James Thordsen
James Thordsen is a Geologist for the USGS Water Resources Mission Area.
Science and Products
Filter Total Items: 15
Chemical composition of formation water in shale and tight reservoirs: A basin-scale perspective
No abstract available.
Authors
Yousif Kharaka, Kathleen Gans, Elisabeth Rowan, James Thordsen, Christopher H. Conaway, Madalyn S. Blondes, Mark A. Engle
Temperature-dependent variations in mineralogy, major element chemistry and the stable isotopes of boron, lithium and chlorine resulting from hydration of rhyolite glass: Constraints from hydrothermal experiments at 150 to 350°C and 25 MPa
Rhyolite-hosted hydrothermal systems in the continental crust contain valuable energy and mineral resources that make them of special interest across several scientific disciplines. Despite extensive research on these systems, the temperature-dependence of chemical reactions between host rocks and aqueous-rich fluids and the mineralogical transformations resulting from these reactions are not well
Authors
Jeffery T. Cullen, Shaul Hurwitz, Jaime D. Barnes, John C. Lassiter, Sarah Penniston-Dorland, Simone Kasemann, James Thordsen
Geochemical data for produced waters from conventional and unconventional oil and gas wells: Results from Colorado, USA
Geochemical data for more than 120,000 oil and natural gas wells from the major sedimentary basins in the USA are listed in the USGS National Produced Waters Geochemical Database [1]. In this summary, we report and discuss the geochemical data on produced waters obtained from published literature and the Colorado Oil and Gas Conservation Commission (COGCC) from close to 4,000 new oil and gas wells
Authors
Yousif Kharaka, Kathleen Gans, James Thordsen, Madalyn S. Blondes, Mark A Engle
Changes in the Chemistry of Groundwater Reacted with CO2: Comparison of Laboratory Results with the ZERT Field Pilot
As part of the ZERT program, sediments from two wells at the ZERT site, located in Bozeman, Montana, USA were reacted with a solution having the composition of local groundwater. A total of 50 water samples were collected from 7 containers placed for 15 days in a glove box with one atmosphere of CO2 to investigate detailed changes in the concentrations of major, minor and trace inorganic compounds
Authors
Yousif K. Kharaka, James J. Thordsen, Atosa A. Abedini, Sarah Beers, Burt Thomas
Comparison of geochemical data obtained using four brine sampling methods at the SECARB Phase III Anthropogenic Test CO2 injection site, Citronelle Oil Field, Alabama
The chemical composition of formation water and associated gases from the lower Cretaceous Paluxy Formation was determined using four different sampling methods at a characterization well in the Citronelle Oil Field, Alabama, as part of the Southeast Regional Carbon Sequestration Partnership (SECARB) Phase III Anthropogenic Test, which is an integrated carbon capture and storage project. In this s
Authors
Christopher Conaway, James J. Thordsen, Michael A. Manning, Paul J. Cook, Robert C. Trautz, Burt Thomas, Yousif K. Kharaka
Carbon isotope analysis of dissolved organic carbon in fresh and saline (NaCl) water via continuous flow cavity ring-down spectroscopy following wet chemical oxidation
This work examines the performance and limitations of a wet chemical oxidation carbon analyser interfaced with a cavity ring-down spectrometer (WCO-CRDS) in a continuous flow (CF) configuration for measuring δ13C of dissolved organic carbon (δ13C-DOC) in natural water samples. Low-chloride matrix (<5 g Cl/L) DOC solutions were analysed with as little as 2.5 mg C/L in a 9 mL aliquot with a precisio
Authors
Christopher Conaway, Randal B. Thomas, Nabil Saad, James J. Thordsen, Yousif K. Kharaka
The energy-water nexus: Potential groundwater-quality degradation associated with production of shale gas
Oil and natural gas have been the main sources of primary energy in the USA, providing 63% of the total energy consumption in 2011. Petroleum production, drilling operations, and improperly sealed abandoned wells have caused significant local groundwater contamination in many states, including at the USGS OSPER sites in Oklahoma. The potential for groundwater contamination is higher when producing
Authors
Yousif K. Kharaka, James J. Thordsen, Christopher H. Conaway, Randal B. Thomas
CO2–rock–brine interactions in Lower Tuscaloosa Formation at Cranfield CO2 sequestration site, Mississippi, U.S.A.
