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湿地土壤和沉积物异化铁还原过程研究进展
引用本文:朱晓艳,袁宇翔,宋长春,姜明.湿地土壤和沉积物异化铁还原过程研究进展[J].湿地科学,2020,18(1):122-128.
作者姓名:朱晓艳  袁宇翔  宋长春  姜明
作者单位:吉林建筑大学,松辽流域水环境教育部重点实验室,吉林长春130118;中国科学院湿地生态与环境重点实验室,中国科学院东北地理与农业生态研究所,吉林长春130102;North Dakota State University,North Dakota 58102,USA;中国科学院湿地生态与环境重点实验室,中国科学院东北地理与农业生态研究所,吉林长春130102
基金项目:国家自然科学基金项目(41601101和41771120);支持“率先行动”中国博士后科学基金会与中国科学院联合资助优秀博士后项目(2015LH0010);博士后国际交流计划项目(20160065)资助。
摘    要:异化铁还原是湿地土壤和沉积物中重要的生物地球化学过程,也是有机质矿化的主要途径之一。湿地干湿交替等过程会使土壤的氧化还原状态发生改变,影响铁元素及与其相关的元素的迁移和转化。总结了湿地土壤和沉积物中异化铁还原过程及其与碳、磷、硫等元素在生物地球化学循环关键过程中的相互作用,阐述了湿地土壤和沉积物中异化铁还原过程对微量金属元素迁移和转化的影响,分析了影响湿地土壤和沉积物异化铁还原过程的主要环境因子。未来相关研究应集中于湿地土壤和沉积物中异化铁还原微生物分析和纯化、不同有机质形式对异化铁还原过程的影响以及异化铁还原对土壤有机质矿化的贡献。

关 键 词:异化铁还原  土壤  沉积物  湿地  迁移  转化

Advance in Dissimilatory Iron Reduction in Wetland Soils and Sediments
ZHU Xiaoyan,YUAN Yuxiang,SONG Changchun,JIANG Ming.Advance in Dissimilatory Iron Reduction in Wetland Soils and Sediments[J].Wetland Science,2020,18(1):122-128.
Authors:ZHU Xiaoyan  YUAN Yuxiang  SONG Changchun  JIANG Ming
Institution:(Key Laboratory of Songliao Aquatic Environment,Ministry of Education,Jilin Jianzhu University,Changchun 130118,Jilin,P.R.China;Key Laboratory of Wetland Ecology and Environment,Northeast Institute of Geography and Agroecology,Chinese Academy of Sciences,Changchun 130102,Jilin,P.R.China;North Dakota State University,Fargo 58102,North Dakota,USA)
Abstract:Dissimilatory iron reduction, an important biogeochemical process in the soils and sediments of the wetlands, is vital for organic matter mineralization. Iron transport and transformation are affected by changes in redox state caused by the alternation of drying and wetting. The relationship between dissimilatory iron reduction and the biogeochemical cycles of carbon was studied, phosphorus and sulfur, as well as the effects on the transport and transformation of the trace elements in the wetlands. The environmental factors which have effects on the dissimilatory iron reduction were also discussed. Future research should focus on separation and purification microorganisms of dissimilatory iron reduction, effects of different forms of organic matter on dissimilatory iron reduction and the contribution of dissimilatory iron reduction on organic matter mineralization in the wetlands.
Keywords:dissimilatory iron reduction  soil  sediment  wetland  transportation  transformation
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