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L3.ANNUAL REPORT FOR 2011 <br /> Lmonitoring for this well began in 2005. The decreases in wells M-10 and 0-1 have occurred <br /> to such an extent that well 0-1 is almost no longer in the hydrocarbon plume and well M-10 <br /> It. is now almost outside the plume. <br /> Before the start of the bioremediation pilot test,no long-term BTEX and TPH concentration <br /> trends for extraction well N-17 and nearby monitoring well N-16 were apparent.This was <br /> Lpotentially due to extraction at N-17 pulling hydrocarbons downgradient from the areas of <br /> higher contamination near the source area,which sustained the hydrocarbon <br /> concentrations.Since the start of the bioremediation pilot test in February 2004,the <br /> L concentrations in wells N-16 and N-17 have shown similar behavior. <br /> Overall,the concentrations of BTEX and TPH constituents began to increase after extraction <br /> L stopped from well N-17 in February 2004. This likely occurred because clean, downgradient <br /> groundwater was no longer being pulled into the capture zone (and into wells N-16 and <br /> N-17) to dilute the BTEX and TPH constituents that were being pulled downgradient from <br /> Lthe source area. Since the initial concentration increases after the extraction was shut down, <br /> a new equilibrium appears to have been established where the naturally occurring processes <br /> are resulting in decreasing concentrations for the BTEX and TPH constituents. <br /> L <br /> 3.2 Effectiveness of the Current Remediation System <br /> LThe current remediation system consists of MNA and the phytoremediation system as <br /> summarized in Section 1.The combination of these two strategies is effective,resulting in a <br /> sitewide decline in TPH and BTEX concentrations in groundwater and a stable-to-shrinking <br /> extent of these constituents in groundwater.As discussed with the RWQCB during <br /> meetings on July 12,2007,and September 21,2007, and reflected in the current MRP issued <br /> 1 by the RWQCB, the steady reduction in hydrocarbon mass,as well as BTEX and TPH <br /> concentrations, at the Site are the result of fate-and-transport processes occurring naturally <br /> in the subsurface.These naturally occurring processes are documented in the Final Site <br /> L Characterization Report(CH2M HILL,2002) and the 3-Year Evaluation of the Bioremediation <br /> Pilot Study(CH2M HILL,2007a).The steady reduction in hydrocarbon mass is shown in the <br /> time-series concentration charts in Appendix D and Appendix E. <br /> i <br /> 3.3 Identification of Data Gaps and Potential Deficiencies/ <br /> ` Redundancies <br /> No data gaps or deficiencies have been identified.Quarterly groundwater monitoring at the <br /> Site was implemented in March 1992.To date, the groundwater monitoring program has <br /> �.r been performed for approximately 19 years and has provided important time-series <br /> information with respect to groundwater elevations and gradients,NAPH thicknesses, and <br /> chemical concentrations in groundwater and surface water. Seasonal patterns in <br /> L groundwater elevation fluctuations,as well as seasonal and long-term trends in BTEX and <br /> TPH concentrations, have been identified,as documented in the Final Site Characterization <br /> Report(CH2M HILL,2002) and in subsequent routine groundwater monitoring reports. <br /> LRobust data have been collected to demonstrate that the naturally occurring processes are <br /> sufficient to result in a continued declining trend of these hydrocarbon constituents without <br /> ES102411183308SCOILW3521.DOC)Ul 12970003 33 <br />