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[ N V 1 R O N M E N T A L <br />� P A R T N[ R 5 I N C <br />August 5, 2002 <br />Ms. Sharman Braff <br />Safeway Inc. <br />5918 Stoneridge Mall Road <br />Pleasanton, CA 94�88-3229 <br />.., , .:. . . . . �. A,,..,... Il.i.,......, i. . ......:_ . ..� <br />Re: Baseline Ground Water Quality Assessment <br />Safeway Slore No. 1484 — Former BP Service Slation <br />4102 RuckerAvenue <br />Everett, Washington <br />EPI Project No. 082163.1 <br />Dear Ms. Braf(: <br />���JU5U5 -CL�j <br />�/�� <br />C�,��, <br />Environmental Fartners, Inc. (EPI) is pleased lo present ttiis baseline ground water quality assessment <br />for the property localed at 4102 Rucker Avenue in Everett, Washington (site). The purpose of this work <br />was lo provide baseline ground water qualily information for the site after the cessation of retail fueling <br />and prior b construction of a new Safeway retail fueling center at the site. The general location of the <br />subjecl property is shown on Figure 7. <br />Ground Water Sampling Procedures <br />On June 7, 2002, EPI sampled a total of six monitoring wells at ihe site and one monitoring well in <br />Rucker Avenue to Ihe east oi the site (i.e., MW-8). Sampling was conducted in coordination witli <br />AMEC, who were on-site collecting ground water samples from several of the wells for BP. EPI split <br />samples from wells sample�l by AMFC (i.e., MW-5, MW-6, MW-7, and MW-B). EPI was not able to <br />sample monitormg well MW-3 because a job trailer was parked on top of the well. EPI also coliected <br />samples (rom wells MW-1 and NW-10. There appear to be several olher wells on the pro�er:y that <br />were not labe�ed on Ihe maps that were provided to EPI by BP. These wells may be air sparging or <br />vapor extraction wells. EPI sampled one o( lhese wells, which they labeled Unknown-1 for the <br />purposes of this work. Well locations are indicated on Figure 2. <br />The depths to water and tolal depth of well were measured using an electronic water level mete:r. To <br />ensure reproducibility of the data, all measuremenls H�ere made to the north side of lhe top surface of <br />the well casing. The average depth to ground vrater was 5.73 feet below grade. According to site data <br />collected during this monitoring evenl, the hydraulic gradient is generally noriherly to northeasterly with <br />a slope of approximately 0.016 (eet per foot. Piezometric elevalion contours are also indicated on <br />Figure 2. <br />