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Micrometeorological Measurements of Methane and Carbon Dioxide Fluxes at a Municipal Landfill

机译:市政垃圾填埋场甲烷和二氧化碳通量的微气象测量

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Continuous and area-integrating monitoring of methane (CH_4) and carbon dioxide (CO_2) emissions was performed for 6 and 9 months, respectively, at a municipal landfill in Finland with the micrometeorological eddy covariance (EC) method. The mean CH_4 emission from June to December was 0.53 mg m~(-2) s~(-1), while the CO_2 emission between February and December averaged 1.78 mg m~(-2) s~(-1). The CH_4 emissions from the summit area of the landfill, where active waste deposition was going on, were 1.7 times as high as from the slope area with a better surface cover. The variation in emissions over the source area of the measurement was high. Significant seasonal variation, linked to air and soil temperature, was only seen in the CO_2 release rates. Results obtained with the EC method were comparable to those measured with closed static chambers. According to the EC measurements, the gas recovery system decreased CH_4 fluxes by 69-79%. The ratio of the measured CH_4 and CO_2 emissions roughly indicated the route of the landfill gas emission, resembling the ratio of the gases measured in the gas wells (1.24) when the emission originated from the area with no oxidizing cover layer and being smaller when CH_4 oxidation had taken place.
机译:使用微气象涡度协方差(EC)方法在芬兰的一个城市垃圾填埋场分别进行了6个月和9个月的甲烷(CH_4)和二氧化碳(CO_2)排放量的连续和区域综合监测。 6月至12月的平均CH_4排放为0.53 mg m〜(-2)s〜(-1),而2月至12月的CO_2排放平均为1.78 mg m〜(-2)s〜(-1)。垃圾填埋场的顶峰区域(正在进行积极的废物沉积)的CH_4排放量是具有良好表面覆盖的斜坡区域的1.7倍。整个测量源区域的发射变化很大。与空气和土壤温度有关的重大季节性变化仅在CO_2释放速率中可见。用EC方法获得的结果与用封闭静态腔室测量的结果相当。根据EC的测量,气体回收系统将CH_4通量降低了69-79%。测得的CH_4与CO_2的排放比例大致表明了填埋气体的排放路线,类似于排放源来自无氧化覆盖层区域时在气井中测得的气体的比例(1.24),而当CH_4时则较小发生了氧化。

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