Iron governs biological activities
in the natural environment as
an essential element. Although the concentrations of dissolved iron
species are primarily regulated by the solubility of iron minerals,
there are additional pathways of the supply of dissolved iron species
from solids. Redox processes play important roles in the dissolution
of iron species from minerals because ferrous ions are more soluble
than ferric ions. In addition, recent studies have indicated that
freezing enhances the dissolution of iron species from oxides in the
presence of acids or ligands. Thus, although freeze-specific phenomena
may play essential roles in the determination of this process of fundamental
and environmental importance, the details have not been elucidated.
In the present paper, the redox behaviors of major iron oxides, that
is, magnetite, maghemite, and hematite, are studied using cyclic voltammetry
in frozen acidic media. The results indicate that freezing facilitates
the leaching of Fe2+ from magnetite but hinders the reduction
of ferric ions in the oxide crystals. The latter is commonly observed
for all iron oxides studied here. This hindrance is caused by the
freeze enrichment of Fe2+ at the interface between the
iron oxide and freeze-concentrated solution and by the surface adsorption
of Fe2+.