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z <br /> Woodward-Clyde <br /> hydrocarbon constituent regardless of depth. As shown, both TPH and BTEX constituents <br /> occur in soil gas concentrically around the area of the removed underground storage <br /> tanks. This pattern suggests that contaminants moved directly downward from the tanks <br /> and ponded either on the groundwater or on a shallow soil horizon. Relatively high TPH, <br /> toluene and xylene concentrations observed at sampling point P136, and high toluene and <br /> xylenes concentrations observed at sampling point P11; suggest that the plume is <br /> moving generally west. <br /> 2.2 Eoil Florinas <br /> WCC subcontracted Datum Exploration and Drilling Company to advance 380 lineal feet <br /> of soil borings and install monitoring wells MW-5 through MW-9 in the boreholes at <br /> the locations shown on Figure 7. A permit to drill these boreholes was obtained from the <br /> San Joaquin Local Health District, a copy of which is included in Appendix B. The <br /> borehole locations were selected after reviewing the results of the soil gas investigation r <br /> with the intent of identifying the downgradient edge of contamination and the direction of <br /> groundwater flow. WCC originally intended to advance 5 boreholes to a depth of 60 feet <br /> and a sixth borehole to a depth of 80 feat with the understanding that groundwater <br /> occurred at a depth of about 40 feet (see WCC 1987). At the time of WCC April 1990 <br /> field work, however, the groundwater level occurred almost 15 feet lower than expected. <br /> The drilling program was modified by OSA so that WCC installed 5 wells (MW-5, -6, - <br /> 7, -8 and, -9) and i soil boring (S-5) instead of the original 6 wells. Soil baring S-5 <br /> was advanced at the northwest comer of the site adjacent to an open excavation of a waste <br /> oil tank that had been recently removed from the site. The total depth of the borehole <br /> was 25 feel, the maximum depth of exploration for the monitoring wells was 70 feel. <br /> All boreholes were advanced using a truck mounted CME 75 drill rig equipped with fl- <br /> inch O.D. hollow-stem augers. Soil samples were collected at 5-toot intervals and logged <br /> according to the Unified Soil Classificatlon System Visual-Manual Procedure ASTM <br /> D2488-84 by a WCC geologist. Logs of the materials encountered while drilling are <br /> presented in Appendix C. Soils penetrated by drilling consisted primarily of clay, clayey <br /> silt and silty clay, with lesser amounts of silt, sandy silt, sand and clayey sand to depths <br /> of 52 to 55 feet. From 55 feel to total depth, the soils consisted generally of poorly i <br /> graded fine grained sand. Groundwater was encountered between 55 and 56 [eel below, <br /> grade. The subsurface Ostribulion of the lithologies encountered is shown on Cross <br /> E <br /> Section A-A', .in Figure 8. <br /> 5 <br />