A highly integrated geochemical program was conducted at the Cranfield CO2-enhanced oil recovery (EOR) and sequestration site, Mississippi, U.S.A.. The program included extensive field geochemical monitoring, a detailed petrographic study, and an autoclave experiment under in situ reservoir conditions. Results show that mineral reactions in the Lower Tuscaloosa reservoir were minor during CO2 inje
Authors
Jiemin Lu, Yousif K. Kharaka, James J. Thordsen, Juske Horita, Athanasios Karamalidis, Craig Griffith, J. Alexandra Hakala, Gil Ambats, David R. Cole, Tommy J. Phelps, Michael A. Manning, Paul J. Cook, Susan D. Hovorka
Transient changes in shallow groundwater chemistry during the MSU ZERT CO2 injection experiment
Food-grade CO2 was injected into a shallow aquifer through a perforated pipe placed horizontally 1–2 m below the water table at the Montana State University Zero Emission Research and Technology (MSU-ZERT) field site at Bozeman, Montana. The possible impact of elevated CO2 levels on groundwater quality was investigated by analyzing 80 water samples taken before, during, and following CO2 injection
Authors
J. A. Apps, Lingyun Zheng, N. Spycher, J.T. Birkholzer, Yousif K. Kharaka, James J. Thordsen, Evangelos Kakouros, R. Trautz
Potential environmental issues of CO2 storage in deep saline aquifers: Geochemical results from the Frio-I Brine Pilot test, Texas, USA
Sedimentary basins in general, and deep saline aquifers in particular, are being investigated as possible repositories for large volumes of anthropogenic CO2 that must be sequestered to mitigate global warming and related climate changes. To investigate the potential for the long-term storage of CO2 in such aquifers, 1600 t of CO2 were injected at 1500 m depth into a 24-m-thick "C" sandstone unit
Authors
Yousif K. Kharaka, James J. Thordsen, Susan D. Hovorka, H. Seay Nance, David R. Cole, Tommy J. Phelps, Kevin G. Knauss
Geochemical data from produced water contamination investigations: Osage-Skiatook Petroleum Environmental Research (OSPER) sites, Osage County, Oklahoma
We report chemical and isotopic analyses of 345 water samples collected from the Osage-Skiatook Petroleum Environmental Research (OSPER) project. Water samples were collected as part of an ongoing multi-year USGS investigation to study the transport, fate, natural attenuation, and ecosystem impacts of inorganic salts and organic compounds present in produced water releases at two oil and gas produ
Authors
James J. Thordsen, Yousif K. Kharaka, Gil Ambats, Evangelos Kakouros, Marvin M. Abbott
Hydrology and subsurface transport of oil-field brine at the U.S. Geological Survey OSPER site "A", Osage County, Oklahoma
Spillage and improper disposal of saline produced water from oil wells has caused environmental damage at thousands of sites in the United States. In order to improve understanding of the fate and transport of contaminants at these sites, the U.S. Geological Survey carried out multidisciplinary investigations at two oil production sites near Skiatook Lake, Oklahoma. As a part of this effort, the h
Authors
William N. Herkelrath, Yousif K. Kharaka, James J. Thordsen, Marvin M. Abbott
Science and Products
Filter Total Items: 15
Chemical composition of formation water in shale and tight reservoirs: A basin-scale perspective
No abstract available.
Authors
Yousif Kharaka, Kathleen Gans, Elisabeth Rowan, James Thordsen, Christopher H. Conaway, Madalyn S. Blondes, Mark A. Engle
Temperature-dependent variations in mineralogy, major element chemistry and the stable isotopes of boron, lithium and chlorine resulting from hydration of rhyolite glass: Constraints from hydrothermal experiments at 150 to 350°C and 25 MPa
Rhyolite-hosted hydrothermal systems in the continental crust contain valuable energy and mineral resources that make them of special interest across several scientific disciplines. Despite extensive research on these systems, the temperature-dependence of chemical reactions between host rocks and aqueous-rich fluids and the mineralogical transformations resulting from these reactions are not well
Authors
Jeffery T. Cullen, Shaul Hurwitz, Jaime D. Barnes, John C. Lassiter, Sarah Penniston-Dorland, Simone Kasemann, James Thordsen
Geochemical data for produced waters from conventional and unconventional oil and gas wells: Results from Colorado, USA
Geochemical data for more than 120,000 oil and natural gas wells from the major sedimentary basins in the USA are listed in the USGS National Produced Waters Geochemical Database [1]. In this summary, we report and discuss the geochemical data on produced waters obtained from published literature and the Colorado Oil and Gas Conservation Commission (COGCC) from close to 4,000 new oil and gas wells
Authors
Yousif Kharaka, Kathleen Gans, James Thordsen, Madalyn S. Blondes, Mark A Engle
Changes in the Chemistry of Groundwater Reacted with CO2: Comparison of Laboratory Results with the ZERT Field Pilot
As part of the ZERT program, sediments from two wells at the ZERT site, located in Bozeman, Montana, USA were reacted with a solution having the composition of local groundwater. A total of 50 water samples were collected from 7 containers placed for 15 days in a glove box with one atmosphere of CO2 to investigate detailed changes in the concentrations of major, minor and trace inorganic compounds
