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KEI -P88-1013 R6 <br /> May 22 , 1996 <br /> Page 4 <br /> River alluvium was deposited by the Calaveras River, Bear Creek and <br /> several lesser streams <br /> Based on the results of our subsurface studies , the site and <br /> vicinity are underlain by fill materials to a depth of approxi- <br /> mately 1 to 5 3 feet below grade The fill is in turn underlain by <br /> alluvium to the maximum depth explored (72 5 feet below grade) <br /> Subsurface conditions are depicted on Geologic Cross-Section A-A' <br /> (Figure 8) The location of the cross-section is shown on Figure <br /> 7 <br /> The alluvium underlying the site consists predominantly of an <br /> irregularly interbedded sequence of silty clays, clayey silts, and <br /> silts Poorly graded to moderately graded sand or interbedded <br /> sandy silt and silty sand units were also encountered in the <br /> borings for the monitoring wells drilled at the site <br /> As of December 1995 , the unsaturated zone is approximately 46 feet/ <br /> thick and consists of interbedded units of silt, silty clay, and <br /> lesser amounts of sand The first water bearing unit beneath the <br /> site (first aquifer) consists largely of silty sand, silt and clay <br /> with much lesser amounts of sand In the eight existing monitoring <br /> wells, the units immediately above and below the water table <br /> consist of fine grained materials <br /> The particle size analysis (sieve only) previously conducted for <br /> the soil sample collected from the saturated zone in the boring for <br /> monitoring well MW13 at a depth of 65/feet below grade indicates <br /> that the sample is composed of 93% fine to medium-grained sand <br /> The sample is classified as sand <br /> DISCUSSION AND RECOMMENDATIONS <br /> Based on the analytical results of the initial ground water samples <br /> collected from monitoring wells MW16 and MW17 on December 19 , 1995, <br /> and subsequent samples collected during the March 11, 1996, <br /> monitoring and sampling event, the extent of petroleum hydrocarbons <br /> in ground water appears to be well defined, except for southeast of <br /> the site source area, in the vicinity of well MW16 , as shown on the <br /> attached Figure 2 Prior to recommending the installation of any <br /> addiL.Luiial muiiicuij ziy wells, KEI zecommeridS C hac, weir KW16 and <br /> MW17 be added to the monitoring and sampling program in order to <br /> verify the initial sampling results In addition, KEI understands <br /> that four Hydropunch borings and a monitoring well have recently <br /> been installed at the Montgomery Ward site Recommendations for <br /> additional work will be made based on the results of the ground <br /> water samples collected from the Unocal wells, as well as the <br /> 16 recent investigations conducted at the Montgomery Ward site <br />