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90343TEXT CON-3 • . <br /> Soil samples were collected for laboratory determination of total <br /> petroleum hydrocarbons and to provide information on subsurface <br /> stratigraphic conditions. Three sets of samples were taken at three foot <br /> intervals beginning at a depth of 3 feet below grade (3 to 4.5 ft; 6 to 7.5 <br /> ft; and 9 to 10.5 ft) . The samplers were collected using a 2.5 inch <br /> diameter by 18 inch long modified California sampler containing three brass <br /> tubes 2.5 inches in diameter and six inches long. The sampler was driven <br /> ahead of the augers to the desired depth by dropping a 140 lb. hammer <br /> approximately 30 inches. The average number of blows (blow count) required <br /> to advance the sampler over a 12 inch increment of the sample interval were <br /> recorded on the boring log. The sampling equipment was cleaned with a low <br /> phosphate detergent and deionized water rinse between each sample drive. <br /> After each drive the sampler was removed from the boring and <br /> disassembled. In general the bottom tube from each drive was retained for <br /> analysis. The tubes were sealed with aluminum foil , a PVC end cap, <br /> electrical tape and stored on ice in a cooler until shipment to the <br /> laboratory. In a few samples, only partial recovery was achieved in the <br /> bottom tube in which case the middle tube was retained for analysis. The <br /> samples were numbered according to boring, sample location and tube <br /> number. For example the third (bottom) tube from the first sample drive <br /> (3.0 to 4.5 ft) in Boring 2 would be labeled B2-1-3. <br /> Of the 12 samples collected, eight were selected for laboratory <br /> analysis. Sample selection was based primarily on the potential for <br /> contamination. All three samples from Boring 2 were selected due to its <br /> location within the spill area. The samples from the lower two drives in <br /> Borings 1 and 3 were selected to assess potential hydrocarbon migration <br /> both through the soil and along the water table. Because the distance from <br /> the source was expected to preclude lateral migration through the soil , <br /> only the sample just above the water table in Boring 4 was retained for <br /> analysis. Standard chain-of-custody procedures were used to track the <br /> collection and shipment of samples. <br />