 8 Nonassociated Natural ...

  19. ,"Texas - RRC District 10 Nonassociated Natural Gas, Wet After...

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    Data for" ,"Data 1","Texas - RRC District 10 Nonassociated Natural ... 7:20:00 AM" "Back to Contents","Data 1: Texas - RRC District 10 Nonassociated Natural ...

  20. ,"Texas - RRC District 4 Onshore Nonassociated Natural Gas, Wet...

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

    Data for" ,"Data 1","Texas - RRC District 4 Onshore Nonassociated ... 7:20:00 AM" "Back to Contents","Data 1: Texas - RRC District 4 Onshore Nonassociated ...

  1. ,"Texas - RRC District 2 Onshore Associated-Dissolved Natural...

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

    Data for" ,"Data 1","Texas - RRC District 2 Onshore ... 7:20:49 AM" "Back to Contents","Data 1: Texas - RRC District 2 Onshore ...

  2. Microsoft Word - 07 Texas Water Plan.doc

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

    monthly regional meetings * TWAA (Texas Water Allocation Assessment) * www.swf.usace.army.mil ("(at bottom) Additional Related Material", "Texas Water Allocation Assessment ...

  3. San Antonio, Texas: Solar in Action (Brochure), Solar America...

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

    Antonio, Texas: Solar in Action (Brochure), Solar America Cities, Energy Efficiency & Renewable Energy (EERE) San Antonio, Texas: Solar in Action (Brochure), Solar America Cities, ...

  4. ,"Texas - RRC District 4 Onshore Associated-Dissolved Natural...

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

    Data for" ,"Data 1","Texas - RRC District 4 Onshore ... 7:20:50 AM" "Back to Contents","Data 1: Texas - RRC District 4 Onshore ...

  5. ,"Texas - RRC District 5 Nonassociated Natural Gas, Wet After...

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

    Data for" ,"Data 1","Texas - RRC District 5 Nonassociated Natural ... 7:20:00 AM" "Back to Contents","Data 1: Texas - RRC District 5 Nonassociated Natural ...

  6. ,"Texas - RRC District 9 Nonassociated Natural Gas, Wet After...

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

    Data for" ,"Data 1","Texas - RRC District 9 Nonassociated Natural ... 7:20:00 AM" "Back to Contents","Data 1: Texas - RRC District 9 Nonassociated Natural ...

  7. ,"Texas - RRC District 2 Onshore Nonassociated Natural Gas, Wet...

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

    Data for" ,"Data 1","Texas - RRC District 2 Onshore Nonassociated ... 7:19:59 AM" "Back to Contents","Data 1: Texas - RRC District 2 Onshore Nonassociated ...

  8. ,"Texas - RRC District 1 Nonassociated Natural Gas, Wet After...

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

    Data for" ,"Data 1","Texas - RRC District 1 Nonassociated Natural ... 7:19:59 AM" "Back to Contents","Data 1: Texas - RRC District 1 Nonassociated Natural ...

  9. Texas A&M University | Princeton Plasma Physics Lab

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

    Texas A&M University Texas A&M University Professor David Staack Dr. Yevgeny Raitses collaborates with Professor David Staack of TAMU Mechanical Engineering Department on ...

  10. ,"Texas - RRC District 3 Onshore Nonassociated Natural Gas, Wet...

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

    Data for" ,"Data 1","Texas - RRC District 3 Onshore Nonassociated ... 7:19:59 AM" "Back to Contents","Data 1: Texas - RRC District 3 Onshore Nonassociated ...

  11. ,"Texas Natural Gas Gross Withdrawals Total Offshore (MMcf)"

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

    Data for" ,"Data 1","Texas Natural Gas Gross Withdrawals Total ... 7:03:02 AM" "Back to Contents","Data 1: Texas Natural Gas Gross Withdrawals Total ...

  12. ,"Texas - RRC District 6 Nonassociated Natural Gas, Wet After...

