{"doi":"10.1039/d0em00063a","title":"Interactions of ferrous iron with clay mineral surfaces during sorption and subsequent oxidation","abstract":"
\n Under anoxic conditions, clay minerals sorb dissolved Fe(\n ii\n ) predominantly by forming surface precipitates, which transform into Fe(\n iii\n )-phases upon aeration.\n
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\n Under anoxic conditions, clay minerals sorb dissolved Fe(\n ii\n ) predominantly by forming surface precipitates, which transform into Fe(\n iii\n )-phases upon aeration.\n
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