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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: 3785

Part 1: Vadose-zone column studies of toluene (enhanced bioremediation) in a shallow unconfined aquifer Part 1: Vadose-zone column studies of toluene (enhanced bioremediation) in a shallow unconfined aquifer

The objectives of the laboratory study described in this paper were (1) to determine the effectiveness of four nutrient solutions and a control in stimulating the microbial degradation of toluene in the unsaturated zone as an alternative to bioremediation methodologies such as air sparging, in situ vitrification, or others (Part I), and (2) to compare the effectiveness of the addition of...
Authors
J.A. Tindall, M.J. Friedel, R.J. Szmajter, S.M. Cuffin

CO2 dynamics in the Amargosa Desert: Fluxes and isotopic speciation in a deep unsaturated zone CO2 dynamics in the Amargosa Desert: Fluxes and isotopic speciation in a deep unsaturated zone

Natural unsaturated-zone gas profiles at the U.S. Geological Survey's Amargosa Desert Research Site, near Beatty, Nevada, reveal the presence of two physically and isotopically distinct CO2 sources, one shallow and one deep. The shallow source derives from seasonally variable autotrophic and heterotrophic respiration in the root zone. Scanning electron micrograph results indicate that at...
Authors
Michelle Ann Walvoord, Robert G. Striegl, David E. Prudic, David A. Stonestrom

Three-dimensional variable-density flow simulation of a coastal aquifer in southern Oahu, Hawaii, USA Three-dimensional variable-density flow simulation of a coastal aquifer in southern Oahu, Hawaii, USA

Three-dimensional modeling of groundwater flow and solute transport in the Pearl Harbor aquifer, southern Oahu, Hawaii, shows that the readjustment of the freshwater–saltwater transition zone takes a long time following changes in pumping, irrigation, or recharge in the aquifer system. It takes about 50 years for the transition zone to move 90% of the distance to its new steady position...
Authors
S. B. Gingerich, C.I. Voss

Zinc adsorption effects on arsenite oxidation kinetics at the birnessite-water interface Zinc adsorption effects on arsenite oxidation kinetics at the birnessite-water interface

Arsenite is more toxic and mobile than As(V) in soil and sediment environments, and thus it is advantageous to explore factors that enhance oxidation of As(III) to As(V). Previous studies showed that manganese oxides, such as birnessite (??-MnO2), directly oxidized As(III). However, these studies did not explore the role that cation adsorption has on As(III) oxidation. Accordingly, the...
Authors
L.E. Power, Y. Arai, D.L. Sparks

A simple method for calculating growth rates of petroleum hydrocarbon plumes A simple method for calculating growth rates of petroleum hydrocarbon plumes

Consumption of aquifer Fe(III) during biodegradation of ground water contaminants may result in expansion of a contaminant plume, changing the outlook for monitored natural attenuation. Data from two research sites contaminated with petroleum hydrocarbons show that toluene and xylenes degrade under methanogenic conditions, but the benzene and ethylbenzene plumes grow as aquifer Fe(III)...
Authors
B.A. Bekins, I.M. Cozzarelli, G.P. Curtis

Biogeochemical controls on diel cycling of stable isotopes of dissolved 02 and dissolved inorganic carbon in the Big Hole River, Montana Biogeochemical controls on diel cycling of stable isotopes of dissolved 02 and dissolved inorganic carbon in the Big Hole River, Montana

Rivers with high biological productivity typically show substantial increases in pH and dissolved oxygen (DO) concentration during the day and decreases at night, in response to changes in the relative rates of aquatic photosynthesis and respiration. These changes, coupled with temperature variations, may impart diel (24-h) fluctuations in the concentration of trace metals, nutrients...
Authors
Stephen R. Parker, Simon R. Poulson, Chris Gammons, Michael D. DeGrandpre

Nitrogen and carbon flow from rock to water: Regulation through soil biogeochemical processes, Mokelumne River watershed, California, and Grand Valley, Colorado Nitrogen and carbon flow from rock to water: Regulation through soil biogeochemical processes, Mokelumne River watershed, California, and Grand Valley, Colorado

Soil denitrification is an ecologically important nitrogen removal mechanism that releases to the atmosphere the greenhouse gas N2O, an intermediate product from the reduction of NO3- to N 2. In this study we evaluate the relationship between soil carbon and denitrification potential in watersheds with bedrock acting as a nonpoint source of nitrogen, testing the hypothesis that nitrate...
Authors
J.M. Holloway, R. L. Smith

Use of tracers and isotopes to evaluate vulnerability of water in domestic wells to septic waste Use of tracers and isotopes to evaluate vulnerability of water in domestic wells to septic waste

In Nebraska, a large number (>200) of shallow sand‐point and cased wells completed in coarse alluvial sediments along rivers and lakes still are used to obtain drinking water for human consumption, even though construction of sand‐point wells for consumptive uses has been banned since 1987. The quality of water from shallow domestic wells potentially vulnerable to seepage from septic...
Authors
Ingrid M. Verstraeten, G.S. Fetterman, M.J. Meyer, T. Bullen, S.K. Sebree

Radium isotopes in Cayuga Lake, New York: Indicators of inflow and mixing processes Radium isotopes in Cayuga Lake, New York: Indicators of inflow and mixing processes

Naturally occurring radium isotopes (223Ra, 224Ra, 226Ra, and 228Ra) were measured in lake and tributary water of Cayuga Lake, New York, during the course of a vernal inflow event in the spring of 2001. A large influx of groundwater, probably from a carbonate aquifer, entered the lake at its extreme southern end early in the vernal inflow event and spread northward, covering an extensive...
Authors
T. F. Kraemer

Use of dissolved and vapor‐phase gases to investigate methanogenic degradation of petroleum hydrocarbon contamination in the subsurface Use of dissolved and vapor‐phase gases to investigate methanogenic degradation of petroleum hydrocarbon contamination in the subsurface

At many sites contaminated with petroleum hydrocarbons, methanogenesis is a significant degradation pathway. Techniques to estimate CH4 production, consumption, and transport processes are needed to understand the geochemical system, provide a complete carbon mass balance, and quantify the hydrocarbon degradation rate. Dissolved and vapor‐phase gas data collected at a petroleum...
Authors
Richard T. Amos, K. Ulrich Mayer, Barbara A. Bekins, Geoffrey N. Delin, Randi L. Williams

Does biofilm contribute to diel cycling of Zn in High Ore Creek, Montana? Does biofilm contribute to diel cycling of Zn in High Ore Creek, Montana?

Concentrations of metals cycle daily in the water column of some mining-impacted streams in the Rocky Mountains of the western USA. We hypothesized that biofilm in High Ore Creek, Montana, USA, sorbs and releases Zn on a diel cycle, and this uptake-and-release cycle controls the total and dissolved (0.45-μm filtered) Zn concentrations. We collected water samples from three sites...
Authors
J.M. Morris, D. A. Nimick, A.M. Farag, J.S. Meyer

Incorporating seepage losses into the unsteady streamflow equations for simulating intermittent flow along mountain front streams Incorporating seepage losses into the unsteady streamflow equations for simulating intermittent flow along mountain front streams

Seepage losses along numerous mountain front streams that discharge intermittently onto alluvial fans and piedmont alluvial plains are an important source of groundwater in the Basin and Range Province of the Western United States. Determining the distribution of seepage loss along mountain front streams is important when assessing groundwater resources of the region. Seepage loss along...
Authors
R.G. Niswonger, David E. Prudic, G. Pohll, J. Constantz
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