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    Data for" ,"Data 1","Texas - RRC District 6 Nonassociated Natural ... 7:20:00 AM" "Back to Contents","Data 1: Texas - RRC District 6 Nonassociated Natural ...

  13. EIS-0518: Annova LNG Brownsville Project; Cameron County, Texas...

    Office of Environmental Management (EM)

    18: Annova LNG Brownsville Project; Cameron County, Texas EIS-0518: Annova LNG Brownsville Project; Cameron County, Texas Summary The Federal Energy Regulatory Commission (FERC) ...

  14. EIS-0501: Golden Pass LNG Export Project; Texas and Louisiana...

    Office of Environmental Management (EM)

    1: Golden Pass LNG Export Project; Texas and Louisiana EIS-0501: Golden Pass LNG Export Project; Texas and Louisiana Summary The Federal Energy Regulatory Commission (FERC) is ...

  15. Green Button Sample from Texas | Department of Energy

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

    from Texas Green Button Sample from Texas These files contain sample Green Button data ... FY 2014 Funding History Detail Spreadsheet NREL's Clean Energy Policy Analyses Project: ...

  16. The petroleum geology of the sub-Andean basins

    SciTech Connect (OSTI)

    Mathalone, J.M.P.

    1996-08-01

    The sub-Andean trend of basins spans the entire length of South America from Venezuela in the north to Argentina in the south. All the basins produce hydrocarbons with the exception of the Argentinean Bolsones complex and the Peruvian Madro de Dios which is prospective but virtually unexplored. There have been some 119 billion barrels of oil and 190 TCF of gas discovered to date, comprising 93% of the continent`s oil reserves. The basins lie immediately east of the Andes mountain range and are mainly asymmetric Upper Tertiary, westerly dipping foreland basins that overlie a series of earlier Tertiary, Mesozoic and Paleozoic depocentres. All the basins have been compressively deformed as recently as the Upper Miocene, by the eastwards growth of the Andean Cordillera. Giant oil and gas fields sourced from shales of varying age, have been found along the whole trend of basins, with a predominance of gas in the south. The rich marine Upper Cretaceous La Luna and equivalent shales of Venezuela, Colombia and Ecuador have been responsible for generating 86% of the hydrocarbons discovered to date in the sub-Andean basins. Proven sources include Devonian, Carboniferous, Permian and Triassic shales in the central area, comprising Peru, Bolivia and northern Argentina. In southern Argentina, oils have been sourced from Uppermost Jurassic and Lower Cretaceous marine and lacustrine shales. Over 7500 wildcat wells have been drilled in basins along the trend, with a 15% success rate. Many of the basins are very lightly explored, with considerable potential for future discoveries.

  17. South Atlantic summary report

    SciTech Connect (OSTI)

    Havran, K.J.; Wiese, J.D.

    1983-12-01

    To date, four Federal offshore oil-and-gas leasing actions have occurred in the South Atlantic Region. Two additional South Atlantic lease offerings remain on the July 1982 final 5-year OCS oil-and-gas leasing schedule before June 1987. The South Atlantic Region consists of three major sedimentary basins: the Carolina Trough, the Blake Plateau, and the Southeast Georgia Embayment. Lease Sale 43, the first in the South Atlantic Region, featured blocks for exploration in the Southeast Georgia Embayment. Offshore operators drilled a total of six exploratory wells on blocks leased in Lease Sale 43. All were dry. The 43 leases from Lease Sale 43 have now expired, some blocks were relinquished earlier by their lease-holders. In the recent Lease Sales 56 and RS-2, and in the South Atlantic Lease Offering (July 1983), blocks leased were largely concentrated in the Carolina Trough Basin. Exploration of these blocks may begin anew in early 1984. The blocks are in deep water and will require careful, long-range planning before drilling can commence. As of July 1983, all 66 leases from the above three sales are active. Two plans of exploration have been approved by Minerals Management Service for exploration on blocks leased in Lease Sale 56. The plans are for Russell Area, Blocks 709 and 710, and Manteo Area, Block 510. Blocks 709 and 710 are held by ARCO, and Block 510 is held by Chevron. Based on current plans of exploration, operations will begin in 1984, first by Chevron, and sometime later by ARCO. Operations will be supported by a temporary service base to be established at Morehead City, North Carolina. 6 references, 4 figures.

