Abstract
Surface x-ray diffraction has been employed to quantitatively assess the surface structure of α -Cr2 O3 (0001) as a function of oxygen partial pressure at room temperature. In ultrahigh vacuum, the surface is found to exhibit a partially occupied double layer of chromium atoms. At an oxygen partial pressure of 1× 10-2 mbar, the surface is determined to be terminated by chromyl species (CrO), clearly demonstrating that the presence of oxygen can significantly influence the structure of α -Cr2 O3 (0001).
| Item Type: | Journal article |
|---|---|
| Faculties: | Geosciences > Department of Earth and Environmental Sciences > Crystallography and Materials Science |
| Subjects: | 500 Science > 550 Earth sciences and geology |
| Language: | English |
| Item ID: | 18777 |
| Date Deposited: | 10. Mar 2014 14:14 |
| Last Modified: | 04. Nov 2020 13:00 |
