Publications
Publications
Filter Total Items: 1258
Water in the Dakota Formation, Hodgeman and northern Ford Counties, southwestern Kansas Water in the Dakota Formation, Hodgeman and northern Ford Counties, southwestern Kansas
No abstract available.
Authors
David H. Lobmeyer, Edward C. Weakly
Hydrologic data for Soldier Creek Basin, Kansas Hydrologic data for Soldier Creek Basin, Kansas
Selected hydrologic data collected in the Soldier Creek basin in Kansas are available on magnetic tape in card-image format. Data on the tape include water discharge in fifteen-minute and daily time intervals; rainfall in fifteen-minute and daily time intervals; concentrations and particle sizes of suspended sediment; particle sizes of bed material; ground-water levels; and chemical...
Authors
William J. Carswell
A method for adjusting values of Manning's roughness coefficient for flooded urban areas A method for adjusting values of Manning's roughness coefficient for flooded urban areas
A method is presented for adjusting values of Manning's roughness coefficient for flooded urban areas on the basis of the density of buildings on a flood plain and verified roughness coefficients for natural conditions. An urban roughness coefficient can be calculated to emulate the water-surface profiles to within 0.06 meter for depths of flow less than 0.6 meter and plus or minus 10...
Authors
H. R. Hejl
Water-resources reconnaissance of Ness County, west-central Kansas Water-resources reconnaissance of Ness County, west-central Kansas
No abstract available.
Authors
Edward D. Jenkins, Marilyn E. Pabst
Geohydrology of the Great Bend Prairie, south-central Kansas Geohydrology of the Great Bend Prairie, south-central Kansas
No abstract available.
Authors
Stuart Wesley Fader, Lloyd E. Stullken
January 1977 water levels, and data related to water-level changes since 1950, western Kansas January 1977 water levels, and data related to water-level changes since 1950, western Kansas
This report contains basic data on water-level measurements in observation wells in western Kansas. Most of the measurements were made in January 1977; a few were made in December 1976 and in February 1977. The measurements were made in mid-winter when pumping was minimal and water levels had recovered from the effects of pumping during the previous irrigation season. This report also...
Authors
Marilyn E. Pabst
Movement of moisture in the unsaturated zone in a loess-mantled area, southwestern Kansas Movement of moisture in the unsaturated zone in a loess-mantled area, southwestern Kansas
A study of moisture movement associated with ponding near Garden City, Kansas, indicates that loess-manted areas have excellent potential for artificial recharge by water spreading. Infiltration stabilized at rates ranging from 0.7 to 2.2 feet (0.2 to 0.7 meter) per day reflecting changes in hydraulic conductivity of soil horizons. Results of the study indicate that the underlying loess...
Authors
Robert C. Prill
Water resources data for Kansas, water year 1976 Water resources data for Kansas, water year 1976
Water resources data for the 1976 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 148 gaging stations; stage and contents for 20 lakes and reservoirs; water quality for 67 gaging stations and 2...
Authors
Water Resources Division U.S. Geological Survey
Changes in the water supply in the Upper Republican Natural Resources District, Southwest Nebraska, from 1952-75 Changes in the water supply in the Upper Republican Natural Resources District, Southwest Nebraska, from 1952-75
Use of ground water for irrigation has increased rapidly in the Upper Republican Natural Resources District in southwestern Nebraska in recent years. The principal aquifer being developed is composed of saturated and gravel of the Ogallala Formation of Tertiary age. Water-level declines of as much as 16 feet (4.9 meters) have occurred. Base flow of major streams draining the aquifer was...
Authors
E.G. Lappala
Saline water in the Little Arkansas River Basin area, south-central Kansas Saline water in the Little Arkansas River Basin area, south-central Kansas
Ground water in unconsolidated deposits of Pleistocene age in part of the Little Arkansas River basin has been polluted by the influx of saline water. The source of the saline water generally is oil-field brine that leaked from disposal ponds on the land surface. Locally, pollution by saline water also has been caused by upwelling of oil-field brine injected under pressure into the "lost
Authors
Robert B. Leonard, Melvin K. Kleinschmidt
Water resources data for Kansas, water year 1975 Water resources data for Kansas, water year 1975
Water resources data for the 1975 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 143 gaging stations; stage and contents for 20 lakes and reservoirs; water quality for 69 gaging stations; and...
Authors
Water Resources Division U.S. Geological Survey