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next monitoring event be utilized to confirm this increase at both the upstream and downstream <br /> monitoring locations. <br /> Soil cover has been placed over the waste material to prevent ponding of stormwater and to <br /> protect surface water. In addition, a perimeter ditch directs stormwater to a basin in the southeast <br /> comer of the site. A smaller ditch collects stormwater from the grinding area in the northeast <br /> comer of the site. Inspection and maintenance procedures for these stormwater control structures <br /> are provided in the site's Stormwater Pollution Prevention Plan. The facility reported that these <br /> control structures effectively directed stormwater from the waste material during the first quarter <br /> 2011. <br /> 2.0 Groundwater Monitoring Program <br /> During the first quarter 2011 monitoring event, groundwater monitoring was performed at the <br /> French Camp Landfill by Del-Tech. Groundwater samples were collected from two background <br /> monitoring wells (MW-6A and MW-7A)and four detection monitoring wells(MW-8A,MW-9A, <br /> MW-913, and MW-10A) during the fast quarter 2011 monitoring event. The analytical results <br /> from samples collected at these wells are used to determine potential landfill-related impacts. <br /> The WDRs stipulate semi-annual sampling of the background monitoring wells and detection <br /> monitoring wells for field parameters (pH, specific conductance, temperature, and turbidity) and <br /> monitoring parameters(bicarbonate, calcium,carbonate, chloride,magnesium, nitrate,potassium, <br /> sodium, sulfate,TDS,and VOCs). <br /> The field results provided by Del-Tech and the laboratory results provided by TestAmerica for <br /> the first quarter 2011 groundwater monitoring event are summarized on Table 2.2. The historical <br /> groundwater data for the background and detection monitoring wells are presented in Appendix <br /> D. Times series concentration plots of historical groundwater data for the monitoring wells are <br /> presented in Appendix E. The concentration limits presented on Table 2.2 were calculated from <br /> background data collected through the third quarter 2010 monitoring event. The statistical <br /> analysis calculations for groundwater monitoring wells are presented in Appendix E. A copy of <br /> the statistical analysis methodology is presented in Appendix C. <br /> As presented on Table 2.2, the following constituents exceeded their respective concentration <br /> limits during the first quarter 2011: calcium at MW-913; chloride at MW-913; potassium at MW- <br /> 913; and field temperature at MW-10A. There were no VOCs detected at a groundwater <br /> monitoring wells during the first quarter 2011 monitoring event. <br /> Historical data from the groundwater monitoring wells were analyzed for temporal trends using <br /> Mann-Kendall / Sen's Slope trend analysis. Graphs and summary tables of the Mann-Kendall / <br /> Sen's Slope analyses for groundwater monitoring wells are presented in Appendix E. <br /> Chloride at MW-10A, potassium at MW-9B, and sulfate at MW-913 exhibited significant <br /> increasing statistical trends. Of these constituents, only potassium at MW-913 exceeded its <br /> concentration limit. Mann-Kendall / Sen's Slope analysis identified significant decreasing <br /> statistical trends in the following constituents: bicarbonate alkalinity at MW-8A, calcium at MW- <br /> 6A, chloride at MW-7A, magnesium at MW-6A and MW-8A, nitrate at MW-8A and MW-10A, <br /> field pH at MW-6A and MW-9B, field specific conductance at MW-7A, TDS at MW-7A and <br /> MW-8A, and field turbidity at MW-7A, MW-9A, and MW-10A. Given that field pH exhibits a <br /> significant decreasing statistical trend at upgradient well MW-6A, the decreasing trend for field <br /> pH at downgradient well MW-913 is likely due to ongoing changes in the natural groundwater <br /> geochemistry at the site. <br />