ENHANCED DIFFUSION IN FE-(1-Y)O AND FE-(3-X)O-4
The self-diffusion of Fe in wuestite and magnetite yields unusual results at low temperatures. This paper presents thermodynamic considerations for these phenomena and suggests defect types related to the diffusion process.
Bibliographic Reference: SOLID STATE IONICS, VOL. 12 (1984), P. 99
Record Number: 1989123014100 / Last updated on: 1987-01-01
Available languages: en