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- <br /> �. RL <br /> excavation and that the S:1LHD be notified in time to with ss all <br /> sampIing. <br /> After waiting until February, 198? , excavation was com-nenced <br /> without DHS approval , although they were notified that such <br /> activities were going to commence. The Dec. 9 , 1988 proposal was <br /> never approved by the DHS, presumeably owing to the fact that "%Ve <br /> have found the plan inadequate and are discontinuing our review <br /> as the work plan does riot specifically address or define the <br /> lateral and vertical extent of soil and/or groundwater contamina- <br /> tion." , quoted from Appendix A- 11 , May, 1959. It would seem that <br /> a proposed additional 3,335 cu. ft . of soil removal at the site <br /> of contamination, which encompassed an area from the surface to <br /> the groundwater vertically and horizontally to surrounding moni- <br /> toring wells, which had tested clean, could be presumed to remove <br /> all contaminated material , not just define extent . However , the <br /> proposal did not include the use of either a registerd geologist <br /> or engineer as is required by County and Tri -Regional guidelines. <br /> Based on the above premise, that all contaminated soil could be <br /> removed, the DHS was informed that owing to many considerations, <br /> including safety, protection of the groundwater from infiltration <br /> through the open pit that still had contaminated soil in it and <br /> time considerations, JTO was going ahead with excavation. 'During <br /> February, -1989 the pit was dug to its approximate size today, <br /> about 160 ' to 180' across at the outer perimeter and 45 ' deep; it <br /> was hater refilled to about 30 ' , its current depth (Figure 4) . <br /> Access ramps and erosion gulleys extend farther out. The original <br /> dug depth of about 45' below ground level (g. l . ) , put the bottom <br /> of the pit well into the ground water table; which had been found <br /> at about -38 to -40 ft g. l . by GTI . (Apendix A-7) . During exca- <br /> vation, he sides were cut with lifts ( terraces) to help prevent <br /> caving of the sidewalls, leaving the bottom of the pit about 10' <br /> to 60' smaller than the top periphery. The total spoil removed <br /> now totaled about 15,000 cu. yds. All clean spoil was placed on <br /> plastic sheeting over asphalt in Pile # 3, contaminated spoil was <br /> placed either in Pile 11 1 or Pile # 2 , also over plastic sheeting <br /> lving either on asphalt paving or concrete slabs. Segregation was <br /> achieved by a combination of visual inspection and odor. JTO re- <br /> ported that water did not immediately enter The hole when digging <br /> below the -3S' groundwater level . A clayey sand was penetrated at <br /> about -40 ' g. l . . at the south end of the excavation and ground- <br /> vater entered the hole thereafter. This clayey sand was logged in <br /> the GTI boring If 5. Water gradually filled the excavation to a <br /> depth of about -35' . 10' deep at the south end of the excavation <br /> (See Appendix 14 map) . The level of the water was measured by a <br /> surveyor and 3TO from the top of the asphalt surface at the top <br /> of tie entrance ramp, about-5G '-_aboC•e mean sea !e�`el : - i5-ivau ------ ------ ------- <br /> put the standing water level about 5 ' higher than either County <br /> Flood Controlrecords (Fig. 5 ) , or levels measured in the <br /> ;monitoring wells . The -35' b . l . elevation was taken in April . <br /> 1989, at' a time when there had not been any recent rainfall . The <br /> 4 <br />