Publications
Publications
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Multiyear Low Flow Of Streams In Northeastern Kansas Multiyear Low Flow Of Streams In Northeastern Kansas
Many existing water supplies in northeastern Kansas are proving inadequate to meet current and expanded future needs. One of the methods by which the use of highly variable streamflow in the area can be evaluated is with the aid of multiyear low-flow frequency information. Using data form 19 streamflow-gaging stations in the study area, maps were developed from which the mean annual...
Authors
W. J. Carswell, S.V. Bond
Statistical summaries of water-quality data for streams draining coal-mined areas, southeastern Kansas Statistical summaries of water-quality data for streams draining coal-mined areas, southeastern Kansas
Summaries of descriptive statistics are compiled for 14 data-collection sites located on streams draining areas that have been shaft mined and strip mined for coal in Cherokee and Crawford Counties in southeastern Kansas. These summaries include water-quality data collected from October 1976 through April 1979. Regression equations relating specific conductance and instantaneous...
Authors
Hugh E. Bevans, Arthur M. Diaz
Simulated water-level declines near Marienthal, west-central Kansas Simulated water-level declines near Marienthal, west-central Kansas
Intensive study in an area of 12-square miles near Marienthal, Kansas, has shown a decrease of 30 to 50 percent in saturated thickness of the Ogallala Formation since the development of irrigation. Projections from a digital model indicated the additional water-level declines that might occur from 1978 to 1989 if the pumpage in the model area was assumed to be one-half, equal to, or...
Authors
Lloyd E. Dunlap
Geohydrology and model analysis for water-supply management in a small area of west-central Kansas Geohydrology and model analysis for water-supply management in a small area of west-central Kansas
The Ogallala Formation in the intensive-study area, an area of 12 square miles in northeastern Wichita County, west-central Kansas, has had a substantial decrease in saturated thickness since the development of irrigation. The annual water-level decline during 1950-78 ranged from 1.08 to 2.22 feet per year. The hydrologic system was investigated to study methods of conserving the...
Authors
Lloyd E. Dunlap, Jack Kume, James G. Thomas
January 1980 water levels, and data related to water-level changes, western and south-central Kansas January 1980 water levels, and data related to water-level changes, western and south-central Kansas
This report contains hydrologic data on water-level measurements in observation wells in western and south-central 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...
Authors
M.E. Pabst
Particle-size analyses of bed and bank material from channels of the Missouri River basin Particle-size analyses of bed and bank material from channels of the Missouri River basin
No abstract available.
Authors
W. R. Osterkamp, A.G. Wiseman
A procedure for predicting concentrations of dissolved solids and sulfate ion in streams draining areas strip mined for coal A procedure for predicting concentrations of dissolved solids and sulfate ion in streams draining areas strip mined for coal
Current trends in increased coal production neccessitate the development of techniques to appraise the environmental degradation that results from strip mining. A procedure is introduced for the prediction of dissolved-solids and sulfate-ion concentrations in streams draining strip-mined areas as functions of the percentage of the drainage area that has been strip mined. These...
Authors
Hugh E. Bevans
The use of minicomputers in a distributed information processing system; feasibility study The use of minicomputers in a distributed information processing system; feasibility study
No abstract available.
Authors
Stanley Miller Longwill, Jesse M. McNellis, Douglas R. Posson
Water Resources Data for Kansas, Water Year 1978 Water Resources Data for Kansas, Water Year 1978
No abstract available.
Authors
Water Resources Division U.S. Geological Survey
Maps showing saturated thickness, January 1979, and percentage decrease in saturated thickness, 1950-79, of unconsolidated aquifer, west-central Kansas Maps showing saturated thickness, January 1979, and percentage decrease in saturated thickness, 1950-79, of unconsolidated aquifer, west-central Kansas
The principal water-yielding formation (unconsolidated aquifer) supplying water to wells in west-central Kansas is comprised of the Ogallala Formation and undifferentiated Pleistocene deposits. About 1,860 square miles of the area are underlain by sufficient saturated material to supply groundwater for irrigation. Saturated thickness in the area ranges from less than 50 feet to about 270...
Authors
Marilyn E. Pabst
Relation of sediment yield to climatic and physical characteristics in the Missouri River basin Relation of sediment yield to climatic and physical characteristics in the Missouri River basin
Data from 64 stream-sediment stations and reservoirs in the plains area and from 15 stream-sediment stations in the mountainous area were analyzed to determine the relation of sediment yield to basin characteristics. Data from each sediment station and reservoir represented at least 7 years of sediment discharge in the plains area or 4 years of sediment discharge in the mountainous area...
Authors
P. R. Jordan
Evaluation of methods for estimating ground-water withdrawals in western Kansas Evaluation of methods for estimating ground-water withdrawals in western Kansas
During 1978, methods of estimating ground-water withdrawals in western Kansas were examined and evaluated, using both existing data from the files of the U.S. Geological Survey and newly collected data. Values for annual ground-water withdrawals reported to the Division of Water Resources, Kansas State Board of Agriculture, by water users probably contain substantial errors because most...
Authors
Claud H. Baker