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0 2.5.3 Leachate and Groundwater Mixing Analyses <br />Since many inorganic constituents may be unaffected by biodegradation processes, <br />calculations were completed to evaluate the magnitude of impacts that could be expected <br />if undiluted leachate were to migrate vertically and mix with groundwater. HDPE liner <br />defects were assumed to be consistent with the default criteria specified by the USEPA's <br />HELP3 computer model, and one foot of leachate head was assumed to be applied on the <br />liner. Attenuation processes in the clay liner and vadose zone were ignored, and <br />leachate/groundwater mixing was assumed to occur at the same rate as saturated flow <br />through the liner. Groundwater flow parameters were assumed to be consistent with <br />those identified by Herst & Associates / Andrews Environmental Engineering <br />([HA/AEE], 2001). <br />As noted by RWQCB staff, the mixing analyses included a calculation error (the number <br />of defects per acre were unintentionally omitted), but, as detailed here in Section 3.1, the <br />conclusion that the impacts on groundwater quality would be statistically insignificant <br />remains true. <br />3.0 ADDITIONAL ANALYSES <br />Recognizing RWQCB staff's recent concerns, additional analyses were completed that <br />considered potential groundwater impacts associated with unattenuated leachate <br />concentrations. As described below, new leachate/groundwater mixing analyses were <br />completed using the historical average leachate concentrations measured at the Forward <br />Landfill. Analyses were then completed that consider the more likely condition of <br />unsaturated leachate flow through the vadose zone beneath the landfill. <br />As requested, additional leachate / groundwater mixing analyses were completed to estimate <br />the potential impacts to groundwater associated with undiluted leachate constituents leaking <br />directly to groundwater from the proposed single composite liner at the Forward Landfill. <br />These calculations conservatively assumed that no leachate would be entrained in the clay <br />liner or vadose zone and that all leaked leachate mixes directly in groundwater. As <br />indicated below, leachate leakage and migration to groundwater is calculated to result in a <br />statistically insignificant increase in constituent concentrations in groundwater. In a real <br />sense, the calculated changes in groundwater chemistry would be undetectable. <br />3.1.1 Liner Leakage Volume <br />The USEPA's HELP3 computer model assumes that a typical high density polyethylene <br />(HDPE) liner defect is approximately 1 square centimeter, and that approximately 4 defects <br />occur over a given acre of liner. Assuming that the hydraulic conductivity of the 2 -foot <br />thick clay section of the liner is equal to 1 E-07 cm/sec, the volume of leachate that will <br />ultimately leak through an acre of lined area in saturated flow is: <br />CA2002-002\Revised Appx A - Leakageldoc\09/19/02 <br />Geologic Associates <br />