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M MJ 11 1 <br /> SY <br /> 4 and possible drainag4 routes to the excavation. Figure 4 <br /> Is a projection of the excavated area, the area of visible <br /> contamination found when excavating and locations of Soil <br /> Borings 3 and 4 and lonitoring Well 3. This figure is not a <br /> true three dimensional projection and was prepared at the <br /> request of the AHD to the best of the writers ability. <br /> Figure S is a copy of a figure from the Versar report which <br /> is appended to the original Hunter & Associates report. This <br /> figure is included as a result of di.scussiofso fdisearlieof <br /> pit seepage. Figure 6 is an altered fig <br /> ureGTI report (also attached to the original Hunter & <br /> Associates report) which shows the contamination measure- <br /> ments found outside the 4scavated area on a geologic cross <br /> section originally prepared by GTI . Figure 7 shows the ;^ , <br /> location of the cress section. . <br /> Dispcoal of pit Seepage <br /> As discussed in the original report of Hunter & Aosocdi tes, <br /> the excavation at ane time was "out <br /> 45' <br /> 5 belov gr <br /> At �- <br /> o ..k <br /> this time, groundwater seeped into the pit t0 a depth Of <br /> about 51 . This groundwater was pumped out and into the <br /> westerly pcnd shown on Figure 1, using transfer hoses from <br /> the pit to the pond. The approximate route of the hoses ns <br /> from the westerly edge of the pit, between mw-1 and Spoil <br /> File No. 1 to the southerly extension of the westerly pond. <br /> prier to filling completely, the groundwater seepage � 9 <br /> been tested for hy&rccarbcn contamination and none w�.s I�Ound <br /> (see original report and appendices) . <br /> Drainage To ??t When Open To -45' <br /> Figures i , 3 and c and 7 shoe; the _"el i- <br /> c::ship of Boil <br /> ri I,gS 3 aIi'd <br /> to the excavation. This reviewer has noted <br /> that the pit, when water from the water table 14x5 draining <br /> *" as an 80' wide observaticr. <br /> into it, could be thought o_ , <br /> well . This aspect is not good if contamination is found <br /> cause it <br /> will not delineate the direclion and location of <br /> the contamination plume, However, it is-an excellentient test <br /> for contamination in general because a large volume of water <br /> has moved from ;-he formations intr,-the well from all <br /> directions. The cress section Of '�he pit (Figure 3) 4 <br /> illustrates the relationship of the bore holes to the <br /> excavation. When water drained from the periphery around the <br /> excavation towards the pit, it should have moved any <br /> contamination into the <br /> pit. Tests made on samples of pit <br /> later seepage never showed any indication of contamination. <br /> - — <br /> ain water through the vadose zone, into <br /> :also, seepage <br /> e r <br /> --- ... .... _ <br /> the water tG'�le _and--then- ...... <br /> -intothe-pit.,shou..l.d.._have bradg L _._.._._. _....._._ _._.__..—.._-- <br /> he pit from the vicinity of holes SB-3 <br /> contaminates into t ._._. <br /> and S^-4 if they had existed in anything other than minor <br /> amounts. This lihely path is shown on Figure 3. <br />