Laserfiche WebLink
Jeff Granberry Biwa <br /> . September 26, 1995 ( 9447-8620) <br /> December 18 and 19 1994 ground water monitoring wells MW-2 through MW-5 were <br /> installed on- and offsite The results of the CPT investigation and laboratory analysis <br /> were used to determine the placement of the four additional wells Wells MW-2 and <br /> MW-5 were installed onsite, while MW-3 and MW-4 were installed in the parking lot of <br /> Saint Bernadette Catholic Church located northeast of the site The soil boring logs and <br /> well completion details are included in Appendix D Laboratory analytical reports of soil <br /> samples collected are included in Appendix C and summarized in Table 2 <br /> January 24,_1995 all of the monitoring wells were gauged Blaine Tech Services, Inc <br /> (Blaine Tech), of San Jose, California gauged and sampled wells MW-2, MW-3, and <br /> MW-4 Blaine Tech's report is included as Appendix E Wells RW-1, MW-1, and <br /> MW-5, are currently incorporated in the VES and were not sampled Gauging data from <br /> the vapor extraction wells were collected by Fugro Figure 4 is a potentiometric surface <br /> map of the January 24, 1995 data The hydraulic gradient calculated from the <br /> January 24, 1995 monitoring event indicated the ground water flowed to the north at <br /> approximately 0 001 ft/ft Well gauging data is summarized in Table 4 Figure 4 is a <br /> distribution map of benzene in ground water which included the ground water samples <br /> collected from the CPT investigation <br /> February 9, 1995 Tom 0 Morrow, Inc of West Sacramento, California was on site to <br /> . survey the top of casing elevation of the wells The survey data are included in <br /> Appendix F An additional well gauging event was performed by Fugro on February 16, <br /> 1995 The data is summarized in Table 4 Figure 6 is the potentiometric surface map <br /> from the February 16, 1995 event These data indicate a gradient to the north at <br /> approximately 0 002 ft/ft <br /> 2.2 Gene Hized Geology and Hydi-ogeology <br /> Soil beneath the site consists of silt and clay to a depth of approximately 14 5 fbg <br /> Below 14 5 fbg, the soil is primarily silty sand Ground water was encountered from 10 5 to 15 <br /> fbg since investigations at the site began in December 1994 <br /> 3 0 RESULTS <br /> The following are the results of the ground water well destruction, UST removal soil <br /> sampling, hand augered boring drilling and sampling, recovery well installation, and soil disposal <br /> performed at the site <br /> 3.1 Ground Water Well Destiuchon <br /> Fugro personnel supervised Gregg Drilling of Martinez, California, decommission wells <br /> MW-1 and RW-1 on May 1, 1995 These wells were inside the estimated limit of UST <br /> . excavation, based on prior investigations and physical boundaries such as structures and property <br /> lines The method of decommissioning, as proposed in the March 8, 1995 Addendum to <br /> February 8, 1995 Soil Management Plea, was approved by Ms Mary Meays of the <br /> SJCPHS/EHD <br /> 94478620 ARP 6 <br />