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2011 Semiannual Groundwater Monitoring and Evaluation Report <br /> Full-Scale In Situ Hexavalent Chromium Reduction Treatment Implementation <br /> Former Marley Cooling Tower Site, Stockton,California January 2012 <br /> 4.2.2.1 Background and Compliance Wells. During the third and fourth quarters of <br /> 2011, Fe concentrations in background and compliance wells ranged from 42J gg/L (MW-325 in <br /> July 2011) to 656 gg/L (MW-201 in July 2011). Fe was detected at concentrations above the <br /> WQO (300 gg/L) and proposed upper background limit concentrations at wells MW-201, MW- <br /> 202, MW-304, and MW-310 during both quarterly sampling events. The Fe concentration also <br /> exceeded the WQO and proposed upper background limit concentration in well MW-7 during <br /> the third quarter of 2011, and the WQO in well MW-7 during the fourth quarter of 2011. Table 6 <br /> presents the proposed upper background concentration limits for background wells in <br /> comparison to historical results and WQOs. <br /> 4.2.2.2 Injection Area Wells. During the third and fourth quarters of 2011, Fe <br /> concentrations in injection area wells ranged from 75J gg/L (MW-320 in July 2011) to <br /> 4,320µg/L (MW-105 in July 2011). Fe was detected at concentrations above the WQO <br /> (300 gg/L) in 28 injection area wells sampled during the third quarter of 2011, and 22 injection <br /> area wells sampled during the fourth quarter. These results are generally consistent with baseline <br /> concentrations or trends evident in the data collected since 2008 (see Graphs 1 through 53). The <br /> presence of ferrous Fe will serve as a continuing source of reduction to potential Cr+6 in these <br /> areas. Based on previous site data, Fe is expected to decrease in concentrations to near <br /> background levels over time. No additional action is recommended at this time regarding the <br /> observed Fe concentrations. <br /> 4.2.3 Manganese <br /> Concentrations of Mn commonly show a temporary increase following application of the <br /> reductant solution. Mn is temporarily mobilized as a result of conversion of ferric hydroxide on <br /> aquifer solids to mobile ferrous Fe, with the resultant reduction of Mn present as a co-precipitate <br /> in the ferric hydroxide to the soluble manganous form. Analytical results for Mn are presented <br /> in Table 5 and on Graphs 1 through 53. <br /> 4.2.3.1 Background and Compliance Wells. During the third and fourth quarters of <br /> 2011, Mn concentrations in background and compliance wells ranged from at or below the <br /> laboratory analytical reporting limit (RL) of 10 gg/L to 70 gg/L (MW-325 in July 2011). <br /> 0) MWH,, <br /> 4-4 <br />