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Mineralogical Magazine; August 2001; v. 65; no. 4; p. 489-507
© 2001 Mineralogical Society of Great Britain and Ireland
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A detailed structural characterization of quartz on heating through the {alpha}–ß phase transition

M. G. Tucker1, D. A. Keen2,{dagger} and M. T. Dove1,*

1 Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK
2 ISIS Faculty, Rutherford Appleton Laboratory, Chilton, Didcot, Oxfordshire OX11 0QX, UK

* E-mail: martin{at}esc.cam.ac.uk

Total neutron scattering measurements, analysed using a modification of the reverse Monte Carlo modelling method to account for long-range crystallographic order, have been used to describe the temperature-dependent behaviour of the structure of quartz. Two key observations are reported. First, the symmetry change associated with the displacive {alpha}–ß phase transition is observed in both the long-range and short-range structural correlations. Secondly, some aspects of the structure, such as the Si–O bond length and the thermally-induced dynamic disorder, the latter of which sets in significantly below the transition, are relatively insensitive to the phase transition. These results are used to show that the {alpha}-domain model of the ß-phase disorder is inappropriate and that the classical soft-mode picture of the phase transition is too simplistic. Instead, it is argued that the structural behaviour is best described in terms of its ability to respond to low-frequency, high-amplitude vibrational modes. This view is supported by additional single-crystal diffuse neutron scattering measurements.

KEYWORDS: structural characterization, quartz, {alpha}–ß transition, total neutron scattering, reverse Monte Carlo modelling




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