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r y y,I S L <br /> Iva <br /> Sampling Ev <br /> On March 10, 1989, the soil in the area about Sample Point 31035 was excavated an <br /> additional 6 feet in depth (from 8.5 feet to 14.0 feet below ground surface). The 14 to 17 <br /> cubic yards of additional) excavated material was stock-piled on plastic sheeting near the <br /> a y feet below round surface consisted of red-brown silt to fine- <br /> excavation. Soil $.5 t 11.0 g <br /> grained sandy silt. At a depth of approximately 11 to 13 feet, a tense of gray-colored soil <br /> was encountered. The gray-colored soli had a sewage-type odor. Below the lense of gray <br /> soil, the red-brown silt to sandy silt was encountered again. After the excavation was <br /> completed, the gray-colored soil was visible on the north side wall, but not visible on the <br /> south, east, or west ssdewalls (Plate 3). <br /> A Kleinfelder geologist collected two samplesof native soil from the excavation. Sample <br /> 22926 was collected from the floor of excavation at a depth of 14 feet, and Sample 22927 <br /> was collected at a depth of 13.5 feet from the north sidewall. Both samples consisted of a <br /> red-brown silt to fine.-grained sandy silt, moderately to well cemented. The locations of the <br /> excavation sampling points from the February 23 and March 10, 1989, sampling events are <br /> shown on the Sample Location/Cross-Section Location Map (Plate 3) and Doss-sections <br /> A-A" and B-B' (Plates 4 and 5). <br /> Soil samples were obtained in clean brass tubes. Sample tubes were decontaminated prior <br /> to sampling by washing in a solution of trisodium phosphate (TSP), followed by a distilled <br /> water rinse. Each tube was retracted, capped with Teflon sheeting and tightly fitting plastic <br /> end caps. Samples were labeled, logged on chain-of-custody and stored on ice until <br /> delivery to California Analytical Laboratories/Enseco in West Sacramento, California. A <br /> representative from the SJLHD, Ms. Lititia Resch, was present throughout the sampling <br /> process. <br /> A photolonization detector (PID) wasused in the field to screen the soil for volatile <br /> organic consultants below 10.3 eV. Neither of the two soil samples showed PTD readings <br /> above ambient background levels. The gray soil had a PID reading of 65 parts per million <br /> by volume. <br /> Analytical Results <br /> The samples were analyzed for TPH extractable (Method 3550) by GC/FID; and BTEX by <br /> EPA Method 8020.The samples were analyzed on a one-week rush turnaround schedule. <br /> TPH and BTEX constituents were below laboratory reporting limits in Samples 22926 and <br /> 22927. In Sample 22927 collected from the wall of the excavation, a late eluting (heavy) <br /> hydrocarbon was indicated. The hydrocarbon was not indicative of fuel hydrocarbons or <br /> diesel associated with the excavated tank. It may be associated with the gray-stained soil <br /> on the north side of the excavation. The late eluding hydrocarbon could not be quantified <br /> or identified further. <br /> Based on the L analytical results, the hydrocarbon contaminants associated with the <br /> excavated diesel tank appears to have been removed. <br /> Meinfelder recommends a copy of this report be submitted to the SJLHD for their review. <br /> If you have any questions or require our services any further, please do not hesitate to <br /> contact us. <br />