Publications
Dive into our publications and explore the science from the Environmental Health Program (Toxic Substances Hydrology and Contaminant Biology).
Filter Total Items: 3785
Identifying fracture‐zone geometry using simulated annealing and hydraulic‐connection data Identifying fracture‐zone geometry using simulated annealing and hydraulic‐connection data
A new approach is presented to condition geostatistical simulation of high‐permeability zones in fractured rock to hydraulic‐connection data. A simulated‐annealing algorithm generates three‐dimensional (3‐D) realizations conditioned to borehole data, inferred hydraulic connections between packer‐isolated borehole intervals, and an indicator (fracture zone or background‐K bedrock)...
Authors
Frederick D. Day-Lewis, Paul A. Hsieh, Steven M. Gorelick
Mobilization of arsenite by dissimilatory reduction of adsorbed arsenate Mobilization of arsenite by dissimilatory reduction of adsorbed arsenate
Sulfurospirillum barnesii is capable of anaerobic growth using ferric iron or arsenate as electron acceptors. Cell suspensions of S. barnesii were able to reduce arsenate to arsenite when the former oxyanion was dissolved in solution, or when it was adsorbed onto the surface of ferrihydrite, a common soil mineral, by a variety of mechanisms (e.g., coprecipitation, presorption). Reduction...
Authors
J. Zobrist, P.R. Dowdle, J.A. Davis, Ronald S. Oremland
Effect of a constructed wetland on disinfection byproducts: Removal processes and production of precursors Effect of a constructed wetland on disinfection byproducts: Removal processes and production of precursors
The fate of halogenated disinfection byproducts (DBPs) in treatment wetlands and the changes in the DBP formation potential as wastewater treatment plant (WWTP)-derived water moves through the wetlands were investigated. Wetland inlet and outlet samples were analyzed for total organic halide (TOX), trihalomethanes (TH M), haloacetic acids (HAA), dissolved organic carbon (DOC), and UV...
Authors
C.E. Rostad, Barbara S. Martin, L. B. Barber, J.A. Leenheer, S.R. Daniel
Estimating formation properties from early-time oscillatory water levels in a pumped well Estimating formation properties from early-time oscillatory water levels in a pumped well
Hydrologists often attempt to estimate formation properties from aquifer tests for which only the hydraulic responses in a pumped well are available. Borehole storage, turbulent head losses, and borehole skin, however, can mask the hydraulic behavior of the formation inferred from the water level in the pumped well. Also, in highly permeable formations or in formations at significant...
Authors
A.M. Shapiro, D.S. Oki
Effects of the flood of 1993 on the chemical characteristics of bed sediments in the Upper Mississippi River Effects of the flood of 1993 on the chemical characteristics of bed sediments in the Upper Mississippi River
Concentrations of pollutants stored in the surficial bed sediments in the navigation pools of the Upper Mississippi River showed a general decrease after the record flood of 1993. Percent clay and total organic carbon in the surficial sediments decreased as a result of an increase in the proportion of coarser sediment. Decreases in pollutant concentration may have been a result of the...
Authors
J. A. Moody, J.F. Sullivan, Howard E. Taylor
Groundwater “fast paths” in the Snake River Plain aquifer: Radiogenic isotope ratios as natural groundwater tracers Groundwater “fast paths” in the Snake River Plain aquifer: Radiogenic isotope ratios as natural groundwater tracers
Preferential flow paths are expected in many groundwater systems and must be located because they can greatly affect contaminant transport. The fundamental characteristics of radiogenic isotope ratios in chemically evolving waters make them highly effective as preferential flow path indicators. These ratios tend to be more easily interpreted than solute-concentration data because their...
