Abstract
The oxidation rates of cobalt and iron as a function of oxide thickness and temperature have been measured in the vicinity of the and crystallographic-phase-transition temperatures using a gravimetric technique. The oxidation rate of both metals changed markedly at the structural-phase-transition temperature. The effects of a crystallographic versus a magnetic phase change on the oxidation rates are compared.
- Received 23 March 1981
DOI:https://doi.org/10.1103/PhysRevB.25.1688
©1982 American Physical Society