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. _ r <br /> s- <br /> j <br /> Page 6 <br /> s <br /> geotextile fabric was encgvrftr d. This fabric separates the native soils bellow the fabric, <br /> from the imported sails abo,r t fob <br /> ric. The imparted fill material consists predominantly <br /> of sandy silt with some loo* Or"Unts of clay. The native soils below the fill material <br /> consists of highly organic peat and clay. <br />��' Labor�tory Testest l�escttts <br /> No visible or olfacto. ry evid��� �f contamination was observed, no contamination was <br /> indicated by the orgonic in any of the soil samples, sidew:alls or bottoms of the <br /> excavations or in the stockpiled.soil. Analytical results of soil samples collected from the <br /> excavations and the stockpiled s0if did not detect any total petroleum hydrocarbons (TPH) as <br /> diesel or benzene, toluene, x e e, or ethyl benzene (STX&E). Neither TPH or STX&E was <br /> detected in a water sample coftecifed from the bottom of the tank excavation. A summary of <br /> analytical results is included as Table 1. <br /> CONCLUSIONS <br /> Based on the findings of this investigation, all diesel contaminated soils associated with the <br /> former diesel underground storage tank have been removed and replaced with clean soils. <br /> Ground water encountered at 4 roximately 13.8feet beto�vgrade was found to contain non- <br /> detectable concentrations df TAH a0d bk)(&E. Previous soil and g ot}r►d water contamination <br /> encountered on the site:was likely the result of asphalt debris present in the fill material used <br /> to construct the building pad. <br /> ' RECOMMENDATIONS <br /> We recommend this site be issued a closure letter by Satz Joaquin County Environmental <br /> Health Division based on the results of this investigation. <br /> a,0e{ <br /> LIMITATIONS <br /> The above conclusions are based on our assessment of conditions indicated to exist as of the <br /> kyyqq;" <br /> dates of our field investigation, April 9-12, 1990. The results of this investigation do not <br />:i <br /> ib:i� <br />