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Distribution of petroleum hydrocarbons and toluene biodegradation, Knox Street fire pits, Fort Bragg, North Carolina
S.L. Harden, J. E. Landmeyer
1996, Water-Resources Investigations Report 96-4066
An investigation was conducted at the Knox Street fire pits, Fort Bragg, North Carolina, to monitor the distribution of toluene, ethylbenzene, and xylene (TEX) in soil vapor, ground water, and ground-water/vapor to evaluate if total concentrations of TEX at the site are decreasing with time, and to quantify biodegradation rates...
Compilation and preliminary interpretations of hydrologic and water-quality data from the Railroad Industrial Area, Fairbanks, Alaska, 1993-94
M. R. Lilly, K. A. McCarthy, A.T. Kriegler, James Vohden, G.E. Burno
1996, Water-Resources Investigations Report 96-4049
Commercial and industrial activities in the Railroad Industrial Area in Fairbanks, Alaska, have resulted in accidental releases of chemicals to the subsurface. Such releases have generated concern regarding local ground-water quality and the potential impact on nearby water-supply wells. Consequently, a study is being conducted to characterize the environmental and...
Results of a seepage investigation at Bear Creek Valley, Oak Ridge, Tennessee, January through September 1994
J. A. Robinson, G.C. Johnson
1996, Open-File Report 95-459
A seepage investigation was conducted of 4,600 acres of Bear Creek Valley southwest of the Y-12 Plant, Oak Ridge, Tennessee, for the period of January through September 1994. The data were collected to help the Y-12 Environmental Restoration Program develop a better understanding of ground-water and surface-water interactions, recharge and...
Low-flow characteristics at selected sites on streams in southern and western Puerto Rico
Luis Santiago-Rivera
1996, Water-Resources Investigations Report 95-4147
Knowledge of the magnitude and frequency of low flows is important for the optimal development of surface-water resources in Puerto Rico. This report presents analyses of low-flow data for 9 continuous-record gaging stations and 105 partial-record stations in southern and western Puerto Rico. The report includes analyses of lowflow data...
Hydrologic and geochemical factors affecting the chemistry of small headwater streams in response to acidic deposition on Catoctin Mountain, north-central Maryland
Karen C. Rice, Owen P. Bricker
1996, Water-Resources Investigations Report 95-4155
Hydrologic and water-quality data were collected at a precipitation-collection station and from two small watersheds on Catoctin Mountain, north- central Maryland, as part of an investigation of episodic acidification and its effects on streamwater quality. Data were collected from June 1990 through December 1993. Descriptions of the water shed instrumentation,...
Estimation of evapotranspiration in the Rainbow Springs and Silver Springs basins in North-Central Florida
Leel Knowles Jr.
1996, Water-Resources Investigations Report 96-4024
Estimates of evapotranspiration (ET) for the Rainbow and Silver Springs ground-water basins in north-central Florida were determined using a regional water-~budget approach and compared to estimates computed using a modified Priestley-Taylor (PT) model calibrated with eddy-correlation data. Eddy-correlation measurements of latent 0~E) and sensible (H) heat flux were made monthly...
Ground-water flow patterns and water budget of a bottomland forested wetland, Black Swamp, eastern Arkansas
G.J. Gonthier, B.A. Kleiss
1996, Water-Resources Investigations Report 95-4192
The U.S. Geological Survey, working in cooperation with the U.S. Army Corps of Engineers, Waterways Experiment Station, collected surface-water and ground-water data from 119 wells and 13 staff gages from September 1989 to September 1992 to describe ground-water flow patterns and water budget in the Black Swamp, a bottomland forested...
Summary of the San Juan structural basin regional aquifer-system analysis, New Mexico, Colorado, Arizona, and Utah
G. W. Levings, J. M. Kernodle, C. R. Thorn
1996, Water-Resources Investigations Report 95-4188
Ground-water resources are the only source of water in most of the San Juan structural basin and are mainly used for municipal, industrial, domestic, and stock purposes. Industrial use increased dramatically during the late 1970's and early 1980's because of increased exploration and development of uranium and coal resources....
Ground-water resources and water-supply alternatives in the Wawona area of Yosemite National Park, California
J. W. Borchers
1996, Water-Resources Investigations Report 95-4229
Planning efforts to implement the 1980 General Management Plan, which recommends relocating park administrative facilities and employee housing from Yosemite Valley in Yosemite National Park, California, have focused on the availability of water at potential relocation sites within the park. Ground-water resources and water-supply alternatives in the Wawona area, one...
Hydrologic and chemical interaction of the Arkansas River and the Equus Beds aquifer between Hutchinson and Wichita, south-central Kansas
N. C. Myers, G.D. Hargadine, Joe B. Gillespie
1996, Water-Resources Investigations Report 95-4191
Large chloride concentrations in Arkansas River water have the potential to degrade water quality in the adjacent Equus beds aquifer between Hutchinson and Wichita, Kansas. The aquifer is an important source of water for municipal, industrial, agricultural, and domestic uses. A three-dimensional, finite-difference, ground-water flow-model program (MODFLOW) was used with...
Postaudit of head and transmissivity estimates and ground-water flow models of Avra Valley, Arizona
R. T. Hanson
1996, Water-Resources Investigations Report 96-4045
Ground water from regional alluvial-aquifer systems is the main source of water in the alluvial basins of Arizona, such as Avra Valley. Ground-water flow models are used to assess ground-water availability and the effects of development on the regional ground-water resources. A postaudit of regional-head and transmissivity estimates and the...
