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� Sailors World, Inc. <br /> Summit Project No..922030 <br />� October 5, 1995 <br /> Page 7 <br />� recorded onto a water level form. The completed forms included the following information: the <br /> probe number; the time of the measurement; the date of the measurement; the depth to the <br />� groundwater surface; the type of ineasuring device used; the initials of the individual collecting <br /> the data; the Summit project number; and the location of the site. The groundwater levels were <br /> measured from a surveyed point at each location: These surveyed points depicted relative <br />� elevations and were referenced to an on-site concrete slab with an assumed elevation of 100.00 <br /> feet. <br /> t� Groundwater elevation data is included in Table 4. These data suggest movement of <br />` groundwater toward the southeast as exhibited on the groundwater contour map (Figure 3). <br /> Based on the inferred groundwater contours generated, the average horizontal gradient was <br />� estimated to be approximately 0.01. Hydraulic conductivity of the soil (probable fill) is expected <br /> h to vary widely with respect to transport of groundwater and dissolved petroleum constituents. <br />� According to Mr. De Santis, the level of Lake Minnetonka was very high in June 1995, <br /> " approximately 6 inches below flood stage. Because the lake level was relatively high and <br /> groundwater elevation data indicated movement toward the lake, groundwater movement away <br />,� from the Lake does not appear likely. A hydrogeologic setting and groundwater contamination <br /> worksheet are included in Appendix V. . <br />� 3.6 Receptor Survey <br />- The purpose of the receptor survey was to identify potential receptors and provide an estimate of <br /> -� the relative risks of adverse impacts to these potential receptors. This assessment evaluated the <br /> following potential receptors: surface water bodies, water wells, utility trenches, and buildings. <br />� The site is located adjacent to a large surface water body, namely Smith Bay of Lake <br /> Minnetonka. Other surface water bodies within approximately '/z mile of the site include other <br />� bays to the northeast and southwest and wetlands to the north and west(Figure 1). <br /> Water well records were obtained from the Minnesota Geological Survey as a part of this <br />� assessment. The well records for the water supply well on the site was not located. The closest <br /> identified wells to the site are Unique Well Numbers 100169 and 205621, located approximately <br /> 500 to 1,000 feet west of the site. Both of these wells are used for domestic putposes. Well <br />'� 100169 is cased to 117 feet below grade and is equipped with a nine foot screen with the bottom <br /> of the screen set at 126 feet below ground surface. Unique Well'Number 205621 has a five-foot <br /> screen set from 215 to 220 feet below grade. Both well logs indicate that at least the upper 125 <br />� feet of soil consists predominantly of clay. A location map for the wells and copies of the well <br /> logs are contained in Appendix VI. <br />� A vapor survey was performed at accessible sewer manholes, a storm sewer catch basin, and two <br /> residential basements located west of the Sailors World Marina in June 1995..Elevated PID or <br />� . <br />� , <br />