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KEI-J87-0413 <br /> May 27, 1987 <br /> Page 2 <br /> native soil was taken from the pit at a depth of 10. 0 feet. <br /> Sampling was done in the presence of Mr. Doug Wilson of the San <br /> Joaquin County Department of Environmental Health. The soil <br /> sample was placed in a clean brass tube, sealed with aluminium <br /> foil and plastic caps, and stored in a cooled ice chest for <br /> delivery to Sequoia Analytical Laboratory in Redwood City, <br /> California. <br /> The subsurface soil exposed in the excavation consisted of silty <br /> sand. No odor was noted in the excavated soil. <br /> ANALYTICAL RESULTS <br /> The soil sample was analyzed for total hydrocarbons (THC--high <br /> boiling fraction) , Volatile Organic Compounds (EPA 8240) , and <br /> total oil and grease, as required by the California Regional <br /> Water Quality Control Board guidelines. The laboratory analyses <br /> show non-detectable levels of all constituents. Copies of the <br /> laboratory analyses and chain of custody form are attached to <br /> this report. <br /> CONCLUSIONS AND RECOMMENDATIONS <br /> The analytical results indicate that the concentrations of total <br /> hydrocarbons and Volatile Organic Compounds are within acceptable <br /> limits. Because of this, we recommend no further investigation <br /> at this time. <br /> Copies of this report and the attachments should be sent to the <br /> San Joaquin County Department of Environmental Health, and to the <br /> Regional Water Quality Control Board. <br /> LIMITATIONS <br /> Soil deposits and rock formations may vary in thickness, <br /> lithology, saturation, strength and other properties across any <br /> site. In addition, environmental changes, either naturally- <br /> occurring or artificially-induced, may cause changes in <br /> groundwater levels and flow paths, thereby changing the extent <br /> and concentration of any contaminants. Our studies assume that <br /> the field and laboratory data are reasonably representative of <br /> the site as a whole, and assume that subsurface conditions are <br /> reasonably conducive to interpolation and extrapolation. <br />