Dear Ross,

something like this can definitely be adapted in the launch mode of TOPAS, it has been done in the past. A few lines for orthorhombic (some minor changes required for trigonal/hexagonal):
prm s400  8349.85430
       prm s040  1967.90075
       prm s004  129.62651
       prm s220  2451.94087
       prm s202  -921.49437
       prm s022     -23.92103
       prm eta  0.49540 min 0 max 1
       prm  mhkl = H^4 s400 + K^4 s040 + L^4 s004 +
                 H^2 K^2 s220 + H^2 L^2 s202 + K^2 L^2 s022;
     prm pp = D_spacing^2 * Sqrt(Max(mhkl,0)) / 1000;
     gauss_fwhm = 1.8/3.1415927 pp (1-eta) Tan(Th) + 0.0001;
     lor_fwhm   = 1.8/3.1415927 pp eta     Tan(Th) + 0.0001;

(this way to set up the "Stephens model" in Topas originates from R. Dinnebier or P.W. Stephens; this is the simplest way to do it if you are not really interested in the meaning of the SHKL parameters)
I may give detailed hints in direct exchange.

Additionally I would like to indicate that something which looks on the first view like anisotropic strain, may instead be anisotropic crystallite size (is S112 positive or negative?) or stacking faults. In particular the latter is very common for "laminar" structures and may give to quite complex diffraction phenomena.

Best regards
Andreas Leineweber


Ross H Colman wrote:
Dear Rietvelders,

I am a PhD student working at UCL (UK) and was wondering if anyone out
there could help me with a diffraction related problem:

I am attempting to refine some neutron diffraction data on a powder
sample that has a very laminar structure. The refinement is acceptable
but close inspection shows that some peaks are modelled poorly compared
to others. The relative intensity of each peak appears to be a good fit
but some peaks are sharper than others whilst some are noticably broadened.

The instrument responsible suggested using anisotropic strain within
Fullprof to attempt to model the peak shape anisotropies (as an ILL
instrument was used to collect the data). This worked quite well and
when considering the crystallite morphologies it seems physically
reasonable.

I have also been using TOPAS to refine the some of the data for
comparison and as a new user have not found a way of including this kind
of anisotropic strain into the refinement.

Is it possible? If so does anybody have an example?

Many thanks for your help

Ross Colman

p.s

If it helps in the discussion, I am analysing a crystal structure with P
-3 m 1 symmetry and so the refinable parameters within Fullprof are
s_400, s_004 and s_112. From a chemical point of view the c direction is
only weekly hydrogen bonded and so the laminar structure seen in SEM
should be within the a-b plane.

________________________________

Ross Colman

G19 Christopher Ingold Laboratories

University College London

Department of Chemistry

20 Gordon Street

London

WC1H 0AJ

Phone: +44 (0)20 7679 4636

Internal: 24636

Email:  ross.col...@ucl.ac.uk <mailto:ross.col...@ucl.ac.uk>




--
Dr. Andreas Leineweber
Max-Planck-Institut fuer Metallforschung
Heisenbergstrasse 3
70569 Stuttgart
Germany
Tel. +49 711 689 3365
Fax. +49 711 689 3312
e-mail: a.leinewe...@mf.mpg.de
home page of department: 
http://www.mf.mpg.de/de/abteilungen/mittemeijer/english/index_english.htm


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