  18. Texas Solar Collaboration Action Plan

    SciTech Connect (OSTI)

    Winland, Chris

    2013-02-14

    Texas Solar Collaboration Permitting and Interconenction Process Improvement Action Plan. San Antonio-specific; Investigate feasibility of using electronic signatures; Investigate feasibility of enabling other online permitting processes (e.g., commercial); Assess need for future document management and workflow/notification IT improvements; Update Information Bulletin 153 regarding City requirements and processes for PV; Educate contractors and public on CPS Energy’s new 2013 solar program processes; Continue to discuss “downtown grid” interconnection issues and identify potential solutions; Consider renaming Distributed Energy Resources (DER); and Continue to participate in collaborative actions.

  19. MASK basin

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

    MASK basin - Sandia Energy Energy Search Icon Sandia Home Locations Contact Us Employee Locator Energy & Climate Secure & Sustainable Energy Future Stationary Power Energy Conversion Efficiency Solar Energy Wind Energy Water Power Supercritical CO2 Geothermal Natural Gas Safety, Security & Resilience of the Energy Infrastructure Energy Storage Nuclear Power & Engineering Grid Modernization Battery Testing Nuclear Energy Defense Waste Management Programs Advanced Nuclear Energy

  20. South Carolina - Compare - U.S. Energy Information Administration (EIA)

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

    South Carolina South Carolina

  1. South Carolina - Rankings - U.S. Energy Information Administration (EIA)

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

    South Carolina South Carolina

  2. South Carolina - Search - U.S. Energy Information Administration (EIA)

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

    South Carolina South Carolina

  3. Oil and gas developments in west Texas and eastern New Mexico in 1983

    SciTech Connect (OSTI)

    Adams, D.R.; Collier, W.W.; Gail, G.J.; Gaines, G.B.; Gibson, W.R.; Miller, H.A. Jr.; Pause, P.H.; Robbins, L.D.

    1984-10-01

    7034 wells were drilled in west Texas and eastern New Mexico in 1983, 17.2% less than in 1982. The success rate for all wells was 79.8% up 1.1% from 1982. The exploratory success rate decreased to 25.4% in 1983 from 26.4% in 1982. The number of exploratory wells drilled in 1983 decreased 27.1% from 1982, and total exploratory footage decreased 30.1%. The severe decline in exploratory drilling during 1983 was anticipated because seismic crew activity had declined during the 2 preceding years. However, 1983 seismic activity increased 2.1% from 1982, reversing the trend. Therefore, because seismic crew activity is usually a reliable leading indicator of trends in exploratory drilling, an increase in Permian basin wildcat drilling is predicted for mid-1985. In 1983, the number of development wells drilled decreased 15.2% from 1982, and total development footage decreased 17.6%. Development success increased by 0.1% to 89.2%. Oil production for 1983 was 550,473,920 bbl, down 1.7% from 1982. Gas production was 1,995,555,963 mcf, down 9.5% from 1982. Overall leasing activity decreased in 1983. The land sales of New Mexico and the University of Texas received only a fraction of the attention normally paid to them. However, leasing was very aggressive in Glasscock, Midland, and Hockley Counties, Texas, of the Midland basin. 6 figures, 3 tables.

  4. Structure and tectonics of the South Caspian Sea

    SciTech Connect (OSTI)

    Aliev, M.; Ozbey, T.

