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<br />.44. <br /> <br />The land and Water Fund of the Rockies <br /> <br /> <br />o <br /> <br />Meeting Water Demand Without Gunnison Water <br /> <br />The estimated total pumping of groundwater from the Denver Basin Aquifers <br />in 1996 was 56,000 AF, virtually all in the South metropolitan areas of Douglas and <br />Arapahoe Counties. Just over half of this use (24,500 AF) was for municipal purpos- <br />es.'" Pumping 56,000 AF is less than 2% of the annual allowable pumping quantity <br />assuming a 100-year aquifer life.'"' Though there has been some localized well <br />pumping drawdowns and loss of hydrostatic pressure, the overall lifetime of the <br />Denver Basin aquifer at this level of production (56,000 AF/yr) may exceed 1000 <br />years. Simplified projections of well development and population growth to the year <br />2100 result in groundwater production estimates of about 300,000 AF per year, <br />approximately 10% of the annual allowable pumping from the Denver Basin <br />aquifers. '" <br /> <br />Despite the potentially long life of Denver Basin groundwater supplies, there <br />are several factors that caution against the use of groundwater as a sole source of <br />municipal supply. First, pumping costs tend to increase over time. As basins are <br />depleted, underground water levels and hydrostatic pressure drop, leading to <br />increased electricity consumption for the same water harvest. Second, the chance of <br />surface subsidence grows as groundwater tables are lowered. Third, pumping water <br />from aquifers drains a non-renewable water supply.'" <br /> <br />To help deal with the south metro area's long-term water needs, Douglas <br />County, the Denver Water Board, and the Colorado River Water Conservation District <br />have been exploring the South Metro Conjunctive Use and Interruptible Supply <br />Project. The project potentially would link groundwater systems serving parts of <br />Douglas and Arapahoe Counties with Blue River and South Platte River water sup- <br />plies conveyed by the Denver Water Department, with a resulting net reduction in the <br />total volume removed from the Denver Basin aquifers.'" If carried out, excess surface <br />water available through storage and delivery infrastructure managed by Denver Water <br />would, in average and wet years, supply water to the Douglas County Water Resource <br />Authority (DCWRA) and, in some cases, recharge Denver Basin aquifers. In dry years, <br />groundwater sources would be available to satisfy DCWRA demands in peak summer <br />months and used to payback "borrowed" water to Denver Water in the fall. <br />Conjunctive use essentially allows storage underground, minimizing evaporative loss <br />and obviating the need for new surface supply structures. <br /> <br />Preliminary studies showed that conjunctive use could yield up to 60,000 AF <br />of supply. More recent studies, based on new modeling of the speed of groundwater <br />recharge, estimate a yield of 27,000 AF. Whatever the ultimate yield produced, a stip- <br />ulation requiring multiple re-use of any new surface supplies delivered to DCWRA <br />members could leverage the yield by a factor of 1.7 or 2.'"' For our MWSI plus sce- <br />nario, this reort uses a factor of 1.5. <br /> <br />Conjunctive use may depend partly on increased imports for the mainstem <br />Colorado River. As such, there may be legitimate opposition to some portion of the <br />conjunctive use potentials we estimate. <br />