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� Sailors World, Inc. <br /> Summit Project No. 922030 - <br />� October 5, 1995 <br /> Page 4 <br />� method. Generally, soil vapor headspace readings decreased with depth, indicating the majority <br /> of petroleum hydrocarbon impacted soil was present in the upper 4 to 5 feet of soil. <br />� The excavation was limited in a southeasterly direction because of the presence of underground <br /> utilities (Figure 2). Subsequently, three hand auger borings were completed in an area southeast <br />� of the excavation. Results of soil headspace screening at these locations indicated soil in this <br /> area was impacted with petroleum hydrocarbons. PID readings at these locations ranged from 66 <br /> to 150 ,ppm. Observations recorded during the excavation activities and related laboratory <br />� , analytical results are included in the attached excavation report(Appendix II). <br /> Impacted soil was transported in May 1993 to C.S. McCrossan, located in Maple Grove, <br />� Minnesota. A total of 130 cubic yards of impacted soil were thermally treated: 60 cubic yazds <br /> previously removed by Foth & Van Dyke and 70 cubic yards removed under the observation of <br /> Summit. <br />� 3.2 Test Probes and Site Geology <br />� On June 15, 1994, eight Geoprobem test probes, P-1 through P-8, were completed and <br /> groundwater samples were collected. Water was not observed at P-7, which was completed to a <br />� depth of 10 below the ground surface. Probe depths ranged from 5 to 10 feet deep and probe <br /> locations aze illustrated on Figure 2. <br />� An additional seven Geoprobe� test probes (labeled P-9 through P-15 on Figure 2) were <br /> completed on 7une 2, 1995. Four of these test probes were completed on the property owned by <br /> Sailors World and three probes were completed on the right-of-way of Counry Road 15. A <br />� Macro-Corem 4-foot long sampling system was utilized to collect soil cores at these test probe <br /> locations. Variable soil types were encountered and soil descriptions included silty clay, sand, <br /> silty sand, and gravel. Much of the soil that was observed may be fill, as indicated by an asphalt <br />� layer that was encountered at approximately 4 feet below the ground surface at test probe <br /> location P-11. Wet soil was encountered at depths ranging from 1.5 to 5 feet below grade. <br /> Observations at several test probe locations indicated that the soil was not consistently <br />� "saturated" or wet at depth. "Dry" soil, or soil that appeared to be below saturation, was observed <br /> underlying coarser, wet soil at P-9, P-11, P-12, and P-14. Several probes were completed near <br /> previous probe locations to evaluate movement of hydrocarbons in the subsurface during the past <br />� year. Probe P-15 was completed in the former UST basin, between the previous probe location <br /> that showed the highest benzene concentrations (P-3) and the probable groundwater discharge <br />� area(Lake Minnetonka). Geoprobe�test probe logs that contain soil descriptions are included in <br /> Appendix III. <br />� . <br />' <br />� <br />