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In this analysis, we examined the exact distance scale over which this electron shuttling may appear. We current results from agar-solidified experimental incubations, containing either AQDS or NOM, where FeRB had been actually separated from ferrihydrite or goethite by 2 cm. Iron speciation and focus measurements paired to a diffusion-reaction design highlighted plainly Fe(III) decrease in the existence of electron shuttles, in addition to the kind of FeRB. Predicated
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