Crystal structure of acicular γ-Fe2O3 particles used in recording media

γ-Fe2O3 particles have been examined by convergent beam electron diffraction to determine the crystal symmetry. The particles have a primitive lattice with an m3m point group and a cubic superstructure with lattice parameter approximately equal to three times the lattice parameter of the magnetite s...

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Veröffentlicht in:Journal of applied physics 1986-03, Vol.59 (5), p.1606-1610
Hauptverfasser: HUEI-MIN HO, GOO, E, THOMAS, G
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creator HUEI-MIN HO
GOO, E
THOMAS, G
description γ-Fe2O3 particles have been examined by convergent beam electron diffraction to determine the crystal symmetry. The particles have a primitive lattice with an m3m point group and a cubic superstructure with lattice parameter approximately equal to three times the lattice parameter of the magnetite structure. This superlattice is a result of cation vacancy ordering. During observation, disordering in the electron microscope occurs and is believed to be caused by electron radiation-enhanced diffusion.
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subjects Condensed matter: structure, mechanical and thermal properties
Exact sciences and technology
Inorganic compounds
Physics
Structure of solids and liquids
crystallography
Structure of specific crystalline solids
Water, oxides, hydroxides, peroxides
title Crystal structure of acicular γ-Fe2O3 particles used in recording media
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