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Water Quality Monitoring Report <br /> Forward Landfill <br /> gradient of 0.002 ft/ft, while groundwater beneath the northern, western, and central <br /> portions of the Forward Unit flows to the southeast at a hydraulic gradient of 0.002 ft/ft. <br /> To calculate the approximate linear groundwater flow velocity for the Forward Unit, <br /> conservative assumptions were used, including a hydraulic conductivity of 875 gallons <br /> per day per square foot (0.04 cm/sec) and an estimated effective porosity of 35 percent <br /> (CH2M Hill, 2000). An estimated groundwater flow velocity was calculated using Darcy's <br /> Law: <br /> Ki cm 0.002 sec— ft <br /> V =—_ [(0.04—)* ]*2835 = 0.648 ft/day <br /> ne sec 0.35 cm —day <br /> where:V=Groundwater flow velocity. <br /> K= Hydraulic conductivity of the water-bearing unit (0.04 cm/sec). <br /> i= Hydraulic gradient: i=0.002 at the site during the third quarter 2014. <br /> ne= Effective porosity(ne=0.35); an estimated value. <br /> The maximum groundwater flow rate is calculated to be 0.648 feet per day (237 <br /> feet/year)to the northwest and southeast. <br /> 2.1.4 Detection Monitoring Program <br /> Field and laboratory results for the Forward Unit groundwater monitoring wells for the <br /> third quarter 2014 monitoring period are summarized in Table 2-2. <br /> Non-Statistical Data Analysis <br /> The California Non-Statistical Data Analysis Method (CNSDAM) was performed for VOCs <br /> detected less than 10 percent of the time in background samples. Under the CNSDAM, a <br /> measurably significant indication of release occurs in a given sample when: two or more <br /> VOCs exceed their respective Method Detection Limits (MDLs); or one or more VOCs <br /> equals or exceeds its respective practical quantitation limit (PQL). During the third <br /> quarter 2014 monitoring period, non-statistical indications of a release were identified <br /> at well MW-2A as a result of a quantifiable concentration of diisopropyl ether (DIPE) <br /> (0.92 µg/L), and at well MW-17 as a result of trace-level concentrations of chloroform <br /> (0.22j µg/L) and trichlorofluoromethane (TCFM) (0.19j µg/L). In a letter dated October <br /> 1, 2014, the RWQCB was notified of these exceedances and retesting is scheduled for <br /> October 2014. The results of the verification sampling will be reported under separate <br /> cover. On behalf of Forward Inc., GLA prepared a letter report dated February 14, 2001 <br /> (RWQCB Case No. 2209),to assess the source and potential impacts of low-level VOCs in <br /> groundwater adjacent to the Forward Landfill. The letter report concluded that the <br /> sporadic detection of low-level VOCs in groundwater (and lysimeter samples) at the <br /> Forward Unit are most likely due to landfill gas from unlined unit WMU-B. Forward has <br /> M:\2014.0012\FA_3Q14.docx 6 <br /> 10/31/2014,Rev.0 <br />