Back to Search Start Over

Modeling Powder X-Ray Diffraction Patterns of the Clay Minerals Society Kaolinite Standards: Kga-1, Kga-1b, and Kga-2

Authors :
G. M. Walker
Boris A. Sakharov
Victor A. Drits
Douglas K. McCarty
Source :
Clays and Clay Minerals. 64:314-333
Publication Year :
2016
Publisher :
Springer Science and Business Media LLC, 2016.

Abstract

Three kaolinite reference samples identified as KGa-1, KGa-1b, and KGa-2 from the Source Clays Repository of The Clay Mineral Society (CMS) are used widely in diverse fields, but the defect structures have still not been determined with certainty. To solve this problem, powder diffraction patterns of the KGa-1, KGa-1b, and KGa-2 samples were modeled. In a kaolinite layer among three symmetrically independent octahedral sites named as A, B, and C and separated from each other by b /3 along the b parameter, the A and B sites are occupied by Al cations, whereas, the C sites located along the long diagonal of the oblique kaolinite unit cell are vacant. The layer displacement vectors t1 and t2 are related by a pseudo-mirror plane from defect-free 1 T c kaolinite enantiomorphs, whereas, the random interstratification within individual kaolinite crystallites creates right-hand and left-hand layer sub-sequences producing structural disorder. A third layer displacement vector, t , located along the long diagonal of the oblique layer unit cell that contains the vacant octahedral site and coincides with the layer pseudo-mirror plane may exist. Thus, a structural model should be defined by the probability of t 1, t 2, and t layer displacement translations W t 1, W t 2, and W t , respectively, determined by simulated experimental X-ray diffraction (XRD) patterns. X-ray diffraction patterns were calculated for structures with a given content of randomly interstratified displacement vectors, and other XRD patterns were calculated for a physical mixture of crystallites having contrasting structural order with only C-vacant layers. The samples differ from each other by the content of high- and low-ordered phases referred to as HOK and LOK. The HOK phase has an almost defect-free structure in which 97% of the layer pairs are related by just the layer displacement vector t 1 and only 3% of the layer pairs form the enantiomorphic fragments. In contrast, the LOK phases in the KGa-1, KGa-1b, and KGa-2 samples differ from HOK phases by the occurrence probabilities for the t 1, t 2, and t layer displacements. In addition, the LOK phases contain stacking faults that displace adjacent layers in arbitrary lengths and directions. Low XRD profile factors (Rp = 8–11%) support the defect structure models. Additional structural defects and previously published models are discussed.

Details

ISSN :
15528367 and 00098604
Volume :
64
Database :
OpenAIRE
Journal :
Clays and Clay Minerals
Accession number :
edsair.doi...........8a5b6f09f690cb5fe8ec6685e68fd8b0
Full Text :
https://doi.org/10.1346/ccmn.2016.0640307