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 |
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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 |