Oxidation of Fe(II) by Flavins under Anoxic Conditions

被引:15
|
作者
Zhang, Peng [1 ]
Van Cappellen, Philippe [2 ,3 ]
Pi, Kunfu [2 ,3 ]
Yuan, Songhu [1 ]
机构
[1] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430078, Hubei, Peoples R China
[2] Univ Waterloo, Water Inst, Ecohydrol Res Grp, Waterloo, ON N2L 3G1, Canada
[3] Univ Waterloo, Dept Earth & Environm Sci, Waterloo, ON N2L 3G1, Canada
基金
加拿大自然科学与工程研究理事会; 中国国家自然科学基金;
关键词
NATURAL ORGANIC-MATTER; EXTRACELLULAR ELECTRON-TRANSFER; IRON REDOX TRANSFORMATIONS; HUMIC SUBSTANCES; CONDITIONS RELEVANT; DESFERRIOXAMINE-B; MOLECULAR-OXYGEN; FE-III; REDUCTION; RIBOFLAVIN;
D O I
10.1021/acs.est.0c02916
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Flavin-mediated electron transfer is an important pathway for Fe(III) reduction by dissimilatory iron-reducing bacteria. Although the mechanisms and kinetics of Fe(III) reduction by reduced flavins have been widely studied, the reaction between Fe(II) and oxidized flavins is rarely investigated. Results of this study show that under anoxic conditions, Fe(II) can be oxidized by the oxidized forms of riboflavin (RBF) and flavin mononucleotide (FMN) at pH 7-9. For instance, at pH 9, 73% of 17.8 mu M Fe(II) was oxidized by 10 mu M RBF within 20 min. Both the rate and extent of oxidation increased with increasing concentrations of oxidized flavins and increasing solution pH. Thermodynamic calculations and kinetic analyses implied that the oxidation of Fe(II) proceeded predominantly via the autodecomposition of Fe2+-RBF- and Fe2+-FMN- complexes, along with minor contributions from direct oxidation of Fe(II) by flavins and flavin radicals. Our findings suggest that the reoxidation of Fe(II) by oxidized flavins may be a rate-controlling factor in microbial Fe(III) reduction via flavin-mediated electron transfer.
引用
收藏
页码:11622 / 11630
页数:9
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