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Migration and transformation of antimony during Fe(II)-induced ferrihydrite recrystallization under anaerobic conditions
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DOI：10.1016/j.apgeochem.2026.106957.png)
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Abstract
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• Fe(II) drives ferrihydrite transformation and controls antimony mobility. • Sb(III) shows a stronger influence on mineral transformation than Sb(V). • Goethite or lepidocrocite formation depends strongly on Fe:Sb molar ratios. • Up to 61% of antimony becomes stably sequestered beyond surface adsorption. • Fe(II)-mediated processes oxidize Sb(III) to Sb(V) under anoxic conditions.
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