D. Kirk Nordstrom (Former Employee)
Science and Products
Filter Total Items: 164
The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California
Jarosite-group minerals accumulate in the form of stalactites and fine-grained mud on massive pyrite in the D drift of the Richmond mine, Iron Mountain, California. Water samples were collected by placing beakers under the dripping stalactites and by extracting pore water from the mud using a centrifuge. The water is rich in Fe3+ and SO4 2−, with a pH of approximately 2.1, which is...
Authors
Heather E. Jamieson, Clare Robinson, Charles N. Alpers, D. Kirk Nordstrom, Alexei Poustovetov, Heather A. Lowers
Major and trace element composition of copiapite-group minerals and coexisting water from the Richmond mine, Iron Mountain, California Major and trace element composition of copiapite-group minerals and coexisting water from the Richmond mine, Iron Mountain, California
Copiapite-group minerals of the general formula AR4(SO4)6(OH)2·nH2O, where A is predominantly Mg, Fe2+, or 0.67Al3+, R is predominantly Fe3+, and n is typically 20, are among several secondary hydrous Fe sulfates occurring in the inactive mine workings of the massive sulfide deposit at Iron Mountain, CA, a USEPA Superfund site that produces extremely acidic drainage. Samples of copiapite...
Authors
H.E. Jamieson, C. Robinson, Charles N. Alpers, R. Blaine McCleskey, D. Kirk Nordstrom, Ronald C. Peterson
Aqueous stability of gadolinium in surface waters receiving sewage treatment plant effluent Boulder Creek, Colorado Aqueous stability of gadolinium in surface waters receiving sewage treatment plant effluent Boulder Creek, Colorado
In many surface waters, sewage treatment plant (STP) effluent is a substantial source of both regulated and unregulated contaminants, including a suite of complex organic compounds derived from household chemicals, pharmaceutical, and industrial and medical byproducts. In addition, STP effluents in some urban areas have also been shown to have a positive gadolinium (Gd) anomaly in the...
Authors
P. L. Verplanck, Howard E. Taylor, D. Kirk Nordstrom, L. B. Barber
Nitrogen transformations in hot spring runoff, Yellowstone National Park, WY Nitrogen transformations in hot spring runoff, Yellowstone National Park, WY
No abstract available.
Authors
JoAnn M. Holloway, D. Kirk Nordstrom, R. L. Smith
Questa baseline and pre-mining ground-water quality investigation 4. Historical surface-water quality for the Red River Valley, New Mexico, 1965 to 2001 Questa baseline and pre-mining ground-water quality investigation 4. Historical surface-water quality for the Red River Valley, New Mexico, 1965 to 2001
Historical water-quality samples collected from the Red River over the past 35 years were compiled, reviewed for quality, and evaluated to determine influences on water quality over time. Hydrologic conditions in the Red River were found to have a major effect on water quality. The lowest sulfate concentrations were associated with the highest flow events, especially peak, rising limb...
Authors
Ann S. Maest, D. Kirk Nordstrom, Sara H. LoVetere
Evaluating remedial alternatives for the Alamosa River and Wightman Fork, near Summitville Mine, Colorado: Application of a reactive transport model to low- and high-flow simulations Evaluating remedial alternatives for the Alamosa River and Wightman Fork, near Summitville Mine, Colorado: Application of a reactive transport model to low- and high-flow simulations
Reactive-transport processes in Wightman Fork and the Alamosa River downstream from the Summitville Mine, south-central Colorado, were simulated at low and high flow using the OTEQ reactive-transport model. The simulations were calibrated using data from synoptic studies conducted during October 1998 and June 1999. Discharge over the 30-km reach from just below the mine site to the...
Authors
J.W. Ball, R.L. Runkel, D. Kirk Nordstrom
Science and Products
Filter Total Items: 164
The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California
Jarosite-group minerals accumulate in the form of stalactites and fine-grained mud on massive pyrite in the D drift of the Richmond mine, Iron Mountain, California. Water samples were collected by placing beakers under the dripping stalactites and by extracting pore water from the mud using a centrifuge. The water is rich in Fe3+ and SO4 2−, with a pH of approximately 2.1, which is...
Authors
Heather E. Jamieson, Clare Robinson, Charles N. Alpers, D. Kirk Nordstrom, Alexei Poustovetov, Heather A. Lowers
Major and trace element composition of copiapite-group minerals and coexisting water from the Richmond mine, Iron Mountain, California Major and trace element composition of copiapite-group minerals and coexisting water from the Richmond mine, Iron Mountain, California
Copiapite-group minerals of the general formula AR4(SO4)6(OH)2·nH2O, where A is predominantly Mg, Fe2+, or 0.67Al3+, R is predominantly Fe3+, and n is typically 20, are among several secondary hydrous Fe sulfates occurring in the inactive mine workings of the massive sulfide deposit at Iron Mountain, CA, a USEPA Superfund site that produces extremely acidic drainage. Samples of copiapite...
Authors
H.E. Jamieson, C. Robinson, Charles N. Alpers, R. Blaine McCleskey, D. Kirk Nordstrom, Ronald C. Peterson
Aqueous stability of gadolinium in surface waters receiving sewage treatment plant effluent Boulder Creek, Colorado Aqueous stability of gadolinium in surface waters receiving sewage treatment plant effluent Boulder Creek, Colorado
In many surface waters, sewage treatment plant (STP) effluent is a substantial source of both regulated and unregulated contaminants, including a suite of complex organic compounds derived from household chemicals, pharmaceutical, and industrial and medical byproducts. In addition, STP effluents in some urban areas have also been shown to have a positive gadolinium (Gd) anomaly in the...
Authors
P. L. Verplanck, Howard E. Taylor, D. Kirk Nordstrom, L. B. Barber
Nitrogen transformations in hot spring runoff, Yellowstone National Park, WY Nitrogen transformations in hot spring runoff, Yellowstone National Park, WY
No abstract available.
Authors
JoAnn M. Holloway, D. Kirk Nordstrom, R. L. Smith
Questa baseline and pre-mining ground-water quality investigation 4. Historical surface-water quality for the Red River Valley, New Mexico, 1965 to 2001 Questa baseline and pre-mining ground-water quality investigation 4. Historical surface-water quality for the Red River Valley, New Mexico, 1965 to 2001
Historical water-quality samples collected from the Red River over the past 35 years were compiled, reviewed for quality, and evaluated to determine influences on water quality over time. Hydrologic conditions in the Red River were found to have a major effect on water quality. The lowest sulfate concentrations were associated with the highest flow events, especially peak, rising limb...
Authors
Ann S. Maest, D. Kirk Nordstrom, Sara H. LoVetere
Evaluating remedial alternatives for the Alamosa River and Wightman Fork, near Summitville Mine, Colorado: Application of a reactive transport model to low- and high-flow simulations Evaluating remedial alternatives for the Alamosa River and Wightman Fork, near Summitville Mine, Colorado: Application of a reactive transport model to low- and high-flow simulations
Reactive-transport processes in Wightman Fork and the Alamosa River downstream from the Summitville Mine, south-central Colorado, were simulated at low and high flow using the OTEQ reactive-transport model. The simulations were calibrated using data from synoptic studies conducted during October 1998 and June 1999. Discharge over the 30-km reach from just below the mine site to the...
Authors
J.W. Ball, R.L. Runkel, D. Kirk Nordstrom
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government