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Formation of iron-doped mullite (Al 4+2 xSi 2−2 xO 10− x) by temperature- and time-resolved X-ray powder diffraction and EXAFS, and by 27Al MAS NMR spectroscopy

Temperature- and time-resolved X-ray powder diffraction and Fe K-edge EXAFS have been recorded simultaneously using synchrotron radiation during the calcination of a gel prepared by hydrothermally processing a mixture of aluminium-, silicon- and iron-acetates. The results, which are supported by 27A...

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Bibliographic Details
Published in:Polyhedron 1999-02, Vol.18 (7), p.1083-1087
Main Authors: Berry, Frank J, Bilsborrow, Robert L, Dent, Andrew J, Mortimer, Michael, Ponton, Clive B, Purser, Beatrice J, Whittle, Karl R
Format: Article
Language:English
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Summary:Temperature- and time-resolved X-ray powder diffraction and Fe K-edge EXAFS have been recorded simultaneously using synchrotron radiation during the calcination of a gel prepared by hydrothermally processing a mixture of aluminium-, silicon- and iron-acetates. The results, which are supported by 27Al MAS NMR studies, show that iron is initially accommodated in the octahedral sites of a poorly crystalline pseudoboehmite-type structure (γ-AlOOH· n H 2O). At ca. 400°C the material becomes amorphous and a small particle highly defective γ-Al 2O 3-type structure develops as the temperature is increased. No evidence for a discrete crystalline silicon-containing phase is observed. The first evidence of the formation of mullite (Al 2 oct (Al 2+2 x tet Si 2−2 x tet ) O 10− x ) in which iron is accommodated in the octahedral sites is observed on reaching 1050°C. The phase develops as a function of time at this temperature.
ISSN:0277-5387
DOI:10.1016/S0277-5387(98)00398-2