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Journal Article | FZJ-2014-04924 |
2014
IUCR
[S.l.]
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Please use a persistent id in citations: http://hdl.handle.net/2128/8118 doi:10.1107/S205327331400802X
Abstract: Symmetric Bragg-case reflections from a thick, ideally imperfect, crystal slab are studied mostly by analytical means. The scattering transfer function of a thin mosaic layer is derived and brought into a form that allows for analytical approximations or easy quadrature. The Darwin-Hamilton equations are generalized, lifting the restriction of wavevectors to a two-dimensional scattering plane. A multireflection expansion shows that wavevector diffusion can be studied independently of the real-space coordinate. Combining analytical arguments and Monte Carlo simulations, multiple Bragg reflections are found to result in a minor correction of the reflected intensity, a moderate broadening of the reflected azimuth angle distribution, a considerable modification of the polar angle distribution, and a noticeable shift and distortion of rocking curves
Keyword(s): Instrument and Method Development (1st) ; Others (1st) ; Instrument and Method Development (2nd)
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