Dear Ana,

Generally, as many of the contributors of this list said, smectites are
only partly crystallised (sometimes turbostratic). Means you may observe
nice 00L peaks, and diffusion bands along HK0 lines. These latters should
be approached using appropriate formalism, actually I think not implemented
in usual programs. You could find out how this formalism works, reading
Dritz and Tchoubar books on the subject. On perfect powders, we (I and A.
Manceau and B. Lanson in Grenoble, LGIT) could simulate diagrams like this
using their formalism, taking account of bimodal compositional faults. Now
on top of this, as in our case, a strong preferred orientation is also
present in the sample. In these cases, we found useful to combine polarised
EXAFS experiments with Quantitative Texture Analysis in order to sort out
structural details. 
Please see on my personal web page, I have placed pdf files on this subject.

daniel



Quantitative Texture Analysis Internet Course:
http://pecdc.univ-lemans.fr/qta/
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Daniel Chateigner
LPEC, UMR-CNRS 06087, Université du Maine-Le Mans
http://pecdc.univ-lemans.fr/lpec.html
av. O. Messiaen, BP535 72085 Le Mans cedex
Tel prof: 33 (0) 243833268
Fax:      33 (0) 243833518 
http://www.univ-lemans.fr/~dchat/danielc/daniel.htm
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