CAJ | 학술논문

异化Fe(Ⅲ)还原微生物是厌氧环境中广泛存在的一类主要微生物类群,它们的共同特征是可以利用Fe(Ⅲ)作为末端电子受体而获得能量.鉴于土壤Fe(Ⅲ)异化还原是厌氧环境中影响碳、氮、磷及金属元素生物地球化学循环的重要因素,对Fe(Ⅲ)异化还原在环境中的作用进行评述,系统介绍了国内外有关Fe(Ⅲ)还原环境效益的研究现状及其发展趋势.
이화Fe(Ⅲ)환원미생물시염양배경중엄범존재적일류주요미생물류군,타문적공동특정시가이이용Fe(Ⅲ)작위말단전자수체이획득능량.감우토양Fe(Ⅲ)이화환원시염양배경중영향탄、담、린급금속원소생물지구화학순배적중요인소,대Fe(Ⅲ)이화환원재배경중적작용진행평술,계통개소료국내외유관Fe(Ⅲ)환원배경효익적연구현상급기발전추세.
Dissimilatory Fe(Ⅲ) reducing microorganisms are dominant groups widely present in variety anaerobic environments, which share the common features with the ability to use Fe(Ⅲ) as the terminal electron aeceptor to gain energy. Fe(Ⅲ) dissimilatory reduction have a major impact on the biogeochemical cycling of carbon, nitrogen, phosphorus and (trace) metals under anaerobic conditions. The effects of soil Fe(Ⅲ) dissimilatory reduction on environment were reviewed in this paper. The status and prospect of the environmental benefits of disimilatory Fe(Ⅲ) reduction were also discussed systemically.