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R2000-258 AUTHORIZING AGREEMENT
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R2000-258 AUTHORIZING AGREEMENT
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Last modified
3/24/2016 2:19:02 PM
Creation date
3/24/2016 2:19:00 PM
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Resolution/Ordinance
Res Ord Num
R2000-258
Res Ord Title
AUTHORIZING AGREEMENT WITH ILLINOIS STATE WATER SURVEY FOR DEWITT WELL FIELD FOLLOW-UP STUDY
Approved Date
12/18/2000
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� � [GI <br /> EXECUTIVE SUMMARY <br /> Layne GeoSciences, Inc. was retained by the City of Decatur (City), Illinois, to � <br /> perform a groundwater modeling study of the underlying aquifers in east-central ' <br /> Illinois. The City owns two wellfields in the area: the DeWitt wellfield comprising II <br /> of eight wells, and the Cisco wellfield consisting of two wells. Both wellfields are '� <br /> intended to be operated only occasionally to supplement the City's surface water i <br />, source. The DeWitt wellfield has a design capacity of 24 MGD for 90 days of <br /> operation. However this capacity has never been verified. The specific goal of the <br /> study was thereFore to utilize the groundwater model to determine the safe <br /> operating capacities of the DeWitt and Cisco wellfields. <br /> The area is underlain by three unconsolidated formations, each representing a <br /> different hydrogeologic unit. From the top, these are the Wedron, Glasford, and <br /> the Banner Formation. Of the three, the Banner Formation is the most <br /> productive unit. Specifically, the thick sand and gravel deposits in the lower <br /> portions of the Banner Formation, referred to as the Mahomet aquifer, is most <br /> prolific aquifer in the area. Both the DeWitt and the Cisco wellfields obtain water <br /> from this unit. The emphasis of this study is therefore on the Mahomet aquifer. <br /> The groundwater model was first calibrated to current-day hydrologic conditions <br /> in the Mahomet aquifer. The calibrated model was then validated to the observed <br /> response (of the Mahomet aquifer) recorded during the 30-day pump test. An <br /> excellent match was obtained between the observed and model simulated aquifer <br /> drawdowns. Results of model calibration indicate that fairly confining conditions <br /> exist at the DeWitt wellfield thereby restricting recharge from infiltration. In the <br /> larger study area, extending from Paxton in the east to Lincoln in the west, <br /> approximately 35 MGD enters the Mahomet aquifer as recharge from the <br /> overlying Glasford aquifer. Approximately 27 MGD of this recharge is withdrawn <br /> for various municipal, industrial, agricultural, and domestic purposes. The <br /> remaining 8 MGD e:cits the study area along the western boundaries of the model. <br /> A series of management simulations were conducted with the calibrated model in <br /> order to estimate the safe operating capacities of the DeWitt and Cisco wellfields. <br /> Simulation results indicate that the wellfield capacity may be limited by excessive <br /> drawdowns in the area. It is recommended that pumpage be distributed between <br /> the DeWitt and Cisco wellfields in order to minimize drawdowns and ma:cimize <br /> wellfield yields. Consideration may be given to increasing wellfield capacity (up to <br /> 6 MGD) in the vicinity of the Cisco wellfield. The probable safe operating yield of <br /> the DeWitt and Cisco wellfields on an equivalent average daily basis is 7-8.5 MGD <br /> combined pumpage. The corresponding total annual withdrawal of 2.5� to 3.10 <br /> billion gallons is the recommended annual pumpage for planning and <br /> management purposes. The groundwater model can be utilized in various ways to <br /> manage groundwater resources in the area on an as-needed basis. For esample, <br /> the safe operating capacities for non-annual periods of operation can also be <br /> determined by the model. <br />
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