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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 />