The empirical PO corrections like March-Dollase or Rietveld-Toraya can correct only for fibre like PO, i.e. symmetrical around one axis. If it is not your case, you can make it fibre like by spinning, if you spin around the PO vector. If not than see J. Appl. Cryst. 28(1995)247-253.

However, there are few other limitations, which are usually completly ignored:

The distribution of crystallites around any pole hkl must be axially symmetrical either, so-called disc- or rod-shape like behavior. No way to do it by spinning ...

Most of implementations of these corrections in the Rietveld codes also assume another condition: The texture axis is parallel (or perpendicular) to the diffraction vector for all measured hkls. This condition is fullfilled only in Bragg-Brentano or Debye-Scherrer geometries.

Surprising that it still works ...


Radovan


Mibeck, Blaise a écrit :
I am learning QPA and am worried about PO.

I wonder why sample spinning isn’t discussed more.

I am luckily able to barrow time on a newer diffractometer with a sample spinner.

Does this reduce PO? Or completely eliminate it? There is a set up variable in GSAS for whether you are spinning the sample – are there guidelines for how many revolutions to spin the sample if you just want to reduce PO?

Thanks to all for there help!!!

Blaise

* * * * * * * * * * * * *

Blaise Mibeck

Research Scientist

Energy & Environmental Research Center

University of North Dakota

15 North 23rd Street, Stop 9018

Grand Forks, ND 58202-9018

Phone: (701) 777-5077

Email: [EMAIL PROTECTED] <mailto:[EMAIL PROTECTED]>

-----Original Message-----
*From:* David L. Bish [mailto:[EMAIL PROTECTED]
*Sent:* Tuesday, October 28, 2008 9:09 AM
*To:* Martin; [EMAIL PROTECTED]; rietveld_l@ill.fr
*Subject:* RE: Quantitative analysis

I agree that it's always best to avoid preferred orientation, but that is easier said than done on a routine basis. I have personally had good luck with the M-D PO correction on many known samples, as long as the PO was not severe.

However, I imagine that Mario's problems are related to microabsorption in this case. Mario, if you can re-measure your data with a Co or Fe tube, it would be a good test of this.

Dave Bish

At 08:51 AM 10/28/2008 -0400, Martin wrote:

Sorry to disagree. Experience tells me otherwise - the March-Dollase correction has nearly always led to poor quant results for me. It most certainly cannot be applied safely. Martin ------------------------------------------ M Vickers
Dept of Chemistry
UCL

------------------------------------------------------------------------


 Subject: Re: Quantitative analysis
 Date: Tue, 28 Oct 2008 02:53:20 -0700
 From: [EMAIL PROTECTED]
 To: Rietveld_l@ill.fr

 Dear Mario,

One more possible problem of applying preferred orientation
corrections in QPA is that not all of them are normalized. For example, the March-Dollase correction is normalized and can be applied safely, but the Rietveld-Toraya correction is inapplicable to QPA as it does not preserve the scale normalization.

 Best regards,
 Leonid

 *******************************************************
 Leonid A. Solovyov
 Institute of Chemistry and Chemical Technology
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 Phone: +7 3912 495663
 Fax: +7 3912 238658
www.icct.ru/eng/content/persons/Sol_LA
<http://www.icct.ru/eng/content/persons/Sol_LA>


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