Abstract

Zinc ferrite was obtained by prolonged dry grinding of stoichiometric powder mixtures of ZnO + α-Fe 2O 3 or ZnCO 3 + α-Fe 2O 3. The kinetics of transformation was studied by X-ray diffraction, Mössbauer spectroscopy and DTA. Crystallite size reduction followed the process, and defect structures resulted. The carbonate decomposed as a necessary step in the process. In the mixture of NiO + α-Fe 2O 3, nickel ferrite was not obtainable, although considerable grain size reduction was observed. This was attributed to the inverse spinel configuration of the nickel ferrite, differing from the normal spinel configuration of the zinc ferrite. In the α-Fe 2O 3 and the zinc ferrite, iron ions occupy octahedral sites, while in ZnO and the ferrite, zinc ions occupy tetrahedral sites, and metal ion—oxygen distance is almost identical. These facilitate the transformation. In the nickel ferrite, iron ions occupy both sites, which calls for high strains of α-Fe 2O 3 before it can undergo transformation. Further implications of the processes are discussed.

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