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J. H. KLEINFELDER &ASSOCIATES <br /> File No. W-2008••1 <br /> November 14, 1985 <br /> t4 Page 3 <br /> foot above the perforated section and one foot bentonite plug was placed above <br /> the sandpack to provide a seal against surface water infiltration. The well was <br /> C <br /> placed inside a locking Brooks box to protect against vandalism. <br /> ' C 3amplinQ Procedure. <br /> 4•= Soil samples were collected at the time of drilling for chemical analyses <br /> at 5-foot intervals from 10 feet to 45 feet below the ground surface. After <br /> F; the sample was removed from the boring, the soil sample was immediately <br /> placed in a refrigerated container and delivered to California Water Labs for <br /> analytical testing. All samples were screened in the field with a <br /> Photoionization detector (PID) for qualitative indication of volatile <br /> hydrocarbons. FID values are shown or the boring logs on Plate IV. <br /> Selection of samples for quantitative chemical analysis was based on field <br /> screening and recommendations of the County Environmental Health <br /> representative present at the site during the time of sampling. A chain-of- <br /> custody form was utilized by Kleinfelder and accompanied the samples to the <br /> laboratory. Copies of the chain-of-custody forms are included in the <br /> Appendix. <br /> D. Water Sam 1� i Procedure. <br /> A water sample was collected from monitoring well (MW-1) on October <br /> 19, 1985. The well was sampled with a teflon bailer and the sample was <br /> vir•ially inspected for product layer and sheen. No product layer or sheen <br /> was observed in or on the bailer. The well was then developed until the <br /> water was relatively clear. after development, approximately five well <br /> " v:;lumes were removed and a water sample was collected in sample bottles <br /> provided by the testing laboratory. The sample bottles were immediately <br /> sealed and placed in a refrigerated container and delivered to California <br />