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Biotransformation of Ni-Substituted Hydrous Ferric Oxide by an Fe(III)-Reducing Bacterium
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文摘
The reductive biotransformation of a Ni2+-substituted (5mol %) hydrous ferric oxide (NiHFO) by Shewanellaputrefaciens, strain CN32, was investigated under anoxicconditions at circumneutral pH. Our objectives were to definethe influence of Ni2+ substitution on the bioreducibilityof the HFO and the biomineralization products formed andto identify biogeochemical factors controlling the phasedistribution of Ni2+ during bioreduction. Incubations withCN32 and NiHFO were sampled after 14 and 32 d, and bothaqueous chemistry and solid phases were characterized.By comparison of these results with a previous study(Fredrickson, J. K.; Zachara, J. M.; Kennedy, D. W.; Dong,H.; Onstott, T. C.; Hinman, N. W.; Li, S. W. Geochim.Cosmochim. Acta 1998, 62, 3239-3257), it was concludedthat coprecipitated/sorbed Ni2+ inhibited the bioreductionof HFO through an undefined chemical mechanism. Mössbauerspectroscopy allowed analysis of the residual HFOphase and the identity and approximate mass percent ofbiogenic mineral phases. The presence of AQDS, a solubleelectron shuttle that obviates need for cell-oxide contact,was found to counteract the inhibiting effect of Ni2+.Nickel was generally mobilized during bioreduction in atrend that correlated with final pH, except in cases wherePO43- was present and vivianite precipitation occurred.CN32 promoted the formation of Ni2+-substituted magnetite(O4) in media with AQDS but withoutPO43-. The formation of this biogenic coprecipitate, however,had little discernible impact on final aqueous Ni2+concentrations. These results demonstrate that coprecipitatedNi can inhibit dissimilatory microbial reduction ofamorphous iron oxide, but the presence of humic acidsmay facilitate the immobilization of Ni within the crystalstructure of biogenic magnetite.

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