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Structure of greenhouse gas-consuming microbial communities in surface soils of a nitrogen-removing experimental drainfield

机译:氮气去除实验排水界表面土壤中温室气体消耗微生物群落的结构

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Septic systems represent a source of greenhouse gases generated by microbial processes as wastewater constituents are degraded. Both aerobic and anerobic wastewater transformation processes can generate nitrous oxide and methane, both of which are potent greenhouse gases (GHGs). To understand how microbial communities in the surface soils above shallow drainfields contribute to methane and nitrous oxide consumption, we measured greenhouse gas surface flux and below-ground concentrations and compared them to the microbial communities present using functional genes pmoA and nosZ. These genes encode portions of particulate methane monooxygenase and nitrous oxide reductase, respectively, serving as a potential sink for the respective greenhouse gases. We assessed the surface soils above three drainfields served by a single household: an experimental layered passive N-reducing drainfield, a control conventional drainfield, and a reserve drainfield not in use but otherwise identical to the control. We found that neither GHG flux, below-ground concentration or soil properties varied among drainfield types, nor did methane oxidizing and nitrous oxide reducing communities vary by drainfield type. We found differences in pmoA and nosZ communities based on depth from the soil surface, and differences in nosZ communities based on whether the sample came from the rhizosphere or surrounding bulk soils. Type I methanotrophs (Gammaproteobacteria) were more abundant in the upper and middle portions of the soil above the drainfield. In general, we found no relationship in community composition for either gene based on GHG flux or below-ground concentration or soil properties (bulk density, organic matter, above-ground biomass). This is the first study to assess these communities in the surface soils above an experimental working drainfield, and more research is needed to understand the dynamics of greenhouse gas production and consumption in these systems.
机译:化粪池系统代表通过微生物过程产生的温室气体来源,因为废水成分降解。有氧和无氧废水转化过程既可以产生氧化二氮和甲烷,两者都是有效的温室气体(GHG)。为了了解浅排水域上表面土壤中的微生物社区有助于甲烷和氧化亚氮消耗,我们测量温室气体表面通量和低于地面浓度,并将它们与使用功能基因PMOA和NOSZ的微生物社区进行了比较。这些基因分别编码颗粒状甲烷单氧基酶和氧化氮还原酶的部分,用作各个温室气体的潜在水槽。我们评估了单个家庭服务的三个流水线上方的表面土壤:实验层叠的被动N-减少流水线,控制传统排水场和不使用的储备排水扇,而是与控制相同。我们发现,在排水平类型中,既不是地下浓度或土壤特性,也不多于甲烷氧化和氧化二氮氧化物减少社区因排水田型而变化。我们发现了基于从土壤表面的深度的PMOA和NoSz社区的差异,以及基于样品是否来自根际或周围散装土壤的NoSz社区的差异。 I型甲蛋白(γ曲线杆菌)在排水界上方的土壤的上部和中间部分更加丰富。通常,我们发现基于GHG助熔剂或地下浓度或土壤性质(堆积密度,有机物,地上生物质)的基因的群落组合中没有任何关系。这是第一次评估这些在实验工作流场的表面土壤中的这些社区的研究,需要更多的研究来了解这些系统中温室气体生产和消费的动态。

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