    1995-08-01

    The South Caspian Basin is a large Alpine intermontane trough located between Azerbaijan and Western Turkmenistan in the South Caspian Sea. It is about 500 km by 300 km in size. The sedimentary section ranges from 10-15 km thickness near the basin edges and reaches has more than 20 km in the deepest part of the basin. All of the known hydrocarbon production is from the Pliocene-Quaternary section. Characteristic features of the South Caspian Basin include: (1) The enormous thickness of the sedimentary sections; (2) Thick, terrigenous Middle Pliocene sediments deposited under conditions of markedly contrasting tectonic movements-rapid sinking of the basin and growth of the surrounding mountain structures; (3) Extensive development of diapirism and mud volcanism and their geostructural association mainly with the marginal zone of the basin; (4) The block nature of the crystalline basement; and (5) The close relationship of the western part of the South Caspian to the Kura Depression. Individual structures can reach 35 kilometers in length with up to 3000 meters of closure. Structures are complicated by a high degree of crestal faulting, and commonly, mud diapirs and volcanoes. Based on the direction and intensity of structuring, five separate structural-tectonic regions can be identified within the South Caspian Basin: the Apsheron-Balkhan Fold Zone, the Apsheron Archipelago, the Baku Archipelago, the Turkmen Structural Terrace, the Central Fold Zone of the South Caspian.

  5. Chattanooga Eagle Ford Rio Grande Embayment Texas- Louisiana...

    Gasoline and Diesel Fuel Update (EIA)

    Permian Basin Illinois Basin Anadarko Basin Greater Green River Basin Cherokee Platform ... Shale Gas Plays, Lower 48 States 0 200 400 100 300 Miles Source: Energy Information ...

  6. Tularosa Basin Play Fairway: Weights of Evidence Models

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

    Adam Brandt

    2015-12-01

    These models are related to weights of evidence play fairway anlaysis of the Tularosa Basin, New Mexico and Texas. They were created through Spatial Data Modeler: ArcMAP 9.3 geoprocessing tools for spatial data modeling using weights of evidence, logistic regression, fuzzy logic and neural networks. It used to identify high values for potential geothermal plays and low values. The results are relative not only within the Tularosa Basin, but also throughout New Mexico, Utah, Nevada, and other places where high to moderate enthalpy geothermal systems are present (training sites).

  7. EA-377 DC Energy Texas | Department of Energy

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

    7 DC Energy Texas EA-377 DC Energy Texas Order authorizing DC Energy Texas to export electric energy to Mexico. EA-377 DCE Texas Order.pdf (1.96 MB) More Documents & Publications Application to export electric energy OE Docket No. EA-377 Alston&Bird LLP EA-403 Frontera Marketing,

  8. Earth sheltered housing in the south central United States

    SciTech Connect (OSTI)

    Grondzik, W.T. (Oklahoma State Univ., Stillwater); Grondzik, C.S.

    1982-01-01

    A detailed study of identified, occupied earth sheltered residences in the south central United States has been conducted by the Oklahoma State University. Selected results from this investigation of more than 150 residences in the states of Arkansas, Colorado, Iowa, Kansas, Missouri, Nebraska, New Mexico, Oklahoma, and Texas are presented, focusing upon the issues of habitability and energy performance of such structures.

  9. Alternative Fuels Data Center: Texas Taxis Go Hybrid

    Alternative Fuels and Advanced Vehicles Data Center [Office of Energy Efficiency and Renewable Energy (EERE)]

    Texas Taxis Go Hybrid to someone by E-mail Share Alternative Fuels Data Center: Texas Taxis Go Hybrid on Facebook Tweet about Alternative Fuels Data Center: Texas Taxis Go Hybrid on Twitter Bookmark Alternative Fuels Data Center: Texas Taxis Go Hybrid on Google Bookmark Alternative Fuels Data Center: Texas Taxis Go Hybrid on Delicious Rank Alternative Fuels Data Center: Texas Taxis Go Hybrid on Digg Find More places to share Alternative Fuels Data Center: Texas Taxis Go Hybrid on AddThis.com...

  10. Basin Destination State

    Gasoline and Diesel Fuel Update (EIA)

    4. Estimated rail transportation rates for coal, basin to state, EIA data Basin Destination State 2008 2009 2010 2008-2010 2009-2010 Northern Appalachian Basin Delaware 26.24 - W...

