THE IMPROPER FERROELASTIC PHASE-TRANSITION OF LETOVICITE, (NH4)(3)H(SO4)(2) - AN OPTICAL BIREFRINGENCE, X-RAY-DIFFRACTION AND RAMAN-SPECTROSCOPIC STUDY
L. Schwalowsky et al., THE IMPROPER FERROELASTIC PHASE-TRANSITION OF LETOVICITE, (NH4)(3)H(SO4)(2) - AN OPTICAL BIREFRINGENCE, X-RAY-DIFFRACTION AND RAMAN-SPECTROSCOPIC STUDY, Phase transitions, 59(1-3), 1996, pp. 61-76
The improper ferroelastic phase transition of synthetic letovicite has
been studied using optical birefringence, hard mode Raman spectroscop
y and X-ray diffraction measurements. The critical point is the L-poin
t on the surface of the Brillouin zone of the rhombohedral high-temper
ature phase. The domain pattern of the ferroelastic phase is related t
o the arms of the L-star leading to orientational domains of the speci
es <(3)over bar mF2/m>. The integrated intensity of the A(g)-Raman-mod
e near 483 cm(-1), the thermal evolution of the spontaneous strain and
coupled quantities like the morphic optical birefringence show a rapi
d saturation on approaching the transition point near 413 K. The satur
ation has been fitted using Landau-type free energy expansions with hi
gh power terms of the order parameter. The non-classical thermal varia
tion of the order parameter is compatible with a Slater instability of
infinite order.