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zNNW <br /> A"grab" groundwater sample was also collected from boring SBI. To collect the water sample, a <br /> core sampler was driven to the desired depth and the screen was exposed to the bed within the <br /> formation. A 0.17 inch diameter PTFE tube equipped with a stainless steel check valve was then <br /> inserted into the rods to the bottom of the sampler. Several attempts to collect a water sample by <br /> creating a positive displacement effect within the tubing were unsuccessful due to the presence of <br /> suspended silt in the water. To enable collection of a groundwater sample, a small diameter PVC <br /> casing with a 5-foot screened interval was inserted to the bottom of the boring. Groundwater <br /> samples were collected through the casing using the PTFE tubing. Samples were immediately <br /> placed into appropriate glass containers, labeled, and placed into a cooled ice chest. <br /> The completed borings were backfilled to the ground surface with neat cement grout. No soil <br /> cuttings were generated. All down-hole drilling and sampling equipment was decontaminated by <br /> washing with a laboratory grade detergent and rinsing with water. Rinseate collected from <br /> decontamination procedures was disposed of via evaporation on the asphalt/concrete surface within <br /> the confines of the investigation area. Soil and groundwater samples were submitted under chain <br /> of custody protocol to Argon Laboratories for analysis. <br /> 4.0 RESULTS OF INVESTIGATION <br /> 4.1 Subsurface Conditions <br /> A non native layer of A/B type baserock approximately 3 inches thick overlies native bedding, <br /> which consists primarily of lean clay and silts to a depth of approximately 22 feet bgs, the <br /> maximum depth explored. Shallow soil in the vicinity of boring SBI tended to have a higher <br /> sand content than the perimeter borings. SB 1 contained lean clay/silt with 25% sand from the <br /> ground surface to approximately 10 feet bgs, poorly graded sand with clay from approximately <br /> 10 feet to 15 feet bgs, and silt and lean clay below 15 feet. Borings SB2 and SB3 contained lean <br /> clay and silt with <5% sand from the ground surface to sixteen feet bgs. Groundwater was <br /> initially encountered at approximately 10 feet bgs in each boring and subsequently rose to <br /> approximately 7 feet bgs. <br /> No petroleum odors or discoloration were noted in samples collected from any borings. FID <br /> readings from the samples ranged from concentrations of I to 10 parts per million (ppm). Soil <br /> boring logs are included in Attachment A. <br /> 4.2 Laboratory Analysis <br /> Soil and groundwater samples were analyzed for total petroleum hydrocarbons as gasoline (TPHg), <br /> benzene, toluene, ethylbenzene and xylenes (BTEX), and organic lead using EPA methods 8015 <br /> modified, 8020, and the LUFT method respectively. In addition, the soil sample collected at 10 feet <br /> bgs from SBI and the groundwater sample were also analyzed for gasoline oxygenate additives <br /> using EPA method 8260. <br /> 4.3 Soil Analytical Results <br /> datalgroundze\baley\summary.doc 3 <br />