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Summary of Data Interpretation <br /> Data from the April 2000 and April 2001 work initially appeared to show the most <br /> elevated concentrations of both soil and dissolved contaminants occur near the irrigation <br /> pipeline Also, on the basis of the soil data, there does not appear to be a deep <br /> contaminant penetration, and contaminants were not detected in the underlying confizimg <br /> strata One unverified report of surface spillage of fuel from an automobile near MW-9 <br /> was relayed to Wright however, the shallow soil sample PB-12-I at 5 feet showed that <br /> contaminants were not detected The PHS-EHD concern of elevated dissolved <br /> contaminants near MW-9 from a nearby shallow contaminant source does not appear <br /> hkely given the vadose soil and capillary soil data since elevated concentrations would be <br /> expected in the vadose soil column Some soil contaminant data near the former tank pit <br /> (P13-13-2 at I 1 5 feet) could be suggestive of a residual source slowly desorbing into <br /> groundwater near the former tank pit Soil samples at the 24- to 26-foot depth showed <br /> that contaminants were not detected, although dissolved contaminants were present <br /> Previous work had mapped the dissolved plume along an axis, which follows the trend of <br /> the former tank pit, along wells MW-3, MW-9 and MW-2 Quarterly momtonng has <br /> historically shown that the dissolved plume is present along this trend with wells MW-8 <br /> and MW-5 consistently clean The dissolved plume is essentially static, with no net <br /> movement downgradient Concentrations within the plume fluctuate, most noteably at <br /> wells MW-3 and MW-9 Contaminants observed at MW-b, in an upgradient position have <br /> consistently been lower than at MW-3, and in our opinion suggest an off-site source <br /> The sample data reported herein support this overall plume Iocation (see Figures 3 and 4 <br /> and dissolved contaminant maps in previous quarterly reports) Soil capillary fringe <br /> samples show residual contaminants, especially just down gradient of the former pit and at <br /> MW-9 The presence of sandy beds at depths of 8-10 feet apparently locally enhanced the <br /> dissolved contaminants migration north toward MW-9 However, some silty and clayey <br /> strata at depths of 3-8 feet appear to have absorbed UST leakage, creating a residual <br /> source at and gust north of the former tank pit Wright interprets a similar residual <br /> occurrence at MW-9 where clayey sand strata appear to have caused contaminants to <br /> absorb onto soil in the vicinity of MW-9 This observation was made in earlier work and <br /> together with that contamiant presence was the primary reason that monitoring well <br /> MW-9 was placed at this location <br /> Page 8 <br />