  11. Basin Destination State

    Annual Energy Outlook [U.S. Energy Information Administration (EIA)]

    3. Estimated rail transportation rates for coal, basin to state, EIA data Basin Destination State 2008 2009 2010 2008-2010 2009-2010 Northern Appalachian Basin Delaware 28.49 - W...

  12. Basin Destination State

    Annual Energy Outlook [U.S. Energy Information Administration (EIA)]

    43 0.0294 W - W W - - - Northern Appalachian Basin Florida 0.0161 W W W W 0.0216 W W W W W Northern Appalachian Basin Illinois W W - - - - - - - - - Northern Appalachian Basin...

  13. Land subsidence associated with hydrocarbon production, Texas Gulf Coast

    SciTech Connect (OSTI)

    Kreitler, C.W.; White, W.A.; Akhter, M.S.

    1988-01-01

    Although ground-water withdrawal has been the predominant cause of land subsidence in the Texas Gulf Coast, localized subsidence and faulting have also resulted from hydrocarbon production. Subsidence was documented as early as the 1920s over the Goose Creek field. Since then, subsidence and/or faulting have been identified over the Saxet, South Houston, Chocolate Bayou, Hastings, Alco-Mag, Clinton, Mykawa, Blue Ridge, Webster, and Caplen oil fields. Oil-production-related subsidence over these fields generally creates few environmental or engineering problems. One exception is the subsidence and faulting over the Caplen oil field on Bolivar Peninsula, where more than 1,000 ac of saltwater marsh has been replaced by subaqueous flats. Subsidence may be occurring over other fields but has not been identified because of limited releveled benchmark data. An evaluation of drill-stem and bottom-hole pressure data for the Frio Formation in Texas indicates extensive depressurization presumably from hydrocarbon production. Nearly 12,000 measurements from a pressure data base of 17,000 measurements indicate some depressurization. Some of the Frio zones have pressure declines of more than 1,500 psi from original hydrostatic conditions. Subsidence and faulting may be associated with these fields in the Frio as well as other Tertiary formations where extensive hydrocarbon production and subsequent depressurization have occurred.

  14. Alternative Fuels Data Center: Texas Transportation Data for Alternative

    Alternative Fuels and Advanced Vehicles Data Center [Office of Energy Efficiency and Renewable Energy (EERE)]

    Fuels and Vehicles Texas Transportation Data for Alternative Fuels and Vehicles to someone by E-mail Share Alternative Fuels Data Center: Texas Transportation Data for Alternative Fuels and Vehicles on Facebook Tweet about Alternative Fuels Data Center: Texas Transportation Data for Alternative Fuels and Vehicles on Twitter Bookmark Alternative Fuels Data Center: Texas Transportation Data for Alternative Fuels and Vehicles on Google Bookmark Alternative Fuels Data Center: Texas

  15. Supporting Texas Manufacturing to Save Energy Now Program | Department of

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

    Energy State and Utility Engagement Activities » Supporting Texas Manufacturing to Save Energy Now Program Supporting Texas Manufacturing to Save Energy Now Program Texas The industrial sector in Texas is very energy intensive, with approximately 53% of all energy consumed in the state occurring in industrial plants. Therefore, Texas industrials have a great opportunity to reduce their energy intensity and related carbon emissions. In 2009, the U.S. Department of Energy's (DOE's) Advanced

  16. Texas Natural Gas Plant Processing

    Gasoline and Diesel Fuel Update (EIA)

    Commercial Consumers (Number of Elements) Texas Natural Gas Number of Commercial Consumers (Number of Elements) Decade Year-0 Year-1 Year-2 Year-3 Year-4 Year-5 Year-6 Year-7 Year-8 Year-9 1980's 294,879 284,013 270,227 1990's 268,181 269,411 292,990 297,516 306,376 325,785 329,287 332,077 320,922 314,598 2000's 315,906 314,858 317,446 320,786 322,242 322,999 329,918 326,812 324,671 313,384 2010's 312,277 314,041 314,811 314,036 317,217 - = No Data Reported; -- = Not Applicable; NA = Not

  17. Cresson, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    is a stub. You can help OpenEI by expanding it. Cresson is a city in Hood County and Johnson County and Parker County, Texas.1 References US Census Bureau Incorporated...

