Sample records for lithology geochemistry salinity

  1. Geochemistry

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

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645U.S. DOE Office of Science (SC) Environmental AssessmentsGeoffrey CampbelllongApplying Geochemistry to Solve Issues

  2. The geochemistry and provenance of Apollo 16 mafic glasses Ryan A. Zeigler *, Randy L. Korotev, Bradley L. Jolliff,

    E-Print Network [OSTI]

    The geochemistry and provenance of Apollo 16 mafic glasses Ryan A. Zeigler *, Randy L. Korotev of the Apollo 16 lunar landing site is composed mainly of feldspathic lithologies but mafic lithologies are also composition of 280 mafic glasses (>10 wt% FeO) from six different Apollo 16 soil samples. A small proportion

  3. Sedimentology and geochemistry of an exceptionally preserved last interglacial sapropel S5 in the Levantine Basin (Mediterranean Sea)

    E-Print Network [OSTI]

    Gilli, Adrian

    Sedimentology and geochemistry of an exceptionally preserved last interglacial sapropel S5 of lithological, geochemical and physical sediment properties is reported from a complete- ly laminated S5 region of the eastern Mediterranean. The thickness of the studied sapropel S5 varies be- tween 85 and 91

  4. Multiphase Sequestration Geochemistry: Model for Mineral Carbonation...

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

    Multiphase Sequestration Geochemistry: Model for Mineral Carbonation. Multiphase Sequestration Geochemistry: Model for Mineral Carbonation. Abstract: Carbonation of formation...

  5. LITHOLOGY-FLUID INVERSION FROM PRESTACK SEISMIC DATA

    E-Print Network [OSTI]

    Eidsvik, Jo

    LITHOLOGY-FLUID INVERSION FROM PRESTACK SEISMIC DATA MARIT ULVMOEN Department of Mathematical of the study is on lithology-fluid inversion from prestack seismic data in a 3D reservoir. The inversion relates the lithology-fluid classes to elastic variables and the seismic data, and it follows the lines

  6. Lithology-Fluid Inversion based on Prestack Seismic Data

    E-Print Network [OSTI]

    Eidsvik, Jo

    Lithology-Fluid Inversion based on Prestack Seismic Data Marit Ulvmoen Summary The focus of the study is on lithology-fluid inversion from prestack seismic data. The target zone is a 3D reservoir model. The likelihood model relates the lithology-fluid classes to elastic variables and the seismic

  7. Geochemistry studies in Eastern Kentucky. Final report

    SciTech Connect (OSTI)

    Negus-de Wys, J.

    1981-04-01T23:59:59.000Z

    Presented here are the results of inorganic geochemical studies on well cuttings from fourteen wells in the Big Sandy Gas Field. Both x-ray fluorescence and x-ray diffraction were used in analysis. Resultant mineralic data and elemental data were mapped by computer and by hand for five intervals of Ohio Shale and for the Berea/Bedford sequence. Comparisons of the geochemistry trend maps were made with lithology, structure, thermal maturation, gas open flow, and paleoenvironment. Techniques used included visual map comparison, computer map comparison programs utilizing correlation coefficients based on grid derived data sets, cluster analysis, x-y plots, and r/sup 2/ (coefficient of determination). A limited number of regional maps are included. It is concluded that inorganic geochemical analysis can be useful in: (1) suggesting paleoenvironmental trends; (2) establishing depositional trends; (3) enhancing exploration in terms of setting limits and pinpointing potential areas for hydrocarbon recovery; and (4) identification of likely locations for large gas fields when used with other geological studies. Elemental data analysis is the most accurate, and can be done quickly and inexpensively. It is concluded that the Big Sandy gas field area is a unique stratigraphic-structural gas trap, in which sedimentary factors, depositional basin features, plant evolution and occurrence, and structural elements all played important roles. Combinations of certain of these ingredients in different amounts may exist in other parts of the basin, and thus, suggest areas for hydrocarbon accumulation and potential recovery.

  8. Overview of fundamental geochemistry basic research at the Oak Ridge National Laboratory

    SciTech Connect (OSTI)

    Anovitz, L.M.; Benezeth, P.; Blencoe, J.G. [and others

    1996-01-01T23:59:59.000Z

    Researchers in ORNL`s Geochemistry and High Temperature Aqueous Chemistry groups are conducting detailed experimental studies of physicochemical properties of the granite-melt-brine system; sorption of water on rocks from steam-dominated reservoirs; partitioning of salts and acid volatiles between brines and steam; effects of salinity on H and O isotope partitioning between brines, minerals, and steam; and aqueous geochemistry of Al. These studies contribute in many ways to cost reductions and improved efficiency in the discovery, characterization, and production of energy from geothermal resources.

  9. Sandia Energy - Geochemistry

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

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch > TheNuclear Press ReleasesInAppliedEnergy StorageGeochemistry Home

  10. WHAT IS MEDICAL MINERALOGY AND GEOCHEMISTRY?

    E-Print Network [OSTI]

    Sahai, Nita

    WHAT IS MEDICAL MINERALOGY AND GEOCHEMISTRY? The connection between human health of medical mineralogy and geochemistry (MMG) focuses on understanding the equilibria and reaction pathways phases with naturally occurring, inorganic solid phases within the human body. Medical mineralogy

  11. Intergrating Magnetotellurics, Soil Gas Geochemistry and Structural...

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

    Intergrating Magnetotellurics, Soil Gas Geochemistry and Structural Analysis to Identify Hidden, High Enthalpy, Extensional Geothermal Systems Intergrating Magnetotellurics, Soil...

  12. Soda Lake Well Lithology Data and Geologic Cross-Sections

    SciTech Connect (OSTI)

    Faulds, James E.

    2013-12-31T23:59:59.000Z

    Comprehensive catalogue of drill?hole data in spreadsheet, shapefile, and Geosoft database formats. Includes XYZ locations of well heads, year drilled, type of well, operator, total depths, well path data (deviations), lithology logs, and temperature data. Plus, 13 cross?sections in Adobe Illustrator format.

  13. Recent advances in coal geochemistry

    SciTech Connect (OSTI)

    Chyi, L.L. (Dept. of Geology, Univ. of Akron, Akron, OH (US)); Chou, C.-L. (Illinois State Geological Survey, 615 E. Peabody Drive, Champaign, IL (US))

    1990-01-01T23:59:59.000Z

    Chapters in this collection reflect the recent emphasis both on basic research in coal geochemistry and on applied aspects related to coal utilization. Geochemical research on peat and coal generates compositional data that are required for the following reasons. First, many studies in coal geology require chemical data to aid in interpretation for better understanding of the origin and evolution of peat and coal. Second, coal quality assessment is based largely on composition data, and these data generate useful insights into the geologic factors that control the quality of coal. Third, compositional data are needed for effective utilization of coal resources and to reflect the recent emphasis on both basic research in coal geochemistry and environmental aspects related to coal utilization.

  14. Author's Copy 2Reviews in Mineralogy & Geochemistry

    E-Print Network [OSTI]

    Truhlar, Donald G

    Author's Copy 2Reviews in Mineralogy & Geochemistry Vol. 71 pp. 19-37, 2010 Copyright © Mineralogical Society of America 1529-6466/10/0071-0002$05.00 DOI: 10.2138/rmg.2010.71.2 The Minnesota Density Functionals and their Applications to Problems in Mineralogy and Geochemistry Yan Zhao Commercial Print Engine

  15. Appendix A Lithologic and Monitor Well Completion Logs

    Office of Legacy Management (LM)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOn AprilA group currentBradleyTableSelling7111A Lithologic and Monitor Well Completion Logs

  16. Lithology and well log study of Campbell E-2 geothermal test...

    Open Energy Info (EERE)

    Pershing County, Nevada Jump to: navigation, search OpenEI Reference LibraryAdd to library Report: Lithology and well log study of Campbell E-2 geothermal test well,...

  17. Flemish fieldstone: unravelling lithological differences and diagenesis Research Unit: Sedimentary Geology and Engineering Geology

    E-Print Network [OSTI]

    Gent, Universiteit

    Flemish fieldstone: unravelling lithological differences and diagenesis Research Unit: Sedimentary Geology and Engineering Geology Topic: Fieldstone, natural stone, diagenesis, microscopy with a great interest in sedimentation processes and diagenesis, in petrology and Flemish stratigraphy

  18. CONTROL ID: 1469463 TITLE: In Situ Techniques for Mineralogy and Geochemistry of Small Bodies

    E-Print Network [OSTI]

    Rossman. George R.

    CONTROL ID: 1469463 TITLE: In Situ Techniques for Mineralogy and Geochemistry of Small Bodies information about their formation histories and evolution. Combined geochemistry and mineralogy measurements measurement techniques that could provide microscopic mineralogy and isotope geochemistry. We will discuss

  19. Earth and Space Sciences Geochemistry 111

    E-Print Network [OSTI]

    Henkel, Werner

    Earth and Space Sciences #12;Geochemistry 111 5 Earth and Space Sciences Research in the realm of Earth and Space Sci- ences focusses on the observation and qualitative and quantitative description of natural phenom- ena on Earth and in the Universe, on the detailed study and experimental and computational

  20. SHIP3QARD ORGANIC GEOCHEMISTRY JOIDES RESOLUTION

    E-Print Network [OSTI]

    with the National Science Foundation. Funding for the program is provided by the following agencies: DepartmentSHIP3QARD ORGANIC GEOCHEMISTRY ON JOIDES RESOLUTION Kay-Christian Bneis Ocean Drilling Program 345 Middlefield Road Menlo Park, CA 94025 OCEAN DRILLING PROGRAM TEXAS A&MUNIVERSITY TECHNICAL NOTE

  1. Salinity driven oceanographic upwelling

    DOE Patents [OSTI]

    Johnson, D.H.

    1984-08-30T23:59:59.000Z

    The salinity driven oceanographic upwelling is maintained in a mariculture device that includes a long main duct in the general shape of a cylinder having perforated cover plates at each end. The mariculture device is suspended vertically in the ocean such that one end of the main duct is in surface water and the other end in relatively deep water that is cold, nutrient rich and relatively fresh in comparison to the surface water which is relatively warm, relatively nutrient deficient and relatively saline. A plurality of elongated flow segregating tubes are disposed in the main duct and extend from the upper cover plate beyond the lower cover plate into a lower manifold plate. The lower manifold plate is spaced from the lower cover plate to define a deep water fluid flow path to the interior space of the main duct. Spacer tubes extend from the upper cover plate and communicate with the interior space of the main duct. The spacer tubes are received in an upper manifold plate spaced from the upper cover plate to define a surface water fluid flow path into the flow segregating tubes. A surface water-deep water counterflow is thus established with deep water flowing upwardly through the main duct interior for discharge beyond the upper manifold plate while surface water flows downwardly through the flow segregating tubes for discharge below the lower manifold plate. During such counterflow heat is transferred from the downflowing warm water to the upflowing cold water. The flow is maintained by the difference in density between the deep water and the surface water due to their differences in salinity. The upwelling of nutrient rich deep water is used for marifarming by fertilizing the nutrient deficient surface water. 1 fig.

  2. FLUID GEOCHEMISTRY AT THE RAFT RIVER GEOTHERMAL FIELD, IDAHO...

    Open Energy Info (EERE)

    HYDROGEOLOGICAL IMPLICATIONS Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Proceedings: FLUID GEOCHEMISTRY AT THE RAFT RIVER GEOTHERMAL FIELD,...

  3. Advances In The Past 20 Years- Geochemistry In Geothermal Exploration...

    Open Energy Info (EERE)

    Past 20 Years- Geochemistry In Geothermal Exploration Resource Evaluation And Reservoir Management Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference...

  4. Water geochemistry study of Indian Wells Valley, Inyo and Kern...

    Open Energy Info (EERE)

    Final report Jump to: navigation, search OpenEI Reference LibraryAdd to library Report: Water geochemistry study of Indian Wells Valley, Inyo and Kern Counties, California....

  5. Geothermal investigations in Idaho. Part 1. Geochemistry and...

    Open Energy Info (EERE)

    in Idaho. Part 1. Geochemistry and geologic setting of selected thermal waters Jump to: navigation, search OpenEI Reference LibraryAdd to library Report: Geothermal investigations...

  6. International Geophysical Conference and Exhibition, 26-29 February 2012 -Brisbane, Australia 1 Structurally constrained lithology characterization using magnetic

    E-Print Network [OSTI]

    22 nd International Geophysical Conference and Exhibition, 26-29 February 2012 - Brisbane meaningful lithologic information directly from geophysical data. Here, we describe a multi-faceted approach

  7. Compiled Multi-Lab Geochemistry Synoptic Survey (LANL, ORNL, LBNL), Barrow, Alaska; 2012

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

    Brent Newman; Heather Throckmorton

    To assess the effects of microtopography and depth on ground water geochemistry in arctic polygonal terrain.

  8. Geochemistry of slow-growing corals : reconstructing sea surface temperature, salinity and the North Atlantic Oscillation

    E-Print Network [OSTI]

    Goodkin, Nathalie Fairbank

    2007-01-01T23:59:59.000Z

    A 225-year old coral from the south shore of Bermuda (64°W, 320N) provides a record of decadal-to-centennial scale climate variability. The coral was collected live, and sub-annual density bands seen in x-radiographs ...

  9. Identification of Source Lithology in the Hawaiian and Canary Islands: Implications

    E-Print Network [OSTI]

    Identification of Source Lithology in the Hawaiian and Canary Islands: Implications for Origins in localities such as the Canary Islands are deficient in SiO2, and mayhavebeengenerated by partial inclusions will be useful to evaluate its importance. In contrast to Hawaii, many ocean island basalts

  10. 12.479 Trace-Element Geochemistry, Fall 2006

    E-Print Network [OSTI]

    Frey, Frederick August

    Focuses on element distribution in rocks and minerals using data obtained from natural and experimental systems. Emphasizes models describing trace-element partitioning and applications of trace-element geochemistry to ...

  11. 12.479 Trace-Element Geochemistry, Spring 2009

    E-Print Network [OSTI]

    Frey, Frederick

    The emphasis of this course is to use Trace Element Geochemistry to understand the origin and evolution of igneous rocks. The approach is to discuss the parameters that control partitioning of trace elements between phases ...

  12. Geology, Water Geochemistry And Geothermal Potential Of The Jemez...

    Open Energy Info (EERE)

    Geology, Water Geochemistry And Geothermal Potential Of The Jemez Springs Area, Canon De San Diego, New Mexico Jump to: navigation, search OpenEI Reference LibraryAdd to library...

  13. Catalog of borehole lithologic logs from the 600 Area, Hanford Site

    SciTech Connect (OSTI)

    Fecht, K R; Lillie, J T

    1982-03-01T23:59:59.000Z

    Rockwell Hanford Operations (Rockwell) geoscientists are studying the Hanford Site subsurface environment to assure safe management operations, disposal, and storage of radioactive waste. As part of this effort, geoscientists have collected geotechnical data from about 3000 boreholes drilled on the Hanford Site since the early 1900s. These boreholes have been used for subsurface geologic, hydrologic, and engineering investigation, water supply, ground-water monitoring, and natural gas production. This report is a catalog of all obtainable (about 800) lithologic logs from boreholes in a portion of the Hanford Site known as the 600 Area.

  14. DOE workshop: Sedimentary systems, aqueous and organic geochemistry

    SciTech Connect (OSTI)

    Not Available

    1993-07-01T23:59:59.000Z

    A DOE workshop on sedimentary systems, aqueous and organic geochemistry was held July 15-16, 1993 at Lawrence Berkeley Laboratory. Papers were organized into several sections: Fundamental Properties, containing papers on the thermodynamics of brines, minerals and aqueous electrolyte solutions; Geochemical Transport, covering 3-D imaging of drill core samples, hydrothermal geochemistry, chemical interactions in hydrocarbon reservoirs, fluid flow model application, among others; Rock-Water Interactions, with presentations on stable isotope systematics of fluid/rock interaction, fluid flow and petotectonic evolution, grain boundary transport, sulfur incorporation, tracers in geologic reservoirs, geothermal controls on oil-reservoir evolution, and mineral hydrolysis kinetics; Organic Geochemistry covered new methods for constraining time of hydrocarbon migration, kinetic models of petroleum formation, mudstones in burial diagenesis, compound-specific carbon isotope analysis of petroleums, stability of natural gas, sulfur in sedimentary organic matter, organic geochemistry of deep ocean sediments, direct speciation of metal by optical spectroscopies; and lastly, Sedimentary Systems, covering sequence stratigraphy, seismic reflectors and diagenetic changes in carbonates, geochemistry and origin of regional dolomites, and evidence of large comet or asteroid impacts at extinction boundaries.

  15. RADIOIODINE GEOCHEMISTRY IN THE SRS SUBSURFACE ENVIRONMENT

    SciTech Connect (OSTI)

    Kaplan, D.; Emerson, H.; Powell, B.; Roberts, K.; Zhang, S.; Xu, C.; Schwer, K.; Li, H.; Ho, Y.; Denham, M.; Yeager, C.; Santschi, P.

    2013-05-16T23:59:59.000Z

    Iodine-129 is one of the key risk drivers for several Savannah River Site (SRS) performance assessments (PA), including that for the Low-Level Waste Disposal Facility in E-Area. In an effort to reduce the uncertainty associated with the conceptual model and the input values used in PA, several studies have recently been conducted dealing with radioiodine geochemistry at the SRS. The objective of this report was to review these recent studies and evaluate their implications on SRS PA calculations. For the first time, these studies measured iodine speciation in SRS groundwater and provided technical justification for assuming the presence of more strongly sorbing species (iodate and organo-iodine), and measured greater iodine sediment sorption when experiments included these newly identified species; specifically they measured greater sorption coefficients (K{sub d} values: the concentration ratio of iodine on the solid phase divided by the concentration in the aqueous phase). Based on these recent studies, new best estimates were proposed for future PA calculations. The new K{sub d} values are greater than previous recommended values. These proposed K{sub d} values reflect a better understanding of iodine geochemistry in the SRS subsurface environment, which permits reducing the associated conservatism included in the original estimates to account for uncertainty. Among the key contributing discoveries supporting the contention that the K{sub d} values should be increased are that: 1) not only iodide (I{sup -}), but also the more strongly sorbing iodate (IO{sub 3}{sup -}) species exists in SRS groundwater (average total iodine = 15% iodide, 42% iodate, and 43% organoiodine), 2) when iodine was added as iodate, the measured K{sub d} values were 2 to 6 times greater than when the iodine was added as iodide, and perhaps most importantly, 3) higher desorption (10 to 20 mL/g) than (ad)sorption (all previous studies) K{sub d} values were measured. The implications of this latter point is that the iodine desorption process would be appreciably slower than the (ad)sorption process, and as such would control the rate (and the PA K{sub d} value) that iodine sorbed to and therefore migrated through the subsurface sediment. High desorption K{sub d} values would result in the “effective K{sub d}” for a reactive transport model being closer to the desorption K{sub d} value (the rate limiting value) than the (ad)sorption K{sub d} value. In summary, our understanding of {sup 129}I geochemistry has greatly improved, reducing the uncertainty associated with the PA’s conceptual model, thereby permitting us to reduce the conservatism presently incorporated in PA input values to describe {sup 129}I fate and transport in the SRS subsurface environment.

  16. COAL QUALITY AND GEOCHEMISTRY, HANNA AND CARBON BASINS, WYOMING

    E-Print Network [OSTI]

    Chapter HQ COAL QUALITY AND GEOCHEMISTRY, HANNA AND CARBON BASINS, WYOMING By G.D. Stricker and M coal beds and zones in the Northern RockyMountains and Great Plains region, U.S. Geological Survey of selected Tertiary coal beds and zones in the Northern Rocky Mountains and Great Plains region, U

  17. COAL QUALITY AND GEOCHEMISTRY, WILLISTON BASIN, NORTH DAKOTA

    E-Print Network [OSTI]

    Chapter WQ COAL QUALITY AND GEOCHEMISTRY, WILLISTON BASIN, NORTH DAKOTA By G.D. Stricker and M coal beds and zones in the Northern RockyMountains and Great Plains region, U.S. Geological Survey of selected Tertiary coal beds and zones in the Northern Rocky Mountains and Great Plains region, U

  18. COAL QUALITY AND GEOCHEMISTRY, GREATER GREEN RIVER BASIN, WYOMING

    E-Print Network [OSTI]

    Chapter GQ COAL QUALITY AND GEOCHEMISTRY, GREATER GREEN RIVER BASIN, WYOMING By G.D. Stricker and M coal beds and zones in the Northern RockyMountains and Great Plains region, U.S. Geological Survey of selected Tertiary coal beds and zones in the Northern Rocky Mountains and Great Plains region, U

  19. Rutile geochemistry and its potential use in quantitative provenance studies

    E-Print Network [OSTI]

    Zack, Thomas

    . Keywords: Rutile; Provenance; Geochemistry; Heavy minerals; Appalachians 1. Introduction The extraction form 16 March 2004; accepted 12 May 2004 Abstract Rutile is among the most stable detrital minerals of mature sediments, where most diagnostic minerals are no longer stable. In contrast to zircon, rutile

  20. ASSISTANT PROFESSOR OF ENVIRONMENTAL GEOCHEMISTRY UNIVERSITY OF CALIFORNIA, BERKELEY

    E-Print Network [OSTI]

    Silver, Whendee

    of Environmental Science, Policy, and Management (http://espm.berkeley.edu), invites applications for a tenure, molecular scale organic-mineral interactions, and reaction/transport modeling of soil processes course in Environmental or Soil Geochemistry, as well as contribute to other Department teaching needs

  1. Naturally Saline Boreal Communities as Models for Reclamation of Saline Oil Sand Tailings

    E-Print Network [OSTI]

    Macdonald, Ellen

    mining. Key words: boreal forest, community ecology, oil sands, ordination, reclamation, salinity mining have saline soils; yet, they are required to have similar biodiversity and productivity mining, with anti- cipated rates of disturbance of 2,000 ha/yr (CONRAD 1999). Saline tailings are left

  2. Joint porosity depth trend estimation and lithology/fluid classification by Bayesian inversion Kjartan Rimstad and Henning Omre

    E-Print Network [OSTI]

    Eidsvik, Jo

    ,0 Sand,Shale,Sand,kc Sand,zc Sand] and the prior model of is p(). We assume that seismic AVO data. The ultimate goal of this study is to clas- sify lithology/fluid from sesimic AVO data using our stochastic Consider a geological model of a reservoir in one dimension, and the four classes oil-, gas- and brine

  3. 2Reviews in Mineralogy & Geochemistry Vol. 64, pp. 5-57, 2006

    E-Print Network [OSTI]

    Ahmad, Sajjad

    2Reviews in Mineralogy & Geochemistry Vol. 64, pp. 5-57, 2006 Copyright © Mineralogical Society with health scientists to contribute expertise in mineralogy, materials characterization, fluid

  4. DALHOUSIE UNIVERSITY, DEPARTMENT OF EARTH SCIENCES Assistant Professor -Geophysics, Sedimentology, or Geochemistry

    E-Print Network [OSTI]

    Brownstone, Rob

    DALHOUSIE UNIVERSITY, DEPARTMENT OF EARTH SCIENCES Assistant Professor - Geophysics, Sedimentology position in Geophysics, Sedimentology, or Geochemistry. The appointment is probationary tenure

  5. Stable isotope geochemistry of sulfur bearing minerals and clay mineralogy of some soils and sediments in Loot Desert, central Iran

    E-Print Network [OSTI]

    Ahmad, Sajjad

    Stable isotope geochemistry of sulfur bearing minerals and clay mineralogy of some soils Keywords: Sulfur geochemistry Gypsum crystallization water Clay mineralogy Palygorskite Iranian soils Loot technique and clay mineralogy were studied in different landforms in Loot Desert, central Iran. Four

  6. alleviate salinity damage: Topics by E-print Network

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

    114 Impact of salinity on cathode catalyst performance in microbial fuel cells (MFCs) Energy Storage, Conversion and Utilization Websites Summary: Impact of salinity on cathode...

  7. Plutonium and Americium Geochemistry at Hanford: A Site Wide Review

    SciTech Connect (OSTI)

    Cantrell, Kirk J.; Felmy, Andrew R.

    2012-08-23T23:59:59.000Z

    This report was produced to provide a systematic review of the state-of-knowledge of plutonium and americium geochemistry at the Hanford Site. The report integrates existing knowledge of the subsurface migration behavior of plutonium and americium at the Hanford Site with available information in the scientific literature regarding the geochemistry of plutonium and americium in systems that are environmentally relevant to the Hanford Site. As a part of the report, key research needs are identified and prioritized, with the ultimate goal of developing a science-based capability to quantitatively assess risk at sites contaminated with plutonium and americium at the Hanford Site and the impact of remediation technologies and closure strategies.

  8. Sedimentary basin geochemistry and fluid/rock interactions workshop

    SciTech Connect (OSTI)

    NONE

    1991-12-31T23:59:59.000Z

    Fundamental research related to organic geochemistry, fluid-rock interactions, and the processes by which fluids migrate through basins has long been a part of the U.S. Department of Energy Geosciences program. Objectives of this program were to emphasize those principles and processes which would be applicable to a wide range of problems associated with petroleum discovery, occurrence and extraction, waste disposal of all kinds, and environmental management. To gain a better understanding of the progress being made in understanding basinal fluids, their geochemistry and movement, and related research, and to enhance communication and interaction between principal investigators and DOE and other Federal program managers interested in this topic, this workshop was organized by the School of Geology and Geophysics and held in Norman, Oklahoma in November, 1991.

  9. Summary of lithologic logging of new and existing boreholes at Yucca Mountain, Nevada, August 1993 to February 1994

    SciTech Connect (OSTI)

    Geslin, J.K.; Moyer, T.C.; Buesch, D.C.

    1995-05-01T23:59:59.000Z

    Yucca Mountain, Nevada, is being investigated as a potential site for a high-level radioactive waste repository. This report summarizes the lithologic logging of new and existing boreholes at Yucca Mountain that was done from August 1993 to February 1994 by the Rock Characteristics Section, Yucca Mountain Project Branch, US Geological Survey (USGS). Units encountered during logging include Quaternary-Tertiary alluvium/colluvium, Tertiary Rainier Mesa Tuff, all units in the Tertiary Paintbrush Group, Tertiary Calico Hills Formation and Tertiary Prow Pass Tuff. We present criteria used for recognition of stratigraphic contacts, logging results as tables of contact depths for core from neutron (UZN) boreholes and graphical lithologic logs for core from non-UZN boreholes, and descriptions of several distinctive nonwelded tuffs recognized in the PTn hydrogeologic unit of the Paintbrush Group.

  10. A Site-Wide Perspective on Uranium Geochemistry at the Hanford Site

    E-Print Network [OSTI]

    PNNL-17031 A Site-Wide Perspective on Uranium Geochemistry at the Hanford Site J. Zachara C. Liu C of River Protection (ORP) #12;#12;PNNL-17031 A Site-Wide Perspective on Uranium Geochemistry at the Hanford with the Pacific Northwest National Laboratory (PNNL) and its collaborators. Significant research has more recently

  11. A post-Caledonian dolerite dyke from Magery, North Norway: age and geochemistry

    E-Print Network [OSTI]

    Andersen, Torgeir Bjørge

    A post-Caledonian dolerite dyke from Magerøy, North Norway: age and geochemistry DAVID ROBERTS-Caledonian dolerite dyke from Magerøy, North Norway: age and geochemistry. Norsk Geologisk Tidsskrift, Vol. 71, pp, Geological Survey of Norway, Post Box 3006-Lade, N-7(}()2 Trondheim, Norway; John G. Mitchell, Department

  12. Reconnaissance Soil Geochemistry at the Riverton Uranium Mill Tailings Remedial Action Site, Fremont

    E-Print Network [OSTI]

    Fleskes, Joe

    Reconnaissance Soil Geochemistry at the Riverton Uranium Mill Tailings Remedial Action Site, Reconnaissance soil geochemistry at the Riverton Uranium Mill Tailings Remedial Action Site, Fremont County.....................................................................................................................................................link Figures Figure 1. Location of 19 soil samples collected from the Riverton Uranium Mill Tailings Remedial

  13. Treating nahcolite containing formations and saline zones

    DOE Patents [OSTI]

    Vinegar, Harold J

    2013-06-11T23:59:59.000Z

    A method for treating a nahcolite containing subsurface formation includes removing water from a saline zone in or near the formation. The removed water is heated using a steam and electricity cogeneration facility. The heated water is provided to the nahcolite containing formation. A fluid is produced from the nahcolite containing formation. The fluid includes at least some dissolved nahcolite. At least some of the fluid is provided to the saline zone.

  14. Hydrology, Salinity, and Salinity Control Possibilities of the Middle Pecos River: A Reconnaissance Report

    E-Print Network [OSTI]

    Miyamoto, S.; Anand, Shilpa; Hatler, Will

    The Middle Pecos River between Malaga, New Mexico, and Girvin, Texas, is known for high salinity. Streamflow salinity during the last decade (1991-2000), for example, averaged 3,500 and 6,150 mg L-1 at Malaga and at the Red Bluff release...

  15. Q AS A LITHOLOGICAL/HYDROCARBON INDICATOR: FROM FULL WAVEFORM SONIC TO 3D SURFACE SEISMIC

    SciTech Connect (OSTI)

    Jorge O. Parra; C.L. Hackert; L. Wilson; H.A. Collier; J. Todd Thomas

    2006-03-31T23:59:59.000Z

    The goal of this project was to develop a method to exploit viscoelastic rock and fluid properties to greatly enhance the sensitivity of surface seismic measurements to the presence of hydrocarbon saturation. To reach the objective, Southwest Research Institute scientists used well log, lithology, production, and 3D seismic data from an oil reservoir located on the Waggoner Ranch in north central Texas. The project was organized in three phases. In the first phase, we applied modeling techniques to investigate seismic- and acoustic-frequency wave attenuation and its effect on observable wave attributes. We also gathered existing data and acquired new data from the Waggoner Ranch field, so that all needed information was in place for the second phase. During the second phase, we developed methods to extract attenuation from borehole acoustic and surface seismic data. These methods were tested on synthetic data constructed from realistic models and real data. In the third and final phase of the project, we applied this technology to a full data set from the Waggoner site. The results presented in this Final Report show that geological conditions at the site did not allow us to obtain interpretable results from the Q processing algorithm for 3D seismic data. However, the Q-log processing algorithm was successfully applied to full waveform sonic data from the Waggoner site. A significant part of this project was technology transfer. We have published several papers and conducted presentations at professional conferences. In particular, we presented the Q-log algorithm and applications at the Society of Exploration Geophysicists (SEG) Development and Production Forum in Austin, Texas, in May 2005. The presentation attracted significant interest from the attendees and, at the request of the SEG delegates, it was placed on the Southwest Research Institute Internet site. The presentation can be obtained from the following link: http://www.swri.org/4org/d15/elecsys/resgeo/ppt/Algorithm.pps In addition, we presented a second application of the Q algorithm at the SEG International Conference in Houston, Texas, in May 2005. The presentation attracted significant interest there as well, and it can be obtained from the following link: http://www.swri.org/4org/d15/elecsys/resgeo/ppt/attenuation.pps.

  16. Infrared Spectroscopy and Stable Isotope Geochemistry of Hydrous Silicate Glasses

    SciTech Connect (OSTI)

    Stolper, Edward

    2007-03-05T23:59:59.000Z

    The focus of this DOE-funded project has been the study of volatile components in magmas and the atmosphere. Over the twenty-one year period of this project, we have used experimental petrology and stable isotope geochemistry to study the behavior and properties of volatile components dissolved in silicate minerals and melts and glasses. More recently, we have also studied the concentration and isotopic composition of CO2 in the atmosphere, especially in relation to air quality issues in the Los Angeles basin.

  17. Comparative assessment of five potential sites for hydrothermal magma systems: geochemistry

    SciTech Connect (OSTI)

    White, A.F.

    1980-08-01T23:59:59.000Z

    A brief discussion is given of the geochemical objectives and questions that must be addressed in such an evaluation. A summary of the currently published literature that is pertinent in answering these questions is presented for each of the five areas: The Geysers-Clear Lake region, Long Valley, Rio Grand Rift, Roosevelt Hot Springs, and the Salton Trough. The major geochemical processes associated with proposed hydrothermal sites are categorized into three groups for presentation: geochemistry of magma and associated volcanic rocks, geochemistry of hydrothermal solutions, and geochemistry of hydrothermal alteration. (MHR)

  18. 14Reviews in Mineralogy & Geochemistry Vol. 78 pp. 543-603, 2014

    E-Print Network [OSTI]

    Duffy, Thomas S.

    14Reviews in Mineralogy & Geochemistry Vol. 78 pp. 543-603, 2014 Copyright © Mineralogical Society Earth materials, relevant to construct a mineralogical model of the interior of our planet

  19. Soils and Brine Geochemistry and Mineralogy of Hyperarid Desert Playa, Ouargla Basin,

    E-Print Network [OSTI]

    Ahmad, Sajjad

    Soils and Brine Geochemistry and Mineralogy of Hyperarid Desert Playa, Ouargla Basin, Algerian. The chemical and mineralogical specificity of this hyperarid ecosystem has been compared to other areas under

  20. 1Reviews in Mineralogy & Geochemistry Vol. 72 pp. 1-4, 2010

    E-Print Network [OSTI]

    Zhang, Youxue

    1Reviews in Mineralogy & Geochemistry Vol. 72 pp. 1-4, 2010 Copyright © Mineralogical Society and Kinetics." The other was a Reviews of Mineralogy volume edited by Lasaga and Kirkpatrick (1981) titled

  1. Neutral carbohydrate geochemistry of particulate material (trap and core sediments) in an eutrophic lake (Aydat,

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    Neutral carbohydrate geochemistry of particulate material (trap and core sediments) in an eutrophic Carbohydrate compositions were determined on sinking particles and core samples from eutrophic lake Aydat; Eutrophic lake; Aydat lake 1. Introduction Polysaccharides are common structural and storage polymers

  2. GEOCHEMISTRY AND ISOTOPE HYDROLOGY OF GROUNDWATERS IN THE STRIPA GRANITE RESULTS AND PRELIMINARY INTERPRETATION

    E-Print Network [OSTI]

    Fritz, P.

    2011-01-01T23:59:59.000Z

    S. Italy). In Isotope Hydrology, IAEA Symposium. Sm-129/53,isotopic variations in hydrology. At. Energy Rev. 14: 621-70 GEOCHEMISTRY AND ISOTOPE HYDROLOGY OF GROUNDWATERS IN THE

  3. Interactions between mantle plumes and mid-ocean ridges : constraints from geophysics, geochemistry, and geodynamical modeling

    E-Print Network [OSTI]

    Georgen, Jennifer E

    2001-01-01T23:59:59.000Z

    This thesis studies interactions between mid-ocean ridges and mantle plumes using geophysics, geochemistry, and geodynamical modeling. Chapter 1 investigates the effects of the Marion and Bouvet hotspots on the ultra-slow ...

  4. Geochemistry and arsenic mobilisation in groundwaters of the Pannonian Basin (Hungary and Romania).

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    , calin.baciu@enviro.ubbcluj.ro, +40 (0) 264 307030 Hug, S.J.,1 , Stephan.hug@eawag.ch, +41 (0) 44 823 and Pollutant Dynamics, ETH Zurich, Switzerland * Corresponding author. The geochemistry of groundwaters from

  5. Ground-water hydrogeology and geochemistry of a reclaimed lignite surface mine

    E-Print Network [OSTI]

    Pollock, Clifford Ralph

    1982-01-01T23:59:59.000Z

    GROUND-WATER HYDROGEOLOGY AND GEOCHEMISTRY OF A RECLAIMED LIGNITE SURFACE MINE A Thesis by CLIFFORD RALPH POLLOCK Submitted to the Graduate College of Texas A&M University in partial fulfillment of the requirement for the degree of MASTER... OF SCIENCE August 1982 Major Subject: Geology GROUND-WATER HYDROGEOLOGY AND GEOCHEMISTRY OF A RECLAIMED LIGNITE SURFACE MINE A Thesis by CLIFFORD RALPH POLLOCK Approved as to sty1e and content by: (Chairman of Committee) ember) (Member (Member) F...

  6. Salinity tolerance and avoidance in juvenile paddlefish, Polyodon spathula

    E-Print Network [OSTI]

    Vignali, Carl R

    1999-01-01T23:59:59.000Z

    tank was used to obtain data on salinity avoidance behavior. Bioassays of high-salinity tolerance indicated 24-h and 96-h lethal limits near 10 and 8 ppt, respectively, whether the fish had been acclimated to freshwater or water with 5-ppt salinity...

  7. Gas Geochemistry of the Dogger Geothermal Aquifer (Paris Basin, France)

    SciTech Connect (OSTI)

    Criaud, A.; Fouillac, C.; Marty, B.; Brach, M.; Wei, H.F.

    1987-01-20T23:59:59.000Z

    The low enthalpy program developed in the Paris Basin provides the opportunity for studying the gas geochemistry of the calcareous aquifer of the Dogger. Hydrocarbons and CO{sub 2} are mainly biogenic, He displays high concentrations. He, Ar and N{sub 2} have multiple origins (radioactive decay, atmospheric migration, biochemical processes). The distribution of the gases in the zones of the basin varies in relation to the general chemistry, sedimentology and hydrodynamics. The gas geothermometers do not apply to this environment but useful estimations of the redox potential of the fluid can be derived from CO{sub 2}/CH{sub 4} and N{sub 2}/NH{sub 4}{sup +} ratios. H{sub 2} and H{sub 2}S are involved in corrosion processes and scaling in the pipes. 12 refs., 3 figs., 2 tabs.

  8. Favorable Geochemistry from Springs and Wells in COlorado

    SciTech Connect (OSTI)

    Zehner, Richard E.

    2012-02-01T23:59:59.000Z

    Citation Information: Originator: Geothermal Development Associates, Reno Nevada Originator: United States Geological Survey (USGS) Originator: Colorado Geological Survey Publication Date: 2012 Title: Favorable Geochemistry Edition: First Publication Information: Publication Place: Reno Nevada Publisher: Geothermal Development Associates, Reno, Nevada Description: This layer contains favorable geochemistry for high-temperature geothermal systems, as interpreted by Richard "Rick" Zehner. The data is compiled from the data obtained from the USGS. The original data set combines 15,622 samples collected in the State of Colorado from several sources including 1) the original Geotherm geochemical database, 2) USGS NWIS (National Water Information System), 3) Colorado Geological Survey geothermal sample data, and 4) original samples collected by R. Zehner at various sites during the 2011 field season. These samples are also available in a separate shapefile FlintWaterSamples.shp. Data from all samples were reportedly collected using standard water sampling protocols (filtering through 0.45 micron filter, etc.) Sample information was standardized to ppm (micrograms/liter) in spreadsheet columns. Commonly-used cation and silica geothermometer temperature estimates are included. Spatial Domain: Extent: Top: 4515595.841032 m Left: 149699.513964 m Right: 757959.309388 m Bottom: 4104156.435530 m Contact Information: Contact Organization: Geothermal Development Associates, Reno, Nevada Contact Person: Richard “Rick” Zehner Address: 3740 Barron Way City: Reno State: NV Postal Code: 89511 Country: USA Contact Telephone: 775-737-7806 Spatial Reference Information: Coordinate System: Universal Transverse Mercator (UTM) WGS’1984 Zone 13N False Easting: 500000.00000000 False Northing: 0.00000000 Central Meridian: -105.00000000 Scale Factor: 0.99960000 Latitude of Origin: 0.00000000 Linear Unit: Meter Datum: World Geodetic System 1984 (WGS ’1984) Prime Meridian: Greenwich Angular Unit: Degree Digital Form: Format Name: Shape file

  9. Calcite Reaction Kinetics in Saline Waters

    E-Print Network [OSTI]

    Finneran, David

    2012-02-14T23:59:59.000Z

    minerals with formation waters are of particular importance in the storage of carbon dioxide and other waste fluids injected into depleted oil/gas reservoirs and/or saline formations (see reviews of Gozalpour et al., 2005; Riahi et al., 2004; Voormeij... and Simandl, 2004; White et al., 2003; Yamasaki, 2003). In particular, the carbonate mineral-water-waste interactions will greatly influence the physical properties (e.g. porosity, permeability) of the subsurface. In order to accurately predict formation...

  10. Use of outcrop analogues to predict lithology influence on the seismic signature Kathleen Baker* and Mike Batzle, Colorado School of Mines, Richard Gibson, Texas A&M University

    E-Print Network [OSTI]

    with outcrop studies, well log and seismic interpretation of deep-water sediments, forward and inverse modeling the interpretation of subsurface information such as well logs, seismic data and regional geologic models. Here we the influence of lithology on the seismic signature. Method To better interpret seismic DHIs it is essential

  11. Postdoctoral fellowship in ore-deposit geology/igneous geochemistry Marie-Curie Initial Training Network ABYSS (ER1)

    E-Print Network [OSTI]

    Demouchy, Sylvie

    Postdoctoral fellowship in ore-deposit geology/igneous geochemistry Marie-Curie Initial Training Network ABYSS (ER1) Training network on reactive geological systems from the mantle to the abyssal sub-Cu-PGE deposits Requirements: Candidates must hold PhD in geology/geochemistry This fellowship is for a period

  12. Petrology and geochemistry of Yamato 984028: a cumulate lherzolitic shergottite with affinities to Y 000027, Y 000047,

    E-Print Network [OSTI]

    Perfect, Ed

    Petrology and geochemistry of Yamato 984028: a cumulate lherzolitic shergottite with affinities 2010 Elsevier B.V. and NIPR All rights reserved. Keywords : Lherzolitic ; Shergottite ; Petrology://ees.elsevier.com/polar/ + MODEL Please cite this article in press as: Amy J.V. Riches et al., Petrology and geochemistry of Yamato

  13. Property:SalinityHIgh | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to:Ezfeedflag Jump to:ID8/Organization RAPID/Contact/ID8/Positionmaterial JumpSalinityHIgh Jump

  14. Modeling CO2 Sequestration in a Saline Reservoir and Depleted...

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

    Modeling CO 2 Sequestration in a Saline Reservoir and Depleted Oil Reservoir to Evaluate The Regional CO 2 Sequestration Potential of The Ozark Plateau Aquifer System,...

  15. alluvial saline sodic: Topics by E-print Network

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

    ability to discriminate and map selected symptoms of salinity in a dryland agricultural area in southern Australia. The symptoms mapped are widespread in this environment: the...

  16. Original article Effects of sodium chloride salinity on root growth

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    either 50 or 250 mM NaCl. Both moderate and high salinity treatment strongly altered root elongation. In contrast, specific respiration of roots was unaffected by the moderate salinity treatment while ecosystems [11].The effects of snow melt have been documented for wetland ecosystems [14] but

  17. Salinity Budget and WRAP Salinity Simulation Studies of the Brazos River/Reservoir System

    E-Print Network [OSTI]

    Wurbs, Ralph; Lee, Chihun

    Concentrations from the Salinity Budget Dataset .................................................. 127 6.7 Statistics for Concentrations at Graford Gage (TM Option 1, Lag Option 1) ........................ 127 6.8 Statistics for Concentrations at Graford Gage... (TM Option 2, Lag Option 1) ........................ 128 6.9 Statistics for Possum Kingdom Storage Concentrations (TM Option 1, Lag Option 1) ....... 128 6.10 Statistics for Possum Kingdom Storage Concentrations (TM Option 2, Lag Option 1...

