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Publications
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Paleohydrology of the Anadarko Basin, central United States Paleohydrology of the Anadarko Basin, central United States
Geohydrologic systems in the Anadarko basin in the central United States are controlled by topography, climate, geologic structures, and aquifer hydraulic properties, all of which are the result of past geologic and hydrologic processes, including tectonics and diagenesis. From Late Cambrian through Middle Ordovician time, a generally transgressive but cyclic sea covered the area. The...
Authors
Donald G. Jorgensen
Accounting for intracell flow in models with emphasis on water table recharge and stream-aquifer interaction: 2. A procedure Accounting for intracell flow in models with emphasis on water table recharge and stream-aquifer interaction: 2. A procedure
Intercepted intracell flow, especially if cell includes water table recharge and a stream ((sink), can result in significant model error if not accounted for. A procedure utilizing net flow per cell (Fn) that accounts for intercepted intracell flow can be used for both steady state and transient simulations. Germane to the procedure is the determination of the ratio of area of influence...
Authors
Donald G. Jorgensen, Donald C. Signor, Jeffrey L. Imes
Load-detention efficiencies in a dry-pond basin Load-detention efficiencies in a dry-pond basin
Inflow and outflow to a dry-pond detention basin in Topeka, Kansas, were monitored for 19 storms during a 14-month period. Samples of runoff were collected automatically at two inflow and one outflow locations. Inflow and outflow constituent loads were computed with subsequent computation of load-detention efficiencies. Three constituents (dissolved solids, ammonia plus organic nitrogen...
Authors
Larry M. Pope, Larry G. Hess
Simulation of precipitation by weather-type analysis Simulation of precipitation by weather-type analysis
A new approach that uses weather-type analysis as a basis for stochastic precipitation modeling was developed and tested for Philadelphia, Pennsylvania. The weather types permit the identification of weather conditions associated with varying frequencies, intensities, and amounts of precipitation. Weather-type frequencies were used to stochastically simulate precipitation for...
Authors
G. J. McCabe, L.E. Hay, L.S. Kalkstein, M. A. Ayers, D.M. Wolock
Water resources data, Kansas, water year 1988 Water resources data, Kansas, water year 1988
No abstract available.
Authors
C.O. Geiger, D.L. Lacock, D.R. Schneider, M.D. Carlson, C.E. Merry
Hydrogeology and ground-water-quality conditions at the Geary County landfill, northeast Kansas, 1988 Hydrogeology and ground-water-quality conditions at the Geary County landfill, northeast Kansas, 1988
Chemical analysis of water from monitoring wells upgradient and downgradient of the Geary County Landfill in Kansas near Junction City indicate the presence of several chemically distinct water types. For the dominant calcium bicarbonate water type, concentrations of inorganic and organic constituents indicate the presence of reducing conditions within the landfill and increased...
Authors
N. C. Myers, P. R. Bigsby
Water resources of Sedgwick County, Kansas Water resources of Sedgwick County, Kansas
Hydrologic data from streams, impoundments, and wells are interpreted to: (1) document water resources characteristics; (2) describe causes and extent of changes in water resources characteristics; and (3) evaluate water resources as sources of supply. During 1985, about 134,200 acre-ft of water (84% groundwater) were used for public (42%), irrigation, (40%), industrial (14%), and...
Authors
H.E. Bevans
Statistical summaries of elemental constituents in streambed-sediments in the lower Kansas River basin; Nebraska, Kansas, and Missouri Statistical summaries of elemental constituents in streambed-sediments in the lower Kansas River basin; Nebraska, Kansas, and Missouri
No abstract available.
Authors
Jean L. Ryder, R. F. Sanzolone
Water supply and demand in Sedgwick County, Kansas Water supply and demand in Sedgwick County, Kansas
Water supplies in Sedgwick County, Kansas, are derived from surface--and groundwater resources. During 1985, public supply, irrigation, and self-supplied industry required 38% of the 56 ,500 acre-ft of appropriated surface water and 57% of the 187 ,800 acre-ft of appropriated groundwater. If the historic (1920-80) annual population growth rate (2.8%) continues, the 126,100 acre ft of...
Authors
Hugh E. Bevans
Water resources data, Kansas, water year 1987 Water resources data, Kansas, water year 1987
Water-resources data for the 1987 water year for Kansas consist of records of stage, discharge, and water quality of streams; elevation, contents, and water quality of lakes or reservoirs; and water levels and water quality of ground-water wells. This report contains records for water discharge at 140 gaging stations; elevation and contents at 24 lakes or reservoirs; water quality at 31...
Authors
C.O. Geiger, D.L. Lacock, J.E. Putnam, C.E. Merry, D.R. Schneider
Hydrologic maps of the High Plains Aquifer, southwestern Kansas, January 1986 Hydrologic maps of the High Plains Aquifer, southwestern Kansas, January 1986
No abstract available.
Authors
Lloyd E. Stullken
Effects of future ground-water pumpage on the High Plains Aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming Effects of future ground-water pumpage on 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