Conduction Band of Hematite Can Mediate Cytochrome Reduction by Fe(II) under Dark and Anoxic Conditions.

While it was recently reported that the conduction band of iron minerals can mediate electron transfer between Fe(II) and different Fe(III) lattice sites during Fe(II)-catalyzed mineral transformation, it is unclear whether such a conduction band mediation pathway occurs in the microbial Fe(II) oxidation system under dark and anoxic subsurface conditions. Here, using cytochrome (-Cyts) as a model protein of microbial Fe(II) oxidation, the kinetics and thermodynamics of -Cyts reduction by Fe(II) were studied. The results showed that the rates of -Cyts reduction were greatly enhanced in the presence of the semiconducting mineral hematite (Hem, α-FeO). The electrochemical experiments separating Fe(II) and -Cyts demonstrated that electrons from Fe(II) to the electrode or from the electrode to -Cyts could directly penetrate hematite, resulting in enhanced current. Independent photochemical and photoluminescence experiments indicated that Cyts could be directly reduced by the conduction band electrons of hematite which were generated under light illumination. In -Cyts+Fe(II)+Hem, the redox potential of Fe(II)-Hem was shifted from -0.15 to -0.18 V and that of -Cyts+Hem changed slightly from -0.05 to -0.04 V. For the bulk hematite, Mott-Schottky plots illustrated that the flat band was shifted negatively and positively in the presence of Fe(II) and oxidized -Cyts, respectively, and the surface electron/charge density was higher in the presence of Fe(II)/-Cyts. As a consequence, the redox gradients from adsorbed Fe(II) to adsorbed -Cyts allow electron transfer across the conduction band of hematite and facilitate -Cyts reduction. This mechanistic study on conduction band-mediating electron transfer could help interpret the role of semiconducting minerals in the microbial Fe(II) oxidation process under dark anoxic conditions.