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01-04-94 12:28PY FROM UTSUREG ON f TO 912094640138 P003/007 <br /> Mr. Derrick Adal • <br /> December 17 , 1993 <br /> Page 3 <br /> collected to determine shallow (e10 foot) , intermediate (10-25 <br /> feet) and deep (30-55 feet) chlorinated hydrocarbon <br /> distributions in all locations. <br /> The absence of chlorinated hydrocarbons in ground water in <br /> the area north of the tank needs to be confirmed by ground water <br /> sampling and analysis. At a minimum, GSU recommends installing <br /> three boreholes with depth-discrete ground water sampling for <br /> both solvents and total petroleum hydrocarbon (TPH) analysis. A <br /> monitoring well may be a requirement of the Regional Water. <br /> Quality Control Board (RWQCB) for tank closures; therefore, the <br /> RWQCB should be consulted. Local ground water elevation <br /> information would be useful. <br /> General Comment 2 : Hydrogeologic Setting <br /> The Report references that ground water elevations for the <br /> LCN site are 5 to 15 feet below sea level (55 to 65 BCS) . This <br /> information conflicts with Exhibit 6 which shows the elevation <br /> of ground water elevation for the site to be at sea level. <br /> Also, the resolution of contours presented in Exhibit 6 is not <br /> clear. This indicates that at a site scale, the hydrogeologic <br /> information lacks sufficient detail to be meaningful. <br /> Recommendation: <br /> Exhibit 6 should clearly show ground water elevation values <br /> at posted well locations for reference. Additionally, <br /> conflicting depth to ground water data should be clarified or <br /> corrected. <br /> General Comment 3: Attenuation of Chlorinated Hydrocarbons <br /> WZI interprets that vertical variations in solvent <br /> concentrations are attributable to attenuation. Therefore, <br /> there is only a slight potential for ground water contamination. <br /> GSU does not concur with this interpretation. With the <br /> exception or Sample T-1 (15 feet) , the chlorinated nydrocarbons <br /> appear to be in the same concentration range for boreholes T-4, <br /> T-6, T-1, and AB-3. Additionally, a shallow sample at T-1 <br /> exhibits a lower value than a deeper sample. The limited data <br /> do not appear to support the attenuation hypothesis. <br /> Boring samples greater than 25 feet BGS at the northwest <br /> edge of the tank and greater than 40 feet BGS for the rest of <br /> the tank area have not been collected. Therefore, the extent of <br /> contamination is not clearly known (see Comment- 1) . <br /> contaminants appear to have migrated at least 40 feet. GSU <br /> interprets that the data represent a potential for ground water <br /> contamination. <br />