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The Arkansas River valley includes most of the usable ground water inside the County, and almost all of the significant ground-h2o supplies are acquired from this location. The quantity of ground drinking water in storage in the sediments of your valley is about 6.1 million acre-feet if an assumed particular yield of 20 % for your sediments is accurate. This quantity of h2o won't characterize the quantity which could finally be withdrawn from the area, but instead a reserve that might be regulated to provide a perennial yield without progressive depletion of storage if other hydrologic aspects impacting the aquifer are identified. In the end, the perennial area will rely on the typical annual recharge. Williams and Lohman (1949, p. 129) estimated The online normal recharge from the Arkansas Valley being about twenty per cent in the yearly precipitation or about 320 acre-ft per square mile per annum in decades of ordinary precipitation. Working experience has revealed this recharge level being somewhere around proper to the Wichita effectively-area region of Harvey County (Stramel, 1956). Nevertheless, this determine would not bear in mind the concurrent normal discharge by seepage into streams and evapotranspiration, and if these losses from the ground-h2o reservoir can be salvaged to be used, the successful recharge rate could well be Substantially increased.

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The sand thickness contour map was geared up by contouring factors of equal sand thickness received from logs of wells and examination holes and isn't going to incorporate silt and clay beds which were existing for the very well web-site. The transmissibility map was ready by applying permeability values obtained from selected pumping tests in the area into the sand and gravel thickness as recorded during the logs of wells and check holes for people formations for which samples ended up obtainable. In Significantly of Arkansas Valley, notably where the overall sand and gravel thickness is best, the permeability of those sediments decreases with depth. The permeability value applied to someone sand and gravel mattress in a properly or check-gap web-site was determined by a comparison on the lithology in the mattress with that of comparable sediments from wells where permeability information derived from pumping checks ended up offered.

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