
Abstract
Anisotropic diffuse scattering of the 1D conductor K-hollandite has been measured at a synchrotron source and compared with measurements with a rotating anode. The intensity gain of more than one order of magnitude and the ability to adjust the wavelength provide the counting statistics in a few hours that are necessary for a quantitative analysis of diffuse phenomena. The main advantage of a synchroton source is the high resolution throughout reciprocal space (low and high Q). Thus, commensurate/incommensurate positions of diffuse layers may be distinguished, weak diffuse maxima become detectable and small peak shifts of diffuse modulations clearly visible.
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-18591-2 |
Language: | English |
Item ID: | 18591 |
Date Deposited: | 10. Mar 2014, 14:11 |
Last Modified: | 04. Nov 2020, 13:00 |