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Mr. Robert McClellon <br />March 7, 2011 <br />Page 4 <br />areas below the historical groundwater table, there will likely also be some kind of "aquitard" <br />layer (perhaps a 40 -mil HDPE membrane) placed between the underdrain and original <br />ground to limit the amount of groundwater collected by the underdrain system (Geologic <br />Associates, 2008). It should be noted that the underdrain in the expansion area is designed in <br />the event that the groundwater table rises to historic levels however, the current groundwater <br />level is far below historic high water table levels and it is unlikely that the historic high <br />groundwater levels will reoccur in the future. <br />Materials will be installed by qualified installation contractors, will be inspected by <br />construction quality assurance monitors, and will be certified by a California -registered <br />engineer. The installation of the composite liner system will create a barrier to LFG <br />migration. In addition, within five (5) years of placing waste in the new cell, the existing <br />LFG collection and control system (GCCS) will be expanded into the new cell to capture <br />LFG generated in the landfill expansion and prevent LFG pressure fronts that could lead to <br />migration. The composite liner system in conjunction with a properly operated and <br />maintained GCCS will provide control of LFG and limit the potential risk of LFG migration <br />from the new cell. <br />Forward Expansion Cross Section <br />The cross section shown in Figure 1 represents the proposed landfill cell expansion, proposed <br />liner system, typical GCCS components, adjacent geology, and a typical proposed LFG <br />monitoring probe. Figure 1 illustrates that the geology in which the LFG monitoring probes <br />are to be installed consists of inter -bedded sandy silt, clayey silt, silt, and clay. If LFG were <br />to migrate from the lined expansion, it would follow the preferential pathways of permeable <br />soils (such as sand, sandy silt, and silt) to the probes, regardless of the set -back distance from <br />the landfill. The migration of LFG in site soils has been confirmed by existing probes on <br />site. <br />In addition, the cross section depicts the construction details of the proposed landfill cell <br />including the geomembrane liner system and the GCCS components. The GCCS is designed <br />to impart a negative pressure (vacuum) to the LCRS and to extraction wells that are to be <br />constructed within the waste mass. Each extraction well is expected to have a negative <br />pressure radius of influence (ROI) up to approximately 150 feet (depending upon the applied <br />vacuum and waste characteristics). This design is intended to create a negative pressure zone <br />of influence through the waste mass and LCRS drainage layer, drawing LFG toward the <br />extraction wells and LCRS system. The spacing of LFG collection wells and operation thereof <br />will be designed to extend the ROI to the edge of waste. <br />Since the permeabilities of the waste mass and LCRS drainage layer are much greater than that <br />of the surrounding liner system and native soils, the preferential pathways for LFG within the <br />cell is through the LCRS drainage layer and the waste mass toward the GCCS. By imparting <br />this negative pressure zone with the waste mass, LFG will be contained within the landfill <br />offsetting any tendency to migrate from the landfill to the probes. The key component in the <br />