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w. ��d9.. wrf':�erzmrieae =aPttr�nertaw. <br /> Subsurfece investigation aesetts <br /> 6131 pacific Ave., Stockton, CA. <br /> Aegis project No. 90.020 <br /> Page 9 <br /> 2.8 SITE HYDROGEOLOGICI__REOIONAL GEOLOGY <br /> A complete review of the is included in Aegis' Pre-Tank <br /> Replacement Site Assessment Work Plan (Aegis March 6, 1990) . <br /> 2.9 WATER WELL INFORMATION <br /> A water well search will be conducted through the state of <br /> California Department of Water Resources to located water wells <br /> within 1/2 mile radius of the Site. <br /> 3.0 RESULTS OF SUBSURFACE INVESTIGATION <br /> A total of fourteen soil borings were advanced at the locations 's <br /> shown on Figure 5. Soil borings B-9 through B-14 were advanced to <br /> 21.0 feet below grade. Soil borings B--2 through B-S were advanced <br /> _ to 46.0. feet below grade, soil boring B-1 was drilled to 55 feet <br /> below grade. Lags of the soil borings are included in Appendix B. <br /> h <br /> A total of 28 soil samples from 'Che borings were submitted to a <br /> state-certified-laboratory for analyses. Copies of laboratory <br /> j reports are included in Appendix C. <br /> 3.1 SOIL CONDITIONS <br /> i <br /> Fourteen soil borings were drilled, sampled and logged, according <br /> to the methods described in Appendix A (B-1 was not sampled) . The <br /> soil borings ranged from 21.0 ft. to 55 ft. below grade. Soil <br /> Boring B-1 was advanced to ground water, away from suspected soil <br /> contamination. <br /> The soil boring logs were used to compile generalized cross <br /> section A-A, ' which is presented in Figure 6. As depicted in the <br /> cross section, silts varying from c3,ayey.to sandy composition <br /> were the predominant soil type encountered (Unified soil <br /> Classification System symbol ML) . Generally silty clays occurred <br /> at shallow depths, followed by interlayered horizons of sandy <br /> silts. Most of the deeper borings ended in clayey silts. Soil <br /> types ranged from a fine grained silty clays to medium grained <br /> silty sand, to sand. As shown on the cross section, soil types <br /> beneath the site generally coarsen with depth. <br />