
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.
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 |
URN: | urn:nbn:de:bvb:19-epub-5773-8 |
Language: | English |
Item ID: | 5773 |
Date Deposited: | 22. Aug 2008, 06:49 |
Last Modified: | 04. Nov 2020, 12:48 |