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2.RESULTS FOR SECOND SEMIANNUAL PERIOD 2014 <br /> Groundwater Analytical Methods <br /> Groundwater samples collected from the sampled monitoring wells were submitted to <br /> Alpha Analytical,Inc., a California-certified analytical laboratory located in Sparks,Nevada. <br /> Copies of the laboratory reports from Alpha Analytical are provided in Appendix B. <br /> Groundwater and quality assurance/quality control(QA/QC) samples were analyzed for <br /> the following: <br /> • Total petroleum hydrocarbons as gasoline (TPHg) and as diesel (TPHd)using United <br /> ' States Environmental Protection Agency (EPA) Method 8015 modified <br /> • Benzene,toluene, ethylbenzene,and total xylenes (BTEX) using EPA Method 8260B <br /> ' The following QA/QC samples were collected: <br /> • Duplicate sample from well N-7 (labeled DUP-1) <br /> ' • One equipment blank sample (labeled EB-1) <br /> • One trip blank sample for the cooler of samples (labeled TB-1) <br /> Sample analyses were conducted within a standard 10-day laboratory turnaround time. <br /> 2.1.2 Results <br /> Groundwater Elevation and Flow <br /> Groundwater level data collected on September 10, 2014, are presented in Table 2,and <br /> elevation contours for these data are shown in Figure 3.These data are included in the <br /> tabulation of the eight most recent historical monitoring events in Appendix C. <br /> Hydrographs of the historical data are provided in Appendix D. <br /> ' Groundwater Elevations <br /> The groundwater elevations and depths to groundwater for the September 10, 2014, data <br /> were as follows. <br /> • Shallow-interval groundwater monitoring wells are constructed with total depths <br /> between 14 and 23.5 feet bgs. Calculated elevations for the shallow-interval <br /> groundwater monitoring wells ranged from 3.04 feet above mean sea level(msl) at <br /> rwell M-2,located in the north portion of the Site near Trapper Slough,to-12.06 feet msl <br /> in well N-8,located in the southeastern portion of the Site. The water level elevations for <br /> M-10 and N-8 were anomalously low compared to prior year results. The low water <br /> level elevation not including these two wells was-10.66 feet msl at M-8. The depth to <br /> groundwater ranged from 2.46 feet bgs at well M-2 to 16.54 feet bgs at well 0-1. <br /> • The deeper-interval groundwater monitoring well (N-24) is constructed at a total depth <br /> of 42 feet bgs. The calculated groundwater elevation for well N-24 was-8.64 feet msl. <br /> The depth to groundwater was at 8.64 feet bgs in the well, above the screened interval. <br /> These data are consistent with historical data,as shown in the hydrographs in Appendix D <br /> (except for the two anomalous wells,M-10 and N-8). <br /> Groundwater Flow <br /> Groundwater flow depends on the physical characteristics of the subsurface materials and <br /> the groundwater gradients. A detailed analysis of groundwater flow for the fourth quarter <br /> ES101214202053SCO 2-3 <br />