Detailed study of irrigation drainage in and near wildlife management areas, west-central Nevada, 1987-90. Part C. Summary of irrigation-drainage effects on water quality, bottom sediment, and biota
Ray J. Hoffman
1994, Water-Resources Investigations Report 92-4024-C
This report presents a summary of the detailed scientific study of Stillwater Wildlife Management Area and other nearby wetlands in west-central Nevada during 1987-90. The work was funded by the National Irrigation Water Quality Program of the U.S. Department of the Interior with the overall objectives of determining (1) the...
Water-resources activities in New England, fiscal year 1993
M.F. Orlando
1994, Open-File Report 94-339
The U.S. Geological Survey has 82 active or complete-except-report projects of hydrologic investigations ongoing within the New England Program Area. Of this total, 23 are data projects. Data projects contain statistics and data on the conditions of surface water, ground water, water quality and (or) water use for the study...
Organic compounds downstream from a treated-wastewater discharge near Dallas, Texas, March 1987
P.M. Buszka, L.B. Barber II, M.P. Schroeder, L.D. Becker
1994, Water-Resources Investigations Report 93-4194
Water and streambed-sediment samples were collected on March 9 and 10,1987 from one site upstream and three sites downstream of the discharge from a municipal wastewater-treatment plant on Rowlett Creek near Dallas, Texas. To extract and separate organic compounds, purgeand-trap, closed-loop stripping, and pH-adjusted solvent extraction methods were used for...
Chemical analyses of ground and surface water from Battle Brook drainage basin, near Princeton, Minnesota
R. B. Wanty, M. L. Tuttle, J.K. Böhlke, Paul H. Briggs
1994, Open-File Report 94-129
No abstract available....
Geohydrology and ground-water quality in the vicinity of a ground-water-contamination site in Rockford, Illinois
R.T. Kay, S. T. Prinos, Frederick L. Paillet
1994, Water-Resources Investigations Report 93-4187
A geohydrologic investigation was performed by the U.S. Geological Survey, in cooperation with the U.S. Environmental Protection Agency, to determine the distribution of volatile organic compounds in a fractured-rock aquifer near the Southeast Rockford Groundwater Contamination Site in Rockford, Ill. The geologic units of concern are the St. Peter Sandstone...
U. S. Geological Survey Federal-State Cooperative Water-Resources Program Fiscal Year 1993
B.K. Gilbert
1994, Open-File Report 94-325
The Federal-State Cooperative Program is a part- nership between the U.S. Geological Survey and State and local agencies. It provides a balanced approach to the study and resolution of water- related problems and to acquiring hydrologic data. The principal program objectives are to: (1) collect, on a systematic basis, data...
Hydrologic data for the Big Spring basin, Clayton County, Iowa, water year 1991
S. J. Kalkhoff, R.L. Kuzniar
1994, Open-File Report 94-56
Hydrologic data were collected in the Big Spring Basin located in Clayton County, Iowa, during the 1991 water year. The data were collected by the U.S. Geological Survey in cooperation with the Iowa Department of Natural Resources, Geological Survey Bureau, to provide information on variation and movement of agricultural chemicals...
Estimation of water withdrawal and distribution, water use, and wastewater collection and return flow in Cumberland, Rhode Island, 1988
M.A. Horn, P. A. Craft, Lisa Bratton
1994, Water-Resources Investigations Report 93-4023
Water-use data collected in Rhode Island by different State agencies or maintained by different public suppliers and wastewater- treatment facilities need to be integrated if these data are to be used in making water- resource management decisions. Water-use data for the town of Cumberland, a small area in northeastern...
Lithologic descriptions of two cores and ground-water-quality data from five counties in the northeastern part of the coastal plain of South Carolina, 1988 and 1991
W. F. Falls
1994, Open-File Report 94-58
This report presents data collected as part of a hydrologic investigation of Darlington, Dillon, Florence, Marion, and Marlboro Counties in the northeastern part of the Coastal Plain of South Carolina. These data include lithologic descriptions of sediment recovered from two continuously cored boreholes and water-quality results for samples collected from...
Estimates of percolation rates and ages of water in unsaturated sediments at two Mojave Desert sites, California-Nevada
David E. Prudic
1994, Water-Resources Investigations Report 94-4160
Thick unsaturated zones in arid regions increasingly are being sought for the burial of radioactive and other hazardous wastes. Estimating percolation rates of water from precipitation at proposed burial sites is important for site assessment. Chloride profiles in unsaturated sediments are used to show differences and similarities in the rates...
The Loma Prieta, California, Earthquake of October 17, 1989 — Hydrologic disturbances
Stuart A. Rojstaczer, editor(s)
1994, Professional Paper 1551-E
Seismic events have long been known to cause changes in the level of oceans, streams, lakes, and the water table. The great San Francisco earthquake of 1906 induced significant hydrologic changes that were qualitatively similar to those changes observed for the Loma Prieta earthquake. What is different is that the...
Black Hills hydrology study
D.G. Driscoll
1994, Open-File Report 94-344
The Black Hills area of western South Dakota is a valuable resource center. The area has attracted numerous residents and industries because of the availability of mineral, timber, agricultural, recreational, and water resources. The water resources of the area have been stressed locally by increasing population, periodic drought, and...
A field-trip guide to Yellowstone National Park, Wyoming, Montana, and Idaho: Volcanic, hydrothermal, and glacial activity in the region
Robert O. Fournier, R.L. Christiansen, R. A. Hutchinson, K. L. Pierce
1994, Bulletin 2099
This field-trip guide was originally prepared for the 7th International Symposium on Water/Rock Interaction (WRI-7) held in July 1992 in Park City, Utah. A large and diversified group of earth scientists and accompanying family members participated in this 3 1/2-day field trip that focused on water/rock interactions over widely ranging...
