Hydrologic data for urban stormwater studies in the Dallas-Fort Worth area, Texas, 1992-94
Stanley Baldys, T. H. Raines, B.L. Mansfield, J.T. Sandlin
1997, Open-File Report 96-482
This report presents precipitation and waterquality data from analyses of 210 samples collected at 30 storm-sewer outfall stations in the Dallas-Fort Worth area, Texas, during February 1992-November 1994. The data were collected to fulfill requirements mandated by the U.S. Environmental Protection Agency to the cities of Arlington, Dallas, Fort Worth,...
Hydrologic and water-quality data from selected sites in the Charleston Harbor Estuary and tributary rivers, South Carolina, water years 1992-95
P.A. Conrads, T.W. Cooney, K.B. Long
1997, Open-File Report 96-418
Hydrogeologic framework and ground-water resources at Seymour Johnson Air Force Base, North Carolina
A.P. Cardinell, S. S. Howe
1997, Open-File Report 96-581
A preliminary hydrogeologic framework of the Seymour Johnson Air Force Base was constructed from published data, available well data, and reports from Air Base files, City of Goldsboro and Wayne County records, and North Carolina Geological Survey files. Borehole geophysical logs were run in selected wells; and the surficial, Black...
Development of an 11- and 14-digit hydrologic unit boundary layer for the Upper Cumberland River Basin using a Geographic Information System
Hugh L. Nelson, Aimee C. Downs, Steve D. Crabtree, Doug H. Hines
1997, Open-File Report 97-618
Development of an 11- and 14-Digit Hydrologic Unit Boundary Layer for the Licking River Basin Using a Geographic Information System
Hugh L. Nelson, Aimee C. Downs, Steve D. Crabtree, Doug H. Hines
1997, Open-File Report 97-615
Development of an 11- and 14-digit hydrologic unit boundary layer for the Big Sandy River Basin using a Geographic Information System
Hugh L. Nelson, Aimee C. Downs, Steve D. Crabtree, Doug H. Hines
1997, Open-File Report 97-617
Wetland losses related to fault movement and hydrocarbon production, southeastern Texas coast
William A. White, Robert A. Morton
1997, Journal of Coastal Research (13) 1305-1320
Time series analyses of surface fault activity and nearby hydrocarbon production from the southeastern Texas coast show a high correlation among volume of produced fluids, timing of fault activation, rates of subsidence, and rates of wetland loss. Greater subsidence on the downthrown sides of faults contributes to more frequent flooding...
Vulnerability of ground water to atrazine leaching in Kent County, Michigan
D. J. Holtschlag, C. L. Luukkonen
1997, Water-Resources Investigations Report 96-4198
A steady-state model of pesticide leaching through the unsaturated zone was used with readily available hydrologic, lithologic, and pesticide characteristics to estimate the vulnerability of the near-surface aquifer to atrazine contamination from non-point sources in Kent County, Michigan. The modelcomputed fraction of atrazine remaining at the water table, RM, was...
Precipitation-runoff and streamflow-routing models for the Willamette River basin, Oregon
Antonius Laenen, John C. Risley
1997, Water-Resources Investigations Report 95-4284
Precipitation-runoff and streamflow-routing models were constructed and assessed as part of a water-quality study of the Willamette River Basin. The study was a cooperative effort between the U.S. Geological Survey (USGS) and the Oregon Department of Environmental Quality (ODEQ) and was coordinated with the USGS National Water-Quality Assessment (NAWQA) study...
What are volcano hazards?
Bobbie Myers, Steven R. Brantley, Peter R. Stauffer, James W. Hendley II
1997, Fact Sheet 002-97
Volcanoes give rise to numerous geologic and hydrologic hazards. U.S. Geological Survey (USGS) scientists are assessing hazards at many of the almost 70 active and potentially active volcanoes in the United States. They are closely monitoring activity at the most dangerous of these volcanoes and are prepared to issue warnings...
A comparison of wetland tree growth response to hydrologic regime in Louisiana and South Carolina
Bobby D. Keeland, William Conner, Rebecca R. Sharitz
1997, Forest Ecology and Management (90) 237-250
Numerous investigations have examined the growth of wetland tree species under a variety of hydrologic conditions. Most studies have compared flooded versus non-flooded conditions in greenhouses or in one to a few field sites near each other or within the same region. Comparisons of wetland tree growth among widely separated...
A study of the temporal variability of atrazine in private well water. part ii: analysis of data
Paul Pinsky, Matthew Lorber, Kent Johnson, Burton Kross, Leon Burmeister, Amina Wilkins, George Hallberg
1997, Environmental Monitoring and Assessment (47) 197-221
In 1988, the Iowa Department of Natural Resources, along withthe University of Iowa, conducted the Statewide Rural WellWater Survey, commonly known as SWRL. A total of 686private rural drinking water wells was selected by use of aprobability sample and tested for pesticides and nitrate. A subsetof these wells, the 10%...
