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<br />Chapter 1: South Platte Basin Inventory <br /> <br />March 21.1998 <br />Page 1-10 <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 />upstream municipal water rights, an analysis of this effect was beyond the scope of this <br />study. For the purposes of this study it was assumed that estimated future flow <br />increases due to metro area RIS and L1RF would be fully included in the Denver and <br />Henderson gage flows, <br /> <br />Increased Future Wastewater Flows From Tributaries. <br /> <br />Denver's PACSM model uses historical gage data to simulate inflows from Plum <br />Creek, Cherry Creek, Bear Creek and Clear Creek to the South Platte. However, it <br />likely that future flows from Cherry Creek, Plum Creek and Clear Creek will increase <br />due to increases in wastewater discharges. <br /> <br />At Near Term demand levels, Douglas County water demands will probably <br />exceed 100,000 acre-feet per year, with most of this supply coming from nontributary <br />groundwater. As a result wastewater flows in the Cherry Creek and Plum Creek basins <br />will increase significantly. While some of this wastewater is likely to be reused through <br />augmentation plans and direct reuse, a net increase in wastewater flows is projected, in <br />both the Cherry Creek and Plum Creek basins. To estimate this net increase in <br />wastewater flow, future Douglas County water demands met by nontributary <br />groundwater, resulting wastewater flows and associated augmentation/reuse plans <br />were estimated based on current County projections (Mulhern, 1995), The net increase <br />in wastewater flows derived from nontributary groundwater sources was calculated <br />taking into account average monthly municipal delivery and wastewater production <br />patterns, augmentation plans and direct reuse plans. The resulting net increase in <br />wastewater ranged from 1 cfs to 20 cfs and averaged 5,700 acre-feet per year. These <br />flows were added to Denver's modeled flows at the Chatfield, Denver and Henderson <br />gages. <br /> <br />Flows from Clear Creek into the South Platte have increased since 1990 by <br />approximately 15 cfs due to wastewater discharges from the Coors/Golden plant no <br />longer being diverted by the Croke Canal. These flow increases are not reflected in <br />Denver's modeled Henderson gage flows. This increased Clear Creek inflow generally <br />affects flows at the Henderson gage during all months except August through October, <br />when intervening irrigation rights on lower Clear Creek divert most of this water. It was <br />assumed for the purposes of this study that these wastewater flows would increase <br />average flows at the Henderson gage by 15 cfs during November though July, <br />Denver's modeled flows at Henderson were adjusted accordingly, <br /> <br />Increased flows from Bear Creek compared to historical gage records were <br />assumed to be negligible, <br /> <br />Junior South Platte Water Riahts, <br /> <br />Hydrosphere Resource Consu~ants. 1002 Walnut Su~e 200. Boulder. CO 80302 <br />