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<br />Table 3 <br />Groundwater Recharge (1,000 Acre-Feet) <br />By County and Aquifer <br />Kansas, 1984 <br />(conto) <br /> <br /> <br /> Aquifer <br /> .-- - <br /> High Great Ozark <br />County Alluvial Glacial Plains Plains Plateau <br />Stafford 0 0 80 0 0 <br />Stanton 0 0 14 0 0 <br />Stevens 0 0 29 0 0 <br />Sumner 83 0 3 0 0 <br />Thomas 0 0 28 0 0 <br />Trego 4 0 13 0 0 <br />Wabaunsee 22 2 0 0 0 <br />Wallace 1 0 13 0 0 <br />Washington 12 3 0 73 0 <br />Wichita 0 0 18 0 0 <br />Wilson 3.1- 0 0 0 0 <br />Woodson 8 0 0 0 0 <br />Wyandotte 14 19 0 0 0 <br />Total 1,466 673 1,525 322 0 <br /> L" <br /> <br />Total <br /> <br />80 <br />14 <br />29 <br />86 <br />28 <br />17 <br />24 <br />14 <br />88 <br />18 <br />31 <br />8 <br />33 <br />3,986 <br /> <br />During the preparation of Table 3, separate estimates were made <br />for the portion of each county that lies within more than one <br />river basino Hence, in these cases, county totals were found by <br />adding the individual estimates for each county-river basin area <br />that were wi thin the specific county of interest. Likewise, <br />river basin totals were found by adding the estimates for each <br />county that lies entirely within the river basin to the estimates <br />for each county-river basin area that lies within the specific <br />river basin of interesto Table 4 shows groundwater recharge by <br />river basin and aquifero <br /> <br />20 <br />