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. © 1998 American Institute of Physics.
Cite
CITATION STYLE
APA
Li, X. G., Chiba, A., Takahashi, S., & Sato, M. (1998). Oxidation characteristics and magnetic properties of iron ultrafine particles. Journal of Applied Physics, 83(7), 3871–3875. https://doi.org/10.1063/1.366619
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free