Published March 1, 1986
| Version v1
Journal article
Crystal structure of acicular γ-Fe2O3 particles used in recording media
Creators
- 1. Department of Materials Science and Mineral Engineering, Materials and Molecular Research Division and the National Center for Electron Microscopy, Lawrence Berkeley Laboratory, University of California, Berkeley, California 94720
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
Additional details
Publishing Information
- Journal Title
- J. Appl. Phys.
- Journal Volume
- 59
- Journal Issue
- 5
- Series
- J. Appl. Phys.
- Journal Page Range
- 1606-1610
- ISSN
- 0021-8979
- CODEN
- JAPIA
INIS
- Country of Publication
- United States
- Country of Input or Organization
- United States
- INIS RN
- 17049980
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- CRYSTAL STRUCTURE; DIFFUSION; ELECTRON DIFFRACTION; ELECTRON MICROSCOPY; IRON OXIDES; LATTICE PARAMETERS; MAGNETIC TAPES; MATERIALS; ORDER-DISORDER TRANSFORMATIONS; SUPERLATTICES; VACANCIES
- Descriptors DEC
- CHALCOGENIDES; COHERENT SCATTERING; CRYSTAL DEFECTS; DIFFRACTION; IRON COMPOUNDS; MAGNETIC STORAGE DEVICES; MEMORY DEVICES; MICROSCOPY; OXIDES; OXYGEN COMPOUNDS; PHASE TRANSFORMATIONS; POINT DEFECTS; SCATTERING; TRANSITION ELEMENT COMPOUNDS