Displacive components of the low-temperature phase transitions in lawsonite

Citation
Hw. Meyer et al., Displacive components of the low-temperature phase transitions in lawsonite, AM MINERAL, 86(4), 2001, pp. 566-577
Citations number
19
Categorie Soggetti
Earth Sciences
Journal title
AMERICAN MINERALOGIST
ISSN journal
0003004X → ACNP
Volume
86
Issue
4
Year of publication
2001
Pages
566 - 577
Database
ISI
SICI code
0003-004X(200104)86:4<566:DCOTLP>2.0.ZU;2-8
Abstract
The phase transitions in deuterated lawsonite were investigated with high-r esolution, time-of-flight neutron diffraction between 2 and 500 K. From the analysis of spontaneous strain data, the thermodynamics of the phase trans ition at 273 K are not changed by the deuteration process. Shifts in atomic positions with temperature indicate continuous changes for a framework oxy gen and for one of the deuterium atoms, whereas for the other deuterium ato m, a more discontinuous behavior was observed in the average structure. Com parison of O . . .D and O . . .O bond lengths with IR data from a non-deute rated lawsonite permits a detailed analysis of assignments of O-H stretchin g modes.