South Cascade Glacier, Washington; hydrologic and meteorological data, 1957-67
M.E. Sullivan
1994, Open-File Report 94-77
Historic hydrologic and meteorological data are compiled for South Cascade Glacier, Washington, USA, a site selected by the U.S. Geological Survey for long-term study of the response of a glacier to climate change and its effect on water resources. The data consist of stream discharge and meteorological data, including precipitation,...
Rainfall, evapotranspiration, total soil-water potential, and soil-water content at a sagebrush site and a replacement-vegetation site near Fort Defiance, Arizona, 1989-91
C. L. Thomas
1994, Open-File Report 94-43
The Navajo Nation Forestry Department established a growth of four species of native grasses and two species of native shrubs on formerly sagebrush- covered land about 6 miles north of Fort Defiance, Arizona. The native grasses and shrubs grew under conditions of natural precipitation and soil fertility. This provided alternate...
Environmental overview and hydrogeologic conditions at Aniak, Alaska
J.M. Dorava
1994, Open-File Report 94-85
The remote Native village of Aniak, on the flood plain of the Kuskokwim River in southwestern Alaska, has long cold winters and short summers that affect both the hydrology of the area and the lifestyle of the residents. Aniak obtains its drinking water from a shallow aquifer in the thick...
National Water Quality Laboratory Profile
Jon W. Raese
1994, Open-File Report 94-366
The National Water Quality Laboratory determines organic and inorganic constituents in samples of surface and ground water, river and lake sediment, aquatic plant and animal material, and precipitation collected throughout the United States and its territories by the U.S. Geological Survey. In water year 1994, the Laboratory produced more than...
Streamflow and selected precipitation data for Yucca Mountain region, southern Nevada and eastern California, water years 1986-90
Thomas G. Kane III, David J. Bauer, Clair M. Martinez
1994, Open-File Report 94-312
Streamflow and precipitation data collected at and near Yucca Mountain, Nevada, during water years 1986-90 are presented in this report. The data were collected and compiled as part of the studies by the U.S. Geological Survey, in cooperation with the U.S. Department of Energy, to characterize surface-water hydrology in the...
Ground-water hydrology of the upper Sevier River Basin, south-central Utah, and simulation of ground-water flow in the valley-fill in Panguitch Valley.
Susan A. Thiros, William C. Brothers
1993, Technical Publication 102
The ground-water hydrology of the upper Sevier River basin, primarily of the unconsolidated valley-fill aquifers, was studied from 1988 to 1989. Recharge to the valley-fill aquifers is mostly by seepage from surface-water sources. Changes in soil-moisture content am water levels were measured in Panguitch Valley both at a flood-irrigated and...
Coupled effects of vertical mixing and benthic grazing on phytoplankton populations in shallow, turbid estuaries
Jeffrey R. Koseff, Jacqueline K. Holen, Stephen G. Monismith, James E. Cloern
1993, Journal of Marine Research (51) 843-868
Coastal ocean waters tend to have very different patterns of phytoplankton biomass variability from the open ocean, and the connections between physical variability and phytoplankton bloom dynamics are less well established for these shallow systems. Predictions of biological responses to physical variability in these environments is inherently difficult because the...
Organic carbon sources and sinks in San Francisco Bay: variability induced by river flow
Alan D. Jassby, T.M. Powell, James E. Cloern
1993, Marine Ecology Progress Series (95) 39-54
Sources and sinks of organic carbon for San Francisco Bay (California, USA) were estimated for 1980. Sources for the southern reach were dominated by phytoplankton and benthic microalgal production. River loading of organic matter was an additional important factor in the...
Spring climate and salinity in the San Francisco Bay Estuary
Daniel R. Cayan, David H. Peterson
1993, Water Resources Research (29) 293-303
Salinity in the San Francisco Bay Estuary almost always experiences its yearly maximum during late summer, but climate variability produces marked interannual variations. The atmospheric circulation pattern impacts the estuary primarily through variations of runoff from rainfall and snowmelt from the Sierra Nevada and, secondarily, through variations in the near-surface...
Mapping playa evaporite minerals with AVIRIS data: A first report from Death Valley, California
J.K. Crowley
1993, Remote Sensing of Environment (44) 337-356
Efflorescent salt crusts in Death Valley, California, were mapped by using Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) data and a recently developed least-squares spectral band-fitting algorithm. Eight different saline minerals were remotely identified, including three borates, hydroboracite, pinnoite, and rivadavite, that have not been previously reported from the Death Valley efflorescent...
Policy and procedures for the management and archival storage of data collected for hydrologic investigations, U.S. Geological Survey, Indiana District
Jeffrey D. Martin, David A. Cohen
1993, Open-File Report 94-61
This report describes the policy and procedures used by the Indiana District of the U.S. Geological Survey, Water Resources Division, to manage and store data collected during hydrologic investigations. It is the policy of the Indiana District that data collected to meet the objectives of projects for hydrologic investigations be...
Hydrology of the Estancia Basin, central New Mexico
R.R. White
1993, Water-Resources Investigations Report 93-4163
The Estancia Basin of central New Mexico is a topographically closed basin that ranges in altitude from 6,000 feet to more than 10,000 feet above sea level. In the center of the basin a valley-fill aquifer of Quaternary age is as much as 400 feet thick. Limestone of the Madera...