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Potential Function of Added Minerals as

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Table 1. Mössbauer Spectroscopy Results (Obtained at 140K) for Iron Minerals Formed During Fe(II) Oxidation by Acidovoraxsp
Figure 1. Oxidation of Fe(II) by the nitrate-reducing Fe(II)-oxidizingthe presence of goethite, hematite, and magnetite nucleation seeds,respectively
Figure 2. growth medium. (A) without additions, (B) in the presence of goethite, (C) in the presence of magnetite, (D) in the presence of magnetite plus 0.42mg mLAcidovoraxoxidized using H57Fe Mössbauer spectra (measured at 140K) of minerals resulting aft
Figure 3. 57Fe Mössbauer spectra (measured at 140K) of minerals resulting after aging of ∼6 mM of 57Fe-enriched Fe(II) medium for 14 days in thepresence of mineral nucleation sites goethite (A), hematite (B), and magnetite (C).
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