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<br />- 2- <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />j <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br /> <br />The overall view of the Denver Basin Aquifers also reveals a complex combination of <br />water use and resource protection. The Denver iBasin Aquifer system consists of the <br />Dawson (upper and lower), Denver, Arapahoe (~pper and lower), and Laramie-Fox <br />Hills aquifers. The aquifers cover an area of ab~ut 6,700 square miles extending from <br />Colorado Springs on the south to Greeley on the north, and from the foothills on the <br />west to Limon on the east (Figure 1 and 2). ' <br /> <br />The Aquifer system contains approximately 300 million ac-tt of drainable storage. To <br />put this quantity of water in perspective, this amounts to a reservoir 15 times greater <br />than the active storage of Lake Powell (20 million ac-ft) , and 400 times greater than the <br />active storage of Blue Mesa Reservoir (750,000 sc.tt). The estimated total pumping of <br />groundwater from the Denver Basin Aquifers in 11996 was 56,000 ac-ft. This is less <br />than 2% (60,000 ac-ft) of the 1 % (3,000,000 ac-ft) annual allowable pumping quantity <br />under the 100 year aquifer life administration criteria provisions of Senate Bill 85-5. <br /> <br />Eventhough some localized well pumping drawdowns and loss of hydrostatic pressure <br />are occurring, the overall Denver Basin aquifer life at this level of production (56,000 <br />af/yr) may exceed 1000 years. Simplified projections of well development and <br />population growth to the year 2100 result in groundwater production estimates of about <br />300,000 ac-tt per year which is about 10% of theiannual allowable pumping from the <br />Denver Basin aquifers under the 100 year aquifer life assumption. Depending on <br />unknown future conditions, this amount could be !significantly different. <br /> <br />The impacts to South Platte River flows and the potential injury to senior water rights <br />due to depletions from ground water pumping arEj not currently evident due to the net <br />increased flow in the South Platte from Denver B~sin aquifer return flows and due to <br />the delayed impacts of pumping. Therefore, wat~r policy decisions related to the long- <br />term use of this nonrenewable resource and the Ijl'lanagement of the South Platte River <br />are not immediately critical. However, these water policy issues must be addressed <br />over the next few years through the development, and use of advanced computer <br />modeling, improved data bases and a more thorough understanding of all the potential <br />causes of injury to senior water rights on the South Platte prior to changing existing <br />statutes. <br /> <br />II. Public Water Policy Issues <br /> <br />This study has raised a number of water policy issues that must be addressed <br />through additional study and public meetings, and by the legislature acting in its <br />role as "decision maker" in public water policy. <br /> <br />The water needs of the Denver metropolilim area and South Platte River basin <br />are increasing as ,a result of population! growth. Water for this increasing <br />population will come from a combination of!six sources: 1) Water conservation 2) <br />Water reuse 3) Trans-basin imports 4) Conversion of in-basin agricultural water <br />