THE IMPROPER FERROELASTIC PHASE-TRANSITION OF LETOVICITE, (NH4)(3)H(SO4)(2) - AN OPTICAL BIREFRINGENCE, X-RAY-DIFFRACTION AND RAMAN-SPECTROSCOPIC STUDY

Citation
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
Citations number
32
Categorie Soggetti
Crystallography,"Physics, Condensed Matter
Journal title
ISSN journal
01411594
Volume
59
Issue
1-3
Year of publication
1996
Part
B
Pages
61 - 76
Database
ISI
SICI code
0141-1594(1996)59:1-3<61:TIFPOL>2.0.ZU;2-F
Abstract
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.