The P21/m↔C2/m displacive phase transition in the synthetic end-member amphibole Na NaMg Mg5 Si8 O22 (OH)2 has been studied by monitoring changes in unit-cell parameters and the intensities of superlattice reflections at 25-400 °C. This amphibole allows investigation of the effects of compositional variations at the A- and B-group sites upon the transition. Polynomial fitting of a 24 Landau potential to the evolution of the order parameter with T yielded a Tc of 257 ± 3 °C, and Landau coefficients compatible with a second-order transition. Structure refinement of single-crystal data collected at 25, 140, 270 and 370 °C allowed modelling of the structural changes as a function of T and symmetry. Crystal-chemical analysis suggests that differences in Tc in cummingtonites and in the crystal of this work depend mainly upon the relations between the aggregate ionic radii of the B- and C-group cations.

The P21/M ↔ C2/m phase transition in synthetic amphibole Na NaMg Mg5 Si8 O22 (OH)2 : thermodynamic and crystal-chemical evaluation / F. Cámara, R. Oberti, G. Iezzi, G. Della Ventura. - In: PHYSICS AND CHEMISTRY OF MINERALS. - ISSN 0342-1791. - 30:9(2003 Oct), pp. 570-581.

The P21/M ↔ C2/m phase transition in synthetic amphibole Na NaMg Mg5 Si8 O22 (OH)2 : thermodynamic and crystal-chemical evaluation

F. Cámara
;
2003

Abstract

The P21/m↔C2/m displacive phase transition in the synthetic end-member amphibole Na NaMg Mg5 Si8 O22 (OH)2 has been studied by monitoring changes in unit-cell parameters and the intensities of superlattice reflections at 25-400 °C. This amphibole allows investigation of the effects of compositional variations at the A- and B-group sites upon the transition. Polynomial fitting of a 24 Landau potential to the evolution of the order parameter with T yielded a Tc of 257 ± 3 °C, and Landau coefficients compatible with a second-order transition. Structure refinement of single-crystal data collected at 25, 140, 270 and 370 °C allowed modelling of the structural changes as a function of T and symmetry. Crystal-chemical analysis suggests that differences in Tc in cummingtonites and in the crystal of this work depend mainly upon the relations between the aggregate ionic radii of the B- and C-group cations.
Amphibole; Displacive phase transition; HT-XRD; Synthesis
Settore GEO/06 - Mineralogia
ott-2003
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/477857
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