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Mr. Gerald Djuth,P.E. <br /> November 3, 2003 <br /> Page 3 <br /> or to optimize data quality. Although Figure 1 shows 7 borings, the actual number of borings <br /> required in the field will depend on observed conditions. <br /> Soil and Groundwater Screening <br /> Before drilling or sampling, all equipment used to generate samples will be cleaned using either <br /> high-pressure water, trisodium phosphate, or equivalent. Wastewater from decontamination will <br /> be captured and recycled through LFC's on-site wastewater treatment system. <br /> Soil samples will be collected and screened for impacts by an experienced GeoTrans field <br /> engineer or hydrogeologist. Each of the borings will be advanced to groundwater using a 2-inch <br /> diameter sampling spoon or equivalent. Samples will be collected continuously below a depth of <br /> 5 feet using a Geoprobe sampler. Immediately upon recovery, samples will be placed into <br /> resealable bags and lithologically logged using the Unified Soil Classification System. The bags <br /> will be marked with the boring location and sample depth and screened for odor. A description <br /> of impacts (if any)will be recorded on the lithologic log. <br /> Before sampling, depth to groundwater will be measured in the Geoprobe borings and in on-site <br /> monitoring wells,using an electric water level probe. Relative groundwater elevations will be <br /> measured using an engineers level. Also, the location of the boring relative to permanent site <br /> features, such as the fence corners, will be measured and recorded. This information will be <br /> combined to determine groundwater flow direction. <br /> Immediately after the boring is completed, depth to water will be measured from a stable datum, <br /> such as a stake or nail driven adjacent to the boring. The time of measurement will be recorded <br /> and a plot of time versus depth to water will be prepared in the field. The water level will be <br /> considered to be equilibrated when either the plot shows an asymptotic recovery trend, or no <br /> change is observed in the water level over a period of 10 minutes." <br /> After equilibrium water levels have been established, a groundwater sample will be collected <br /> through the Geoprobe boring,using a peristaltic pump with new polyethylene and silicone <br /> tubing, or equivalent. <br /> Soils and groundwater from the borings will be screened using odor, since the groundwater <br /> standard is odor based. Soil and groundwater samples collected at each of the boring locations <br /> will be labeled and maintained until the program is complete. At that time, soil and/or <br /> groundwater samples from intermediate points may be selected for analysis to show <br /> downgradient hydrocarbon decay. Sample selection will be based on the length of the plume and <br /> the perceived usefulness that the additional data might provide. <br />