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American Mineralogist; July 2000; v. 85; no. 7-8; p. 971-979
© 2000 Mineralogical Society of America
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Phase transitions induced by solid solution in stuffed derivatives of quartz: A powder synchrotron XRD study of the LiAlSiO4-SiO2 join

Hongwu Xu1,*, Peter J. Heaney2 and George H. Beall3

1 Department of Geosciences and Princeton Materials Institute, Princeton University, Princeton, New Jersey 08544, U.S.A.
2 Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, U.S.A.
3 Corning Incorporated, Sullivan Park FR-51, Corning, New York 14831, U.S.A.

The crystal structures of stuffed derivatives of quartz within the Li1–xAl1–xSi1+xO4 system have been refined by Rietveld analysis of powder synchrotron X-ray diffraction (XRD) data. Our results reveal an Al-Si order-disorder transition at x = ~0.3 and a ß-{alpha} displacive transformation at x = ~0.65. Structural variations across the series result from an interplay of three mechanisms: tetrahedral tilting associated with Al-Si order-disorder; Li positional disorder along structural channels parallel to c; and tetrahedral rotation related to the ß-{alpha} transition. At both microscopic (local bonding) and macroscopic (spontaneous strain) scales, the substitution of Li+ and Al3+ for Si4+ closely mimics temperature in its effect on the quartz framework.







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