Publications
Dive into our publications and explore the science from the Environmental Health Program (Toxic Substances Hydrology and Contaminant Biology).
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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
Volatilization of ethylene dibromide from water Volatilization of ethylene dibromide from water
Overall mass-transfer coefficients for the volatilization of ethylene dibromide from water were measured simultaneously with the oxygen absorption coefficient in a laboratory stirred tank. Coefficients were measured as a function of mixing conditions in the water for two windspeeds. The ethylene dibromide mass-transfer coefficient depended on windspeed; the ethylene dibromide liquid-film
Authors
R. E. Rathbun, D. Y. Tai
Thermodynamics of aragonite-strontianite solid solutions: Results from stoichiometric solubility at 25 and 76°C Thermodynamics of aragonite-strontianite solid solutions: Results from stoichiometric solubility at 25 and 76°C
Dissolution of synthetic strontianite-aragonite solid solutions was followed analytically to stoichiometric saturation using large solid to solution ratios in CO2-H2O solution at 25 and 76°C. The compositional dependence of the equilibrium constant was calculated from the composition of saturated (stoichiometric) solutions and used to calculate the activities and activity coefficients of...
Authors
Niel Plummer, E. Busenberg
Stable isotope dilution analysis of hydrologic samples by inductively coupled plasma mass spectrometry Stable isotope dilution analysis of hydrologic samples by inductively coupled plasma mass spectrometry
Inductively coupled plasma mass spectrometry is employed in the determination of Ni, Cu, Sr, Cd, Ba, Ti, and Pb in nonsaline, natural water samples by stable isotope dilution analysis. Hydrologic samples were directly analyzed without any unusual pretreatment. Interference effects related to overlapping isobars, formation of metal oxide and multiply charged ions, and matrix composition...
Authors
John R. Garbarino, Howard E. Taylor
Playa-lake basins on the Southern High Plains of Texas and New Mexico: Part I. Hydrologic, geomorphic, and geologic evidence for their development Playa-lake basins on the Southern High Plains of Texas and New Mexico: Part I. Hydrologic, geomorphic, and geologic evidence for their development
Playa-lake basins of the Southern High Plains, Texas and New Mexico, may originate wherever water periodically can collect in a surficial depression. They expand, however, by hydrologic and geomorphic processes including (1) dissolution of lithologic carbonates by infiltrating water; (2) transport downward of fine-grained clastic and organic material by the infiltrating ground water...
Authors
Waite Osterkamp, W.W. Wood
Transport of reacting solutes subject to a moving dissolution boundary: Numerical methods and solutions Transport of reacting solutes subject to a moving dissolution boundary: Numerical methods and solutions
A moving boundary problem which arises during transport with precipitation-dissolution reactions is solved by three different numerical methods. Two of these methods (one explicit and one implicit) are based on an integral formulation of mass balance and lead to an approximation of a weak solution. These methods are compared to a front-tracking scheme. Although the two approaches are...
Authors
Catherine Willis, Jacob Rubin
Chemical reactions simulated by ground-water-quality models Chemical reactions simulated by ground-water-quality models
Recent literature concerning the modeling of chemical reactions during transport in ground water is examined with emphasis on sorption reactions. The theory of transport and reactions in porous media has been well documented. Numerous equations have been developed from this theory, to provide both continuous and sequential or multistep models, with the water phase considered for both...
Authors
David B. Grove, Kenneth G. Stollenwerk
Sources and flux of natural gases from Mono Lake, California Sources and flux of natural gases from Mono Lake, California
The ability to identify a formation mechanism for natural gas in a particular environment requires consideration of several geochemical factors when there are multiple sources present. Four primary sources of methane have been identified in Mono Lake. Two of these sources were associated with numerous natural gas seeps which occur at various locations in the lake and extend beyond its...
Authors
Ronald S. Oremland, L.G. Miller, Michael J. Whiticar
Crude oil identification with electrothermal vaporization-multiple wavelength absorption spectrometry Crude oil identification with electrothermal vaporization-multiple wavelength absorption spectrometry
A spectrometric technique utilizing electrothermal vaporization (graphite furnace) and gas phase-multiple wavelength absorption with photodiode array detection is used to characterize crude oil.
Authors
J.M. Shekiro, R. K Skogerboe, Howard E. Taylor
A study of metal ion adsorption at low suspended-solid concentrations A study of metal ion adsorption at low suspended-solid concentrations
A procedure for conducting adsorption studies at low suspended solid concentrations in natural waters (
Authors
Cecily C.Y. Chang, J.A. Davis, James S. Kuwabara
Reduction of selenate to selenide by sulfate-respiring bacteria: Experiments with cell suspensions and estuarine sediments Reduction of selenate to selenide by sulfate-respiring bacteria: Experiments with cell suspensions and estuarine sediments
Washed cell suspensions of Desulfovibrio desulfuricans subsp. aestuarii were capable of reducing nanomolar levels of selenate to selenide as well as sulfate to sulfide. Reduction of these species was inhibited by 1 mM selenate or tungstate. The addition of 1 mM sulfate decreased the reduction of selenate and enhanced the reduction of sulfate. Increasing concentrations of sulfate...
Authors
J.P. Zehr, Ronald S. Oremland
Processes and kinetics of Cd2+ sorption by a calcareous aquifer sand Processes and kinetics of Cd2+ sorption by a calcareous aquifer sand
The rate of Cd2+ sorption by a calcareous aquifer sand was characterized by two reaction steps, with the first step reaching completion in 24 hours. The second step proceeded at a slow and nearly constant rate for at least seven days. The first step includes a fast adsorption reaction which is followed by diffusive transport into either a disordered surface film of hydrated calcium...
Authors
C. C. Fuller, J.A. Davis