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<br />3-2 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />in the canal vary from 15 to 36 percent and are estimated to average 30 <br />percent with the existing system and 25 percent with the project, <br /> <br />Losses are fairly constant throughout the length of the canal as indi- <br />cated on Table 8, Combined seepage and gate losses presently average <br />about 0.89 cfs/mi, <br /> <br />Due to the operation requirements during anyone irrigation season. the <br />water losses vary, During low water years, such as 1976. canal flow is <br />intermittent and the canal never "seasons" with attendant hi gh seepage <br />losses resulting, During normal water years. the flow is continuous <br />allowing the canal to be "seasoned" which substantially reduces the <br />seepage losses. <br /> <br />A summary of the canal losses, intercepted flow, bypassed flows and <br />canal diversions are shown on Table 10 with the existing system for the <br />years 1967 (above normal water supply). 1976 (below normal water supply) <br />and for the average water supply with the project, <br /> <br />Project canal losses were determined uSing the average year water supply <br />with the project from Table 10 and subtracting the proposed improvement <br />water savings from the existing losses, A summary of the average year <br />existing and project losses is shown on Table 9. <br /> <br />WATER SUPPLY <br /> <br />The Amity system receives water from Arkansas River Diversions and in- <br />tercepted flows at various points along the system, River diversions <br />are measured using a 20-foot Parshall Flume; tributary inflows are <br />calculated by multiplying estimated net inflow rates times duration for <br />each tributary. Historical diversions from the Arkansas River and re- <br />leases from the Great Plains Reservoirs are shown in Table 11, As shown <br />by the table. the volumes of water diverted into the system from all <br />sources have varied during the past twenty-three years by a factor of <br />nearly ten, The minimum water diverted occurred in 1964 and totalled <br />16,200 acre-feet. The maximum water diverted occurred in 1966 and to- <br />talled 140.700 acre-feet, The average flow diverted equals 73.900 <br />acre~feet. Table 2 in the Summary shows the existing and project <br />added water supply for the average year. The existing supply is 54,950 <br />acre-feet. <br /> <br />The project will add 6,740 acre-feet to the annual average supply based <br />on diversions since 1960. The increase will be realized by restoring <br />historical diversion capacity at Big Sandy Creek and by reducing canal <br />losses by rehabilitation of old and leaking structures. No new water <br />rights are involved, Total supply will be 61.700 acre-feet. <br /> <br />WATER RIGHTS <br /> <br />Decreed flow and storage rights are listed in Appendix C, The flow <br />rights total 3193,5 cfs and decreed storage is 280,752 acre-feet, <br />