Authors
Thomas M. Johnson, Robert C. Roback, Travis L. McLing, Thomas D. Bullen, Donald J. DePaolo, Christine Doughty, Randall J. Hunt, Robert W. Smith, L. DeWayne Cecil, Michael T. Murrell
Occurrence of pesticides in rain and air in urban and agricultural areas of Mississippi, April-September 1995 Occurrence of pesticides in rain and air in urban and agricultural areas of Mississippi, April-September 1995
In April 1995, the US Geological Survey began a study to determine the occurrence and temporal distribution of 49 pesticides and pesticide metabolites in air and rain samples from an urban and an agricultural sampling site in Mississippi. The study was a joint effort between the National Water-Quality Assessment and the Toxic Substances Programs and was part of a larger study examining...
Authors
R.H. Coupe, M.A. Manning, W.T. Foreman, D. A. Goolsby, M.S. Majewski
Comparison of enzyme-linked immunosorbent assay and gas chromatography procedures for the detection of cyanazine and metolachlor in surface water samples Comparison of enzyme-linked immunosorbent assay and gas chromatography procedures for the detection of cyanazine and metolachlor in surface water samples
Enzyme-linked immunosorbent assay (ELISA) data from surface water reconnaissance were compared to data from samples analyzed by gas chromatography for the pesticide residues cyanazine (2-[[4-chloro-6-(ethylamino)-l,3,5-triazin-2-yl]amino]-2-methylpropanenitrile ) and metolachlor (2-chloro-N-(2-ethyl-6-methylphenyl)-N-(2-methoxy-1-methylethyl)acetamide). When ELISA analyses were...
Authors
S.M. Schraer, D.R. Shaw, M. Boyette, R.H. Coupe, E.M. Thurman
Authigenic molybdenum formation in marine sediments: A link to pore water sulfide in the Santa Barbara Basin Authigenic molybdenum formation in marine sediments: A link to pore water sulfide in the Santa Barbara Basin
Pore water and sediment Mo concentrations were measured in a suite of multicores collected at four sites along the northeastern flank of the Santa Barbara Basin to examine the connection between authigenic Mo formation and pore water sulfide concentration. Only at the deepest site (580 m), where pore water sulfide concentrations rise to >0.1 μM right below the sediment water interface...
Authors
Yen Zheng, Robert F. Anderson, A. VanGeen, J. Kuwabara
Modeling the influence of variable pH on the transport of zinc in a contaminated aquifer using semiempirical surface complexation models Modeling the influence of variable pH on the transport of zinc in a contaminated aquifer using semiempirical surface complexation models
Land disposal of sewage effluent resulted in contamination of a sand and gravel aquifer (Cape Cod, Massachusetts) with zinc (Zn). The distribution of Zn was controlled by pH‐dependent adsorption; the Zn extended 15 m into the 30‐m‐thick sewage plume within approximately 100 m of the source but only 2–4 m into the plume between 100 and 400 m downgradient. A two‐dimensional vertical cross...
Authors
D.B. Kent, R.H. Abrams, J.A. Davis, J.A. Coston, D.R. LeBlanc
Multispecies reactive tracer test in an aquifer with spatially variable chemical conditions Multispecies reactive tracer test in an aquifer with spatially variable chemical conditions
A field investigation of multispecies reactive transport was conducted in a well‐characterized, sand and gravel aquifer on Cape Cod, Massachusetts. The aquifer is characterized by regions of differing chemical conditions caused by the disposal of secondary sewage effluent. Ten thousand liters of groundwater with added tracers (Br, Cr(VI), and EDTA complexed with Pb, Zn, Cu, and Ni) were...
Authors
J.A. Davis, D.B. Kent, J.A. Coston, K.M. Hess, J.L. Joye
Characterizing multiple timescales of stream and storage zone interaction that affect solute fate and transport in streams Characterizing multiple timescales of stream and storage zone interaction that affect solute fate and transport in streams
The fate of contaminants in streams and rivers is affected by exchange and biogeochemical transformation in slowly moving or stagnant flow zones that interact with rapid flow in the main channel. In a typical stream, there are multiple types of slowly moving flow zones in which exchange and transformation occur, such as stagnant or recirculating surface water as well as subsurface...
Authors
Jungyill Choi, Judson W. Harvey, Martha H. Conklin