The Arkansas River valley includes a lot of the usable floor drinking water in the County, and the vast majority of massive ground-water provides are obtained from this place. The amount of floor h2o in storage throughout the sediments in the valley is about 6.1 million acre-ft if an assumed unique yield of twenty % for your sediments is appropriate. This volume of h2o won't symbolize the amount that could eventually be withdrawn from the area, but fairly a reserve that might be controlled to deliver a perennial generate without progressive depletion of storage if other hydrologic things influencing the aquifer are acknowledged. In the long run, the perennial subject will rely upon the average once-a-year recharge. Williams and Lohman (1949, p. 129) estimated The web common recharge during the Arkansas Valley to be about 20 percent in the once-a-year precipitation or about 320 acre-toes per square mile each year in yrs of typical precipitation. Expertise has shown this recharge amount being about correct for your Wichita very well-field location of Harvey County (Stramel, 1956). On the other hand, this figure doesn't bear in mind the concurrent organic discharge by seepage into streams and evapotranspiration, and if these losses from the ground-drinking water reservoir may be salvaged for use, the productive recharge fee might be A lot better.
The floor of most of the Ninnescah-Wellington Upland is underlain by loess, which overlies sand and gravel partially of the realm. The bedrock area could be the Wellington Formation in about the eastern one particular-third plus the Ninnescah Shale in the western two-thirds.
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The sand thickness contour map was ready by contouring factors of equal sand thickness received from logs of wells and test holes and does not include things like silt and clay beds which were current at the well web site. The transmissibility map was well prepared by implementing permeability values acquired from picked pumping checks in the region into the sand and gravel thickness as recorded from the logs of wells and test holes for people formations for which samples had been available. In A lot of Arkansas Valley, particularly where by the entire sand and gravel thickness is greatest, the permeability of those sediments decreases with depth. The permeability price applied to someone sand and gravel bed in a well or exam-hole web page was determined by a comparison on the lithology of the bed with that of similar sediments from wells the place permeability info derived from pumping checks have been out there.
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In Subarea C1, drilled wells lower than a hundred and fifty ft deep get hold of drinking water from Remedy openings in gypsum and anhydrite beds within the lower Component of the Wellington Development. The water is usually below artesian stress but flows within the floor in just a few destinations. Many creeks inside the subarea have Slash into or close to the water-bearing, zone, and large springs and seeps offer a perennial move from the creeks.
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The Arkansas Valley is characterized by its Severe flatness and the badly created floor drainage on the land flanking the Arkansas River. The area is underlain by alluvial sediments of Pliocene to Current age which have been the most efficient water-bearing rocks inside the County.