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Geohydrology of southwestern Kansas Geohydrology of southwestern Kansas

Southwestern Kansas is one of the principal areas of ground-water development for irrigation in the State, and many reports are available concerning ground-water conditions in the area. The purposes of this investigation were to consolidate and update data, to determine the extent and effects of irrigation development on the ground-water resource, to determine the chemical quality of the...
Authors
Edwin D. Gutentag, David H. Lobmeyer, Steven E. Slagle

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

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

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

Variation of alluvial-channel width with discharge and character of sediment Variation of alluvial-channel width with discharge and character of sediment

Use of channel measurements to estimate discharge characteristics of alluvial streams has shown that little agreement exists for the exponent of the width-discharge relation. For the equation Q = aWAb, where Q is mean discharge and WA is active-channel width, it is proposed that the exponent, b, should be of fixed value for most natural, perennial, alluvial stream channels and that the...
Authors
W. R. Osterkamp

Water-resources investigations in Kansas; fiscal year 1978 Water-resources investigations in Kansas; fiscal year 1978

Hydrologic investigations in Kansas during fiscal year 1978 consisted of collecting and analyzing data to assess the State 's water resources, describe the framework of hydrologic systems , and provide quantity and quality of water data for optimum development and management. Surface-water studies were made to analyze long-term records of streamflow, basin and stream-channel...
Authors
Harold E. McGovern, L. J. Combs

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

January 1979 water levels, and data related to water-level changes, western and south-central Kansas January 1979 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
Marilyn E. Pabst

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

Multiyear low flow in southeastern Kansas Multiyear low flow in southeastern Kansas

Many existing water supplies in southeastern Kansas are proving inadequate to meet current and expanded future needs. One of the methods in which the use of highly variable streamflow in the area can be evaluated is with the aid of multiyear low-flow frequency information. Data from 19 stream-gaging stations in the study area and a base period of 1940-77 were used to develop maps from...
Authors
William J. Carswell

Methods for determination of inorganic substances in water and fluvial sediments Methods for determination of inorganic substances in water and fluvial sediments

Chapter Al of the manual contains methods used by the U.S. Geological Survey to collect, preserve, and analyze water samples for their content of dissolved minerals and gases. Among the topics discussed are selection of sampling sites, frequency of sampling, sampling equipment, sample preservation, laboratory equipment and instrumental techniques, accuracy and precision of analysis, and...
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