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January 1986 water levels, and data related to water-level changes, western and south-central Kansas January 1986 water levels, and data related to water-level changes, western and south-central Kansas
Hydrologic data related to water level measurements were made in observation wells in western and south-central Kansas. The measurements were made in midwinter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water-level changes from a ' base...
Authors
B.J. Dague
Altitude and configuration of the water table in the High Plains regional aquifer system of Kansas, 1975 Altitude and configuration of the water table in the High Plains regional aquifer system of Kansas, 1975
No abstract available.
Authors
Lloyd E. Stullken, Marilyn E. Pabst
Geohydrology of and potential for fluid disposal in the Arbuckle Aquifer in Kansas Geohydrology of and potential for fluid disposal in the Arbuckle Aquifer in Kansas
The Arbuckle aquifer is an extensive aquifer that contains mostly saline water and that immediately overlies Precambrian ' basement ' rocks throughout Kansas, except for major uplift areas where it has been removed by erosion. In the southeast part of the state, it is a major freshwater aquifer. The upper part of the Arbuckle contains significant oil and gas reservoirs in central and...
Authors
J. E. Carr, H.E. McGovern, Tony Gogel, J.H. Doveton
Hydrologic characteristics of soils in parts of Arkansas, Colorado, Kansas, Missouri, Nebraska, New Mexico, Oklahoma, South Dakota, and Texas Hydrologic characteristics of soils in parts of Arkansas, Colorado, Kansas, Missouri, Nebraska, New Mexico, Oklahoma, South Dakota, and Texas
Certain physical characteristics of soils, including permeability, available water capacity, thickness, and topographic position, have a definite effect on the hydrology of an area. They control the rate at which precipitation infiltrates or is transmitted through the soil, and thus they have a significant role in determining the rates both of ground-water recharge and surface runoff. In...
Authors
Jack T. Dugan
Selected papers in the hydrologic sciences, 1986 Selected papers in the hydrologic sciences, 1986
West Point Reservoir is a multiple-purpose project on the Chattahoochee River about 112 river kilometers downstream from Atlanta on the Alabama-Georgia border. Urbanization has placed large demands on the Chattahoochee River, and water quality below Atlanta was degraded even before impoundment. Water-quality, bottom-sediment, and fish-tissue samples were collected from the reservoir to...
Two-hundred years of hydrogeology in the United States Two-hundred years of hydrogeology in the United States
The Hydrogeology Division of the Geological Society of America (GSA) sponsored a symposium entitled ' Hydrogeology in the United States, 1776- 1976 ' at the annual meeting of the GSA on November 9, 1976. The symposium was organized to provide a forum for discussion of major eras in the history of American hydrogeology and to contribute to the bicentennial celebration of the founding of...
Authors
J.E. Moore, S. W. Lohman, E.B. Chase
Water resources data, Kansas, water year 1985 Water resources data, Kansas, water year 1985
No abstract available.
Authors
C.O. Geiger, D.L. Lacock, J.E. Putnam, B.L. Riche, C.E. Merry
Digital simulation of ground-water flow in the High Plains Aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming Digital simulation of ground-water flow in the High Plains Aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming
No abstract available.
Authors
R. R. Luckey, E. D. Gutentag, F.J. Heimes, J.B. Weeks
Altitude and configuration of the water table in the High Plains Aquifer in Kansas, 1960 Altitude and configuration of the water table in the High Plains Aquifer in Kansas, 1960
The High Plains aquifer in Kansas is part of a regional aquifer 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. The aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits. In western...
Authors
Marilyn E. Pabst, Lloyd E. Stullken
Availability of water for irrigation in the South Fork Solomon River Valley, Webster Reservoir to Waconda Lake, north-central Kansas Availability of water for irrigation in the South Fork Solomon River Valley, Webster Reservoir to Waconda Lake, north-central Kansas
No abstract available.
Authors
Robert D. Burnett, Thomas B. Reed
National water summary 1984: Hydrologic events, selected water-quality trends, and ground-water resources National water summary 1984: Hydrologic events, selected water-quality trends, and ground-water resources
Water year 1984 was a year of extreme hydrologic conditions. For the third consecutive year, precipitation and resulting runoff were well above long-term averages in most of the Nation and as much as 400 percent above average in the Southwest. National flood damages during the year were the third highest in a 10-year period (1975-84) an estimated $3.5 to $4 billion. In many of the larger...
Authors
By
Water Resources Mission Area, Oklahoma-Texas Water Science Center, Pennsylvania Water Science Center, Utah Water Science Center, Dakota Water Science Center, Central Midwest Water Science Center, Upper Midwest Environmental Sciences Center, Upper Midwest Water Science Center, Central Plains Water Science Center
Design of a sediment data-collection program in Kansas as affected by time trends Design of a sediment data-collection program in Kansas as affected by time trends
Data collection programs need to be re-examined periodically in order to insure their usefulness, efficiency, and applicability. The possibility of time trends in sediment concentration, in particular, makes the examination with new statistical techniques desirable. After adjusting sediment concentrations for their relation to streamflow rates and by using a seasonal adaptation of...
Authors
P. R. Jordan