Abstract
The constant momentum transfer averaging method has been used to determine the surface structure of the Ag(110) surface. A contraction of 8% of the first layer spacing compared to the bulk value is found by comparing the shape of the averaged intensity profiles with kinematic calculations rather than the position of the peaks. This result agrees well with that obtained by a multiple scattering calculation.
Dokumententyp: | Zeitschriftenartikel |
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Fakultät: | Geowissenschaften > Department für Geo- und Umweltwissenschaften > Kristallographie und Materialwissenschaft |
Themengebiete: | 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie |
URN: | urn:nbn:de:bvb:19-epub-5773-8 |
Sprache: | Englisch |
Dokumenten ID: | 5773 |
Datum der Veröffentlichung auf Open Access LMU: | 22. Aug. 2008, 06:49 |
Letzte Änderungen: | 04. Nov. 2020, 12:48 |