Abstract In situ high pressure X-ray diffraction study was performed on celsian (Cls97Or3) from Jakobsberg, Sweden. A single-crystal of celsian was loaded in an ETH-type diamond anvil cell and unit-cell parameters were measured at 20 different pressures up to 6.0 GPa at room T. The evolution of the unit-cell parameters and volume as a function of pressure shows a discontinuity at P > 5.59 GPa indicating a displacive first-order phase transition. The P-V data were fitted by a second-order Birch-Murnaghan EoS only up to 2.55 GPa, because for P > 2.55 GPa a slight change in the compressional behavior of the unit-cell volume is observed. The resulting EoS coefficients are V0 = 1461.4(1) Å3 and KT0 = 88.1 (6) GPa. A second crystal of celsian was loaded in the DAC cell and single-crystal in situ HP X-ray diffraction was performed at P = 0.0001, 2.1, 4.2, 5.5, 5.9, 6.5 and 7.8 GPa. The data collections between 0 and 5.5 GPa show only a- and b-type reflections confirming the I2/c space group. The appearance of c and d-type reflections at 5.9, 6.5 and 7.8 GPa, the analysis of the systematic absence and the structural refinements define the HP phase transition as an I2/c - P21/c transition. The most significant changes with compression in celsian are the deformation in the Ba polyhedra and the variation in the T-O-T angles.

High-pressure structural configuration and phase transition in celsian, BaAl2Si2O8

CURETTI, Nadia;BENNA, Piera;BRUNO, Emiliano
2017-01-01

Abstract

Abstract In situ high pressure X-ray diffraction study was performed on celsian (Cls97Or3) from Jakobsberg, Sweden. A single-crystal of celsian was loaded in an ETH-type diamond anvil cell and unit-cell parameters were measured at 20 different pressures up to 6.0 GPa at room T. The evolution of the unit-cell parameters and volume as a function of pressure shows a discontinuity at P > 5.59 GPa indicating a displacive first-order phase transition. The P-V data were fitted by a second-order Birch-Murnaghan EoS only up to 2.55 GPa, because for P > 2.55 GPa a slight change in the compressional behavior of the unit-cell volume is observed. The resulting EoS coefficients are V0 = 1461.4(1) Å3 and KT0 = 88.1 (6) GPa. A second crystal of celsian was loaded in the DAC cell and single-crystal in situ HP X-ray diffraction was performed at P = 0.0001, 2.1, 4.2, 5.5, 5.9, 6.5 and 7.8 GPa. The data collections between 0 and 5.5 GPa show only a- and b-type reflections confirming the I2/c space group. The appearance of c and d-type reflections at 5.9, 6.5 and 7.8 GPa, the analysis of the systematic absence and the structural refinements define the HP phase transition as an I2/c - P21/c transition. The most significant changes with compression in celsian are the deformation in the Ba polyhedra and the variation in the T-O-T angles.
2017
44
3
181
192
http://link.springer.de/link/service/journals/00269/index.htm
Celsian; Crystal structure; Equation of state; High-pressure studies; Phase transition; Materials Science (all); Geochemistry and Petrology
Curetti, Nadia; Benna, Piera; Bruno, Emiliano
File in questo prodotto:
File Dimensione Formato  
Celsiana 2016.pdf

Accesso aperto

Descrizione: Articolo principale
Tipo di file: POSTPRINT (VERSIONE FINALE DELL’AUTORE)
Dimensione 858.79 kB
Formato Adobe PDF
858.79 kB Adobe PDF Visualizza/Apri
Benna_Phys Chem Minerals_2017.pdf

Accesso riservato

Tipo di file: PDF EDITORIALE
Dimensione 842.78 kB
Formato Adobe PDF
842.78 kB Adobe PDF   Visualizza/Apri   Richiedi una copia

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2318/1625072
Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus 5
  • ???jsp.display-item.citation.isi??? 4
social impact