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Borings were advanced using a Geoprob& Model 5400 equipped with a GH-40 Soil Probing <br /> Hammer. Prior to drilling operations, Fisch obtained an "Application for We1llPump Permit" <br /> from PHS/EHD to install the soil borings (Appendix A). <br /> Drilling and sampling activities were conducted on August 6, in general accordance with <br /> procedures described in the Work Plan. The initial boring (B1-1) was drilled to a total depth <br /> of 20 feet below ground surface (bgs) and was located approximately 10 feet away from the i <br /> northwestern edge of the former tank(Figure 2). Per the Work Plan, continuous-core samples <br /> were collected from the initial boring using a 4-foot long, 2-inch diameter, Macro-Core Open <br /> Tube Sampler equipped with a clear, polyvinyl chloride (PVC) "plastic liner. Following <br /> extraction from the Macro-Core Sampler, core tubes were typically cut in half, capped, labeled <br /> and temporarily stored in an ice-cooled chest. A lithologic log was prepared during drilling <br /> based on examination of the soil cores and utilizing the Unified Soil Classification System and <br /> generally accepted geologic interpretive descriptions (Appendix A). Soil cores were examined { <br /> for the presence of staining, discoloration, or odors indicative of petroleum hydrocarbon j <br /> contamination. In addition, a photoionization detector (PID) was used to check for the <br /> priesence of petroleum hydrocarbon vapors in the open borehole. No indications of petroleum <br /> hydrocarbons were noted during drilling of the three borings at the`site. After reviewing the j <br /> Iithologic log and PID recordings, Carol Oz of PHS/EHD requested that three soil samples at <br /> 8:? 13, and 18 feet bgs be submitted to the laboratory for PHC analysis. <br /> 3 <br /> LGroundwater was present in the open borehole after the boring had been advanced to about 10 ' <br /> feet bgs. A groundwater sample .was collected at this.depth by inserting a 1-inch diameter <br /> PIC tube, machine slotted with 0.001-inch diameter openings, from the bottom of the boring <br /> to the surface. Prior to collecting the groundwater sample, the depth-to-water wasmeasured <br /> using an electric water-level sounder lowered into the PVC tubing. One quarter,inch diameter <br /> LTeflon tubing, equipped with a check valve at the submerged end, was then inserted into the <br /> slotted PVC tube. Groundwater was brought to the surface within the Teflon tube by moving <br /> the Teflon tube up and down in a piston-like motion. <br /> jE <br /> Two additional borings, B1-2, and B1-3 were drilled to a total depth of 19.0 feet bgs and were <br /> located approximately 10 feet south and 10 feet east of the former tank, respectively (Figure <br /> 2). At the request of Carol Oz of PHS/EHD, soil samples were collected in each of these <br /> borings at depths of 13 and 18 feet bgs for laboratory submittal. Samples were collected using i <br /> a"2-foot long, 1-inch diameter, Lange-Bore Soil Sampler equipped with a clear acetate plastic <br /> liner. A groundwater sample was collected in each of the two borings at a depth of 12 feet bgs <br /> using the method described above. -The three borings were subsequently grouted to the surface <br /> with neat cement per PHS/EHD guidelines. <br /> 1 <br /> 3 <br /> 961171INVRP151S1 USTINV.1tP7' <br /> .I� <br /> BOYAJIAN & ROSS, INC. <br /> Environmental Scientists & Engineers <br /> EE <br />