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WSP11713
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Last modified
1/26/2010 3:18:37 PM
Creation date
10/12/2006 5:07:42 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8112.600
Description
Arkansas White Red Basins Interagency Committee - AWRBIAC -- Reports
Basin
Arkansas
Water Division
2
Date
1/1/1978
Author
AWRBIAC
Title
Specific Problem Analysis Summary Report - 1975 National Assessment of Water and Related Land Resources - Part 2 of 2
Water Supply Pro - Doc Type
Report/Study
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<br />C) <br />(:"" ' <br />N <br />c.n <br />-..:! <br />I-L <br /> <br />Groundwater - The major aquifera of the region are the alluvium <br />and terrace deposits adjacent to the North Canadian River; the <br />Ogallala formation in Beaver, Cimarron and Texas Counties; and the <br />Dakota and Cheyenne sandstones in western Cimarron County. <br /> <br />Development and Utilization - As a result of the lack of de- <br />veloped surface water supplies, groundwater usage has intensified <br />and is utilized to a great extent. Evolution of irrigation began <br />in the 1930's with fewer than 30 wells. Augmentation of irriga- <br />tion wells continued at a slow rate until the year 1964. In 1960, <br />400 wells in the Panhandle provided.'water to irrigate an estimated <br />80,000 acres; by 1965 the number had more than doubled with about <br />975 wells irrigating 220,000 acres. In 1971 there were 1,846 wells <br />irrigating 344,040 acres. Today, approximately 2,200 high capacity <br />wells are irrigating over 400,000 acres and this development is <br />continuing to increase each year. 90% of the municipal and <br />industrial supplies and 80% of the irrigation supplies are pres- <br />ently being taken from groundwater sources. <br /> <br />Wells that are closely spaced and pumped for perIods of time <br />at hIgh rates (Irrigation wells) create a cone of depression sround <br />the pumped wells. As these extend outward, they overlsp each other <br />and reduce the quantity of water available to both wells. This <br />situation has become fairly common in heavily developed areas. <br />The greatest concentration of high capacity occurs in the areas <br />south of Guymon, north of Goodwell, and in the northwestern part <br />of Texas county. <br /> <br />The policies concerning and administration of groundwater in <br />Oklahoma is vested in the Oklahoma Water Resources Board under <br />suthority of Title 82 of the Oklahoma State Statutes. <br /> <br />The Oklahoma groundwater law was adopted on August 26, 1949, <br />wIth an effective date of July 1, 1973. Vested rights were granted <br />to those individuals and entities who had utIlized groundwater for <br />benefIcIal uses prIor to the effective date of the Oklahoma ground- <br />wate[' law. Groundwater usage is granted to Bny landowner for <br />domestiL usage without a permit. Usage greater than domestic <br />needs is approprIated and regulated through groundwater permits. <br />To conserve and protect the groundwater re90urces of the state <br />and to provide reasonable regulations for the taking and use of <br />groundwater are duties and responsibilities of the Oklahoma Water <br />Rcsources Board. <br /> <br />Due to large scale groundwater mining practices, the Oklahoma <br />Water Resources Board, when reasoned necessary and in the publit's <br />interest, can initiate the designation of critical groundwater <br />areas. After surveys of the designated c.ri.tic.al areas have been <br />completed, adjudication of rights is permitted to insure the <br />protection of designated critical areas. <br /> <br />111 <br />
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