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WEISS ASSOCIATES <br /> G.Boggs 29 June 1988/page'4 <br /> to ground water extraction and/or seasonal variations in recharge. Therefore, at the time <br /> of the hydrocarbon leak, the water table may have been lower than it i£ +presently, <br /> allowing the leaked hydrocarbons to accumulate below the present water _table. Of the <br /> twelve saturated soil samples analyzed during previous phases of the site investigation <br /> (reported on 10 June and 15 October 1987), the 20.7 ft boring 13-2 sample was the only one <br /> containing hydrocarbons. This suggests that the distribution of hydrocarbons in saturated <br /> soil at the site is quite limited since they have been identified only in the vicinity of this <br /> sample. <br /> 4. RATIONALE FOR MW-4 <br /> Proposed monitoring well MW-4 will be located at the southwestern corner of' the <br /> tank pit to monitor ground water directly beneath and adjacent to the edge of the . <br /> concrete slab. As indicated by analytic results for samples-collected under the slab, the <br /> majority of leaked hydrocarbons appear to have migrated laterally along the slab and <br /> then downward into unsaturated soil. Leaked hydrocarbons move downward through <br /> unsaturated soil, by gravity, until they reach the water table,.where they become a source <br /> of hydrocarbons in ground water. Therefore, analysis of ground water samples from a <br /> monitoring well, located immediately adjacent to the concrete slab should provide the <br /> earliest detection of hydrocarbons in ground water. <br /> A source-area well such as proposed well MW-4 should ideally be screened at and <br /> above the water table. However, the upper 6 to 7 ft. of saturated soil beneath the <br /> southwest corner of the tank pit may be low-permeability silty clay. A well monitoring <br /> the water-bearing zone at 25 to 34 ft, and also screening into the unsaturated zone, would <br /> create a conduit for the downward migration of hydrocarbons, if they are present, <br /> through the low-permeability sediments. Therefore, if no water-bearing sediments are <br /> encountered above 25 ft during the drilling of the boring for MW-4, well MW-4 will <br /> screen only the continuous water bearing zone between 25 and 34 ft and will not screen <br /> into the unsaturated zone. If shallower water-bearing sediments are encountered, the well <br /> will be screened in the shallower sediments. <br /> REPORT PREPARATION <br /> Following the excavation closure, a comprehensive reportwill be prepared that <br /> includes: <br /> o A summary of all previous work at the site including all figures, boring logs and <br /> tabulated analytic and water level data. <br /> o Descriptions of field procedures for the tank pit excavation, sampling and <br /> backfilling. <br />