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feet bgs to <1 ppm in all soil samples collected below 55 feet bas (see borehole log, <br /> Appendix B). <br /> • The augers and sampling equipment were steam cleaned prior to drilling the boring and <br /> the sampling equipment was washed with a TSP solution and rinsed in clean water <br /> between each sampling interval. <br /> LITHOLOGY OF SOIL. SAMPLES <br /> During the drilling and sampling operations the WEGE geologist maintained a log of the <br /> materials encountered (see Appendix B). The top 26 of section consisted of medium <br /> brown silty clay, and stiff dry clay with occasional strong petroleum odor beginning at 20 <br /> feet below ground surface (bgs). A six foot layer of medium grained sand containing <br /> smaller lenses of silt and clay was encountered between 20 and 26 feet bgs. A color <br /> change from medium brown sediments to greenish gray occurs at 26 feet bgs. The <br /> section from 26 feet to 48 feet consists of a stiff greenish clay with some petroleum odor <br /> that grades downward to clay with silt. The section from 48 feet to the base of the soil <br /> boring at 80 feet bgs consists of a greenish gray to dark gray silt and clay with fine to <br /> very fine sand layers occurring at 52.5-56 feet bgs, 60-64 feet bgs and 78-80 feet bgs. No <br /> petroleum odor was noted in any of the samples collected below 50 feet_ <br /> PRESERVATION OF SOIL SAMPLES <br /> The ends of the brass sleeves containing the soil samples were sealed with a Teflon film <br /> and further protected with plastic caps. Each sleeve was labeled with site name, date, <br /> time, sample location, and analyses to be performed. Each labeled soil sample was <br /> placed in a separate zip lock bag, deposited in and ice chest, and cooled to 4'C. The soil <br /> samples and accompanying chain of custody documentation were delivered to Kiff <br /> Analytical Laboratories (DHS# 2236), on December 13, 2000. <br /> COLLECTION OF GROUNDWATER SAMPLES FROM S—BI- <br /> Three <br /> 1Three groundwater samples were collected during the drilling of TH1 using <br /> "hydropunch" techniques. The water samples were collected from the two foot screened <br /> interval of the hydropunch tool at the depths of 60-62 feet bgs, 70-72 feet bgs, and 80-82 <br /> feet bgs. <br /> The auger and bit were advanced to three feet above the top of the desired sampling <br /> interval at which point a hydropunch tip and screen was inserted through the hollow stem <br /> auger at the end of a hollow rod and driven five feet into the formation at the base of the <br /> test hole. The covering of the screened interval of the hydropunch tool was then retracted <br /> two feet to allow groundwater to enter the tool. Groundwater samples were collected <br /> from the screened tip of the hydropunch tool with a mini bailer through the hollow rod. <br /> The water samples were decanted into 4 VOA vials with no airspace and preserved with <br /> 0.5 ml of HCL. The water samples were labeled and preserved as described above for the <br /> soil samples. <br /> ARC SRPT 312101 3 <br />