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July 21, 1991 Harding Lawson Associates <br /> • Revised July 25, 1991 <br /> 17060, 025. 03 <br /> Mr. Hal Miller <br /> The Southland Corporation <br /> Page 2 <br /> activities MW-A and MW-7 (formerly MW-B) , near the tank <br /> backfill, were destroyed. The remaining 14 HLA wells were <br /> left intact. <br /> GROUNDWATER SAMPLING <br /> On June 10 and 11, 1991, HLA collected groundwater samples <br /> from all 14 monitoring wells. Before sampling, we purged at <br /> least three casing volumes from each well while monitoring <br /> temperature, pH, and conductivity. After those parameters <br /> stabilized, groundwater samples were collected with a clean <br /> stainless steel bailer, and decanted directly into <br /> laboratory-prepared volatile organic analysis (VOA) vials. <br /> The samples were labeled and placed into an ice-chilled <br /> cooler for transportation, under chain-of-custody, to a <br /> state-certified chemical testing laboratory. Between wells, <br /> all purging and sampling equipment was cleaned with an <br /> Alconox solution and rinsed with de.ionized water. A <br /> duplicate sample and a laboratory-provided trip blank were <br /> analyzed to provide quality control. <br /> CHEMICAL TESTING <br /> Samples were sent to Superior Analytical Laboratories in <br /> Martinez, California, and analyzed for total petroleum <br /> hydrocarbons (TPH) as gasoline, using EPA Test Method 8015; <br /> and for benzene, toluene, ethylbenzene, and xylenes (BTEX) , <br /> using EPA Test Method 8020 . The results of chemical analyses <br /> are presented in Table 1, along with groundwater data from <br /> preceding phases of site investigation and characterization. <br /> Laboratory data sheets and chain of custody are included in <br /> the Appendix. <br /> GROUNDWATER GRADIENT <br /> Water level measurements were obtained using a chalked steel <br /> tape accurate to 0. 01 feet. Well survey and water level data <br /> are presented in Table 2 . The water levels in each of the <br /> wells have declined relative to previous periodic <br /> measurements. Our calculations indicate a northeasterly <br /> hydraulic gradient, which is consistent with previous data <br /> for the site. <br />