Abstract
The surface structure of α-Fe2 O3 (1 over(1, ̄) 0 2) was studied under two different surface preparation conditions using crystal truncation rod (CTR) diffraction. Wet chemical and mechanical polishing (CMP) at 298 K results in a crystalline surface termination in which the top layer of iron atoms is absent compared to the stoichiometric bulk termination. Annealing in air at 773 K resulted in a transformation of the surface to a structure consistent with hydroxylation of the stoichiometric termination. These results agree with theoretical predictions of Lo et al. [C.S. Lo, K.S. Tanwar, A.M. Chaka, T.P. Trainor, Phys. Rev. B 75 (2007) 075425] and clearly show an ambient pressure surface preparation path leading to a stoichiometric hydroxylated surface, which is apparently a meta-stable configuration at room temperature.
| Original language | English |
|---|---|
| Pages (from-to) | L59-L64 |
| Journal | Surface Science |
| Volume | 601 |
| Issue number | 12 |
| DOIs | |
| State | Published - Jun 15 2007 |
Keywords
- Crystal truncation rods
- Hematite (1 over(1, ̄) 0 2)
- Iron oxide
- Surface X-ray diffraction
- Surface annealing
- Surface preparation
- Surface structure
- α-FeO