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Molecular-weight-dependent redox cycling of humic substances of paddy soils over successive anoxic and oxic alternations
Tan, Wenbing1; Wang, Guoan2; Zhao, Xinyu1; Dang, Qiuling3; Li, Renfei1; Xi, Beidou1; Jiang, Jie4; Zhang, Hui1; Li, Dan1; Cui, Dongyu1; Jia, Yufu2,5
2019
发表期刊LAND DEGRADATION & DEVELOPMENT
ISSN1085-3278
卷号30期号:9页码:1130-1144
摘要Humic substances (HSs) are critical to regulating methane cycling in temporary anoxic systems because their redox-active functional groups can sustainably shuttle electrons from microorganisms to oxygen (O-2) over successive anoxic and oxic alternations. Whether the relative amount of these redox-active functional groups involved in redox cycles is associated with the overall chemical structures of HS still remains poorly understood. In this study, variations in the reducing capacities (RCs) of HSs extracted from paddy soils were monitored over consecutive cycles of reduction by iron-reducing microorganisms and oxidation by O-2. Our results show that about 10-40% of the microbially reduced redox-active moieties within HS, which were reoxidised by O-2, cannot restore the same redox state as those before microbial reduction. The restoration extents of RCs of HSs after microbial reduction and O-2 reoxidation were greatly negatively correlated with average molecular weight (AMW). The microbially reduced HSs having large AMWs (>1,000 Da) were more kinetically difficult to restore by O-2 from a reduced state to an oxidised state than were those having small AMWs (<1,000 Da) possibly because the former, which underwent process of microbial reduction and O-2 reoxidation, were more easily sheltered by other parts of HS structures than were the latter. Nevertheless, the unsheltered redox-active groups that accounted for about 50-85% in HSs can be fully reversible and sustainable to switch between a reduced state and an oxidised state over successive redox cycles. Our results can help to understand the redox dynamics of HSs in biogeochemical cycles in environments.
关键词humic substances microbial reduction molecular weight redox cycling reoxidation by O-2
学科领域Environmental Sciences ; Soil Science
DOI10.1002/ldr.3299
收录类别SCI
语种英语
WOS关键词NATURAL ORGANIC-MATTER ; MICROBIAL REDUCTION ; ELECTRON-ACCEPTORS ; OPTICAL-PROPERTIES ; METHANE PRODUCTION ; FUNCTIONAL-GROUPS ; NITROUS-OXIDE ; FLUORESCENCE ; ACIDS ; RECALCITRANCE
WOS研究方向Environmental Sciences & Ecology ; Agriculture
WOS记录号WOS:000470932100010
出版者WILEY
文献子类Article
出版地HOBOKEN
EISSN1099-145X
资助机构National Key Research and Development Program of China [2017YFA0605003] ; National Natural Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [51325804, 41501242]
作者邮箱xibeidou@yeah.net
引用统计
被引频次:3[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ibcas.ac.cn/handle/2S10CLM1/19687
专题植被与环境变化国家重点实验室
作者单位1.Chinese Res Inst Environm Sci, State Key Lab Environm Criteria & Risk Assessment, Beijing 100012, Peoples R China
2.Chinese Res Inst Environm Sci, State Environm Protect Key Lab Simulat & Control, Beijing 100012, Peoples R China
3.China Agr Univ, Coll Resources & Environm Sci, Beijing 100193, Peoples R China
4.Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China
5.Beijing Forestry Univ, Coll Environm Sci & Engn, Beijing 100083, Peoples R China
6.Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China
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GB/T 7714
Tan, Wenbing,Wang, Guoan,Zhao, Xinyu,et al. Molecular-weight-dependent redox cycling of humic substances of paddy soils over successive anoxic and oxic alternations[J]. LAND DEGRADATION & DEVELOPMENT,2019,30(9):1130-1144.
APA Tan, Wenbing.,Wang, Guoan.,Zhao, Xinyu.,Dang, Qiuling.,Li, Renfei.,...&Jia, Yufu.(2019).Molecular-weight-dependent redox cycling of humic substances of paddy soils over successive anoxic and oxic alternations.LAND DEGRADATION & DEVELOPMENT,30(9),1130-1144.
MLA Tan, Wenbing,et al."Molecular-weight-dependent redox cycling of humic substances of paddy soils over successive anoxic and oxic alternations".LAND DEGRADATION & DEVELOPMENT 30.9(2019):1130-1144.
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