Re: Powder Diffraction Discussion Group on Facebook

2015-06-09 Thread Roberto R. de Avillez
Indeed I find the list one of my best resources and when I have some 
doubt on a subject, I search the old posts.


Kind regards,
Roberto

Roberto Ribeiro de Avillez
Professor Associado
Dept de Engenharia Química e de Materiais
Pontifícia Universidade Católica do Rio de Janeiro
tel. +55 21 3527 1233

On 06/09/2015 12:34 PM, Alan Hewat wrote:


the Rietveld mailing list is still where the best knowledgeable is


That's encouraging Alan. Thanks. Concerning the number of posts you 
are right - there are fewer now. I would like to think it's because we 
have an archive now, and people profit from past answers rather than 
asking the same questions over again, which used to be common. Or 
perhaps its because there are now more channels of information.


While the number of posts has diminished, the number of members has 
grown continually. There are now more than 1500, but some well known 
names only post when they see a particularly interesting question. 
Whenever there is a good question, we receive good answers.


As for insults, I thought Radovan's cleavage between Troglodytes and 
Tweeters was quite amusing. And every time we have a little 
controversy, we get new members.


One shouldn't assume that because fewer people post, there are fewer 
people interested. But certainly prepare a graph if you wish. Just 
don't post it to all 1500+ members :-)


Kind regards, Alan.
__
*   Dr Alan Hewat, NeutronOptics, Grenoble, FRANCE *
alan.he...@neutronoptics.com +33.476.98.41.68
http://www.NeutronOptics.com/hewat
__


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Re: on high pressure data indexing and unit cell reduction

2014-03-03 Thread Roberto R. de Avillez
Cell conversion may be done with the programs provided by Bilbao 
Crystallography Server (http://www.cryst.ehu.es/). Consider using the 
programs:

GENPOS and CELLTRAN.

On 03/03/2014 05:55 PM, Young, Lindsay wrote:


Hello all - I've gotten stuck at a point in my data refinement, I'd 
appreciate it if someone has any suggestions for me.



I have been trying to index high pressure data. It was collected using 
a diamond anvil cell with a 2d detector. I integrated the data on GSAS 
II, using the penetration correction. I opened this data on Jade to do 
peak fitting, and indexed the resulting peak list in Topas. I managed 
to get a reasonable monoclinic cell - but it is not in standard cell 
notation - the angle for beta is 142 degrees, and I would like see 
this cell represented such that is between 90 and 130 degrees.



I tried indexing this peak list in Treor and Dicvol, with no 
results. I then tried putting the unit cell from Topas into hklgen, 
taking the peaks it generated (which do match those in the pattern), 
and indexing them with Treor and Dicvol, but neither program turns out 
any results. I did tweak the standard settings of both programs to try 
to get results, but this was not successful.



The idea is, if we can get the same result in another program as we 
did in Topas, it could further show that the result is correct.



Does anyone know how I can convert this cell? Is there a unit cell 
reduction program I could use? If you need any additional information 
please let me know!




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Re: TOPAS full axial model

2010-02-15 Thread Roberto R. de Avillez

Hi Lukasz,

You are talking about fundamental parameters approach to Rietveld as 
proposed by Alan Coelho (CHEARY, R. W. e COELHO A., J. Appl. Cryst.,31, 
1998, 851-861. ) The sample length is the length of the sample measured 
in the axial direction (in mm). It is the illuminated area, so it must 
depend on the source length if you consider the axial divergence. I 
usually fit all the fundamental parameters using a diffraction from a 
standard sample and making restrictions for the allowed variations. Then 
I use the fitted values as the instrument parameters for my samples that 
use the same geometric arrangement.


Best regards,
Roberto de Avillez

Łukasz Kruszewski escreveu:

Hello to all!
My name's Lukasz Kruszewski, my interest recently is the mineralogy of 
burning coal dumps. I'm trying to obtain the unit cell parameters of 
some members of the alunite group, analysed on Bruker D5005 
diffractometer (Co Ka, Bragg-Brentano, RS = 0.6mm wide, FDS = 1 deg.) 
with use for an article. I pack powdered samples as thin layer on a 
glass slide with limiters. I would like to kindly ask for help in 
understanding well the FULL AXIAL MODEL in the INSTRUMENT section of 
TOPAS program. I know that the SOURCE LENGTH, SAMPLE LENGTH and RS 
length should be FIXED, but I don't know actually does the SAMPLE 
LENGHT means. Do I understand well that its the length of the beam 
focusation area only, or the whole length of the glass slide, or the 
'working' distance between source and detector?

I would be grateful for any tips (-:
With best regards,
Lukasz Kruszewski
Instutite of Geochemistry, Mineralogy and Petrology
Faculty of Geology
University of Warsaw


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--
Roberto Ribeiro de Avillez
Professor Associado
Pontifícia Universidade Católica
Dept Engenharia de Materiais
tel. 55+ 21+ 3527 1250
e-mail: avil...@puc-rio.br



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