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Last modified
7/29/2009 9:42:37 PM
Creation date
10/12/2006 4:04:26 AM
Metadata
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Template:
Water Supply Protection
File Number
8040.500
Description
Section D General Studies - Ground Water
Date
7/1/1999
Author
SDU, BOR, USEPA,USGA
Title
High Plains States Ground Water Publications - Huron Recharge Demonstration Project Summary
Water Supply Pro - Doc Type
Report/Study
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<br />4.5 <br /> <br />4 <br /> <br /> \ <br /> t ...., 1995 Rech rge <br /> fi ~ "'" <br /> :::;r- 1994 Rec arge -- <br />... <br />.... <br />,-,- , <br /> <br />. <br /> <br />(/) 3.5 <br />~ <br />CD <br />- <br />~ 3 <br />-0 <br />III <br />CD 2.5 <br />I <br />o <br />:s 2 <br />CD <br />E <br />o <br />'E 1.5 <br />CD <br />- <br />~ 1 <br /> <br />"" <br />V.oJ <br /> <br />o <br />-1500 <br /> <br />-1000 -500 0 500 1000 <br />Distance From Recharge Well, meters <br /> <br />1500 <br /> <br />Figure 6. Graph showing the effects of artificial recharge. <br /> <br />. <br /> <br />magnesium even though they were predicted to precipitate. Upon pumping of the injection <br />well shortly after recharge, most of the water quality parameters exhibited a decrease in <br />concentration for the first 24 hours, after which the water quality stabilized at concentra- <br />tions intermediate between the injected and the native groundwater. <br /> <br />Aquifer tests in 1994 before and after the recharge event indicated a decrease in trans- <br />missivity of about 20 percent. This decrease was attributed to air entrainment in the aquifer <br />during injection and to some initial physical clogging within the filter pack around the well <br />due to settling and shifting. This hypothesis was supported by the fact that the results of an <br />aquifer test prior to the 1995 recharge event were similar to the pre-injection test conducted <br />in 1994. <br /> <br />The Huron Recharge Project has demonstrated that: <br /> <br />. Recharge is hydraulically feasible in buried glacial aquifers. However, high natural <br />water levels in the aquifer due to abnormally high precipitation and subsequent <br />natural recharge decreased the scope of the desired artificial recharge. <br /> <br />. Aquifer tests conducted before the 1994 and 1995 artificial recharge events indicated <br />very little change in either the transmissivity or specific capacity of the aquifer. Air <br />entrainment within the aquifer during artificial recharge did reduce artificial . <br />recharge efficiency. <br /> <br />14 <br />
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