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<br />Chapter 1: South Platte Basin Inventory <br /> <br />March 21,1998 <br />Page 1-12 <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 />Chanoes in St. Vrain, Bio Thompson and Cache La Poudre Flows. <br /> <br />Growth in municipal and industrial water use in these South Platte <br />tributary basins has resulted in increased return flow volumes and a change in <br />return flow patterns due to the fact that municipal water use is generally less <br />consumptive than irrigation use and because there are proportionately more <br />winter season return flows due to wastewater discharges. <br /> <br />Future M&l water use in these basins will also utilize 48,000 acre-feet per <br />year of Windy Gap project water, which will add return flows to the South Platte <br />basin. While return flows from Windy Gap water are fully reusable, these return <br />flows were included in our estimate of future Kersey flows and accounted for <br />separately as part of the reusable portion of future flows. <br /> <br />Future urban growth in this region will also result in increases runoff from <br />impervious surfaces (RIS), <br /> <br />These changes in flows were estimated by quantifying the total change in <br />municipal water use within the St. Vrain, Big Thompson and Cache La Poudre <br />Basins between 1950 and 1980 and between 1980 and 2025 based on best <br />available information and projections, Municipal and domestic water use within <br />this northern region has increased from approximately 48,000 acre-feet per year <br />in 1950 to approximately 105,000 acre-feet per year in 1980, By the year 2020, <br />municipal use is project to reach approximately 260,000 acre-feet per year <br />(NCWCD, 1991), The net increase in return flows due to: 1) changes of irrigation <br />water rights and CBT units from irrigation uses to municipal uses, 2) use of <br />additional Windy Gap supplies, and 3) increased RIS is estimated to be <br />approximately 76,000 acre-feet per year between 1950 and 2025 and 60,000 <br />acre-feet per year between 1980 and 2025, These increases were added to the <br />Kersey gage flows incrementally between 1950 and 1980 using monthly <br />coefficients representative of RIS (discussed in Chapter 4) and of the difference <br />between typical municipal and irrigation return flow patterns, <br /> <br />Also, since 1953 the CBT project has delivered an annual average of <br />approximately 230,000 acre-feet of supplemental water supply to agricultural, <br />municipal and rural domestic water users within the Northern Colorado Water <br />Conservancy District Approximately one half of this supplemental supply has <br />returned to the South Platte above the Kersey gage. This can be seen in the <br />historical records for the stream gages at the mouths of the Cache La Poudre, <br />Big Thompson and St Vrain rivers. While the monthly pattern of CBT return <br />flows varies from year to year, stream flows out of these South Platte tributaries <br />have generally increased in all months of the year. A monthly CBT return flow <br />pattern was estimated by calculating the return flow resulting from 190,000 acre- <br />feet per year of CBT deliveries using a simplified irrigation depletion model and <br /> <br />Hydrosphere Resource Consuttan!s. 1002 Walnu! Sune 200, Boulder, CO 80302 <br />