Rietveld refinement of disordered illite-smectite mixed-layer structures by a recursive algorithm; I, One-dimensional patterns

X-ray diffraction patterns of oriented mounts of clay minerals are often used in clay mineralogy for qualitative and quantitative purposes. Frequently occurring stacking defects, in particular, can be characterized by this technique. Modeling of these diffraction profiles has become an important too...

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Published inClays and clay minerals Vol. 60; no. 5; pp. 507 - 534
Main Authors Ufer, Kristian, Kleeberg, Reinhard, Bergmann, Jörg, Dohrmann, Reiner
Format Journal Article
LanguageEnglish
Published Cham Clay Minerals Society 01.10.2012
The Clay Minerals Society
Springer International Publishing
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Summary:X-ray diffraction patterns of oriented mounts of clay minerals are often used in clay mineralogy for qualitative and quantitative purposes. Frequently occurring stacking defects, in particular, can be characterized by this technique. Modeling of these diffraction profiles has become an important tool in obtaining structural information about the nature of stacking order. Manual matching of calculated and observed patterns is time consuming and user dependent. Automatic refinement procedures are, therefore, desirable. An improved approach for the treatment of disordered layer structures within a Rietveld refinement is presented here. The recursive calculation of structure factors, similar to that of the simulation program DIFFaX, was introduced in the Rietveld code BGMN. Complete implementation is formulated within the interpreter language of the Rietveld code and is transparent as well as flexible. Such a method has opened the application of Rietveld refinement to patterns of oriented mounts where only basal reflections of stacking disordered structures were recorded. The DIFFaX code was used to simulate basal reflections of illite-smectite mixed layers (I-S) with different ratios of illitic and smectitic layers and with different degrees of long-range ordering (Reichweite). Rietveld refinements with these simulated patterns were used to evaluate the application of this new approach. Several I-S with different degrees of ordering were also chosen as tests for the refinement of basal reflections. The samples were prepared as standard air-dried and ethylene glycol-solvated, oriented specimens. Realistic structural parameters were obtained for the composition and ordering of the I-S.
Bibliography:0009-8604(20121001)60:5L.507;1-
(QE) Geology
ObjectType-Article-1
SourceType-Scholarly Journals-1
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content type line 23
ISSN:0009-8604
1552-8367
DOI:10.1346/CCMN.2012.0600507