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Methane oxidation in homogenous soil covers of landfills: a finite - element analysis of the influence of gas diffusion coefficient

机译:垃圾填埋场均质土壤甲烷氧化:气体扩散系数影响的有限元分析

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摘要

Methane produced in municipal landfills covered with a soil layer diffuses to the atmosphere. Counterdiffusion of oxygen down the soil creates an oxic zone where biochemical oxidation of methane by methanotrophic microorganisms can take place. Oxidation is possible only in that part of the oxic zone where both the substrates, i.e., methane ond oxygen are present simultanously. Biochemical oxidation of methane is governed by Michaelis-Menten kinetics. The solution of the equation system comprising the Michaelis-Menten equation generalized for the two substrates, i.e., methane and oxygen and the Fick's diffusion equation was found numerically with the use of the finite element method. Results of the calculations were presented for the steady - stateconditions in a homogenous soil layer with constant (in space and time) gas diffusion coefficient and kinetic parameters, i.e., the Michaelis constant (K_M) and the maximum oxidation rate. The effect of the gas diffusion coefficient on the distributionprofiles of methane, oxygen and actual methanotrophic activity, as well as on the depth of oxygenation zone and on the methane oxidation capacity in the soil layer is discussed.
机译:在覆盖有土壤层的市政垃圾填埋场中产生的甲烷扩散到大气中。氧气在土壤中的反向扩散会形成一个含氧区域,甲烷在其中会发生甲烷氧化营养微生物的生化氧化。氧化仅在两个底物(即甲烷和氧气)同时存在的氧化区部分才可能进行。甲烷的生化氧化取决于Michaelis-Menten动力学。使用有限元方法在数值上找到了方程系统的解,该方程组包括针对两种衬底即甲烷和氧气而推广的迈克尔斯-门腾方程,以及菲克扩散方程。给出了均质土壤层中稳态条件的计算结果,该均质土壤层具有恒定(时空)气体扩散系数和动力学参数,即米氏常数(K_M)和最大氧化速率。讨论了气体扩散系数对甲烷,氧气和实际甲烷营养活动的分布曲线,氧化层深度和土壤层甲烷氧化能力的影响。

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