  18. Butterfield, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    stub. You can help OpenEI by expanding it. Butterfield is a census-designated place in El Paso County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  19. Westway, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    a stub. You can help OpenEI by expanding it. Westway is a census-designated place in El Paso County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  20. Sparks, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    is a stub. You can help OpenEI by expanding it. Sparks is a census-designated place in El Paso County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  1. Canutillo, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    a stub. You can help OpenEI by expanding it. Canutillo is a census-designated place in El Paso County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  2. Fabens, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    is a stub. You can help OpenEI by expanding it. Fabens is a census-designated place in El Paso County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  3. Scurry, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    Map This article is a stub. You can help OpenEI by expanding it. Scurry is a town in Kaufman County, Texas.1 References US Census Bureau Incorporated place and minor civil...

  4. Getting CFLs Home in Longview, Texas

    Office of Energy Efficiency and Renewable Energy (EERE)

    Inefficient light bulbs can drive up electricity bills and drain homeowners' wallets. With that in mind, government officials in the east Texas city of Longview established a light bulb swap program that is projected to save participating households $242.

  5. Texas Legal Review | OpenEI Community

    Open Energy Info (EERE)

    Texas Legal Review Home > Blogs > Alevine's blog Alevine's picture Submitted by Alevine(5) Member 29 July, 2013 - 14:46 BHFS flora and fauna leasing Legal review permitting roadmap...

  6. Bryan Texas Utilities- SmartHOME Program

    Broader source: Energy.gov [DOE]

    The Bryan Texas Utilities (BTU) SmartHOME Programs offers incentives to owners of single- and multi-family homes for insulation, windows, and solar screens.The incentive amount may not be less than...

  7. Highlands, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    a stub. You can help OpenEI by expanding it. Highlands is a census-designated place in Harris County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  8. Barrett, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    a stub. You can help OpenEI by expanding it. Barrett is a census-designated place in Harris County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  9. Atascocita, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    stub. You can help OpenEI by expanding it. Atascocita is a census-designated place in Harris County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  10. Aldine, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    is a stub. You can help OpenEI by expanding it. Aldine is a census-designated place in Harris County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  11. Channelview, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    stub. You can help OpenEI by expanding it. Channelview is a census-designated place in Harris County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  12. Cloverleaf, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    stub. You can help OpenEI by expanding it. Cloverleaf is a census-designated place in Harris County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  13. Crosby, Texas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    is a stub. You can help OpenEI by expanding it. Crosby is a census-designated place in Harris County, Texas.1 References US Census Bureau 2005 Place to 2006 CBSA Retrieved...

  14. Strategic Energy LLC (Texas) | Open Energy Information

    Open Energy Info (EERE)

    Strategic Energy LLC Place: Texas References: EIA Form EIA-861 Final Data File for 2010 - File220101 EIA Form 861 Data Utility Id 18193 This article is a stub. You can help...

  15. Assessment of Wind/Solar Co-located Generation in Texas

    SciTech Connect (OSTI)

    Steven M. Wiese

    2009-07-20

    This paper evaluates the opportunity to load co-located wind and solar generation capacity onto a constrained transmission system while engendering only minimal losses. It quantifies the economic and energy opportunities and costs associated with pursuing this strategy in two Texas locations – one in west Texas and the other in south Texas. The study builds upon previous work published by the American Solar Energy Society (ASES) which illuminated the potential benefits of negative correlation of wind and solar generation in some locations by quantifying the economic and energy losses which would arise from deployment of solar generation in areas with existing wind generation and constrained transmission capacity. Clean Energy Associates (CEA) obtained and incorporated wind and solar resource data and the Electric Reliability Council of Texas (ERCOT)) load and price data into a model which evaluates varying levels of solar thermal, solar photovoltaic (PV) and wind capacity against an assumed transmission capacity limit at each of the two locations.

