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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 />I <br /> <br />Total diverted volume in Table IV-2 accounts for all water diverted from the Poudre River <br />into the canal. Records are kept on a continuous basis at the canal measuring flume located <br />downstream of the main headgate. Water passing through the flume includes: direct <br />diversion rights, reservoir calls from Fossil Creek Reservoir, exchanges with other irrigation <br />companies, return flows, and excess storm flow. A breakdown of the individual components <br />that account for the total diverted flow is not available. <br /> <br />B. Firm Yield. The firm, or safe yield, of a canal is generally defined as "the maximum <br />quantity of water which can be guaranteed during a critical dry period". The safe yield of <br />diversion was not evaluated by analysis of the available flow of water in the Cache La Poudre <br />River. It was evaluated only by review of the past history or record of flow into the main <br />canal. <br /> <br />From a review of Figures IV-2 through IV-7, it can be seen that the canal normally begins <br />diverting water in May and reaches a peak in mid June, which corresponds to the peak runoff <br />in the river. At the end of June, there is a substantial decline in the diverted flows. This <br />typically starts the reservoir season of canal operation. Diverted flows during late July, <br />August, and September are typically from release out of Fossil Creek Reservoir and from <br />return flows and stormwater in the Poudre River. The amount of water that can be diverted is <br />dependant on available flow in the Poudre. If direct runoff is available, water can be diverted <br />by the Company on a reliable basis. However, during a drought period, the Company comes <br />out of priority and cannot divert the desired flow rates. Over a 7-year period, the Poudre <br />River has fluctuated in peak virgin river flows from a low of 1308 cfs in 1987 to a high of <br />3785 cfs in 1991. However, the peak diversion rate and the total amount of water diverted <br />has increased between 1987 and 1992. This increase in total volume could be attributed to <br />increased return flows entering the Poudre above the diversion structure. The Poudre River is <br />very complicated in operation from the first diversion in the canyon to the NCLPIC diversion <br />structure. Numerous irrigation diversions deliver water to the various irrigation companies. <br />Many companies have agreements for exchanges whereby they divert at an upstream location <br />and release it downstream. Also, return flows come from agricultural runoff as well as urban <br />runoff from the developed areas in the City of Fort Collins. <br /> <br />The safe yield of the canal could be considered to be the minimum diverted flow experienced <br />by the canal for the year 1987, which is approximately 21,000 acre-feet. <br /> <br />It is not certain what the safe yield would be with the present makeup of the system and could <br />not be determined without analyzing the whole Cache La Poudre system. If the water storage <br />record is studied for the years from 1987 to 1992, the results would indicate that a minimum <br />diverted volume would yield approximately 21,000 acre-feet. <br /> <br />PAGE - 5 - Chapter IV <br />