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Headspace <br />1.0 <br />2.0 <br />2.0 <br />0 <br />.•»‘Av <br />'/<:■ <br />smi <br />■:4 <br />mm►- -- ■! <br />mm <br />Hi <br />mm <br />w. <br />-4i-. <br />•4.■jii <br />MooitoriB»weUiMW-IO»ndMW-llarefreeofEPA«01/602p»niBetera. MoBiu>ri»*w*HMW-10hada <br />coBceBtniiOB of U Biicro»«Bi per liter (u*/l) of beazeoe. This low cooeoBtratioo ij <br />jiapect due to the ubiquitous nature of this compound in our environment. Monitonni well MW-12 <br />contained very low cOBceniratiOBS of xylenes, l.l-dichtofoethylene, 1,1-diehloroethane. and toluene. The <br />__of these parameters are aU below recommended allowable limio for drinkin* water. <br />.aalytical results from MW-10. MW-II. and MW-12 an provided in Appendix C. <br />a n mscUSSlQW <br />t <br />■>■1 Hy<r«wl»g , . <br />The water table of the unconfined aquifer at the site generelly occurs eight to ten feet below the <br />ground surface. Flow in this surficial aquifer U toward the south-southeast as discussed in our <br />December 23, 19S7 report. <br />Monitoring welU MW -4D, MW-10, and MW-11 are all screened at the same approximate elevation and are <br />25 feet below the ground surface. Together, these wells show that flow in the 20 to 25 foot interval is <br />toward the north-northwest. This apparent reversal in flow direction is suspected to be due to the <br />influence of the drainage trench and buried sewer Une along the eastern edge of the WSI property line, <br />between monitoring wells MW-10, MW-11, and monitoring well MW-4D and therefore is thought to be <br />very localized (Figure 2). We believe that shallower wells would reflect this same pattern and that <br />ground water flow in the 20-25 foot interval is similar to shallow ground water flow observed across the <br />site. <br />4.2 Fxfgwt of Soil end Ground Water ContlBliwitiftll <br />Soil and ground water contamination are primarily restricted to the area between monitoring weUs MW- <br />2 and MW-4. ConU Tunant conditions identified in this area are discussed in our December 23. 19d7 <br />report. The aerial extent of soil and ground water contamination is outlined in Figure 3. <br />The vertical extent of VOC contamination is restricted to the upper 25 feet of the site. Boring logs of <br />monitoring well MW-4D (Delta ’s May 24. 1987 report) show the presence of a sand unit between 21 and <br />24 feet. It is likely that the contaminants are moving through sand lenses such as this one. Our <br />objective for remediation will be to intersect as many of these sand lenses as possible with the recovery <br />trench. <br />mm-- <br />mi- <br />m-'-'A- <br />mm <br />|L • v4 <br />\l <br />Mm <br />,.Vr <br />kjl <br />i.l Ceneral <br />Delta recommends <br />concentrations iden <br />trench system wouh <br />out system at the <br />evaluated. Modifi <br />assessed. <br />^.2 Conceptual Pea <br />The east end of the <br />single total fluids S’ <br />aeration system for <br />into the sanitary se< <br />mass balance of th< <br />1.3 Wacovgrv Trcnc <br />The recovery trend <br />The total lengt'i of <br />18 feet. A crcss-s« <br />be dependent on th <br />the bottom of the i <br />coarse washed gravi <br />A plastic liner wil <br />prevent fine grainet <br />clean soil removed < <br />contaminant concer <br />hNu photoionizatio <br />The recovery sump <br />of approximately 11 <br />well cover. The su <br />long slots cut at 45