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<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 /> <br />The most critical water use month, with the lowest end-of-month reservoir storage, would have <br />occurred in July of 1955 under the assumptions made. Starting with only the Morrison Operating <br />Reservoir full in January 1950 as a start date for modelling parameters, and with water demands <br />of 1,290 EQR, Cooley Reservoir would not be able to fill completely until July of 1952, two and <br />a half years after initial filling begun. This assumes no "free water available" and that water <br />could only be diverted under priority. Once the Cooley Reservoir is full in 1952, the following <br />series of three drought years, beginning in 1954, uses almost all water storage by July 1955. <br />Thereafter, the reservoir begins filling again and almost regains full capacity in August of 1957. <br /> <br />The amount of water that could be pumped into the Cooley Reservoir every month is based upon <br />the total water available for storage with the existing water rights and the storage in the reservoir <br />at that month. If the reservoir is full, only make-up water for evaporation and seepage is pumped <br />into the reservoir. If the reservoir is not full, all water available for storage will be pumped into <br />the reservoir until it is full. The computer model for this operation study shows that in the wet <br />years of 1952 and 1953, when the reservoirs were full, approximately 206 acre-feet of additional <br />water could have been stored, but was not diverted. <br /> <br />If Cooley Reservoir is enlarged to 600 acre-feet, Morrison would be able to store all water <br />available under their present water rights during the model period of 1950 to 1957. With this <br />additional storage, Morrison could serve up to 1,475 EQR. A copy of this model run is shown <br />in the Appendix, Tables 2A to 2H. Figure II-C shows the storage volume throughout the 8-year <br />study periOd for a scenario with 1,475 EQR. <br /> <br />The maximum average monthly flow rate available for delivery to storage is determined by the <br />model to be 1.6 cfs. Instantaneous diversions may be higher, therefore, a pumping rate of 2.5 <br />cfs is recommended for filling Cooley Reservoir. In summary, Morrison's present water rights <br />portfolio will allow for 4.45 cfs diversion from Bear Creek into the treatment plant, but the filling <br />rate into the Cooley Reservoir need not be more than 2.5 cfs. <br /> <br />B. EXISTING RAW WATER DELIVERY SYSTEM <br /> <br />The existing raw water intake system consists of a diversion dam and intake screen on Bear <br />Creek, at approximate elevation 5990 feet. A concrete weir check dam structure in the creek <br />maintains a water level to the intake screen. In 1983, flooding on Bear Creek washed out the <br />check dam and a new concrete weir was constructed as an emergency replacement. The <br />system is presently constructed to route floods over the weir, and around the intake area to the <br /> <br />70-0SO.03S:MSTR.PLN <br /> <br />II-7 <br />