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Building on our understanding of abiotic Fe(II)-catalyzed mineralogical modifications, the suppression of ferrihydrite transformation in FSi + Cl fractions in amended soils could eventually lead to a slower turnover of ferrihydrite, possibly keeping the carbon sequestration potential associated with this mineral. Alternatively, in both bulk soils and FSa portions, the degree to which mineral transformation happen appeared to be contingent from the quality for the amendment used. The co
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