Numéro |
J. Phys. III France
Volume 5, Numéro 11, November 1995
|
|
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Page(s) | 1809 - 1832 | |
DOI | https://doi.org/10.1051/jp3:1995228 |
J. Phys. III France 5 (1995) 1809-1832
Lattice Defects and Mechanical Behaviour of Quartz SiO 2
J. C. DoukhanLaboratoire Structure et Propriétés de l'Etat Solide, (associated CNRS 234), Université Sciences et Technologies de Lille, 59655 Villeneuve d'Ascq cedex, France
(Received 16 June 1995, accepted 28 July 1995)
Abstract
Quartz has the chemical composition SiO
2. It is an abundant mineral in the Earth crust and its mechanical properties govern the rheological behaviour of a number
of crustal rocks. Quartz is also a material widely used in industry (resonators, filters ...) owing to its remarkable piezoelectric
properties. Very small amounts of water in the quartz lattice dramatically affect its mechanical properties. The mechanical
strength of "wet" quartz is at least 10 times lower than that of "dry" quartz. This effect of water on quartz has been called
hydrolytic weakening. The piezoelectric performances of resonators are also dramatically reduced by the presence of amounts
of water as small as
at. ppm. In order to get better performances, crystal growers have investigated the grown-in lattice defects (dislocations,
twins, occurrence of water and other chemical impurities) and their influence on piezoelectric performances. The community
of mineral physicists have also investigated the lattice defects in quartz, especially dislocations, and the physical factors
influencing their mobility. They have also investigated the behaviour of quartz under extreme dynamic pressure; this situation
corresponds to shock waves generated by the impact of meteorites on the Earth's surface. The aim of this article is to review
the mechanical behaviour of quartz under various thermomechanical conditions and the role of the impurity "water" on the relevant
physical properties of quartz.
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