D. Kirk Nordstrom (Former Employee)
Science and Products
Filter Total Items: 164
Aqueous pyrite oxidation by dissolved oxygen and by ferric iron Aqueous pyrite oxidation by dissolved oxygen and by ferric iron
Rates of aqueous, abiotic pyrite oxidation were measured in oxygen-saturated and anaerobic Fe(III)-saturated solutions with initial pH from 2 to 9. These studies included analyses of sulfite, thiosulfate, polythionates and sulfate and procedures for cleaning oxidation products from pyrite surfaces were evaluated. Pyrite oxidation in oxygen-saturated solutions produced (1) rates that were...
Authors
Carl O. Moses, D. Kirk Nordstrom, Janet S. Herman, Aaron L. Mills
WATEQ4F - a personal computer Fortran translation of the geochemical model WATEQ2 with revised data base WATEQ4F - a personal computer Fortran translation of the geochemical model WATEQ2 with revised data base
A FORTRAN 77 version of the PL/1 computer program for the geochemical model WATEQ2, which computes major and trace element speciation and mineral saturation for natural waters has been developed. The code (WATEQ4F) has been adapted to execute on an IBM PC or compatible microcomputer. Two versions of the code are available, one operating with IBM Professional FORTRAN and an 8087 or 89287...
Authors
J.W. Ball, D. Kirk Nordstrom, D.W. Zachmann
Interaction of acid mine drainage with waters and sediments of West Squaw Creek in the West Shasta Mining District, California Interaction of acid mine drainage with waters and sediments of West Squaw Creek in the West Shasta Mining District, California
Acid mine drainage has acidified large volumes of water and added high concentrations of dissolved heavy metals to West Squaw Creek, a California stream draining igneous rocks of low acid-neutralizing capacity. During mixing of the acid sulfate stream waters in the South Fork of West Squaw Creek with an almost equal volume of dilute uncontaminated water, Cu, Zn, Mn, and Al remained in...
Authors
L.H. Filipek, D. Kirk Nordstrom, W. H. Ficklin
Solubility and stability of scorodite, FeAsO4.2H2O: Discussion Solubility and stability of scorodite, FeAsO4.2H2O: Discussion
Reported solubility data for a synthetic scorodite and the techniques used to prepare the synthetic phase are questioned. (A.M. 70-838, 72-852)-J.A.Z.
Authors
D. Kirk Nordstrom, George A. Parks
The geochemical behavior of aluminum in acidified surface waters The geochemical behavior of aluminum in acidified surface waters
Speciation calculations for aluminum, in water samples taken from a drainage basin containing acid mine waters, demonstrate a distinct transition from conservative behavior for pH. below 4.6 to nonconservative behavior for pH. above 4.9. This transition corresponds to the pK for the first hydrolysis constant of the aqueous aluminum ion and appears to be a consistent phenomenon...
Authors
D. Kirk Nordstrom, J.W. Ball
Major and trace-element analyses of acid mine waters in the Leviathan Mine drainage basin, California/Nevada; October, 1981 to October, 1982 Major and trace-element analyses of acid mine waters in the Leviathan Mine drainage basin, California/Nevada; October, 1981 to October, 1982
Water issuing from the inactive Leviathan open-pit sulfur mine has caused serious degradation of the water quality in the Leviathan/Bryant Creek drainage basin which drains into the East Fork of the Carson River. As part of a pollution abatement project of the California Regional Water Quality Control Board, the U.S. Geological Survey collected hydrologic and water quality data for the...
Authors
J.W. Ball, D. Kirk Nordstrom
Science and Products
Filter Total Items: 164
Aqueous pyrite oxidation by dissolved oxygen and by ferric iron Aqueous pyrite oxidation by dissolved oxygen and by ferric iron
Rates of aqueous, abiotic pyrite oxidation were measured in oxygen-saturated and anaerobic Fe(III)-saturated solutions with initial pH from 2 to 9. These studies included analyses of sulfite, thiosulfate, polythionates and sulfate and procedures for cleaning oxidation products from pyrite surfaces were evaluated. Pyrite oxidation in oxygen-saturated solutions produced (1) rates that were...
Authors
Carl O. Moses, D. Kirk Nordstrom, Janet S. Herman, Aaron L. Mills
WATEQ4F - a personal computer Fortran translation of the geochemical model WATEQ2 with revised data base WATEQ4F - a personal computer Fortran translation of the geochemical model WATEQ2 with revised data base
A FORTRAN 77 version of the PL/1 computer program for the geochemical model WATEQ2, which computes major and trace element speciation and mineral saturation for natural waters has been developed. The code (WATEQ4F) has been adapted to execute on an IBM PC or compatible microcomputer. Two versions of the code are available, one operating with IBM Professional FORTRAN and an 8087 or 89287...
Authors
J.W. Ball, D. Kirk Nordstrom, D.W. Zachmann
Interaction of acid mine drainage with waters and sediments of West Squaw Creek in the West Shasta Mining District, California Interaction of acid mine drainage with waters and sediments of West Squaw Creek in the West Shasta Mining District, California
Acid mine drainage has acidified large volumes of water and added high concentrations of dissolved heavy metals to West Squaw Creek, a California stream draining igneous rocks of low acid-neutralizing capacity. During mixing of the acid sulfate stream waters in the South Fork of West Squaw Creek with an almost equal volume of dilute uncontaminated water, Cu, Zn, Mn, and Al remained in...
Authors
L.H. Filipek, D. Kirk Nordstrom, W. H. Ficklin
Solubility and stability of scorodite, FeAsO4.2H2O: Discussion Solubility and stability of scorodite, FeAsO4.2H2O: Discussion
Reported solubility data for a synthetic scorodite and the techniques used to prepare the synthetic phase are questioned. (A.M. 70-838, 72-852)-J.A.Z.
Authors
D. Kirk Nordstrom, George A. Parks
The geochemical behavior of aluminum in acidified surface waters The geochemical behavior of aluminum in acidified surface waters
Speciation calculations for aluminum, in water samples taken from a drainage basin containing acid mine waters, demonstrate a distinct transition from conservative behavior for pH. below 4.6 to nonconservative behavior for pH. above 4.9. This transition corresponds to the pK for the first hydrolysis constant of the aqueous aluminum ion and appears to be a consistent phenomenon...
Authors
D. Kirk Nordstrom, J.W. Ball
Major and trace-element analyses of acid mine waters in the Leviathan Mine drainage basin, California/Nevada; October, 1981 to October, 1982 Major and trace-element analyses of acid mine waters in the Leviathan Mine drainage basin, California/Nevada; October, 1981 to October, 1982
Water issuing from the inactive Leviathan open-pit sulfur mine has caused serious degradation of the water quality in the Leviathan/Bryant Creek drainage basin which drains into the East Fork of the Carson River. As part of a pollution abatement project of the California Regional Water Quality Control Board, the U.S. Geological Survey collected hydrologic and water quality data for the...
Authors
J.W. Ball, D. Kirk Nordstrom
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