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Selected hydrologic relationships for Soldier Creek, northeastern Kansas Selected hydrologic relationships for Soldier Creek, northeastern Kansas

Hydrologic data from Soldier Creek basin were compared with relations from statewide data. The quantity and quality of streamflow were affected mostly by soils, slopes, and land use. Average annual precipitation during the study (196476) was 35.12 inches, or 2.3 percent greater than the long-term (1929-76) average. The average streamflow in Soldier Creek at Topeka, Kansas, was 23 percent...
Authors
William J. Carswell

Preliminary data from Arbuckle test wells, Miami, Douglas, Saline, and Labette counties, Kansas Preliminary data from Arbuckle test wells, Miami, Douglas, Saline, and Labette counties, Kansas

Preliminary data are presented for test wells in Kansas that were completed in Cambrian and Ordovician rocks of the Arbuckle Group in late 1979 and early 1980. Included in the report are hole history, electrical logs, geology (sample descriptions and cores), hydrologic testing, and geochemistry. These wells were drilled as part of a cooperative investigation between the U.S. Geological...
Authors
Tony Gogel

Geohydrology of southwestern Kansas Geohydrology of southwestern Kansas

No abstract available.
Authors
Edwin D. Gutentag, David H. Lobmeyer, Steven E. Slagle

Analysis and computer simulation of stream-aquifer hydrology, Arkansas River valley, southwestern Kansas Analysis and computer simulation of stream-aquifer hydrology, Arkansas River valley, southwestern Kansas

A study was made, in cooperation with the Division of Water Resources, Kansas State Board of Agriculture, to determine geohydrologic conditions underlying nearly 110,000 acres of the Arkansas River Valley between the Colorado-Kansas State line and the Bear Creek Fault zone in southwestern Kansas. The Arkansas River meanders atop and interacts hydraulically with the area's unconfined sand...
Authors
R.A. Barker, Lloyd E. Dunlap, C. G. Sauer

Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980 Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980

The High Plains aquifer in Kansas is part of a regional system that extends into Colorado, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part of the State. This aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits. In western Kansas, the...
Authors
Marilyn E. Pabst, Lloyd E. Stullken

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

Evaluating methods for determining water use in the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming, 1979 Evaluating methods for determining water use in the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming, 1979

The volume and areal distribution of ground-water withdrawals (pumpage) for irrigation during 1980 are required for the High Plains Regional Aquifer-System Analysis. In 1979, approaches and instrumentation that might be suitable for application to 1980 water-use determinations were tested. Pumpage was sampled by monitoring time of operation and discharge of irrigation wells during the...
Authors
Frederick J. Heimes, Richard R. Luckey

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

Preliminary analysis of regional-precipitation periodicity Preliminary analysis of regional-precipitation periodicity

Precipitation variability plays a major role in nearly every aspect of the hydrologic cycle. Precipitation is not a random event, but it occurs after a sequence of prerequi-sites has been fulfilled. Recent investigations have shown that activity of the sun can affect atmospheric vorticity, an important factor in precipitation formation. Solar activity is known to be periodic; therefore...
Authors
Charles A. Perry
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