  18. 11Reviews in Mineralogy & Geochemistry Vol. 68, pp. XXX-XXX, 2007

    E-Print Network [OSTI]

    11Reviews in Mineralogy & Geochemistry Vol. 68, pp. XXX-XXX, 2007 Copyright © Mineralogical Society, mineralogy, and isotopic distributions of oxygen in cometary materials can provide unique insights have been linked to short-period comets by their unequilibrated mineralogy, fragile structure, fine

  19. Thursday, March 15, 2007 POSTER SESSION II: MARS SEDIMENTS AND GEOCHEMISTRY: ANALOGS AND MINERALOGY

    E-Print Network [OSTI]

    Rathbun, Julie A.

    Thursday, March 15, 2007 POSTER SESSION II: MARS SEDIMENTS AND GEOCHEMISTRY: ANALOGS AND MINERALOGY D. L. Geochemical and Mineralogical Analysis of a "Simple" Evaporite with Organic Carbon and Colorado provides a setting with chemical and mineralogical characteristics relevant to what may be found

  20. 2Reviews in Mineralogy & Geochemistry Vol. 75 pp. 7-46, 2013

    E-Print Network [OSTI]

    Wang, Xiaorui "Ray"

    2Reviews in Mineralogy & Geochemistry Vol. 75 pp. 7-46, 2013 Copyright © Mineralogical Society of America 1529-6466/13/0075-0002$00.00 DOI: 10.2138/rmg.2013.75.2 Carbon Mineralogy and Crystal Chemistry and thus is unique in the diversity of its mineralogical roles. Carbon has the ability to bond to itself

  1. 4Reviews in Mineralogy & Geochemistry Vol. 75 pp. 79-107, 2013

    E-Print Network [OSTI]

    Downs, Robert T.

    4Reviews in Mineralogy & Geochemistry Vol. 75 pp. 79-107, 2013 Copyright © Mineralogical Society of silicate minerals in igneous rocks (Bowen 1915, 1928), implies that Earth's crustal mineralogy has changed of the mineralogical record has led to a growing realization that varied physical, chemical, and biological processes

  2. RoBOT: "Rocks Beneath Our Toes" An experiential learning opportunity in mineralogy and geochemistry

    E-Print Network [OSTI]

    Baxter, Ethan F.

    RoBOT: "Rocks Beneath Our Toes" An experiential learning opportunity in mineralogy with Boston University undergraduates to analyze the mineralogy and unravel the unique story that each rock into modern scientific methods of geochemistry and mineralogy and to unlock for them the exciting

  3. ELSEVIER Sedimentary Geology 124 (1999) 131147 UPb ages and geochemistry of granite pebbles from the Devonian

    E-Print Network [OSTI]

    Dörr, Wolfgang

    ELSEVIER Sedimentary Geology 124 (1999) 131­147 U­Pb ages and geochemistry of granite pebbles from 1998 Abstract The geochemical composition of some garnet-bearing biotite granite pebbles within from two samples. The granites have suffered low-grade metamorphism as shown by the development

  4. Carbon geochemistry of serpentinites in the Lost City Hydrothermal System (30N, MAR)

    E-Print Network [OSTI]

    Gilli, Adrian

    Massif (Mid-Atlantic Ridge, 30°N) was exam- ined to characterize carbon sources and speciation in oceanic. The speciation of carbon de- pends on the chemical and physical conditions prevailing in the reservoir, and itsCarbon geochemistry of serpentinites in the Lost City Hydrothermal System (30°N, MAR) Ade

  5. Author's personal copy Tungsten geochemistry and implications for understanding the Earth's interior

    E-Print Network [OSTI]

    Mcdonough, William F.

    Author's personal copy Tungsten geochemistry and implications for understanding the Earth Keywords: tungsten uranium basalt core mantle concentration ratio The concentration of tungsten (W of tungsten (W) was sequestered into the core (Jagoutz et al., 1979; Sun, 1982; Newsom and Palme, 1984

  6. tice sites of calcium carbonate and affect Mars' soil geochemistry, and calcium carbonate can

    E-Print Network [OSTI]

    Kounaves, Samuel P.

    tice sites of calcium carbonate and affect Mars' soil geochemistry, and calcium carbonate can sample. 18. Estimation of the concentration of calcium carbonate in the sample is uncertain because qualification model (17). Other carbonates have decomposition temperatures that are lower than that of calcite

  7. SPATIAL FACTOR ANALYSIS OF STREAM SEDIMENT GEOCHEMISTRY DATA FROM SOUTH GREENLAND

    E-Print Network [OSTI]

    SPATIAL FACTOR ANALYSIS OF STREAM SEDIMENT GEOCHEMISTRY DATA FROM SOUTH GREENLAND Allan A. Nielsen1 and Greenland, Thoravej 8, DK-2400 København NV, Denmark. ast@geus.dk SUMMARY This paper describes from South Greenland. Kriged MAF images are compared with kriged images based on varimax rotated

  8. Organic Geochemistry of the CenomanianTuronian Bahloul Formation Petroleum Source Rock, Central and Northern Tunisia

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    1 Organic Geochemistry of the Cenomanian­Turonian Bahloul Formation Petroleum Source Rock, Central and around diapirs of the Triassic salt. Key words: Organic matter, Petroleum Source Rock, Cenomanian (TOC) determination, Rock-Eval pyrolysis, extractable organic matter content (EOM) fractionation

  9. Abstract, International Applied Geochemistry Symposium, 2009 Peat groundwater as a medium for surficial geochemical exploration

    E-Print Network [OSTI]

    Abstract, International Applied Geochemistry Symposium, 2009 1 Peat groundwater as a medium-mail: stew.hamilton@ontario.ca) ABSTRACT: Kimberlite-specific chemical responses are visible in shallow peat and migrated through the Tyrell Sea sediment into shallow peat groundwater. The presence of elevated values

  10. Geochemistry of peat over kimberlites in the Attawapiskat area, James Bay Lowlands, northern Canada

    E-Print Network [OSTI]

    Geochemistry of peat over kimberlites in the Attawapiskat area, James Bay Lowlands, northern Canada by peatlands. Peat samples were examined in the Attawapiskat area, a region of discontinuous permafrost, where more than 19 kimberlite pipes have been found beneath a cover of peat (2­4 m thick) and Quaternary

  11. Rare sulfur and triple oxygen isotope geochemistry of volcanogenic sulfate aerosols

    E-Print Network [OSTI]

    Bindeman, Ilya N.

    Rare sulfur and triple oxygen isotope geochemistry of volcanogenic sulfate aerosols I.N. Bindeman a of Technology, Pasadena, CA, USA c Department of Earth and Planetary Sciences, McGill University, Montreal, Que., Canada d Department of Geology and Earth System Science Interdisciplinary Center, University of Maryland

  12. Effects of environmental salinity and dietary protein levels on digestibility in four species of penaeid shrimp 

    E-Print Network [OSTI]

    Coelho, Silvio Romero de C.

    1984-01-01T23:59:59.000Z

    at four salinities. 52 Apparent digestibility for Penaeus joponious fed three diets at four salinities. 53 VIII Apparent digestibility for Penaeus sty Iirost~s fed three diets at four salinities. 54 Apparent digestibility for Penaeus vannamei fed... digestibility for Penaeus sty Hrost~s fed three diets at four salinities 58 XIII Protein digestibility for Penaeus oannamei fed three diets at four salinities. 59 Apparent digestibility for four penaeid shrimp fed a 20% protein diet at four salinities...

  13. GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS, VOL. ???, XXXX, DOI:10.1029/, The influence of non-uniform ambient noise on1

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS, VOL. ???, XXXX, DOI:10.1029/, The influence of non, Institute of Geophysics, ETH Zurich, Sonneggstrasse 5, Zurich, Switzerland. T. Nissen-Meyer, Institute of Geophysics, ETH Zurich, Sonneggstrasse 5, Zurich, Switzerland. Olaf Schenk, Institute of Computational

  14. Remedial Action Plan and Site Design for Stabilization of the Inactive Uranium Mill Tailings Sites at Slick Rock, Colorado: Appendix B to Attachment 3, Lithologic logs and monitor well construction information. Final report

    SciTech Connect (OSTI)

    NONE

    1995-09-01T23:59:59.000Z

    This volume contains lithology logs and monitor well construction information for: NC processing site; UC processing site; and Burro Canyon disposal site. This information pertains to the ground water hydrology investigations which is attachment 3 of this series of reports.

  15. Implications of Carbonate Petrology and Geochemistry for the Origin of Coal Balls from the Kalo Formation (Moscovian, Pennsylvanian) of Iowa

    E-Print Network [OSTI]

    Jones, Courtney

    2012-10-19T23:59:59.000Z

    IMPLICATIONS OF CARBONATE PETROLOGY AND GEOCHEMISTRY FOR THE ORIGIN OF COAL BALLS FROM THE KALO FORMATION (MOSCOVIAN, PENNSYLVANIAN) OF IOWA A Thesis by COURTNEY PAGE JONES Submitted to the Office of Graduate Studies of Texas A...&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE August 2012 Major Subject: Geology IMPLICATIONS OF CARBONATE PETROLOGY AND GEOCHEMISTRY FOR THE ORIGIN OF COAL BALLS FROM THE KALO FORMATION...

  16. Migration and trapping of CO? in saline aquifers

    E-Print Network [OSTI]

    MacMinn, Christopher William

    2012-01-01T23:59:59.000Z

    Mitigation of climate change requires a reduction in atmospheric carbon dioxide (C0 2) emissions. One promising tool for achieving this is the large-scale injection of CO2 into deep saline aquifers. After injection, upward ...

  17. Temperature and salinity variability in thermohaline staircase layers

    E-Print Network [OSTI]

    Stuebe, David Allen

    2005-01-01T23:59:59.000Z

    A moored profiler record from the western tropical North Atlantic provides the first continuous time series of temperature, salinity and velocity profiles in a thermohaline staircase. Variations in the intensity of layering ...

  18. Mark your Calendars Water Supply, Agriculture and Salinity Management Workshop

    E-Print Network [OSTI]

    Johnson, Eric E.

    presentations. The committee will do their best to accommodate oral presenters. Hotel Information: The Esmeralda-State Salinity Coalition and Coachella Valley Water District ESMERALDA RESORT AND SPA 44-400 INDIAN WELLS LANE

  19. Geosynthetics in a salinity-gradient solar pond environment

    SciTech Connect (OSTI)

    Lichwardt, M.A.; Comer, A.I.

    1997-11-01T23:59:59.000Z

    This paper describes the latest in salinity-gradient solar pond lining systems. The high-temperature, high-salinity environment unique to a salinity-gradient solar pond resulted in failure of the geomembrane liner at the El Paso Solar Pond Test Facility after only eight years of operation. Research involved in pond reconstruction led to the selection of a lining system consisting of a flexible polypropylene (PP) geomembrane for the sidewalls and a specially formulated geosynthetic clay liner (GCL) on the bottom of the pond. The two liners have been installed and a comprehensive test program is being conducted to measure their performance. The environment encountered in a salinity-gradient solar pond will be discussed as well as material selection criteria and the design of the two liners. Preliminary results of the GCL performance monitoring will also be presented.

  20. Migration of saline solutions in variably saturated porous media

    E-Print Network [OSTI]

    Selker, John

    more than 4 million liters of highly saline solutions have leaked from radioactive waste storage tanks environments; it is uncommon for concentrations resulting from agrochemicals and other contaminants to 0169

  1. Validation of Innovative Exploration Technologies for Newberry Volcano: Geochemistry data from 55-29 and 46-16 wells at Newberry 2012

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

    Jaffe, Todd

    Validation of Innovative Exploration Technologies for Newberry Volcano: Geochemistry data from 55-29 and 46-16 wells at Newberry 2012

  2. Diagnosis and Management of Salinity Problems In Irrigated Pecan Productions

    E-Print Network [OSTI]

    Miyamoto, S.

    field test conducted in a citrus orchard shows improved salt leaching under mulch. Table 3. The target leaching fraction (LF) to control soil salinity below 2.5 dS m -1 in the saturation extract. Irrig. Water salinity sandy clayey sandy clayey d.... Miyamoto Professor and Soil Scientist Texas A&M University Agricultural Research Center at El Paso Introduction Pecans, along with Almonds and Walnuts, are among the salt sensitive tree crops currently grown under irrigation. Yet, many...

  3. Agricultural Losses from Salinity in California’s Sacramento-San Joaquin Delta

    E-Print Network [OSTI]

    Medellín-Azuara, Josué; Howitt, Richard E.; Hanak, Ellen; Lund, Jay R.; Fleenor, William E.

    2014-01-01T23:59:59.000Z

    hydrodynamic and salinity transport modeling of the Sacramento–San Joaquinhydrodynamic and salinity transport modeling to provide irriga- tion water salinity levels for various locations in California’s Sacramento–San Joaquinhydrodynamic, water salinity, and eco- nomic models can provide insights into controversial management issues. KEY WORDS Sacramento–San Joaquin

  4. Convective stability analysis of the long-term storage of carbon dioxide in deep saline aquifers

    E-Print Network [OSTI]

    Zhang, Dongxiao

    formations, such as unmineable coal beds, depleting oil reservoirs, depleting gas reservoirs, and deep saline

  5. Carbon-14 geochemistry at the Savannah River Site

    SciTech Connect (OSTI)

    Roberts, Kimberly A.; Kaplan, Daniel I.

    2013-05-10T23:59:59.000Z

    Carbon-14 is among the key radionuclides driving risk at the E-Area Low-Level Waste Disposal Facility on the Savannah River Site (SRS). Much of this calculated risk is believed to be the result of having to make conservative assumptions in risk calculations because of the lack of site-specific data. The original geochemical data package (Kaplan 2006) recommended that performance assessments and composite analyses for the SRS assume that {sup 14}C did not sorbed to sediments or cementitious materials, i.e., that C-14 K{sub d} value (solid:liquid concentration ratio) be set to 0 mL/g (Kaplan 2006). This recommendation was based primarily on the fact that no site-specific experimental work was available and the assumption that the interaction of anionic {sup 14}C as CO{sub 2}{sup 2-}) with similarly charged sediments or cementitious materials would be minimal. When used in reactive transport equations, the 0 mL/g Kd value results in {sup 14}C not interacting with the solid phase and moving quickly through the porous media at the same rate as water. The objective of this study was to quantify and understand how aqueous {sup 14}C, as dissolved carbonate, sorbs to and desorbs from SRS sediments and cementitious materials. Laboratory studies measuring the sorption of {sup 14}C, added as a carbonate, showed unequivocally that {sup 14}C-carbonate K{sub d} values were not equal to 0 mL/g for any of the solid phases tested, but they required several months to come to steady state. After six months of contact, the apparent K{sub d} values for a clayey sediment was 3,000 mL/g, for a sandy sediment was 10 mL/g, for a 36-year-old concrete was 30,000 mL/g, and for a reducing grout was 40 mL/g. Furthermore, it was demonstrated that (ad)sorption rates were appreciably faster than desorption rates, indicating that a kinetic sorption model, as opposed to the steady-state K{sub d} model, may be a more accurate description of the {sup 14}C-carbonate sorption process. A second study demonstrated that the {sup 14}C-carbonate sorbed very strongly onto the various materials and could not be desorbed by anion exchanged with high concentrations of carbonate or nitrate. High phosphate concentrations were able to desorb {sup 14}C-carbonate from the 36-year-old concrete sample, but not the clayey sediment sample. Together these geochemistry studies support the use of non-zero K{sub d} values in risk calculations on the SRS. For performance assessment (PA) calculations, {sup 14}C would be moving with the groundwater, remaining in contact with sediment for days, not months. Therefore for purposes of SRS risk calculations, it is appropriate to select sorption values after a couple days of contact, departing from the traditional definition that states K{sub d} values reflect the system under steady state conditions. Such an “apparent K{sub d} value,” would be expected to provide a better (and more conservative) estimate of what to expect under SRS PA conditions. Based on these results, recommended apparent K{sub d} values for use in the PA are 1 mL/g for sandy sediments and 30 mL/g for clayey sediments.

  6. Salinity tolerance in plants: attempts to manipulate ion transport

    E-Print Network [OSTI]

    Vadim Volkov

    2014-11-06T23:59:59.000Z

    Ion transport is the major determining factor of salinity tolerance in plants. A simple scheme of a plant cell with ion fluxes provides basic understanding of ion transport and the corresponding changes of ion concentrations under salinity. The review describes in detail basic principles of ion transport for a plant cell, introduces set of transporters essential for sodium and potassium uptake and efflux, analyses driving forces of ion transport and compares ion fluxes measured by several techniques. Study of differences in ion transport between salt tolerant halophytes and salt-sensitive plants with an emphasis on transport of potassium and sodium via plasma membranes offers knowledge for increasing salinity tolerance. Effects of salt stress on ion transport properties of membranes show huge opportunities for manipulating ion transport. Several attempts to overexpress or knockout ion transporters for changing salinity tolerance are described. Future perspectives are questioned with more attention given to potential candidate ion channels and transporters for altered expression. The potential direction of increasing salinity tolerance by modifying ion channels and transporters is discussed and questioned. An alternative approach from synthetic biology is to modify the existing membrane transport proteins or create new ones with desired properties for transforming agricultural crops. The approach had not been widely used earlier and leads also to theoretical and pure scientific aspects of protein chemistry, structure-function relations of membrane proteins, systems biology and physiology of stress and ion homeostasis.

  7. SOLPOND: a simulation program for salinity gradient solar ponds

    SciTech Connect (OSTI)

    Henderson, J.; Leboeuf, C.M.

    1980-01-01T23:59:59.000Z

    A computer simulation design tool was developed to simulate dynamic thermal performance for salinity gradient solar ponds. Dynamic programming techniques allow the user significant flexibility in analyzing pond performance under realistic load and weather conditions. Finite element techniques describe conduction heat transfer through the pond, earth, and edges. Results illustrate typical thermal performance of salinity gradient ponds. Sensitivity studies of salty pond thermal performance with respect to geometry, load, and optical transmission are included. Experimental validation of the program with an operating pond is also presented.

  8. Influence of Tributaries on Salinity of Amistad International Reservoir

    E-Print Network [OSTI]

    Miyamoto, S.; Yuan, Fasong; Anand, Shilpa

    in this reach might be a result of saline water intrusion, resulting from dissolution of geological salts (Miyamoto et al., 2005). Soil Depth No Overflow Overflow Difference Conductivity of the saturation extract (dS m -1 ) 0 - 1 (cm) 200 10 190 0 - 5 (cm...) 13 - - 1 - 120 (cm) 35 5 30 5 - 15 (cm) 9 0 - 60 (cm) 8 Salinity of soil extract (g L -1 ) 0 - 1 (cm) 200 6 194 0 - 5 (cm) 9 - - 1 - 120 (cm) 24 3 21 5 - 15 (cm) 6 0 - 60 (cm) 6 Salt storage (tons/ha) 2 - 0 - 1 (cm) 10 0.3 10 0 - 1 (cm) 0.5 - - 1...

  9. POSTDOCTORAL FELLOW: BASIN-SCALE MODELING AND SALINITY MANAGEMENT

    E-Print Network [OSTI]

    . If not, please email us at work-at-iwmi@cgiar.org The International Water Management Institute (wwwPOSTDOCTORAL FELLOW: BASIN-SCALE MODELING AND SALINITY MANAGEMENT Tashkent, Uzbekistan Please note: The International Water Management Institute (IWMI) (www.iwmi.org) is looking for a person with a PhD in hydrology

  10. Saline absorption in calcium silicate brick observed by NMR scanning

    E-Print Network [OSTI]

    Eindhoven, Technische Universiteit

    Saline absorption in calcium silicate brick observed by NMR scanning L. Pel #3; , K. Kopinga #3 in calcium-silicate brick was investigated by nuclear magnetic resonance scanning. This method hasCl solution in a calcium silicate brick will be discussed. 2 Theory If gravity is neglected, the isothermal

  11. Delta Hydrodynamics and Water Salinity with Future Conditions

    E-Print Network [OSTI]

    Pasternack, Gregory B.

    , Comparing Futures for the Sacramento-San Joaquin Delta, prepared by a team of researchers from the CenterDelta Hydrodynamics and Water Salinity with Future Conditions Technical Appendix C William E of California All rights reserved San Francisco, CA Short sections of text, not to exceed three paragraphs, may

  12. The budgets of heat and salinity in NEMO M. Hieronymus

    E-Print Network [OSTI]

    Nycander, Jonas

    of the ocean is seen to be dominated by penetrative shortwave radiation, which is so influ- ential that we Keywords: Heat budget Salinity budget NEMO Isoneutral diffusion Shortwave penetration a b s t r a c in the Nucleus for European Modelling of the Ocean (NEMO) model. It is seen that the heat fluxes in NEMO

  13. Study of Chelyabinsk LL5 meteorite fragment with a light lithology and its fusion crust using Mössbauer spectroscopy with a high velocity resolution

    SciTech Connect (OSTI)

    Maksimova, Alevtina A.; Petrova, Evgeniya V.; Grokhovsky, Victor I. [Department of Physical Techniques and Devices for Quality Control, Institute of Physics and Technology, Ural Federal University, Ekaterinburg, 620002 (Russian Federation); Oshtrakh, Michael I., E-mail: oshtrakh@gmail.com; Semionkin, Vladimir A. [Department of Physical Techniques and Devices for Quality Control, Institute of Physics and Technology, Ural Federal University, Ekaterinburg, 620002, Russian Federation and Department of Experimental Physics, Institute of Physics and Technology, Ura (Russian Federation)

    2014-10-27T23:59:59.000Z

    Study of Chelyabinsk LL5 ordinary chondrite fragment with a light lithology and its fusion crust, fallen on February 15, 2013, in Russian Federation, was carried out using Mössbauer spectroscopy with a high velocity resolution. The Mössbauer spectra of the internal matter and fusion crust were fitted and all components were related to iron-bearing phases such as olivine, pyroxene, troilite, Fe-Ni-Co alloy, and chromite in the internal matter and olivine, pyroxene, troilite, Fe-Ni-Co alloy, and magnesioferrite in the fusion crust. A comparison of the content of different phases in the internal matter and in the fusion crust of this fragment showed that ferric compounds resulted from olivine, pyroxene, and troilite combustion in the atmosphere.

  14. Plant Water Use and Growth in Response to Soil Salinity in Irrigated Agriculture

    E-Print Network [OSTI]

    Runkle, Benjamin Reade

    2009-01-01T23:59:59.000Z

    Journal of Sustainable Agriculture, 27(1): 5-50. Feng, G. ,Salinity in Irrigated Agriculture by Benjamin Reade KrepsSalinity in Irrigated Agriculture by Benjamin Reade Kreps

  15. Addressing agricultural salinity in the American West : harnessing behavioral diversity to institutional design

    E-Print Network [OSTI]

    Kock, Beaudry E. (Beaudry Evan)

    2010-01-01T23:59:59.000Z

    Salinity accumulation in the Lower Arkansas Basin (LAB) of Colorado threatens environmental quality, the agricultural economy and the potential for efficient reuse of water. Salinity is a threat to "hydraulic sustainability", ...

  16. The influence of salinity on the mechanical behavior of high plasticity soils

    E-Print Network [OSTI]

    Fahy, Brian Patrick

    2014-01-01T23:59:59.000Z

    This thesis investigates the influence of salinity on the mechanical behavior of smectitic rich high plasticity soils resedimented with pore fluid salinities ranging from 0 to 256 g/L. An extensive laboratory testing program ...

  17. Harmonic analysis of climatological sea surface salinity Tim P. Boyer and Sydney Levitus

    E-Print Network [OSTI]

    Harmonic analysis of climatological sea surface salinity Tim P. Boyer and Sydney Levitus Ocean: Boyer, T. P., and S. Levitus, Harmonic analysis of climatological sea surface salinity, J. Geophys. Res

  18. Agricultural Losses from Salinity in California’s Sacramento-San Joaquin Delta

    E-Print Network [OSTI]

    Medellín-Azuara, Josué; Howitt, Richard E.; Hanak, Ellen; Lund, Jay R.; Fleenor, William E.

    2014-01-01T23:59:59.000Z

    hydrodynamic and salinity transport modeling of the Sacramento–San Joaquin Delta: sea level rise and water diversion effects.

  19. Effect of permeability anisotropy on buoyancy-driven flow for CO2 sequestration in saline aquifers

    E-Print Network [OSTI]

    Firoozabadi, Abbas

    ) in deep saline aquifers is considered one of the most effective methods for carbon sequestration., 48, W09539, doi:10.1029/2012WR011939.* 1. Introduction [2] Carbon sequestration in deep salineEffect of permeability anisotropy on buoyancy-driven flow for CO2 sequestration in saline aquifers

  20. Effects of correcting salinity with altimeter measurements in an equatorial Pacific ocean model

    E-Print Network [OSTI]

    van Leeuwen, Peter Jan

    Effects of correcting salinity with altimeter measurements in an equatorial Pacific ocean model in a tropical Pacific ocean model run for the period 1993­1997. Salinity and temperature corrections salinity with altimeter measurements in an equatorial Pacific ocean model, J. Geophys. Res., 107(C12), 8001

  1. Conservative behavior of uranium vs. salinity in Arctic sea ice and brine Christelle Not a,

    E-Print Network [OSTI]

    Available online 23 December 2011 Keywords: Uranium Salinity Sea ice Brine Seawater Arctic UraniumConservative behavior of uranium vs. salinity in Arctic sea ice and brine Christelle Not a, ,1 disequilibrium The conservative behavior of uranium (U) with respect to salinity in open ocean waters is widely

  2. Re-evaluating the 238 U-salinity relationship in seawater: Implications for the

    E-Print Network [OSTI]

    Buesseler, Ken

    ) is still the most widely referenced value for determining uranium concentrations in seawater from salinityRe-evaluating the 238 U-salinity relationship in seawater: Implications for the 238 U­234 Th form 13 July 2011 Accepted 14 July 2011 Available online 23 July 2011 Keywords: Uranium Salinity

  3. Geochemistry, geochronology, and cathodoluminescence imagery of the Salihli and Turgutlu granites (central Menderes Massif, western Turkey): Implications for

    E-Print Network [OSTI]

    Geochemistry, geochronology, and cathodoluminescence imagery of the Salihli and Turgutlu granites-type, peraluminous granites (Salihli and Turgutlu) that intrude the Alasehir detachment which bounds the northern Mediterranean floor along the Hellenic trench. In situ Th­Pb ion microprobe monazite ages from the granites

  4. EMSL Geochemistry, Biogeochemistry and Subsurface Science-Science Theme Advisory Panel Meeting

    SciTech Connect (OSTI)

    Brown, Gordon E.; Chaka, Anne; Shuh, David K.; Roden, Eric E.; Werth, Charles J.; Hess, Nancy J.; Felmy, Andrew R.; Rosso, Kevin M.; Baer, Donald R.; Bailey, Vanessa L.; Bowden, Mark E.; Grate, Jay W.; Hoyt, David W.; Kuprat, Laura R.; Lea, Alan S.; Mueller, Karl T.; Oostrom, Martinus; Orr, Galya; Pasa-Tolic, Ljiljana; Plata, Charity; Robinson, E. W.; Teller, Raymond G.; Thevuthasan, Suntharampillai; Wang, Hongfei; Wiley, H. S.; Wilkins, Michael J.

    2011-08-01T23:59:59.000Z

    This report covers the topics of discussion and the recommendations of the panel members. On December 8 and 9, 2010, the Geochemistry, Biogeochemistry, and Subsurface Science (GBSS) Science Theme Advisory Panel (STAP) convened for a more in-depth exploration of the five Science Theme focus areas developed at a similar meeting held in 2009. The goal for the fiscal year (FY) 2011 meeting was to identify potential topical areas for science campaigns, necessary experimental development needs, and scientific members for potential research teams. After a review of the current science in each of the five focus areas, the 2010 STAP discussions successfully led to the identification of one well focused campaign idea in pore-scale modeling and five longer-term potential research campaign ideas that would likely require additional workshops to identify specific research thrusts. These five campaign areas can be grouped into two categories: (1) the application of advanced high-resolution, high mass accuracy experimental techniques to elucidate the interplay between geochemistry and microbial communities in terrestrial ecosystems and (2) coupled computation/experimental investigations of the electron transfer reactions either between mineral surfaces and outer membranes of microbial cells or between the outer and inner membranes of microbial cells.

  5. Saline as the Sole Contrast Agent for Successful MRI-guided Epidural Injections

    SciTech Connect (OSTI)

    Deli, Martin, E-mail: martin.deli@web.de [University of Witten/Herdecke, Department of Radiology and Microtherapy, Groenemeyer Institute for Microtherapy (GIMT) (Germany); Fritz, Jan, E-mail: jfritz9@jhmi.edu [Johns Hopkins University School of Medicine, Russell H. Morgan Department of Radiology and Radiological Science (United States); Mateiescu, Serban, E-mail: mateiescu@microtherapy.de; Busch, Martin, E-mail: busch@microtherapy.de [University of Witten/Herdecke, Department of Radiology and Microtherapy, Groenemeyer Institute for Microtherapy (GIMT) (Germany); Carrino, John A., E-mail: jcarrin2@jhmi.edu [Johns Hopkins University School of Medicine, Russell H. Morgan Department of Radiology and Radiological Science (United States); Becker, Jan, E-mail: j.becker@microtherapy.de; Garmer, Marietta, E-mail: garmer@microtherapy.de; Groenemeyer, Dietrich, E-mail: dg@microtherapy.de [University of Witten/Herdecke, Department of Radiology and Microtherapy, Groenemeyer Institute for Microtherapy (GIMT) (Germany)

    2013-06-15T23:59:59.000Z

    Purpose. To assess the performance of sterile saline solution as the sole contrast agent for percutaneous magnetic resonance imaging (MRI)-guided epidural injections at 1.5 T. Methods. A retrospective analysis of two different techniques of MRI-guided epidural injections was performed with either gadolinium-enhanced saline solution or sterile saline solution for documentation of the epidural location of the needle tip. T1-weighted spoiled gradient echo (FLASH) images or T2-weighted single-shot turbo spin echo (HASTE) images visualized the test injectants. Methods were compared by technical success rate, image quality, table time, and rate of complications. Results. 105 MRI-guided epidural injections (12 of 105 with gadolinium-enhanced saline solution and 93 of 105 with sterile saline solution) were performed successfully and without complications. Visualization of sterile saline solution and gadolinium-enhanced saline solution was sufficient, good, or excellent in all 105 interventions. For either test injectant, quantitative image analysis demonstrated comparable high contrast-to-noise ratios of test injectants to adjacent body substances with reliable statistical significance levels (p < 0.001). The mean table time was 22 {+-} 9 min in the gadolinium-enhanced saline solution group and 22 {+-} 8 min in the saline solution group (p = 0.75). Conclusion. Sterile saline is suitable as the sole contrast agent for successful and safe percutaneous MRI-guided epidural drug delivery at 1.5 T.

  6. Geochemistry and materials studies in support of the Magma Energy Extraction Program

    SciTech Connect (OSTI)

    Westrich, H.R.; Weirick, L.J.

    1986-01-01T23:59:59.000Z

    Geochemistry and materials studies are being performed in support of the Magma Energy Extraction Program. The scope of the studies is dictated by the sites under consideration and the designs of the drilling and energy extraction systems. The work has been largely restricted to characterizing magmatic environments at sites of interest and testing engineering materials in laboratory simulated rhyolite magmatic environments. The behavior of 17 commercially available materials has been examined at magmatic conditions. Analysis of reaction products reveal that oxidation, and not sulfidation, is the main corrosion problem for most alloys in rhyolite, and that reaction with other magmatic components is limited. Considerations of corrosion resistance, high-temperature strength, and cost indicate nickel-base superalloys offer the most promise as candidates for use in rhyolitic magma.

  7. Saline County, Missouri: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere IRaghuraji Agro Industries Pvt Ltd Jump to:RoscommonSBY SolutionsChangeOklahoma: Energy708215°,74853°,Saline

  8. USD 307 Ell-Saline Wind Project | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to:Ezfeedflag JumpID-fTri Global Energy LLC Place: Dallas,UGIURDB Ell-Saline Wind Project Jump

  9. A Simple Model for Estimating Water Balance and Salinity of Reservoirs and Outflow

    E-Print Network [OSTI]

    Miyamoto, S; Yuan, F; Anand, Shilpa

    2010-08-23T23:59:59.000Z

    on flow and salinity of the stream and the floodplains. The first part deals with water and salt balance in reservoirs. The primary purpose of the model is to predict outflow salinity from the reservoir storage and inflow information in advance... management strategy, yet the method to predict outflow salinity has not been adequately examined. The study reported here examined the water and salt balance in a reservoir using a two-layer model. This model assumes that inflow blends with the storage...

  10. Analysis of the salinity regime of the Mississippi River - Gulf Outlet Channel

    E-Print Network [OSTI]

    Amstutz, David E

    1964-01-01T23:59:59.000Z

    Intersecting Channel Polynomial Coefficients (A ) n, m A Tendency Summary n, m Average Tidal Lag and Amplitude Change From Gage Station N-140A 16 30 35 LIST OF FIGURES FIGURE NO. PAGE Area Map Mississippi River ? Gulf Outlet Channel Station... of salinity and tidal data gathering stations are shown in Figure 2. The average time required for tidal propagation be- tween these two stations is 5. 0 hours. The sampling programs began at station TABLE 1 ACCURACY OF CHANNEL SALINITY DATA Salinity...

  11. Geological and petrophysical characterization of the Ferron Sandstone for 3-D simulation of a fluvial-deltaic reservoir. Deliverable 2.5.4, Ferron Sandstone lithologic strip logs, Emergy & Sevier Counties, Utah: Volume I

    SciTech Connect (OSTI)

    Allison, M.L.

    1995-12-08T23:59:59.000Z

    Strip logs for 491 wells were produced from a digital subsurface database of lithologic descriptions of the Ferron Sandstone Member of the Mancos Shale. This subsurface database covers wells from the parts of Emery and Sevier Counties in central Utah that occur between Ferron Creek on the north and Last Chance Creek on the south. The lithologic descriptions were imported into a logging software application designed for the display of stratigraphic data. Strip logs were produced at a scale of one inch equals 20 feet. The strip logs were created as part of a study by the Utah Geological Survey to develop a comprehensive, interdisciplinary, and qualitative characterization of a fluvial-deltaic reservoir using the Ferron Sandstone as a surface analogue. The study was funded by the U.S. Department of Energy (DOE) under the Geoscience/Engineering Reservoir Characterization Program.

  12. THE OHIO RIVER VALLEY CO2 STORAGE PROJECT - PRELIMINARY ASSESSMENT OF DEEP SALINE RESERVOIRS AND COAL SEAMS

    SciTech Connect (OSTI)

    Michael J. Mudd; Howard Johnson; Charles Christopher; T.S. Ramakrishnan, Ph.D.

    2003-08-01T23:59:59.000Z

    This report describes the geologic setting for the Deep Saline Reservoirs and Coal Seams in the Ohio River Valley CO{sub 2} Storage Project area. The object of the current project is to site and design a CO{sub 2} injection facility. A location near New Haven, WV, has been selected for the project. To assess geologic storage reservoirs at the site, regional and site-specific geology were reviewed. Geologic reports, deep well logs, hydraulic tests, and geologic maps were reviewed for the area. Only one well within 25 miles of the site penetrates the deeper sedimentary rocks, so there is a large amount of uncertainty regarding the deep geology at the site. New Haven is located along the Ohio River on the border of West Virginia and Ohio. Topography in the area is flat in the river valley but rugged away from the Ohio River floodplain. The Ohio River Valley incises 50-100 ft into bedrock in the area. The area of interest lies within the Appalachian Plateau, on the western edge of the Appalachian Mountain chain. Within the Appalachian Basin, sedimentary rocks are 3,000 to 20,000 ft deep and slope toward the southeast. The rock formations consist of alternating layers of shale, limestone, dolomite, and sandstone overlying dense metamorphic continental shield rocks. The Rome Trough is the major structural feature in the area, and there may be some faults associated with the trough in the Ohio-West Virginia Hinge Zone. The area has a low earthquake hazard with few historical earthquakes. Target injection reservoirs include the basal sandstone/Lower Maryville and the Rose Run Sandstone. The basal sandstone is an informal name for sandstones that overlie metamorphic shield rock. Regional geology indicates that the unit is at a depth of approximately 9,100 ft below the surface at the project site and associated with the Maryville Formation. Overall thickness appears to be 50-100 ft. The Rose Run Sandstone is another potential reservoir. The unit is located approximately 1,100 ft above the basal sandstone and is 100-200 ft thick. The storage capacity estimates for a 20-mile radius from the injection well ranged from 39-78 million tons (Mt) for each formation. Several other oil and gas plays have hydraulic properties conducive for injection, but the formations are generally only 5-50 ft thick in the study area. Overlying the injection reservoirs are thick sequences of dense, impermeable dolomite, limestone, and shale. These layers provide containment above the potential injection reservoirs. In general, it appears that the containment layers are much thicker and extensive than the injection intervals. Other physical parameters for the study area appear to be typical for the region. Anticipated pressures at maximum depths are approximately 4,100 psi based on a 0.45 psi/ft pressure gradient. Temperatures are likely to be 150 F. Groundwater flow is slow and complex in deep formations. Regional flow directions appear to be toward the west-northwest at less than 1 ft per year within the basal sandstone. Vertical gradients are downward in the study area. A review of brine geochemistry indicates that formation fluids have high salinity and dissolved solids. Total dissolved solids ranges from 200,000-325,000 mg/L in the deep reservoirs. Brine chemistry is similar throughout the different formations, suggesting extensive mixing in a mature basin. Unconsolidated sediments in the Ohio River Valley are the primary source of drinking water in the study area.

  13. Exploration Geochemistry

    E-Print Network [OSTI]

    Michelson, David G.

    and environmental constraints. eter Winterburn #12;M D R U Societal demands for mineral resources continue to spur and restrictive policy changes. The discovery of new mineral resources requires increasing risk, increasing costs ­ Global Exploration for Vale. His research interests centre on innovation of cost-effective, robust

  14. Lithologically Controlled | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere I Geothermal Pwer Plant Jump to:Landowners and WindLightingLinthicum, Maryland:source HistoryLite

  15. Spatial delineation of groundwater salinity using deep time domain electromagnetic geophysical measurements: A feasibility study

    E-Print Network [OSTI]

    Gvirtzman, Haim

    , as well as brine, beneath the Judea Desert, Israel. We used the deep time domain electromagnetic (TDEM) is characterized by 5­15 W m, saline groundwater (104 brine, saline and brine) exist in the subsurface within the exploration depth interval of the applied TDEM

  16. MINERALOGY AND GENESIS OF SMECTITES IN AN ALKALINE-SALINE ENVIRONMENT OF PANTANAL WETLAND, BRAZIL

    E-Print Network [OSTI]

    Ahmad, Sajjad

    MINERALOGY AND GENESIS OF SMECTITES IN AN ALKALINE-SALINE ENVIRONMENT OF PANTANAL WETLAND, BRAZIL, Universidade de Sa~o Paulo (USP), Av. Prof. Dr. Lineu Prestes, 338, 05508-900, Sa~o Paulo, Brazil 2 Soil-saline lake of Nhecola^ndia, a sub-region of the Pantanal wetland, Brazil, and then to identify the mechanisms

  17. Electrical properties of saline ices and ice-silicate mixtures: geophysical and astrobiological consequences (Invited)

    E-Print Network [OSTI]

    Stillman, David E.

    MR22A-05 Electrical properties of saline ices and ice-silicate mixtures: geophysical) electrical-properties measurements of laboratory- produced saline ice, salt hydrates, and ice-silicate cutoff. In ice-silicate mixtures, brine channels are evident above the eutectic temperature only when

  18. A Mechanism of Improved Oil Recovery by Low-Salinity Waterflooding in Sandstone Rock

    E-Print Network [OSTI]

    Nasralla, Ramez

    2013-05-02T23:59:59.000Z

    -salinity water has an impact on the rock wettability; the more reduction in water salinity, the more a water-wet rock surface is produced. In addition, NaCl solutions made the rock more water-wet compared to CaCl2 or MgCl2 at the same concentration. Low...

  19. The mechanical behavior of normally consolidated soils as a function of pore fluid salinity

    E-Print Network [OSTI]

    Horan, Aiden James

    2012-01-01T23:59:59.000Z

    Pore fluid salinities in the Gulf of Mexico area can reach levels of 250 grams of salt per liter of pore fluid (g/1). It is now necessary to determine the effect that this salinity level can play on the mechanical behaviors ...

  20. Variation in hydraulic conductivity of mangroves: influence of species, salinity, and nitrogen and phosphorus availability

    E-Print Network [OSTI]

    Ling, Sharon Ewe Mei

    Variation in hydraulic conductivity of mangroves: influence of species, salinity, and nitrogen identity and variation in salinity and nutrient availability influence the hydraulic conductivity of mangroves. Using a fertilization study of two species in Florida, we found that stem hydraulic conductivity

  1. Local and remote impacts of a tropical Atlantic salinity anomaly Juliette Mignot

    E-Print Network [OSTI]

    Local and remote impacts of a tropical Atlantic salinity anomaly Juliette Mignot and Claude, the salinity increase leads to a rapid deepening and cooling of the surface mixed layer. This induces a deepening of the equatorial undercurrent and an intensication of the south equatorial current. A remote

  2. Soil and groundwater characteristics of saline sites supporting boreal mixedwood forests in northern Alberta

    E-Print Network [OSTI]

    Macdonald, Ellen

    Soil and groundwater characteristics of saline sites supporting boreal mixedwood forests September 2009. Lilles, E. B., Purdy, B. G., Chang, S. X. and Macdonald, S. E. 2010. Soil and groundwater, pH, and nutrient and moisture availabilities) and groundwater at six naturally saline sites

  3. Geology and geochemistry of the Geyser Bight Geothermal Area, Umnak Island, Aleutian Islands, Alaska

    SciTech Connect (OSTI)

    Nye, C.J. (Alaska Univ., Fairbanks, AK (USA). Geophysical Inst. Alaska Dept. of Natural Resources, Fairbanks, AK (USA). Div. of Geological and Geophysical Surveys); Motyka, R.J. (Alaska Dept. of Natural Resources, Juneau, AK (USA). Div. of Geological and Geophysical Surveys); Turner, D.L. (Alaska Univ., Fairbanks, AK (USA). Geophysical Inst.); Liss, S.A. (Alaska Dept. of Natural Resources, Fairba

    1990-10-01T23:59:59.000Z

    The Geyser Bight geothermal area is located on Umnak Island in the central Aleutian Islands. It contains one of the hottest and most extensive areas of thermal springs and fumaroles in Alaska, and is only documented site in Alaska with geysers. The zone of hot springs and fumaroles lies at the head of Geyser Creek, 5 km up a broad, flat, alluvial valley from Geyser Bight. At present central Umnak is remote and undeveloped. This report describes results of a combined program of geologic mapping, K-Ar dating, detailed description of hot springs, petrology and geochemistry of volcanic and plutonic rock units, and chemistry of geothermal fluids. Our mapping documents the presence of plutonic rock much closer to the area of hotsprings and fumaroles than previously known, thus increasing the probability that plutonic rock may host the geothermal system. K-Ar dating of 23 samples provides a time framework for the eruptive history of volcanic rocks as well as a plutonic cooling age.

