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Hydrochemistry of aquifer systems and relation to regional flow patterns in Cretaceous and older rocks underlying Kansas, Nebraska, and parts of Arkansas, Colorado, Missouri, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming Hydrochemistry of aquifer systems and relation to regional flow patterns in Cretaceous and older rocks underlying Kansas, Nebraska, and parts of Arkansas, Colorado, Missouri, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming

Aquifer systems in Cretaceous and older rocks of the Central Midwest are divided on the basis of hydrochemistry and ground-water flow patterns in the Plains subregion, the Western Interior Plains aquifer system contains sodium chloride type water with large concentrations of dissolved solids. Ion ratios suggest that the water was derived from seawater by concentration and by depletion of...
Authors
Claud H. Baker, Robert B. Leonard

Atrazine in surface water and relation to hydrologic conditions within the Delaware River Basin Pesticide Management Area, Northeast Kansas, July 1992 through December 1994 Atrazine in surface water and relation to hydrologic conditions within the Delaware River Basin Pesticide Management Area, Northeast Kansas, July 1992 through December 1994

Since about 1960, atrazine has been used as an effective pre- and postemergent herbicide in the production of corn and grain sorghum. Atrazine is a triazine-class herbicide and was the most frequently detected herbicide in surface water of the lower Kansas River Basin of southeast Nebraska and northeast Kansas (Stamer and Zelt, 1994). Approximately 95 percent of the atrazine applied in...
Authors
Larry M. Pope

United States Geological Survey, programs in Kansas United States Geological Survey, programs in Kansas

No abstract available.
Authors
Water Resources Division U.S. Geological Survey

Hydrogeology and water-quality conditions at the City of Olathe Landfill, east-central Kansas, 1990-93 Hydrogeology and water-quality conditions at the City of Olathe Landfill, east-central Kansas, 1990-93

Water quality at the City of Olathe Landfill in east-central Kansas was examined in relation to hydrogeologic conditions to help determine the effects of the landfill on shallow ground water. This study focused on the Wyandotte and Plattsburg Limestones underlying the landfill. The Wyandotte Limestone underlies the entire landfill, whereas the overlying Plattsburg Limestone crops out...
Authors
P.P. Rasmussen, J.C. Shockley, D. A. Hargadine

Water-level changes in the High Plains aquifer — Predevelopment to 1993 Water-level changes in the High Plains aquifer — Predevelopment to 1993

Water-level change in the High Plains aquifer underlying parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming results from differences in recharge from precipitation and ground-water withdrawals for irrigation. From the beginning of irrigation development (1940) to 1980, water levels declined in several areas, and exceeded 100 feet in parts of the...
Authors
J. T. Dugan, D. A. Cox

Water resources on and near Indian lands in northeastern Kansas and southeastern Nebraska; hydrologic data through 1990 Water resources on and near Indian lands in northeastern Kansas and southeastern Nebraska; hydrologic data through 1990

Four Kansas Indian Tribes, the Iowa, Kickapoo, Potawatomi, and Sac & Fox are interested in developing the water resources on and near their respective tribe lands. This report presents climatic and geohydrologic data that are useful in describing the available water resources in the 4,005-square-mile area in northeastern Kansas and southeastern Nebraska. Climatological data for 1961- 90...
Authors
L.D. Brewer, T. J. Trombley, M.L. Pomes

Geohydrology and saline ground-water discharge to the South Fork Ninnescah River in Pratt and Kingman Counties, south-central Kansas Geohydrology and saline ground-water discharge to the South Fork Ninnescah River in Pratt and Kingman Counties, south-central Kansas

Saline ground water discharges to the South Fork Ninnescah River in Pratt and Kingman Counties from the adjacent alluvial aquifer. Electromagnetic terrain surveys in this area indicated that the saline ground water is entering the river in intermittent reaches along the channel. The chloride concentration in the river near Murdock exceeds 250 milligrams per liter 75 percent of the time...
Authors
Joe B. Gillespie, G.D. Hargadine

Effects of reservoirs on flood discharges in the Kansas and the Missouri River basins, 1993 Effects of reservoirs on flood discharges in the Kansas and the Missouri River basins, 1993

The floods of 1993 were of historic magnitude as water in the Missouri and the Mississippi Rivers reached levels that exceeded many of the previous observed maximums. Although large parts of the flood plains of both rivers upstream from St. Louis, Missouri, were inundated, water levels would have been even higher had it not been for the large volume of runoff retained in flood-control...
Authors
Charles A. Perry

Sensitivity of water resources in the Delaware River basin to climate variability and change Sensitivity of water resources in the Delaware River basin to climate variability and change

Because of the greenhouse effect, projected increases in atmospheric carbon dioxide levels might cause global warming, which in turn could result in changes in precipitation patterns and evapotranspiration and in increases in sea level. This report describes the greenhouse effect; discusses the problems and uncertainties associated with the detection, prediction, and effects of climate...
Authors
Mark A. Ayers, David M. Wolock, Gregory J. McCabe, Lauren E. Hay, Gary D. Tasker
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