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Y <br /> w� <br /> - � <br /> �.-rte-. <br /> w <br /> ItN G1: 0t, 0t, IC ]Z F. Stll: ItCIiS , <br /> J.Randall/15 SCPCCMher 1989 <br /> the former location of the pump islands. <br /> i <br /> During the period from 27 February 1989 to 2 March 1989,rive borings,B-1 through 13-5.were <br /> g drilled and completed as 4-inch diameter monitor wells MW-1 through MW-5,respectively, Wells MW- <br /> 1 and MW-5 were screened from 8 fl below grade to 328 ft and 24.5 ft, respectively. Wells hiW-2 <br /> through MW-4 were screened from between 16 ft and 17 ft to between 20 ft and 24 ft. The screen was <br /> terminated at the top of the confining layer,below the first water-bearing zone. Screens were brought <br /> up higher in wells MW-1 and MW-5 to capture any liquid hydrocarbons teat might be present. <br /> • y, Soil samples were collected from all live borings at approximately 5-ft intervals and sent under <br /> chain-of-custody to Central Coast Analytical Services (CCAS) of San Luis Obispo, California, for <br /> analysis by EPA Method 524.2. TPPH were dctected only in borings B-1,B-2 and B-5,on the southern <br /> half of the site, and primarily in the first 16 ft of soil below the ground surface. The TPPH <br /> ® concentrations ranged from 4 ppm to 390 ppm. BTEX were not dctected in soil samples collected <br /> from borings B-3 and B-4. BTEX were detected in soil samples collected from borings B-1,B-2 and <br /> B-5,with benzene concentrations ranging from 0.2 ppm to O.94 ppm. Groundwater samples were taken <br /> from the completed monitoring wells MW-1 through MW-5 on 22 March 1989 and sent under chain- <br /> of-custody to CCAS for analysis, TPPH,reported as gasoline,were detected in wells MXV-1,MW-2 and <br /> MW-3 at 30,000 ppb,9,000 ppb,and 4,000 ppb,respectively, BTEX were detected in samples from wells <br /> MW-1, MW-2,and MW-5 with the highest concentration of benzene detected in the sample from well <br /> MW-1 at 3,600 ppb. In addition,1,2-dichlorobenzene(1,2-DCB)was detected at 10 ppb and Freon-113 <br /> was detected at 20 ppb in the sample from well MW-5, historic analS,ic results are included in Table <br /> 1. The estimated direction of groundwater flow was based on depth-to-water measurements taken on <br /> y the 22 March 1989(Table 2). <br /> GROUNDWATER SAMPLING <br /> W--IIs MW-1 through MW-5 were sampled on 12June 1989 by WGR environmental technicians <br /> Beverley Ualdwin and Madeleine Stanger.according to WGR's standard operating procedure(SOP-4) <br /> included-as Appendix A. All purged water was collected and temporarily stored onsite in 55-gallons <br /> drums pending results of laboratory analyses- The groundwater samples and laboratory supplied travel <br /> blanks,made up of deionized water at the laboratory,were sent under chain-of-custody to Central Coast <br /> Analytical Services(CCAS) of San Luis Obispo,California. The chain-of-custody forms are included <br /> i as Appendix B, <br /> 3 <br /> 10112SC7 <br />