Publications
Dive into our publications and explore the science from the Environmental Health Program (Toxic Substances Hydrology and Contaminant Biology).
Filter Total Items: 3785
Ground-water quality in five areas of differing land use in Nassau and Suffolk counties, Long Island, New York Ground-water quality in five areas of differing land use in Nassau and Suffolk counties, Long Island, New York
No abstract available.
Authors
C.E. LeaMond, R.J. Haefner, S.J. Cauller, P. E. Stackelberg
Hydrologic data from the study of acidic contamination in the Miami Wash-Pinal Creek area, Arizona, water years 1990-91 Hydrologic data from the study of acidic contamination in the Miami Wash-Pinal Creek area, Arizona, water years 1990-91
No abstract available.
Authors
S.A. Longsworth, A.M. Taylor
Floating sample-collection platform with stage-activated automatic water sampler for streams with large variation in stage Floating sample-collection platform with stage-activated automatic water sampler for streams with large variation in stage
A floating sample-collection platform is described for stream sites where the vertical or horizontal distance between the stream-sampling point and a safe location for the sampler exceed the suction head of the sampler. The platform allows continuous water sampling over the entire storm-runoff hydrogrpah. The platform was developed for a site in southern Illinois.
Authors
Stephen R. Tarte, A.R. Schmidt, Daniel J. Sullivan
Compilation and interpretation of water-quality and discharge data for acidic mine waters at Iron Mountain, Shasta County, California, 1940-91 Compilation and interpretation of water-quality and discharge data for acidic mine waters at Iron Mountain, Shasta County, California, 1940-91
No abstract available.
Authors
Charles N. Alpers, D. Kirk Nordstrom, J.M. Burchard
Tensiometers: Theory, construction, and use Tensiometers: Theory, construction, and use
Standard tensiometers are used to measure matric potential as low as −870 cm of water in the unsaturated zone by creating a saturated hydraulic link between the soil water and a pressure sensor. The direction and, in some cases, quantity of water flux can be determined using multiple installations. A variety of commercial and fabricated tensiometers are commonly used. Saturated porous...
Authors
D.I. Stannard
Floodplain storage of mine tailings in the Belle Fourche river system: a sediment budget approach Floodplain storage of mine tailings in the Belle Fourche river system: a sediment budget approach
Arsenic‐contaminated mine tailings that were discharged into Whitewood Creek at Lead, South Dakota, from 1876 to 1978, were deposited along the floodplains of Whitewood Creek and the Belle Fourche River. The resulting arsenic‐contaminated floodplain deposit consists mostly of overbank sediments and filled abandoned meanders along White‐wood Creek, and overbank and point‐bar sediments...
Authors
D. C. Marron
Improved apparatus for measuring hydraulic conductivity at low water content Improved apparatus for measuring hydraulic conductivity at low water content
A modification of the steady-state centrifuge method (SSCM) for unsaturated hydraulic conductivity (K) measurement improves the range and adjustability of this method. The modified apparatus allows mechanical adjustments to vary the measured K by a factor of 360. In addition, the use of different flow-regulating ceramic materials can give a total K range covering about six orders of...
Authors
J. R. Nimmo, K.C. Akstin, K.A. Mello
Large lake basins of the southern High Plains: Ground-water control of their origin? Large lake basins of the southern High Plains: Ground-water control of their origin?
The origin of the ∼40-50 topographically large lake basins on the southern High Plains of Texas and New Mexico has been an enigma. Previous workers have considered deflation or evaporite dissolution at depth and subsequent collapse as the most probable mechanisms. However, the eolian hypotheses have been unable to provide convincing arguments as to how the wind selectively erodes the...
Authors
W.W. Wood, W. E. Sanford, C.C. Reeves
Determination of subsurface fluid contents at a crude-oil spill site Determination of subsurface fluid contents at a crude-oil spill site
Measurement of the fluid-content distribution at sites contaminated by immiscible fluids, including crude oil, is needed to better understand the movement of these fluids in the subsurface and to provide data to calibrate and verify numerical models and geophysical methods. A laboratory method was used to quantify the fluid contents of 146 core sections retrieved from boreholes aligned...
Authors
K.M. Hess, W.N. Herkelrath, H.I. Essaid
Humic substances and trace metals associated with Fe and Al oxides deposited in an acidic mountain stream Humic substances and trace metals associated with Fe and Al oxides deposited in an acidic mountain stream
Hydrous iron and aluminum oxides are deposited on the streambed in the confluence of the Snake River and Deer Creek, two streams in the Colorado Rocky Mountains. The Snake River is acidic and has high concentrations of dissolved Fe and Al. These metals precipitate at the confluence with the pristine, neutral pH, Deer Creek because of the greater pH (4.5-6.0) in the confluence. The...
Authors
Diane M. McKnight, R.L. Wershaw, K.E. Bencala, G. W. Zellweger, G. L. Feder
Aquatic insects as bioindicators of trace element contamination in cobble-bottom rivers and streams Aquatic insects as bioindicators of trace element contamination in cobble-bottom rivers and streams
In one river, Cu, Cd, Pb, and Zn were analysed in insects and in fine bed sediments over a 381-km reach downstream of a large copper mining complex. In another river, As contamination from a gold mine was assessed in insects and bed sediments over a 40-km reach. All insect taxa collected in contaminated river reaches had elevated whole-body trace element concentrations, but few species...
Authors
D.J. Cain, S. N. Luoma, J.L. Carter, S.V. Fend
Ground-water models cannot be validated Ground-water models cannot be validated
Ground-water models are embodiments of scientific hypotheses. As such, the models cannot be proven or validated, but only tested and invalidated. However, model testing and the evaluation of predictive errors lead to improved models and a better understanding of the problem at hand. In applying ground-water models to field problems, errors arise from conceptual deficiencies, numerical...
Authors
Leonard F. Konikow, J.D. Bredehoeft