ABSTRACT
The quinol form (AHDS) of 9,10-anthraquinone-2,6-disulfonate (AQDS) was used as a titrant to determine bioavailability of Fe(III) in pure iron minerals and several soils. AHDS oxidation to AQDS was coupled to Fe(III) reduction to Fe(ll) in biological media consisting of trace salts and vitamins, providing estimates of bioavailability consistentwith the biogeochemical mechanisms and conditions that control Fe(III) availability to iron-reducing bacteria. Iron(III) oxide sources were synthetic oxides (amorphous and crystalline) and three soils separated into two size fractions each (0-500 and 500-1000 microm). This titration gave a measurement of the amount of Fe(III) available to dissimilatory iron-reducing bacteria and was compared to hydroxylamine reduction, oxalate extraction, and biological reduction by Shewanella alga BrY. The advantage of AHDS titration over existing chemical techniques is that it can be performed at normal soil pH and ionic strength, and it allows for distinction of iron(III) oxides rendered unavailable by sorption of Fe(II) or by other pH-dependent geochemical processes. This approach also allows distinction of Fe(III) present in micropores that is not directly available to bacteria but bioavailable in the presence of an electron shuttle capable of transporting electrons into the micropores.