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The Arkansas River valley is made up of the vast majority of usable floor water within the County, and many of the substantial floor-h2o materials are attained from this area. The quantity of ground water in storage within the sediments from the valley is about 6.1 million acre-ft if an assumed certain produce of twenty % for that sediments is accurate. This quantity of drinking water won't characterize the quantity that would finally be withdrawn from the region, but alternatively a reserve which could be controlled to supply a perennial yield with out progressive depletion of storage if other hydrologic elements affecting the aquifer are known. Ultimately, the perennial field will depend on the average annual recharge. Williams and Lohman (1949, p. 129) believed The online regular recharge while in the Arkansas Valley to get about 20 percent of the once-a-year precipitation or about 320 acre-toes for each square mile per year in a long time of usual precipitation. Working experience has demonstrated this recharge fee being close to right to the Wichita perfectly-industry place of Harvey County (Stramel, 1956). On the other hand, this figure will not keep in mind the concurrent all-natural discharge by seepage into streams and evapotranspiration, and if these losses from more info the bottom-drinking water reservoir might be salvaged to be used, the productive recharge charge could well be A great deal increased.
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The Arkansas Valley is characterized by its Intense flatness as well as the badly created surface drainage from the land flanking the Arkansas River. The area is underlain by alluvial sediments of Pliocene to Recent age which have been the most efficient drinking water-bearing rocks from the County.
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The event of floor h2o, inside Subarea D2 is not uniform; usually effectively yields are small, but suitable for farm and domestic use. The land surface inside the subarea slopes toward the foremost streams and is underlain in part by loess and several colluvium and domestically by just a soil more than bedrock. The northeastern part of the subarea flanking the Arkansas Valley is underlain by loess that regionally attains a thickness of about seventy five ft and includes sandy zones close to the base. The decrease Element of the loess is saturated, and wells penetrating sandy zones get hold of sufficient drinking water for domestic and stock use. In those aspects of Subarea D2 flanking the Ninnescah Valley, the loess and colluvium are slender, along with the drinking water table is commonly in bedrock.
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