Models for the amorphization of compressed crystals
- 9 December 1996
- journal article
- Published by IOP Publishing in Journal of Physics: Condensed Matter
- Vol. 8 (50) , 10907-10918
- https://doi.org/10.1088/0953-8984/8/50/017
Abstract
A permanently bonded diamond network, with flexible bond lengths and angles, is characterized by computer simulation and used as the reference state for a perturbation treatment that favours tetrahedral bond angles. At low temperatures the perturbed system has three phases separated by two sets of van der Waals loops. The intermediate-pressure phase is an open crystal which, like ice or quartz, expands when cooled and collapses under pressure to an amorphous solid. Two-dimensional honeycomb networks show the same behaviour.Keywords
This publication has 34 references indexed in Scilit:
- Reversible first-order transition between two H2O amorphs at ∼0.2 GPa and ∼135 KThe Journal of Chemical Physics, 1994
- Mechanical instability in ice I h. A mechanism for pressure-induced amorphizationThe Journal of Chemical Physics, 1992
- Pressure-induced phase transitions in clathrate hydratesThe Journal of Chemical Physics, 1991
- Memory Glass: An Amorphous Material Formed from AlPO 4Science, 1990
- Pressure induced amorphization of ice IhThe Journal of Chemical Physics, 1990
- Pressure-induced amorphization of crystalline silicaNature, 1988
- An apparently first-order transition between two amorphous phases of ice induced by pressureNature, 1985
- ‘Melting ice’ I at 77 K and 10 kbar: a new method of making amorphous solidsNature, 1984
- Synthesis of a perovskite-type polymorph of CaSiO3Earth and Planetary Science Letters, 1975
- Observations on the inversion of Stishovite to silica glassJournal of Geophysical Research, 1963