首页> 外文期刊>Environmental Science & Technology >Stable Isotope Pulse-Chasing and Compound Specific Stable Carbon Isotope Analysis of Phospholipid Fatty Acids To Assess Methane Oxidizing Bacterial Populations in Landfill Cover Soils
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Stable Isotope Pulse-Chasing and Compound Specific Stable Carbon Isotope Analysis of Phospholipid Fatty Acids To Assess Methane Oxidizing Bacterial Populations in Landfill Cover Soils

机译:磷脂脂肪酸的稳定同位素脉冲追踪和化合物特定的稳定碳同位素分析,以评估垃圾掩埋土壤中甲烷氧化细菌的数量

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The oxidation of methane by bacteria residing in soils constitutes an important terrestrial methane sink. These bacteria are particularly abundant in the covering soils of landfill caps due to the supply of high concentrations of methane from the landfill below. Only about 0.1% of soil bacteria are amenable to available methods of culturing, resulting in the need for a method of in situ analysis. A combination of phospholipid fatty acid (PLFA) analysis and stable isotopic labeling has been employed in this investigation as a means of cultivation-independent bacterial analysis. Soil samples taken from the profiles of two landfill caps, one of clay and one of sand, were incubated with 13{sup left}C-labeled methane. PLFAs were analyzed by gas chromatography/combustion/isotope ratio mass spectrometry (GC/C/IRMS) in order to determine their 13{sup left}C content, from which the PLFA distribution of the methane-oxidizing bacteria was calculated. Neither landfill cap supported communities of bacteria capable of oxidizing ambient levels of methane but only those elevated levels that are usually attributable to landfills. The clay-capped landfill profile exhibited a change in the methane-oxidizing bacterial community with depth, whereas the sand-capped landfill site displayed a mixture of both type I and II methanotrophs throughout the profile. Two additional samples, taken from sites where methane production was evident, were particularly dominated by type II methanotrophic bacteria.
机译:残留在土壤中的细菌对甲烷的氧化构成了重要的陆地甲烷汇。由于从下面的垃圾填埋场供应高浓度的甲烷,这些细菌在垃圾填埋场盖的覆盖土壤中特别丰富。仅约0.1%的土壤细菌适合于可用的培养方法,导致需要原位分析方法。磷脂脂肪酸(PLFA)分析和稳定的同位素标记相结合已在这项研究中用作不依赖培养的细菌分析的手段。将取自两个垃圾填埋场盖(粘土之一和沙子之一)的剖面的土壤样品与13 C标记的甲烷一起孵育。通过气相色谱/燃烧/同位素比质谱法(GC / C / IRMS)分析PLFA,以确定它们的13C含量,由此计算出甲烷氧化细菌的PLFA分布。这两个垃圾填埋场上限都不能支持能够氧化甲烷水平的细菌群落,而只能支持通常归因于垃圾填埋场的那些升高的水平。粘土覆盖的垃圾填埋场剖面显示甲烷氧化细菌群落随深度的变化,而沙子覆盖的垃圾填埋场在整个剖面内显示出I型和II型甲烷营养菌的混合物。另外两个样品是从明显产生甲烷的地点采集的,尤其是II型甲烷营养细菌。

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