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i <br /> i <br /> Since borings MW-11 through MW-12 were drilled near previous CPT <br /> borings for the installation of groundwater monitoring wells, and since <br /> the sandy sediments present beneath the site presented the possibility of <br /> heaving (flowing) sands during drilling, the bottom of the auger was <br /> iplugged with a wooden block and no soil sampling was conducted in these <br /> borings In these borings, the drilling was halted at the desired depth o f <br /> the bottom of the well to be constructed, and the wooden plug at the <br /> bottom of the augers was knocked out with a 140-1b hammer dropped <br /> through the augers prior to the construction of the monitoring wells <br /> i <br /> Drilling equipment was steam-cleaned prior to use, and sampling <br /> equipment was washed with a TSP solution between sampling intervals to <br /> prevent cross-contamination Rinsate was contained on-site in sealed and <br /> ilabeled 55-gallon steel drums Drill cuttings were contained in steel bins <br /> and were transported to Forward Landfill for disposal <br /> i <br /> 5 . 0 SUBSURFACE LITHOLOGY AND HYDROGEOLOGY <br /> Sediments encountered during drilling generally consisted of sand of <br /> relatively high permeability from beneath the asphalt/concrete surface to <br /> approximately 18-feet bgs, followed by low permeability clayey and silty <br /> isediments from approximately 18-feet bgs to approximately 37-feet bgs <br /> Below 37-feet bgs lies sediments with high permeability until a depth of at <br /> r least 50-feet bgs is reached Below 50-feet bgs, the sediment layers <br /> 1 become discontinuous with high, medium and low permeability layers at <br /> various depths in different portions of the site until a depth of 120-feet <br /> bgs in reached where a relatively continuous layer of low permeability <br /> sediments is encountered At a depth of 130-feet bgs, a relatively <br /> continuous layer of high permeability sand is encountered Two geologic <br /> icross-sections have been prepared for this site The location of the <br /> geologic cross-sections is shown on Figure 4, and the geologic cross- <br /> sections are presented as Figures 5 and 6 <br /> Groundwater was encountered between 11 and 12-feet bgs The boring <br /> logs and well construction details are included as Appendix C <br /> 6 . 0 ANALYTICAL RESULTS FOR SOIL <br /> i <br /> The soil samples collected from 11 5-feet bgs (the capillary zone) in <br /> borings P-1, P-2, P-3, P-4, MW-13 and MW-14 were submitted to Kiff <br /> Analytical of Davis, California (ELAP 2236) for analyses The soil samples <br /> i Franks One Stop Report — May 2000 <br /> -8- <br />