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r <br /> MS <br /> RE <br /> Site Assessment Report April 5, 1991 <br /> 139 South Center,Stockton,CA Page 10 <br /> sUBSURFACE CONDiTIONS <br /> SOILS <br /> The subsurface materials encountered during this Investigation consisted primarily of <br /> interbedded clayey sills,sandy silts,silty clays,and clean,well graded fine gravelly sand lenses up to <br /> 2-feet In thickness. The ilthobgies encamtered are illustrated on Figure 4,which presents a cross- <br /> section of the soils which were encountered. The water-t�*aring zone occurs in and below the sandy <br /> silts and appeers to be unconfined. Groundwater was encountered between 46-and 49-feet below <br /> — grsde. The results of the laboratory analyses of soil samples collected in the field from approximately <br /> 1-to 2-feet above the first encountered groundwater in the borings for MW-2.MW-3 and MW-4,and from <br /> 1-,6-and 10-feet alcove the first encountered groundwater In the boring for MW-1.alt reported non- <br /> detectable concentrations of BTEC and TPI+as-gasoline compounds. Copies of the laboratory reports <br /> are presented in Appendix F. <br /> a <br /> GROUNDWATER <br /> At the Urne of rronitoring-well Installation(February 14-15, 1991,and February 19, 1991), <br /> approximately 45 to 49-feet below grade,and aFnroxlmately 32-to <br /> groundwater was encountered at app y 44-to <br /> :-, 37-feet below sea level. When the groundwater was monitored,Its eleva.lon was approximately <br /> 46-feet below grade,suggesting unconfined conditions. The monitoring data collected on fvWch 8, <br /> 1991,were combined with the surveyed wellhead elevation data to produce the potentiornetric surface <br /> map presented as Figure S. The map shows a southeast groundwater slope <br /> wt-,ase gmdient Is <br /> M, <br /> approximately 0.002 foot-per-P--',t(ft/ft). This is a relatively shallow gradient <br /> The results of the labcratory analyses performed on the groundwater samples obtained from the <br /> rm <br /> site on March 8, 1991,Indicated measurable concentrations of TPl+as-gasollne in the water samples <br /> collected from monitoring wells MWA and MW-2(1,400 ppb and M. ppb,respectively). The laboratory <br /> t <br /> �• manHests and Chain-OfZtrstody Manifests are included In AppendIx D and summarized In Table 3. <br /> Figure 6 shows the TPH-as-gasoline concentration and benzene concertratlon!a?each well. <br /> .. Depth to water measurements made following development suggests a variable groundwater <br /> gradient direction. See Appendlx F for measurements of depth-to-groundwater before and after <br /> well development <br /> C GROUNDWATER <br /> W Tecwtiot.OGv INC. <br /> 4 ;� <br />