Magnetite Oxidation: A Proposed Mechanism
Umberto Colombo 1,
Franco Gazzarrini 1,
Giuseppe Lanzavecchia 1, and
Giuseppe Sironi 1
1 Montecatini Co., "G. Donegani" Research Institute, Novara, Italy
All magnetites are oxidized topotactically with formation of solid solution at temperatures below 400°C. The oxidation of hematite-free magnetites proceeds to
Fe2O3, whereas in the presence of hematite epitaxial growth of
Fe2O3 takes place, with excess iron ions being returned to the solid solution. A method for synthesizing maghemite from natural magnetites is indicated.