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Timnath-Connell Substitute Water Supply Plan Page 3 of 7 <br />March 31, 2017 <br /> <br />The remaining 1.5 BEDC shares not used for recharge will continue to be used to irrigate the portion <br />of the John Weitzel Farm still in agricultural production. <br />The diversions available at the farm headgate for the 4.0 shares used on the John Weitzel <br />property were estimated to total 365.20 acre-feet per year, and the historical consumptive use of <br />the 4.0 BEDC shares was estimated to be 168.99 acre-feet. This quantification is based on the <br />average headgate diversions for the Box Elder Ditch for the years 1950 to 2014, assuming 10% ditch <br />loss and 55% field efficiency for flood irrigation. Historic consumptive use was determined as the <br />lesser of the water available for crop consumption or potential crop consumptive use if a full water <br />supply was available. One-third (65.40 acre-feet) of the return flows from the use of the 4.0 shares <br />were assumed to occur as surface return flows and the remaining two-thirds (130.80 acre-feet) <br />were assumed to occur as subsurface return flows. Subsurface return flows were lagged to the <br />river using the AWAS stream depletion model with the following parameters: <br />• Distance from the irrigated property centroid to the river (X) = 3,300 ft <br />• Alluvial aquifer width (W) = 5,000 ft <br />• Specific yield (S) = 0.2 <br />• Transmissivity (T) = 50,000 (gpd/ft) <br />The monthly net accretion/depletion for the 4.0 BEDC shares were calculated as the monthly <br />diversions available at the farm headgate, minus the surface return flow obligation and lagged <br />subsurface return flow obligation for that month. The monthly net accretion/depletion for the 2.5 <br />BEDC shares to be delivered to recharge were calculated by pro-rating the monthly net <br />accretion/depletion for the 4.0 BEDC shares. <br />The expected volume of water available for diversion into the recharge pond for the subject <br />2.5 shares is 228.25 acre-feet per year. This figure represents the pro-rata average headgate <br />diversion less a 10% ditch loss. The pro-rata historical consumptive use credit for the 2.5 shares is <br />estimated to total 105.62 acre-feet for this plan period and the pro-rata return flow obligation for <br />the 2.5 shares is estimated to be 122.63 acre-feet. The evaporation losses from the recharge pond <br />(shown in Water Balance table) are estimated to total 20.82 acre-feet per year, resulting in a net <br />amount of 207.43 acre-feet of water delivered to recharge. <br />The lagged accretions from the Timnath-Connell recharge pond were estimated by the <br />Applicant’s consultant using the AWAS stream depletion model with the following parameters: <br />• Distance from the recharge pond centroid to the river (X) = 3,500 ft <br />• Alluvial aquifer width (W) = 5,300 ft <br />• Specific yield (S) = 0.2 <br />• Transmissivity (T) = 50,000 (gpd/ft) <br />The lagged accretions to the Cache la Poudre River are estimated to total 248.91 acre-feet <br />during this plan period. This amount includes deliveries to recharge from previous years. Pursuant <br />to previously submitted accounting, 286.54 acre-feet were diverted into the recharge site during <br />the 2012 irrigation season, 257.27 acre-feet were diverted into the recharge site during the 2013 <br />irrigation season, 502.69 acre-feet were diverted into the recharge site during the 2014 irrigation <br />season, 407.81 were diverted into the recharge site during the 2015 irrigation season, and 240.11 <br />were diverted into the recharge site during the 2016 irrigation season. In addition in 2014, and <br />2015 long periods of no call on the Cache La Poudre River allowed for considerable amount of free <br />river water to be delivered into the recharge pond beyond the historic yields of the 2.5 Box Elder <br />shares. The summer and winter return flow obligations from the use of the 2.5 Box Elder Ditch <br />shares will be maintained under this substitute water supply plan. A monthly breakdown of the