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subsurface air supply were combusting (most or all of these temperature <br /> probes are believed to have been destroyed during landfill closure). They <br /> recommended engineering considerations for landfill closure to control <br /> landfill fires, including a cover system with an impermeable <br /> geomembrane and a gas collection system. Parametrix (1992a) recognized <br /> that permeable lava tubes could supply air for subsurface combustion <br /> even after closure with the recommended engineering controls,and <br /> recommended that geophysical surveys be performed to identify lava <br /> tubes and such tubes be grout-sealed to prevent air flow. <br /> A Landfill Closure/Post Closure Plan was approved in 1993. ERM has <br /> not yet obtained a copy of this plan;however,we did review the response <br /> to comments on the plan by Parametrix (1993a). The Hawaii Department <br /> of Health (HDOH) expressed concerns on the heat resistance of the <br /> geomembrane liner system. ERM understands based on discussions with <br /> the County of Hawaii that this liner has in fact failed in certain locations <br /> due to excessive heat. Parametrix (1993b) stated that during closure, <br /> "sealing these [landfill] side slopes off, air will be eliminated from the <br /> refuse, thereby shutting off the oxygen supply,and'smothering' the <br /> subsurface fires...If temperature monitoring indicates that there are areas <br /> which are not cooling off as rapidly as others, a barrier trench,filled with <br /> low-permeability grout will be installed in native soil adjacent to the <br /> elevated temperatures, to effectively block lava tubes in the area." <br /> During closure of the landfill in 1992 and 1993,a gas-collection system <br /> consisting of perforated HDPE piping within 3-foot-square, gravel-filled <br /> trenches at 150-foot centers was installed and operated. Due to low <br /> methane concentrations in the collected gas stream that were not suitable <br /> for combustion treatment, the system ceased operations in February 1993 <br /> (Parametrix 1993b). A final cover system with 30-mil PVC geomembrane <br /> liner and 2 feet of cover soil was installed in late 1993. Temperature and <br /> gas monitoring probes were installed during Phase II cover installation, <br /> and routinely monitored after closure (Parametrix,1995a). Temperatures <br /> above 120°F were observed in several temperature probes;however, <br /> landfill gases were not identified at perimeter gas monitoring locations. <br /> By September 1995, during Phase 3 Closure Work, temperatures in <br /> vertical gas extraction wells reached 182°F, exceeding material design <br /> capabilities (Parametrix,1995a). Several depressions or sinkholes were <br /> identified,with several feet of subsidence and smoke odors. Parametrix <br /> (1997a) summarized six quarterly monitoring events from 1995 through <br /> February 1997. Although they concluded that the landfill was fairly <br /> stable, they indicated that"Although temperatures are fairly stable and <br /> not alarmingly high,they do not reflect what may be happening deep in <br /> the landfill. With the collection wells and trenches closed,there is no flow <br /> ERM 2 KAILUA-KONA LANDFILL/0061204-3/14/2008 <br />