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Insights into the Effect of Soil pH on N2O and N2 Emissions and Denitrifier Community Size and Activity

机译:洞察土壤pH值对N2O和N2排放以及反硝化菌群落大小和活性的影响

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摘要

The objective of this study was to investigate how changes in soil pH affect the N2O and N2 emissions, denitrification activity, and size of a denitrifier community. We established a field experiment, situated in a grassland area, which consisted of three treatments which were repeatedly amended with a KOH solution (alkaline soil), an H2SO4 solution (acidic soil), or water (natural pH soil) over 10 months. At the site, we determined field N2O and N2 emissions using the 15N gas flux method and collected soil samples for the measurement of potential denitrification activity and quantification of the size of the denitrifying community by quantitative PCR of the narG, napA, nirS, nirK, and nosZ denitrification genes. Overall, our results indicate that soil pH is of importance in determining the nature of denitrification end products. Thus, we found that the N2O/(N2O + N2) ratio increased with decreasing pH due to changes in the total denitrification activity, while no changes in N2O production were observed. Denitrification activity and N2O emissions measured under laboratory conditions were correlated with N fluxes in situ and therefore reflected treatment differences in the field. The size of the denitrifying community was uncoupled from in situ N fluxes, but potential denitrification was correlated with the count of NirS denitrifiers. Significant relationships were observed between nirS, napA, and narG gene copy numbers and the N2O/(N2O + N2) ratio, which are difficult to explain. However, this highlights the need for further studies combining analysis of denitrifier ecology and quantification of denitrification end products for a comprehensive understanding of the regulation of N fluxes by denitrification.
机译:这项研究的目的是调查土壤pH的变化如何影响N2O和N2排放,反硝化活性和反硝化菌群落的规模。我们在草原地区建立了一个野外试验,该试验由三种处理组成,这些处理在10个月内反复用KOH溶液(碱性土壤),H2SO4溶液(酸性土壤)或水(天然pH值土壤)进行了修改。在现场,我们使用 15 N气体通量法确定了田间N2O和N2的排放量,并收集了土壤样品,用于测量潜在的反硝化活性并通过定量PCR定量反硝化群落的规模。 narG,napA,nirS,nirK和nosZ反硝化基因。总体而言,我们的结果表明土壤pH值对于确定反硝化最终产品的性质至关重要。因此,我们发现,由于总反硝化活性的变化,N2O /(N2O + N2)的比率随着pH的降低而增加,而未观察到N2O产生的变化。在实验室条件下测得的反硝化活性和N2O排放与原位N通量相关,因此反映了现场的处理差异。反硝化菌群的大小与原位氮通量无关,但潜在的反硝化作用与NirS反硝化剂的数量相关。观察到nirS,napA和narG基因拷贝数与N2O /(N2O + N2)之比之间存在显着关系,这很难解释。但是,这突出了需要进行进一步研究,结合反硝化剂生态学分析和反硝化最终产物的定量分析,以全面了解反硝化作用对氮通量的调节作用。

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