1975 Volume 61 Issue 9 Pages 2160-2166
The change of crystal structure during the reduction of iron oxide and the growth mechanism of fibrous iron were investigated. In order to elucidate the crystallographic transition of Fe2O3 during the reduction, platelets of Fe2O3 single crystal with flat (0001) plane (approx. 5 mm in width and 0.5 mm in thickness) were used as samples. Each of Fe3O4, FeO, and Fe was prepared by the reduction of the Fe2O3 sample at 750°C in the CO-CO2 mixture with an appropriate composition for each. The structures of the products were analyzed by X-ray diffraction including the Lane methods and scanning electron microscopy (SEM).
The X-ray diffraction revealed that (0001) plane of Fe203 changed to (111) plane of Fe3O4 and (111) plane of FeO by epitaxial reactions. SEM revealed that as the reduction proceeded, steps parallel to (0001) plane of Fe2O3 appeared remarkably, and fibrous iron grew from some nuclei on the steps. The fibrous iron was never seen on (0001) plane of Fe2O3, and the direction of most active growth was [2110] of Fe2O3.