Source, transport, and partitioning of metals between water, colloids, and bed sediments of the Animas River, Colorado
S. E. Church, B. A. Kimball, D.L. Fey, D.A. Ferderer, T. J. Yager, R. B. Vaughn
1997, Open-File Report 97-151
No abstract available....
Preliminary hydrogeologic assessment of a ground-water contamination area in Wolcott, Connecticut
J. R. Stone, G. D. Casey, R.A. Mondazzi, T.W. Frick
1997, Open-File Report 97-219
Contamination of ground water by volatile organic compounds and inorganic constituents has been identified at a number of industrial sites in the Town of Wolcott, Connecticut. Contamination is also present at a municipal landfill in the City of Waterbury that is upgradient from the industrial sites in...
U.S. Geological Survey Middle Rio Grande Basin Study; Proceedings of the first annual workshop, Denver, Colorado, November 12-14, 1996
James R. Bartolino, editor(s)
1997, Open-File Report 97-116
Approximately 40 percent (about 600,000 people) of the total population of New Mexico lives within the Middle Rio Grande Basin, which includes the City of Albuquerque. Ongoing analyses of the central portion of the Middle Rio Grande Basin by the U.S. Geological Survey (USGS) in cooperation with the City of Albuquerque...
How does streamflow affect metals in the upper Arkansas River?
Michael E. Lewis, Melanie L. Clark
1997, Fact Sheet 226-96
No abstract available....
Methods to identify areas susceptible to irrigation-induced selenium contamination in the western United States
Ralph L. Seiler
1997, Fact Sheet 038-97
No abstract available....
Nutrient and trace-element enrichment of Coeur d'Alene Lake, Idaho
Paul F. Woods, Michael A. Beckwith
1997, Water Supply Paper 2485
The limnological characteristics and geochemistry of lakebed sediments in Coeur d'Alene Lake were assessed during 1991-92 because of the possible interaction of nutrient enrichment with the highly enriched trace-element concentrations stored in the lakebed. The scope included characterization of physical, chemical, and biological variables; quantification of hydrologic, nutrient, and trace-element...
Water-quality and hydrogeologic data used to evaluate the effects of farming systems on ground-water quality at the Management Systems Evaluation Area near Princeton, Minnesota, 1991-95
M.K. Landon, G. N. Delin, K.J. Nelson, C.P. Regan, J.A. Lamb, S.J. Larson, P. D. Capel, J. L. Anderson, R.H. Dowdy
1997, Open-File Report 97-22
The Minnesota Management Systems Evaluation Area (MSEA) project was part of a multi-scale, inter-agency initiative to evaluate the effects of agricultural management systems on water quality in the midwest corn belt. The research area was located in the Anoka Sand Plain about 5 kilometers southwest of Princeton, Minnesota. The ground-water-quality...
Regional diagenetic patterns in the St. Peter Sandstone; implications for brine migration in the Illinois Basin
Janet K. Pitman, Martin B. Goldhaber, Christoph Spoetl
1997, Bulletin 2094-A
Diagenetic minerals and alteration patterns in the Ordovician St. Peter Sandstone, Illinois Basin, record varied hydrologic and chemical conditions during the basin?s long and complex geologic history. Major diagenetic events modifying the St. Peter Sandstone include (1) mechanical compaction, (2) early K-feldspar overgrowth and dolospar precipitation, (3) burial quartz, dolospar, anhydrite, and calcite cementation, and (4) carbonate-cement...
Changes in flow in the Beaver-North Canadian River basin upstream from Canton Lake, western Oklahoma
Kenneth L. Wahl, Robert L. Tortorelli
1997, Water-Resources Investigations Report 96-4304
This report presents the results of an evaluation of hydrologic data for the Beaver-North Canadian River basin upstream from Canton Lake in western Oklahoma. It examines the climatic and hydrologic data for evidence of trends. The hydrologic data examined includes total annual flow, base flow, and annual peak discharges. This study...
A method for evaluating water-level response to hydrologic stresses in karstic wetlands in central Florida, using a simple water-balance model
E. R. German
1997, Water-Resources Investigations Report 96-4216
Potentiometric surface and hydrologic conditions of the upper aquifer in the Manatí-Vega Baja area, north central Puerto Rico, March 1995
Carlos Conde-Costas, Gilberto Rodriguez-Rodriguez
1997, Water-Resources Investigations Report 96-4184
No abstract available....
Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through December 1996
J.D. Torikai
1997, Open-File Report 97-114
Hydrogeology and potential for ground-water development, carbonate-rock aquifers, southern Nevada and southeastern California
T. J. Burbey
1997, Water-Resources Investigations Report 95-4168
Seventeen hydrographic areas in southern Nevada were assessed for the ground-water development potential of the underlying carbonate-rock aquifers on the basis of geologic and hydrologic information developed as part of the Nevada Carbonate Aquifers Study and information compiled from previous investigations. All selected areas lie within a miogeoclinal belt where...