Organic Matter from Redoximorphic Soils Accelerates and Sustains Microbial Fe(III) Reduction

Microbial reduction of Fe­(III) minerals is a prominent process in redoximorphic soils and is strongly affected by organic matter (OM). We herein determined the rate and extent of microbial reduction of ferrihydrite (Fh) with either adsorbed or coprecipitated OM by Geobacter sulfurreducens. We focus...

Ausführliche Beschreibung