Abstract
We have studied the kinetics of the transitions between the Fe2O3 and Fe3O4 phases as thin epilayers (∼2.5 nm) on Al2O3 (001) substrates using time-resolved reflection high energy electron diffraction. The different iron oxide phases were identified using a combination of in-situ and ex-situ characterizations. The transition from an α-Fe2O3 (001) epilayer to a Fe3O4 (111) epilayer through thermal reduction was found to be determined by the Fe-O bonding energy, resulting in a long time scale. The oxidation at high temperature converts a Fe3O4 (111) epilayer to an α-Fe2O3 (001) epilayer quickly; at low temperature, a γ-Fe2O3 (111) epilayer was slowly generated instead. By repeating the deposition/thermal reduction processes, a thicker Fe3O4 (111) film was obtained, which exhibit high crystallinity and moderate magnetic coercivity.
| Original language | English |
|---|---|
| Article number | 085313 |
| Journal | Journal of Applied Physics |
| Volume | 120 |
| Issue number | 8 |
| DOIs | |
| State | Published - 28 Aug 2016 |