Cristobalite-Related Phases in the KAlO2–KAlSiO4 System
A study of the K-rich end of the potassium aluminate–silica system (K1−xAl1−xSixO2; 0≤x≤0.25) at temperatures up to 1500°C has confirmed the existence of a cubic cristobalite-type solid solution extending to x≈0.235 at 1500°C. The end member, KAlO2, transforms on cooling to an orthorhombic KGaO2-typ...
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Published in | Journal of solid state chemistry Vol. 147; no. 2; pp. 624 - 630 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
San Diego, CA
Elsevier Inc
01.11.1999
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | A study of the K-rich end of the potassium aluminate–silica system (K1−xAl1−xSixO2; 0≤x≤0.25) at temperatures up to 1500°C has confirmed the existence of a cubic cristobalite-type solid solution extending to x≈0.235 at 1500°C. The end member, KAlO2, transforms on cooling to an orthorhombic KGaO2-type structure at 531°C (orthorhombic Pbca: a=5.4327(8), b=10.924(2), c=15.469(2) Å, Z=16). The room temperature structure has been modeled using chemically restrained refinement of Guinier-Hägg X-ray powder diffraction (XRD) data by the Rietveld method (reduced χ2=0.074, wRp=0.065, Rp=0.049). With progressive substitution of SiO2 into KAlO2 the cubic-to-orthorhombic phase transition temperature is lowered. A new cristobalite-related phase field has been identified as existing close to room temperature between x≈0.10 and 0.125. The XRD data for this phase can be indexed to a tetragonal superstructure with ar=2√2ap and cr=2cp (r=resultant, p=parent). Analysis of K-rich specimens by XRD and differential scanning calorimetry required extreme care to avoid rapid degradation by atmospheric moisture. |
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Bibliography: | ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 |
ISSN: | 0022-4596 1095-726X |
DOI: | 10.1006/jssc.1999.8426 |