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10/12/88 Special
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10/12/88 Special
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Last modified
5/21/2025 11:10:45 AM
Creation date
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Meetings
Meeting Document Type
Agenda
Document Title
Planning & Zoning Commission - Special
Document Date
10/12/1988
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42. <br /> <br />43. <br /> <br />44. <br /> <br />45. <br /> <br />46. <br /> <br />Sampling data collected during the Remedial Investigation (RI) and <br />Interim studies Report (ISR) demonstrated that the landfill <br />facility has resulted in local contamination of groundwater by <br />volatile organic compounds (VOC's). Nineteen specific VOC's were <br />observed consistently in the unconsolidated sand aquifers located <br />downgradient of the landfill site. VOC contamination is reaching <br />groundwater within the Upper Sand and tunnel valley aquifers. <br />These aquifers are bounded by the Grantsburg till and St. Lawrence <br />Formation bedrock aquitards (p. 35, EIS). <br /> <br />The pathway of release has been the percolation of leachate <br />through the unlined bottom of the landfill and then through the <br />unsaturated sands. The source of leachate generation is believed <br />to be water infiltration through mixed municipal solid waste <br />(garbage) deposited in the landfill since its inception. The <br />bedrock aquifers appear not to be affected. Near surface soils <br />beyond the WMMI landfill property line, local air quality and <br />nearby surface water bodies have not been affected by the <br />contamination (p.35, EIS). <br /> <br />The contaminant plume originating at the landfill follows the <br />direction of regional groundwater flow towards the south- <br />southeast, until it encounters a tunnel valley and the local <br />bedrock high located on the west edge of the Hunters Hill's <br />subdivision. At this point the plume has deflected with a <br />southern lobe flowing to the south and slightly west, following <br />the higher pe---meabi!ity sediments of the tunnel valley. North of <br />the bedrock high the plume margin has reached only as far as <br />monitoring well number 35BB, which is located 200 feet east of <br />Sunfish Lake Blvd. at the southern end of Sunfish Lake (p.36, <br />E~S) . <br /> <br />The contaminant plume extends approximately 2,500 feet southeast <br />of the limits of fill placement, and is roughly 2,500 feet in <br />width at its broadest point. The area of the plume with ~he <br />highest concentrations (above !,000 ug/!) of the contamination is <br />located ir~.ediate!y southeast of the landfill and extends to 1,600 <br />feet from ~he landfill. Maxin"-.n total VOC concentrations are <br />cbse_-ved to be approximately 3,000 ug/! in an area of the tunnel <br />valley a~aifer ir-n-e~iate!y east cf the fill area. Ethyl ether and <br />tetrahydrofuran (THF) appear to be ~he predominant compounds in <br />the groundwater east cf the landfill while halogenated VOC's <br />appear to be predominant in the groundwater souuh of the fill area <br />(p.36, EiS). <br /> <br />'That the response action which has been approved by the MPCA <br />(resulting from ~ne 1985 consent order) to address ground water <br /> ~-=~ ~ has five basic components: <br />c ........... a._on <br /> <br />- A final cover system with surface ~anoff controls and a double <br /> barrier to limit infiltrauicn cf water. <br />- A groundwater f!o~ barrier well system to restrict migration of <br /> contaminants from the site. <br />- A ground water recovery we!! system to capture and treat <br /> contamination that has already migrated from the site. <br /> <br />6 <br /> <br /> <br />
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