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Water resources of Sedgwick County, Kansas Water resources of Sedgwick County, Kansas

Hydrologic data from streams, impoundments, and wells are interpreted to: (1) document water resources characteristics; (2) describe causes and extent of changes in water resources characteristics; and (3) evaluate water resources as sources of supply. During 1985, about 134,200 acre-ft of water (84% groundwater) were used for public (42%), irrigation, (40%), industrial (14%), and...
Authors
H.E. Bevans

U.S. Geological Survey second national symposium on Water quality; abstracts of the technical sessions, Orlando, Florida, November 12-17, 1989 U.S. Geological Survey second national symposium on Water quality; abstracts of the technical sessions, Orlando, Florida, November 12-17, 1989

The U.S Geological Survey (USGS) compiled and analyzed existing hydrologic and water-quality data from over 200 stream and estuary stations of the Abemarle-Pamlico estuarine system (A/P) to identify long-term temporal and spatial trends. The dataset included seven stations of the USGS National Stream Quality Accounting Network, two stations of the National Atmospheric Precipitation...

Water supply and demand in Sedgwick County, Kansas Water supply and demand in Sedgwick County, Kansas

Water supplies in Sedgwick County, Kansas, are derived from surface--and groundwater resources. During 1985, public supply, irrigation, and self-supplied industry required 38% of the 56 ,500 acre-ft of appropriated surface water and 57% of the 187 ,800 acre-ft of appropriated groundwater. If the historic (1920-80) annual population growth rate (2.8%) continues, the 126,100 acre ft of...
Authors
Hugh E. Bevans

Water-level changes in the High Plains aquifer underlying parts of South Dakota, Wyoming, Nebraska, Colorado, Kansas, New Mexico, Oklahoma, and Texas: Predevelopment through nonirrigation season 1987-88 Water-level changes in the High Plains aquifer underlying parts of South Dakota, Wyoming, Nebraska, Colorado, Kansas, New Mexico, Oklahoma, and Texas: Predevelopment through nonirrigation season 1987-88

The changes in water levels in the High Plains aquifer from the nonirrigation season 1986-87 through the nonirrigation season 1987-88 and from the nonirrigation season 1979-80 through the nonirrigation season 1987-88 are presented in maps for the entire High Plains aquifer area. Water level changes are caused by interacting changes in precipitation, land use, and annual pumpage. Water...
Authors
W. M. Kastner, D. E. Schild, D. S. Spahr

Hydrogeology and ground-water-quality conditions at the Geary County landfill, northeast Kansas, 1988 Hydrogeology and ground-water-quality conditions at the Geary County landfill, northeast Kansas, 1988

Chemical analysis of water from monitoring wells upgradient and downgradient of the Geary County Landfill in Kansas near Junction City indicate the presence of several chemically distinct water types. For the dominant calcium bicarbonate water type, concentrations of inorganic and organic constituents indicate the presence of reducing conditions within the landfill and increased...
Authors
N. C. Myers, P. R. Bigsby

Water-resources activities of the U.S. Geological Survey in Kansas; fiscal years 1987 and 1988 Water-resources activities of the U.S. Geological Survey in Kansas; fiscal years 1987 and 1988

The principal mission of the U.S. Geological Survey, Water Resources Division, in Kansas is to investigate the occurrence, quantity, quality, distribution, and movement of surface and groundwater throughout the State. Primary activities include the systematic collection, analysis, and interpretation of hydrologic data, evaluation of water demands, and water resources research. Hydrologic
Authors
L. J. Combs

Simulation of precipitation by weather-type analysis Simulation of precipitation by weather-type analysis

A new approach that uses weather-type analysis as a basis for stochastic precipitation modeling was developed and tested for Philadelphia, Pennsylvania. The weather types permit the identification of weather conditions associated with varying frequencies, intensities, and amounts of precipitation. Weather-type frequencies were used to stochastically simulate precipitation for...
Authors
G. J. McCabe, L.E. Hay, L.S. Kalkstein, M. A. Ayers, D.M. Wolock

Description of data files compiled for the Central Midwest Regional Aquifer-System Analysis Description of data files compiled for the Central Midwest Regional Aquifer-System Analysis

Several types of geologic and hydrologic data were collected and compiled as part of the Central Midwest Regional Aquifer-System Analysis. The study described the hydrology of Cambrian-age through Cretaceous-age rocks in all of Kansas and Nebraska and parts of eight other states. Information from both water wells and petroleum wells was obtained from numerous State, Federal, and private...
Authors
John O. Helgesen, Cristi V. Hansen

Summary of the U.S. Geological Survey and U.S. Bureau of Land Management national coal-hydrology program, 1974-84 Summary of the U.S. Geological Survey and U.S. Bureau of Land Management national coal-hydrology program, 1974-84

During the decade 1974-84, the U.S. Geological Survey and the U.S. Bureau of Land Management cooperated on investigations to collect information and to study hydrologic processes related to development and mining of federally owned coal. In addition, the U.S. Geological Survey conducted similar investigations related to nonfederally owned coal. As a result of these nationwide...

US Geological Survey Toxic Substances Hydrology Program: Proceedings of the technical meeting, Phoenix, Arizona, September 26-30, 1988 US Geological Survey Toxic Substances Hydrology Program: Proceedings of the technical meeting, Phoenix, Arizona, September 26-30, 1988

Crude oil floating at the surface of a shallow aquifer of glacial outwash, near Bemidji, Minnesota, is altered by geochemical processes. Hydrocarbons from the oil are attenuated by several reactions that include aerobic and anaerobic microbial degradation. These degradation reactions result in the development of geochemical facies in the shallow groundwater system. Groundwater most...

Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas

A study was conducted to evaluate the effects of potential development of the Dakota aquifer on the layered-aquifer system above Permian rocks in a 5,000-square-mile area of southwestern Kansas. This aquifer system, which consists of five layers, includes the Cheyenne aquifer, the Kiowa confining unit, the Dakota aquifer, the Niobrara-Graneros confining unit, and the High Plains aquifer...
Authors
Kenneth R. Watts
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