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探讨土壤 pH 值对 N(2)O 和 N(2)排放以及反硝化菌群落大小和活性的影响。

Insights into the effect of soil pH on N(2)O and N(2) emissions and denitrifier community size and activity.

机构信息

Biology Centre of the ASCR, v. v. i., Institute of Soil Biology, and University of South Bohemia, Faculty of Science, Na Sádkách 7, 370 05 Ceské Budejovice, Czech Republic.

出版信息

Appl Environ Microbiol. 2010 Mar;76(6):1870-8. doi: 10.1128/AEM.02484-09. Epub 2010 Jan 29.

Abstract

The objective of this study was to investigate how changes in soil pH affect the N(2)O and N(2) 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 H(2)SO(4) solution (acidic soil), or water (natural pH soil) over 10 months. At the site, we determined field N(2)O and N(2) emissions using the (15)N 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 N(2)O/(N(2)O + N(2)) ratio increased with decreasing pH due to changes in the total denitrification activity, while no changes in N(2)O production were observed. Denitrification activity and N(2)O 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 N(2)O/(N(2)O + N(2)) 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.

摘要

本研究旨在探讨土壤 pH 值的变化如何影响 N(2)O 和 N(2)排放、反硝化活性以及反硝化群落的大小。我们建立了一个野外实验,该实验位于一个草原地区,在 10 个月的时间里,反复用 KOH 溶液(碱性土壤)、H(2)SO(4)溶液(酸性土壤)或水(自然 pH 值土壤)处理了三个处理组。在现场,我们使用 (15)N 气体通量法测定了 N(2)O 和 N(2)排放,并采集了土壤样品,通过定量 PCR 测定潜在反硝化活性和反硝化群落的大小,以测定 narG、napA、nirS、nirK 和 nosZ 反硝化基因。总的来说,我们的结果表明,土壤 pH 值对反硝化终产物的性质具有重要影响。因此,我们发现由于总反硝化活性的变化,N(2)O/(N(2)O+N(2)) 比值随着 pH 值的降低而增加,而 N(2)O 的产生没有变化。在实验室条件下测量的反硝化活性和 N(2)O 排放与原位 N 通量相关,因此反映了野外处理的差异。反硝化群落的大小与原位 N 通量脱耦,但潜在的反硝化与 NirS 反硝化剂的计数相关。nirS、napA 和 narG 基因拷贝数与 N(2)O/(N(2)O+N(2)) 比值之间存在显著关系,这很难解释。然而,这突显了需要进一步研究将反硝化生态学分析与反硝化终产物的定量相结合,以全面了解反硝化对 N 通量的调控。

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