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which indicates that groundwater generally flows to the north-northeast towards the <br />Austin Unit, at an average hydraulic gradient of approximately 0.003 ft/ft. Locally, a <br />south-southwest gradient was also noted in the northwest corner of the Forward Unit. <br />To calculate the approximate linear groundwater flow velocity for the site, conservative <br />assumptions were used, including a hydraulic conductivity of 875 gallons per day per <br />square foot (0.04 cm/sec) and an estimated effective porosity of 35 percent (CH2M Hill <br />2000). An estimated groundwater flow velocity was calculated using Darcy's Law: <br />' !fir = [( 0.04 CMl * 0.003 l * 2835 sec fta 0.972 Jt ` tOcxt, <br />J11C sec 0.35 ern - dam, <br />where: V= Groundwater flow velocity. <br />K = Hydraulic conductivity of the water -bearing unit (0.04 cm/sec). <br />i = Hydraulic gradient: i ;t5 0.003 for the site during the third quarter 2011. <br />n,= Effective porosity (n, = 0.35); an estimated value. <br />The groundwater flow rate is calculated to be 0.972 feet/day (355 feet/year). <br />2.1.4 Detection Monitoring Program <br />Field and laboratory results for the groundwater monitoring wells for the third quarter <br />2011 are summarized in Table 2-2. The organic results for the Forward Unit indicate that <br />1,1-dichloroethane (1,1 -DCA), cis-l,2-dichloroethene (cis-1,2-DCE), <br />dichlorodifluoromethane (DCDFM) and trichlorofluoromethane (TCFM) were measured <br />at estimated trace concentrations (between the method detection limit [MDL] and the <br />PQL) in the sample collected from well MW -14. In addition, diisopropyl ether (DIPS) <br />was measured above the PQL in the sample collected from well MW -2A; and <br />tetrachloroethene (PCE) and trichloroethene (TCE) was measured above the PQL in the <br />sample collected from well MW -14. <br />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 <br />in 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. The <br />particular VOCs detected in samples during the current monitoring period appear to <br />support this conclusion. Forward has continued to minimize gas related impacts to <br />groundwater by limiting interim fill areas that promote ponding of water. Furthermore, <br />in accordance with CCR Title 27, Section 20937, Forward continues to install additional <br />landfill gas extraction wells, as needed, and make adjustments to the LFG wells. <br />CA2011-0050\FA_3Q I I.d"x 5 Geo -Logic Associates <br />