Kinetics of Methane Oxidation in a Landfill Cover Soil: Temporal Variations, a Whole-Landfill Oxidation Experiment, and Modeling of Net CH4 Emissions
文摘
Rates and controlling variables for methanotrophicoxidationof methane at a northeastern Illinois landfill with pumpedgas recovery were examined in a field study from Juneto December 1995. Cover materials consisted of a simpleclay-topsoil sequence without geomembranes. Through useof a static enclosure (closed chamber) technique supplemented by soil gas concentration profiles and fieldincubations, the study concentrated on proximal (near gasrecovery well) and distal (between well) sites establishedin 1994. A personal computer-based three-dimensionalfinite-difference model was also developed which includes bothgaseous mass transfer (CH4, CO2,O2) and microbial CH4oxidation. Mass transfer is modeled through amodifiedchemical potential gradient within a cubic network ofnodes; a strict mass balance for each gas is maintainedthrough successive timesteps. Methane-oxidizingconditionswith no net CH4 emissions to the atmospherepersistedinto full winter conditions in December, 1995. Rates ofCH4oxidation (negative fluxes) from closed chamberexperimentswere similar to rates obtained from in vitrofieldincubations with initial headspace CH4 at ambientatmosphericconcentrations (1-2 ppmv). Composited data from thechamber tests and field incubations demonstrated thatoxidation rates were able to rapidly increase over 4 orders ofmagnitude as a direct kinetic response to broad ranges ofinitial CH4 concentrations (from ambient to 8.4 vol %).Themaximum observed rate was 48 g m-2day-1. Kinetic plotsindicated at least two major trophic groups of methanotrophs: a CH4-limited group (low CH4; ambientO2) and an O2-limited group (high CH4; subambient O2).The whole-landfill CH4 oxidation experiment was conducted over a2day period when the pumped gas recovery system wasshut down and restarted; oxidation rates increased andthendecreased more than 2 orders of magnitude in responseto changing CH4 concentrations. Although themodelingrelies on theoretical considerations for both gaseous fluxanddevelopment of microbial populations, the LandfillCH4Emissions Model requires a limited number of inputvariablesand provides a practical tool for order-of-magnitudeprediction of net CH4 fluxes at fieldsites.