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).
Dokumententyp: | Zeitschriftenartikel |
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Fakultät: | Geowissenschaften > Department für Geo- und Umweltwissenschaften > Kristallographie und Materialwissenschaft |
Themengebiete: | 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie |
Sprache: | Englisch |
Dokumenten ID: | 18777 |
Datum der Veröffentlichung auf Open Access LMU: | 10. Mrz. 2014, 14:14 |
Letzte Änderungen: | 04. Nov. 2020, 13:00 |