  4. Trace-element geochemistry of coal resource development related to environmental quality and health

    SciTech Connect (OSTI)

    Not Available

    1980-01-01T23:59:59.000Z

    This report assesses for decision makers and those involved in coal resource development the environmental and health impacts of trace-element effects arising from significant increases in the use of coal, unless unusual precautions are invoked. Increasing demands for energy and the pressing need for decreased dependence of the United States on imported oil require greater use of coal to meet the nation's energy needs during the next decade. If coal production and consumption are increased at a greatly accelerated rate, concern arises over the release, mobilization, transportation, distribution, and assimilation of certain trace elements, with possible adverse effects on the environment and human health. It is, therefore, important to understand their geochemical pathways from coal and rocks via air, water, and soil to plants, animals, and ultimately humans, and their relation to health and disease. To address this problem, the Panel on Trace Element Geochemistry of Coal Resource Development Related to Health (PECH) was established. Certain assumptions were made by the Panel to highlight the central issues of trace elements and health and to avoid unwarranted duplication of other studies. Based on the charge to the Panel and these assumptions, this report describes the amounts and distribution of trace elements related to the coal source; the various methods of coal extraction, preparation, transportation, and use; and the disposal or recycling of the remaining residues or wastes. The known or projected health effects are discussed at the end of each section.

  5. A Conceptual Model of the Surface Salinity Distribution in the Oceanic Hadley Cell JOHAN NILSSON AND HEINER KRNICH

    E-Print Network [OSTI]

    Nilsson, Johan

    : The former process acts to build up salinity differences, whereas the circulation in combination with small-scale by pure freshwater and the very high salinity at which pre- cipitation of salt occurs. Rather, the large-scale salinity variations are shaped by the global-scale surface fresh- water flux and the oceanic circulation

  6. The redox and iron-sulfide geochemistry of Salt Pond and the thermodynamic constraints on native magnetotactic bacteria

    E-Print Network [OSTI]

    Canovas, Peter A

    2006-01-01T23:59:59.000Z

    Salt pond is a meromictic system with an outlet to the sea allowing denser seawater to occupy the monimolimnion while the mixolimnion has relatively low salinity and is the site of greater mixing and microbial activity. ...

  7. Simplified 1-D Hydrodynamic and Salinity Transport Modeling of the Sacramento–San Joaquin Delta: Sea Level Rise and Water Diversion Effects

    E-Print Network [OSTI]

    Fleenor, William E.; Bombardelli, Fabian

    2013-01-01T23:59:59.000Z

    Hydrodynamic and Salinity Transport Modeling of the Sacramento–San Joaquinhydrodynamic and salinity transport mod- eling of the Sacramento–San Joaquin

  8. Fluid Dynamics of Carbon Dioxide Disposal into Saline Aquifers

    SciTech Connect (OSTI)

    Garcia, Julio Enrique

    2003-12-18T23:59:59.000Z

    Injection of carbon dioxide (CO{sub 2}) into saline aquifers has been proposed as a means to reduce greenhouse gas emissions (geological carbon sequestration). Large-scale injection of CO{sub 2} will induce a variety of coupled physical and chemical processes, including multiphase fluid flow, fluid pressurization and changes in effective stress, solute transport, and chemical reactions between fluids and formation minerals. This work addresses some of these issues with special emphasis given to the physics of fluid flow in brine formations. An investigation of the thermophysical properties of pure carbon dioxide, water and aqueous solutions of CO{sub 2} and NaCl has been conducted. As a result, accurate representations and models for predicting the overall thermophysical behavior of the system CO{sub 2}-H{sub 2}O-NaCl are proposed and incorporated into the numerical simulator TOUGH2/ECO{sub 2}. The basic problem of CO{sub 2} injection into a radially symmetric brine aquifer is used to validate the results of TOUGH2/ECO2. The numerical simulator has been applied to more complex flow problem including the CO{sub 2} injection project at the Sleipner Vest Field in the Norwegian sector of the North Sea and the evaluation of fluid flow dynamics effects of CO{sub 2} injection into aquifers. Numerical simulation results show that the transport at Sleipner is dominated by buoyancy effects and that shale layers control vertical migration of CO{sub 2}. These results are in good qualitative agreement with time lapse surveys performed at the site. High-resolution numerical simulation experiments have been conducted to study the onset of instabilities (viscous fingering) during injection of CO{sub 2} into saline aquifers. The injection process can be classified as immiscible displacement of an aqueous phase by a less dense and less viscous gas phase. Under disposal conditions (supercritical CO{sub 2}) the viscosity of carbon dioxide can be less than the viscosity of the aqueous phase by a factor of 15. Because of the lower viscosity, the CO{sub 2} displacement front will have a tendency towards instability. Preliminary simulation results show good agreement between classical instability solutions and numerical predictions of finger growth and spacing obtained using different gas/liquid viscosity ratios, relative permeability and capillary pressure models. Further studies are recommended to validate these results over a broader range of conditions.

  9. Wetland Flow and Salinity Budgets and Elements of a Decision Support System toward Implementation of Real-Time Seasonal Wetland Salinity Management

    SciTech Connect (OSTI)

    Quinn, N.W.T.; Ortega, R.; Rahilly, P.; Johnson, C.B.

    2011-12-17T23:59:59.000Z

    The project has provided science-based tools for the long-term management of salinity in drainage discharges from wetlands to the San Joaquin River. The results of the project are being used to develop best management practices (BMP) and a decision support system to assist wetland managers adjust the timing of salt loads delivered to the San Joaquin River during spring drawdown. Adaptive drainage management scheduling has the potential to improve environmental compliance with salinity objectives in the Lower San Joaquin River by reducing the frequency of violation of Vernalis salinity standards, especially in dry and critically dry years. The paired approach to project implementation whereby adaptively managed and traditional practices were monitored in a side-by-side fashion has provided a quantitative measure of the impacts of the project on the timing of salt loading to the San Joaquin River. The most significant accomplishments of the project has been the technology transfer to wetland biologists, ditch tenders and water managers within the Grasslands Ecological Area. This “learning by doing” has build local community capacity within the Grassland Water District and California Department of Fish and Game providing these institutions with new capability to assess and effectively manage salinity within their wetlands while simultaneously providing benefits to salinity management of the San Joaquin River.

  10. Geochemistry and migration of contaminants at the Weldon Spring chemical plant site, St. Charles County, Missouri, 1989--91

    SciTech Connect (OSTI)

    Schumacher, J.G.

    1993-12-31T23:59:59.000Z

    Investigations were conducted by the US Geological Survey in cooperation with the US Department of Energy at the Weldon Spring chemical plant site to determine the geochemistry of the shallow aquifer and geochemical controls on the migration of uranium and other constituents from the raffinate (waste) pits. Water-quality analyses from monitoring wells at the site and vicinity property indicate that water in the shallow aquifer is a calcium magnesium bicarbonate type that is at equilibrium with respect to calcite and slightly supersaturated with respect to dolomite.

  11. Geochemistry of /sup 210/Pb in the southeastern, US estuarine system

    SciTech Connect (OSTI)

    Storti, F.W.

    1980-11-01T23:59:59.000Z

    This study was an attempt to determine the geochemical behavior of /sup 210/Pb in southeastern salt marsh estuaries. As a part of this study the /sup 210/Pb dating technique was applied to natural and anthropogenic deposits of the region. /sup 210/Pb activity of sediment and water from the Georgia coastal area was measured by alpha spectroscopy. The effects of grain size and carbon content of the sediment on /sup 210/Pb concentrations was evaluated and the activity of /sup 210/Pb in dissolved and particulate phases of rivers was measured as a function of salinity. Ages and sedimentation rates of sedimentary deposits were also determined for some deposits. /sup 210/Pb activity in dissolved and particulate phases of rivers showed no clear trends as functions of salinity. River particulate activities were three to four times higher than dissolved activities. The relationship between /sup 210/Pb activity in salt marsh sediments and grain size was highly significant. Direct application of the /sup 210/Pb method to date and determine sedimentation rates of natural and anthropogenic deposits was partially successful. The anthropogenic deposits, however, had to be dated on the basis of normalizing /sup 210/Pb activities to grain size (% silt and clay) and carbon content (% carbon).

  12. Enhanced Oil Recovery in High Salinity High Temperature Reservoir by Chemical Flooding 

    E-Print Network [OSTI]

    Bataweel, Mohammed Abdullah

    2012-02-14T23:59:59.000Z

    Studying chemical enhanced oil recovery (EOR) in a high-temperature/high-salinity (HT/HS) reservoir will help expand the application of chemical EOR to more challenging environments. Until recently, chemical EOR was not recommended at reservoirs...

  13. CO[subscript 2] migration in saline aquifers. Part 2. Capillary and solubility trapping

    E-Print Network [OSTI]

    MacMinn, C. W.

    The large-scale injection of carbon dioxide (CO[subscript 2]) into saline aquifers is a promising tool for reducing atmospheric CO[subscript 2] emissions to mitigate climate change. An accurate assessment of the post-injection ...

  14. Enhanced Oil Recovery in High Salinity High Temperature Reservoir by Chemical Flooding

    E-Print Network [OSTI]

    Bataweel, Mohammed Abdullah

    2012-02-14T23:59:59.000Z

    Studying chemical enhanced oil recovery (EOR) in a high-temperature/high-salinity (HT/HS) reservoir will help expand the application of chemical EOR to more challenging environments. Until recently, chemical EOR was not recommended at reservoirs...

  15. The influence of geothermal sources on deep ocean temperature, salinity, and flow fields

    E-Print Network [OSTI]

    Speer, Kevin G. (Kevin George)

    1988-01-01T23:59:59.000Z

    This thesis is a study of the effect of geothermal sources on the deep circulation, temperature and salinity fields. In Chapter 1 background material is given on the strength and distribution of geothermal heating. In ...

  16. Physiological Effects of Saline Water on Two Economically Important Horticultural Crops in South Texas

    E-Print Network [OSTI]

    Simpson, Catherine Ross

    2013-12-02T23:59:59.000Z

    Citrus and watermelons are valuable economic crops worldwide, contributing approximately $120 million combined each year in Texas alone. Both citrus and watermelons are sensitive to saline conditions, which can be problematic in the Lower Rio...

  17. Excessive Hyperthermic Necrosis of a Pulmonary Lobe after Hypertonic Saline-Enhanced Monopolar Radiofrequency Ablation

    SciTech Connect (OSTI)

    Kim, Tae Sung, E-mail: tskim@smc.samsung.co.kr; Lim, Hyo K. [Sungkyunkwan University School of Medicine, Department of Radiology and Center for Imaging Science, Samsung Medical Center (Korea, Republic of); Kim, Hojoong [Sungkyunkwan University School of Medicine, Division of Pulmonary and Critical Care Medicine, The Department of Medicine, Samsung Medical Center (Korea, Republic of)

    2006-02-15T23:59:59.000Z

    Although there has been a feasibility study of saline-enhanced radiofrequency ablation of the lung in rabbits, there has been no report on hypertonic saline-enhanced radiofrequency ablation of human pulmonary tumors or its complication. We report a case in which a large necrotic cavity was produced in the lung after hypertonic saline-enhanced radiofrequency ablation of recurrent metastatic tumor from hepatocellular carcinoma. Although hypertonic saline-enhanced radiofrequency ablation is powerful and efficient in local ablation, it is difficult to predict the exact extent of ablation, especially in the lungs. This can be dangerous, as there is a high chance of producing an ablation area much larger than expected and, hence, major complications. Special attention is required not to overablate while using this technique.

  18. The response of New Guinea impatiens to varying salinity levels in a subirrigation system

    E-Print Network [OSTI]

    Todd, Nancy Morgan

    1996-01-01T23:59:59.000Z

    Subirrigation is an alternative irrigation method for greenhouse crops. Lack of leaching poses the problem of high salt buildup in the root zone. The objective of this study was to determine the effects of saline irrigation water on a greenhouse...

  19. Physical and chemical effects of CO2 storage in saline aquifers of the southern North Sea 

    E-Print Network [OSTI]

    Heinemann, Niklas

    2013-07-01T23:59:59.000Z

    One of the most promising mitigation strategies for greenhouse gas accumulation in the atmosphere is carbon capture and storage (CCS). Deep saline aquifers are seen as the most efficient carbon dioxide (CO2) storage sites, ...

  20. The production of temperature and salinity variance and covariance : implications for mixing

    E-Print Network [OSTI]

    Schanze, Julian J. (Julian Johannes)

    2013-01-01T23:59:59.000Z

    Large-scale thermal forcing and freshwater fluxes play an essential role in setting temperature and salinity in the ocean. A number of recent estimates of the global oceanic freshwater balance as well as the global oceanic ...

  1. PROFESSIONAL SERVICE Chair Technical and Economic Committee, CVSALTS Central Valley Salinity Coalition, (2008

    E-Print Network [OSTI]

    Quinn, Nigel

    -2008 Berkeley Laboratory Delegate, White House Conference on Industrial Ecology Department of Energy, Water-Energy, Central Valley Salinity Coalition, CVSALTS SOCIAL/CIVIC Yolo Polo Club Sutter Buttes Polo Club Wine

  2. EFFECT OF SALINITY ON THE DIELECTRIC PROPERTIES OF GEOLOGICAL MATERIALS : IMPLICATION FOR SOIL

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    . Dielectric mixing models were first calibrated by means of experimental measurements before being used of SAR data (AIRSAR, PALSAR). Keywords- Earth, evaporites, dielectric mixing model, IEM, Mars, polarimetry, radar backscattering, salinity, SAR, soil moisture. I. INTRODUCTION The measurement of soil

  3. The influence of copper and bicarbonate ions on the corrosion of aluminum alloys saline solutions

    E-Print Network [OSTI]

    Becerra-Diaz, Alcibiades

    1972-01-01T23:59:59.000Z

    THE INFLUENCE OF COPPER AND BICARBONATE IONS ON THE CORROSION OF ALUMINUM ALLOYS IN SALINE SOLUTIONS A Thesis by ALCIBIADES BECERRA-DIAZ Submitted to the Graduate College of Texas A&M University in partial fulfillment of the requirement... for the degree of MASTER OF SCIENCE August 1972 Major Subject: Mechanical Engineerinq THE INFLUENCE OF COPPER AND BICARBONATE IONS ON THE CORROSION OF ALUMINUM ALLOYS IN SALINE SOLUTIONS A Thesis by ALCIBIADES BECERRA-DIAZ Approved as to sty1e...

  4. OPTIMAL GEOLOGICAL ENVIRONMENTS FOR CARBON DIOXIDE DISPOSAL IN SALINE AQUIFERS IN THE UNITED STATES

    SciTech Connect (OSTI)

    Susan D. Hovorka

    1999-02-01T23:59:59.000Z

    Recent research and applications have demonstrated technologically feasible methods, defined costs, and modeled processes needed to sequester carbon dioxide (CO{sub 2}) in saline-water-bearing formations (aquifers). One of the simplifying assumptions used in previous modeling efforts is the effect of real stratigraphic complexity on transport and trapping in saline aquifers. In this study we have developed and applied criteria for characterizing saline aquifers for very long-term sequestration of CO{sub 2}. The purpose of this pilot study is to demonstrate a methodology for optimizing matches between CO{sub 2} sources and nearby saline formations that can be used for sequestration. This project identified 14 geologic properties used to prospect for optimal locations for CO{sub 2} sequestration in saline-water-bearing formations. For this demonstration, we digitized maps showing properties of saline formations and used analytical tools in a geographic information system (GIS) to extract areas that meet variably specified prototype criteria for CO{sub 2} sequestration sites. Through geologic models, realistic aquifer properties such as discontinuous sand-body geometry are determined and can be used to add realistic hydrologic properties to future simulations. This approach facilitates refining the search for a best-fit saline host formation as our understanding of the most effective ways to implement sequestration proceeds. Formations where there has been significant drilling for oil and gas resources as well as extensive characterization of formations for deep-well injection and waste disposal sites can be described in detail. Information to describe formation properties can be inferred from poorly known saline formations using geologic models in a play approach. Resulting data sets are less detailed than in well-described examples but serve as an effective screening tool to identify prospects for more detailed work.

  5. The effect of environmental salinity on organoleptic characteristics of penaeid shrimp

    E-Print Network [OSTI]

    Papadopoulos, Linda Suter

    1984-01-01T23:59:59.000Z

    Papadopoulos, B. S. , Texas AAN University Chairman of Advisory Committee: Dr. Gunner Firms The effects of environmental salinity on the moisture content, sodium chloride content, free amino acid (FAA) concentration and organoleptic characteristics... parts per thousand (ppt) to either 10, 30 or 50 ppt. In a second trial, salinities were acutely changed from 25 ppt to either 10 or 50 ppt. Shrimp from both trials were analyzed for tissue moisture, chloride and FAA. Statistical analysis indicated...

  6. Journal of the Geological Society, London, Vol. 155, 1998, pp. 773785. Printed in Great Britain Mineralogy, sulphur isotope geochemistry and the development of sulphide structures

    E-Print Network [OSTI]

    Mineralogy, sulphur isotope geochemistry and the development of sulphide structures at the Broken Spur mineralogy and sulphur isotope analysis. Young mound sulphides from Broken Spur have a pyrrhotite- dominated mineralogy unusual for bare ridge vent systems. However, pyrrhotite is metastable and is ultimately converted

  7. 13.21 Geochemistry of the Rare-Earth Element, Nb, Ta, Hf, and Zr Deposits RL Linnen, University of Western Ontario, London, ON, Canada

    E-Print Network [OSTI]

    Chakhmouradian, Anton

    13.21 Geochemistry of the Rare-Earth Element, Nb, Ta, Hf, and Zr Deposits RL Linnen, University of rare metals in natural fluids 551 13.21.2.2.2 Aqueous complexation and mineral solubility 552 13 Acknowledgments 564 References 564 13.21.1 Introduction Rare-element mineral deposits, also called rare-metal

  8. Low-Salinity Waterflooding to Improve Oil Recovery - Historical Field Evidence

    SciTech Connect (OSTI)

    Eric P. Robertson

    2007-11-01T23:59:59.000Z

    Waterflooding is by far the most widely applied method of improved oil recovery. Crude oil/brine/rock interactions can lead to large variations in the displacement efficiency of wa-terfloods. Laboratory water-flood tests and single-well tracer tests have shown that injection of dilute brine can increase oil recovery, but work designed to test the method on a field scale has not yet been undertaken. Historical waterflood records could unintentionally provide some evidence of improved recovery from waterflooding with lower salinity brine. Nu-merous fields in the Powder River basin of Wyoming have been waterflooded using low salinity brine (about 500 ppm) obtained from the Madison limestone or Fox Hills sandstone. Three Minnelusa formation fields in the basin were identified as potential candidates for waterflood comparisons based on the salinity of the connate and injection water. Historical pro-duction and injection data for these fields were obtained from the public record. Field waterflood data were manipulated to be displayed in the same format as laboratory coreflood re-sults. Recovery from fields using lower salinity injection wa-ter was greater than that using higher salinity injection wa-ter—matching recovery trends for laboratory and single-well tests.

  9. Impact-driven pressure management via targeted brine extraction Conceptual studies of CO2 storage in saline formations

    E-Print Network [OSTI]

    Birkholzer, J.T.

    2013-01-01T23:59:59.000Z

    of active pumping, water extraction wells can also bescenarios in which water extraction wells operate as passivemanagement via extraction of native saline water has been

  10. Hydrocarbon geochemistry of the strait of Georgia: Modification of a Fraser River dominated regime by ocean dumping

    SciTech Connect (OSTI)

    Yunker, M.B.; Macdonald, R.W.; Paton, D. [Inst. of Ocean Sciences, Sidney, British Columbia (Canada)] [and others

    1996-12-31T23:59:59.000Z

    Despite the presence of Canada`s third largest city and of the largest river reaching the west coast of Canada, the study of the environmental and geochemical aspects of hydrocarbon distributions in the lower Fraser River and adjacent Strait of Georgia has not progressed beyond the cataloguing of environmental concentrations. Hence hydrocarbon distributions in the lower Fraser River are only poorly understood and very little is known about either the role that the Fraser River plays in defining the hydrocarbon geochemistry of the Strait of Georgia or how hydrocarbon distributions in the strait are being modified by shipping or dredging activities associated with the port of Vancouver. This report describes the results of analysis from sediments and particulate samples.

  11. FY 1984 and FY 1985 geochemistry and materials studies in support of the Magma Energy Extraction Program

    SciTech Connect (OSTI)

    Westrich, H.R.; Weirick, L.J.; Cygan, R.T.; Reece, M.; Hlava, P.F.; Stockman, H.W.; Gerlach, T.M.

    1986-04-01T23:59:59.000Z

    Geochemistry and materials studies are being performed in support of the Magma Energy Extraction Program. The work is largely restricted to: (1) characterizing magmatic environments at sites of interest, (2) testing engineering materials in laboratory simulated magmatic environments, (3) investigating chemical mass transport effects inherent in designs for direct contact heat exchangers, and (4) evaluating degassing hazards associated with drilling into and extracting energy from shallow magma. Magma characterization studies have been completed for shallow magma at Long Valley, Coso volcanic field, and Kilauea volcano. The behavior of 17 commercially available materials has been examined in rhyolite magma at 850/sup 0/C and 200 MPa for periods up to seven days. Analysis of reaction products from materials tests to date indicate that oxidation is the main corrosion problem for most alloys in rhyolitic magma. Considerations of corrosion resistance, high-temperature strength, and cost indicate nickel-base superalloys offer the most promise as candidates for use in rhyolitic magma.

  12. Information technology and decision support tools for stakeholder-driven river basin salinity management

    SciTech Connect (OSTI)

    Quinn, N.W.T; Cozad, D.B.; Lee, G.

    2010-01-01T23:59:59.000Z

    Innovative strategies for effective basin-scale salinity management have been developed in the Hunter River Basin of Australia and more recently in the San Joaquin River Basin of California. In both instances web-based stakeholder information dissemination has been a key to achieving a high level of stakeholder involvement and the formulation of effective decision support salinity management tools. A common element to implementation of salinity management strategies in both river basins has been the concept of river assimilative capacity for controlling export salt loading and the potential for trading of the right to discharge salt load to the river - the Hunter River in Australia and the San Joaquin River in California. Both rivers provide basin drainage and the means of exporting salt to the ocean. The paper compares and contrasts the use of monitoring, modeling and information dissemination in the two basins to achieve environmental compliance and sustain irrigated agriculture in an equitable and socially and politically acceptable manner.

  13. Effect of increasing copper and salinity on glycerol production by Dunaliella salina

    SciTech Connect (OSTI)

    Lustigman, B.; McCormick, J.M.; Dale, G.; McLaughlin, J.J.A.

    1987-02-01T23:59:59.000Z

    Dunaliella salina is a green marine flagellate whose main storage product is glycerol. Its ability to grow in waters which vary greatly in salinity is due to its ability to form glycerol, the intracellular concentration of which is directly proportional to the extracellular salinity. Copper is an essential trace element needed in small quantities by algae for plastocyanin production. However, at high concentrations it acts as an effective algicide. Dunaliella species have been shown to have an unusual resistance to copper toxicity. The authors examined the effects of lethal and sublethal concentrations of copper on growth and glycerol production in dunaliella saline, in order to determine if adaptation to copper toxicity will result in an increase in production of glycerol.

  14. Salinity-induced hydrate dissociation: A mechanism for recent CH4 release on Mars

    SciTech Connect (OSTI)

    Madden, Megan Elwood [ORNL; Ulrich, Shannon M [ORNL; Onstott, Tullis [Princeton University; Phelps, Tommy Joe [ORNL

    2007-01-01T23:59:59.000Z

    Recent observations of CH4 in the Martian atmosphere suggest that CH4 has been added relatively recently. Several mechanisms for recent CH4 release have been proposed including subsurface biological methanogenesis, abiogenic hydrothermal and/or volcanic activity, dissociation of CH4 hydrates, atmospheric photolysis, or addition of organics via bolide impact. This study examines the effects of increasing salinity on gas hydrate stability and compares estimates of the Martian geothermal gradient to CH4 and CO2 hydrate stability fields in the presence of high salinity brines. The results demonstrate that salinity increases alone result in a significant decrease in the predicted hydrate stability zone within the Martian subsurface and may be a driving force in CH4 hydrate destabilization. Active thermal and/or pressure fluctuations are not required in order for CH4 hydrates to be the source of atmospheric CH4.

  15. The influence of irrigation water salinity on optimal nitrogen, phosphorus, and potassium liquid fertilizer rates

    E-Print Network [OSTI]

    Campos Nu?n?ez, Ricardo

    1990-01-01T23:59:59.000Z

    of poor quality water (high in soluble salts) and high concentrations of water-soluble fertilizers can induce salt damage in plants. The objective of this work was to investigate the effects of salinity in irrigation water on optimal fertilization rates... in salt-sensitive tropical foliage. Spafhiphyllum 'Petite' and Dieffenbachia 'Camille' were grown using 9 levels of water-soluble fertilizers (0, 25, 50, 100, 200, 400, 800, 1600, 3200 mg I N in a 3-1-2 ratio of N-P205-K20), and two levels of salinity...

  16. The effect of NaCl salinity on bell pepper photosynthesis

    E-Print Network [OSTI]

    Bethke, Paul Carl

    1989-01-01T23:59:59.000Z

    annuum cv. Tambel-2, were grown in hydroponics and then salinized to 0, 50, 100 or 150 mM NaC1. Photosynthetic rates of individual leaves were measured on several occasions during the salinization period (usually 10 to 14 d) with an ' open' gas...-exchange system. These rates were reduced by NaC1 concentrations of 100 mM or higher. Stomatal conductance was concurrently reduced, but nonstomatal effects seem to be primarily responsible for decreases in photosynthesis. The correlation between either leaf...

  17. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR: VERNON FIELD, ISABELLA COUNTY, MI

    SciTech Connect (OSTI)

    James R. Wood; W. Quinlan

    2003-10-01T23:59:59.000Z

    The principal objective of this demonstration project is to test surface geochemical techniques for detecting trace amounts of light hydrocarbons in pore gases as a means of reducing risk in hydrocarbon exploration and production. During this reporting period, a new field demonstration, Springdale Prospect in Manistee County, Michigan was begun to assess the validity and usefulness of the microbial surface geochemical technique. The surface geochemistry data showed a fair-to-good microbial anomaly that may indicate the presence of a fault or stratigraphic facies change across the drilling path. The surface geochemistry sampling at the original Bear Lake demonstration site was updated several months after the prospect was confirmed and production begun. As expected, the anomaly appears to be diminishing as the positive (apical) anomaly is replaced by a negative (edge) anomaly, probably due to the pressure draw-down in the reservoir.

  18. A method for quick assessment of CO2 storage capacity in closed and semi-closed saline formations

    E-Print Network [OSTI]

    Zhou, Quanlin

    , USA 1. Introduction Geological carbon dioxide (CO2) sequestration in deep forma- tions (e.g., saline of the U.S. Department of Energy (USDOE) Carbon Sequestration Regio 2008 Published on line 21 March 2008 Keywords: Geological CO2 sequestration Storage capacity Saline

  19. Sensitivity analysis of three-dimensional salinity simulations in North San Francisco Bay using the unstructured-grid SUNTANS model

    E-Print Network [OSTI]

    Fringer, Oliver B.

    and the confluence of the Sacramento­San Joaquin Rivers and comprises San Pablo Bay, Suisun Bay and Central Bay and San Joaquin rivers, while high inflows result in enhanced salinity stratification and gravitationalSensitivity analysis of three-dimensional salinity simulations in North San Francisco Bay using

  20. f your soil has a high salinity content, the plants growing there will not be as vigorous as they would

    E-Print Network [OSTI]

    I f your soil has a high salinity content, the plants growing there will not be as vigorous as they would be in normal soils. Seeds will germinate poorly, if at all, and the plants will grow slowly much you water them. Routine soil testing can identify your soil's salinity levels and suggest measures

  1. Managing the risk of CO2 leakage from deep saline aquifer reservoirs through the creation of a hydraulic barrier

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    - up in the storage reservoir. For some man-made leakages (e.g. abandoned well), and more importantlyGHGT-10 Managing the risk of CO2 leakage from deep saline aquifer reservoirs through the creation emissions. Depleted oil and gas fields or saline aquifers are seen as possible storage reservoirs

  2. Origin of groundwater salinity and hydrogeochemical processes in the confined Quaternary aquifer of the Pearl River Delta, China

    E-Print Network [OSTI]

    Jiao, Jiu Jimmy

    Origin of groundwater salinity and hydrogeochemical processes in the confined Quaternary aquifer of groundwater salinity and the major hydrogeochemical processes controlling the groundwater evolution­2009, and groundwater samples were collected for major ion (Ca2þ ; Mg2þ ; Naþ ; Kþ ; NHþ 4 ; Cl À ; SO2À 4 and HCOÀ 3

  3. TWO-DIMENSIONAL REACTIVE TRANSPORT MODELING OF CO2 INJECTION IN A SALINE AQUIFER AT THE SLEIPNER SITE

    E-Print Network [OSTI]

    Boyer, Edmond

    model of long-term geological storage of carbon dioxide. A data set from the Utsira formation assemblages are considered in the Utsira formation, a sand formation that is highly permeable and a shale or gas reservoirs, (ii) unmineable coal beds and (iii) saline aquifers. Deep saline aquifers offer

  4. A Numerical Model for the Simulation of the Hydrodynamic Flow and of the Salinity Evolution

    E-Print Network [OSTI]

    Colominas, Ignasi

    actions (dredging, building of docks, spillages, etc.) on the marine habitat, and to evaluate to a real case: the analysis of the possible effects of dredging Los Lombos del Ulla, a formation the actual salinity level with the predicted situation if the different dredging options were executed. Some

  5. A rate and state friction law for saline ice Ben Lishman,1

    E-Print Network [OSTI]

    Feltham, Daniel

    coefficient of friction. This law describes dry friction. Bowden and Hughes [1939] proposed that the lowA rate and state friction law for saline ice Ben Lishman,1 Peter Sammonds,1,2 and Danny Feltham2 ice friction models are necessary to predict the nature of interactions between sea ice floes

  6. Don Juan Pond, Antarctica: Near-surface CaCl2-brine feeding Earth's most saline

    E-Print Network [OSTI]

    Marchant, David R.

    Don Juan Pond, Antarctica: Near-surface CaCl2-brine feeding Earth's most saline lake lineae (RSL), thought to represent seasonal brines, has sparked interest in analogous environments watershed and show that this, together with small amounts of meltwater, are capable of generating brines

  7. Instruments and Methods A non-destructive method for measuring the salinity and solid

    E-Print Network [OSTI]

    Worster, M. Grae

    rejected into the underlying ocean or remains within highly saline brine in the interstices between the pure, fresh-water ice crystals. It is the volume fraction of this brine, the so-called liquid fraction and others, 2000). A first-principles predictive model of the brine volume evolution is therefore required

  8. GEOLOGY, December 2007 1063 Semi-arid and arid rivers typically exhibit increasing salinity levels

    E-Print Network [OSTI]

    Asmerom, Yemane

    of a sedimentary brine source. These groundwater fluxes, while very small (. Furthermore, 36 Cl/Cl ratios and 234 U values for these brines are close to secular equilibrium, indicating brine ages on the order of millions of years. The recognition of a substantial geologic salinity source

  9. THE EFFECTS OF NON-CONDENSIBLE GAS AND SALINITY ON STEAM ADSORPTION

    E-Print Network [OSTI]

    Stanford University

    THE EFFECTS OF NON-CONDENSIBLE GAS AND SALINITY ON STEAM ADSORPTION A REPORT SUBMITTED for his constant help in my navigating the Latex maze. 111 ... #12;Abstract Water adsorption in geothermal and experimental results in- dicate that water adsorption exists in the vapor-dominated type of reservoir

  10. Integrated salinity reduction and water recovery in an osmotic microbial desalination cell{

    E-Print Network [OSTI]

    anode to generate an electric driving force that stimulates ion migration from its middle chamber into the anode (anions) and the cathode (cations), respectively; as a result, salinity in the middle chamber can diffusion and water osmosis have also been discussed. Water migration into the middle chamber via osmosis

  11. NOBOB-S: Salinity/Brine Exposure as a Biocide for Application to NOBOB Residuals

    E-Print Network [OSTI]

    , eggs and spores of many taxa within the sediments and residual water of their ballast tanks (Niimi a voluntary "best management practices" approach for residual ballast water and sediment for NOBOB vesselsNOBOB-S: Salinity/Brine Exposure as a Biocide for Application to NOBOB Residuals Primary

  12. Seasonal Changes in Bacterial and Archaeal Gene Expression Patterns across Salinity Gradients in the

    E-Print Network [OSTI]

    their metabolic activities, microbial populations mediate the impact of high gradient regions on ecologicalSeasonal Changes in Bacterial and Archaeal Gene Expression Patterns across Salinity Gradients in nitrogen and carbon metabolism in the CRCM. Initial experiments with the environmental microarrays were

  13. Testing models for the Messinian salinity crisis: The Messinian record in Almera, SE Spain

    E-Print Network [OSTI]

    Riding, Robert

    Testing models for the Messinian salinity crisis: The Messinian record in Almería, SE Spain Juan C Fuentenueva s.n., Universidad de Granada, 18002 Granada, Spain b School of Earth, Ocean and Planetary Sciences, SE Spain, display excellent exposures of Messinian (Late Miocene) sequences. The Sorbas, Almería

  14. Remediation of CO2 Leakage from Deep Saline Aquifer Storage Based on Reservoir and Pollution

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    Remediation of CO2 Leakage from Deep Saline Aquifer Storage Based on Reservoir and Pollution Hazards and Safety of CO2 Storage" Division, Orléans, FRANCE www.brgm.fr References Audigane, P., Chiaberge, C., Lions, J., Humez, P., 2009. Modeling of CO2 leakage through an abandoned well from a deep

  15. Controls on the regional-scale salinization of the Ogallala aquifer, Southern High Plains, Texas, USA

    E-Print Network [OSTI]

    Banner, Jay L.

    of Kentucky, Lexington, KY 40506-0053, USA b Department of Geological Sciences, The University of TexasControls on the regional-scale salinization of the Ogallala aquifer, Southern High Plains, Texas, USA Sunil Mehtaa, *, Alan E. Fryara , Jay L. Bannerb a Department of Geological Sciences, University

  16. Soil mineral genesis and distribution in a saline lake landscape of the Pantanal Wetland, Brazil

    E-Print Network [OSTI]

    Ahmad, Sajjad

    Soil mineral genesis and distribution in a saline lake landscape of the Pantanal Wetland, Brazil S Geografia, Universidade de São Paulo, São Paulo, Brazil b Soil & Water Sciences Program, Department São Paulo, Piracicaba, Brazil a b s t r a c ta r t i c l e i n f o Article history: Received 20 August

  17. Soil morphological control on saline and freshwater lake hydrogeochemistry in the Pantanal of Nhecolndia, Brazil

    E-Print Network [OSTI]

    Boyer, Edmond

    morphological control on saline and freshwater lake hydrogeochemistry in the Pantanal of Nhecolândia, Brazil L-MS, Brazil 4 ­ Laboratório de Pedologia, Departamento de Geografia, Universidade de São Paulo C.P. 8105, 05508-900, São Paulo, Brazil 5 - UFMS, Departamento de Geografia, Campus de Três Lagoas, Av. Ranulfo

  18. Using Trends and Geochemical Analysis to Assess Salinity Sources along the Pecos River, Texas

    E-Print Network [OSTI]

    Hoff, Aaron

    2012-07-16T23:59:59.000Z

    Increasing salinity has been a growing concern for users of waters from the Pecos River and the reservoirs it feeds in the Texas portion of the River's watershed. Irrigation water diverted from the river in the northern reach of this watershed...

  19. Water relation characteristics and photosynthesis of saline-stressed seedlings of non-halophyte species

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    Water relation characteristics and photosynthesis of saline-stressed seedlings of non of the present study was to ex- amine the distribution of salts and its effect on photosynthesis for non as relative values against 0% treatment. Photosynthesis by O. asiaticus var. aurantiacus decreased

  20. Small-scale features of temperature and salinity surface fields in the Christophe Maes,1

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    the onset and build-up phases of El Ni~no/ Southern Oscillation (ENSO) events in coupled numerical modelsSmall-scale features of temperature and salinity surface fields in the Coral Sea Christophe Maes,1 August 2013; accepted 11 August 2013. [1] The small-scale features in sea surface temperature

  1. Using tracer experiments to determine deep saline aquifers caprocks transport characteristics for carbon dioxide storage

    E-Print Network [OSTI]

    Boyer, Edmond

    for carbon dioxide storage P. Bachaud1,2 , Ph. Berne1 , P. Boulin1,3,4 , F. Renard5,6 , M. Sardin2 , J caprocks from a deep saline aquifer in the Paris basin. Introduction Storage of carbon dioxide in deep bubble. Determination of the diffusion properties is also required since they will govern how dissolved

  2. Capacitive mixing power production from salinity gradient energy enhanced through exoelectrogen-

    E-Print Network [OSTI]

    thermolytic solutions that can be used to capture waste heat energy as salinity gradient energy. Forced our expanding water and energy infrastructures across the globe, the development of sustainable dual energy generation and water treatment process is highly desirable. A combined capacitive mixing

  3. Hydraulic barrier design and applicability for managing the risk of CO2 leakage from deep saline

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    Hydraulic barrier design and applicability for managing the risk of CO2 leakage from deep saline modifying the leak hydraulic properties (e.g. permeability) may be unfeasible. An appealing option.e. by creating a hydraulic barrier. The present article presents and discusses the operational and strategic

  4. SUPPORTING INFORMATION Photochemical Chlorine and Bromine Activation from Artificial Saline Snow

    E-Print Network [OSTI]

    Meskhidze, Nicholas

    1 SUPPORTING INFORMATION Photochemical Chlorine and Bromine Activation from Artificial Saline Snow@chem.utoronto.ca Additional Results Ozone concentration Since the dark ozonation of frozen NaCl/NaBr solutions is known. The products of the photodissociation of ozone adsorbed to an ice surface at relatively warm temperatures

  5. The Economics of CO2 Transport by Pipeline and Storage in Saline Aquifers and Oil Reservoirs

    E-Print Network [OSTI]

    The Economics of CO2 Transport by Pipeline and Storage in Saline Aquifers and Oil Reservoirs Sean T Description Date 0 Original document 1/29/2008 1 Estimate for carbon content of crude oil was incorrect (see p an invaluable summer at the Bureau of Economic Geology at the University of Texas at Austin working with Sue

  6. The Effect of Increased Salinity on Diversity and Abundance of Diatoms

    E-Print Network [OSTI]

    Boyer, Elizabeth W.

    drainage or Marcellus Shale groundwater enters a system and significantly increases salinity, or when ecosystem. The recent Marcellus Shale drilling for natural gas in regions of New York, Pennsylvania, West was reported to be >50,000 µS/cm before the bloom took place. It is possible that discharge of the Marcellus

  7. Salinity Effects on the Degree of Hydrophobicity and Longevity for Superhydrophobic Fibrous Coatings

    E-Print Network [OSTI]

    Tafreshi, Hooman Vahedi

    Salinity Effects on the Degree of Hydrophobicity and Longevity for Superhydrophobic Fibrous, Inc. J Appl Polym Sci 000: 000­000, 2011 Key words: biomimetic; superhydrophobic coatings; fibers are typically classified as superhydrophobic. Superhydrophobicity is exhibited in materials with a combination

  8. Holocene Salnia sediments of West Caicos, British West Indies: stratigraphy, mineralogy, and pore-water geochemistry

    SciTech Connect (OSTI)

    Rosoff, D.B.; Dwyer, G.S.; Leaver, J.; Perkins, R.D.; Lloyd, R.M.

    1989-03-01T23:59:59.000Z

    A study of east Salina on West Caicos, British West Indies, has shown it to be the site of active gypsum and dolomite formation. East salina, 3 km long and 0.25 km wide, is situated in an elongate depression between Holocene oolitic dunes to the east and eolianite ridges of Pleistocene age to the west. The thickness of the Holocene sediment package in the salina ranges from 3 m in the center to less than 0.5 m at the edges. The salina sediments exhibit an overall restrictive-upward sequence which grades from open-marine packstone and grainstone at the base through algally laminated mud and into a gypsum mush in the uppermost part of the section. A thin algal mat encrusted with gypsum and ephemeral halite covers the salina surface. This sequence is virtually identical in scale and appearance to prograding sabkha sequences reported from the Persian Gulf. Carbonate phases present in these sediments include aragonite, high- and low-magnesium calcite, and protodolomite. Protodolomite is found as an alteration product in the open-marine sediments and within a thin, lithified Holocene basal layer that overlies laminated calichecrust on the underlying Pleistocene bed rock. Analyses of pore waters reveal that they approach normal marine salinity at the base of the salina sequence and become hypersaline upward. Mineralogical changes in the salina sequence are reflected in the ionic character of the pore waters. Field observations indicate that interstitial water within the sequence is under hydraulic head and rises and falls with the tides.

  9. Percutaneous Radiofrequency Lung Ablation Combined with Transbronchial Saline Injection: An Experimental Study in Swine

    SciTech Connect (OSTI)

    Kawai, T., E-mail: t-kawai@hosp.yoka.hyogo.jp; Kaminou, T., E-mail: kaminout@grape.med.tottori-u.ac.jp; Sugiura, K.; Hashimoto, M.; Ohuchi, Y.; Adachi, A. [Tottori University, Division of Radiology, Department of Pathophysiological and Therapeutic Science, Faculty of Medicine (Japan); Fujioka, S.; Ito, H. [Tottori University, Division of Organ Pathology, Department of Microbiology and Pathology, Faculty of Medicine (Japan); Nakamura, K. [Hakuai Hospital, Department of Radiology (Japan); Ihaya, T. [Sanin Rosai Hospital, Department of Radiology (Japan); Ogawa, T. [Tottori University, Division of Radiology, Department of Pathophysiological and Therapeutic Science, Faculty of Medicine (Japan)

    2010-02-15T23:59:59.000Z

    To evaluate the efficacy of radiofrequency lung ablation with transbronchial saline injection. The bilateral lungs of eight living swine were used. A 13-gauge bone biopsy needle was inserted percutaneously into the lung, and 1 ml of muscle paste was injected to create a tumor mimic. In total, 21 nodules were ablated. In the saline injection group (group A), radiofrequency ablation (RFA) was performed for 11 nodules after transbronchial saline injection under balloon occlusion with a 2-cm active single internally cooled electrode. In the control group (group B), conventional RFA was performed for 10 nodules as a control. The infused saline liquid showed a wedge-shaped and homogeneous distribution surrounding a tumor mimic. All 21 RFAs were successfully completed. The total ablation time was significantly longer (13.4 {+-} 2.8 min vs. 8.9 {+-} 3.5 min; P = 0.0061) and the tissue impedance was significantly lower in group A compared with group B (73.1 {+-} 8.8 {Omega} vs. 100.6 {+-} 16.6 {Omega}; P = 0.0002). The temperature of the ablated area was not significantly different (69.4 {+-} 9.1{sup o}C vs. 66.0 {+-} 7.9{sup o}C; P = 0.4038). There was no significant difference of tumor mimic volume (769 {+-} 343 mm{sup 3} vs. 625 {+-} 191 mm{sup 3}; P = 0.2783). The volume of the coagulated area was significantly larger in group A than in group B (3886 {+-} 1247 mm{sup 3} vs. 2375 {+-} 1395 mm{sup 3}; P = 0.0221). Percutaneous radiofrequency lung ablation combined with transbronchial saline injection can create an extended area of ablation.

