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<br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Artificial Recharge of Ground Waler in Colorado <br />A Slalr:wide ASlieMlment <br /> <br />I <br /> <br />- <br /> <br />1 Figurel-lb Denver Basin aquifer <br />recharge project ASR well A-ro. <br /> <br />o <br />. <br />, <br />- <br />. <br />~ <br />. <br />. <br />:1,1 <br />c <br />~ <br />'" <br /> <br /> <br />I <br />I <br /> <br />'-'.'~' ~1 <br />- - <br /> <br />r -:-- == ~ - ~~. ~!":~:.~."I <br />~:~'--"~~"~~i <br /> <br />Figure I-l<l nillon Reservoir (torn Frisc:-o M;uina durinu the Slnnmer <br />2002 drought <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Artificial recharge in some fashion has been used for centuries. During the last several hundred <br />years. nomads in Turkmenistan have been collecting infrequent surface runoff into an infiltration <br />pit located in sand dunes where the surface \\/atcr recharges ncar-surface ground water. Ground <br />\vater is then available for extraction from a series ofhand4dug wells surrounding the pit cven <br />during dry periods (Pync, 1995). A tribal community in western India has also been applying <br />artificial recharge to enhance ,vater supply and improve water quality obtained from a tank <br />excavated in fine sand and clay (Pyne. 1995). Closer to home. California began practicing <br />artificial recharge by routing stornl runofTinto infiltration (spreading) basins around the turn of <br />the century. Interest in artificial recharge grew in California and New York during the 1930s as <br />a way to conserve or enhance ground.water resources (Weeks. 2002). <br /> <br />In Colorado. the earliest documented application ofartilicial recharge began at Olds Reservoir in <br />Wcld County when local farmers took advantage ofa leaky reservoir built several decades <br />earlier. Surface water was diverted into the little used structure in order to maintain water levels <br />in the underlying alluvial aquifer (Skinner. 1963). In 1959, the Colorado Agricultural <br />Experiment Station (CAES) initialed a study of artificial and natural recharge in Colorado that <br />was funded by the Forty-second Colorado General Assembly under Senate Bill No. 336. There <br />is very little documentation of the results of this study. however. it was initiated to consider <br />artificial recharge in the following basins (CSU. 1960): <br /> <br />. South Platte River Basin <br />. Arkansas River Basin <br />. Colorado High Plains Ogallala formation <br />. San Luis Valley <br />. Denver Basin bedrock aquifers <br /> <br />4 <br />