Quartz: structural and thermodynamic analyses across the α ↔ β transition with origin of negative thermal expansion (NTE) in β quartz and calcite
The temperature variation, T, of the crystal structure of quartz, SiO2, from 298 to 1235 K was obtained with synchrotron powder X‐ray diffraction data and Rietveld structure refinements. The polymorphic transformation from P3221 (low‐T, α quartz) to P6222 (high‐T, β quartz) occurs at a transition te...
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Veröffentlicht in: | Acta crystallographica Section B, Structural science, crystal engineering and materials Structural science, crystal engineering and materials, 2016-04, Vol.72 (2), p.249-262 |
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