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通过β变形菌氨氧化细菌的同位素分馏分析和 amoA 丰度揭示牛粪堆肥过程中氧化亚氮排放的来源。

Source of nitrous oxide emissions during the cow manure composting process as revealed by isotopomer analysis of and amoA abundance in betaproteobacterial ammonia-oxidizing bacteria.

机构信息

Hokkaido Research Subteam for Waste Recycling System, National Agricultural Research Center for Hokkaido Region, National Agricultural and Food Research Organization, 1 Hitsujigaoka, Sapporo 062-8555, Japan.

出版信息

Appl Environ Microbiol. 2010 Mar;76(5):1555-62. doi: 10.1128/AEM.01394-09. Epub 2010 Jan 4.

DOI:10.1128/AEM.01394-09
PMID:20048060
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC2832385/
Abstract

A molecular analysis of betaproteobacterial ammonia oxidizers and a N(2)O isotopomer analysis were conducted to study the sources of N(2)O emissions during the cow manure composting process. Much NO(2)(-)-N and NO(3)(-)-N and the Nitrosomonas europaea-like amoA gene were detected at the surface, especially at the top of the composting pile, suggesting that these ammonia-oxidizing bacteria (AOB) significantly contribute to the nitrification which occurs at the surface layer of compost piles. However, the (15)N site preference within the asymmetric N(2)O molecule (SP = delta(15)N(alpha) - delta(15)N(beta), where (15)N(alpha) and (15)N(beta) represent the (15)N/(14)N ratios at the center and end sites of the nitrogen atoms, respectively) indicated that the source of N(2)O emissions just after the compost was turned originated mainly from the denitrification process. Based on these results, the reduction of accumulated NO(2)(-)-N or NO(3)(-)-N after turning was identified as the main source of N(2)O emissions. The site preference and bulk delta(15)N results also indicate that the rate of N(2)O reduction was relatively low, and an increased value for the site preference indicates that the nitrification which occurred mainly in the surface layer of the pile partially contributed to N(2)O emissions between the turnings.

摘要

采用β-变形菌氨氧化微生物的分子分析和 N(2)O 同位素分析,研究了牛粪堆肥过程中 N(2)O 排放的来源。在表面,特别是在堆肥堆的顶部,检测到大量的 NO(2)(-) - N 和 NO(3)(-) - N 和类似于欧洲硝化单胞菌的 amoA 基因,表明这些氨氧化细菌(AOB)对堆肥表层发生的硝化作用有显著贡献。然而,不对称 N(2)O 分子中的(15)N 位点偏好性(SP = delta(15)N(alpha) - delta(15)N(beta),其中(15)N(alpha) 和(15)N(beta) 分别代表氮原子中心和末端位点的(15)N/(14)N 比值)表明,堆肥刚翻堆时的 N(2)O 排放源主要来自反硝化过程。基于这些结果,翻堆后积累的 NO(2)(-) - N 或 NO(3)(-) - N 的减少被确定为 N(2)O 排放的主要来源。位点偏好和 bulk delta(15)N 结果也表明,N(2)O 还原的速率相对较低,位点偏好值的增加表明主要发生在堆肥表层的硝化作用部分导致了翻堆之间的 N(2)O 排放。

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