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The Arkansas River valley is made up of most of the usable ground water inside the County, and almost all of the significant floor-h2o materials are obtained from this region. The quantity of floor h2o in storage within the sediments in the valley is about 6.1 million acre-ft if an assumed distinct produce of twenty per cent for the sediments is right. This volume of water will not depict the amount that can finally be withdrawn from the region, but rather a reserve that may be regulated to provide a perennial generate without the need of progressive depletion of storage if other hydrologic elements affecting the aquifer are identified. Finally, the perennial industry will depend on the average annual recharge. Williams and Lohman (1949, p. 129) estimated the net average recharge in the Arkansas Valley to be about twenty % with the yearly precipitation or about 320 acre-ft per sq. mile every year in yrs of typical precipitation. Encounter has proven this recharge rate to become roughly correct with the Wichita perfectly-subject place of Harvey County (Stramel, 1956). On the other hand, this determine doesn't take into consideration the concurrent organic discharge by seepage into streams and evapotranspiration, and when these losses from the bottom-h2o reservoir can be salvaged to be used, the efficient recharge amount would be much bigger.
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Wells penetrating the Ninnescah Shale are often under 100 feet in depth, and the h2o is thought to happen in crevices, Answer openings, and bedding planes within the weathered part of the development. Very well yields with the Ninnescah Shale normally are greater than from your Wellington Formation and may range between one gpm to approximately 75 gpm according to the quantity of openings penetrated by the perfectly. The very well produce that might be envisioned at a certain area cannot be predicted, but a source enough for domestic and stock use could be developed in almost all of the subarea.
The region has become divided into two subareas on The premise on the occurrence of floor drinking water. The two subareas are revealed on Figure twenty since the Loess-sand Subarea (D1) as well as the Loess-shale Subarea (D2). Subarea D1 is largely confined to your uplands but does incorporate the tiny deserted valley from the southwest corner in the County where floor-water conditions are very similar. Inside of Subarea D1 the surface substance is loess that ranges in thickness from the featheredge to about 40 toes. The loess is underlain by deposits of sand and gravel containing some silt.