Publications
Dive into our publications and explore the science from the Environmental Health Program (Toxic Substances Hydrology and Contaminant Biology).
Filter Total Items: 3784
Solution of the advection-dispersion equation in two dimensions by a finite-volume Eulerian-Lagrangian localized adjoint method Solution of the advection-dispersion equation in two dimensions by a finite-volume Eulerian-Lagrangian localized adjoint method
We extend the finite-volume Eulerian-Lagrangian localized adjoint method (FVELLAM) for solution of the advection-dispersion equation to two dimensions. The method can conserve mass globally and is not limited by restrictions on the size of the grid Peclet or Courant number. Therefore, it is well suited for solution of advection-dominated ground-water solute transport problems. In test...
Authors
Richard W. Healy, T.F. Russell
Partition characteristics of polycyclic aromatic hydrocarbons on soils and sediments Partition characteristics of polycyclic aromatic hydrocarbons on soils and sediments
The partition behavior was determined for three polycyclic aromatic hydrocarbons (PAHs), i.e., naphthalene, phenanthrene, and pyrene, from water to a range of soil and sediment samples. The measured partition coefficients of the individual PAHs between soil/sediment organic matter (SOM) and water (i.e., K(oc) values) are relatively invariant either for the 'clean' (uncontaminated) soils...
Authors
C. T. Chiou, S.E. Mcgroddy, D. E. Kile
Field study and simulation of diurnal temperature effects on infiltration and variably saturated flow beneath an ephemeral stream Field study and simulation of diurnal temperature effects on infiltration and variably saturated flow beneath an ephemeral stream
Two experiments were performed to investigate flow beneath an ephemeral stream and to estimate streambed infiltration rates. Discharge and stream-area measurements were used to determine infiltration rates. Stream and subsurface temperatures were used to interpret subsurface flow through variably saturated sediments beneath the stream. Spatial variations in subsurface temperatures...
Authors
Anne Dudek Ronan, David E. Prudic, Carl E. Thodal, Jim Constantz
Type curves to determine the relative importance of advection and dispersion for solute and vapor transport Type curves to determine the relative importance of advection and dispersion for solute and vapor transport
The relative importance of advection and dispersion for both solute and vapor transport can be determined from type curves or concentration, flux, or cumulative flux. The dimensionless form of the type curves provides a means to directly evaluate the importance of mass transport by advection relative to that of mass transport by diffusion and dispersion. Type curves based on an...
Authors
J.A. Garges, A. L. Baehr
Changes in the isotopic and chemical composition of ground water resulting from a recharge pulse from a sinking stream Changes in the isotopic and chemical composition of ground water resulting from a recharge pulse from a sinking stream
The Little River, an ephemeral stream that drains a watershed of approximately 88 km2 in northern Florida, disappears into a series of sinkholes along the Cody Scarp and flows directly into the carbonate Upper Floridan aquifer, the source of water supply in northern Florida. The changes in the geochemistry of ground water caused by a major recharge pulse from the sinking stream were...
Authors
B. G. Katz, J.S. Catches, T.D. Bullen, R. L. Michel
Results from the hydrodynamic element of the 1994 entrapment zone study in Suisun Bay Results from the hydrodynamic element of the 1994 entrapment zone study in Suisun Bay
The entrapment zo as long been considered an important region of the San Francisco estuary. It has been the subject of several previous studies, and its location has been suggested as an index of condition of the estuarine ecosystem.A close correlate of this location, X2 1, is now used as a management objective on the basis that X2 is correlated with the abundance or survival of several...
Authors
J.R. Burau, J. W. Gartner, M. Stacey
Preferential flow and transport of nitrate and bromide in claypan soil Preferential flow and transport of nitrate and bromide in claypan soil
The in situ measurement of water flow and chemical transport through clay pan soils is crucial to understanding potential water contamination from agricultural sources. It is important due to the large areal extent of these soils in agricultural regions of the midwestern United States and because of preferential flow paths caused by desiccation cracks, worms burrowing, and root...
Authors
B. P. Kelly, M.L. Pomes
Preliminary estimates of residence times and apparent ages of ground water in the Chesapeake Bay watershed, and water-quality data from a survey of springs Preliminary estimates of residence times and apparent ages of ground water in the Chesapeake Bay watershed, and water-quality data from a survey of springs
Knowledge of the residence times of the ground-water systems in Chesapeake Bay watershed helps resource managers anticipate potential delays between implementation of land-management practices and any improve-ments in river and estuary water quality. This report presents preliminary estimates of ground-water residence times and apparent ages of water in the shallow aquifers of the...
Authors
Michael J. Focazio, Niel Plummer, John K. Bohlke, Eurybiades Busenberg, L. Joseph Bachman, David S. Powars
Bacterial oxidation of dibromomethane and methyl bromide in natural waters and enrichment cultures Bacterial oxidation of dibromomethane and methyl bromide in natural waters and enrichment cultures
Bacterial oxidation of14CH2Br2 and14CH3Br was measured in freshwater, estuarine, seawater, and hypersaline-alkaline samples. In general, bacteria from the various sites oxidized similar amounts of14CH2Br2 and comparatively less 14CH3Br. Bacterial oxidation of14CH3Br was rapid in freshwater samples compared to bacterial oxidation of 14CH3Br in more saline waters. Freshwater was also the...
Authors
K.D. Goodwin, J.K. Schaefer, R.S. Oremland
Comparing nocturnal eddy covariance measurements to estimates of ecosystem respiration made by scaling chamber measurements at six coniferous boreal sites Comparing nocturnal eddy covariance measurements to estimates of ecosystem respiration made by scaling chamber measurements at six coniferous boreal sites
During the growing season, nighttime ecosystem respiration emits 30–100% of the daytime net photosynthetic uptake of carbon, and therefore measurements of rates and understanding of its control by the environment are important for understanding net ecosystem exchange. Ecosystem respiration can be measured at night by eddy covariance methods, but the data may not be reliable because of...
Authors
M.B. Lavigne, M. G. Ryan, D.E. Anderson, D. D. Baldocchi, P.M. Crill, D.R. Fitzjarrald, M. L. Goulden, S.T. Gower, J.M. Massheder, J.H. McCaughey, M. Rayment, Robert G. Striegl
Anaerobic aquifer transformations of 2,4-Dinitrophenol under different terminal electron accepting conditions Anaerobic aquifer transformations of 2,4-Dinitrophenol under different terminal electron accepting conditions
We evaluated the susceptibility of 2,4-dinitrophenol (2,4-DNP) and 2,4-diaminophenol to anaerobic biodegradation in aquifer slurries. Aquifer microorganisms depleted 2,4-DNP at rates of 25, 9 and 0.4 μM/day under methanogenic, sulfate-reducing and nitrate-reducing conditions, respectively. Rates of abiotic, 2,4-DNP loss in autoclaved control incubations were 7.2, 6.2 and 0.95 μM/day...
Authors
L.R. Krumholz, J.M. Suflita
The stable isotope geochemistry of jarosite The stable isotope geochemistry of jarosite
No abstract available.
Authors
R. O. Rye, Charles N. Alpers