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The Arkansas River valley is made up of the vast majority of usable ground drinking water while in the County, and the majority of the massive ground-drinking water materials are obtained from this spot. The amount of floor water in storage in the sediments of the valley is about 6.one million acre-toes if an assumed unique yield of 20 per cent for the sediments is suitable. This quantity of h2o will not represent the amount that would ultimately be withdrawn from the realm, but relatively a reserve which could be regulated to supply a perennial generate without the need of progressive depletion of storage if other hydrologic elements impacting the aquifer are acknowledged. Finally, the perennial field will depend upon the normal once-a-year recharge. Williams and Lohman (1949, p. 129) believed the net typical recharge inside the Arkansas Valley being about twenty percent from the annual precipitation or about 320 acre-ft for each square mile a year in decades of normal precipitation. Expertise has proven this recharge fee to get somewhere around suitable for the Wichita nicely-area location of Harvey County (Stramel, 1956). Nonetheless, this figure isn't going to bear in mind the concurrent natural discharge by seepage into streams and evapotranspiration, and if these losses from the bottom-h2o reservoir could be salvaged to be used, the helpful recharge level could be Significantly better.
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Generalized ground-water places and subareas within the County are shown on Figure 20 and are stated from the part with get more info the report that follows.
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Inside Subarea C1, drilled wells a lot less than 150 feet deep get hold of h2o from Answer openings in gypsum and anhydrite beds from the lower A part of the Wellington Formation. The drinking water is often less than artesian stress but flows in the floor in just a few destinations. Quite a few creeks within the subarea have Minimize into or close to the h2o-bearing, zone, and large springs and seeps supply a perennial stream during the creeks.