Authors
Yousif K. Kharaka, James J. Thordsen, Atosa A. Abedini, Sarah Beers, Burt Thomas
Comparison of geochemical data obtained using four brine sampling methods at the SECARB Phase III Anthropogenic Test CO2 injection site, Citronelle Oil Field, Alabama
The chemical composition of formation water and associated gases from the lower Cretaceous Paluxy Formation was determined using four different sampling methods at a characterization well in the Citronelle Oil Field, Alabama, as part of the Southeast Regional Carbon Sequestration Partnership (SECARB) Phase III Anthropogenic Test, which is an integrated carbon capture and storage project. In this s
Authors
Christopher Conaway, James J. Thordsen, Michael A. Manning, Paul J. Cook, Robert C. Trautz, Burt Thomas, Yousif K. Kharaka
Carbon isotope analysis of dissolved organic carbon in fresh and saline (NaCl) water via continuous flow cavity ring-down spectroscopy following wet chemical oxidation
This work examines the performance and limitations of a wet chemical oxidation carbon analyser interfaced with a cavity ring-down spectrometer (WCO-CRDS) in a continuous flow (CF) configuration for measuring δ13C of dissolved organic carbon (δ13C-DOC) in natural water samples. Low-chloride matrix (<5 g Cl/L) DOC solutions were analysed with as little as 2.5 mg C/L in a 9 mL aliquot with a precisio
Authors
Christopher Conaway, Randal B. Thomas, Nabil Saad, James J. Thordsen, Yousif K. Kharaka
The energy-water nexus: Potential groundwater-quality degradation associated with production of shale gas
Oil and natural gas have been the main sources of primary energy in the USA, providing 63% of the total energy consumption in 2011. Petroleum production, drilling operations, and improperly sealed abandoned wells have caused significant local groundwater contamination in many states, including at the USGS OSPER sites in Oklahoma. The potential for groundwater contamination is higher when producing
Authors
Yousif K. Kharaka, James J. Thordsen, Christopher H. Conaway, Randal B. Thomas
CO2–rock–brine interactions in Lower Tuscaloosa Formation at Cranfield CO2 sequestration site, Mississippi, U.S.A.
A highly integrated geochemical program was conducted at the Cranfield CO2-enhanced oil recovery (EOR) and sequestration site, Mississippi, U.S.A.. The program included extensive field geochemical monitoring, a detailed petrographic study, and an autoclave experiment under in situ reservoir conditions. Results show that mineral reactions in the Lower Tuscaloosa reservoir were minor during CO2 inje
Authors
Jiemin Lu, Yousif K. Kharaka, James J. Thordsen, Juske Horita, Athanasios Karamalidis, Craig Griffith, J. Alexandra Hakala, Gil Ambats, David R. Cole, Tommy J. Phelps, Michael A. Manning, Paul J. Cook, Susan D. Hovorka
Transient changes in shallow groundwater chemistry during the MSU ZERT CO2 injection experiment
Food-grade CO2 was injected into a shallow aquifer through a perforated pipe placed horizontally 1–2 m below the water table at the Montana State University Zero Emission Research and Technology (MSU-ZERT) field site at Bozeman, Montana. The possible impact of elevated CO2 levels on groundwater quality was investigated by analyzing 80 water samples taken before, during, and following CO2 injection
Authors
J. A. Apps, Lingyun Zheng, N. Spycher, J.T. Birkholzer, Yousif K. Kharaka, James J. Thordsen, Evangelos Kakouros, R. Trautz
Potential environmental issues of CO2 storage in deep saline aquifers: Geochemical results from the Frio-I Brine Pilot test, Texas, USA
Sedimentary basins in general, and deep saline aquifers in particular, are being investigated as possible repositories for large volumes of anthropogenic CO2 that must be sequestered to mitigate global warming and related climate changes. To investigate the potential for the long-term storage of CO2 in such aquifers, 1600 t of CO2 were injected at 1500 m depth into a 24-m-thick "C" sandstone unit
Authors
Yousif K. Kharaka, James J. Thordsen, Susan D. Hovorka, H. Seay Nance, David R. Cole, Tommy J. Phelps, Kevin G. Knauss
Geochemical data from produced water contamination investigations: Osage-Skiatook Petroleum Environmental Research (OSPER) sites, Osage County, Oklahoma
We report chemical and isotopic analyses of 345 water samples collected from the Osage-Skiatook Petroleum Environmental Research (OSPER) project. Water samples were collected as part of an ongoing multi-year USGS investigation to study the transport, fate, natural attenuation, and ecosystem impacts of inorganic salts and organic compounds present in produced water releases at two oil and gas produ
Authors
James J. Thordsen, Yousif K. Kharaka, Gil Ambats, Evangelos Kakouros, Marvin M. Abbott
Hydrology and subsurface transport of oil-field brine at the U.S. Geological Survey OSPER site "A", Osage County, Oklahoma
Spillage and improper disposal of saline produced water from oil wells has caused environmental damage at thousands of sites in the United States. In order to improve understanding of the fate and transport of contaminants at these sites, the U.S. Geological Survey carried out multidisciplinary investigations at two oil production sites near Skiatook Lake, Oklahoma. As a part of this effort, the h
Authors
William N. Herkelrath, Yousif K. Kharaka, James J. Thordsen, Marvin M. Abbott