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A �AI3RIA <br /> Constant rate test recovery data from well S-1 were analyzed by the Theis Recovery method to <br /> estimate the hydraulic conductivity and transmissivity of this water-bearing zone The results <br /> should be considered approximate for the reasons previously discussed The hydraulic <br /> conductivity and transnussivity yielded from the Theis Recovery analysts of well S-1 constant <br /> rate test recovery data are 3 93 mlday and 12 9 m2/day This hydraulic conductivity is consistent <br /> with fine-grained sand (Todd, 1980) <br /> Mass Removal A total of 6,455 gallons of groundwater was extracted from S-1 and S-1-85 over <br /> the duration of this mass removal event Table 4 presents the pump test extraction data, <br /> analytical results of groundwater samples, and mass removal data The chemical analytical data <br /> collected during pumping were used to determine the mass of TPHg, benzene, MTBE, and 1,2- <br /> DCA removed during this event At the end of pumping, a total of 0 001 pound of MTBE, 188 <br /> pounds of TPHg,0 103 pounds of benzene, and 0 019 pounds of 1,2-DCA were removed <br /> SITE CONCEPTUAL MODEL UPDATE <br /> The data collected during this investigation did not significantly change the site conceptual <br /> model (SCM) for this site other than the finding that a former service station was present on the <br /> property north of the subject site This fact could affect the SCM if this former site is found to <br /> have had a historical release We have proposed assessment work on the property where the <br /> former service station was located The property owner has denied us access to the property <br /> The CPT investigation did not identified any other laterally continuous coarse-grained zone <br /> deeper than the one occurring at approximately 110 fbg The updated SCM is presented in <br /> Appendix J <br /> CONCLUSIONS <br /> Records Research Cambria's records research determined a former service station was present <br /> on the property north of the subject site Based on the fact that a service station was located <br /> north of the Shell site and that the predominant shallow groundwater flow direction is toward the <br /> southeast, it is possible that a release from this former service station may be contributing to <br /> groundwater impact in the vicinity of both sites Cambria has proposed work to investigate this <br /> former service station, but we have been denied access to the property to perform the <br /> investigation SJCEHD staff has offered to help discuss our property access request with the <br /> property owner <br /> 0797 10 <br />