  10. Simplified 1-D Hydrodynamic and Salinity Transport Modeling of the Sacramento–San Joaquin Delta: Sea Level Rise and Water Diversion Effects

    E-Print Network [OSTI]

    Fleenor, William E.; Bombardelli, Fabian

    2013-01-01T23:59:59.000Z

    Hydrodynamic and Salinity Transport Modeling of the Sacramento–San Joaquin Delta: Sea Level Rise and Water Diversion Effects

  11. The Next-Generation Massively Parallel Reactive Flow and Transport Code PFLOTRAN: Application to CO2 Storage in Saline Aquifers P. Lichtner

    E-Print Network [OSTI]

    Mills, Richard

    to investigate sequestration of CO2 in vari- ous geologic media including depleted oil reservoirs and saline

  12. Dungeness Crab Dredging Entrainment Studies in the Lower Columbia River, 2002 – 2004: Loss Projections, Salinity Model, and Scenario Analysis

    SciTech Connect (OSTI)

    Pearson, Walter H.; Williams, Greg D.; Skalski, John R.

    2005-01-01T23:59:59.000Z

    Dungeness crab studies conducted in 2002 for the Portland District of the U.S. Army Corps of Engineers (Corps) constituted a major step forward in quantifying crab entrainment through statistical projections of adult equivalent loss (AEL) and loss to the fishery (LF) from proposed construction and maintenance dredging in the Columbia River navigation channel (Pearson et al. 2002, 2003). These studies also examined the influence of bottom salinity on crab abundance and entrainment rates. Additional sampling was conducted in 2004 to tighten loss projections, further develop the crab salinity model, and apply the model to assess correlations of entrainment rates and projected losses with seasonal salinity changes.

  13. SALINITY AND SODICITY INTERACTIONS OF WEATHERED MINESOILS IN NORTHWESTERN NEW MEXICO AND NORTH EASTERN ARIZONA

    SciTech Connect (OSTI)

    Brent Musslewhite; Song Jin

    2006-05-01T23:59:59.000Z

    Weathering characteristics of minesoils and rooting patterns of key shrub and grass species were evaluated at sites reclaimed for 6 to 14 years from three surface coal mine operations in northwestern New Mexico and northeastern Arizona. Non-weathered minesoils were grouped into 11 classifications based on electrical conductivity (EC) and sodium adsorption ratio (SAR). Comparisons of saturated paste extracts, from non-weathered and weathered minesoils show significant (p < 0.05) reductions in SAR levels and increased EC. Weathering increased the apparent stability of saline and sodic minesoils thereby reducing concerns of aggregate slaking and clay particle dispersion. Root density of four-wing saltbush (Atriplex canascens), alkali sacaton (Sporobolus airoides), and Russian wildrye (Psathyrostachys junceus) were nominally affected by increasing EC and SAR levels in minesoil. Results suggest that saline and sodic minesoils can be successfully reclaimed when covered with topsoil and seeded with salt tolerant plant species.

  14. Process for producing modified microorganisms for oil treatment at high temperatures, pressures and salinity

    DOE Patents [OSTI]

    Premuzic, Eugene T. (East Moriches, NY); Lin, Mow (Rocky Point, NY)

    1996-02-20T23:59:59.000Z

    This invention relates to the preparation of new, modified organisms, through challenge growth processes, that are viable in the extreme temperature, pressure and pH conditions and salt concentrations of an oil reservoir and that are suitable for use in microbial enhanced oil recovery. The modified microorganisms of the present invention are used to enhance oil recovery and remove sulfur compounds and metals from the crude oil. The processes are comprised of steps which successively limit the carbon sources and increase the temperature, pressure and salinity of the media. This is done until microbial strains are obtained that are capable of growing in essentially crude oil as a carbon source and at a temperature range from about 70.degree. C. to 90.degree. C., at a pressure range from about 2,000 to 2,500 psi and at a salinity range from about 1.3 to 35%.

  15. Process for producing modified microorganisms for oil treatment at high temperatures, pressures and salinity

    DOE Patents [OSTI]

    Premuzic, E.T.; Lin, M.

    1996-02-20T23:59:59.000Z

    This invention relates to the preparation of new, modified organisms, through challenge growth processes, that are viable in the extreme temperature, pressure and pH conditions and salt concentrations of an oil reservoir and that are suitable for use in microbial enhanced oil recovery. The modified microorganisms of the present invention are used to enhance oil recovery and remove sulfur compounds and metals from the crude oil. The processes are comprised of steps which successively limit the carbon sources and increase the temperature, pressure and salinity of the media. This is done until microbial strains are obtained that are capable of growing in essentially crude oil as a carbon source and at a temperature range from about 70 C to 90 C, at a pressure range from about 2,000 to 2,500 psi and at a salinity range from about 1.3 to 35%. 68 figs.

  16. Soil and plant responses from land application of saline-sodic waters: Implications of management

    SciTech Connect (OSTI)

    Vance, G.F.; King, L.A.; Ganjegunte, G.K. [University of Wyoming, Laramie, WY (United States). Department for Renewable Resources

    2008-09-15T23:59:59.000Z

    Land application of co-produced waters from coalbed natural gas (CBNG) wells is one management option used in the Powder River Basin (PRB) of Wyoming and Montana. Unfortunately the co-produced CBNG waters may be saline and/or sodic. The objective of this study was to examine the effects of irrigation with CBNG waters on soils and plants in the PRB. Soil properties and vegetation responses resulting from 1 to 4 yr of saline sodic water (electrical conductivity (EC) 1.6-4.8 dS m{sup -1} sodium adsorption ratio (SAR), 17-57 mmol L- applications were studied during 2003 and 2004 field seasons on sites (Ustic Torriorthent Haplocambid, Haplargid and Paleargid) representing native range grasslands seeded grass hayfields and alfalfa hayfields. Parameters measured from each irrigated site were compared directly with representative non-irrigated sites. Soil chemical and physical parameters including pH, EC, SAR, exchangeable sodium percent, texture, bulk density, infiltration and Darcy flux rates, were measured at various depth intervals to 120 cm. Mulitple-year applications of saline sodic water produced consistent trends of increased soil EC AND SAR values to depths of 30 cm reduced surface infiltration rates and lowered Darcy flux rates to 120 cm. Significant differences (p {le} 0.05) were determined between irrigated and non-irrigated areas for EC, SAR infiltration rates and Darcy flux (p {le} 0.10) at most sites. Saline sodic CBNG water applications significantly increased native perennial grass biomass production and cover on irrigated as compared with non-irrigated sites; however overall species evenness decreased. Biological effects were variable and complex reflecting site-specific conditions and water and soil management strategies.

  17. Oil Recovery Increases by Low-Salinity Flooding: Minnelusa and Green River Formations

    SciTech Connect (OSTI)

    Eric P. Robertson

    2010-09-01T23:59:59.000Z

    Waterflooding is by far the most widely used method in the world to increase oil recovery. Historically, little consideration has been given in reservoir engineering practice to the effect of injection brine composition on waterflood displacement efficiency or to the possibility of increased oil recovery through manipulation of the composition of the injected water. However, recent work has shown that oil recovery can be significantly increased by modifying the injection brine chemistry or by injecting diluted or low salinity brine. This paper reports on laboratory work done to increase the understanding of improved oil recovery by waterflooding with low salinity injection water. Porous media used in the studies included outcrop Berea sandstone (Ohio, U.S.A.) and reservoir cores from the Green River formation of the Uinta basin (Utah, U.S.A.). Crude oils used in the experimental protocols were taken from the Minnelusa formation of the Powder River basin (Wyoming, U.S.A.) and from the Green River formation, Monument Butte field in the Uinta basin. Laboratory corefloods using Berea sandstone, Minnelusa crude oil, and simulated Minnelusa formation water found a significant relationship between the temperature at which the oil- and water-saturated cores were aged and the oil recovery resulting from low salinity waterflooding. Lower aging temperatures resulted in very little to no additional oil recovery, while cores aged at higher temperatures resulted in significantly higher recoveries from dilute-water floods. Waterflood studies using reservoir cores and fluids from the Green River formation of the Monument Butte field also showed significantly higher oil recoveries from low salinity waterfloods with cores flooded with fresher water recovering 12.4% more oil on average than those flooded with undiluted formation brine.

  18. Corrosion behavior of newly developed TiAgFe dental alloys in neutral saline solution

    E-Print Network [OSTI]

    Zheng, Yufeng

    Corrosion behavior of newly developed Ti­Ag­Fe dental alloys in neutral saline solution B. B. Zhang, B. L. Wang, L. Li and Y. F. Zheng* The corrosion behavior of Ti­5Ag­xFe alloys (x ¼ 1, 2.5, 5 wt) Ti,Ti­ 5Ag­xFe alloys exhibited higher corrosion potentials, lower current densities, and larger

  19. The influence of copper and bicarbonate ions on the corrosion of aluminum alloys saline solutions 

    E-Print Network [OSTI]

    Becerra-Diaz, Alcibiades

    1972-01-01T23:59:59.000Z

    Min. 99. 0 Remainder Remainder 1. Beryllium 0. 0008 Maximum for welding electrode and filler wire only ~Tem er The 1100-H14 Aluminum Alloy has been strain-hardened without supplementary thermal treatment. The 5052-H32 Aluminum Alloy has been...THE INFLUENCE OF COPPER AND BICARBONATE IONS ON THE CORROSION OF ALUMINUM ALLOYS IN SALINE SOLUTIONS A Thesis by ALCIBIADES BECERRA-DIAZ Submitted to the Graduate College of Texas A&M University in partial fulfillment of the requirement...

  20. Supplement to Diagnosis and Management of Salinity Problems in Irrigated Pecan Production: Salt Leaching

    E-Print Network [OSTI]

    Miyamoto, S.

    (e. g., Hanson and Bendixen, 1995). The flow under drip irrigation is largely unsaturated flow, and the evaporation-driven salinity increase associated with high frequency sprinkler irrigation is minimal with drip systems. This method... of leaching irrigation depend largely upon the existing irrigation system, and the types of soils involved. Several items, however, should be kept in mind. We already mentioned that it is preferable to apply leaching irrigation during the dormant period...

  1. Water Balance, Salt Loading, and Salinity Control Options of Red Bluff Reservoir, Texas

    E-Print Network [OSTI]

    Miyamoto, S.; Yuan, Fasong; Anand, Shilpa

    objectives: i) to outline water balance of the reservoir, ii) to establish salt loading trends over the past several decades, and iii) to evaluate the impact of salt loading on salinity of the reservoir and its outflow. We also outlined the needs... presumably has less seepage losses. The study reported here was conducted i) for examining the reservoir water balance of Red Bluff over the past several decades, ii) for establishing salt loading trends, and iii) for evaluating the impact of salt...

  2. Steric sea level variations during 19571994: Importance of salinity John I. Antonov

    E-Print Network [OSTI]

    ­3000 m layer during the 1957­1994 period resulted in a sea level rise at a mean rate of about 0.55 mm per sea level rise at a rate of 1.3 ± 0.5 mm/yr if the added water comes from sources other than floating and salinity variability, steric sea level, sea level rise, climate change, Labrador sea Citation: Antonov, J

  3. Tolerant Turf: Collaborators work to improve turfgrasses' response to drought and salinity

    E-Print Network [OSTI]

    Smith, Courtney

    2011-01-01T23:59:59.000Z

    , recurrent droughts, and increasing public demands on water resources mean that less potable water will be available for irrigation of turf landscapes and golf courses in the future. Chandra, assistant professor of turfgrass breeding and molecular... genetics at the Texas AgriLife Research and Extension Center at Dallas, and researchers from #18;ve other universities have partnered with three objectives in mind#30;to develop, improve, and commercialize drought- and salinity-tolerant turfgrass. #29...

  4. Wetland Plant Guide for Assessing Habitat Impacts of Real-Time Salinity Management

    SciTech Connect (OSTI)

    Quinn, Nigel W.T.; Feldmann, Sara A.

    2004-10-15T23:59:59.000Z

    This wetland plant guide was developed to aid moist soil plant identification and to assist in the mapping of waterfowl and shorebird habitat in the Grassland Water District and surrounding wetland areas. The motivation for this habitat mapping project was a concern that real-time salinity management of wetland drainage might have long-term consequences for wildfowl habitat health--changes in wetland drawdown schedules might, over the long term, lead to increased soil salinity and other conditions unfavorable to propagation of the most desirable moist soil plants. Hence, the implementation of a program to monitor annual changes in the most common moist soil plants might serve as an index of habitat health and sustainability. Our review of the current scientific and popular literature failed to identify a good, comprehensive field guide that could be used to calibrate and verify high resolution remote sensing imagery, that we had started to use to develop maps of wetland moist soil plants in the Grassland Water District. Since completing the guide it has been used to conduct ground truthing field surveys using the California Native Plant Society methodology in 2004. Results of this survey and a previous wetland plant survey in 2003 are published in a companion LBNL publication summarizing 4 years of fieldwork to advance the science of real-time wetland salinity management.

  5. Comparison of methods for geologic storage of carbon dioxide in saline formations

    SciTech Connect (OSTI)

    Goodman, Angela L. [U.S. DOE; Bromhal, Grant S. [U.S. DOE; Strazisar, Brian [U.S. DOE; Rodosta, Traci D. [U.S. DOE; Guthrie, William J. [U.S. DOE; Allen, Douglas E. [ORISE; Guthrie, George D. [U.S. DOE

    2013-01-01T23:59:59.000Z

    Preliminary estimates of CO{sub 2} storage potential in geologic formations provide critical information related to Carbon Capture, Utilization, and Storage (CCUS) technologies to mitigate CO{sub 2} emissions. Currently multiple methods to estimate CO{sub 2} storage and multiple storage estimates for saline formations have been published, leading to potential uncertainty when comparing estimates from different studies. In this work, carbon dioxide storage estimates are compared by applying several commonly used methods to general saline formation data sets to assess the impact that the choice of method has on the results. Specifically, six CO{sub 2} storage methods were applied to thirteen saline formation data sets which were based on formations across the United States with adaptations to provide the geologic inputs required by each method. Methods applied include those by (1) international efforts – the Carbon Sequestration Leadership Forum (Bachu et al., 2007); (2) United States government agencies – U.S. Department of Energy – National Energy Technology Laboratory (US-DOE-NETL, 2012) and United States Geological Survey (Brennan et al., 2010); and (3) the peer-reviewed scientific community – Szulczewski et al. (2012) and Zhou et al. (2008). A statistical analysis of the estimates generated by multiple methods revealed that assessments of CO{sub 2} storage potential made at the prospective level were often statistically indistinguishable from each other, implying that the differences in methodologies are small with respect to the uncertainties in the geologic properties of storage rock in the absence of detailed site-specific characterization.

  6. High Resolution Simulation and Characterization of Density-Driven Flow in CO2 Storage in Saline Aquifers

    E-Print Network [OSTI]

    are routinely used to study the process of carbon dioxide (CO2) sequestration in saline aquifers. In this paper TOUGH2-MP. 1. Introduction Geologic carbon dioxide (CO2) sequestration involves injecting CO2

  7. Avicennia germinans (black mangrove) vessel architecture is linked to chilling and salinity tolerance in the Gulf of Mexico

    E-Print Network [OSTI]

    Madrid, Eric N.; Armitage, Anna R.; Lopez-Portillo, Jorge

    2014-09-26T23:59:59.000Z

    Over the last several decades, the distribution of the black mangrove Avicennia germinans in the Gulf of Mexico has expanded, in part because it can survive the occasional freeze events and high soil salinities characteristic of the area. Vessel...

  8. Community Metabolism Along Nutrient and Salinity Gradients of the Potomac River Estuary: An Application from Continuous Monitoring Sites

    E-Print Network [OSTI]

    Boynton, Walter R.

    Community Metabolism Along Nutrient and Salinity Gradients of the Potomac River Estuary to make metabolism estimates. We used data from 14 of these locations from March through October 2007

  9. Storage capacity and injection rate estimates for CO? sequestration in deep saline aquifers in the conterminous United States

    E-Print Network [OSTI]

    Szulczewski, Michael Lawrence

    2009-01-01T23:59:59.000Z

    A promising method to mitigate global warming is injecting CO? into deep saline aquifers. In order to ensure the safety of this method, it is necessary to understand how much CO? can be injected into an aquifer and at what ...

  10. Storing carbon dioxide in saline formations : analyzing extracted water treatment and use for power plant cooling.

    SciTech Connect (OSTI)

    Dwyer, Brian P.; Heath, Jason E.; Borns, David James; Dewers, Thomas A.; Kobos, Peter Holmes; Roach, Jesse D.; McNemar, Andrea; Krumhansl, James Lee; Klise, Geoffrey T.

    2010-10-01T23:59:59.000Z

    In an effort to address the potential to scale up of carbon dioxide (CO{sub 2}) capture and sequestration in the United States saline formations, an assessment model is being developed using a national database and modeling tool. This tool builds upon the existing NatCarb database as well as supplemental geological information to address scale up potential for carbon dioxide storage within these formations. The focus of the assessment model is to specifically address the question, 'Where are opportunities to couple CO{sub 2} storage and extracted water use for existing and expanding power plants, and what are the economic impacts of these systems relative to traditional power systems?' Initial findings indicate that approximately less than 20% of all the existing complete saline formation well data points meet the working criteria for combined CO{sub 2} storage and extracted water treatment systems. The initial results of the analysis indicate that less than 20% of all the existing complete saline formation well data may meet the working depth, salinity and formation intersecting criteria. These results were taken from examining updated NatCarb data. This finding, while just an initial result, suggests that the combined use of saline formations for CO{sub 2} storage and extracted water use may be limited by the selection criteria chosen. A second preliminary finding of the analysis suggests that some of the necessary data required for this analysis is not present in all of the NatCarb records. This type of analysis represents the beginning of the larger, in depth study for all existing coal and natural gas power plants and saline formations in the U.S. for the purpose of potential CO{sub 2} storage and water reuse for supplemental cooling. Additionally, this allows for potential policy insight when understanding the difficult nature of combined potential institutional (regulatory) and physical (engineered geological sequestration and extracted water system) constraints across the United States. Finally, a representative scenario for a 1,800 MW subcritical coal fired power plant (amongst other types including supercritical coal, integrated gasification combined cycle, natural gas turbine and natural gas combined cycle) can look to existing and new carbon capture, transportation, compression and sequestration technologies along with a suite of extracting and treating technologies for water to assess the system's overall physical and economic viability. Thus, this particular plant, with 90% capture, will reduce the net emissions of CO{sub 2} (original less the amount of energy and hence CO{sub 2} emissions required to power the carbon capture water treatment systems) less than 90%, and its water demands will increase by approximately 50%. These systems may increase the plant's LCOE by approximately 50% or more. This representative example suggests that scaling up these CO{sub 2} capture and sequestration technologies to many plants throughout the country could increase the water demands substantially at the regional, and possibly national level. These scenarios for all power plants and saline formations throughout U.S. can incorporate new information as it becomes available for potential new plant build out planning.

  11. Property:LithologyInfo | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere I Geothermal PwerPerkins County, Nebraska:PrecourtOid JumpEligSysSize JumpTechDsc JumpAlpha3

  12. Geochemistry of the Banded Iron Formations and their Host Rocks in the Eastern Desert of Egypt BACKUS, Ethan L.1, GAGNON, Kelli E.1, EL-SHAZLY, Aley K.1, and KHALIL, Khalil Isaac2

    E-Print Network [OSTI]

    El-Shazly, Aley

    Geochemistry of the Banded Iron Formations and their Host Rocks in the Eastern Desert of Egypt University, Egypt Sponsored by NSF-OISE-1004021 Session 92:T3. Sigma Gamma Epsilon Undergraduate Research over 30,000 km2 in the central Eastern Desert of Egypt. The deposits most resemble Algoma-type iron

  13. Cumulative soil chemistry changes from land application of saline-sodic waters

    SciTech Connect (OSTI)

    Ganjegunte, G.K.; King, L.A.; Vance, G.F. [University of Wyoming, Laramie, WY (United States). Department for Renewable Resources

    2008-09-15T23:59:59.000Z

    Management of large volumes (60,000 ha-m) of co-production water associated with coal bed natural gas (CBNG) water extraction is a potential concern in the Powder River Basin (PRB) of Wyoming and Montana due to elevated water salinity and sodicity levels. Land application of saline-sodic CBNG water is a common water management method being practiced in the PRB, which can result in deterioration in soil quality. The objective of this study was to evaluate effects from 1 to 4 yr of land application with CBNG water on soil chemical properties at six study sites (fine to loamy, mixed to smectitic, mesic, Ustic Ardisols and Entisols) in the Wyoming PRB region. Changes in chemistry of soils collected from six depths irrigated with CBNG water were compared with representative non-irrigated soils. Applications of CBNG water significantly increased soil EC, SAR, and ESP values (up to 21, 74, and 24 times, respectively) compared with non-irrigated soils. Differences in soil chemical properties between an irrigated and non-irrigated coarse-textured soil were less than that of fine-textured soils, emphasizing texture as an important factor for salinity buildup. Pretreatment of CBNG water using a sulfur burner and application of gypsum and elemental S soil amendments reduced soil pH but did not prevent the build-up of salts and sodium. Study results suggest that current CBNG water management strategies are not as effective as projected. Additional research is needed to develop management strategies appropriate for mitigating adverse effects of CBNG water irrigation.

  14. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR; VERNON FIELD, ISABELLA COUNTY, MI.

    SciTech Connect (OSTI)

    James R. Wood; A. Wylie; W. Quinlan

    2004-01-01T23:59:59.000Z

    The principal objective of this demonstration project is to test surface geochemical techniques for detecting trace amounts of light hydrocarbons in pore gases as a means of reducing risk in hydrocarbon exploration and production. During this reporting period, a new field demonstration, Springdale Prospect in Manistee County, Michigan was begun to assess the validity and usefulness of the microbial surface geochemical technique. The surface geochemistry data showed a fair-to-good microbial anomaly that may indicate the presence of a fault or stratigraphic facies change across the drilling path. The main news this reporting period is the confirmed discovery of producing hydrocarbons at the State Springdale & O'Driscoll No.16-16 demonstration well in Manistee County. This well was spudded in late November, tested and put on production in December 2003. To date it is flowing nearly 100 barrels of liquid hydrocarbons per day, which is a good well in Michigan. Reserves have not been established yet. The surface geochemistry sampling at the Springdale demonstration site will be repeated this spring after the well has been on production for several months to see if the anomaly pattern changes. We expect that the anomaly will diminish as the original positive (apical) anomaly is replaced by a negative (edge) anomaly, probably due to the pressure draw-down in the reservoir. This is the behavior that we observed at the Bear lake demonstration well reported last quarter.

  15. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR: VERNON FIELD, ISABELLA COUNTY, MI.

    SciTech Connect (OSTI)

    James R. Wood; W. Quinlan

    2003-07-01T23:59:59.000Z

    The principal objective of this demonstration project is to test surface geochemical techniques for detecting trace amounts of light hydrocarbons in pore gases as a means of reducing risk in hydrocarbon exploration and production. As part of the project, a field demonstration was undertaken to assess the validity and usefulness of the microbial surface geochemical technique. The surface geochemistry data showed a strong anomaly in the Myrtle Beach area that would justify drilling by itself and even more so in conjunction with the structural interpretation from the 3D seismic data. The Myrtle Beach geochemical survey indicated a good to excellent prospect which was confirmed by drilling. Presented in this quarterly report is the Case History and Well Summary for the Myrtle Beach area in Burke County, North Dakota. This case history presents the important technical details regarding the geochemistry and the two vertical wells that are part of this field demonstration, and the applicability of these results to other demonstration projects. This format could be duplicated for other demonstration projects and is being used on all subsequent field demonstrations as they near completion.

  16. The effects of salinity on the growth and survival of the postlarval stages of Gambusia affinis

    E-Print Network [OSTI]

    Omundson, Glenn Erwin

    1963-01-01T23:59:59.000Z

    of MASTER OP SCIBNCB january l963 Ma Jor Subject: Biological Oceanography THE EFFECTS OF SALINIIY ON THE GROWTH AND SURVIVAL OF THE POSI'LARVAL STAGES OF GAMBUSIA AFFINIS A Thesis Glenn Erwln Omundson h aved as to style and content by: Irman of Com... on the growth of the poetlarval stages of Gambusia affinis, This was accomplished by controlling all environmental factors other than salinity, l. e. , temperature, food, light, pH and fish per unit volume of water. CHAPTER II MATERIALS AND METHODS...

  17. Impact of background flow on dissolution trapping of carbon dioxide injected into saline aquifers

    E-Print Network [OSTI]

    Rapaka, Saikiran

    2011-01-01T23:59:59.000Z

    While there has been a large interest in studying the role of dissolution-driven free convection in the context of geological sequestration, the contribution of forced convection has been largely ignored. This manuscript considers CO$_2$ sequestration in saline aquifers with natural background flow and uses theoretical arguments to compute the critical background velocity needed to establish the forced convective regime. The theoretical arguments are supported by two dimensional high-resolution numerical simulations which demonstrate the importance of forced convection in enhancing dissolution in aquifers characterised by low Rayleigh numbers.

  18. Respiratory response of the sea anemone Bunodosoma cavernata (Bosc) to changes in temperature and salinity

    E-Print Network [OSTI]

    Retzer, Kent Arnold

    1985-01-01T23:59:59.000Z

    of Respiratory Rate . 6 2 Analysis of Variance Procedure for 0-2 Hour Average. . . 12 3 Analysis of Variance Procedure for 30 Minutes 13 Duncan's Multiple Range Test for 30 Minutes and 0-2 Hour Average and Acclimation Temperature 5 Duncan's Multiple Range... Test for 30 Minutes and 0-2 Hour Average and Experimental Temperature . 15 16 6 Duncan's Multiple Range Test for 30 Minutes and 0-2 Hour Average and Experimental Salinity 17 7 Duncan's Multiple Range Test for 30 Minutes and 0-2 Hour Average...

  19. Effects of Salinity and Specific Ions on Seedling Emergence and Growth of Onions

    E-Print Network [OSTI]

    Miyamoto, S.; Martinez, I.; Niu, G.

    Rio Grande Valley. Harkey silt loam was collected in September of 2006 from the A P horizon of a field planted to cotton in previous years at two locations; the middle of a disked field, and a flat water check-in basin. These samples are numbered... 1 and 2, respectively (Table 1). In addition, the third soil sample designated as Harkey silt loam 3 was used after leaching a check-in basin with tap water in October, 2006 in order to have a soil sample with low salinity. These samples were air...

  20. Flow Instabilities During Injection of CO2 into SalineAquifers

    SciTech Connect (OSTI)

    Garcia, Julio E.; Pruess, Karsten

    2003-04-15T23:59:59.000Z

    Injection of carbon dioxide (CO{sub 2}) into saline aquifers has been proposed as a means to reduce greenhouse gas emissions (geological carbon sequestration). The injection process can be classified as immiscible displacement of an aqueous phase by a less dense and less viscous gas phase. Under disposal conditions (supercritical CO{sub 2}) the viscosity of carbon dioxide can be less than the viscosity of the aqueous phase by a factor of 15. Because of the lower viscosity, the CO{sub 2} displacement front will have a tendency towards instability so that waves or rounded lobes of saturation may appear and grow into fingers that lead to enhanced dissolution, bypassing, and possibly poor sweep efficiency. This paper presents an analysis, through high-resolution numerical simulations, of the onset of instabilities (viscous fingering) during injection of CO{sub 2} into saline aquifers. We explore the influence of viscosity ratio, relative permeability functions, and capillary pressure on finger growth and spacing. In addition, we address the issues of finger triggering, convergence under grid refinement and boundary condition effects. Simulations were carried out on scalar machines, and on an IBM RS/6000 SP (a distributed-memory parallel computer with 6080 processors) with a parallelized version of TOUGH2.

  1. Monitoring of saline tracer movement with vertically distributed self-potential measurements at the HOBE agricultural test site, Voulund, Denmark

    E-Print Network [OSTI]

    Jougnot, Damien; Haarder, Eline B; Looms, Majken C

    2015-01-01T23:59:59.000Z

    The self-potential (SP) method is sensitive to water fluxes in saturated and partially saturated porous media, such as those associated with rainwater infiltration and groundwater recharge. We present a field-based study at the Voulund agricultural test site, Denmark, that is, to the best of our knowledge, the first to focus on the vertical self-potential distribution prior to and during a saline tracer test. A coupled hydrogeophysical modeling framework is used to simulate the SP response to precipitation and saline tracer infiltration. A layered hydrological model is first obtained by inverting dielectric and matric potential data. The resulting model that compares favorably with electrical resistance tomography models is subsequently used to predict the SP response. The electrokinetic contribution (caused by water fluxes in a charged porous soil) is modeled by an effective excess charge approach that considers both water saturation and pore water salinity. Our results suggest that the effective excess char...

  2. Geochemistry of FBC waste-coal slurry solid mixtures. Final technical report, September 1, 1992--August 31, 1993

    SciTech Connect (OSTI)

    Dreher, G.B.; Roy, W.R.; Steele, J.D.; Heidari, M. [Illinois State Geological Survey, Champaign, IL (United States)

    1993-12-31T23:59:59.000Z

    The three tasks conducted in this research project were related to understanding the geochemistry and mineralogy of the co-disposal of fluidized bed combustion (FBC) wastes with coal slurry solid (CSS) from a coal preparation plant. During coal cleaning, pyrite, other heavy minerals and rock fragments are separated from the coal and discharged in an aqueous slurry to an impoundment. After dewatering and closure of the impoundment, the pyrite can oxidize and produce acid that can migrate into the underlying groundwater system. The addition of FBC residue to the CSS will buffer the pore water pH to approximately 7.8. In Task 1, soluble components and acid-base react ion products from mixtures of FBC waste and CSS were extracted for 3 to 180 days in aqueous batch experiments. The results of these extractions showed that, eventually, the extracts would attain a pH between 7 and 8. That pH range is characteristic of an aqueous system in equilibrium with calcite, gypsum, and atmospheric carbon dioxide. After 180 days, the mean calcium concentration in all of the extracts was 566{+-}18 mg/L and sulfate concentrations averaged 2420{+-}70 mg/L. In Task 2, three extracts from CSS/FBC residue mixtures were prepared for use in experiments to determine the adsorption/desorption reactions that occur between solutes in the extracts and two common Illinois soils. Time constraints allowed the use of only two of the extracts for adsorption studies. The concentrations of most solutes were not significantly lowered by adsorption at the pH of the extract-soil suspension, nor over a wide range of pH. The results suggest that the type of solutes that were released by the CSS/FBC residue mixture would not be attenuated by adsorption. In a modified Task 3, the literature on the kinetics of pyrite oxidation in near-neutral to alkaline pH was reviewed in preparation for future development of a computer model of pyrite oxidation in CSS/FBC residue codisposal.

  3. Non-Fickian Diffusion Affects the Relation between the Salinity and Hydrate Capacity Profiles in Marine Sediments

    E-Print Network [OSTI]

    Denis S Goldobin

    2012-06-20T23:59:59.000Z

    On-site measurements of water salinity (which can be directly evaluated from the electrical conductivity) in deep-sea sediments is technically the primary source of indirect information on the capacity of the marine deposits of methane hydrates. We show the relation between the salinity (chlorinity) profile and the hydrate volume in pores to be significantly affected by non-Fickian contributions to the diffusion flux---the thermal diffusion and the gravitational segregation---which have been previously ignored in the literature on the subject and the analysis of surveys data. We provide amended relations and utilize them for an analysis of field measurements for a real hydrate deposit.

  4. Well injectivity during CO2 storage operations in deep saline aquifers6 1: Experimental investigation of drying effects, salt precipitation and7

    E-Print Network [OSTI]

    Boyer, Edmond

    Carbon Capture and Storage (CCS) is a technique than can potentially limit the accumulation29-17Jan2014 #12;3 1. Introduction51 52 Geological sequestration of CO2 into deep saline aquifers studied54 much less than mature oil & gas reservoirs. Injection of carbon dioxide into saline aquifers55

  5. An investigation of a method of determining the salinity of sea water by the electrical conduction method without the use of electrodes

    E-Print Network [OSTI]

    Adams, William Floyd

    1954-01-01T23:59:59.000Z

    than 2. 5 ~. Thus, ths standaxd watt- mster used in this investigation cauM be usai to detect salinity ebangm of ons yart pmr thxnxsexxi, since it ws obis to detect salinity changes of tem yarts yer thxsxsand in t?dm ixmmstigstiom. If a by...

  6. Subseabed Disposal Project annual report, FY85 to termination of project: Physical Oceanography and Water Column Geochemistry Studies, October 1984 through May 1986

    SciTech Connect (OSTI)

    Kupferman, S.L. (ed.)

    1987-05-01T23:59:59.000Z

    This report covers the work of the Physical Oceanography and Water Column Geochemistry (POWCG) Studies Group of the Subseabed Disposal Project (SDP) from October 1984 to termination of the project in May 1986. The overview of the work includes an introduction, general descriptions of the activities, and a summary. Detailed discussions are included as appendices. During the period of this report the POWCG Studies Group held a meeting to develop a long-term research plan for the Nares Abyssal Plain, which was recently designated as a study area for the Environmental Study Group of the SDP. The POWCG Studies Group has also planned and participated in two interdisciplinary oceanographic missions to the Nares which have resulted in the acquisition of data and samples which can be used to begin to understand the workings of the ecosystem at the site, and for developing a preliminary site assessment. The papers in the appendices have been processed for inclusion in the Energy Data Base.

  7. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR: VERNON FIELD, ISABELLA COUNTY, MI.

    SciTech Connect (OSTI)

    James R. Wood; T.J. Bornhorst; S.D. Chittick; William B. Harrison; W. Quinlan

    2002-01-01T23:59:59.000Z

    In this reporting period, we extended the fault study to include more faults and developed new techniques to visualize the faults. We now have used data from the Dundee Formation to document 11 major faults in the Michigan Basin and are in the process of reviewing data from other horizons. These faults appear to control the locations of many of the large anticlinal structures in the Michigan Basin and likely controlled fluid movements as well. The surface geochemistry program is also moving along well with emphasis on measuring samples collected last sampling season. The new laboratory is now functional and has been fully staffed as of December. The annual project review has been set for March 7-9 in Tampa, Florida. Contracts are being prepared for drilling the Bower's prospects in Isabella County, Michigan, this spring or summer.

  8. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR: VERNON FIELD, ISABELLA COUNTY, MI

    SciTech Connect (OSTI)

    James R. Wood; A. Wylie; W. Quinlan

    2004-04-01T23:59:59.000Z

    One of the main objectives of this demonstration project is to test surface geochemical techniques for detecting trace amounts of light hydrocarbons in pore gases as a means of reducing risk in hydrocarbon exploration and production. As part of the project, several field demonstrations were undertaken to assess the validity and usefulness of the microbial surface geochemical technique. The important observations from each of these field demonstrations are briefly reviewed in this annual report. These demonstrations have been successful in identifying the presence or lack of hydrocarbons in the subsurface and can be summarized as follows: (1) The surface geochemistry data showed a fair-to-good microbial anomaly that may indicate the presence of a fault or stratigraphic facies change across the drilling path of the State Springdale & O'Driscoll No.16-16 horizontal demonstration well in Manistee County, Michigan. The well was put on production in December 2003. To date, the well is flowing nearly 100 barrels of liquid hydrocarbons per day plus gas, which is a good well in Michigan. Reserves have not been established yet. Two successful follow-up horizontal wells have also been drilled in the Springdale area. Additional geochemistry data will be collected in the Springdale area in 2004. (2) The surface geochemistry sampling in the Bear Lake demonstration site in Manistee County, Michigan was updated after the prospect was confirmed and production begun; the original subsurface and seismic interpretation used to guide the location of the geochemical survey for the Charlich Fauble re-entry was different than the interpretation used by the operator who ultimately drilled the well. As expected, the anomaly appears to be diminishing as the positive (apical) microbial anomaly is replaced by a negative (edge) anomaly, probably due to the pressure draw-down in the reservoir. (3) The geochemical sampling program over the Vernon Field, Isabella County, Michigan is now interpreted as a large negative anomaly associated with the entire field. The results of the State Smock horizontal well and the Bowers 4-25 well confirmed the lack of additional recoverable hydrocarbons in the Vernon Field. (4) The surface geochemistry data showed a strong anomaly in the Myrtle Beach, Burke County, North Dakota area that would justify drilling by itself and even more so in conjunction with the structural interpretation from the geological and geophysical data; the microbial values here were the highest we have observed. The Myrtle Beach geochemical survey indicated a good to excellent prospect which was confirmed by drilling, however, a pipeline has not yet been completed that would allow the wells to be placed into production. We also present in this annual report the results of recent efforts to map carbonate facies tracts in the middle Devonian Dundee and Rogers City Limestones using gamma ray, bulk density, and photoelectric effect geophysical well log amplitudes. This work was undertaken to identify fairways for exploration in the Dundee and Rogers City where surface geochemical techniques could then be used to screen potential leads.

  9. Quality Control of Temperature and Salinity from CTD based on Anomaly Detection

    E-Print Network [OSTI]

    Castelão, Guilherme P

    2015-01-01T23:59:59.000Z

    The CTD is a set of sensors used by oceanographers to measure fundamental hydrographic properties of the oceans. It is characterized by a high precision product, only achieved if a quality control procedure identifies and removes the bad samples. Such procedure has been traditionally done by a sequence of independent tests that minimize false negatives. It is here proposed a novel approach to identify the bad samples as anomalies in respect to the typical behavior of good data. Several tests are combined into a single multidimensional evaluation to provide a more flexible classification criterion. The traditional approach is reproduced with an error of 0.04%, otherwise, the Anomaly Detection technique surpasses the reference if calibrated by visual inspection. CoTeDe is a Python package developed to apply the traditional and the Anomaly Detection quality control of temperature and salinity data from CTD, and can be extended to XBT, ARGO and other sensors.

  10. Simulation of Coupled Processes of Flow, Transport, and Storage of CO2 in Saline Aquifers

    SciTech Connect (OSTI)

    Wu, Yu-Shu; Chen, Zizhong; Kazemi, Hossein; Yin, Xiaolong; Pruess, Karsten; Oldenburg, Curt; Winterfeld, Philip; Zhang, Ronglei

    2014-09-30T23:59:59.000Z

    This report is the final scientific one for the award DE- FE0000988 entitled “Simulation of Coupled Processes of Flow, Transport, and Storage of CO2 in Saline Aquifers.” The work has been divided into six tasks. In task, “Development of a Three-Phase Non-Isothermal CO2 Flow Module,” we developed a fluid property module for brine-CO2 mixtures designed to handle all possible phase combinations of aqueous phase, sub-critical liquid and gaseous CO2, supercritical CO2, and solid salt. The thermodynamic and thermophysical properties of brine-CO2 mixtures (density, viscosity, and specific enthalpy of fluid phases; partitioning of mass components among the different phases) use the same correlations as an earlier fluid property module that does not distinguish between gaseous and liquid CO2-rich phases. We verified the fluid property module using two leakage scenarios, one that involves CO2 migration up a blind fault and subsequent accumulation in a secondary “parasitic” reservoir at shallower depth, and another investigating leakage of CO2 from a deep storage reservoir along a vertical fault zone. In task, “Development of a Rock Mechanical Module,” we developed a massively parallel reservoir simulator for modeling THM processes in porous media brine aquifers. We derived, from the fundamental equations describing deformation of porous elastic media, a momentum conservation equation relating mean stress, pressure, and temperature, and incorporated it alongside the mass and energy conservation equations from the TOUGH2 formulation, the starting point for the simulator. In addition, rock properties, namely permeability and porosity, are functions of effective stress and other variables that are obtained from the literature. We verified the simulator formulation and numerical implementation using analytical solutions and example problems from the literature. For the former, we matched a one-dimensional consolidation problem and a two-dimensional simulation of the Mandel-Cryer effect. For the latter, we obtained a good match of temperature and gas saturation profiles, and surface uplift, after injection of hot fluid into a model of a caldera structure. In task, “Incorporation of Geochemical Reactions of Selected Important Species,” we developed a novel mathematical model of THMC processes in porous and fractured saline aquifers, simulating geo-chemical reactions associated with CO2 sequestration in saline aquifers. Two computational frameworks, sequentially coupled and fully coupled, were used to simulate the reactions and transport. We verified capabilities of the THMC model to treat complex THMC processes during CO2 sequestration by analytical solutions and we constructed reactive transport models to analyze the THMC process quantitatively. Three of these are 1D reactive transport under chemical equilibrium, a batch reaction model with equilibrium chemical reactions, and a THMC model with CO2 dissolution. In task “Study of Instability in CO2 Dissolution-Diffusion-Convection Processes,” We reviewed literature related to the study of density driven convective flows and on the instability of CO2 dissolution-diffusion-convection processes. We ran simulations that model the density-driven flow instability that would occur during CO2 sequestration. CO2 diffused through the top of the system and dissolved in the aqueous phase there, increasing its density. Density fingers formed along the top boundary, and coalesced into a few prominent ones, causing convective flow that forced the fluid to the system bottom. These simulations were in two and three dimensions. We ran additional simulations of convective mixing with density contrast caused by variable dissolved CO2 concentration in saline water, modeled after laboratory experiments in which supercritical CO2 was circulated in the headspace above a brine saturated packed sand in a pressure vessel. As CO2 dissolved into the upper part of the saturated sand, liquid phase density increases causing instability and setting off convective mixing. We obtained good agreement

  11. Feasibility of Geophysical Monitoring of Carbon-Sequestrated Deep Saline Aquifers

    SciTech Connect (OSTI)

    Mallick, Subhashis; Alvarado, Vladimir

    2013-09-30T23:59:59.000Z

    As carbon dioxide (CO{sub 2}) is sequestered from the bottom of a brine reservoir and allowed to migrate upward, the effects of the relative permeability hysteresis due to capillary trapping and buoyancy driven migration tend to make the reservoir patchy saturated with different fluid phases over time. Seismically, such a patchy saturated reservoir induces an effective anisotropic behavior whose properties are primarily dictated by the nature of the saturation of different fluid phases in the pores and the elastic properties of the rock matrix. By combining reservoir flow simulation and modeling with seismic modeling, it is possible to derive these effective anisotropic properties, which, in turn, could be related to the saturation of CO{sub 2} within the reservoir volume any time during the post-injection scenario. Therefore, if time-lapse seismic data are available and could be inverted for the effective anisotropic properties of the reservoir, they, in combination with reservoir simulation could potentially predict the CO{sub 2} saturation directly from the time-lapse seismic data. It is therefore concluded that the time-lapse seismic data could be used to monitor the carbon sequestrated saline reservoirs. But for its successful implementation, seismic modeling and inversion methods must be integrated with the reservoir simulations. In addition, because CO{sub 2} sequestration induces an effective anisotropy in the sequestered reservoir and anisotropy is best detected using multicomponent seismic data compared to single component (P-wave) data, acquisition, processing, and analysis is multicomponent seismic data is recommended for these time-lapse studies. Finally, a successful implementation of using time-lapse seismic data for monitoring the carbon sequestrated saline reservoirs will require development of a robust methodology for inverting multicomponent seismic data for subsurface anisotropic properties.

