The study of the different oxides of iron (II) and iron (III) was carried out potentiometrically in
normalLiCl‐normalKCl
eutectic at 470°C by means of an yttria‐stabilized zirconia electrode indicator of the oxide ion activity and an iron electrode indicator of the ferrous ion activity. These measurements were complemented by the determination of cyclic voltammograms and by x‐ray diffraction and infrared spectrophotometry analysis of certain compounds formed. The main results obtained are the following: strong oxidizing power (oxidation of Cl− ions into
Cl2
) and high oxoacidity (great stability of ferric oxide) of Fe3+ ions; possible redissolution of
Fe2O3
in the oxide ion rich media by the formation of ferrate (III) ion;
FeO2−·Fe2+
ions react with O2− ions to form ferrous oxide, which is probably stabilized in the form of a solid solution
normalFeO‐LiFeO2
of composition
Fe1−yLiyO
. Magnetic oxide,
Fe3O4
, is stable and can be obtained by the action of oxide ions on a mixture of iron (II) and iron (III). The standard potentials of the different electrochemical systems, which involve iron in its different oxidation states, and the expressions of these potentials as a function of the oxide ion activity and different concentrations were given. The solubility products of iron oxides were also determined; the values corresponding to ferrous oxide, magnetic oxide, and ferric oxide are, respectively, 10−5.4, 10−36.3, and 10−29.6(molality scale). The constant of formation of ferrate (III) ion (from ferric oxide) has the rough value 101.9 mol · kg−1. These results were assembled in the form of a potential
−pO2−
equilibrium diagram which shows, in particular, that in oxobasic media, magnetic oxide disproportionates into ferrate (III) and
normalFeO
. In the presence of a high concentration of oxide anion,
normalFeO
leads to the formation of metallic iron because of its disproportionation into
FeO2−
and Fe (s).