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...

Full description

Saved in:
Bibliographic Details
Published inJournal of solid state chemistry Vol. 147; no. 2; pp. 624 - 630
Main Authors Husheer, Shamus L.G., Thompson, John G., Melnitchenko, Alexandra
Format Journal Article
LanguageEnglish
Published San Diego, CA Elsevier Inc 01.11.1999
Elsevier
Subjects
Online AccessGet full text

Cover

Loading…
More Information
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.
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