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Hydrologic and related data for water-supply planning in an intensive-study area, northeastern Wichita County, Kansas Hydrologic and related data for water-supply planning in an intensive-study area, northeastern Wichita County, Kansas

Data are presented that result from an intensive geohydrologic study for water-supply planning in a 12-square-mile area in northeastern Wichita County, Kansas. These data include records of wells, test drilling, chemical analyses, ground-water levels, rainfall, soilmoisture, well yield, solar radiation, crop yield, and crop acreage. Data indicate that water levels in the unconsolidated...
Authors
Jack Kume, L. E. Dunlap, E. D. Gutentag, J.G. Thomas

Determination of peak discharge from rainfall data for urbanized basins, Wichita, Kansas Determination of peak discharge from rainfall data for urbanized basins, Wichita, Kansas

Rainfall and runoff data from urbanized drainage basins in the Wichita area, Kansas, were used to evaluate the Soil Conservation Service synthetichydrograph method of computing flood hydrographsfrom rainfall data. The method was tested on six basins where the impervious surface ranged from 11 percent on the least urbanized basin to 40 percent on the most urbanized. Twenty-two of the...
Authors
C.O. Peek, P. R. Jordan

Chemical quality of water in abandoned zinc mines in northeastern Oklahoma and southeastern Kansas Chemical quality of water in abandoned zinc mines in northeastern Oklahoma and southeastern Kansas

Onsite measurements of pH, specific conductance, and water temperature show that water temperatures in seven mine shafts in northeastern Oklahoma and southeastern Kansas is stratified. With increasing sampling depth, specific conductance and water temperature tend to increase, and pH tends to decrease. Concentrations of dissolved solids and chemical constituents in mine-shaft water, such...
Authors
Stephen J. Playton, Robert Ellis Davis, Roger G. McClaflin

Guidelines for the use of structural versus regression analysis in geomorphic studies Guidelines for the use of structural versus regression analysis in geomorphic studies

Simple-regression and structural analysis are similar methods of developing a linear relation from a bivariant group of data. Regression analysis is a useful curve-fitting technique, but often is misapplied to geomorphic data sets. When error components can be identified for both variables, the statistical technique of structural analysis is preferred. If regression results are available
Authors
W. R. Osterkamp, Jesse M. McNellis, Paul Robert Jordan

Water resources data for Kansas, water year 1977 Water resources data for Kansas, water year 1977

Water resources data for the 1977 water year for Kansas consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality in wells. This report contains discharge records for 149 gaging stations; stage and contents for 20 lakes and reservoirs; water quality for 77 gaging stations and 2...
Authors
Water Resources Division U.S. Geological Survey

Map showing saturated thickness of unconsolidated aquifer in southwestern Kansas, January 1978 Map showing saturated thickness of unconsolidated aquifer in southwestern Kansas, January 1978

The principal aquifer in the 13-county area of southwestern Kansas occurs in the heterogeneous, unconsolidated alluvial deposits of Tertiary and Quaternary age. The main body of this ground-water reservoir is designated as the unconsolidated aquifer. The map showing the saturated thickness of deposits in the unconsolidated aquifer was prepared by comparing maps showing the altitude and
Authors
Marilyn E. Pabst

Ground-water availability in the Hayes-Red Willow, Frenchman, and Meeker-Driftwood irrigation districts, southwest Nebraska Ground-water availability in the Hayes-Red Willow, Frenchman, and Meeker-Driftwood irrigation districts, southwest Nebraska

Surface-water supplies are diminishing in the Hitchcock-Red Willow and Frenchman Valley Irrigation Districts in southwest Nebraska. Stream depletions due to ground-water withdrawals upstream from Enders Reservoir (northwest of the study area) have resulted in a shortage of about 8,700 acre-feet per year. The availability of ground water to supply part of this deficit was examined. Two...
Authors
E.G. Lappala, P.F. Hemphill, R.E. Booker

January 1978 water levels, and data related to water-level changes since 1940 or 1950, western Kansas January 1978 water levels, and data related to water-level changes since 1940 or 1950, western Kansas

This report contains basic data on water-level measurements in observation wells in western Kansas. The measurements were made in mid-winter, mostly in January, when pumping was minimal and water levels had recovered from the effects of pumping during the previous irrigation season. This report also provides basic hydrologic data for relating water-level changes from a "base-reference...
Authors
Marilyn E. Pabst

Floods in Kansas City, Missouri and Kansas, September 12-13, 1977 Floods in Kansas City, Missouri and Kansas, September 12-13, 1977

The storm of September 12-13, 1977, produced as much as 16 inches of rainfall in the Kansas City, Missouri-Kansas area, left 25 persons dead, many homeless, and caused over 50 million dollars in damages. Data from National Weather Service recording rain gages indicate the storm came in two bursts within 24 hours. Flood hydrographs developed from streamflow records in the area also...
Authors
Leland D. Hauth, William J. Carswell

Description of data-collection system and synopsis of selected hydrologic data for Soldier Creek Basin, Kansas Description of data-collection system and synopsis of selected hydrologic data for Soldier Creek Basin, Kansas

Soldier Creek basin is a long, narrow basin encompassing an area of about 290 square miles almost directly north of Topeka, Kansas. A wide range of hydrologic data has been collected in the basin since the spring of 1964. These data include rainfall, stream discharge, sediment concentrations, chemical quality of water, and ground-water altitudes. The data collection system consists of 7...
Authors
William J. Carswell
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