  16. Source rocks of the Sub-Andean basins

    SciTech Connect (OSTI)

    Raedeke, L.D. )

    1993-02-01

    Seven source rock systems were mapped using a consistent methodology to allow basin comparison from Trinidad to southern Chile. Silurian and Devonian systems, deposited in passive margin and intracratonic settings, have fair-good original oil/gas potential from central and northern Bolivia to southern Peru. Kerogens range from mature in the foreland to overmature in the thrust belt. Permian to Carboniferous deposition in local restricted basins formed organic-rich shales and carbonates with very good original oil/gas potential, principally in northern Bolivia and southern Peru. Late Triassic to early Jurassic marine shales and limestones, deposited in deep, narrow, basins from Ecuador to north-central maturity. Locally, in the Cuyo rift basin of northern Argentina, a Triassic lacustrine unit is a very good, mature oil source. Early Cretaceous to Jurassic marine incursions into the back-arc basins of Chile-Argentina deposited shales and limestones. Although time transgressive (younging to the south), this system is the principal source in southern back-arc basins, with best potential in Neuquen, where three intervals are stacked A late Cretaceous marine transgressive shale is the most important source in northern South America. The unit includes the La Luna and equivalents extending from Trinidad through Venezuela, Colombia, Ecuador, and into northern Peru. Elsewhere in South America upper Cretaceous marine-lacustrine rocks are a possible source in the Altiplano and Northwest basins of Bolivia and Argentina. Middle Miocene to Oligocene source system includes shallow marine, deltaic, and lacustrine sediments from Trinidad to northern Peru.

  17. Texas site selection and licensing status

    SciTech Connect (OSTI)

    Avant, R.V. Jr.

    1989-11-01

    Texas has identified a potential site in Hudspeth County in far West Texas near the town of Fort Hancock. Over the past year the Texas Low-Level Radioactive Waste Disposal Authority has been conducting detailed geology, hydrology, meteorology, soils, and flora and fauna evaluations. An authorization by the Board of Directors of the Authority to proceed with a license application, assuming that the detailed evaluation indicates that the site is suitable, is expected by September. A prototype license has been prepared in anticipation of the order to proceed with licensing, and the formal license application is expected to be submitted to the Texas Department of Health-Bureau of Radiation Control in December, meeting the license application milestone. Although site selection processes in all siting areas across the country have experienced organized opposition, El Paso County has funded a particularly well-organized, well-financed program to legally and technically stop consideration of the Fort Hancock site prior to the licensing process. Many procedural, regulatory, and technical issues have been raised which have required responses from the Authority in order to proceed with licensing. This has provided a unique perspective of what to expect from well-organized opposition at the licensing stage. This paper presents an update on the Texas siting activity with detailed information on the site evaluation and license application. Experience of dealing with issues raised by opposition relating to NRC guidelines and rules is also discussed.

  18. City of Brady, Texas (Utility Company) | Open Energy Information

    Open Energy Info (EERE)

    Brady, Texas (Utility Company) Jump to: navigation, search Name: City of Brady Place: Texas Phone Number: (325) 597-2152 Website: bradytx.usindex.aspx?nid609 Outage Hotline:...

  19. TCEQ - Map of Texas Groundwater Conservation Districts | Open...

    Open Energy Info (EERE)

    Map of Texas Groundwater Conservation Districts Jump to: navigation, search OpenEI Reference LibraryAdd to library Map: TCEQ - Map of Texas Groundwater Conservation DistrictsInfo...

  20. Jackson Electric Coop, Inc (Texas) | Open Energy Information

    Open Energy Info (EERE)

    Jackson Electric Coop, Inc (Texas) Jump to: navigation, search Name: Jackson Electric Coop, Inc Place: Texas Phone Number: 361-771-4400 or 979-245-3029 Website: jecec.com...