Article(id=1226855199319441643, tenantId=1146029695717560320, journalId=1192105938417971205, issueId=1226855188863038235, articleNumber=null, orderNo=null, doi=10.13343/j.cnki.wsxb.20240430, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=research-article, receivedDate=1721059200000, receivedDateStr=2024-07-16, revisedDate=null, revisedDateStr=null, acceptedDate=1730044800000, acceptedDateStr=2024-10-28, onlineDate=1770434673385, onlineDateStr=2026-02-07, pubDate=1748966400000, pubDateStr=2025-06-04, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1770434673385, onlineIssueDateStr=2026-02-07, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1770434673385, creator=13701087609, updateTime=1770434673385, updator=13701087609, issue=Issue{id=1226855188863038235, tenantId=1146029695717560320, journalId=1192105938417971205, year='2025', volume='65', issue='6', pageStart='2321', pageEnd='2769', issueExtLink='null', onlineDate='null', pubDate='null', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=0, createTime=1770434670891, creator=13701087609, updateTime=1770435273893, updator=13701087609, preIssue=null, nextIssue=null, ext={EN=IssueExt(id=1226857718103851267, tenantId=1146029695717560320, journalId=1192105938417971205, issueId=1226855188863038235, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1226857718103851268, tenantId=1146029695717560320, journalId=1192105938417971205, issueId=1226855188863038235, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null}, startPage=2325, endPage=2337, ext={EN=ArticleExt(id=1226855200237994251, articleId=1226855199319441643, tenantId=1146029695717560320, journalId=1192105938417971205, language=EN, title=Aerobic ammonia-oxidizing microorganisms and the mechanisms of nitrous oxide production: a review, columnId=1192149543727808575, journalTitle=Acta Microbiologica Sinica, columnName=Review, runingTitle=null, highlight=null, articleAbstract=

The rising level of atmospheric nitrous oxide (N₂O) has garnered the attention of researchers to microorganism-mediated N₂O synthesis in recent years. According to the recent studies, one of the main sources of N₂O in the world is the nitrification process carried out by aerobic aerobic ammonia oxidizing microorganisms (AOMs). We summarized the taxa of AOMs, the ecological distribution of AOMs, the environmental factors influencing the distribution, and the hotspots, pathways, and influencing factors of AOM-mediated N₂O production. Finally, we prospected the future research directions in this field. This review improves our understanding of AOMs and their mechanisms of N₂O production.

, correspAuthors=Ping LI, authorNote=null, correspAuthorsNote=, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, authorCompany=null, fund=null, authors=null, authorsList=Rui MA, Yaqi WANG, Helin WANG, Ping LI), CN=ArticleExt(id=1226855201445953911, articleId=1226855199319441643, tenantId=1146029695717560320, journalId=1192105938417971205, language=CN, title=好氧氨氧化微生物类群及其介导的氧化亚氮产生机制综述, columnId=1192149543882997826, journalTitle=微生物学报, columnName=综述, runingTitle=null, highlight=null, articleAbstract=

近年来，随着氧化亚氮(nitrous oxide, N₂O)在大气中浓度的逐年上升，微生物介导的N₂O产生机制日益引起学界的关注。近期研究表明，好氧氨氧化微生物(aerobic ammonia oxidizing microorganisms, AOMs)参与的氨氧化过程是全球N₂O的主要来源之一。本文从AOMs的种群分类、各类群的生态分布特点及影响其分布的环境因素、AOMs介导N₂O产生的热点地区、AOMs产生N₂O的途径及其影响因素进行归纳总结，并对未来的研究方向进行了展望。本综述有助于进一步理解AOMs类群及其产N₂O机制。

