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Publications
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Real-time water-quality monitoring for protection of wildlife at Quivira National Wildlife Refuge, South-Central Kansas Real-time water-quality monitoring for protection of wildlife at Quivira National Wildlife Refuge, South-Central Kansas
Stream stage and discharge and the quality of water flowing from Rattlesnake Creek into the Quivira National Wildlife Refuge in south-central Kansas are being monitored by the U.S. Geological Survey in cooperation with the U.S. Fish and Wildlife Service using an innovative, real-time monitoring approach. Continuously recorded data and data from periodic collection of water-quality...
Authors
Victoria G. Christensen
Occurrence of dissolved solids, nutrients, pesticides, and fecal coliform bacteria during low flow in the Marion Lake watershed, central Kansas, 1998 Occurrence of dissolved solids, nutrients, pesticides, and fecal coliform bacteria during low flow in the Marion Lake watershed, central Kansas, 1998
No abstract available.
Authors
David P. Mau, Larry M. Pope
Water Resources Data, Kansas, Water Year 1998 Water Resources Data, Kansas, Water Year 1998
Water-resources data for the 1998 water year for Kansas consist of records of stage, discharge, and water quality of streams; elevation and contents of lakes and reservoirs; and water levels of ground-water wells. This report contains records for water discharge at 149 gaging stations; elevation and contents at 19 watershed lakes and reservoirs; and water-level data at 19 wells. Also...
Authors
J.E. Putnam, D.L. Lacock, D.R. Schneider, M.D. Carlson
Estimation of potential runoff-contributing areas in the Kansas-Lower Republican River basin, Kansas Estimation of potential runoff-contributing areas in the Kansas-Lower Republican River basin, Kansas
Digital soils and topographic data were used to estimate and compare potential runoff-contributing areas for 19 selected subbasins representing soil, slope, and runoff variability within the Kansas-Lower Republican (KLR) River Basin. Potential runoff-contributing areas were estimated separately and collectively for the processes of infiltration-excess and saturation-excess overland flow...
Authors
Kyle E. Juracek
Digital map of water-level changes in the High Plains Aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming, 1980 to 1994 Digital map of water-level changes in the High Plains Aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming, 1980 to 1994
This data set consists of digital water-level-change contour for the High Plains aquifer in the Central United States, 1980 to 1994. The High Plains aquifer extends from south of 32 degrees to almost 44 degrees north latitude and from 96 degrees 30 minutes to 104 degrees west longitude. The aquifer underlies about 174,000 square miles in parts of Colorado, Kansas, Nebraska, New Mexico...
Authors
Brian C. Fischer, Virginia L. McGuire
Water use in Kansas, 1990 and 1995 Water use in Kansas, 1990 and 1995
This fact sheet illustrates comparative water use from ground and surface sources for 1990 and 1995 for the largest categories of use in Kansas: public supply, irrigation, industrial and mining, livestock, and thermoelectric power generation. Total populations, including those served by public-water suppliers and those using private wells, also are illustrated. These data are organized...
Authors
J. F. Kenny
General-circulation-model simulations of future snowpack in the western United States General-circulation-model simulations of future snowpack in the western United States
April 1 snowpack accumulations measured at 311 snow courses in the western United States (U.S.) are grouped using a correlation-based cluster analysis. A conceptual snow accumulation and melt model and monthly temperature and precipitation for each cluster are used to estimate cluster-average April 1 snowpack. The conceptual snow model is subsequently used to estimate future snowpack by...
Authors
G.J. McCabe, D.M. Wolock
Surface water-ground water interaction: Herbicide transport into municipal collector wells Surface water-ground water interaction: Herbicide transport into municipal collector wells
During spring runoff events, herbicides in the Platte River are transported through an alluvial aquifer into collector wells located on an island in the river in 6 to 7 d. During two spring runoff events in 1995 and 1996, atrazine [2-chloro-4-ethylamino-6-isopropylamino-s-triazine] concentrations in water from these wells reached approximately 7 µg/L, 70 times more than the background
Authors
Ingrid M. Verstraeten, J.D. Carr, G. V. Steele, E.M. Thurman, K.C. Bastian, D.F. Dormedy
Water-Level Changes, 1980 to 1997, and Saturated Thickness, 1996-97, In the High Plains Aquifer Water-Level Changes, 1980 to 1997, and Saturated Thickness, 1996-97, In the High Plains Aquifer
The High Plains aquifer underlies one of the major agricultural regions in the world, including parts of eight States--Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. In the area underlain by the High Plains aquifer (called the High Plains region in this report), the total number of acres irrigated with ground water expanded rapidly after 1940: 1949--2...
Authors
Virginia L. McGuire, B.C. Fischer, C.P. Stanton
Geomorphic effects of overflow dams on the lower Neosho River, Kansas Geomorphic effects of overflow dams on the lower Neosho River, Kansas
The purpose of this report is to characterize the geomorphic (channel-changing) effects of overflow dams on the lower Neosho River channel in southeastern Kansas. Specifically, the report describes the types, upstream and downstream extents, and stability of the geomorphic effects in relation to site-specific, human-caused and natural conditions that may affect the channel’s response to...
Authors
Kyle E. Juracek
Estimation of potential runoff-contributing areas in Kansas using topographic and soil information Estimation of potential runoff-contributing areas in Kansas using topographic and soil information
Digital topographic and soil information was used to estimate potential runoff-contributing areas throughout Kansas. The results then were used to compare 91 selected subbasins representing soil, slope, and runoff variability. Potential runoff-contributing areas were estimated collectively for the processes of infiltration-excess and saturation-excess overland flow using a set of...
Authors
Kyle E. Juracek
Metolachlor and its metabolites in tile drain and stream runoff in the canajoharie creek watershed Metolachlor and its metabolites in tile drain and stream runoff in the canajoharie creek watershed
Water samples collected during April−November 1997 from tile drains beneath cultivated fields in central New York indicate that two metabolites of the herbicide metolachlormetolachlor ESA (ethanesulfonic acid) and OA (oxanilic acid)can persist in agricultural soils for 4 or more years after application and that fine-grained soils favor the transport of metolachlor ESA over metolachlor...
Authors
P. J. Phillips, G. R. Wall, E.M. Thurman, D. A. Eckhardt, J. Vanhoesen