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Publications

Dive into our publications and explore the science from the Environmental Health Program (Toxic Substances Hydrology and Contaminant Biology).

Filter Total Items: 3784

Oxidation of aromatic contaminants coupled to microbial iron reduction Oxidation of aromatic contaminants coupled to microbial iron reduction

THE contamination of sub-surface water supplies with aromatic compounds is a significant environmental concern1,2. As these contaminated sub-surface environments are generally anaerobic, the microbial oxidation of aromatic compounds coupled to nitrate reduction, sulphate reduction and methane production has been studied intensively1-7. In addition, geochemical evidence suggests that Fe...
Authors
Derek R. Lovley, M.J. Baedecker, D.J. Lonergan, I.M. Cozzarelli, Elizabeth J.P. Phillips, D. I. Siegel

Requirement for a microbial consortium to completely oxidize glucose in Fe(III)- reducing sediments Requirement for a microbial consortium to completely oxidize glucose in Fe(III)- reducing sediments

In various sediments in which Fe(III) reduction was the terminal electron-accepting process, [14C]glucose was fermented to 14C-fatty acids in a manner similar to that observed in methanogenic sediments. These results are consistent with the hypothesis that, in Fe(III)-reducing sediments, fermentable substrates are oxidized to carbon dioxide by the combined activity of fermentative...
Authors
Derek R. Lovley, Elizabeth J.P. Phillips

Simulation of calcite dissolution and porosity changes in saltwater mixing zones in coastal aquifers Simulation of calcite dissolution and porosity changes in saltwater mixing zones in coastal aquifers

Thermodynamic models of aqueous solutions have indicated that the mixing of seawater and calcite-saturated fresh groundwater can produce a water that is undersaturated with respect to calcite. Mixing of such waters in coastal carbonate aquifers could lead to significant amounts of limestone dissolution. The potential for such dissolution in coastal saltwater mixing zones is analyzed by...
Authors
Ward E. Sanford, Leonard F. Konikow

Convergent radial dispersion: A Laplace transform solution for aquifer tracer testing Convergent radial dispersion: A Laplace transform solution for aquifer tracer testing

A Laplace transform solution was obtained for the injection of a tracer in a well situated in a homogeneous aquifer where steady, horizontal, radially convergent flow has been established due to pumping at a second well. The standard advection-dispersion equation for mass transfer was used as the controlling equation. For boundary conditions, mass balances that account for mixing of the...
Authors
Allen F. Moench

Transport of microspheres and indigenous bacteria through a sandy aquifer: Results of natural- and forced-gradient tracer experiments Transport of microspheres and indigenous bacteria through a sandy aquifer: Results of natural- and forced-gradient tracer experiments

Transport of indigenous bacteria through sandy aquifer sediments was investigated in forced- and natural-gradient tracer teste. A diverse population of bacteria was collected and concentrated from groundwater at the site, stained with a DNA-specific fluorochrome, and injected back into the aquifer. Included with the injectate were a conservative tracer (Br- or Cl-) and bacteria-sized (0...
Authors
R.W. Harvey, L.H. George, R. L. Smith, D.R. LeBlanc

Organic markers as source discriminants and sediment transport indicators in south San Francisco Bay, California Organic markers as source discriminants and sediment transport indicators in south San Francisco Bay, California

Sediment samples from nearshore sites in south San Francisco Bay and from streams flowing into that section of the Bay have been characterized in terms of their content of biogenic and anthropogenic molecular marker compounds. The distributions, input sources, and applicability of these compounds in determining sediment movement are discussed. By means of inspection and multivariate...
Authors
F. D. Hostettler, J. B. Rapp, K.A. Kvenvolden, N L. Samuel

Solubility of jarosite solid solutions precipitated from acid mine waters, Iron Mountain, California Solubility of jarosite solid solutions precipitated from acid mine waters, Iron Mountain, California

Because of the common occurrence of 15 to 25 mole percent hydronium substitution on the alkali site in jarosites, it is necessary to consider the hydronium content of jarosites in any attempt at rigorous evaluation of jarosite solubility or of the saturation state of natural waters with respect to jarosite. A Gibbs free energy of 3293.5±2.1 kJ mol-1 is recommended for a jarosite solid...
Authors
Charles N. Alpers, D. Kirk Nordstrom, J.W. Ball

Modification of a method-of-characteristics solute-transport model to incorporate decay and equilibrium-controlled sorption or ion exchange Modification of a method-of-characteristics solute-transport model to incorporate decay and equilibrium-controlled sorption or ion exchange

The U.S. Geological Survey computer model of two-dimensional solute transport and dispersion in ground water (Konikow and Bredehoeft, 1978) has been modified to incorporate the following types of chemical reactions: (1) first-order irreversible rate-reaction, such as radioactive decay; (2) reversible equilibrium-controlled sorption with linear, Freundlich, or Langmuir isotherms; and (3)...
Authors
D.J. Goode, Leonard F. Konikow

Physical and chemical characteristics of a metal-contaminated overbank deposit, west-central South Dakota, USA Physical and chemical characteristics of a metal-contaminated overbank deposit, west-central South Dakota, USA

The deposit along the Belle Fourche River is typically up to 2 m thick and extends about 90 m away from the channel along the insides of meander bends. The sediments contain above-background levels of copper, iron, manganese, zinc, and particularly arsenic. An influx at high streamflow of uncontaminated sediment from terraces and the premining floodplain as well as from tributaries...
Authors
D. C. Marron

Chemical hydrogeology in natural and contaminated environments Chemical hydrogeology in natural and contaminated environments

Chemical hydrogeology, including organic and inorganic aspects, has contributed to an increased understanding of groundwater flow systems, geologic processes, and stressed environments. Most of the basic principles of inorganic-chemical hydrogeology were first established by investigations of organic-free, regional-scale systems for which simplifying assumptions could be made. The...
Authors
W. Back, M.J. Baedecker

Coprecipitation and redox reactions of manganese oxides with copper and nickel Coprecipitation and redox reactions of manganese oxides with copper and nickel

Open-system, continuous-titration experiments have been done in which a slow flux of ∼0.02 molar solution of Mn2+ chloride, nitrate, or perchlorate with Cu2+ or Ni2+ in lesser concentrations was introduced into an aerated reactor solution held at constant temperature and at constant pH by a pH-stat titrator that added dilute NaOH. The resulting mixtures of metal oxyhydroxides and their...
Authors
J.D. Hem, Carol J. Lind, C. E. Roberson
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