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<br />; <br />/ <br /> <br />, 0052 <br /> <br />Modification of John Martin outlet works <br /> <br />In order to provide for a simple and acceptable means of discharging <br />river inflows from the permanent fish pool at John Martin Reservoir, at <br />such times as the reservoir would be at this minimum elevation, some mod- <br />ification of the existing outlet structure woUld be necessary to provide <br />for automatic operation. An allowance of ~)20,000 is made in the total <br />cost estimate to provide for this modification and has been included in <br />the cost of the Granada Reservoir. <br /> <br />Total project cost <br /> <br />The following tabulation summarizes the project cost based oh July <br />1953 prices and as corrected to conform to the projected price index of <br />l80 (l939 . 100)~ <br /> <br />Feature <br /> <br />Construction Costs <br />Projected <br />price <br />. ind8x <br /> <br />April <br />1953 <br /> <br />Arkansas Diversion Dam . , . $ 406;000 <br />Diversion Canal. . , . . .. .l22jOOO <br />Granada Reservoir. . . . . . ii>, 168. 000 <br />-'~ <br />Total. . . . . . . . . "$7,296,000 $5,326,000 <br />*Cost includes ~20,000 for modification of John <br />Martin Outlet. (i-ell, 11 '% ?<.A., t q If" 'I> <br /> <br />The annual operation, maintenance and replacement costs of the <br />Granada Project have been estimated to be ~)5,400. This cost is distri- <br />buted as follows: <br /> <br />$ 296,000 <br />89,000 <br />4, 94l,000 <br /> <br />Feature <br /> <br />Annual. <br />O.lIi.&R. <br /> <br />Arkansas Diversion Dam. . . . . . .~p2, 960 <br />Diversion canal. . . . , . . , ., 890 <br />Granada Reservoir · · . . · · . ..". g,t5g <br />Total. . . . . . . . . . . .' .~~ , 0 <br /> <br />WATER SUPPLY <br /> <br />Source of water <br /> <br />Water 1'01' the potential Granada Reservoir Project would be obtained <br />from the outflow of the Arkansas River at the 6010rado-Kansas State line <br />surplus to the requirements of the water usors in Kansas above Garden <br />City. These surplus flows would consist principally of winter roturn <br />flows and flood flows originating between John Martin Reservoir and the <br /> <br />-3- <br /> <br />