Abstract
(TMA)2[OsF6] has at room temperature a rhombohedral structure (space group R3̄) which is pseudo-cubic (K2[PtCl6]-type). a=8.0565(6) Å, c = 20.020(3) Å (hexagonal setting). Double refraction decreases linearly with increasing temperature and disappears above 434 K which indicates cubic symmetry of the high temperature phase. The change from the cubic high temperature structure to the rhombohedral structure is characterized by a ferrorotative tilt of the [OsF6] octahedra and the TMA tetrahedra. Evidence of ferroelasticity follows from the switching of the trigonal c-axis by the application of directional pressure. The phase transitions of (TMA)2[OsF6] (Fm3̄m → R3̄) and of the recently reported (TMA)2[PtF6] and (TMA)2[IrF6] (Fm3̄m → I4/m) are described by Landau’s theory.
Item Type: | Journal article |
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Faculties: | Geosciences > Department of Earth and Environmental Sciences > Crystallography and Materials Science |
Subjects: | 500 Science > 550 Earth sciences and geology |
Language: | English |
Item ID: | 18460 |
Date Deposited: | 10. Mar 2014, 14:08 |
Last Modified: | 04. Nov 2020, 13:00 |