Physics
Scientist
Evolution of Fe(II) Mineralization Induced by Dissimilatory Iron-reducing Bacteria
Hillslope asymmetry maps reveal widespread, multi-scale organization
Reductive Dissolution and Biomineralization of Iron Oxides Under Dynamic Flow Conditions
Secondary mineralization pathways induced by dissimilatory iron reduction of ferrihydrite under advective flow
Structural constraints of ferric (hydr)oxides on dissimilatory iron reduction and the fate of Fe(II)
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