  12. The blue crab Callinectes sapidus inhabits estuarine environments that range in salinity from full-strength sea water

    E-Print Network [OSTI]

    Kinsey, Stephen

    The blue crab Callinectes sapidus inhabits estuarine environments that range in salinity from full euryhaline organisms, blue crabs have evolved compensatory mechanisms to minimize perturbations to the intracellular environment during osmotic stress. While the hemolymph of blue crabs fluctuates iso- osmotically

  13. 2004-2005 Texas Water Resources Institute Mills Scholarship Application Water Management, Soil Salinity and Landscape Ecology in Laguna

    E-Print Network [OSTI]

    Herbert, Bruce

    2004-2005 Texas Water Resources Institute Mills Scholarship Application Water Management, Soil-exist, sustainable water resource management strategies must be developed (Hutjes, 1998). The development Management, Soil Salinity and Landscape Ecology in Laguna Atascosa National Wildlife Refuge Nature of Problem

  14. Environmental sensor networks and continuous data quality assurance to manage salinity within a highly regulated river basin

    SciTech Connect (OSTI)

    Quinn, N.W.T.; Ortega, R.; Holm, L.

    2010-01-05T23:59:59.000Z

    This paper describes a new approach to environmental decision support for salinity management in the San Joaquin Basin of California that focuses on web-based data sharing using YSI Econet technology and continuous data quality management using a novel software tool, Aquarius.

  15. Changes in the resistance to water movement through the soil/plant pathway in salinized sunflower (Helianthus giganteus)

    E-Print Network [OSTI]

    Balint, Donna Elizabeth

    1993-01-01T23:59:59.000Z

    of transpiration values, resistance to water flow across the roots, and between roots and leaves could be calculated. By 5 and 6 days of salinization, there were increases in the resistance to water flow across roots at the 75 mM and higher salt levels...

  16. MODELING OF CO2 LEAKAGE UP THROUGH AN ABANDONED WELL FROM DEEP SALINE AQUIFER TO SHALLOW FRESH

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    1 MODELING OF CO2 LEAKAGE UP THROUGH AN ABANDONED WELL FROM DEEP SALINE AQUIFER TO SHALLOW FRESH restricted to: (i) supercritical CO2 injection and storage within the Dogger reservoir aquifer, (ii) CO2 the cement-rock formation interface in the abandoned well (iii) impacts on the Albian aquifer water quality

  17. Total thermoelectric-power withdrawals Freshwater thermoelectric-power withdrawals Saline-water thermoelectric-power withdrawals

    E-Print Network [OSTI]

    Total thermoelectric-power withdrawals Freshwater thermoelectric-power withdrawals Saline-water thermoelectric-power withdrawals Louisiana New Hampshire Florida Idaho Washington Oregon Nevada California New,000 9,000 to 13,000 Thermoelectric-power withdrawals by water quality and State, 2005. Estimated Use

  18. Impact of porous medium desiccation during anhydrous CO2 injection in deep saline aquifers: up scaling from experimental

    E-Print Network [OSTI]

    Boyer, Edmond

    flow rate and capillary properties on the desiccation mechanisms. Keywords: supercritical CO2, dryingImpact of porous medium desiccation during anhydrous CO2 injection in deep saline aquifers: up - France Abstract Injection of CO2 in geological reservoirs or deep aquifers is nowadays studied

  19. HARMONIC FUNCTIONS FOR SEA-SURFACE TEMPERATURES AND SALINITIES, KOKO HEAD, OAHU, 1956-69, AND SEA-SURFACE

    E-Print Network [OSTI]

    HARMONIC FUNCTIONS FOR SEA-SURFACE TEMPERATURES AND SALINITIES, KOKO HEAD, OAHU, 1956-69, AND SEA-SURFACE TEMPERATURES, CHRISTMAS ISLAND, 1954-69 GUNTHER It SECKEL' AND MARIAN Y. Y. YONG' ABSTRACT Harmonic functions, with daily sampling, are on average 0.07° C. Harmonic analysis spanning the entire sampling duration shows

  20. Sandia Energy - Molecular Geochemistry

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

    molecular spectroscopy, and molecular simulation to complex multicomponent and multiphase systems; particular emphasis on the use of molecular simulation and various...

  1. Comments on: Geochemistry

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

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2Climate,CobaltColdin679April

  2. Sandia Energy - Geochemistry

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

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch > TheNuclear Press ReleasesInAppliedEnergy Storage

  3. Sandia Energy - Molecular Geochemistry

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

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645U.S. DOE Office of ScienceandMesa del Sol Home Distribution Grid Integration Permalink Gallery Mesa delMissionMolecular

  4. EXPERIMENTAL DESIGN APPLICATIONS FOR MODELING AND ASSESSING CARBON DIOXIDE SEQUESTRATION IN SALINE AQUIFERS

    SciTech Connect (OSTI)

    Rogers, John

    2014-08-31T23:59:59.000Z

    This project was a computer modeling effort to couple reservoir simulation and ED/RSM using Sensitivity Analysis, Uncertainty Analysis, and Optimization Methods, to assess geologic, geochemical, geomechanical, and rock-fluid effects and factors on CO2 injectivity, capacity, and plume migration. The project objective was to develop proxy models to simplify the highly complex coupled geochemical and geomechanical models in the utilization and storage of CO2 in the subsurface. The goals were to investigate and prove the feasibility of the ED/RSM processes and engineering development, and bridge the gaps regarding the uncertainty and unknowns of the many geochemical and geomechanical interacting parameters in the development and operation of anthropogenic CO2 sequestration and storage sites. The bottleneck in this workflow is the high computational effort of reactive transport simulation models and large number of input variables to optimize with ED/RSM techniques. The project was not to develop the reactive transport, geomechanical, or ED/RSM software, but was to use what was commercially and/or publically available as a proof of concept to generate proxy or surrogate models. A detailed geologic and petrographic mineral assemblage and geologic structure of the doubly plunging anticline was defined using the USDOE RMOTC formations of interest data (e.g., Lower Sundance, Crow Mountain, Alcova Limestone, and Red Peak). The assemblage of 23 minerals was primarily developed from literature data and petrophysical (well log) analysis. The assemblage and structure was input into a commercial reactive transport simulator to predict the effects of CO2 injection and complex reactions with the reservoir rock. Significant impediments were encountered during the execution phase of the project. The only known commercial reactive transport simulator was incapable of simulating complex geochemistry modeled in this project. Significant effort and project funding was expended to determine the limitations of both the commercial simulator and the Lawrence Berkeley National Laboratory (LBNL) R&D simulator, TOUGHREACT available to the project. A simplified layer cake model approximating the volume of the RMOTC targeted reservoirs was defined with 1-3 minerals eventually modeled with limited success. Modeling reactive transport in porous media requires significant computational power. In this project, up to 24 processors were used to model a limited mineral set of 1-3 minerals. In addition, geomechanical aspects of injecting CO2 into closed, semi-open, and open systems in various well completion methods was simulated. Enhanced Oil Recovery (EOR) as a storage method was not modeled. A robust and stable simulation dataset or base case was developed and used to create a master dataset with embedded instructions for input to the ED/RSM software. Little success was achieved toward the objective of the project using the commercial simulator or the LBNL simulator versions available during the time of this project. Several hundred realizations were run with the commercial simulator and ED/RSM software, most having convergence problems and terminating prematurely. A proxy model for full field CO2 injection sequestration utilization and storage was not capable of being developed with software available for this project. Though the chemistry is reasonably known and understood, based on the amount of effort and huge computational time required, predicting CO2 sequestration storage capacity in geologic formations to within the program goals of ±30% proved unsuccessful.

  5. Energy issues for construction of 10 nm sized electrostatic traps in saline solution

    E-Print Network [OSTI]

    Jingkun Guo; Zijin Lei; Shengyong Xu

    2015-05-02T23:59:59.000Z

    Microsized electrostatic tweezers for trapping and manipulating charged microparticles have been demonstrated in previous work. Nanosized electrostatic tweezers may play an important role in nanoscience and bioscience, yet it remains as a technical challenge. We presented here simulations on an artificial nanostructure of certain charge distribution. Energy-related issues in terms of electrostatic energy, entropy and free energy were discussed in detail for such a system working in an ionic saline solution. The results showed that at a nanostructure dimension of ten nanometers, it was still feasible to trap a smaller charged nanoparticle, and the entropy term induced by charge distribution was found critical in the total amount of free energy. The trapping performance is found affected by the choice of device material due to van der Waals interactions. In addition, possible interplays among the modeled nanostructures with varied charge distribution were calculated. This work may provide useful clues for construction of artificial electrostatic nano-tweezers, and it may also help for a better understand for the interplays among a variety of bio-macromolecules in a live cell.

  6. Influence of geothermal sources on deep ocean temperature, salinity, and flow fields. Doctoral thesis

    SciTech Connect (OSTI)

    Speer, K.G.

    1988-06-01T23:59:59.000Z

    The thesis studies the effect of geothermal sources on the deep circulation, temperature and salinity fields. In Chapter 1 background material is given on the strength and distribution of geothermal heating. In Chapter 2 evidence for the influence of a hydrothermal system in the rift valley of the Mid-Atlantic Ridge on nearby property fields and a model of the flow around such a heat source are presented, with an analysis of a larger-scale effect. Results of an analytical model for a heat source on a Beta-plane in Chapter 3 show how the response far from the source can have a structure different from the forcing because of its dependence on two parameters: a Peclet number (the ratio of horizontal advection and vertical diffusion), and a Froude-number-like parameter (the ratio of long wave phase speed to background flow speed) which control the relative amount of damping and advection of different vertical scales. The solutions emphasize the different behavior of a dynamical field like temperature compared to tracers introduced at the source. These ideas are useful for interpreting more-complicated solutions from a numerical model presented in the final chapter.

  7. Increasing gas hydrate formation temperature for desalination of high salinity produced water with secondary guests

    SciTech Connect (OSTI)

    Cha, Jong-Ho [ORISE; Seol, Yongkoo [U.S. DOE

    2013-01-01T23:59:59.000Z

    We suggest a new gas hydrate-based desalination process using water-immiscible hydrate formers; cyclopentane (CP) and cyclohexane (CH) as secondary hydrate guests to alleviate temperature requirements for hydrate formation. The hydrate formation reactions were carried out in an isobaric condition of 3.1 MPa to find the upper temperature limit of CO2 hydrate formation. Simulated produced water (8.95 wt % salinity) mixed with the hydrate formers shows an increased upper temperature limit from ?2 °C for simple CO2 hydrate to 16 and 7 °C for double (CO2 + CP) and (CO2 + CH) hydrates, respectively. The resulting conversion rate to double hydrate turned out to be similar to that with simple CO2 hydrate at the upper temperature limit. Hydrate formation rates (Rf) for the double hydrates with CP and CH are shown to be 22 and 16 times higher, respectively, than that of the simple CO2 hydrate at the upper temperature limit. Such mild hydrate formation temperature and fast formation kinetics indicate increased energy efficiency of the double hydrate system for the desalination process. Dissociated water from the hydrates shows greater than 90% salt removal efficiency for the hydrates with the secondary guests, which is also improved from about 70% salt removal efficiency for the simple hydrates.

  8. Routine metabolism and critical oxygen concentration for juvenile red drum Sciaenops ocellatus as functions of water hardness and salinity 

    E-Print Network [OSTI]

    Schlechte, John Warren

    1989-01-01T23:59:59.000Z

    ROUTINE METABOLISM AND CRITICAL OXYGEN CONCENTRATION FOR JUVENILE RED DRUM SCIAENOPS OCELLATUS AS FUNCTIONS OF WATER HARDNESS AND SALINITY A Thesis by JOHN WARREN SCHLECHTE Submitted to the Office of Graduate Studie~ of Texas A&M University... in partial fulf illmert of the r equirements for the degree of MASTER OF SCIENLF May 19BS' Major Subject: Wildlife and Fisheries Sciences RQLIT INE METABOL I SM AND CRITICAL OXYGEN CONCENTRAT ION FOR JUVENILE RED DRUM SCIAENOPS QCELLATUS AS FUNCTIONS QF...

  9. Electrochemical corrosion behavior of biomedical Ti22Nb and Ti22Nb6Zr alloys in saline medium

    E-Print Network [OSTI]

    Zheng, Yufeng

    Electrochemical corrosion behavior of biomedical Ti­22Nb and Ti­22Nb­6Zr alloys in saline medium B addition and potentiodynamic polarization on the microstructure and corrosion resistance of Ti­22Nb and Ti­22Nb­6Zr alloy samples.The corrosion tests were carried out in 0.9% NaCl at 37 8C and neutral p

  10. ECO2N - A New TOUGH2 Fluid Property Module for Studies of CO2Storage in Saline Aquifers

    SciTech Connect (OSTI)

    Pruess, Karsten; Spycher, Nicholas

    2006-04-17T23:59:59.000Z

    ECO2N is a fluid property module for the TOUGH2 simulator (Version 2.0) that was designed for applications to geologic storage of CO{sub 2} in saline aquifers. It includes a comprehensive description of the thermodynamics and thermophysical properties of H{sub 2}O-NaCl-CO{sub 2} mixtures, that reproduces fluid properties largely within experimental error for the temperature, pressure and salinity conditions of interest(10 C {le} T {le} 110 C; P {le} 600 bar; salinity up to full halite saturation). Flow processes can be modeled isothermally or non-isothermally, and phase conditions represented may include a single (aqueous or CO{sub 2}-rich) phase, as well as two-phase mixtures. Fluid phases may appear or disappear in the course of a simulation, and solid salt may precipitate or dissolve. ECO2N can model super- as well as sub-critical conditions, but it does not make a distinction between liquid and gaseous CO{sub 2}. This paper highlights significant features of ECO2N, and presents illustrative applications.

  11. Scaling of capillary trapping in unstable two-phase flow: Application to CO[subscript 2] sequestration in deep saline aquifers

    E-Print Network [OSTI]

    Szulczewski, Michael L.

    The effect of flow instabilities on capillary trapping mechanisms is a major source of uncertainty in CO2 sequestration in deep saline aquifers. Standard macroscopic models of multiphase flow in porous media are unable to ...

  12. The Footprint of the CO[subscript 2] Plume during Carbon Dioxide Storage in Saline Aquifers: Storage Efficiency for Capillary Trapping at the Basin Scale

    E-Print Network [OSTI]

    Juanes, Ruben

    We study a sharp-interface mathematical model of CO[subscript 2] migration in deep saline aquifers, which accounts for gravity override, capillary trapping, natural groundwater flow, and the shape of the plume during the ...

  13. Simplified 1-D Hydrodynamic and Salinity Transport Modeling of the Sacramento–San Joaquin Delta: Sea Level Rise and Water Diversion Effects

    E-Print Network [OSTI]

    Fleenor, William E.; Bombardelli, Fabian

    2013-01-01T23:59:59.000Z

    salinity simulations of sea level rise scenarios. AppendixSan Joaquin Delta: Sea Level Rise and Water Diversiona 1-D model of sea level rise in an estuary must account for

  14. The effect of temperature, salinity and pH on the fertilizability of the ova and fertilizing capacity of sperm of Fundulus heteroclitus

    E-Print Network [OSTI]

    Foster, Robert Sanford

    1975-01-01T23:59:59.000Z

    THE EFFECT OF TEMPERATURE, SALINITY AND PH ON THE FERTILIZABILITY OF THE OVA AND FERTILIZING CAPACITY OF SPERM OF FUNDULUS HETEROCLITUS A Thesis by Robert Sanford Foster, IY Submitted to the Graduate College of Texas A&M University... in partial fulfillment of the requirement for the degree of MASTER OF SCIENCE May 1975 Major Subject: Biology THE EFFECT OF TEMPERATURE, SALINITY AND PH ON THE FERTILIZABILITY OF THE OVA AND FERTILIZING CAPACITY OF SPERM OF FUNDULUS HETEROCLITUS A...

  15. Deltaic sedimentation in saline, alkaline Lake Bogoria, Kenya: Response to environmental change

    SciTech Connect (OSTI)

    Renaut, R.W. (Univ. of Saskatchewan, Saskatoon (Canada). Dept. of Geological Sciences); Tiercelin, J.J. (Univ. Bretagne Occidentale, Brest (France). Domaines Oceaniques)

    1993-03-01T23:59:59.000Z

    Lake Bogoria is a meromictic, saline (90 g/l TDS), alkaline (pH: 10.3) lake with Na-CO[sub 3]-Cl waters, located in a narrow half-graben in the central Kenya Rift. It is fed by hot springs, direct precipitation, and a series of ephemeral streams that discharge into the lake via small deltas and fan-deltas. Examination of the exposed deltas and >50 short cores from the lake floor, have revealed a wide range of deltaic and prodeltaic sediments, including turbidites and subaqueous debris-flow deposits. Studies of 3 long cores and the exposed delta stratigraphy have shown how the style of deltaic sedimentation has responded to environmental changes during the last 30,000 years. During humid periods when lake level is high the lake waters are fresher and less dense. Theoretically, high sediment yield and more constant discharge may promote underflow (hyperpycnal flow), generating low-density turbidity currents. In contrast, during low stages with dense brine, the less dense, inflowing waters carry fine sediment plumes toward the center of the lake where they settle from suspension (hypopycnal flow). Although applicable as a general model, the sediment record shows that reality is more complex. Variations in meromixis and level of the chemocline, together with local and temporal differences in sediment yield and discharge, may permit density flows even when the lake is under a predominant hypopycnal regime. During periods of aridity when sodium carbonate evaporites were forming, exposed delta plains were subject to desiccation with local development of calcrete and zeolitic paleosols.

  16. Geochemical evolution of highly alkaline and saline tank wasteplumes during seepage through vadose zone sediments

    SciTech Connect (OSTI)

    Wan, Jiamin; Tokunaga, Tetsu K.; Larsen, Joern T.; Serne, R. Jeff

    2002-12-01T23:59:59.000Z

    Leakage of highly saline and alkaline radioactive waste from storage tanks into underlying sediments is a serious environmental problem at the Hanford Site in Washington State. This study focuses on geochemical evolution of tank waste plumes resulting from interactions between the waste solution and sediment. A synthetic tank waste solution was infused into unsaturated Hanford sediment columns (0.2, 0.6, and 2 m )maintained at 70 C to simulate the field contamination process. Spatially and temporally resolved geochemical profiles of the waste plume were obtained. Thorough OH- neutralization (from an initial pH 14 down to 6.3) was observed. Three broad zones of pore solutions were identified to categorize the dominant geochemical reactions: the silicate dissolution zone (pH>10), pH-neutralized zone (pH 10 to 6.5), and displaced native sediment pore water (pH 6.5 to 8). Elevated concentrations of Si, Fe, and K in plume fluids and their depleted concentrations in plume sediments reflected dissolution of primary minerals within the silicate dissolution zone. The very high Na concentrations in the waste solution resulted in rapid and complete cation exchange, reflected in high concentrations of Ca and Mg at the plume front. The plume-sediment profiles also showed deposition of hydrated solids and carbonates. Fair correspondence was obtained between these results and analyses of field borehole samples from a waste plume at the Hanford Site. Results of this study provide a well-defined framework for understanding waste plumes in the more complex field setting and for understanding geochemical factors controlling transport of contaminant species carried in waste solutions that leaked from single-shell storage tanks in the past.

  17. Geochemical evolution of highly alkaline and saline tank waste plumes during seepage through vadose zone sediments

    SciTech Connect (OSTI)

    Wan, Jiamin; Tokunaga, Tetsu K.; Larsen, Joern T.; Serne, R JEFFREY.

    2004-02-01T23:59:59.000Z

    Leakage of highly saline and alkaline radioactive waste from storage tanks into underlying sediments is a serious environmental problem at the Hanford Site in Washington State. This study focuses on geochemical evolution of tank waste plumes resulting from interactions between the waste solution and sediment. A synthetic tank waste solution was infused into unsaturated Hanford sediment columns (0.2, 0.6, and 2 m) maintained at 70C to simulate the field contamination process. Spatially and temporally resolved geochemical profiles of the waste plume were obtained. Thorough OH neutralization (from an initial pH 14 down to 6.3) was observed. Three broad zones of pore solutions were identified to categorize the dominant geochemical reactions: the silicate dissolution zone (pH > 10), pH-neutralized zone (pH 10 to 6.5), and displaced native sediment pore water (pH 6.5 to 8). Elevated concentrations of Si, Fe, and K in plume fluids and their depleted concentrations in plume sediments reflected dissolution of primary minerals within the silicate dissolution zone. The very high Na concentrations in the waste solution resulted in rapid and complete cation exchange, reflected in high concentrations of Ca and Mg at the plume front. The plume-sediment profiles also showed deposition of hydrated solids and carbonates. Fair correspondence was obtained between these results and analyses of field borehole samples from a waste plume at the Hanford Site. Results of this study provide a well-defined framework for understanding waste plumes in the more complex field setting and for understanding geochemical factors controlling transport of contaminant species carried in waste solutions that leaked from single-shell storage tanks in the past.

  18. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR: VERNON FIELD, ISABELLA COUNTY, MI.

    SciTech Connect (OSTI)

    James R. Wood; T.J. Bornhorst; William B. Harrison; W. Quinlan

    2002-04-01T23:59:59.000Z

    The fault study continues to find more faults and develop new techniques to visualize them. Data from the Dundee Formation has been used to document 11 major faults in the Michigan Basin which have now been verified using data from other horizons. These faults control the locations of many of the large anticlinal structures in the Michigan Basin and likely controlled fluid movements as well. The surface geochemistry program is also moving along well with emphasis on measuring samples collected last sampling season. The new GC laboratory is now functional and has been fully staffed as of December. The annual project review was held March 7-9 in Tampa, Florida. Contracts are being prepared for drilling the Bower's prospects in Isabella County, Michigan, this spring or summer. A request was made to extend the scope of the project to include the Willison Basin. A demonstration well has been suggested in Burke County, N. Dakota, following a review of 2D seismic and surface geochem. A 3D seismic survey is scheduled for the prospect.

  19. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR: VERNON FIELD, ISABELLA COUNTY, MI

    SciTech Connect (OSTI)

    James R. Wood; W. Quinlan

    2003-04-01T23:59:59.000Z

    The principal objective of the study was to test a new analytical technique, Solid-Phase Microextraction (SPME), for detecting trace amounts of light hydrocarbons in pore gases as a means of reducing risk in hydrocarbon exploration and production. This involved measuring the effectiveness of SPME to extract hydrocarbons under controlled conditions in the laboratory. As part of the study, a field demonstration was undertaken to assess the validity and usefulness of the laboratory results. Presented in this quarterly report is the condensed version of the Case History and Well Summary for the Bear Lake area in Manistee County, Michigan. The full version will be in the annual report. The condensed case history presents the important technical details regarding the geochemistry and horizontal lateral for Bear Lake, as well as the field demonstration results and the applicability of these results to other demonstration projects. This format could be duplicated for other demonstration projects and will be used on all subsequent field demonstrations as they near completion.

  20. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR: VERNON FIELD, ISABELLA COUNTY, MI

    SciTech Connect (OSTI)

    James R. Wood; W. Quinlan

    2003-01-01T23:59:59.000Z

    Presented in this quarterly report is the Case History and Well Summary for the Vernon Field demonstration project in Isabella County, Michigan. This new case history and well summary format organizes and presents the technical and historical details of the Vernon Field demonstration, as well as the field demonstration results and the applicability of these results to other demonstration projects. This format could be duplicated for other demonstration projects and will be used on all subsequent field demonstrations as they near completion. Planning for the annual project meeting in Tampa, Florida has begun. This meeting will be held March 7-9, 2003 at the same site as the last three meetings. The goals of this project were to: (1) test the use of multi-lateral wells to recover bypassed hydrocarbons and (2) to access the potential of using surface geochemistry to reduce drilling risk. Two new demonstration wells, the State-Smock and the Bowers 4-25, were drilled to test the Dundee Formation at Vernon Field for bypassed oil. Neither well was commercial, although both produced hydrocarbon shows. An extensive geochemical survey in the vicinity of Vernon Field, covering much of Isabella County, has produced a base map for interpretation of anomalies in Michigan. Several potential new anomalies were discovered that could be further investigated.

  1. Characterization of the geology, geochemistry, hydrology and microbiology of the in-situ air stripping demonstration site at the Savannah River Site

    SciTech Connect (OSTI)

    Eddy, C.A.; Looney, B.B.; Dougherty, J.M.; Hazen, T.C.; Kaback, D.S.

    1991-05-01T23:59:59.000Z

    The Savannah River Site is the location of an Integrated Demonstration Project designed to evaluate innovative remediation technologies for environmental restoration at sites contaminated with volatile organic contaminants. This demonstration utilizes directionally drilled horizontal wells to deliver gases and extract contaminants from the subsurface. Phase I of the Integrated Demonstration focused on the application and development of in-situ air stripping technologies to remediate soils and sediments above and below the water table as well as groundwater contaminated with volatile organic contaminants. The objective of this report is to provide baseline information on the geology, geochemistry, hydrology, and microbiology of the demonstration site prior to the test. The distribution of contaminants in soils and sediments in the saturated zone and groundwater is emphasized. These data will be combined with data collected after the demonstration in order to evaluate the effectiveness of in-situ air stripping. New technologies for environmental characterization that were evaluated include depth discrete groundwater sampling (HydroPunch) and three-dimensional modeling of contaminant data.

  2. Subtask 2.17 - CO{sub 2} Storage Efficiency in Deep Saline Formations

    SciTech Connect (OSTI)

    Gorecki, Charles; Liu, Guoxiang; Braunberger, Jason; Klenner, Robert; Ayash, Scott; Dotzenrod, Neil; Steadman, Edward; Harju, John

    2014-02-01T23:59:59.000Z

    As the field of carbon capture and storage (CCS) continues to advance, and large-scale implementation of geologic carbon dioxide (CO{sub 2}) storage progresses, it will be important to understand the potential of geologic formations to store meaningful amounts of CO{sub 2}. Geologic CO{sub 2} storage in deep saline formations (DSFs) has been suggested as one of the best potential methods for reducing anthropogenic CO{sub 2} emission to the atmosphere, and as such, updated storage resource estimation methods will continue to be an important component for the widespread deployment of CCS around the world. While there have been several methodologies suggested in the literature, most of these methods are based on a volumetric calculation of the pore volume of the DSF multiplied by a storage efficiency term and do not consider the effect of site-specific dynamic factors such as injection rate, injection pattern, timing of injection, pressure interference between injection locations, and overall formation pressure buildup. These volumetric methods may be excellent for comparing the potential between particular formations or basins, but they have not been validated through real-world experience or full-formation injection simulations. Several studies have also suggested that the dynamic components of geologic storage may play the most important role in storing CO{sub 2} in DSFs but until now have not directly compared CO{sub 2} storage resource estimates made with volumetric methodologies to estimates made using dynamic CO{sub 2} storage methodologies. In this study, two DSFs, in geographically separate areas with geologically diverse properties, were evaluated with both volumetric and dynamic CO{sub 2} storage resource estimation methodologies to compare the results and determine the applicability of both approaches. In the end, it was determined that the dynamic CO{sub 2} storage resource potential is timedependent and it asymptotically approaches the volumetric CO{sub 2} storage resource potential over very long periods of time in the two systems that were evaluated. These results indicate that the volumetric assessments can be used as long as the appropriate storage efficiency terms are used and it is understood that it will take many wells over very long periods of time to fully realize the storage potential of a target formation. This subtask was funded through the Energy & Environmental Research Center (EERC)– U.S. Department of Energy (DOE) Joint Program on Research and Development for Fossil Energy-Related Resources Cooperative Agreement No. DE-FC26-08NT43291. Nonfederal funding was provided by the IEA Greenhouse Gas R&D Programme.

  3. Kinetic model for predicting the concentrations of active halogens species in chlorinated saline cooling waters. Final report

    SciTech Connect (OSTI)

    Haag, W.R.; Lietzke, M.H.

    1981-08-01T23:59:59.000Z

    A kinetic model has been developed for describing the speciation of chlorine-produced oxidants in seawater as a function of time. The model is applicable under a broad variety of conditions, including all pH range, salinities, temperatures, ammonia concentrations, organic amine concentrations, and chlorine doses likely to be encountered during power plant cooling water chlorination. However, the effects of sunlight are not considered. The model can also be applied to freshwater and recirculating water systems with cooling towers. The results of the model agree with expectation, however, complete verification is not feasible at the present because analytical methods for some of the predicted species are lacking.

  4. Response of the Toxic Dinoflagellate Karenia brevis to Current and Projected Environmental Conditions: Salinity and Global Climate Change 

    E-Print Network [OSTI]

    Errera, Reagan Michelle

    2013-05-03T23:59:59.000Z

    for management and mitigation. Our current knowledge of K. brevis indicates that toxin concentrations depend on a variety of factors, including bloom age, clonal differences, salinity, and light (Roszell et al., 1990; Baden and Tomas, 1988; Loret et al., 2002...; Brown et al., 2006; Magana and Villareal, 2006; Lekan and Tomas, 2010). Bloom age does not affect toxin concentration per cell; rather 3 as K. brevis blooms age and enter a maturing stage PbTx-2 declines with a simultaneous increase in PbTx-3, a...

  5. Glaciation and saline-freshwater mixing as a possible cause of cave formation in the eastern midcontinent region of the United States: A conceptual model

    SciTech Connect (OSTI)

    Panno, S.V. (Illinois State Geological Survey, Champaign (USA)); Bourcier, W.L. (Lawrence Livermore National Lab., CA (USA))

    1990-08-01T23:59:59.000Z

    We present a hypothesis for the formation of caves and associated karst features near the southern margins of the Illinois, Michigan, and Appalachian basins. Spatial and temporal relations among intracratonic basins, karstic terrain, and continental glaciation suggest that Pleistocene glaciation may have initiated the discharge of saline waters from the margins of these basins. Glaciation-induced discharge of saline waters could result from the consolidation of sediments due to the overlying pressure of glacial ice, and flushing of underlying aquifers as a result of bottom melting in recharge areas of basic aquifers. The upward migration of basin-derived saline waters into near-surface aquifers would result in the mixing of saline waters with infiltrating glacial meltwater and meteoric water. The development of a vertically restricted zone of mixing of saline and fresh water in limestone aquifers would result in the dissolution of limestone; this mechanism could be responsible for the formation, or at least the initiation of, some caves and associated karst features in the midcontinent region.

  6. A GIS COST MODEL TO ASSESS THE AVAILABILITY OF FRESHWATER, SEAWATER, AND SALINE GROUNDWATER FOR ALGAL BIOFUEL PRODUCTION IN THE UNITED STATES

    SciTech Connect (OSTI)

    Venteris, Erik R.; Skaggs, Richard; Coleman, Andre M.; Wigmosta, Mark S.

    2013-03-15T23:59:59.000Z

    A key advantage of using microalgae for biofuel production is the ability of some algal strains to thrive in waters unsuitable for conventional crop irrigation such as saline groundwater or seawater. Nonetheless, the availability of sustainable water supplies will provide significant challenges for scale-up and development of algal biofuels. We conduct a limited techno-economic assessment based on the availability of freshwater, saline groundwater, and seawater for use in open pond algae cultivation systems. We explore water issues through GIS-based models of algae biofuel production, freshwater supply, and cost models for supplying seawater and saline groundwater. We estimate that combined, within the coterminous US these resources can support production on the order of 9.46E+7 m3 yr-1 (25 billion gallons yr-1) of renewable biodiesel. Achievement of larger targets requires the utilization of less water efficient sites and relatively expensive saline waters. Geographically, water availability is most favorable for the coast of the Gulf of Mexico and Florida peninsula, where evaporation relative to precipitation is moderate and various saline waters are economically available. As a whole, barren and scrub lands of the southwestern US have limited freshwater supplies so accurate assessment of alternative waters is critical.

  7. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR: VERNON FIELD, ISABELLA COUNTRY, MI

    SciTech Connect (OSTI)

    James R. Wood; A. Wylie; W. Quinlan

    2004-04-01T23:59:59.000Z

    The principal objective of this demonstration project is to test surface geochemical techniques for detecting trace amounts of light hydrocarbons in pore gases as a means of reducing risk in hydrocarbon exploration and production. A major part of the remaining project will focus on using surface geochemistry to delineate prospects. A Niagaran reef field geochemical survey, the Bagley Prospect area in Otsego County, Michigan is scheduled to take place this summer. Previous wells drilled in Bagley Prospect area in the early 1970's and in place in late 2002 and early 2003 resulted in discoveries and numerous hydrocarbon shows in the Brown Niagaran reservoir interval. The Bagley region is still considered an area of interest by the industry and appears ripe for a geochemical survey. Our industry partner is interested in a possible test in the Bagley prospect because subsurface geophysical and geological interpretation indicates the presence of structures. Anomalous production and pressure data further suggest the region is not yet well understood and should not be considered mature. The most recent well, the Bagley 1-22A sidetrack, was unsuccessful at locating a new reef culmination to the south of the original vertical well and did not encounter hydrocarbon shows. The sidetrack and well were plugged and abandoned. The proposed geochemical survey will concentrate on areas away from the Bagley 1-22A to the north and west but will include the entire prospect so that the existing data can be used in interpretations. Bagley appears to offer a unique combination of potential and data for a geochemical study that focuses on looking for new oil in an area that has exhausted traditional geologic and geophysical methods. The Bear Lake pinnacle reef trend in Manistee County, Michigan, is also scheduled for further geochemical work this summer. Industry interest, mostly by small companies, is picking up in this area and it is also ripe for targeted geochemical surveys for the same reasons cited above.

  8. Geochemistry of U and Th and its Influence on the Origin and Evolution of the Crust of Earth and the Biological Evolution

    E-Print Network [OSTI]

    Xuezhao Bao; Ali Zhang

    2007-10-16T23:59:59.000Z

    We have investigated the migration behaviors of uranium (U) and thorium (Th) in Earth and other terrestrial planets. Theoretical models of U and Th migration have been proposed. These models suggest that the unique features of Earth are closely connected with its unique U and Th migration models and distribution patterns. In the Earth, U and Th can combine with oxidative volatile components and water, migrate up to the asthenosphere position to form an enrichment zone (EZ) of U and Th first, and then migrate up further to the crusts through magmatism and metamorphism. We emphasize that the formation of an EZ of U, Th and other heat-producing elements is a prerequisite for the formation of a plate tectonic system. The heat-producing elements, currently mainly U and Th, in the EZ are also the energy sources that drive the formation and evolution of the crust of Earth and create special granitic continental crusts. In other terrestrial planets, including Mercury, Venus, and Mars, an EZ can not be formed because of a lack of oxidative volatile components and water. For this reason, a plate tectonic system can not been developed in these planets. We also emphasize the influence of U and Th in EZ on the development and evolution of life on Earth. We propose that since the Earth and planets were born in a united solar system, there should be some common mechanisms to create the similarities and differences between them. We have tried to develop an integrated view to explain some problems in the tectonics of Earth and evolution, bio-evolution, and planetary dynamics through U and Th geochemistry. We believe that a comprehensive exploration on energy sources and their evolution is a good way to build bridges between different disciplines of science in order to better understand the Earth and planets.

  9. USING RECENT ADVANCES IN 2D SEISMIC TECHNOLOGY AND SURFACE GEOCHEMISTRY TO ECONOMICALLY REDEVELOP A SHALLOW SHELF CARBONATE RESERVOIR: VERNON FIELD, ISABELLA COUNTY, MI.

    SciTech Connect (OSTI)

    James R. Wood; T.J. Bornhorst; S.D. Chittichk; William B. Harrison; W. Quinlan

    2001-01-01T23:59:59.000Z

    The geochemical sampling team collected additional 148 samples at Vernon Field along 5 new traverses. Most of the locations were sampled for three types of analyses: microbial, iodine and enzyme leach; no results from the second batch of samples were available in time for this report. In addition to the sampling, a study was begun on the feasibility of collecting and analyzing hydrocarbon gases (C1-C8) directly. Although several companies offer these services, the cost ($200-300/sample w/o sampling fee) is high, on par with the cost of a 3D seismic survey, and may not include the raw data. However direct sampling of reservoir gases collecting in the soil appear to offer the best approach and should be included in this study. It would probably work well at Vernon Field. It may be possible to lower costs considerably; initial estimates of $20/sample for GCMS (Gas Chromatography--mass spectrometry) analysis are attractive and might induce to Michigan producers to include soil surveys in their routine field work-ups. A complete set of digital data was assembled for Vernon Field and nearby locations. The set consists of well locations, formation top picks, lithologies and scanned images of driller's reports and scout tickets. Well logs are still being located. The annual meeting for the Class Revisit work group is tentatively scheduled for the week of March 1-7 in Tampa, Fl. By that time all of the geochemical data will be available and final decisions regarding drilling can be made.

  10. The Effects of Dry Density and Pore-water Salinity on the Physical and Microbiological Characteristics of Compacted 100% Bentonite

    SciTech Connect (OSTI)

    Stroes-Gascoyne, S.; Hamon, C.J.; Dixon, D.A.; Kohle, C.L. [Atomic Energy of Canada Limited, Whiteshell Laboratories, Pinawa, MB, R0E 1L0 (Canada); Maak, P. [Ontario Power Generation, 700 University Avenue, Toronto ON, M5G 1X6 (Canada)

    2007-07-01T23:59:59.000Z

    This study examined the conditions required to suppress microbial activity in compacted bentonite, such that microbially influenced corrosion (MIC) of copper waste containers, surrounded by compacted bentonite in a future deep geologic repository, would become insignificant. Experiments were carried out to determine the effects of dry density and pore-water salinity on swelling pressure, water activity (a{sub w}) and the culturable microbial community in compacted bentonite. A dry density {>=} 1.6 g/cm{sup 3} ensures that a{sub w} is < 0.96 and the swelling pressure > 2 MPa. Both conditions suppress microbial culturability below background levels (2.1 x 10{sup 2} Colony-Forming Units/g) in as-purchased bentonite. Under such conditions, cells likely survive as dormant cells or inactive spores, which greatly reduces the possibility of significant MIC. Observations in natural clay-rich environments support these findings. (authors)

  11. Corrosion protection of Arctic offshore structures: Final report. [Effects of temperature and salinity on required cathodic protection current

    SciTech Connect (OSTI)

    Sackinger, W.M.; Rogers, J.C.; Feyk, C.; Theuveny, B.

    1985-10-01T23:59:59.000Z

    Results are presented for a research program on corrosion prevention for Arctic offshore structures which are in contact with sea ice for a significant portion of the year. The electrical method most adaptable for structure protection involves the injection of impressed current from several remote anodes buried just beneath the sea floor. The electrical resistivity of annual sea ice as a function of temperature and salinity is presented. Details of the interface layers formed between sea ice and steel in the presence of current injection are shown. A computer program was developed to enable the calculation of protective current density into the structure, in the presence of ice rubble and ridges around the structure. The program and the results of an example calculation are given for a caisson- retained island structure. 81 refs., 103 figs., 3 tabs.

  12. Large-scale impact of CO2 storage in deep saline aquifers: A sensitivity study on pressure response in stratified systems

    E-Print Network [OSTI]

    Zhou, Quanlin

    Large-scale impact of CO2 storage in deep saline aquifers: A sensitivity study on pressure response storage potential of all the geological CO2 storage options and are widely distributed throughout the globe in all sedimentary basins.ForCO2 storage tohaveasignificantimpact on atmospheric levels

  13. CASTAt'ffiA 62(2): 112-118. J1JNE 1997 Plant Diversity Along a Salinity Gradient of Four

    E-Print Network [OSTI]

    Newman, Michael C.

    of the Patuxent River (Anderson et al. ~968), York River (Wass and Wright 1969), and James River (Atkinson et al was measured in four tidal marshes on the York and Pamunkey Rivers, Virginia. Each marsh represented and freshwater salinity gradient on the Mattaponi River, Virginia. However, these studies did not measure

  14. Well injectivity during CO2storage operations in deep saline aquifers 6 Part 2: Numerical simulations of drying, salt deposit mechanisms and role of7

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    1 1 2 3 4 5 Well injectivity during CO2storage operations in deep saline aquifers ­6 Part 2 or industrial units and stored in underground geological reservoirs.30 Return on experience withCO2 injection-well field scale is proposed. This approach is of major40 importance because it makes it possible

  15. New Mexico Water Resources Research Institute, New Mexico State University http://wrri.nmsu.edu Utilization of Saline and Other Impaired Waters for

    E-Print Network [OSTI]

    Johnson, Eric E.

    used for turf irrigation and increase the efficiency of irrigation systems in turf areas. The study irrigation systems on changes in soil chemical properties at several depths in the turfgrass root zone://wrri.nmsu.edu Utilization of Saline and Other Impaired Waters for Turfgrass Irrigation Bernd Leinauer, Extension Plant

  16. CO2 Saline Storage Demonstration in Colorado Sedimentary Basins: Applied Studies in Reservoir Assessment and Dynamic Processes Affecting Industrial Operations

    SciTech Connect (OSTI)

    Nummedal, Dag; Sitchler, Alexis; McCray, John; Mouzakis, Katherine; Glossner, Andy; Mandernack, Kevin; Gutierrez, Marte; Doran, Kevin; Pranter, Matthew; Rybowiak, Chris

    2012-09-30T23:59:59.000Z

    This multitask research project was conducted in anticipation of a possible future increase in industrial efforts at CO2 storage in Colorado sedimentary basins. Colorado is already the home to the oldest Rocky Mountain CO2 storage site, the Rangely Oil Field, where CO2-EOR has been underway since the 1980s. The Colorado Geological Survey has evaluated storage options statewide, and as part of the SW Carbon Sequestration Partnership the Survey, is deeply engaged in and committed to suitable underground CO2 storage. As a more sustainable energy industry is becoming a global priority, it is imperative to explore the range of technical options available to reduce emissions from fossil fuels. One such option is to store at least some emitted CO2 underground. In this NETL-sponsored CO2 sequestration project, the Colorado School of Mines and our partners at the University of Colorado have focused on a set of the major fundamental science and engineering issues surrounding geomechanics, mineralogy, geochemistry and reservoir architecture of possible CO2 storage sites (not limited to Colorado). Those are the central themes of this final report and reported below in Tasks 2, 3, 4, and 6. Closely related to these reservoir geoscience issues are also legal, environmental and public acceptance concerns about pore space accessibility—as a precondition for CO2 storage. These are addressed in Tasks 1, 5 and 7. Some debates about the future course of the energy industry can become acrimonius. It is true that the physics of combustion of hydrocarbons makes it impossible for fossil energy to attain a carbon footprint anywhere nearly as low as that of renewables. However, there are many offsetting benefits, not the least that fossil energy is still plentiful, it has a global and highly advanced distribution system in place, and the footprint that the fossil energy infrastructure occupies is orders of magnitude smaller than renewable energy facilities with equivalent energy capacity. Finally, inexpensive natural gas here in North America is pushing coal for electricity generation off the market, thus reducing US CO2 emissions faster than any other large industrialized nation. These two big factors argue for renewed efforts to find technology solutions to reduce the carbon footprint (carbon dioxide as well as methane and trace gases) of conventional and unconventional oil and gas. One major such technology component is likely to be carbon capture, utilization and storage.

