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� Sailors World, Inc. <br /> Summit Project No. 922030 <br />� October 5, 1995 <br /> Page 3 <br />� 2.3 Site Location and Description <br />� The subject site is located on County Road 15, approximately S miles west of Wayzata, <br /> Minnesota. The site is located in the SEl/a of the SWt/a of the NWl/a of the SEl/a of Section 10, <br /> Township 117 North, Range 23 West, in Hennepin Counry (Figure 1). Site structures and <br />� features include a club house building, several temporary garage units, and an asphalt pazking lot <br /> used for boat storage and vehicle pazking. It is Summit's understanding that a geotextile-type <br /> liner underlies the parking lot to control watei. . <br />� The area surroundin the site consists of Lake <br /> g Minnetonka to the northeast and southeast, a <br /> former commercial business to the southwest, and a residential area to the northwest (Figures 1 <br />� and 2). According to Mr. De Santis, the former business located to the southwest was at one <br /> time a gasoline station, and was more recently converted to a transmission repair service station. <br /> The building appeared to be abandoned and inactive during recent site visits performed by <br />� Summit. <br /> � A water supply well is located approximately 20 feet southwest of the club house (Figure 3). A <br /> � well log for this well was not available. According to Mr. De Santis, the water well on his <br /> property was constructed approximately 25 years ago and is estimated to be 240 feet deep. <br />� 2.4 Regional Geology and Hydrogeology <br />� Su�cial deposits underlying the site consist predominately of lacustrine sand and loamy sand. <br /> Peat underlies organic-rich loam and manmade beaches in some areas. Underlying this material <br /> is a thick sequence of glacial till that is characteristic of the Lake Minnetonka region. This <br />� sequence of clay appears to be a confining layer and separates surficial deposits from deeper <br /> glacial deposits and the underlying bedrock. The St. Peter Sandstone Formation is present <br /> beneath the unconsolidated material and is estimated to be 200 to 400 feet below the ground <br />� ' surface (Balaban, N.H., 1989). <br />}� 3.0 PROJECT RESULTS <br />� 3.1 Excavation <br /> On August 13, 1992, Summit personnel observed the removal of a 4,000-gallon capaciry UST <br />� and approximately 70 cubic yazds of petroleum impacted soil. The location of the excavation is <br /> illustrated on Figure 2. During the excavation, soil samples were screened for indications of <br /> organic vapors using a photoionization detector (PID) equipped with a 10.6 electron volt lamp � <br />� and calibrated for direct reading in parts per million (ppm) of benzene on a volume basis. The <br /> instrument was calibrated at the beginning of the day using ambient air as zero gas and 100 ppm <br /> isobutylene in air as the calibration gas. Soil samples were screened using a jar headspace <br />� <br />� . <br />