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a <br /> 1 A S S O C I A T E S I N C <br /> i <br /> for seasonal water level fluctuations The screen slot size is 0 020-inch Well construction details <br /> are depicted on the well logs contained in Appendix A <br /> ' 2.4 Monitoring Well Development <br /> Groundwater monitoring wells MW 1, MW2, and MW3 were developed on August 14, 1998 <br /> Each well was purged until the extracted water was relatively sediment free Development/purge <br /> logs are included in Appendix C Purgewater was temporarily stored on site in 55-gallon drums <br /> After fluid levels had been allowed to stabilize, groundwater levels were obtained from wells <br /> MW1, MW2, and MW3 Fluid levels were taken on August 14, 1998, utilizing an electronic <br /> water probe capable of measuring with an accuracy of 1/100 of a foot Groundwater flowed to <br /> the southwest at 0 05 feet per feet Groundwater elevation data are presented in Table 2 <br /> ' 2_5 Groundwater Sampling and Analysis <br /> On August 14, 1998, groundwater samples were collected from wells MW1, MW2, and MW3 <br /> The samples were collected after purging a mnmmum of three well volumes and stabilization of <br /> ' electric conductivity, pH, and temperature Field development/purge logs are presented in <br /> Appendix C Subsequent to purging, groundwater was sampled and transferred to appropriate <br /> sample containers, using clean, disposable bailers with bottom emptying devices to reduce <br /> volatilization Sample containers were then labeled with sample identification, placed on ice, and <br /> shipped under chain-of-custody to Sequoia Analytical <br /> The groundwater samples from wells MW1, MW2, and MW3 were analyzed by Sequoia for <br /> TPHg, TPHd, BTEX, oxygenate fuel additives, EDB, DCA, and total lead Groundwater <br /> ' analytical results are summarized in Table 3, and laboratory data sheets are presented to Appendix <br /> D <br /> ' 3.0 SUBSURFACE CONDITIONS <br /> Lean clay with sand was encountered in soil boring MWl in the upper 11 5 to 15 feet of the soil <br /> ' column Soil from depths between 11 5 to 15 feet bgs and 16 5 to 20 feet bgs consisted of silty <br /> sand Soil from depths between 16 5 to 20 feet bgs and 29 feet bgs consisted of sand with gravel <br /> Lean clay with sand was encountered in soil borings MW2 and MW3 In the upper 6 5 to 10 feet <br /> of the soil column Soil from depths between 6 5 to 10 feet bgs and 11 5 to 15 feet bgs consisted <br /> of clayey sand in boring MW3 and silty sand in boring MW2 Soil from depths between 11 5 to <br /> 15 feet bgs to 28 feet bgs, the maximum depth explored, consisted of sand and gravel <br /> 4.0 ANALYTICAL RESULTS <br /> ' 4_1 Soil Analytical Results <br /> Soil samples collected from borings MW 1 and MW3 contained no detectable concentrations of <br /> BTEX, oxygenate fuel additives, EDB, DCA, or total lead TPHd was detected at a low <br /> W\62500-qe oAs\sunm doe 3 <br />