  17. Training Students to Analyze Spatial and Temporal Heterogeneities in Reservoir and Seal Petrology, Mineralogy, and Geochemistry: Implications for CO{sub 2} Sequestration Prediction, Simulation, and Monitoring

    SciTech Connect (OSTI)

    Bowen, Brenda

    2013-09-30T23:59:59.000Z

    The objective of this project was to expose and train multiple students in geological tools that are essential to reservoir characterization and geologic sequestration including but not limited to advanced petrological methods, mineralogical methods, and geochemical methods; core analysis, and geophysical well-log interpretation. These efforts have included training of multiple students through geologically based curriculum and research using advanced petrological, mineralogical, and geochemical methods. In whole, over the last 3+ years, this award has supported 5,828 hours of student research, supporting the work of several graduate and undergraduate students. They have all received training directly related to ongoing CO{sub 2} sequestration demonstrations. The students have all conducted original scientific research on topics related to understanding the importance of lithological, textural, and compositional variability in formations that are being targeted as CO{sub 2} sequestration reservoirs and seals. This research was linked to the Mount Simon Sandstone reservoir and overlying Eau Claire Formation seal in the Illinois Basin- a system where over one million tons of CO{sub 2} are actively being injected with the first large-scale demonstration of anthropogenic CO{sub 2} storage in the U.S. Student projects focused specifically on 1) reservoir porosity characterization and evaluation, 2) petrographic, mineralogical, and geochemical evidence of fluid-related diagenesis in the caprock, 3) textural changes in reservoir samples exposed to experimental CO{sub 2} + brine conditions, 4) controls on spatial heterogeneity in composition and texture in both the reservoir and seal, 5) the implications of small-scale fractures within the reservoir, and 6) petrographic and stable isotope analyses of carbonates in the seal to understand the burial history of the system. The student-led research associated with this project provided real-time and hands-on experience with a relevant CO{sub 2} system, provided relevant information to the regional partnerships who are working within these formations, and provides more broadly applicable understanding and method development for other carbon capture and storage systems.

  18. Stratigraphic Relations and Lithologic Variations in the Jemez...

    Open Energy Info (EERE)

    rhyolite volcanism from >13 to 6 Ma, (3) hypabyssal and volcanic rocks of the Cochiti mining district probably represent the exhumed interior of a Keres Group volcano(s), (4)...

  19. The determination of lithology from core physical properties measurements

    E-Print Network [OSTI]

    Clark, Paula Ann

    2006-08-16T23:59:59.000Z

    (10 -6 SI) ? (10 -8 m 3 /kg) Iron-bearing minerals Biotite 1,500 to 2,900 5 to 52 to 95 to 98 Orthopyroxene, olivines, amphiboles 1,500 to 1,800 1 to 43 to 50 to 130 iron a 3,900,000 50,000 to 2,000,000 Iron sulfides Pyrite 35-5,000 11...

  20. Lithology and Alteration Mineralogy of Reservoir Rocks at Coso...

    Open Energy Info (EERE)

    of the upwelling plume were investigated using petrographic and analytical analyses of reservoir rock and vein material. The nature of the low-angle outflow zone and the...

  1. Lithology and alteration mineralogy of reservoir rocks at Coso...

    Open Energy Info (EERE)

    of the upwelling plume were investigated using petrographic and analytical analyses of reservoir rock and vein material. The nature of the low-angle outflow zone and the...

  2. Lithologic Descriptions and Temperature Profiles of Five Wells in the

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere I Geothermal Pwer Plant Jump to:Landowners and WindLightingLinthicum, Maryland:source HistoryLite Trough

  3. Lithologic Descriptions and Temperature Profiles of Five Wells...

    Open Energy Info (EERE)

    and temperature profiles of the southern and western Valles caldera region have been well constrained with the use of data from the VC-1, AET-4, WC 23-4, PC-1, and PC-2 wells....

  4. Property:CapRockLithology | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to: navigation,PillarPublicationType Jump to: navigation, search This isCapRockAge Jump

  5. Property:HostRockLithology | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to:Ezfeedflag Jump to: navigation,ProjectStartDate Jump to:Property Edit withpurpose

  6. Lithology and Alteration Mineralogy of Reservoir Rocks at Coso Geothermal

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to: navigation, searchOf KilaueaInformation Other AlternativePark, Arizona:Lithium

  7. Lithology and alteration mineralogy of reservoir rocks at Coso Geothermal

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to: navigation, searchOf KilaueaInformation Other AlternativePark, Arizona:LithiumArea,

  8. Stratigraphic Relations and Lithologic Variations in the Jemez Volcanic

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere IRaghuraji Agro Industries Pvt LtdShawangunk,SoutheastSt.SteepStimulationStoneacreStow,AnalysisMexico |Field,

  9. Core Lithology State of Hawaii Scientific Observation Hole 4 Kilauea

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand JumpConceptual Model, clickInformationNew|Core Analysis At Geysers| Open EnergyAl., 1987)

  10. Core Lithology State of Hawail Scientific Observation Hole 2 Kilauea

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand JumpConceptual Model, clickInformationNew|Core Analysis At Geysers| Open EnergyAl., 1987)Volcano,

  11. Geology, hydrothermal petrology, stable isotope geochemistry, and fluid inclusion geothermometry of LASL geothermal test well C/T-1 (Mesa 31-1), East Mesa, Imperial Valley, California, USA

    SciTech Connect (OSTI)

    Miller, K.R.; Elders, W.A.

    1980-08-01T23:59:59.000Z

    Borehole Mesa 31-1 (LASL C/T-1) is an 1899-m (6231-ft) deep well located in the northwestern part of the East Mesa Geothermal Field. Mesa 31-1 is the first Calibration/Test Well (C/T-1) in the Los Alamos Scientific Laboratory (LASL), Geothermal Log Interpretation Program. The purpose of this study is to provide a compilation of drillhole data, drill cuttings, well lithology, and formation petrology that will serve to support the use of well LASL C/T-1 as a calibration/test well for geothermal logging. In addition, reviews of fluid chemistry, stable isotope studies, isotopic and fluid inclusion geothermometry, and the temperature log data are presented. This study provides the basic data on the geology and hydrothermal alteration of the rocks in LASL C/T-1 as background for the interpretation of wireline logs.

  12. Sandia National Laboratories: Molecular Geochemistry

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

    of aqueous uranyl carbonate interacting with the basal surface of sodium montmorillonite. Free energy profiles for cation adsorption to gibbsite surface calculated from molecular...

  13. Frontiers in Geochemistry Seminar Series

    E-Print Network [OSTI]

    and local water structure. More info: Dr. Kevin Rosso, 371-6357 Wednesday February 15, 2012 ETB Columbia

  14. Light and electron microscopic studies of the nanobenthic diatom, Nitzschia ovalis Arnott, Section Lanceolatae, as compared to related forms, and the effect of temperature and salinity on its growth rate

    E-Print Network [OSTI]

    Medlin, Linda Karen

    1977-01-01T23:59:59.000Z

    Selection and Maintenance of Diatoms to be Studied . 13 Preparation of Glassware and Culture Media. Preparation and Examination of Cells. Determination of Temperature and Salinity Tolerances and Optima for the growth of Nitzschia ovalis Arnott RESULTS... Light Microscopy. Electron Microscopy Salinity and Temperature Tolerances and Optima. DISCUSSION. Morphological Studies Physiological Studies SUMMARy LITERATURE. APPENDIX A. VITA. 15 18 20 24 24 46 110 124 124 131 139 141 149 BIST...

  15. The effects of Biozyme on the germination and emergence of bean (Phaseolus vulgaris L.) and sweet corn (Zea mays L.) seeds under suboptimal temperatures, pesticide overdose, and salinity stress 

    E-Print Network [OSTI]

    Campos Cruz, Armando

    1994-01-01T23:59:59.000Z

    THE EFFECTS OF BIOZYME? ON THE GERMINATION AND EMERGENCE OF BEAN (Phaseolus vulgaris L) AND SWEET CORN (Zea mays L. ) SEEDS UNDER SUBOPTIMAL TEMPERATURES, PESTICIDE OVERDOSE, AND SALINITY STRESS A Thesis by ARMANDO CAMPOS CRUZ Submitted... vulgaris L) AND SWEET CORN (Zea mays I ) SEEDS UNDER SUBOPTIMAL TEMPERATURES, PESTICIDE OVERDOSE, AND SALINITY STRESS A Thesis by ARMANDO CAMPOS CRUZ Submitted to Texas A&M University in partial fulfillment of the requirements for the degree...

  16. A method for quick assessment of CO2 storage capacity in closedand semi-closed saline formations

    SciTech Connect (OSTI)

    Zhou, Q.; Birkholzer, J.; Tsang, C.F.; Rutqvist, J.

    2008-02-10T23:59:59.000Z

    Saline aquifers of high permeability bounded by overlying/underlying seals may be surrounded laterally by low-permeability zones, possibly caused by natural heterogeneity and/or faulting. Carbon dioxide (CO{sub 2}) injection into and storage in such 'closed' systems with impervious seals, or 'semi-closed' systems with nonideal (low-permeability) seals, is different from that in 'open' systems, from which the displaced brine can easily escape laterally. In closed or semi-closed systems, the pressure buildup caused by continuous industrial-scale CO{sub 2} injection may have a limiting effect on CO{sub 2} storage capacity, because geomechanical damage caused by overpressure needs to be avoided. In this research, a simple analytical method was developed for the quick assessment of the CO{sub 2} storage capacity in such closed and semi-closed systems. This quick-assessment method is based on the fact that native brine (of an equivalent volume) displaced by the cumulative injected CO{sub 2} occupies additional pore volume within the storage formation and the seals, provided by pore and brine compressibility in response to pressure buildup. With nonideal seals, brine may also leak through the seals into overlying/underlying formations. The quick-assessment method calculates these brine displacement contributions in response to an estimated average pressure buildup in the storage reservoir. The CO{sub 2} storage capacity and the transient domain-averaged pressure buildup estimated through the quick-assessment method were compared with the 'true' values obtained using detailed numerical simulations of CO{sub 2} and brine transport in a two-dimensional radial system. The good agreement indicates that the proposed method can produce reasonable approximations for storage-formation-seal systems of various geometric and hydrogeological properties.

  17. Modeling of fate and transport of co-injection of H2S with CO2 in deep saline formations

    SciTech Connect (OSTI)

    Zhang, W.; Xu, T.; Li, Y.

    2010-12-15T23:59:59.000Z

    The geological storage of CO{sub 2} in deep saline formations is increasing seen as a viable strategy to reduce the release of greenhouse gases into the atmosphere. However, costs of capture and compression of CO{sub 2} from industrial waste streams containing small quantities of sulfur and nitrogen compounds such as SO{sub 2}, H{sub 2}S and N{sub 2} are very expensive. Therefore, studies on the co-injection of CO{sub 2} containing other acid gases from industrial emissions are very important. In this paper, numerical simulations were performed to study the co-injection of H{sub 2}S with CO{sub 2} in sandstone and carbonate formations. Results indicate that the preferential dissolution of H{sub 2}S gas (compared with CO{sub 2} gas) into formation water results in the delayed breakthrough of H{sub 2}S gas. Co-injection of H{sub 2}S results in the precipitation of pyrite through interactions between the dissolved H{sub 2}S and Fe{sup 2+} from the dissolution of Fe-bearing minerals. Additional injection of H{sub 2}S reduces the capabilities for solubility and mineral trappings of CO{sub 2} compared to the CO{sub 2} only case. In comparison to the sandstone (siliciclastic) formation, the carbonate formation is less favorable to the mineral sequestration of CO{sub 2}. Different from CO{sub 2} mineral trapping, the presence of Fe-bearing siliciclastic and/or carbonate is more favorable to the H{sub 2}S mineral trapping.

  18. Managing Soil Salinity

    E-Print Network [OSTI]

    Provin, Tony; Pitt, John L.

    2001-07-13T23:59:59.000Z

    helps the water move downward through the soil. While deep tillage will help temporarily, the parts of the soil not permanently broken up may reseal. Leaching: Leaching can be used to reduce the salts in soils. You must add enough low-salt water...

  19. Managing Soil Salinity 

    E-Print Network [OSTI]

    Provin, Tony; Pitt, John L.

    2001-07-13T23:59:59.000Z

    both surface water and groundwater often are a combina- tion of sodium, calcium, potassium, magnesium, chlo- rides, nitrates, sulfates, bicarbonates and carbonates (Table 1). These salts often originate from the earth?s crust. They also can result from... Magnesium sulfate MgSO 4 Gypsum Calcium sulfate CaSO 4 2H 2 O Street salt Calcium chloride CaCl 2 2H 2 O Muriate of potash Potassium chloride KCl Muriate of sulfate Potassium sulfate K2SO 4 seen. Fortunately, plants take up many salts in the form...

  20. Numerical Modeling Studies of The Dissolution-Diffusion-Convection ProcessDuring CO2 Storage in Saline Aquifers

    SciTech Connect (OSTI)

    Pruess, Karsten; Zhang, Keni

    2008-11-17T23:59:59.000Z

    For purposes of geologic storage, CO2 would be injected into saline formations at supercritical temperature and pressure conditions, and would form a separate phase that is immiscible with the aqueous phase (brine). At typical subsurface temperature and pressure conditions, supercritical CO2 (scCO2) has lower density than the aqueous phase and would experience an upward buoyancy force. Accordingly, the CO2 is expected to accumulate beneath the caprock at the top of the permeable interval, and could escape from the storage formation wherever (sub-)vertical pathways are available, such as fractures or faults through the caprock, or improperly abandoned wells. Over time, an increasing fraction of CO2 may dissolve in the aqueous phase, and eventually some of the aqueous CO2 may react with rock minerals to form poorly soluble carbonates. Dissolution into the aqueous phase and eventual sequestration as carbonates are highly desirable processes as they would increase permanence and security of storage. Dissolution of CO2 will establish phase equilibrium locally between the overlying CO2 plume and the aqueous phase beneath. If the aqueous phase were immobile, CO2 dissolution would be limited by the rate at which molecular diffusion can remove dissolved CO2 from the interface between CO2-rich and aqueous phases. This is a slow process. However, dissolution of CO2 is accompanied by a small increase in the density of the aqueous phase, creating a negative buoyancy force that can give rise to downward convection of CO2-rich brine, which in turn can greatly accelerate CO2 dissolution. This study explores the process of dissolution-diffusion-convection (DDC), using high-resolution numerical simulation. We find that geometric features of convection patterns are very sensitive to small changes in problem specifications, reflecting self-enhancing feedbacks and the chaotic nature of the process. Total CO2 dissolution rates on the other hand are found to be quite robust against modest changes in problem parameters, and are essentially constant as long as no dissolved CO2 reaches the lower boundary of the system.

  1. A finite difference model describing the dynamic effects of horizontal salinity gradients on the mean circulation of a shallow rectangular basin

    E-Print Network [OSTI]

    Elliott, Brady Allen

    1973-01-01T23:59:59.000Z

    is the bar-built estuary. It is formed by the development of an offshore barrier beach partly or wholly en- closing a sound. It has large horizontal dimensions and very shallow depths. There are usually several sources of freshwater inflow along... terms dominate the secondary effects. If its value is greater than one then the salinity (density) effects dominate. As examples he stated that in the Thames (D = . 8) the non-linear convective terms A would dominate, whereas in the Hersey estuary (D...

  2. Factors influencing the growth, recruitment success, and distribution of Farfantepenaeus aztecus (Crustacea:Penaeidae) in high and low salinity salt marshes

    E-Print Network [OSTI]

    Aubele, Michael Charles

    2001-01-01T23:59:59.000Z

    and sampling dates. Regression analyses were calculated to determine possible relationships between brown shrimp density and selected abiotic and biotic parameters. For all tests, density data were log transformed to achieve homogeneity of variances...), and dissolved oxygen (mg/I) in West Bay in 1996 and 1997. Temperature Salinity Dissolved Oxygen Date min. max. min. max. min. max. 9 Apr96 22 Apr 96 17 May 96 30 May 96 13 Jun 96 18 Jul 96 29 Aug 96 22 Sep 96 17 Oct 96 20&22 Nov 96 13 Feb 97 27 Feb...

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

    SciTech Connect (OSTI)

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

    2013-03-01T23:59:59.000Z

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

  4. 0361-0128/01/3361/933-22 $6.00 933 Introduction

    E-Print Network [OSTI]

    Banks, David

    -Pb deposits of Mississippi Valley type is thought to be related to brine mi- gration within sedimentary basins that generation and circu- lation of the ore-forming brines in the Maestrat basin took Geochemistry of the Fluids by the mixing of two distinct fluids: fluid A, a high salinity brine, with salinity greater than 26 wt percent

  5. Use of environmental sensors and sensor networks to develop water and salinity budgets for seasonal wetland real-time water quality management

    SciTech Connect (OSTI)

    Quinn, N.W.T.; Ortega, R.; Rahilly, P.J.A,; Royer, C.W.

    2009-10-01T23:59:59.000Z

    Successful management of river salt loads in complex and highly regulated river basins such as the San Joaquin of California presents significant challenges to Information Technology. Models are used as means of simulating major hydrologic processes in the basin which affect water quality and can be useful as tools for organizing basin information in a structured and readily accessible manner. Models can also be used to extrapolate the results of system monitoring since it is impossible to collect data for every point and non-point source of a pollutant in the Basin. Fundamental to every model is the concept of mass balance. This paper describes the use of state-of-the-art sensor technologies deployed in concert to obtain the first water and salinity budgets for a 60,000 hectare tract of seasonally managed wetlands in the San Joaquin Basin of California.

  6. Monitoring CO 2 sequestration into deep saline aquifer and associated salt intrusion using coupled multiphase flow modeling and time lapse electrical resistivity tomography

    SciTech Connect (OSTI)

    Chuan Lu; CHI Zhang; Hai Hanag; Timothy C. Johnson

    2014-04-01T23:59:59.000Z

    Successful geological storage and sequestration of carbon dioxide (CO2) require efficient monitoring of the migration of CO2 plume during and after large-scale injection in order to verify the containment of the injected CO2 within the target formation and to evaluate potential leakage risk. Field studies have shown that surface and cross-borehole electrical resistivity tomography (ERT) can be a useful tool in imaging and characterizing solute transport in heterogeneous subsurface. In this synthetic study, we have coupled a 3-D multiphase flow model with a parallel 3-D time-lapse ERT inversion code to explore the feasibility of using time-lapse ERT for simultaneously monitoring the migration of CO2 plume in deep saline formation and potential brine intrusion into shallow fresh water aquifer. Direct comparisons of the inverted CO2 plumes resulting from ERT with multiphase flow simulation results indicate the ERT could be used to delineate the migration of CO2 plume. Detailed comparisons on the locations, sizes and shapes of CO2 plume and intruded brine plumes suggest that ERT inversion tends to underestimate the area review of the CO2 plume, but overestimate the thickness and total volume of the CO2 plume. The total volume of intruded brine plumes is overestimated as well. However, all discrepancies remain within reasonable ranges. Our study suggests that time-lapse ERT is a useful monitoring tool in characterizing the movement of injected CO2 into deep saline aquifer and detecting potential brine intrusion under large-scale field injection conditions.

  7. Long-term Variations of CO2 Trapped in Different Mechanisms in Deep Saline Formations: A Case Study of the Songliao Basin, China

    SciTech Connect (OSTI)

    Zhang, Wei; Li, Yilian; Xu, Tianfu; Cheng, Huilin; Zheng, Yan; Xiong, Peng

    2008-06-10T23:59:59.000Z

    The geological storage of CO{sub 2} in deep saline formations is increasing seen as a viable strategy to reduce the release of greenhouse gases to the atmosphere. There are numerous sedimentary basins in China, in which a number of suitable CO{sub 2} geologic reservoirs are potentially available. To identify the multi-phase processes, geochemical changes and mineral alteration, and CO{sub 2} trapping mechanisms after CO{sub 2} injection, reactive geochemical transport simulations using a simple 2D model were performed. Mineralogical composition and water chemistry from a deep saline formation of Songliao Basin were used. Results indicate that different storage forms of CO{sub 2} vary with time. In the CO{sub 2} injection period, a large amount of CO{sub 2} remains as a free supercritical phase (gas trapping), and the amount dissolved in the formation water (solubility trapping) gradually increases. Later, gas trapping decreases, solubility trapping increases significantly due to migration and diffusion of the CO{sub 2} plume, and the amount trapped by carbonate minerals increases gradually with time. The residual CO{sub 2} gas keeps dissolving into groundwater and precipitating carbonate minerals. For the Songliao Basin sandstone, variations in the reaction rate and abundance of chlorite, and plagioclase composition affect significantly the estimates of mineral alteration and CO{sub 2} storage in different trapping mechanisms. The effect of vertical permeability and residual gas saturation on the overall storage is smaller compared to the geochemical factors. However, they can affect the spatial distribution of the injected CO{sub 2} in the formations. The CO{sub 2} mineral trapping capacity could be in the order of ten kilogram per cubic meter medium for the Songliao Basin sandstone, and may be higher depending on the composition of primary aluminosilicate minerals especially the content of Ca, Mg, and Fe.

  8. The effects of Biozyme on the germination and emergence of bean (Phaseolus vulgaris L.) and sweet corn (Zea mays L.) seeds under suboptimal temperatures, pesticide overdose, and salinity stress

    E-Print Network [OSTI]

    Campos Cruz, Armando

    1994-01-01T23:59:59.000Z

    of Biozyme on the Germination and Emergence of Bean (Phaseolus vulgaris L ) and Sweet Corn (Zea mays L. ) Seeds Under Suboptimal Temperatures, Pesticide Overdose, and Salinity Stress. (May 1994) Armando Campos Cruz, B S. , Instituto Tecnologico y de... thanks go to Grupo Bioquimico Mexicano S. A. de C. V. , for their financial assistance and support of my research project without which this work could not have been completed, and to the Department of Horticultural Sciences of Texas A&M University...

  9. Biomass production, forage quality, and cation uptake of Quail bush, four-wing saltbush, and seaside barley irrigated with moderately saline-sodic water

    SciTech Connect (OSTI)

    Bauder, J.W.; Browning, L.S.; Phelps, S.D.; Kirkpatrick, A.D. [Montana State University, Bozeman, MT (United States)

    2008-07-01T23:59:59.000Z

    The study reported here investigated capacity of Atriplex lentiformis (Torr.) S. Wats. (Quail bush), Atriplex X aptera A. Nels. (pro sp.) (Wytana four-wing saltbush), and Hordeum marinum Huds. (seaside barley) to produce biomass and crude protein and take up cations when irrigated with moderately saline-sodic water, in the presence of a shallow water table. Water tables were established at 0.38, 0.76, and 1.14m below the surface in sand-filled columns. The columns were then planted to the study species. Study plants were irrigated for 224 days; irrigation water was supplied every 7 days equal to water lost to evapotranspiration (ET) plus 100mL (the volume of water removed in the most previous soil solution sampling). Water representing one of two irrigation sources was used: Powder River (PR) or coalbed natural gas (CBNG) wastewater. Biomass production did not differ significantly between water quality treatments but did differ significantly among species and water table depth within species. Averaged across water quality treatments, Hordeum marinum produced 79% more biomass than A. lentiformis and 122% more biomass than Atriplex X aptera, but contained only 11% crude protein compared to 16% crude protein in A. lentiformis and 14% crude protein in Atriplex X aptera. Atriplex spp. grown in columns with the water table at 0.38m depth produced more biomass, took up less calcium on a percentage basis, and took up more sodium on a percentage basis than when grown with the water table at a deeper depth. Uptake of cations by Atriplex lentiformis was approximately twice the uptake of cations by Atriplex X aptera and three times that of H. marinum. After 224 days of irrigation, crop growth, and cation uptake, followed by biomass harvest, EC and SAR of shallow groundwater in columns planted to A. lentiformis were less than EC and SAR of shallow ground water in columns planted to either of the other species.

  10. Mineralogy and geochemistry of recent carbonate sediments

    E-Print Network [OSTI]

    Sommer, Sheldon E

    1964-01-01T23:59:59.000Z

    -calcite). A large loss of certain trace elements (e. g. magnesium, strontium and barium) occurs during diagenesis (Stehli and Hower, 1961), Aragonite formed at or near the surface of the earth is metastable relative to calcite. The free energy difference...-calciMs. Clearly then, Sr/Ca and Mg/Ca ratios, when used in conjunction with a knowledge of carbonate mineralogy, can act as diagenetic indicators (Pilkey and Hower, 1960). Magnesium released in the conversion of high Mg- to low Mg- calcites, as well...

  11. MARK E. CONRAD Center for Isotope Geochemistry

    E-Print Network [OSTI]

    Ajo-Franklin, Jonathan

    with stable isotopes, fate and transport of groundwater contaminants, vadose zone hydrology, metal uptake by lichens, paleoclimatic patterns in California and stable isotope systematics of clay minerals. Geologist of gold property in the Mother Lode of California. Exploration Geologist (Anaconda Minerals Company; 6

  12. Geochemistry of Aluminum in High Temperature Brines

    SciTech Connect (OSTI)

    Benezeth, P.; Palmer, D.A.; Wesolowski, D.J.

    1999-05-18T23:59:59.000Z

    The objective ofthis research is to provide quantitative data on the equilibrium and thermodynamic properties of aluminum minerals required to model changes in permeability and brine chemistry associated with fluid/rock interactions in the recharge, reservoir, and discharge zones of active geothermal systems. This requires a precise knowledge of the thermodynamics and speciation of aluminum in aqueous brines, spanning the temperature and fluid composition rangesencountered in active systems. The empirical and semi-empirical treatments of the solubility/hydrolysis experimental results on single aluminum mineral phases form the basis for the ultimate investigation of the behavior of complex aluminosilicate minerals. The principal objective in FY 1998 was to complete the solubility measurements on boehmite (AIOOH) inNaC1 media( 1 .O and 5.0 molal ionic strength, IOO-250°C). However, additional measurements were also made on boehmite solubility in pure NaOH solutions in order to bolster the database for fitting in-house isopiestic data on this system. Preliminary kinetic Measurements of the dissolution/precipitation of boehmite was also carried out, although these were also not planned in the earlier objective. The 1999 objectives are to incorporate these treatments into existing codes used by the geothermal industry to predict the chemistry ofthe reservoirs; these calculations will be tested for reliability against our laboratory results and field observations. Moreover, based on the success of the experimental methods developed in this program, we intend to use our unique high temperature pH easurement capabilities to make kinetic and equilibrium studies of pH-dependent aluminosilicate transformation reactions and other pH-dependent heterogeneous reactions.

  13. Characterization Well R-22 Geochemistry Report

    SciTech Connect (OSTI)

    Patrick Longmire

    2002-09-01T23:59:59.000Z

    This report provides analytical results for groundwater collected during four characterization-sampling rounds conducted at well R-22 from March 2001 through March 2002. Characterization well R-22 was sampled from March 6 through 13, 2001; June 19 through 26, 2001; November 30 through December 10, 2001; and February 27 through March 7, 2002. The goal of the characterization efforts was to assess the hydrochemistry and to determine whether or not contaminants are present in the regional aquifer in the vicinity of the well. A geochemical evaluation of the analytical results for the well is also presented in this report.

  14. Geochemistry of Surface-Atmosphere Interactions on

    E-Print Network [OSTI]

    Withers, Paul

    state of the surface? #12;Carbonates on Venus ¥ CaCO3+SiO2 = CaSiO3+CO2(g) ¥ Psurface = Pbuffer. ¥ S in lower atmosphere is kinetically controlled ¥ CaCO3 + SO2 = CaSO4 + CO removes SO2 , deposits CaSO4 ¥ Fe rates ¥ Need more data, new spacecraft instruments #12;Handy Minerals ¥ SiO2 Quartz ¥ CaCO3 Calcite ¥ Ca

  15. ES 6216 Isotope Geochemistry Student Presentation Guidelines

    E-Print Network [OSTI]

    Black, Robert X.

    Supplementary material Boundary conditions and numerical solution of Equation 4 The travelling of the interior solution and the other parameters. Non-existence of advancing contact-line solutions to Equation 1 then the elastic term in (1) dominates the gravitational term as r R and the dominant asymptotic balance (i

  16. Characterization Well R-7 Geochemistry Report

    SciTech Connect (OSTI)

    P.Longmire; F.Goff

    2002-12-01T23:59:59.000Z

    This report provides analytical results for four groundwater-sampling rounds conducted at characterization well R-7. The goal of the characterization efforts was to assess the hydrochemistry and to determine if contaminants from Technical Area (TA)-2 and TA-21 of the Los Alamos National Laboratory (LANL or the Laboratory) are present in the regional aquifer in the vicinity of the well. Figure 1.0-1 shows the well's location in the narrow upper part of Los Alamos Canyon, between the inactive Omega West reactor and the mouth of DP Canyon. Well R-7 is in an excellent location to characterize the hydrology and groundwater chemistry in both perched groundwater and the regional aquifer near sites of known Laboratory effluent release, including radionuclides and inorganic chemicals (Stone et al. 2002, 72717). The Risk Reduction and Environmental Stewardship-Remediation (RRES-R) Program (formerly the Environmental Restoration [ER] Project) installed well R-7 as part of groundwater investigations to satisfy requirements of the ''Hydrogeologic Workplan'' (LANL 1998, 59599) and to support the Laboratory's ''Groundwater Protection Management Program Plan'' (LANL 1996, 70215). Well R-7 was designed primarily to provide geochemical or water quality and hydrogeologic data for the regional aquifer within the Puye Formation. This report also presents a geochemical evaluation of the analytical results for well R-7 and provides hydrogeochemical interpretations using analytical results for groundwater samples collected at the well. Discussion of other hydrogeochemical data collected within the east-central portion of the Laboratory, however, is deferred until they can be evaluated in the context of sitewide information collected from other RRES and Hydrogeologic Workplan characterization wells (R-8A, R-9, and R-9i). Once all deep groundwater investigations in the east-central portion of the Laboratory are completed, geochemical and hydrogeologic conceptual models for the Los Alamos Canyon watershed may be included in a groundwater risk analysis. These models will include an evaluation of potential contaminant transport pathways. Well R-7 was completed on March 9, 2001, with three screens (363.2 to 379.2 ft, 730.4 to 746.4 ft, and 895.5 to 937.4 ft). Screen No.2 was dry during characterization sampling. Four rounds of groundwater characterization samples, collected from a perched zone and the regional aquifer from depths of 378.0 ft (screen No.1) and 915.0 ft (screen No.3), were chemically characterized for radionuclides, metals and trace elements, major ions, high-explosive (HE) compounds, total organic carbon, dissolved organic carbon, organic compounds, and stable isotopes (H, N, and O). Although well R-7 is primarily a characterization well, its design and construction also meet the requirements of a Resource Conservation and Recovery Act (RCRA)-compliant monitoring well as described in the US Environmental Protection Agency (EPA) document ''RCRA Groundwater Monitoring: Draft Technical Guidance,'' November 1992, EPA 530-R-93- 001. Incorporation of this well into a Laboratory-wide groundwater-monitoring program will be considered, and more specifically evaluated (e.g., sampling frequency, analytes, etc.), when the results of the well R-7 characterization activities are comprehensively evaluated in conjunction with other groundwater investigations in the ''Hydrogeologic Workplan'' (LANL 1998, 59599).

  17. EMSL Geochemistry, Biogeochemistry and Subsurface Science

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

    of Standards and Technology (NIST) David Shuh Lawrence Berkeley National Laboratory (LBNL) Eric Roden (offsite) University of Wisconsin Charles Werth University of Illinois at...

  18. Petroleum geochemistry of San Juan sag, Colorado

    SciTech Connect (OSTI)

    Clayton, J.L.; Gries, R.R. (Geological Survey, Denver, CO (USA))

    1989-09-01T23:59:59.000Z

    Recently, oil and gas shows have been reported in Cretaceous and Tertiary rocks of the San Juan sag, and minor oil production has been established from volcanic rocks (Kirby Petroleum 1 Jynnifer well, Sec. 9, TT40N, R5E). Potential source rocks present in the San Juan sag are the upper and lower (including the Niobrara Member) Mancos Shale (Upper Cretaceous). The combined upper and lower Mancos Shale is about 660 m thick and contains between about 0.5 and 5.5% organic carbon, although most values are between about 1.5 and 2.0%. The Niobrara Member of the lower Mancos Shale has the highest overall organic matter content in the section (organic carbon averages > 2.0%). Pyrolysis and solvent extraction yields (typically 2,000-6,000 and 1,000-4,000 ppm, respectively) indicate that the upper and lower Mancos Shale and the Niobrara Member are all good potential source rocks for oil and gas. Oil-source rock correlations using gas chromatography, mass spectrometry, and stable carbon isotope ratios indicate that the upper Mancos Shale is the most likely source for the oil produced from the 1 Jynnifer discovery well. The source of the oil produced from the nearby Gramps field is less certain but may be the lower Mancos Shale or Niobrara Member. The hydrocarbon generation history of the San Juan sag is complex because of highly variable heat flow in the area caused by Oligocene volcanism. Sills have caused thermal alteration of organic matter in shales on a local scale, and larger volcanic bodies may have produced proportionally larger thermal effects. Localized heating may have caused thermal decomposition of carbonate minerals and generation of high CO{sub 2} gas deposits. Higher regional heat flow associated with volcanism was important in the source rock maturation of this area and maturation was relatively recent (Oligocene to present).

  19. Mineralogy, geochemistry, and 40 Ar geochronology

    E-Print Network [OSTI]

    Africa 3163 and paired stones: Comparisons with Apollo samples Jillian A. Hudgins a , Simon P. Kelley b, and melt pockets, which are absent in the Apollo granulitic breccias. Although the Apollo and meteorite regions of the Moon. Based on mineral- ogical and geochemical differences between the Apollo and meteorite

  20. Intergrating Magnetotellurics, Soil Gas Geochemistry and Structural

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

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels DataDepartment of Energy Your Density Isn't YourTransport(FactDepartment of EnergyIndustry15Among States in theWAPA1 DOEAnalysis to

  1. Property:Geochemistry | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to:Ezfeedflag Jump to: navigation, search PropertyCalculatedCenter

  2. Environmental Geochemistry of Rads | Environmental Radiation Protection

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

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645U.S. DOE Office of Science (SC) Environmental Assessments (EA) / Environmental Impact Statements

  3. Miocene core complex development and coeval supradetachment basin evolution of Paros, Greece

    E-Print Network [OSTI]

    Bargnesi, Evan Anthony

    2011-05-23T23:59:59.000Z

    (Brichau et al., 2006), detrital ages of the hanging wall rocks (Sanchez-Gomez et al., 2002) and new lithologic and structural mapping (Papp, 2007). This study builds on the foundation laid by these authors and contributes to the growing body of science... and Geochemistry, 58, 441–448. Sanchez-Gomez, M., Avigad, D., Heimann, A., 2002. Geochronology of clasts in allochthonous Miocene sedimentary sequence on Mykonos and Paros Islands: implications for backarc extension in the Aegean Sea. Journal...

  4. Salinity Control in Irrigation Agriculture.

    E-Print Network [OSTI]

    Lyerly, Paul J.; Longenecker, Donald E.

    1962-01-01T23:59:59.000Z

    streams and under- ground sources contain dissolved substances known chemically as salts. Ocean water contains approximately 3 percent salts, or 40 tons of salts per acre-foot of water. Waters used for irriga- tion generally contain .1 to 5 tons... of salt per acre-foot of water. In general terms, salt is thought of as table alt; however, thousands of different salts are known. Examples of common salts in irrigation water are table salt (sodium chloride), Epsom salt (magnesium sulfate), gypsum...

  5. Salinity Control in Irrigation Agriculture.

    E-Print Network [OSTI]

    Longenecker, Donald E.; Lyerly, Paul J.

    1957-01-01T23:59:59.000Z

    substances I chemically as salts. Ocean water contains rimately 3 percent salts, or 40 tons of salts .-foot of water. Waters used for irriga- ~erally contain .1 to 5 tons of salt per acre- water. . -er acrf +ion gen 'pot of ,.. ,enera1 terms, salt... and rock materials through which .he water must seep before becoming available inr irrigation. Mountain streams often contain less than one-tenth ton of salt per acre-foot of .rater. Drainage waters and ground waters in lesert valleys may contain...

  6. Irrigation Water Quality Salinity Management

    E-Print Network [OSTI]

    Small Potassium sulfate K2SO4 Small Sodium bicarbonate NaHCO3 Small Calcium carbonate CaCO3 Very Small concentration as related to the concentration of calcium and magnesium, and 3 Irrigation Water Quality Standards Na2SO4 Moderate to large Calcium chloride CaCl2 Moderate Calcium sulfate (gypsum) CaSO4 2H2O Moderate

  7. Effect of Soaking in Hot Saline Solution and Humid Atmosphere on the Passive Film Behavior of a Ni-Cr-Mo Alloy

    SciTech Connect (OSTI)

    P. Pharkya; J.H. Payer

    2006-06-09T23:59:59.000Z

    Alloy 22, a Ni-Cr-Mo alloy, is the candidate material for fabrication of canisters for disposal of high-level and spent nuclear fuel waste in the proposed Yucca Mountain repository in Nevada. This paper investigated the passive film behavior and corrosion properties on Alloy 22 as a function of soaking in hot, saline environments and in hot, humid atmospheres. Environmental parameters include potential, temperature, pH in chloride and multi-species solutions. Hot, humid exposures are planned for temperatures up to 300 C. Soaking times are planned to extend for up to 1000 hours. This work is part of a multi-investigator study to determine the durability of passive films and localized corrosion processes in metal exposed to moist particulate and deposits. Of particular interest are the long-term stability of the passive film and the effects of soaking in aqueous solutions or hot, humid atmospheres. A combination of electrochemical methods measure changes in passive film properties, and a combination of surface analysis techniques are used to characterize the film composition and structure. Electrochemical methods include Potentiodynamic Polarization tests for the general corrosion behavior; along with Electrochemical Impedance Spectroscopy (EIS) and Mott-Schottky (M-S) analysis for electronic properties of the passive films. Alterations in the chemical composition and structure of the passive film are characterized using X-ray Photoelectron Spectroscopy (XPS), Auger Electron Spectroscopy (AES) and Transmission Electron Microscopy (TEM). Results for freshly formed films are shown in figure 1. The EIS results show that the interfacial impedance increased with increasing potential to maximum within the passive range and then decreased as the potential was increased further. interfacial impedance was found to decrease with increasing temperature. Mott-Schottky analysis indicated that the oxide film which is n-type in the passive region changes to p-type in the transpassive region. Figure 2 shows the representative chemical soaking results at 90 C for up to 240 hours; the interfacial impedance increased with soaking time. Results from this work are combined with those from collaborative studies to correlate the passive film properties with the resistance to localized corrosion using multi-crevice assemblies and micro-corrosion cells. The passive film growth and dissolution are interpreted with reference to processes based on the point defect model.

  8. Development of Science-Based Permitting Guidance for Geological Sequestration of CO2 in Deep Saline Aquifers Based on Modeling and Risk Assessment

    SciTech Connect (OSTI)

    Jean-Philippe Nicot; Renaud Bouroullec; Hugo Castellanos; Susan Hovorka; Srivatsan Lakshminarasimhan; Jeffrey Paine

    2006-06-30T23:59:59.000Z

    Underground carbon storage may become one of the solutions to address global warming. However, to have an impact, carbon storage must be done at a much larger scale than current CO{sub 2} injection operations for enhanced oil recovery. It must also include injection into saline aquifers. An important characteristic of CO{sub 2} is its strong buoyancy--storage must be guaranteed to be sufficiently permanent to satisfy the very reason that CO{sub 2} is injected. This long-term aspect (hundreds to thousands of years) is not currently captured in legislation, even if the U.S. has a relatively well-developed regulatory framework to handle carbon storage, especially in the operational short term. This report proposes a hierarchical approach to permitting in which the State/Federal Government is responsible for developing regional assessments, ranking potential sites (''General Permit'') and lessening the applicant's burden if the general area of the chosen site has been ranked more favorably. The general permit would involve determining in the regional sense structural (closed structures), stratigraphic (heterogeneity), and petrophysical (flow parameters such as residual saturation) controls on the long-term fate of geologically sequestered CO{sub 2}. The state-sponsored regional studies and the subsequent local study performed by the applicant will address the long-term risk of the particular site. It is felt that a performance-based approach rather than a prescriptive approach is the most appropriate framework in which to address public concerns. However, operational issues for each well (equivalent to the current underground injection control-UIC-program) could follow regulations currently in place. Area ranking will include an understanding of trapping modes. Capillary (due to residual saturation) and structural (due to local geological configuration) trappings are two of the four mechanisms (the other two are solubility and mineral trappings), which are the most relevant to the time scale of interest. The most likely pathways for leakage, if any, are wells and faults. We favor a defense-in-depth approach, in which storage permanence does not rely upon a primary seal only but assumes that any leak can be contained by geologic processes before impacting mineral resources, fresh ground water, or ground surface. We examined the Texas Gulf Coast as an example of an attractive target for carbon storage. Stacked sand-shale layers provide large potential storage volumes and defense-in-depth leakage protection. In the Texas Gulf Coast, the best way to achieve this goal is to establish the primary injection level below the total depth of most wells (>2,400 m-8,000 ft). In addition, most faults, particularly growth faults, present at the primary injection level do not reach the surface. A potential methodology, which includes an integrated approach comprising the whole chain of potential events from leakage from the primary site to atmospheric impacts, is also presented. It could be followed by the State/Federal Government, as well as by the operators.

  9. Hydraulic Fracture Optimization with a Pseudo-3D Model in Multi-layered Lithology 

    E-Print Network [OSTI]

    Yang, Mei

    2011-10-21T23:59:59.000Z

    Hydraulic Fracturing is a technique to accelerate production and enhance ultimate recovery of oil and gas while fracture geometry is an important aspect in hydraulic fracturing design and optimization. Systematic design ...

  10. RADIOACTIVITY DOSAGE OF ORNAMENTAL GRANITIC ROCKS BASED ON CHEMICAL, MINERALOGICAL AND LITHOLOGICAL DATA

    SciTech Connect (OSTI)

    Salas, H.T.; Nalini, H.A. Jr.; Mendes, J.C.

