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THE CO-OXIDATION OF METHANE AND DICHLOROMETHANE IN LANDFILL BIO-COVER

机译:垃圾填埋生物覆盖物中甲烷和二氯甲烷的共氧化

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Municipal solid waste landfills are a major source for anthropogenic methane (CH4) emissions.A reduction in these CH4 emissions can be done by utilizing methanotrophic bacteria present in landfillcover. The affect of non-methane organic compounds (NMOCs) on the rate of CH4 oxidation has notbeen effectively studied. This paper addresses the presence of dichloromethane (DCM) on the oxidativecapacity of CH4 by these methanotrophic bacteria. This was done by using laboratory scale batch studieswith stabilized compost and gas chromatography to determine the co-oxidation rates of CH4 and DCM forthree atmospheric temperatures (5°C, 22°C and 35°C) and for three DCM concentrations. The resultsshowed that a DCM headspace concentration of only 3 ppmv resulted in a significant decrease in the CH4oxidation rate and that DCM had been completely oxidized. At a concentration of 21 ppmv there was noCH4 or DCM oxidation. Temperature played a major role, with very little oxidation occurring attemperatures of 5°C compared to those at 22°C and 35°C. Finally no oxidation of DCM occurred in theabsence of CH4 from the batch reactor. Major conclusions from the study are that it will be critical toreduce the NMOC concentrations in landfill gas if CH4 is to be oxidized by a bio-cover. One way toachieve this would be to increase restrictions on the type of waste that can be dumped in landfills, thusreducing DCM and other NMOC concentrations.
机译:市政固体垃圾填埋场是人为甲烷(CH4)排放的主要来源。 可以通过利用垃圾填埋场中存在的甲烷营养细菌来减少这些CH4的排放 覆盖。非甲烷有机化合物(NMOCs)对CH4氧化速率的影响尚未发现 经过有效研究。本文解决了在氧化剂中存在二氯甲烷(DCM)的问题。 这些甲烷营养细菌具有CH4的能力。这是通过实验室规模的批处理研究完成的 用稳定的堆肥和气相色谱法测定CH4和DCM的共氧化速率 三个大气温度(5°C,22°C和35°C)和三个DCM浓度。结果 表明DCM顶空浓度仅为3 ppmv导致CH4显着降低 氧化速率,表明DCM已被完全氧化。在21 ppmv的浓度下,没有 CH4或DCM氧化。温度起主要作用,在此温度下很少发生氧化 5°C的温度与22°C和35°C的温度相比。最后,DCM中没有发生DCM的氧化。 分批反应器中不存在CH4。该研究的主要结论是,这对于 如果CH4被生物覆盖物氧化,则可以降低垃圾填埋气中的NMOC浓度。一种方法 实现这一目标将是增加对可倾倒在垃圾填埋场中的废物类型的限制,因此 降低DCM和其他NMOC浓度。

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