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The structure of "orthorhombic" KAlSiO (sub 4) -Ol; evidence for Al-Si order from MAS NMR data combined with Rietveld refinement and electron microscopy

Miguel Gregorkiewitz, Ying Li, Timothy J. White, Ray L. Withers and Isabel Sobrados
The structure of "orthorhombic" KAlSiO (sub 4) -Ol; evidence for Al-Si order from MAS NMR data combined with Rietveld refinement and electron microscopy (in A tribute to Joseph V. Smith (1928-2007), Ross J. Angel (editor), Ian Parsons (editor) and Robert F. Martin (editor))
The Canadian Mineralogist (December 2008) 46 (6): 1511-1526

Abstract

Dry synthesis of KAlSiO (sub 4) at temperatures from 900 to 1500 degrees C yielded products with slightly different powder X-ray-diffraction patterns. "Orthorhombic" K (sub x) Al (sub x) Si (sub 2-x) O (sub 4) -O1 with x nearly equal 1 was obtained as a substantially single phase after heating at 1000 degrees C for one day; we refined its crystal structure from powder X-ray-diffraction data in space group P12 (sub 1) 1 [MM = 158.17 g/mol, a 15.669(2), b 9.057(1), c 8.621(1) Aa, beta 90.16(1) degrees , V 1223.5 Aa (super 3) , Z = 12, D (sub x) = 2.57 g cm (super -3) , R (sub B) = 0.080]. It is composed of a relatively open [AlSiO (sub 4) ] framework that is a topological variant of tridymite (t) having the supercell (s) metric a (sub s) nearly equal 3a (sub t) , b (sub s) nearly equal a (sub t) +2b (sub t) , c (sub s) nearly equal c (sub t) . The space group P12 (sub 1) 1 allows for Al-Si ordering, and refinement of distance-least-squares restrained models, although problematic owing to the pronounced pseudosymmetry, indicates preference for an ordered pattern where Al and Si are distributed on alternating tetrahedra [dSi-O/dAl-O = 1.628(1)/1.719(1) Aa], so that every SiO (sub 4) tetrahedron is coordinated to four AlO (sub 4) tetrahedra and vice versa. The alternating distribution was independently inferred from (super 29) Si and (super 27) Al MAS NMR spectroscopic data, and the framework model obtained from Rietveld refinement with Si on tetrahedron T1 could be used to successfully simulate the observed Si(Al (sub 4) ) doublet peak in the (super 29) Si spectrum. Electron diffraction showed that triple twinning with a rotation of 120 degrees around c of the metrically almost hexagonal P12 (sub 1) 1 cell is ubiquitous and enhances, in the diffraction experiment, the pseudosymmetry inherited from the tridymite subcell. Furthermore, the diffraction aspect of single individuals (P (super *) 2 (sub 1) (super *) ) confirms that the screw axes 2 (sub 1) --and--2 (sub 1) of the orthorhombic supergroup P2 (sub 1) 2 (sub 1) 2 (sub 1) are only approximated.


ISSN: 0008-4476
EISSN: 1499-1276
Coden: CAMIA6
Serial Title: The Canadian Mineralogist
Serial Volume: 46
Serial Issue: 6
Title: The structure of "orthorhombic" KAlSiO (sub 4) -Ol; evidence for Al-Si order from MAS NMR data combined with Rietveld refinement and electron microscopy
Title: A tribute to Joseph V. Smith (1928-2007)
Author(s): Gregorkiewitz, MiguelLi, YingWhite, Timothy J.Withers, Ray L.Sobrados, Isabel
Author(s): Angel, Ross J.editor
Author(s): Parsons, Ianeditor
Author(s): Martin, Robert F.editor
Affiliation: Universita di Siena, Dipartimento di Scienze della Terra, Siena, Italy
Affiliation: Virginia Polytechnic Institute and State University, Blacksburg, VA, United States
Pages: 1511-1526
Published: 200812
Text Language: English
Publisher: Mineralogical Association of Canada, Ottawa, ON, Canada
References: 55
Accession Number: 2009-031296
Categories: Mineralogy of silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 4 tables
Secondary Affiliation: University of Edinburgh, GBR, United KingdomMcGill University, CAN, CanadaNanyang Technological University, SGP, SingaporeAustralian National University, AUS, AustraliaCSIC, Instituto de Ciencia de Materiales, ESP, Spain
Country of Publication: Canada
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, copyright, Mineralogical Association of Canada. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 200917
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