    2004-10-03T23:59:59.000Z

    One hundred samples of granitic rock were collected from granite traders in Belo Horizonte. Autoradiography, optical microscopy, diffractometry, and chemical analysis (X-ray spectrometry, X-ray fluorescence, neutron activation, gravimetry and electron probe microanalysis) were used to determine the mineral assemblages and lithotypes. Autoradiographic results for several samples showed the presence of monazite, allanite and zircon. Chemical analysis revealed concentrations of uranium of {le} 30ppm, and thorium {le} 130ppm. Higher concentrations generally correlated with high concentrations of light rare earths in silica-rich rocks of granitic composition. Calculations were made of radioactive doses for floor tiles in a standard room for samples with total concentration of uranium and thorium greater than 60ppm. On the basis of calculations of {sup 232}Th, {sup 40}K and {sup 226}Ra from Th, K and U analysis, the doses calculated were between 0.11 and 0.34 mSv/year, which are much lower than the acceptable international exposure standard of 1.0 mSv/year.

  11. Hydraulic Fracture Optimization with a Pseudo-3D Model in Multi-layered Lithology

    E-Print Network [OSTI]

    Yang, Mei

    2011-10-21T23:59:59.000Z

    -layered reservoir, (3) The upwards and downwards growth of the fracture tip from the crack center....

  12. Bedrock structure, lithology and ground water: influences on slope failure initiation in Davis County, Utah

    E-Print Network [OSTI]

    Ala, Souren Nariman

    1990-01-01T23:59:59.000Z

    , for his input. The Salt Lake City office of Dames and Moore generously provided for me to print the results of my Viii geophysical surveys. Mr. Roger Fallon of Salt Lake City did us a great service by flying us around the Wasatch Front canyons; much... Complex between Farmington and Stone Creeks. . . . . . . . . . . . pocket INTRODUCTION Rapid population growth in the urban area along the eastern border of the Great Salt Lake, Utah, has led to residential development in the western foothills...

  13. Hybrid optimization for lithologic inversion and time-lapse monitoring using a binary formulation

    E-Print Network [OSTI]

    of prior geologic information and rapid build- up of large-scale model features, whereas the latter guides topology creates difficulties when regional field or small-scale resid- uals resulting from shallow sources

  14. The foraminiferal and lithologic characteristics of the Reklaw formation of Leon, Robertson and Milam counties, Texas

    E-Print Network [OSTI]

    Davis, Kenneth Eugene

    1961-01-01T23:59:59.000Z

    with the power auger was a piece of tubing four inches ln diameter, with two "Ln shaped cutting':teeth at the base. 15 As the teeth cut on the bottom of the hole the material was forced irrto the tubing preventing contamination 6f' strata. from"bbove. Samples... the portable power auger to obtain samples from unexposed local- ities and who critically read the manuscript. The writer is grateful to Mr. C. M. Maggio and Mr. D. I. Miller for their aid in collecting samples . ABSTRACT The Reklaw formation of Leon...

  15. The effects of lithology and initial fault angle in physical models of fault-propagation folds

    E-Print Network [OSTI]

    McLain, Christopher Thomas

    2001-01-01T23:59:59.000Z

    Experimentally deformed physical rock models are used to examine the effects of changing mechanical stratigraphy and initial fault angle on the development of fault-propagation folds over a flat-ramp-flat thrust geometry. This study also...

  16. Corrigendum A Correction to Identification of Source Lithology in the Hawaiian and Canary Islands

    E-Print Network [OSTI]

    : Implications for Origins Journal of Petrology 2011, volume 52, pp. 113-146 HERZBERG, C. DEPARTMENT OF EARTH-mail: journals.permissions@ oup.com JOURNAL OF PETROLOGY VOLUME 52 NUMBER 5 PAGES1047 2011 doi:10.1093/petrology/egr012 atRutgersUniversityLibraries/TechnicalServicesonMay16,2011petrology

  17. Lithology and well log study of Campbell E-2 geothermal test well, Humboldt

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere I Geothermal Pwer Plant Jump to:Landowners and WindLightingLinthicum, Maryland:source HistoryLiteHouse

  18. Lithologic descriptions and temperature profiles of five wells in the southwestern Valles caldera region, New Mexico

    SciTech Connect (OSTI)

    Shevenell, L.; Goff, F.; Miles, D.; Waibel, A.; Swanberg, C.

    1988-01-01T23:59:59.000Z

    The subsurface stratigraphy and temperature profiles of the southern and western Valles caldera region have been well constrained with the use of data from the VC-1, AET-4, WC 23-4, PC-1 and PC-2 wells. Data from these wells indicate that thermal gradients west of the caldera margin are between 110 and 140)degrees)C/km, with a maximum gradient occurring in the bottom of PC-1 equal to 240)degrees)C/km as a result of thermal fluid flow. Gradients within the caldera reach a maximum of 350)degrees)C/km, while the maximum thermal gradient measured southwest of the caldera in the thermal outflow plume is 140)degrees)C/km. The five wells exhibit high thermal gradients (>60)deghrees)C/km) resulting from high conductive heat flow associated with the Rio Grande rift and volcanism in the Valles caldera, as well as high convective heat flow associated with circulating geothermal fluids. Gamma logs run in four of the five wells appear to be of limited use for stratigraphic correlations in the caldera region. However, stratigraphic and temperature data from the five wells provide information about the structure and thermal regime of the southern and western Valles caldera region. 29 refs., 9 figs. 2 tabs.

  19. Dataset: Soda Lake Well Lithology Data and Geologic Cross-Sections | DOE

    Office of Scientific and Technical Information (OSTI)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItem Not Found Item Not Found The itemAIR57451 Clean Energy5655994DP-1513 .AssessmentData

  20. Core Lithology From the State of Hawaii Scientific Observation Hole 1,

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand JumpConceptual Model, clickInformationNew|Core Analysis At Geysers| Open EnergyAl., 1987) |

  1. Core Lithology, Valles Caldera No. 1, New Mexico | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand JumpConceptual Model, clickInformationNew|Core Analysis At Geysers| Open EnergyAl.,

  2. Carbonate GeochemistryCarbonate Geochemistry Everything useful you need to know

    E-Print Network [OSTI]

    Miami, University of

    - = CaCO3 At equilibrium Ksp = CaCO3/ [Ca 2+ ] [CO3 2-] #12;2/25/2009 5 Concentrations of elements the concentration of the otherother For CaCO3 the IMP = 0.011 x 0.0002 The effective molality is called the activity

  3. T2Well/ECO2N Version 1.0: Multiphase and Non-Isothermal Model for Coupled Wellbore-Reservoir Flow of Carbon Dioxide and Variable Salinity Water

    SciTech Connect (OSTI)

    Pan, L.; Oldenburg, C.M.; Wu, Y.-S.; Pruess, K.

    2011-02-14T23:59:59.000Z

    At its most basic level, the injection of CO{sub 2} into geologic CO{sub 2} storage sites involves a system comprising the wellbore and the target reservoir. The wellbore is the only conduit available to emplace CO{sub 2} into reservoirs for long-term storage. At the same time, wellbores in general have been identified as the most likely conduit for CO{sub 2} and brine leakage from geologic carbon sequestration (GCS) sites, especially those in sedimentary basins with historical hydrocarbon production. We have developed a coupled wellbore and reservoir model for simulating the dynamics of CO{sub 2} injection and leakage through wellbores. The model describes the following processes: (1) upward or downward wellbore flow of CO{sub 2} and variable salinity water with transition from supercritical to gaseous CO{sub 2} including Joule-Thomson cooling, (2) exsolution of CO{sub 2} from the aqueous phase as pressure drops, and (3) cross flow into or interaction with layers of surrounding rock (reservoirs). We use the Drift-Flux Model and related conservation equations for describing transient two-phase non-isothermal wellbore flow of CO{sub 2}-water mixtures under different flow regimes and interacting with surrounding rock. The mass and thermal energy balance equations are solved numerically by a finite difference scheme with wellbore heat transmission to the surrounding rock handled either semi-analytically or numerically. The momentum balance equation for the flow in the wellbore is solved numerically with a semi-explicit scheme. This manual provides instructions for compilation and use of the new model, and presents some example problems to demonstrate its use.

  4. Analysis of the structural parameters that influence gas production from the Devonian shale. Annual progress report, 1979-1980. Volume III. Data repository and reports published during fiscal year 1979-1980: production, unsponsored research

    SciTech Connect (OSTI)

    Negus-De Wys, J.; Dixon, J. M.; Evans, M. A.; Lee, K. D.; Ruotsala, J. E.; Wilson, T. H.; Williams, R. T.

    1980-10-01T23:59:59.000Z

    This document consists of the following papers: inorganic geochemistry studies of the Eastern Kentucky Gas Field; lithology studies of upper Devonian well cuttings in the Eastern Kentucky Gas Field; possible effects of plate tectonics on the Appalachian Devonian black shale production in eastern Kentucky; preliminary depositional model for upper Devonian Huron age organic black shale in the Eastern Kentucky Gas Field; the anatomy of a large Devonian black shale gas field; the Cottageville (Mount Alto) Gas Field, Jackson County, West Virginia: a case study of Devonian shale gas production; the Eastern Kentucky Gas Field: a geological study of the relationships of Ohio Shale gas occurrences to structure, stratigraphy, lithology, and inorganic geochemical parameters; and a statistical analysis of geochemical data for the Eastern Kentucky Gas Field.

  5. Soil Salinity Abatement Following Hurricane Ike 

    E-Print Network [OSTI]

    Mueller, Ryan

    2012-10-19T23:59:59.000Z

    . The initial salt levels in November 2008 had an electrical conductivity (ECe) of the inundated soils as high as 26.7 dS/m. Fifty-four percent of the soils sampled in the 0-15 cm horizons and 9% in the 15-30 cm horizons of the edge area had an ECe >= 4 d...

  6. Characterizing Salinity Tolerance in Greenhouse Roses

    E-Print Network [OSTI]

    Solis Perez, Alma R.

    2011-08-08T23:59:59.000Z

    Among ornamental plants, roses (Rosa L.) are considered the most economically important, being among the most popular garden shrubs, as well as the favorite cut flowers sold by florists. In the past roses have been classified as fairly salt...

  7. Is Salinity Variability a Benthic Disturbance?

    E-Print Network [OSTI]

    Van Diggelen, Amanda

    2014-05-07T23:59:59.000Z

    Secondary Primary Lavaca Bay Matagorda Bay A, B C, D 1988-2009 Guadalupe Secondary Primary Upper San Antonio Bay Lower San Antonio Bay A, B C, D 1987-2000, 2004-2013 Mission- Aransas Secondary Primary Copano Bay Aransas Bay A, B...

  8. Salinity routing in reservoir system modeling

    E-Print Network [OSTI]

    Ha, Mi Ae

    2007-04-25T23:59:59.000Z

    in several major river basins in Texas and neighboring states. WRAP is the river/reservoir system simulation model incorporated in the Water Availability Modeling (WAM) System applied by agencies and consulting firms in Texas in planning and water right...

  9. Salinity patterns in the Houston Ship Channel

    E-Print Network [OSTI]

    Withers, Richard Ercelray

    1969-01-01T23:59:59.000Z

    to the highly stratified. It is also subject to heavy industrial waste loading and large volumes of urban storm runoff. Further, the tidal action in ihe channel is relatively minor, The mean tide elevation normally varies from one to two feet. A multiple... linear regression analysis is us d to derive the prediction eouation. The parameters are included in the regression analysis raised to various combinations of powers to expedite a non-linear analysis. The best ? fit predic- tion equation is determined...

  10. Calcite Reaction Kinetics in Saline Waters 

    E-Print Network [OSTI]

    Finneran, David

    2012-02-14T23:59:59.000Z

    results. Overall, these findings may be useful in understanding and predicting the interaction and reactivity of the host carbonate minerals in subsurface reservoirs to the injection of CO2 although much work needs to be completed at elevated temperatures...

  11. Ses Salines > UIB (en transport pblic)

    E-Print Network [OSTI]

    Oro, Daniel

    Durada: 51 min. Cost mitjà del viatge1 : 9'42 Emissions addicionals (CO2): 10,54 Kg Emissions addicionals (SO2): 0,006 Kg Durada: 100 min. Cost mitjà del viatge2 : 1,21 Emissions addicionals (CO2): 0 kg 1 any Temps acumulat3 : 12,47 dies Despesa per any3 : 3.317'25 Emissions addicionals (CO2): 3

  12. Saline, Michigan: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere IRaghuraji Agro Industries Pvt Ltd Jump to:RoscommonSBY SolutionsChangeOklahoma:Open Energy

  13. Property:SalinityAverage | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to:Ezfeedflag Jump to:ID8/Organization RAPID/Contact/ID8/Positionmaterial Jump

  14. The geochemistry of uranium in the Orca Basin

    E-Print Network [OSTI]

    Weber, Frederick Fewell

    1979-01-01T23:59:59.000Z

    . , 1974). Substantial uranium enrichments have been reported by many investigators for samples taken from aroxic environments (Strom, 1948; Starik et al. , '1961; Swanson, 1961; Sackett and Cook, 1969; Kolodny and Kaplan, 1969; Bertine et al. , 1970...) ~ Degens et al. , (1977) report concentrations of uranium as high as 60ppm, more than an order of magnitude enrich- meut, for Black Sea sediments. If marine reducing environments are found with uranium concentrations apuroaching 100ppm, they will begin...

  15. The marine geochemistry of iron and iron isotopes

    E-Print Network [OSTI]

    Bergquist, Bridget A., 1973-

    2004-01-01T23:59:59.000Z

    This thesis addressed questions about the Fe cycle by measuring detailed profiles and transects of Fe species in the ocean and also by exploring the use of a new tracer of Fe, Fe isotopic fractionation. In the subtropical ...

  16. The geochemistry of uranium in the Orca Basin 

    E-Print Network [OSTI]

    Weber, Frederick Fewell

    1979-01-01T23:59:59.000Z

    as uranium concentrations dzop to an average of 2. dppm, indicative of relatively low uranium bearing pelagic particle deposition. Furthermore, the 13 C values become heavier in this region, lacking a large terrest. rial component. This evidence suggests... 39 the basin walls. It may be possible that these particles at the brine/seawater interface incorporate any uranium reduced in this zone and carry it to the brine perimeter where it is deposited. Unfortunately, attempts to accurately core...

  17. Heavy metal geochemistry of the Pontchartrain-Maurepas estuarine complex

    SciTech Connect (OSTI)

    Flowers, G.C. (Tulane Univ., New Orleans, LA (USA)); Isphording, W.C. (Univ. of South Alabama, Mobile (USA))

    1990-09-01T23:59:59.000Z

    The Pontchartrain-Maurepas estuarine complex has become the focus of an intense debate concerning hydraulic shell dredging and its effects. Besides disrupting the benthic community, it has been alleged by the opponents of shell dredging that the mining process releases harmful concentrations of heavy metals into the water column. Bottom sediment heavy metal data combined with ion-site partitioning analyses provide a basis for estimating heavy metal release during dredging. The concentrations of Cu, Cr, Ni, Fe, Zn, V, Co, Pb, and Ba were determined for bottom sediment samples collected during 1987. The areal distribution of metals in the complex is controlled largely by sediment texture. As the clay content of the sediment increases, so does metal content. This observation seems to hold for most estuaries along the northern Gulf of Mexico. The concentrations of all metals except Pb were found to be positively correlated with Fe-content. Comparison of average metal contents with data from other estuaries along the Gulf Coast indicates that the complex has not been heavily impacted by anthropogenic input of metals. Because dredging disrupts redox conditions in the sediment, the potential release of metals into the water column is a real concern. However, partitioning analyses indicate that the majority of metal present in the bottom sediments is in relatively stable phases. The metal content of the exchangeable and organic phases, which are most easily affected by redox changes, was found to be minor. The rapid process of hydraulic shell mining, the positive Eh of the lake water, and the fine-grained suspended sediments result in a minor impact of dredging on water quality. Released metals are rapidly scavenged by adsorption and coprecipitation reactions.

  18. Organic geochemistry and stable isotope constraints on Precambrian biogeochemical processes

    E-Print Network [OSTI]

    Thomas, Katherine S., S.M. Massachusetts Institute of Technology

    2011-01-01T23:59:59.000Z

    Details of the biogeochemical cycles and the dominant mechanisms present in Precambrian remain heavily debated topics. The events of the Late Proterozoic onset to glaciations and what types of early life existed in the ...

  19. 1 INTRODUCTION The geochemistry of clayrocks is of current inter-

    E-Print Network [OSTI]

    Boyer, Edmond

    placed in the degassing cell immediately after coring in order to minimize at- mospheric contamination in Europe. The isotope ratios (C, O) of the gas and of the carbonate minerals were also obtained. The stable

  20. The geochemistry of redox sensitive trace metals in sediments

    SciTech Connect (OSTI)

    Morford, J.L.; Emerson, S. [Univ. of Washington, Seattle, WA (United States). School of Oceanography] [Univ. of Washington, Seattle, WA (United States). School of Oceanography

    1999-06-01T23:59:59.000Z

    The authors analyzed the redox sensitive elements V, Mo, U, Re and Cd in surface sediments from the Northwest African margin, the US Northwest margin and the Arabian Sea to determine their response under a range of redox conditions. Where oxygen penetrates 1 cm or less into the sediments, Mo and V diffuse to the overlying water as Mn is reduced and remobilized. Authigenic enrichments of U, Re and Cd are evident under these redox conditions. With the onset of sulfate reduction, all of the metals accumulate authigenically with Re being by far the most enriched. General trends in authigenic metal accumulation are described by calculating authigenic fluxes for the 3 main redox regimes: oxic, reducing where oxygen penetrates {le} 1 cm, and anoxic conditions. Using a simple diagenesis model and global estimates of organic carbon rain rate and bottom water oxygen concentrations, the authors calculate the area of sediments below 1,000 m water depth in which oxygen penetration is {le} 1 cm to be 4% of the ocean floor. They conclude that sediments where oxygen penetrates {le} 1 cm release Mn, V and Mo to seawater at rates of 140%--260%, 60%--150% and 5%--10% of their respective riverine fluxes, using the authigenic metal concentrations and accumulation rates from this work and other literature. These sediments are sinks for Re, Cd and U, with burial fluxes of 70%--140%, 30%--80% and 20%--40%, respectively, of their dissolved riverine inputs. They modeled the sensitivity of the response of seawater Re, Cd and V concentrations to changes in the area of reducing sediments where oxygen penetrates {le} 1 cm. The analysis suggests a negligible change in seawater Re concentration, whereas seawater concentrations of Cd and V could have decreased and increased, respectively, by 5%--10% over 20 kyr if the area of reducing sediments increased by a factor of 2 and by 10%--20% if the area increased by a factor of 3. The concentration variations for a factor of 2 increase in the area of reducing sediments are at about the level of uncertainty of Cd/Ca and V/Ca ratios observed in foraminifera shells over the last 40 kyr. This implies that the area of reducing sediments in the ocean deeper than 1,000 m (4%) has not been greater than twice the present value in the recent past.

  1. Evaluating mantle and crustal processes using isotope geochemistry

    E-Print Network [OSTI]

    Saal, Alberto Edgardo

    2000-01-01T23:59:59.000Z

    Geochemical studies are fundamental for understanding how the dynamic Earth works and evolves. These studies place constraints on the composition, formation, age, distribution, evolution and scales of geochemically distinct ...

  2. Geochemistry and Isotopes of Fluids from Sulphur Springs, Valles...

    Open Energy Info (EERE)

    a deep reservoir temperature of 215 to 280C. Comparison of 13C and 18O between CaCO3 from well cuttings and CO2 from fumarole steam indicates a fractionation temperature...

  3. A Summary of the Geology, Geochemistry, and Geophysics of the...

    Open Energy Info (EERE)

    Area, Utah Authors S. H. Ward, W. T. Parry, W. P. Nash, W. R. Sill, K. L. Cook, R. B. Smith, D. S. Chapman, F. H. Brown, J. A. Whelan and J. R. Bowman Published Journal...

  4. Geothermal: Sponsored by OSTI -- Geochemistry Sampling for Traditional...

    Office of Scientific and Technical Information (OSTI)

    for Traditional and Multicomponent Equilibrium Geothermometry in Southeast Idaho Geothermal Technologies Legacy Collection HelpFAQ | Site Map | Contact Us HomeBasic Search...

  5. www.emsl.pnl.gov GEOCHEMISTRY/BIOGEOCHEMISTRY

    E-Print Network [OSTI]

    . These scientific advances are accomplished through strong, multidisciplinary collaborations between an engaged user on efficient conversions of light energy into biofuel. Researchers from PNNL and Washington University in St

  6. Geochemistry of arsenic and antimony in Galveston Bay, Texas

    E-Print Network [OSTI]

    Tripp, Anthony Roy

    1988-01-01T23:59:59.000Z

    as no concentration change in dissolved arsenic or antimony was measured due to adsorption or desorption when river water high in SPM and sea water were mixed over a time period of 72 hours. Though the bulk chemical character of the bayous of Galveston Island.... . . . . . . . . . . . . . . Dissolved arsenic profile for mixing experiment using Brazos River Water. . Data for dissolved arsenic and antimony from mixing experiments using Atchafalaya River Water. . . . . . . . . . . . . . . . . . . . . 54 57 58 59 29. Results of adsorption...

  7. Seismicity And Fluid Geochemistry At Lassen Volcanic National...

    Open Energy Info (EERE)

    Springs Lake, and has an outflow plume of degassed liquid that boils again beneath Terminal Geyser. Three distinct seismogenic zones (identified as the West, Middle, and East...

  8. UNCORRECTEDPROOF Hydrogeology and geochemistry of near-shore submarine

    E-Print Network [OSTI]

    rates based on tidal signal and hydraulic gradient analysis indicate a fresh submarine groundwater by Elsevier Ltd. doi:10.1016/j.ecss.2007.07.020 ARTICLE IN PRESS Please cite this article in press as: June A

  9. Mercury Surface, Space Environment, Geochemistry, and Ranging Mission

    E-Print Network [OSTI]

    Mojzsis, Stephen J.

    ·Carnegie Institution of Washington ·NASA Goddard Space Flight Center ·University of Michigan ·Southwest's atmosphere generated? Does Mercury have ice at its poles? Combining an ultraviolet spectrometer and infrared McClintock Other organizations involved: ·The Johns Hopkins University Applied Physics Laboratory

  10. Revised version Organic Geochemistry 21, 517-523, 1994.

    E-Print Network [OSTI]

    Boyer, Edmond

    matter and of biological marker ratios below the zone of silica diagenesis. SAMPLES AND METHODS Mineral form a major component with an unusually clear record of silica diagenesis with depth. At Oki Ridge

  11. THE ORGANIC GEOCHEMISTRY OF ANCIENT SEDIMENTS PART II

    E-Print Network [OSTI]

    1966-01-01T23:59:59.000Z

    1965) Change in Green River Oil Shale Paraffins with Depth.in the Green Hiver' Oil-Shale, as a ftmction of depth (

  12. Isotope Geochemistry of Thermal and Nonthermal Waters in the...

    Open Energy Info (EERE)

    geothermal fluids display a positive oxygen 18 shift of not less than 2 because of rock-water isotopic exchange at 220-300C. The Valles geothermal system is capped by a...

  13. Revised version Organic Geochemistry 22, 1023-1027, 1994.

    E-Print Network [OSTI]

    . Abstract- A Pliocene oil shale (Pula, Hungary), a C3 plant Triticum aestivum and a C4 plant Zea mays were-alkane, n-alkene, Pula oil shale, Botryococcus braunii, alga, plant, waxes, sediment. INTRODUCTION n-rich, Pliocene deposit from Pula (Hungary). The bulk carbon isotope ratio of this oil shale was also determined

  14. COAL QUALITY AND GEOCHEMISTRY, POWDER RIVER BASIN, WYOMING AND MONTANA

    E-Print Network [OSTI]

    in the Powder River Basin in Wyoming and Montana (fig. PQ-1) is considered to be "clean coal." For the location

  15. Gas Geochemistry Of The Valles Caldera Region, New Mexico And...

    Open Energy Info (EERE)

    Region, New Mexico And Comparisons With Gases At Yellowstone, Long Valley And Other Geothermal Systems Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal...

  16. Geochemistry And Geothermometry Of Spring Water From The Blackfoot...

    Open Energy Info (EERE)

    a direct result of high potassium concentrations in the water. A correction for carbon dioxide applied to the Na-K-Ca geothermometer lowers the estimated temperatures of the...

  17. The Role of Geochemistry and Stress on Fracture Development and...

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

    J. McLennan: Rock mechanics, rock property measurements, fracture stimulation in oil and gasgeothermal industry Students: D. Brinton (B.S.M.S), K. McLin (Ph.D.), J....

  18. Geochemistry And Geothermometry Of Spring Water From The Blackfoot

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are being directedAnnualPropertyd8c-a9ae-f8521cbb8489InformationFrenchtown,Jump to:Locations In TheReservoir

  19. Geochemistry Of The Lake City Geothermal System, California, Usa | Open

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are being directedAnnualPropertyd8c-a9ae-f8521cbb8489InformationFrenchtown,Jump to:Locations In TheReservoirEnergy

  20. Geochemistry of Thermal Waters in Long Valley, Mono County, California |

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are being directedAnnualPropertyd8c-a9ae-f8521cbb8489InformationFrenchtown,Jump to:Locations In

  1. Geothermal Exploration Using Surface Mercury Geochemistry | Open Energy

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to: navigation, search OpenEI Reference LibraryAdd to library WebWesternLondon,Valley, Nv |

  2. Invited review article Geochemistry of subduction zone serpentinites: A review

    E-Print Network [OSTI]

    . The geochemical data of serpentinites shows little mobility of compatible and rare earth el- ements (REE, CNRS, 1381 rue de la Piscine, 38400 Grenoble Cedex 09, France c Department of Earth Sciences their subduction as well as their impact in the global geochemical cycle. When studying serpentinites

  3. The geochemistry of phosphate in the Mississippi River delta 

    E-Print Network [OSTI]

    Thyne, Geoffrey Dickerson

    1980-01-01T23:59:59.000Z

    product of diagenesis may be the result of a slow mineral equilibria, but the short term control of interstitial con- centrations in early diagenetic reactions may be adsorption reactions. CHEN et al. (1973), HARTER (1968), HINGSTON et al. (1967... concentrations wi 1 1 depend on flux out of the sediments and mineral equilibria, rather than control by adsorption on clay minerals. The remaining adsorbed phosphate will move from the solid to dissolved phase as interstitial concentrations are reduced...

  4. Surface Mercury Geochemistry As A Guide To Volcanic Vent Structure...

    Open Energy Info (EERE)

    (contrast values > 1.5) occur within Novarupta Basin. High-magnitude, active Hg2 enrichment was found on the Turtle, a dome-like feature northeast of the Novarupta extrusive...

  5. Seismicity And Fluid Geochemistry At Lassen Volcanic National Park,

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere IRaghuraji Agro Industries Pvt Ltd JumpInformationScotts Corners, NewSeeger EngineeringCalifornia-

  6. Advances In The Past 20 Years- Geochemistry In Geothermal Exploration

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to:Ezfeedflag JumpID-fTriWildcat 1AMEE Jump to:Ohio:Ads-tecInformation Circa 2007 Jump

  7. Isotope Geochemistry of Thermal and Nonthermal Waters in the Valles

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are8COaBulkTransmissionSitingProcess.pdfGetecGtelInterias Solar Energy JumpIrem GeothermalIselin,Isofoton SA

  8. Isotope Geochemistry Of Minerals And Fluids From Newberry Volcano, Oregon |

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to: navigation, searchOf Kilauea Volcano, Hawaii | OpenSuperior WindOpen Energy Information

  9. Geothermal investigations in Idaho. Part 1. Geochemistry and geologic

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are8COaBulkTransmissionSitingProcess.pdf Jump1946865°,Park,2005)EnergyAmatitlan Geothermal Areagreenhouse

  10. Noble Gas Geochemistry In Thermal Springs | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are beingZealand Jump to: navigation, searchOfRoseConcerns Jump to:Neppelsource History(CTI PFAN)FossilWindSprings Jump

  11. Crustal Geophysics and Geochemistry Science Center | Open Energy

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are being directedAnnualProperty EditCalifornia:PowerCER.pngRoofs and Heat

  12. Geochemistry and Isotopes of Fluids from Sulphur Springs, Valles Caldera,

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are8COaBulkTransmissionSitingProcess.pdf Jump1946865°,Park, Texas:Webinars/PuestaGenevaGeoLectric PowerTechniquesNew

  13. Geology, Water Geochemistry And Geothermal Potential Of The Jemez Springs

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov You are8COaBulkTransmissionSitingProcess.pdf Jump1946865°,Park,2005) | Open Energy(Blackwell, EtRaftArea, Canon De San

  14. An AVO method toward direct detection of lithologies combining P-P and P-S reflection data 

    E-Print Network [OSTI]

    Carcuz Jerez, Juan Ramon de Jesus

    2004-09-30T23:59:59.000Z

    -space models: uncon- solidated shale/sand, shale/salt, gas shale/limestone, and lime- stone/salt [VP : P¡wave velocity; VS : S¡wave velocity; and ½ : density]. : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : 14 2.2 Numerical values... considered in this chapter. The estimated values approximate the actual ones with an error no greater than 1 percent. : : : : : : : : : : : : : : : : : : : : : : : : 26 3.1 Elastic parameters for an isotropic half-space similar to the shale/salt model from...

  15. Foraminiferal and lithologic characteristics through the zone of the Midway-Wilcox contact in Bastrop, Williamson, and Milam counties, Texas

    E-Print Network [OSTI]

    Miller, David Irving

    1962-01-01T23:59:59.000Z

    to deterniae tho sedincntcry parsactors of qccrtilc deviatioa, qaartile shewacss, and qacrtile hartesis. The perceatages of sca, silt, snd clay~ the coefficient of sorting~ sad the ne4isa 4isnetor were nsefal ia iaterpreting the eaviroancatal coaditioas... (1807, p. 62) ia a revised versioa ef the Eoceae ca4 Gretaceoas ef iiabswa. peeress (1050, p. 10?20) aced the ease "Wills peiat" or "Easel Clays" te 4esigaate the Midway Creep ef Texas. Ia the saae pablicatioa, pcarose applied the tera "Tueler Selt...

  16. ERRATA SHEET for ''Lithology and Stratigraphy of Holes Drilled in LANL-Use Areas of the Nevada Test Site''

    SciTech Connect (OSTI)

    L. B. Prothro; S. L. Drellack, Jr.; B. M. Allen

    2001-12-01T23:59:59.000Z

    A conversion error has been discovered in the physical property data table for Emplacement Hole U-19bg (Supplemental Data) presented on Page 89. Data in the column labeled ''Bulk Density (g/cc)'' are actually presented in pounds per cubic foot rather than grams per cubic centimeter. The following table presents the bulk density values for U-19bg in pounds per cubic foot and grams per cubic centimeter.

  17. Lithologic influences on groundwater recharge through incised glacial till from profile to regional scales: Evidence from glaciated Eastern

    E-Print Network [OSTI]

    Szilagyi, Jozsef

    and Jozsef Szilagyi3,4 Received 3 May 2013; revised 11 December 2013; accepted 18 December 2013. [1 of both recharge rates and mechanisms. Citation: Gates, J. B., G. V. Steele, P. Nasta, and J. Szilagyi

  18. An AVO method toward direct detection of lithologies combining P-P and P-S reflection data

    E-Print Network [OSTI]

    Carcuz Jerez, Juan Ramon de Jesus

    2004-09-30T23:59:59.000Z

    -space models: uncon- solidated shale/sand, shale/salt, gas shale/limestone, and lime- stone/salt [VP : P¡wave velocity; VS : S¡wave velocity; and ½ : density]. : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : 14 2.2 Numerical values... considered in this chapter. The estimated values approximate the actual ones with an error no greater than 1 percent. : : : : : : : : : : : : : : : : : : : : : : : : 26 3.1 Elastic parameters for an isotropic half-space similar to the shale/salt model from...

  19. AVA simultaneous inversion of partially stacked seismic amplitude data for the spatial delineation of lithology and fluid units of deepwater

    E-Print Network [OSTI]

    Torres-Verdín, Carlos

    in the world. The field is located in the Block 608 of the Green Canyon area, approximately 280 km south of New manuscript received December 22, 2005; published onlineAugust 7, 2006. 1 Chevron Energy Technology Company

  20. The new prophet : Harold C. Urey, scientist, atheist, and defender of religion

    E-Print Network [OSTI]

    Shindell, Matthew Benjamin

    2011-01-01T23:59:59.000Z

    Geochemistry of Critical Materials and the Development ofGeochemistry of Critical Materials and the Development ofGeochemistry of Critical Materials and the Development of

  1. Fees are subject to change. See studyguide.au.dk *PLACE OF STUDY

    E-Print Network [OSTI]

    geology, sedimentology, climate and palaeoenvironments, hydrogeology, and geochemistry. Teaching focuses

  2. An Appraisal of Underground Radioactive Waste Disposal in Argillaceous and Crystalline Rocks: Some Geochemical, Geomechanical, and Hydrogeological Questions

    E-Print Network [OSTI]

    Apps, J.A.

    2011-01-01T23:59:59.000Z

    fields of geochemistry, geomechanics, and hydrogeology toinvolving geochemistry, geomechanics, and hydrogeology mustto identify those areas in geomechanics, hydrogeo­ logy, and

  3. Geophysical inversion using petrophysical constraints with application to lithology differentiation Jiajia Sun and Yaoguo Li, Center for Gravity, Electrical and Magnetic Studies, Colorado School of Mines

    E-Print Network [OSTI]

    Jiajia Sun and Yaoguo Li, Center for Gravity, Electrical and Magnetic Studies, Colorado School of Mines

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

    SciTech Connect (OSTI)

    Dunn, Thomas L.

    1996-10-01T23:59:59.000Z

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

  5. The lithology, environment of deposition, and reservoir properties of sandstones in the Upper Queen Formation (Guadalupian, Permian) at Concho Bluff Queen Field, Crane County, Texas

    E-Print Network [OSTI]

    Newsom, Douglas Floyd

    1989-01-01T23:59:59.000Z

    and phosphorus in the body. Bauelle Pacific Northwest Laboratories (BPNL) and Bmokhaven National Laboratory (BNL) conducted studies employing in vivo neutron activation analysis to estimate total body calcium 'Ihese studies concluded that calcium content could... that the 2 MeV neutrons produced Ca-49 activity levels approximately 10 times higher than those using 14 Mev neutrons. The lower energy neutmns thexmalized inside the body volume and caused a greater number of Ca-48 atoms to be activated. At BNL, live...

  6. The lithology, environment of deposition, and diagenesis of the Queen Formation at McFarland, McFarland North, and Magutex Queen Fields, Andrews County, Texas

    E-Print Network [OSTI]

    Holley, Carolayne Elizabeth

    1988-01-01T23:59:59.000Z

    of the samples was examined and measured with a petrographic microscope. The detrital and authigenic minerals and visual porosity of 125 thin sections were counted across bedding using the line method, and point-counting proceeded until 100 monocrystalline... quartz grains were counted per section. The detrital grains were classified as monocrystalline quartz, polycrystalline quartz, feldspar, rock fragments, other grains, and matrix. Cements and porosity were also counted. Each component part counted...

  7. Lithologic characteristics, depositional environments and geometries of reservoir and nonreservoir facies in the Queen Formation (Guadalupian, Permian) of Moose and Virey Fields, Midland County, Texas

    E-Print Network [OSTI]

    Aller, Gregory Shane

    1999-01-01T23:59:59.000Z

    30 of township 16 south, range 30 east of Eddy County, New Mexico, penetrates all 1, 710 feet of the Artesia Group. Thicknesses of the formations that make up the Artesia Group at this locality are as follows: Grayburg (360 feet), Queen (420 feet... of the Midland Basin of the larger Permian Basin, just five miles (8 km) east of the Central Basin Platform, and includes portions of sections 10, 15, 21, 22, 27-29, 31-33, and 40-42 of block 41, township 3 south (Figures 2, 5). The maximum distance across...

  8. A linear, temperature compensated, high frequency salinity measuring device

    E-Print Network [OSTI]

    Kelly, Minton Jones

    1951-01-01T23:59:59.000Z

    Bmole tu'oe an% fil. l 8~, 'ith BeraLlry 48re GSB(1 31Tlce tae 81 1ctroL 8 81 818 Could( 18 c(+i '" -2 ui l 11 i ~ '8 p o jt1$'v] v . luce, e' 8& f col &1, lee ir i OE 1 conn::ct'on ie . ". '~B to tho n~: o; ry. . he "1". Oo;&o11 betuesn the l lc 'C'iry...

  9. Surfactant loss: Effects of temperature, salinity, and wettability

    SciTech Connect (OSTI)

    Noll, L.A.; Gall, B.L.; Crocker, M.E.; Olsen, D.K.

    1989-05-01T23:59:59.000Z

    Adsorption of sodium dodecylsulfate, Triton X-100, decyltrimethylammonium bromide surfactants onto silica gel and Berea sandstone mineral surfaces has been studied as a function of temperature, solution salt concentration, and mineral surface wettability. Adsorption studies using a flow calorimeter were conducted using pure surfactants and minerals. The studies were then extended to the adsorption of one type of commercial surfactant onto both consolidated and crushed Berea sandstone using column techniques. This has allowed the comparison of different methods to evaluate surfactant losses from flowing rather than static surfactant solutions. 20 refs., 15 figs., 37 tabs.

  10. METABOLIC RESPONSES TO ENVIRONMENTAL SALINITY IN THE CLAM CORBULA AMURENSIS

    E-Print Network [OSTI]

    VISUALIZATION, MINING, AND ANALYSIS OF TIME- SERIES MICROARRAY EXPERIMENTS By: Ben Dalziel Computer Science: Genevieve K. Walden Ecology and Systematic Biology Faculty Advisor: Dr. Robert Patterson ANALYSIS OF SRAM' GREEN ROOF By: Jessica Van Den Berg and Christopher Quock Ecology and Systematic Biology Faculty Advisor

  11. Formation Damage due to CO2 Sequestration in Saline Aquifers

    E-Print Network [OSTI]

    Mohamed, Ibrahim Mohamed 1984-

    2012-10-25T23:59:59.000Z

    Carbon dioxide (CO2) sequestration is defined as the removal of gas that would be emitted into the atmosphere and its subsequent storage in a safe, sound place. CO2 sequestration in underground formations is currently being considered to reduce...

  12. antarctic saline lakes: Topics by E-print Network

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

    are incorporated in the authigenically formed carbonates, smectites, and micas minerals) and, probably, iron-enriched micas (ferric-illite) in surface and subsurface...

  13. Fluid Dynamics of Carbon Dioxide Disposal into Saline Aquifers

    E-Print Network [OSTI]

    Garcia, Julio Enrique

    2003-01-01T23:59:59.000Z

    natural gas ?a, storage in aquifers in the midwestern U.S states of Illinois and Indiana and salt caverns

  14. -density set by salinity -non-linear equation of state

    E-Print Network [OSTI]

    Washington at Seattle, University of

    Dickson, CEFAS Changes in Arctic Climate are related to the Arctic Oscillation (AO) From D.Thompson, based A CHALLENGE TO MEASURE 80N Greenland Russia Alaska Lom onosov Ridge Mendeleev Ridge Nansen-Gakkel R Eurasian 80N Greenland Russia Alaska Lom onosov Ridge Mendeleev Ridge Nansen-Gakkel R Eurasian Basin Canadian

  15. Gulf stream temperature, salinity and transport during the last millennium

    E-Print Network [OSTI]

    Lund, David Charles

    2006-01-01T23:59:59.000Z

    Benthic and planktonic foraminiferal [delta]18O ([delta 18Oc) from a suite of well-dated, high-resolution cores spanning the depth and width of the Straits of Florida reveal significant changes in Gulf Stream cross-current ...

  16. acute salinity challenges: Topics by E-print Network

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

    challengeS in UnderStanding earth'S dynamic SyStemS January 2009 Long-range Science PLan for SeiSmoLogy WorkSmoLogicaL granD chaLLengeS in unDerStanDing earth'S Dynamic SyStemS...

  17. An Opto-Electric Micropump for Saline Fluids

    E-Print Network [OSTI]

    Reza Kiani Iranpour; Seyyed Nader Rasuli

    2014-05-07T23:59:59.000Z

    A novel method to pump fluid in lab on chip devices with velocities up to tens of micrometer per second is introduced. A focused laser beam locally heats up an electrolyte. A net charge tends to accumulate in the heat-absorbing area, due to unequal tendencies of positive and negative ions to move in the presence of the temperature gradient. An external electric field then exerts a net force on the accumulated charge and consequently on water. This causes flow of water, with velocities up to tens of micrometer per second, for a simple NaCl+water solution. The method lets us change direction and amount of fluid pumping, simply by replacing the focal area.

  18. Flow Instabilities During Injection of CO2 into Saline Aquifers

    E-Print Network [OSTI]

    Garcia, Julio E.; Pruess, Karsten

    2008-01-01T23:59:59.000Z

    processes in oil reservoirs. Petrol. Trans. AIME, Vargaftik,by gas or water drive. Petrol. Trans. AIME, 195:91–98.uid displacement in sands. Petrol. Trans. AIME, x 10 T (s) (

  19. algerian saline steppes: Topics by E-print Network

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

    38 Retreating or Standing: Responses of Forest Species and Steppe Species to Climate Change in Arid Eastern Central Environmental Sciences and Ecology Websites Summary:...

  20. altitude saline wetland: Topics by E-print Network

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

    D. A. Zuwerink; Robert J. Gates 107 Functional Assessment for a Proposed Stormwater Treatment Wetland. Open Access Theses and Dissertations Summary: ??Urbanization can...

  1. Formation Damage due to CO2 Sequestration in Saline Aquifers 

    E-Print Network [OSTI]

    Mohamed, Ibrahim Mohamed 1984-

    2012-10-25T23:59:59.000Z

    the amount of CO2 emitted into the atmosphere. However, a better understanding of the chemical and physical interactions between CO2, water, and formation rock is necessary before sequestration. These interactions can be evaluated by the change in mineral...

  2. Saline County, Arkansas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere IRaghuraji Agro Industries Pvt Ltd Jump to:RoscommonSBY SolutionsChangeOklahoma: Energy708215°, -92.539603°

  3. Saline County, Illinois: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere IRaghuraji Agro Industries Pvt Ltd Jump to:RoscommonSBY SolutionsChangeOklahoma: Energy708215°,

  4. Saline County, Kansas: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere IRaghuraji Agro Industries Pvt Ltd Jump to:RoscommonSBY SolutionsChangeOklahoma: Energy708215°,74853°,

  5. Saline County, Nebraska: Energy Resources | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page onYou are now leaving Energy.gov You are now leaving Energy.gov YouKizildere IRaghuraji Agro Industries Pvt Ltd Jump to:RoscommonSBY SolutionsChangeOklahoma:

  6. co2-saline-storage | netl.doe.gov

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

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level:Energy: Grid Integration Redefining What'sis Taking Over OurThe Iron4 Self-Scrubbing:,, , ., ..., ,+ . :,2013 NETL CO2 Capture

  7. Geothermal well log interpretation state of the art. Final report

    SciTech Connect (OSTI)

    Sanyal, S.K.; Wells, L.E.; Bickham, R.E.

