The reductive biotransformation of a Ni
2+-substituted (5mol %) hydrous ferric oxide (NiHFO) by
Shewanellaputrefaciens, strain CN32, was investigated under anoxicconditions at circumneutral pH. Our objectives were to definethe influence of Ni
2+ substitution on the bioreducibilityof the HFO and the biomineralization products formed andto identify biogeochemical factors controlling the phasedistribution of Ni
2+ 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 Ni
2+ 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 Ni
2+.Nickel was generally mobilized during bioreduction in atrend that correlated with final pH, except in cases wherePO
43- was present and vivianite precipitation occurred.CN32 promoted the formation of Ni
2+-substituted magnetite(
O
4) in media with AQDS but withoutPO
43-. The formation of this biogenic coprecipitate, however,had little discernible impact on final aqueous Ni
2+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.