Simulation of water quality for Salt Creek in northeastern Illinois
Charles S. Melching, T.J. Chang
1996, Open-File Report 96-318
Water-quality processes in the Salt Creek watershed in northeastern Illinois were simulated with a computer model. Selected waste-load scenarios for 7-day, 10-year low-flow conditions were simulated in the stream system. The model development involved the calibration of the U.S. Environmental Protection Agency QUAL2E model to water-quality constituent concentration data collected...
Geographic, geologic, and hydrologic summaries of intermontane basins of the northern Rocky Mountains, Montana
Eloise Kendy, R.E. Tresch
1996, Water-Resources Investigations Report 96-4025
This report combines a literature review with new information to provide summaries of the geography, geology, and hydrology of each of 32 intermontane basins in western Montana. The summary of each intermontane basin includes concise descriptions of topography, areal extent, altitude, climate, 1990 population, land and water use, geology, surface...
Geohydrology and conceptual model of a ground-water-flow system near a Superfund site in Cheshire, Connecticut
J. R. Stone, P. M. Barlow, J.J. Starn
1996, Open-File Report 96-162
Degradation of ground-water quality has been identified in an area of the north-central part of the town of Cheshire, Connecticut. An investigation by the U.S. Geological Survey, in cooperation with the U.S. Environmental Protection Agency, was done during 1994-95 to characterize the unconsolidated glacial deposits and the sedimentary bedrock, integrate...
Hydrogeology of structurally extended terrain in the eastern Great Basin of Nevada, Utah, and adjacent states, from geologic and geophysical models
M. D. Dettinger, Donald H. Schaefer
1996, Hydrologic Atlas 694-D
The Great Basin of the western United States encompasses most of Nevada and western Utah (fig. 1). The climate of the region is semiarid to arid, with most precipitation falling as winter Show. The region is characterized by internal drainage (generally no hydrologic outlet to the ocean). Water resources in...
Water-resources investigations in Wisconsin
D. E. Maertz
1996, Open-File Report 96-333
PROBLEM: Surface-water information is needed for surveillance, planning, design, hazard warning, operation, and management in water-related fields such as water supply, hydroelectric power, flood control, irrigation, bridge and culvert design, wildlife management, pollution abatement, flood-plain management, and water-resources development. An appropriate data base is necessary to provide this information. OBJECTIVE: The...
Low-flow characteristics of streams in Maryland and Delaware
David H. Carpenter, Donald C. Hayes
1996, Water-Resources Investigations Report 94-4020
Hydrologic information on the variability of streamflow during low-flow periods is needed for the effective management of surface-water resources in Maryland and Delaware. Low-flow characteristics derived from streamflow under natural conditions are presented for 94 continuousrecord gaging stations in Maryland, Delaware, and surrounding States, and for 131 low-flow partial-record gaging...
Peak-flow frequency estimates through 1994 for gaged streams in South Dakota
M.J. Burr, K.L. Korkow
1996, Open-File Report 96-202
Annual peak-flow data are listed for 250 continuous-record and crest-stage gaging stations in South Dakota. Peak-flow frequency estimates for selected recurrence intervals ranging from 2 to 500 years are given for 234 of these 250 stations. The log-Pearson Type III procedure was used to compute the frequency relations for the...
Ground-Water Discharge to Biscayne Bay
Vicente Quinones-Aponte
1996, Fact Sheet 131-96
Introduction  The South Florida Ecosystem Restoration Program is an intergovernmental effort, involving a number of agencies, to reestablish and maintain the ecosystem of south Florida. One element of the restoration effort is the development of a firm scientific basis for resource decision making. The U.S. Geological Survey (USGS), one of...
South Florida Ecosystem Program; gaging flows in northeastern Florida Bay
Eduardo Patino
1996, Fact Sheet 130-96
IntroductionThe South Florida Ecosystem Restoration Program is an intergovernmental effort, involving a number of agencies, to reestablish and maintain the ecosystem of south Florida. One element of the restoration effort is the development of a firm scientific basis for resource decision making. The U.S. Geological Survey (USGS), one of the...
Geochemical and isotopic composition of ground water with emphasis on sources of sulfate in the upper Floridan Aquifer in parts of Marion, Sumter, and Citrus counties, Florida
Laura A. Sacks
1996, Water-Resources Investigations Report 95-4251
In inland areas of northwest central Florida, sulfate concentrations in the Upper Floridan aquifer are extremely variable and sometimes exceed drinking water standards (250 milligrams per liter). This is unusual because the aquifer is unconfined and near the surface, allowing for active recharge. The sources of sulfate and geochemical processes...
Water-quality assessment of the Connecticut, Housatonic, and Thames River Basins study unit: Analysis of available data on nutrients, suspended sediments, and pesticides, 1972-92
Marc J. Zimmerman, Stephen J. Grady, Elaine C. Todd Trench, Sarah M. Flanagan, Martha G. Nielson
1996, Water-Resources Investigations Report 95-4203
This retrospective report examines available nutrient, suspended sediment, and pesticide data in surface and ground water in the Connecticut, Housatonic and Thames Rivers Study Unit of the National Water-Quality Assessment Program. The purpose of this study is to improve the understanding of natural and anthropogenic factors affecting water quality in...
Technique for estimating magnitude and frequency of peak flows in Delaware
J.J. Dillow
1996, Water-Resources Investigations Report 95-4153
Methods are presented for estimating peak-flow magnitudes of selected frequencies for drainage basins in Delaware. The methods were developed by generalized least-squares regression techniques using data from 74 streamflow-gaging stations in and near Delaware, and apply to peak flows with recurrence intervals of 2, 5, 10, 25, 50, 100, and...