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 μM Fe(II) was oxidized by 10 μM 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.