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<br />IV-15 <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 />than directly to the Townireservoir is that in-pond <br />filtration reduces water turbidity. <br /> <br />caoacitv and Ooeration. Town personnel estimate <br />current capacity of the infiltration pipeline (when <br />supplied by ditch water) ~s 110,000 to 120,000 gpd. <br />Greater flows may be obta~ned, but at a reduction of <br />water quality. This woulq indicate that gravels <br />around the perforated pip~line are not clogged (or <br />else flow would be restricted), but that silting is <br />occurring which is "washed out" with high flow <br />rates. No records are available of capacity of the <br />infiltration line without diversion of ditch water <br />to the infiltration ponds; Obviously, the ditch <br />water represents a differ~nt water right. <br /> <br />The infiltration line a1sq responds fairly quickly <br />to irrigation of hay fielqs upstream from the <br />infiltration line. In times past, direct flow water <br />released from Gurley Reservoir (which the Town was <br />incapable of using or storing), has been used to <br />water the hay fields to recharge groundwater <br />conditions around the pipeline. In effect, direct <br />flow has been "stored" inithe ground and collected <br />as required by the Town. IUse of direct flow for <br />this application would not be normal, however, <br />because during direct flow periods farmers also have <br />their own water to use, a~d fields are likely being <br />watered already. <br /> <br />Maintenance. Roots were cleaned out of infiltration <br />lines in 1989, and silt was cleaned out of some of <br />the ponds 3 years ago. O~her ponds were cleaned 6 <br />years ago. <br /> <br />4. Water Available from SubsUrface Riahts. <br /> <br />A summary of water flows which have been variously <br />estimated by observers are as follows: <br /> <br />Gardner Sorina <br />Summer - 45,000-55,QOO gpd (.075 to .078 cfs) <br />winter - 20,000-25,000 gpd (.031 to .039 cfs) <br /> <br />i <br />Infiltration Pond System <br />Summer - 110,000 gpd maximum (.170 cfs) (with <br />ditch diversions <br />winter - No information <br /> <br />It is probable that a substantial portion of the <br />water from the subsurface:flows is recharged by flow <br />in Gurley Ditch. However; the winter flows should <br />not be affected by irriga~ion after January 1. <br />