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® The overall shape of the PCE plume is relatively symmetrical from an apparent source located <br /> near the northern boundary of the landfill. The source location appears to be centered between <br /> well MW-5 (LFG probe GW-1) and well MW-8, and is likely a result of LFG contact with <br /> groundwater in the shallow aquifer. The apparent western edge of VOC impacted groundwater <br /> adjacent to the landfill is the western edge of the Corcoran Clay Formation, (Figures 2 and 5). <br /> The apparent eastern edge of VOC impacted groundwater adjacent to the landfill is well SB-1, <br /> which is an apparent groundwater high elevation point in the shallow aquifer(Figure 2). The <br /> plume of impacted groundwater is elongated in the direction of groundwater flow, which is <br /> generally to the north-northeast from the landfill. <br /> This interpretation is based on the review of data from only two monitoring events from the three <br /> off site wells. A more definitive interpretation can be made after at least four monitoring events <br /> collected through at least one complete climatic cycle. The minimum amount of data for a <br /> rudimentary calculation of average VOC concentrations within the plume is also four data points. <br /> Whether the plume is increasing or decreasing cannot be determined from the limited data <br /> available. However, because the landfill was closed over 16 years ago in 1996, and surrounding <br /> conditions, such as the construction of freeways, have not changed, it is likely that the VOC <br /> plume extent is relatively stable. Data from the off-site wells (MW-9A, MW-l0A and MW- <br /> 11 A)will indicate if the extent of the plume is changing with time. <br /> Deep Aquifer <br /> -6 own gradient): <br /> Concentrations of all parameters were within established concentration limits where the limits <br /> could be determined(Table 2). <br /> Based on output from the Sanitas statistical software, an increasing trend is reported in the <br /> concentration of TDS and a decreasing trend is reported in the concentration of chloride this <br /> quarter(Table 3). However,the changes in concentration are very small. Report of a"trend"by <br /> Sanitas software is an artifact of the software. <br /> No VOCs were reported at this well this quarter. Other than false positives, no VOCs have been <br /> reported since Toluene was reported in 2005 when the well was first installed. These Toluene <br /> data indicate that this compound was probably introduced by the drilling company when this <br /> well was installed in 2003,but quickly reduced to "trace"in three quarters. Excluding probable <br /> contamination during well construction and compounds also found the QC blanks, no VOC has <br /> been reported in this well. Therefore,there has been no indication of impact from the landfill at <br /> this well. <br /> MW-7(UP gradient): <br /> Concentrations of all the parameters analyzed were within established concentration limits this <br /> quarter except for Electrical Conductivity(Table 2). A comparison of general water quality <br /> parameters between MW-7 (up-gradient) and MW-6 (downgradient) indicates better water <br /> • quality downgradient of the landfill. This indicates that the landfill has no affect on the deep <br /> aquifer. <br /> Corral Hollow Sanitary Landfill 13 Department of Public Works/Solid Waste <br /> 3rd Quarter 2012 Groundwater Monitoring County of San Joaquin—October 30,2012 <br />