Abstract
Oxidation of Fe ultrafine particles has been studied in air at temperatures ranging from 300 to 873 K. It is found that γ-Fe2O3 and α-Fe2O3 are formed at different temperatures, which leads to significant changes in the particle features and magnetic properties.
Original language | English |
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Pages (from-to) | 3871-3875 |
Number of pages | 5 |
Journal | Journal of Applied Physics |
Volume | 83 |
Issue number | 7 |
DOIs | |
Publication status | Published - 1998 |
Externally published | Yes |
ASJC Scopus subject areas
- Physics and Astronomy(all)