Sat. Redfern et Cmb. Henderson, MONOCLINIC ORTHORHOMBIC PHASE-TRANSITION IN THE K2MGSI5O12 LEUCITE ANALOG, The American mineralogist, 81(3-4), 1996, pp. 369-374
The high-temperature cell parameters of K2MgSi5O12 have been measured
by X-ray powder diffraction between room temperature and 842 K. A firs
t-order ferroelastic phase transition between the room-temperature P2(
1)/c structure and a high-temperature Pbca structure occurs at 622 K.
The spontaneous strain behaves as the order parameter for the transiti
on, following a simple Landau model. Simple lattice dynamics simulatio
n of the magnesiosilicate framework reveals that acoustic mode softeni
ng drives the elastic instability. The first-order character of the tr
ansition is attributed to a large excess volume, which arises from col
lapse of the framework around the alkali site. At higher temperatures
the orthorhombic cell edges converge toward a metrically cubic structu
re, but this transformation requires Mg-Si disorder, which was not obs
erved on the time scale of these experiments.