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�eCember 22, 1998 <br /> 41017 002 <br /> Mr <br /> HS/EiHD el Kith <br /> Page 4 t"tard'" Law'son Associates <br /> On <br /> July I3 1998, HLA submitted, via facsimile, the over <br /> July <br /> Margaret Lagor,a of the Site Mitigation grow excavation and sariiplin ry <br /> p Ms Lagorio approved thew,rko k Plan (HLA, 1998d)to <br /> On Jul , P on the afternoon of <br /> onsite Y 13 1998, the remaining UST sidewalls and bottom were <br /> The piping associated with e removed from <br /> tracks T}te , in the UST`vas removed back to were it tv <br /> p p was cut at this the excavation and stockpiled <br /> The removed piping was steam-cleanedtas dee with <br /> Gout, and the ends bent over and scatent under the adjacent railroad <br /> 1998, overexcavation of the rim of ii7i a hove and rinseate scaled with cold w <br /> Operator had been instructed that during the <br /> sods was performed and groundw Leri was no onsite weld <br /> encountering groundwater g the overexcavation process to avoid di On July 14, <br /> encountered The <br /> On Jul digging to deeply and potentially <br /> Y 15, 1998, Mr Kith and Ms La <br /> samples (T-5 through T-16 gor'o of the PHS/E <br /> (T-5 and T_s Hz] directed the collection of twelve additional soil <br /> were from the locations shown on Plate 3 <br /> Portion of the excavatiolncted from soils that had been beneath the c <br /> The tyvo remaining UST removal samples <br /> depths ranging overexcavation of im concrete bottom of the UST in the northern <br /> the fo g 8 from approximatel 8 5 pacted soils resulted in a circular variable- <br /> rrrir UST sidewalls Y to 10 5 feet bgs This ditch w <br /> whether overexcavation had m remainingas located in width dace with <br /> 10 samples (T-7 through T_ the area immediate! <br /> one) was collected to chemically ed su�cient im 25) were confirmation Y airsess <br /> Y Profile the stock pacted soil On Jul rrnation samples to assess <br /> pile of Impacted Y 1h, 1993, a composite sample (four-to <br /> Based on the analytical results (discussed below pacted soils for offsite disposal <br /> concentrations ofTPk-1 The two areas were olid ttvo areas wre indicated to have soil with <br /> north east(sample 1'-H sides of the excavation g the ditch <br /> these two areas le avoid sidesencoof the <br /> on the northwest(samples T-g nd Tt9l'1e <br /> (Plate 3) Additional overexcavation r ) and <br /> arrived onsite to observe the final round confirm On JuI <br /> to collect Y 21, 1998, Mr Harlin Proceeded carefully m <br /> samples in the two remainin im rination samples The u Knoll of the PHS/EffD <br /> impacted soil in these areas g pacted areas that would define the vertical and tat <br /> P rpose of the final sampling round was <br /> the excavation and samples T 2l throe ples -17 throw <br /> $ 23 tv�e ad�ctea aio llected aloe eras extent of <br /> excavation g the ditch iii <br /> g the ditch in the northeast side of the side of <br /> the northwest <br /> The final shape ofthe excavation was <br /> ranging ftom approximate) roughly circular with a di <br /> excavation had a de Y $ 0 to 11 5 feet b diameter of approximate) 90 <br /> pth of <br /> gs Groundwater tvas not encountered Y feet and depths <br /> of approximately 70 feet y 8 feet bgs, this consisted of the area beneath the mafoMY°f the <br /> The remainder of the excavation consisted of a circular <br /> overexcavation of impacted soils <br /> The ditch teas Iocatad e UST With a diameter <br /> range of aPProximately 8 0 to 11 5 feet b ditch resulting from <br /> and soils encountered during excavation activities exhibitedlust outside of the former sidewall and it had a depth <br /> gs LirhologieS of samples collected during <br /> borderline clay/slit ranging similar Iitholo i g these removal activities <br /> or clayey from reddish brotsn silt <br /> Y y silt contained S to percentY clay to clayey es Soils were fine-grained <br /> and dark grayish brined discoloration thfine-grained sand y y silt, whereas occasionally the silty <br /> Locally within apparentlyImpacted t3 clay and <br /> as observed soil, dark gray <br />