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Work Plan-Soil and Groundwater Remediation <br /> + CSUS Multi-Campus Regional Center,Stockton,CA <br /> March 3,2003 <br />{ Page 3 of 3 <br /> 1, <br /> The January ll, 2002 report recommended quarterly groundwater monitoring, additional lateral and <br /> vertical groundwater characterization, and soil over-excavation. The soil over-excavation was a <br /> suggested remedial alternative that was most likely to result in rapid mitigation of site contamination. h1 <br /> a letter dated April 26, 2002 to Mr. Bailey of CSUS; Ms. Setliff of the SJCEHD agreed with the <br /> monitoring and additional groundwater investigation portion of the recommendations, but requested the <br /> evaluation of the feasibility of at least two remedial options for the site. <br /> Il <br /> Condor prepared a Problem Assessment Work Plan (PAWP) for the site dated January 23, 2003, to <br /> describe additional groundwater investigation at the site. The PAWP was prepared at the request of Mr. <br /> David Rosso for the Trustees of the California State University in response to a letter dated April 26, <br /> t 2002 from Ms. Setliff of the SJCEHD. The purpose of the work is to further investigate the lateral and <br /> Vertical extent of petroleum hydrocarbon contamination in groundwater at the site through the proposed <br /> F. installation of direct push borings to further evaluate the site hydrogeology; collection of discrete interval <br /> �. groundwater samples, and installation of at least one shallow monitor well and one deep monitor well to <br /> verify the results of the direct push sampling over time. As requested by the SJCEHD, the PAWP also <br /> included a remedial feasibility evaluation that compares and discusses remedial techniques for site <br /> remediation. Over-excavation and in-situ groundwater remediation has 'been selected to minimize total <br /> 'remediation time. <br /> Condor has conducted four quarterly monitoring events at the site (December 2001; June, September, and <br /> December, 2002); field activities included measurement of water levels and collection of water samples <br /> from the three monitor wells, MW-1, MW-2, and MW 3. The quarterly monitoring data indicate that <br /> -� !groundwater conditions at the site have remained relatively static. Monitor well MW-1 is located up <br /> gradient of the contaminant plume, and, to date, no petroleum hydrocarbon constituents have been <br /> detected in the groundwater samples collected from MW-1. Toluene and 1,2-dichloroethane (1,2-DCA) <br /> have consistently been detected in the groundwater samples collected from monitor well MW-2; f <br /> ' Benzene, ethylbenzene, total xylenes, total petroleum hydrocarbons quantified as gasoline (TPH-G), and <br /> '1,2-DCA were also detected in the groundwater samples collected from monitor well MW-2 during the <br /> December 2002 monitoring event. A slight petroleum odor has consistently been noted in the field <br /> l `inspection samples collected from monitor well MW-3. BTEX, TPH-G, methyl tertiary-butyl. ether <br /> I (MTBE), and 1,2-DCA have consistently been detected in the groundwater samples collected•from <br /> monitor well MW-3. In addition, tertiary-butanol (TBA) was detected in the groundwater sample <br /> collected from MW-3 during the December 2001 monitoring event. The groundwater gradient direction <br /> has fluctuated from slightly north of cast to southeast. <br /> # <br /> 3.0 SITE GEOLOGY <br /> Cross sections (Figure 4, Appendix A) through the hydrocarbon impacted soil at the site and are shown <br /> in Figures 5, 6, and 7, Appendix A. Soils underlying the site consist predominantly of interbedded clays <br /> and silts with interspersed thin beds of sand. Silty and sandy horizons form discontinuous, undulatory <br /> 4 interbeds and lenticular features. <br /> The clay stratum underlying the site varies in composition from dominantly stiff..to very stiff, fine- <br /> grained clay to silty/sandy clay. The silty horizons range in composition from clayey silt to sandy silt; a <br /> relatively continuous silty horizon with clay interbeds is present immediately below the former <br /> excavation area (Figures 5, 6, and 7, Appendix A) from approximately 14-32 feet below ground surface F <br /> '(bgs). This silty horizon appears to pinch out rapidly to the north, east and south of the former excavation G <br /> area. <br /> ' � 1 <br /> 4 <br /> La CONDOR l <br /> f J <br />