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<br />II-16 <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 />I <br /> <br />measUl"ements taken on the Colorado River near Cisco, Utah, the Colorado River <br />near De Eeque, and th<;l Cqlorl1do River at Glenwood Springs. The results ob- <br />tained from the suspended sediment measUl"ements were then checked against the <br />yield calculated on the basis of the State of Colorado Sediment Yield <br />(2)( 17) <br />Map prepared by the Colorado Land Use Canmission in 1974. <br /> <br />Da11y suspended sediment measUl"ements have been taken by the USGS <br />on the Colorado River near Cisco, Utah, since water year 1942. These meaSUl"e- <br />ments were correlated by ,linear regression with daily measUl"ements taken on <br />the Colorado HiveI' near De Beque in water years 1975 and 1976. The corre- <br />lation equation was also qhecj<:ed against miscellaneous measUl"ements taken near <br />De Beque and at Glenwood Springs. The correlation is excellent. The average <br />annual sedimenl~ load (tons per year) measUl"ed near Cisco, Utah and the esti- <br />mated load near De Beque, which is equivalent to the sediment inflow to Una <br />Reservoir, are shown in Table II-6. The average annual suspended load near <br />Cisco is 11,7'55,000 tons/year and the estimated load near De Beque is <br />1,615,000 tons/year. By increasing the suspended load value by 10% to reflect <br />the unmeasUl"ed bedload, the sediment inflow to Una Reservoir is estimated to <br />average 1,776,000 tons per year. This estimate is considered reliable since <br />it is based on 39 years of daily measUl"ements and results of similar magnitude <br />were obtained from the State Sediment Yield Map. <br /> <br />The average density of the sediments that would flow into the <br />reservoir was E!stimated based on various suspended sediment size distribution <br />measUl"ements tsLken by the USBR at Rulison Bridge on the Colorado River about <br />18 miles upstream of Parachute. Based on these measurements the average sedi- <br />ment load conststs of 46.6% bedload and sands, 30.3% silts, and 23.1% clays. <br />The average dEmsity of deposited sediments within the reservoir would be <br />approximately 80 1 b/ft. 3 (pef) after 50 years of consolidation based upon <br />this distribution of sediment sizes. <br /> <br />2. Reservoir Trap Efficiency and Sediment Deposition <br /> <br />The reservoir trap efficiency was estimated by means of Churchill's <br />(1) <br />method and would average 90% over the first 100 years of reservoir life. <br />The sediment volume that would be trapped in the reservoir over the first 100 <br />