    1980-01-01T23:59:59.000Z

    An in-depth study of the state of the art in Geothermal Well Log Interpretation has been made encompassing case histories, technical papers, computerized literature searches, and actual processing of geothermal wells from New Mexico, Idaho, and California. A classification scheme of geothermal reservoir types was defined which distinguishes fluid phase and temperature, lithology, geologic province, pore geometry, salinity, and fluid chemistry. Major deficiencies of Geothermal Well Log Interpretation are defined and discussed with recommendations of possible solutions or research for solutions. The Geothermal Well Log Interpretation study and report has concentrated primarily on Western US reservoirs. Geopressured geothermal reservoirs are not considered.

  8. Lunar and Planetary Science Conference, 20th, Houston, TX, Mar. 13-17, 1989, Proceedings

    SciTech Connect (OSTI)

    Sharpton, V.L.; Ryder, G.

    1990-01-01T23:59:59.000Z

    Topics discussed include the petrology and geochemistry of the moon, the geology of the moon, lunar regolith processes and resources, the petrology and geochemistry of achondrites, comets and interplanetary dust, shock and terrestrial cratering, the geology of Mars, and the geology of Venus. Papers are presented on silicate liquid immiscibility in isothermal crystallization experiments; highly evolved and ultramafic lithologies from Apollo 14 soils; the relationship between orbital, earth-based, and sample data for lunar landing sites; and the volcanotectonic evolution of Mare Frigoris. Attention is also given to glass variants and multiple HASP trends in Apollo 14 regolith breccias, the characterization of lunar ilmenite resources, the U-Th-Pb systematics of the Estherville mesosiderite, and the extraterrestrial halogen and sulfur contents of the stratosphere. Other papers are on argon-40/argon-39 dating of impact craters; the outliers of dust along the southern margin of the Tharsis region, Mars; and the geology of southern Guinevere Planitia, Venus, based on analyses of Goldstone radar data.

  9. Corrosion-induced gas generation in a nuclear waste repository: Reactive geochemistry and multiphase flow effect

    E-Print Network [OSTI]

    Xu, T.

    2009-01-01T23:59:59.000Z

    conditions. The kinetic rate expression is given in the next6 of 6 2.2. Kinetic Rate Expression Similar to dissolution

  10. Linking Molecular Microbiology and Geochemistry to Better Understand Microbial Ecology in Coastal Marine Sediments

    E-Print Network [OSTI]

    Reese, Brandi Kiel

    2012-02-14T23:59:59.000Z

    The overall objective of the research presented here was to combine multiple geochemical parameters and molecular characterizations to provide a novel view of active microbial community ecology of sediments in a large-river deltaic estuary...

  11. Geochemistry and arsenic behaviour in groundwater resources of the Pannonian Basin (Hungary and Romania)

    E-Print Network [OSTI]

    Wehrli, Bernhard

    and Romania) Helen A.L. Rowland a,d, , Enoma O. Omoregie b , Romain Millot c , Cristina Jimenez d,e , Jasmin Faculty of Environmental Sciences, University of Babes-Bolyai, Cluj Napoca, Romania e Institute handling by R. Fuge a b s t r a c t Groundwater resources in the Pannonian Basin (Hungary, Romania, Croatia

  12. GEOCHEMISTRY AND ISOTOPE HYDROLOGY OF GROUNDWATERS IN THE STRIPA GRANITE RESULTS AND PRELIMINARY INTERPRETATION

    E-Print Network [OSTI]

    Fritz, P.

    2011-01-01T23:59:59.000Z

    the Ca++ and Ba++ chemistry, and uranium solution is redoxchemistry samples collect dissolved gas samples collect uraniumUranium-238 Helium-4 and other noble gases. RESULTS AND DISCUSSION 3.1 Groundwater Chemistry

  13. The distribution and geochemistry of iridium in river suspended material and marine sediments 

    E-Print Network [OSTI]

    Fenner, Frederick Donald

    1983-01-01T23:59:59.000Z

    suggest that Ni, Co and Ir enrichment mechanisms may be similar. Apparent Ir enrichments were found in a mid-Cretaceous shale and a Mediterranean Sea sapropel. It is possible that this Ir precipitated from seawater as a sulfide under reducing... Sapropels and Mid-Cretaceous Marine Black Shales Sources of Iridium The Argument for Iridium Enhancement in the Deep-Sea by Geochemical Processes: Ferromanganese Nodules SUMMARF AND CONCLUSIONS REFERENCES APPENDIX A APPENDIX B APPENDIX C APPENDIX...

  14. Uranium geochemistry in soil and groundwater at the F and H seepage basins

    SciTech Connect (OSTI)

    Serkiz, S.M.; Johnson, W.H.

    1994-09-01T23:59:59.000Z

    For 33 years, low activity liquid wastes from the chemical separation areas at the U.S. Department of Energy`s Savannah River Site were disposed of in unlined seepage basins. Soil and associated pore water samples of widely varying groundwater chemistries and contaminant concentrations were collected from the region downgradient of these basins using cone penetrometer technology. Analysis of samples using inductively coupled plasma - mass spectrometry has allowed the investigation of uranium partitioning between the aqueous phase and soil surfaces at this site. The distribution of uranium was examined with respect to the solution and soil chemistry (e.g., pH, redox potential, cation and contaminant concentration) and aqueous-phase chemical speciation modeling. The uranium soil source term at the F- and H-Area Seepage Basins (FHSB) is much smaller than has been used in previous modeling efforts. This should result in a much shorter remediation time and a greater effectiveness of a pump-and-treat design than previously predicted. Distribution coefficients at the (FHSB) were found to vary between 1.2 to 34,000 1 kg{sup {minus}1} for uranium. Differences in sorption of these elements can be explained primarily by changes in aqueous pH and the associated change in soil surface charge. Sorption models were fit directly to sorption isotherms from field samples. All models underestimated the fraction of uranium bound at low aqueous uranium concentrations. Linear models overestimated bound uranium at locations where the aqueous concentration was greater than 500 ppb. Mechanistic models provided a much better estimate of the bound uranium concentrations, especially at high aqueous concentrations. Since a large fraction of the uranium at the site is associated with the low-pH portion of the plume, consideration should be given to pumping water from the lowest pH portions of the plume in the F-Area.

  15. Geochemistry of deep-sea hydrothermal vent fluids from the Mid-Cayman Rise, Caribbean Sea

    E-Print Network [OSTI]

    McDermott, Jill Marie

    2015-01-01T23:59:59.000Z

    This thesis examines the controls on organic, inorganic, and volatile species distributions in hydrothermal fluids venting at Von Damm and Piccard, two recently discovered vent fields at the ultra slow spreading Mid-Cayman ...

  16. Corrosion-induced gas generation in a nuclear waste repository: Reactive geochemistry and multiphase flow effect

    SciTech Connect (OSTI)

    Xu, T.; Senger, R.; Finsterle, S.

    2008-10-15T23:59:59.000Z

    Corrosion of steel canisters, stored in a repository for spent fuel and high-level nuclear wastes, leads to the generation and accumulation of hydrogen gas in the backfilled emplacement tunnels, which may significantly affect long-term repository safety. Previous studies used H{sub 2} generation rates based on the volume of the waste or canister material and the stoichiometry of the corrosion reaction. However, iron corrosion and H{sub 2} generation rates vary with time, depending on factors such as amount of iron, water availability, water contact area, and aqueous and solid chemistry. To account for these factors and feedback mechanisms, we developed a chemistry model related to iron corrosion, coupled with two-phase (liquid and gas) flow phenomena that are driven by gas-pressure buildup associated with H{sub 2} generation and water consumption. Results indicate that by dynamically calculating H{sub 2} generation rates based on a simple model of corrosion chemistry, and by coupling this corrosion reaction with two-phase flow processes, the degree and extent of gas pressure buildup could be much smaller compared to a model that neglects the coupling between flow and reactive transport mechanisms. By considering the feedback of corrosion chemistry, the gas pressure increases initially at the canister, but later decreases and eventually returns to a stabilized pressure that is slightly higher than the background pressure. The current study focuses on corrosion under anaerobic conditions for which the coupled hydrogeochemical model was used to examine the role of selected physical parameters on the H{sub 2} gas generation and corresponding pressure buildup in a nuclear waste repository. The developed model can be applied to evaluate the effect of water and mineral chemistry of the buffer and host rock on the corrosion reaction for future site-specific studies.

  17. Light hydrocarbon geochemistry of brines and sediments of the red sea

    E-Print Network [OSTI]

    Burke, Roger Allen

    1979-01-01T23:59:59.000Z

    'involved an equi] ibrat. ion pro" e:!urc in conjunctior. with headspace sampling. Although the hot ?stets cooled con & derably from t1&e& r in si. '&, temperatu& e. upon ascent. from the depths, they were. stiJ 1 very warm at the time. of sa?&pl. !. ng... the amount in the head. . pace and water. The primary light hydrocarbon standard. used was an Air Products and Chemica1 s, Inc . cai ibrated standard ga nu xture w 'th 30 pps&v metiaane 0. 3 ppmv ethane snd 6. 2 ppmv propane. Duplicate analyses of methane...

  18. Corrosion-induced gas generation in a nuclear waste repository: Reactive geochemistry and multiphase flow effect

    E-Print Network [OSTI]

    Xu, T.

    2009-01-01T23:59:59.000Z

    Lying Repositories for Nuclear Waste, NAGRA Technical Reporthost rock formation for nuclear waste storage. EngineeringGas Generation in a Nuclear Waste Repository: Reactive

  19. Strontium isotope geochemistry of soil and playa deposits near Yucca Mountain, Nevada

    SciTech Connect (OSTI)

    Marshall, B.D.; Mahan, S.A.

    1994-12-31T23:59:59.000Z

    The isotopic composition of strontium contained in the carbonate fractions of soils provides an excellent tracer which can be used to test models for their origin. This paper reports data on surface coatings and cements, eolian sediments, playas and alluvial fan soils which help to constrain a model for formation of the extensive calcretes and fault infilling in the Yucca Mountain region. The playas contain carbonate with a wide range of strontium compositions; further work will be required to fully understand their possible contributions to the pedogenic carbonate system. Soils from an alluvial fan to the west of Yucca Mountain show that only small amounts of strontium are derived from weathering of silicate detritus. However, calcretes from a fan draining a carbonate terrane have strontium compositions dominated locally by the limestone strontium component. Although much evidence points to an eolian source for at least some of the strontium in the pedogenic carbonates near Yucca Mountain, an additional component or past variation of strontium composition in the eolian source is required to model the pedogenic carbonate system.

  20. Petrology, geochemistry, and palynology of Joggins Formation (Westphalian A) coals, Cumberland basin, Nova Scotia

    SciTech Connect (OSTI)

    Hower, J.C. [Univ. of Kentucky Center for Applied Energy Research, Lexington, KY (United States); Calder, J.H. [Nova Scotia Dept. of Natural Resources, Halifax (Canada); Cortland, F.E. [Kentucky Geological Survey, Lexington, KY (United States)] [and others

    1996-09-01T23:59:59.000Z

    Five Westphalian A coals were collected from the Joggins Formation section exposed along Chignecto Bay at Joggins, Nova Scotia. Several of the coal beds along the bay were mined beginning in the early 17th century. There has been little detailed investigation of the coal beds of this classic section. The lowermost coal, the Upper Coal 29 (Fundy), is a high-vitrinite coal with a spore assemblage dominated by arboreous lycopod spores with tree ferns subdominant. The upper portions of the coal bed have the highest ratio of well-preserved to poorly-preserved telinite of any of the coals investigated. Coal 19 (Forty Brine) has 88% total vitrinite but, unlike the Fundy coal bed, the telinite has a poor preservation ratio and half of the total vitrinite population comprises gelocollinite and vitrodetrinite. The latter coal bed is directly overlain by a basin-wide limestone bed. The Lower Kimberly (Coal 15) shows good preservation of vitrinite with relatively abundant telinite among the total vitrinite. The Upper Kimberly, which underlies the tetrapod-bearing lycopsid trees found by Lyell and Dawson in 1852, exhibits an upward decrease in arboreous lycopod spores and an increase in the tree fern spore Punctatisporites minutus. The megaspore record is similarly dominated by Lagenicularugosa paralycopodites and tree fern spores. Telinite preservation increases upwards in the Upper Kimberly but overall is well below the preservation ratio of the Fundy coal bed. The coals are all high sulfur, up to 13.7% total sulfur for the lower lithotype of the Fundy coal bed. The Kimberly coals are not only high in total and pyritic sulfur, but also have high concentrations of chalcophile elements.

  1. Geochemistry of Natural Components in the Near-Field Environment, Yucca Mountain, Nevada

    SciTech Connect (OSTI)

    Peterman, Zell E. [Yucca Mountain Project Branch, U.S. Geological Survey, MS 963 Box 25046 Denver Federal Center, 6th and Kipling Sts., Denver, CO, 80225 (United States); Oliver, Thomas A. [c/o U.S. Geological Survey, S.M. Stoller Corporation, MS 421 Box 25046 Denver Federal Center, Denver, CO, 80225 (United States)

    2007-07-01T23:59:59.000Z

    The natural near-field environment in and around the emplacement drifts of the proposed nuclear waste repository at Yucca Mountain, Nevada, includes the host rock, dust, seepage, and pore water. The chemical compositions of these components have been determined for assessing possible chemical and mineralogical reactions that may occur after nuclear waste is emplaced. The rock hosting the proposed repository is relatively uniform as shown by a mean coefficient of variation (CV) of 9 percent for major elements. In contrast, compositional variations of dust (bulk and water-soluble fractions), pore water, and seepage are large with mean CVs ranging from 28 to 64 percent. (authors)

  2. Helium and lead isotope geochemistry of oceanic volcanic rocks from the East Pacific and South Atlantic

    E-Print Network [OSTI]

    Graham, David W. (David William)

    1987-01-01T23:59:59.000Z

    The isotopic evolution of helium and lead in the Earth is coupled by virtue of their common radioactive parents uranium and thorium. The isotopic signatures in oceanic volcanic rocks provide constraints on the temporal ...

  3. Results of investigations at the Zunil geothermal field, Guatemala: Well logging and brine geochemistry

    SciTech Connect (OSTI)

    Adams, A.; Dennis, B.; Van Eeckhout, E.; Goff, F.; Lawton, R.; Trujillo, P.E.; Counce, D.; Archuleta, J. (Los Alamos National Lab., NM (USA)); Medina, V. (Instituto Nacional de Electrificacion, Guatemala City (Guatemala). Unidad de Desarollo Geotermico)

    1991-07-01T23:59:59.000Z

    The well logging team from Los Alamos and its counterpart from Central America were tasked to investigate the condition of four producing geothermal wells in the Zunil Geothermal Field. The information obtained would be used to help evaluate the Zunil geothermal reservoir in terms of possible additional drilling and future power plant design. The field activities focused on downhole measurements in four production wells (ZCQ-3, ZCQ-4, ZCQ-5, and ZCQ-6). The teams took measurements of the wells in both static (shut-in) and flowing conditions, using the high-temperature well logging tools developed at Los Alamos National Laboratory. Two well logging missions were conducted in the Zunil field. In October 1988 measurements were made in well ZCQ-3, ZCQ-5, and ZCQ-6. In December 1989 the second field operation logged ZCQ-4 and repeated logs in ZCQ-3. Both field operations included not only well logging but the collecting of numerous fluid samples from both thermal and nonthermal waters. 18 refs., 22 figs., 7 tabs.

  4. Relative chronology of crust formation on asteroid Vesta: Insights from the geochemistry of diogenites

    E-Print Network [OSTI]

    Brest, Université de

    Oce´aniques), I.U.E.M., Place Nicolas Copernic, 29280 Plouzane´ Cedex, France c Antarctic Meteorite (Domaines Oce´aniques), I.U.E.M., Place Nicolas Copernic, 29280 Plouzane´ Cedex, France. Tel.: +33 (0) 2 98

  5. Cost-Effective Cementitious Material Compatible with Yucca Mountain Repository Geochemistry

    SciTech Connect (OSTI)

    Dole, LR

    2004-12-17T23:59:59.000Z

    The current plans for the Yucca Mountain (YM) repository project (YMP) use steel structures to stabilize the disposal drifts and connecting tunnels that are collectively over 100 kilometers in length. The potential exist to reduce the underground construction cost by 100s of millions of dollars and improve the repository's performance. These economic and engineering goals can be achieved by using the appropriate cementitious materials to build out these tunnels. This report describes the required properties of YM compatible cements and reviews the literature that proves the efficacy of this approach. This report also describes a comprehensive program to develop and test materials for a suite of underground construction technologies.

  6. Fe isotope and trace element geochemistry of the Neoproterozoic syn-glacial Rapitan iron formation

    E-Print Network [OSTI]

    Long, Bernard

    pattern likely records a steep isotopic gradient across the iron chemocline in Rapitan seawater. © 2011 metabolism, and function as a micronu- trient (Anbar, 2004; Beard et al., 2003a; Johnson et al., 2008a). Iron

  7. Effects of pore-scale physics on uranium geochemistry in Hanford sediments

    SciTech Connect (OSTI)

    Hu, Qinhong; Ewing, Robert P.

    2013-11-25T23:59:59.000Z

    Overall, this work examines a key scientific issue, mass transfer limitations at the pore-scale, using both new instruments with high spatial resolution, and new conceptual and modeling paradigms. The complementary laboratory and numerical approaches connect pore-scale physics to macroscopic measurements, providing a previously elusive scale integration. This Exploratory research project produced five peer-reviewed journal publications and eleven scientific presentations. This work provides new scientific understanding, allowing the DOE to better incorporate coupled physical and chemical processes into decision making for environmental remediation and long-term stewardship.

  8. 4Reviews in Mineralogy & Geochemistry Vol. 72 pp. 107-170, 2010

    E-Print Network [OSTI]

    Zhang, Youxue

    diffusion in glasses, and laser-ablation inductively coupled mass spectrometry (LA-ICPMS), which is being

  9. Introduction Introduction to a Special Issue on Geochemistry of Chalcophile and Siderophile

    E-Print Network [OSTI]

    to laser ablation methods, which has led to a number of studies on the CSE contents of individual rock PGMs. Two papers address this issue. Pagé et al. present in situ laser ablation inductively- coupled roughly equal distribution between the oxide phases. Another innovative use of laser ablation techniques

  10. Trace-element geochemistry of gradient hole cuttings: Beowawe geothermal area, Nevada

    SciTech Connect (OSTI)

    Christensen, O.D.

    1980-12-01T23:59:59.000Z

    Multielement geochemical analysis of drill cuttings from 26 shallow temperature-gradient drill holes and of surface rock samples reveals trace element distributions developed within these rocks as a consequence of chemical interaction with thermal fluid within the Beowawe geothermal area. The presently discharging thermal fluids are dilute in all components except silica, suggesting that the residence time of these fluids within the thermal reservoir has been short and that chemical interaction with the reservoir rock minimal. Interaction between these dilute fluids and rocks within the system has resulted in the development of weak chemical signatures. The absence of stronger signatures in rocks associated with the present system suggests that fluids have had a similar dilute chemistry for some time. The spatial distribution of elements commonly associated with geothermal systems, such as As, Hg and Li, and neither laterally nor vertically continuous. This suggests that there is not now, nor has there been in the past, pervasive movement of thermal fluid throughout the sampled rock but, instead, that isolated chemical anomalies represent distinct fluid-flow chanels. Discontinuous As, Li and Hg concentrations near White Canyon to the east of the presently active surface features record the effects of chemical interaction of rocks with fluids chemically unlike the presently discharging fluids. The observed trace element distributions suggest that historically the Beowawe area has been the center of more than one hydrothermal event and that the near-surface portion of the present hot-water geothermal system is controlled by a single source fracture, the Malpais Fault, or an intersection of faults at the sinter terrace.

  11. GEOCHEMISTRY AND ISOTOPE HYDROLOGY OF GROUNDWATERS IN THE STRIPA GRANITE RESULTS AND PRELIMINARY INTERPRETATION

    E-Print Network [OSTI]

    Fritz, P.

    2011-01-01T23:59:59.000Z

    GROUNDWATERS IN THE STRIPA GRANITE ReSULTS AND PRELIMINARYG~UUNDWATERS IN THE STRIPA GRANITE K~SULTS AND PRELIMINARYPermeability Test of the Granite in the Stripa Mine and

  12. doi:10.1016/j.gca.2004.07.010 Geochemistry of a chert breccia

    E-Print Network [OSTI]

    Yehoshua, Kolodny

    12, 2004) Abstract--A complex history of diagenetic interactions between a siliceous sediment are carried by apatite, trapped as detritus in the matrix. The concentration of lithium in the matrix is high

  13. The biostratigraphy, palaeoecology and geochemistry of a long lacustrine sequence from NW Greece

    E-Print Network [OSTI]

    Frogley, Michael Reginald

    acquired an important profile in recent years. We have gradually become aware through issues such as global warming that human impact upon the environment can have far ranging consequences. By gaining clearer insights into the mechanisms that drove... acquired an important profile in recent years. We have gradually become aware through issues such as global warming that human impact upon the environment can have far ranging consequences. By gaining clearer insights into the mechanisms that drove...

  14. Geochemistry of volcanic rocks from the Geysers geothermal area, California Coast Ranges

    E-Print Network [OSTI]

    source of geothermal energy, is ulti- 0024-4937/$ - see front matter D 2005 Published by Elsevier BGeochemistry of volcanic rocks from the Geysers geothermal area, California Coast Ranges Axel K Potsdam, Germany c Philippine Geothermal, Inc., Makati, Philippines Received 1 May 2004; accepted 25 May

  15. Evolution of porosity and geochemistry in Marcellus Formation black shale during weathering

    SciTech Connect (OSTI)

    Jin, Lixin [University of Texas at El Paso] [University of Texas at El Paso; Ryan, Mathur [Juniata College, Huntingdon] [Juniata College, Huntingdon; Rother, Gernot [ORNL] [ORNL; Cole, David [Ohio State University] [Ohio State University; Bazilevskaya, Ekaterina [Pennsylvania State University, University Park, PA] [Pennsylvania State University, University Park, PA; Williams, Jennifer [Pennsylvania State University] [Pennsylvania State University; Alex, Carone [Pennsylvania State University] [Pennsylvania State University; Brantley, S. L. [Pennsylvania State University, University Park, PA] [Pennsylvania State University, University Park, PA

    2013-01-01T23:59:59.000Z

    Soils developed on the Oatka Creek member of the Marcellus Formation in Huntingdon, Pennsylvania were analyzed to understand the evolution of black shale matrix porosity and the associated changes in elemental and mineralogical composition during infiltration of water into organic-rich shale. Making the reasonable assumption that soil erosion rates are the same as those measured in a nearby location on a less organic-rich shale, we suggest that soil production rates have on average been faster for this black shale compared to the gray shale in similar climate settings. This difference is attributed to differences in composition: both shales are dominantly quartz, illite, and chlorite, but the Oatka Creek member at this location has more organic matter (1.25 wt.% organic carbon in rock fragments recovered from the bottom of the auger cores and nearby outcrops) and accessory pyrite. During weathering, the extremely low-porosity bedrock slowly disaggregates into shale chips with intergranular pores and fractures. Some of these pores are eitherfilled with organic matter or air-filled but remain unconnected, and thus inaccessible to water. Based on weathering bedrock/soil profiles, disintegration is initiated with oxidation of pyrite and organic matter, which increases the overall porosity and most importantly allows water penetration. Water infiltration exposes fresh surface area and thus promotes dissolution of plagioclase and clays. As these dissolution reactions proceed, the porosity in the deepest shale chips recovered from the soil decrease from 9 to 7% while kaolinite and Fe oxyhydroxides precipitate. Eventually, near the land surface, mineral precipitation is outcompeted by dissolution or particle loss of illite and chlorite and porosity in shale chips increases to 20%. As imaged by computed tomographic analysis, weathering causes i) greater porosity, ii) greater average length of connected pores, and iii) a more branched pore network compared to the unweathered sample. This work highlights the impact of shale water O2interactions in near-surface environments: (1) black shale weathering is important for global carbon cycles as previously buried organic matter is quickly oxidized; and (2) black shales weather more quickly than less organic- and sulfide-rich shales, leading to high porosity and mineral surface areas exposed for clay weathering. The fast rates of shale gas exploitation that are ongoing in Pennsylvania, Texas and other regions in the United States may furthermore lead to release of metals to the environment if reactions between water and black shale are accelerated by gas development activities in the subsurface just as they are by low-temperature processes in ourfield study.

  16. Geology, volcanology and geochemistry Drainage pattern and regional morphostructure at Melka Kunture (Upper Awash, Ethiopia) ........................83

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    at Melka Kunture (Upper Awash, Ethiopia) ........................83 Guillaume Bardin, Jean-Paul Raynal, Guy Kieffer Volcanic markers in coarse alluvium at Melka Kunture (Upper Awash, Ethiopia (Upper Awash, Ethiopia) ....................................................103 Gérard Poupeau, Guy

  17. Trace element geochemistry of ordinary chondrite chondrules: the type I/type II chondrule dichotomy

    E-Print Network [OSTI]

    Jacquet, Emmanuel; Gounelle, Matthieu

    2015-01-01T23:59:59.000Z

    We report trace element concentrations of silicate phases in chondrules from LL3 ordinary chondrites Bishunpur and Semarkona. Results are similar to previously reported data for carbonaceous chondrites, with rare earth element (REE) concentrations increasing in the sequence olivine ~ 10 K/h) than type I chondrules. Appreciable Na concentrations (3-221 ppm) are measured in olivine from both chondrule types; type II chondrules seem to have behaved as closed systems, which may require chondrule formation in the vicinity of protoplanets or planetesimals. At any rate, higher solid concentrations in type II chondrule forming regions may explain the higher oxygen fugacities they record compared to type I chondrules. Type I and type II chondrules formed in different environments and the correlation between high solid concentrations and/or oxygen fugacities with rapid cooling rates is a key constraint that chondrule formation models must account for.

  18. The Role of Geochemistry and Stress on Fracture Development and Proppant Behavior in EGS Reservoirs

    Broader source: Energy.gov [DOE]

    Project objective: Develop Improved Methods For Maintaining Permeable Fracture Volumes In EGS Reservoirs.

  19. Geochemistry of the Yegua Aquifer system and its relation to microbial processes

    E-Print Network [OSTI]

    Schlichenmeyer, Jeannette Leone

    1996-01-01T23:59:59.000Z

    in southwestern North Dakota and northwestern South Dakota They noted a decrease in sulfate and an increase in HS- along the hydrologic flow path. In a study of the Black Creek aquifer in South Carolina, Chapelle and McMahon (1991) found evidence that sulfate... in South Carolina, Fredrickson et aL (1991) found higher viable counts in the coarse sands of the Middendorf formation than in the fine sands of the Cape Fear formation, or in lignites and lignite-sands. Also, at the Savannah River Site higher numbers...

  20. Aqueous geochemistry of the Thermopolis hydrothermal system, southern Bighorn Basin, Wyoming, U.S.A.

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

    Kaszuba, John P. [University of Wyoming; Sims, Kenneth W.W. [University of Wyoming; Pluda, Allison R.

    2014-03-01T23:59:59.000Z

    The Thermopolis hydrothermal system is located in the southern portion of the Bighorn Basin, in and around the town of Thermopolis, Wyoming. It is the largest hydrothermal system in Wyoming outside of Yellowstone National Park. The system includes hot springs, travertine deposits, and thermal wells; published models for the hydrothermal system propose the Owl Creek Mountains as the recharge zone, simple conductive heating at depth, and resurfacing of thermal waters up the Thermopolis Anticline.

  1. An investigation of the geology and geochemistry of radon in shear zones

    SciTech Connect (OSTI)

    Schumann, R.R.; Stanton, M.R.; Gundersen, L.C.S. [Geological Survey, Denver, CO (United States); Gates, A.E. [Rutgers--the State Univ., Newark, NJ (United States). Dept. of Geology; Schultz, A.P. [Geological Survey, Reston, VA (United States); Speer, J.A. [North Carolina Univ., Raleigh, NC (United States). Dept. of Marine, Earth and Atmospheric Sciences

    1991-12-31T23:59:59.000Z

    In this study we will characterize the four principal geologic terrains that cause the highest and most extensive indoor radon problems in the United States, we will predict their national distribution, and we will define the climatic and chemical processes that affect uranium and radium siting in rocks and soils, and ultimately their emanation and radon potential. We have chosen nine sheared granite plutons from different climatic areas across the United States, two faulted carbonate terrains from an and area and a humid area, and three sites within the fractured Pierre shale and the glacial deposits derived from it in the northern Great Plains. The results of our studies for the last four years have established that in order to understand and accurately predict radon transport and availability in rocks, soils, and ground water, the factors affecting radon emanation must be quantitatively described and basic models developed to understand the processes involved. Three phases of the project were worked on this (1) Preliminary assessment of the Alleghenian granites and compilation of data for establishing the relation between heat flow and radon production and availability, (2) development of a field emanation protocol, and (3) ongoing geochemical examination of shear zone processes.

  2. Petrology and Geochemistry of Neoproterozoic Arc Plutons Beneath the Atlantic Coastal Plain, SRS, SC

    SciTech Connect (OSTI)

    Maryak, M.

    1998-10-21T23:59:59.000Z

    In this report is presented first a brief review of the regional geologic setting of the Savannah River Site, descriptions of the plutonic rock units sampled here, whole rock geochemical data on the plutonic igneous rocks, and finally, a discussion of how the crystalline basement rocks of the Savannah River Site formed and how they may correlate with other terranes exposed in the Piedmont of the Carolinas, Georgia, and Virginia.

  3. Geochemistry of silicate-rich rocks can curtail spreading of carbon dioxide in subsurface aquifers

    E-Print Network [OSTI]

    Cardoso, S. S. S.; Andres, J. T. H.

    2014-12-11T23:59:59.000Z

    of carbon sequestration and dissolution rates in the subsurface, suggesting that pooled carbon dioxide may remain in the shallower regions of the formation for hundreds to thousands of years. The deeper regions of the reservoir can remain virtually carbon... interests. References 1. Marini, L. Geochemical Sequestration of Carbon Dioxide. (Elsevier 2007). 2. IPCC Special Report on Carbon Dioxide Capture and Storage, edited by Metz B. et al. (Cambridge University Press, UK and New York, USA, 2005). 3. Falkowski...

  4. 7Reviews in Mineralogy & Geochemistry Vol. 68, pp. 93-140, 2008

    E-Print Network [OSTI]

    Grossman, Lawrence

    to the compositions of coexisting Ti3+ -bearing fassaitic clinopyroxene + melilite pairs in natural inclusions shows temperatures where diffusion of Fe2+ becomes very slow. Two dynamic models for enrichment of oxygen relative to carbon and hydrogen were investigated quantitatively: radial transport of water ice-rich migrators across

  5. The marine geochemistry of dissolved gallium: A comparison with dissolved aluminum

    SciTech Connect (OSTI)

    Orians, K.J.; Bruland, K.W. (Univ. of California, Santa Cruz (USA))

    1988-12-01T23:59:59.000Z

    Dissolved Ga concentrations in the pacific Ocean range from 2 to 30 picomolar: they are low in surface waters (2-12 pM), with a subsurface maximum at 150-300 m (6-17 pM), a mid-depth minimum from 500 to 1,000 m (4-10 pM) and increasing values with depth to a maximum in the bottom waters (12-30 pM). The highest concentrations are in the central gyre, with lower values toward the north and east where productivity and particle scavenging increase. Dissolved Ga concentrations in the surface waters of the northwest Atlantic are nearly an order of magnitude higher than in the central North pacific, with higher values in the Gulf Stream than in the continental slope boundary region. The vertical distributions and horizontal transects indicate three sources of dissolved Ga to the oceans. The surface distribution reflects an eolian source with no net fluvial input to the open ocean; the subsurface maximum (a feature not seen for North Pacific dissolved Al) is attributed to vertical exchange processes; the source for the deep waters of the North Pacific is from a sediment surface remineralization process or a pore water flux. Scavenging removal throughout the water column is evident in the vertical profiles for both dissolved Ga and Al, with intensified removal in the boundary regions where productivity and particle scavenging are at a maximum. Residence times of dissolved Ga in surface waters are nearly an order of magnitude longer than the corresponding values for Al.

  6. GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS, VOL. ???, XXXX, DOI:10.1029/, Crustal and upper mantle structure beneath1

    E-Print Network [OSTI]

    Boyer, Edmond

    of Southampton, Southampton, U.K. 8 Yemen Geological Survey and mineral Resources Board, Sana'a, Yemen. 9 Sana] and how it is connected with global mantle flow [e.g.30 Montelli et al., 2006; Boschi et al., 2007, 2008

  7. Detrital geochronology and geochemistry of CretaceousEarly Miocene strata of Nepal: implications for timing and

    E-Print Network [OSTI]

    Najman, Yani

    rocks has traditionally relied upon petrographic data sets from sandstones [1]. In regions where source of northern Pakistan and India as Early to Middle Eocene (~52 Ma). Eocene strata in the Tethyan portion of the central part of the Himalayan orogenic belt consist of shallow marine carbonate rocks that lack evidence

  8. Mineralogy and Geochemistry of Pb, Zn and Ag Mine Tailings Originating From Carbonate-Rich Deposits

    E-Print Network [OSTI]

    McClure, Roberta 1981-

    2012-11-29T23:59:59.000Z

    at many acid mine drainage sites around the world, environmental problems related to mining activities in the Zimapan study site include acid mine drainage, and heavy metal and arsenic contamination of surface and ground water. Arsenicosis, or arsenic... toxicity, is common in people who reside in the Zimapan area due to high concentrations of arsenic in the public water supply (Armienta et al., 1996). Many studies have been conducted to determine sources and sinks for As contamination. Mining...

  9. Corrosion-induced gas generation in a nuclear waste repository: Reactive geochemistry and multiphase flow effect

    E-Print Network [OSTI]

    Xu, T.

    2009-01-01T23:59:59.000Z

    L.W. 1982. Factors affecting the corrosion of metals inatmosphere, Atmospheric Corrosion, Ed. W.H. Ailov, New York.P. , Minet, Y. 2007. Iron corrosion in Callovo–Oxfordian

  10. The geochemistry and petrogenesis of the Tertiary igneous rocks of the Eagle Mountains, Van Horn, Texas

    E-Print Network [OSTI]

    Nelson, Ronald Alan

    1972-01-01T23:59:59.000Z

    Alkaline Ign ~ ~ cons ~ ~ ~ Rocks 21 42 D I S CUSS I QN e ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ Petrogenesis 50 50 Source magma. Fractionation . ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 50 52 Origin of West Texas Nagmas... of Permian and Cretaceous age. The only Permian rocks in the area are represented by the Hueco Limestone Formation. The Cretaceous System, however, is represented by the entire Comanche and Gulf Series (Fig. 2). The Hueco Formation is of marine origin...

  11. The distribution and geochemistry of iridium in river suspended material and marine sediments

    E-Print Network [OSTI]

    Fenner, Frederick Donald

    1983-01-01T23:59:59.000Z

    Sapropels and Mid-Cretaceous Marine Black Shales Sources of Iridium The Argument for Iridium Enhancement in the Deep-Sea by Geochemical Processes: Ferromanganese Nodules SUMMARF AND CONCLUSIONS REFERENCES APPENDIX A APPENDIX B APPENDIX C APPENDIX... Samples weighing from 0. 1 to 0. 5 grams were accurately weighed into 2/5 dram attached cap polyethlylene vials and sealed. Standards consisting of USGS standard rocks GSP-1 and AGV-1 and an in-house standar- dized marine sediment were prepared...

  12. 12Reviews in Mineralogy & Geochemistry Vol. 70 pp. 533-569, 2009

    E-Print Network [OSTI]

    Zhu, Chen

    issues for which chemical reaction kinetics play a significant role; these include carbon sequestration contamination. Let's take carbon sequestration as an example. Geological carbon sequestration--the injection to geological carbon sequestration involves the accurate prediction of reaction kinetics among CO2, brine

  13. Geochemistry of formation waters from the Lower Silurian Clinton Formation (Albion Sandstone), eastern Ohio

    SciTech Connect (OSTI)

    Sanders, L.L. (Illinois Univ., Chicago (United States))

    1991-10-01T23:59:59.000Z

    Waters of the petroleum-bearing Clinton formation (Albion Sandstone) of eastern Ohio are highly concentrated brines with average total dissolved solids (TDS) of 250,000 ppm. Sodium, calcium, and chloride account for 97% of the TDS. Distribution of divalent metal chlorides (MCl{sub 2}) allows inference of an up-dip paleoflow direction, although present-day flow is probably down-dip paleoflow direction, although present-day flow is probably down-dip. Solute distribution may have been emplaced during early basin development; it thus provides a snapshot of paleoflow. Formation structure alone can not explain MCl{sub 2} trends; they probably also are controlled by regional variation in salt thickness. Major constituent data do not indicate that membrane filtration affected the waters. High bromide content (mean = 1,860 ppm) of the water indicates that they originated from evaporating seawater. They probably are related genetically to the Salina evaporite group. Calculations show that several subsequent diagenetic reactions can account for the observed major ion composition. Recrystallization of aragonite and dolomitization of calcite probably occurred as the waters moved through the big Lime and/or the Packer Shell carbonates. Cation exchange and chlorite formation probably altered water composition during interaction with shales of the Cabot Head formation and within the Clinton. Minor constituents of the waters appear to be controlled by reactions with clays.

  14. Implications of formation water movement based on isotopic data and elemental geochemistry, southwestern Ontario

    SciTech Connect (OSTI)

    Frape, S.K.; Dollar, P.; Fritz, P.; Travail, R.A.; McNutt, R.H.; MacQueen, R.W.

    1986-08-01T23:59:59.000Z

    Formation waters in Paleozoic sediments analyzed for /sup 2/H, /sup 18/O, /sup 87/Sr//sup 86/Sr, tritium, and major/minor contents show the following. (1) The stable isotope contents are typical for formation brines, but have /sup 18/O and /sup 2/H values that group according to formation age, with waters in Cambrian strata being most depleted; and the most concentrated brines do not compare well to known Michigan basin brines. Many waters are Ca-Na-Cl brines similar to typical Canadian shield brines, although the origin of the various chemical species may be masked by intense rock-water interaction. (2) The /sup 87/Sr//sup 86/Sr values for Cambrian brines range from 0.7095 to 0.7102. In one detailed study, the brine and calcite cement had the same value (0.7095), which is slightly higher than Cambrian seawater (0.7091-0.7092), and indicates that the cement precipitated from the brine during diagenesis. The reservoir rock has a /sup 87/Sr//sup 86/Sr value of 0.7330, indicating little or no water/rock exchange. Sr isotopic values for Ordovician brines range from 0.7095 to 0.7103, which is higher than Ordovician seawater (0.7085). In contrast, the Silurian Salina Formation brines and Silurian seawater values are the same (0.7085-0.7087). Despite an active tectonic history, causing considerable faulting and movement within Paleozoic and Precambrian rock strata, the isotopic results for the Cambrian indicate isotopic equilibrium between brine and cement; therefore, these formation waters have not moved since the calcite formed.

  15. Geochemistry of selected oils and rocks from the central portion of the West Siberian basin, Russia

    SciTech Connect (OSTI)

    Peters, K.E.; Huizinga, B.J. (Chevron Overseas Petroleum Inc., San Ramon, CA (United States)); Kontorovich, A.Eh.; Andrusevich, V.E. (Inst. of Geology, Novosibirsk (Russian Federation)); Moldowan, J.M. (Chevron Petroleum Technology Co., Richmond, CA (United States)); Demaison, G.J. (Petroscience Inc., Walnut Creek, CA (United States)); Stasova, O.F. (NPO SIBGEO, Novosibirsk (Russian Federation))

    1993-05-01T23:59:59.000Z

    Six analyzed oils, produced from Middle jurassic to Upper Cretaceous strata in the Middle Ob region of the West Siberian basin, show biomarker and stable carbon isotope compositions indicating an origin from the Upper Jurassic Bazhenov Formation. The chemical compositions of these oils are representative of more than 85% of the reserves in West Siberia (Kontorovich et al., 1975). Bazhenov-sourced oil in Cenomanian strata in the Van-Egan field underwent biodegradation in the reservoir, resulting in a low API gravity, an altered homohopane distribution, and the appearance of 25-norhopanes without alteration of the steranes. High API gravity oil from the Salym field has surpassed the peak of the oil window, consistent with abnormally high temperatures and pressures in the Bazhenov source rock from which it is produced. The remaining oils are very similar, including samples from Valanginian and Bathonian-Callovian intervals in a sequence of stacked reservoirs in the Fedorov field. Bazhenov rock samples from the study area contain abundant oil-prone, marine organic matter preserved under anoxic conditions. While the Upper Jurassic Vasyugan Formation shows lower oil-regenerative potential than the Bazhenov Formation, it cannot be excluded as a source rock because insufficient sample was available for biomarker analysis. Core from the Lower to Middle Jurassic Tyumen Formation in the YemYegov 15 well was compared with the oils because it is thermally mature and shows TOC and HI values, indicating slightly more favorable oil-generative characteristics than the average for the formation (2.75 wt. % for 270 samples; 95 mg HC/g TOC for 25 samples). The core contains terrigenous, gas-prone organic matter that shows no relationship with the analyzed oils. 59 refs., 15 figs., 8 tabs.

  16. GEOCHEMISTRY OF PARTICULATE AND DISSOLVED INORGANIC CARBON IN THE CENTRAL NORTH PACIFIC

    E-Print Network [OSTI]

    Luther, Douglas S.

    -carbonate system of the open ocean is still not completely understood today. This investigation incorporated both for 15 months at the Hawaii Ocean Time-series station, ALOHA, was predominantly controlled waters are a very small sink for anthropogenic CO2, this CO2 has penetrated to a depth of 700 m

  17. Uranium Geochemistry in Vadose Zone and Aquifer Sediments from the 300 Area Uranium Plume

    SciTech Connect (OSTI)

    Zachara, John M.; Davis, Jim A.; Liu, Chongxuan; McKinley, James P.; Qafoku, Nik; Wellman, Dawn M.; Yabusaki, Steven B.

    2005-07-21T23:59:59.000Z

    This report documents research conducted by the RCS Project to update the record of decision for the 300-FF-5 Operable Unit on the Hanford Site.

  18. PART II, Tackling Grand Challenges in Geochemistry: Q&A with...

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

    for scientific research and industrial development, and HFIR is a powerful reactor-based source. We use these in a couple of ways. One way (at HFIR) relies on the fact that...

  19. Radiocarbon and stable isotope geochemistry of organic matter in the Amazon headwaters, Peruvian Andes

    E-Print Network [OSTI]

    McClain, Michael

    (such as resuspension or photosynthesis) may control riverine POM composition as opposed to terrestrial consistency in the geochemical composition of organic matter (OM) in the Amazon, leading to the conclusion

  20. m)T7(T^/f^\\ \\ / Riso-R-430 The Geochemistry

    E-Print Network [OSTI]

    -LEVEL HASTE 22 Uranium 31 Neptunium 35 Plutonium 38 Americium 41 CHEMISTRY OF TECHNETIUM 44 ADSORPTION, stability-diagrams for the transuranium elements from uranium to americium under diverse conditions have GROUNDWATER COMPOSITIONS 7 COMPLEX CHEMISTRY 12 CRITICAL ANION CONCENTRATION IN GROUND WATERS 17 THE CHEMISTRY