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Water Research, 2017, 122: 96-113., articleTitle=Quantifying nitrous oxide production pathways in wastewater treatment systems using isotope technology: a critical review, refAbstract=null)], funds=[Fund(id=1227680963593961974, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, awardId=42177068, language=EN, fundingSource=National Natural Science Foundation of China(42177068), fundOrder=null, country=null), Fund(id=1227680963715596800, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, awardId=42177068, language=CN, fundingSource=国家自然科学基金(42177068), fundOrder=null, country=null)], companyList=[AuthorCompany(id=1227680957604495562, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, xref=null, ext=[AuthorCompanyExt(id=1227680957608689869, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, companyId=1227680957604495562, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=State Key Laboratory of Geomicrobiology and Environmental Changes, China University of Geosciences, Wuhan, Hubei, China), AuthorCompanyExt(id=1227680957625467084, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, companyId=1227680957604495562, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=中国地质大学(武汉)，地质微生物与环境全国重点实验室，湖北 武汉)])], figs=[ArticleFig(id=1227680961551335854, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, language=EN, label=Figure 1, caption=Phylogenetic evolutionary tree based on 16S rRNA gene sequences of aerobic ammonia oxidizing microorganisms, figureFileSmall=hIBoW1DSFg4cCPTkO6sFNg==, figureFileBig=OlvIEvQTnb/CjiBvelE90A==, tableContent=null), ArticleFig(id=1227680961651999156, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, language=CN, label=图1, caption=好氧氨氧化菌基于16S rRNA基因序列的系统发育树, figureFileSmall=hIBoW1DSFg4cCPTkO6sFNg==, figureFileBig=OlvIEvQTnb/CjiBvelE90A==, tableContent=null), ArticleFig(id=1227680961756856766, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, language=EN, label=Figure 2, caption=Schematic diagram of N₂O production pathway of aerobic ammonia oxidizing microorganisms.A: Three pathways of AOB-mediated N₂O production; B: Two hypotheses for AOA-mediated N₂O production. AMO: Ammonia monooxygenase; HAO: Hydroxylamine oxidoreductase; NOO: Nitric oxide oxidase; NIR: Nitrite reductase; NOR: Nitric oxide reductase; Cyt P460: Cytochrome P460; NXOR: Nitroxyl oxidoreductase; Cu-HAO: Copper hydroxylamine oxidoreductase; Cu-NIR: Copper nitrite reductase., figureFileSmall=9NA6vH73rr7yu21rboMr/Q==, figureFileBig=oGOcac5VgYyWKZBZXC93bw==, tableContent=null), ArticleFig(id=1227680961882685901, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, language=CN, label=图2, caption=好氧氨氧化菌N₂O产生途径示意图, figureFileSmall=9NA6vH73rr7yu21rboMr/Q==, figureFileBig=oGOcac5VgYyWKZBZXC93bw==, tableContent=null), ArticleFig(id=1227680961970766296, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, language=EN, label=Table 1, caption=

Summary of typical hotspots and flux of N₂O

, figureFileSmall=null, figureFileBig=null, tableContent=

Hotspots	Samplinng environments	N2O flux or concentration	Reference
Various types of soil	Alkaline, neutral purple soil	103.71 ng/(g·d)	[63]
	Oil palm soil	408.57 ng/(g·h)	[60]
	Forest soil	18.86 ng/(g·h)	[61]
	Agricultural soil	226.60 μg/(m2·h)	[62]
Marine	The eastern tropical south Pacific	13.73 ng/(L·d)	[65]
	The eastern tropical north Pacific	13.20 ng/d	[64]
Various freshwater systems	River	580.80 μg/(m2·d)	[68]
	Stream	264.00 μg/(m2·h)	[69]
	Lake	69.41 g/(m2·y)	[67]
	Sewage treatment system	7.00 μg/(g·min)	[66]
Various types of sediments	Plateau wetland sediment	50.29 ng/(g·d)	[71]
	Thawing Yedoma permafrost	1.72 mg/(m2·d)	[72]
	Estuarine sediment	9.24 ng/(g·h)	[70]

), ArticleFig(id=1227680963354886630, tenantId=1146029695717560320, journalId=1192105938417971205, articleId=1226855199319441643, language=CN, label=表1, caption=

典型N₂O释放热点区域及其通量

, figureFileSmall=null, figureFileBig=null, tableContent=

Hotspots	Samplinng environments	N2O flux or concentration	Reference
Various types of soil	Alkaline, neutral purple soil	103.71 ng/(g·d)	[63]
	Oil palm soil	408.57 ng/(g·h)	[60]
	Forest soil	18.86 ng/(g·h)	[61]
	Agricultural soil	226.60 μg/(m2·h)	[62]
Marine	The eastern tropical south Pacific	13.73 ng/(L·d)	[65]
	The eastern tropical north Pacific	13.20 ng/d	[64]
Various freshwater systems	River	580.80 μg/(m2·d)	[68]
	Stream	264.00 μg/(m2·h)	[69]
	Lake	69.41 g/(m2·y)	[67]
	Sewage treatment system	7.00 μg/(g·min)	[66]
Various types of sediments	Plateau wetland sediment	50.29 ng/(g·d)	[71]
	Thawing Yedoma permafrost	1.72 mg/(m2·d)	[72]
	Estuarine sediment	9.24 ng/(g·h)	[70]

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