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International
Tables for Crystallography Volume G Definition and exchange of crystallographic data Edited by J. R. Hester and B. McMahon © International Union of Crystallography 2026 |
International Tables for Crystallography (2026). Vol. G. Early view chapter
https://doi.org/10.1107/97809553602060001011 Chapter 4.2 Core dictionary (coreCIF) |
Core dictionary version 3.3.0
_refine_ls.extinction_method
Name:_refine_ls.extinction_method
Aliases:
_refine_ls_extinction_method
_refine.ls_extinction_method
Definition:
A description of the extinction correction method applied with the
data item _refine_ls.extinction_coef. This description should
include information about the correction method, either 'Becker-
Coppens' or 'Zachariasen'. The latter is sometimes referred to as
the 'Larson' method even though it employs Zachariasen's formula.
The Becker-Coppens procedure is referred to as 'type 1' when
correcting secondary extinction dominated by the mosaic spread;
as 'type 2' when secondary extinction is dominated by particle
size and includes a primary extinction component; and as 'mixed'
when there are types 1 and 2.
For the Becker-Coppens method it is also necessary to set the
mosaic distribution as either 'Gaussian' or 'Lorentzian'; and the
nature of the extinction as 'isotropic' or 'anisotropic'. Note
that if either the 'mixed' or 'anisotropic' corrections are applied
the multiple coefficients cannot be contained in the
_refine_ls.extinction_coef and must be listed in _refine.special_details.
References:
Becker, P. J. & Coppens, P. (1974). Acta Cryst. A30, 129-153.
Zachariasen, W. H. (1967). Acta Cryst. 23, 558-564.
Larson, A. C. (1967). Acta Cryst. 23, 664-665.
Examples:| Zachariasen |
| 'B-C type 2 Gaussian isotropic' |
Type: Text
Category:
refine_ls