|
|
|
|||||||||||||||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |

1 Bayerisches Geoinstitut, University of Bayreuth, D-95440, Bayreuth, Germany
2 Laboratory of Crystallography, University of Bayreuth, D-95440, Bayreuth, Germany
3 Dipartimento di Scienze Mineralogiche e Petrologiche, Università di Torino, Via Valperga Caluso 35, I-10125, Torino, Italy
4 Dipartimento di Scienze della Terra, Università di Parma, Parco Area delle Scienze 157/A, 43100 Parma, Italy
5 HASHI Institute for Silicate Science Nishinakanobu, 1-9-25, Shinagawa, Tokyo 142-0054, Japan
6 Institute of Crystallography, University of Technology, Rheinisch-Westfälische 11 Technische Hochschule Aachen, Jägerstrasse 17/19, D-52056 Aachen, Germany
Synthetic NaGaSi2O6-pyroxene, space group C2/c, was investigated at low temperature between 295 to 110 K by X-ray diffraction. The evolution of the unit-cell parameters as a function of temperature does not indicate any structural phase transition down to 110 K. Calculated values for the Debye temperature,
D, and the Grüneisen parameter,
, are 653(39) and 0.84(8) K, respectively, close to those of other pyroxenes. Five complete intensity data collections were performed at 295, 235, 190, 145, and 110 K to investigate the temperature dependence of the crystal structure. The space group remains C2/c down to 110 K, but anomalies were found between 235 and 190 K for the temperature dependencies of the volume and strain of the M1 polyhedron. This anomalous behavior could be related to variations of the Ga-O2(C1,D1) bond length and the O1(A1,B1)-Ga-O2(C1,D1) bond angle. The C2/c-P
phase transition observed in a previous work for NaTiSi2O6 at about 200 K did not occur for NaGaSi2O6 down to the minimum temperature investigated in this work. This is not due to the different ionic radius at M1 site or to a different tetrahedral chain extension between these two compositions but it is likely due to unfilled t2g orbitals, which do not exist in NaGaSi2O6.
Key Words: Clinopyroxene crystal structure X-ray diffraction low temperature
This article has been cited by other articles:
![]() |
K. S. Knight and G. D. Price POWDER NEUTRON-DIFFRACTION STUDIES OF CLINOPYROXENES. I. THE CRYSTAL STRUCTURE AND THERMOELASTIC PROPERTIES OF JADEITE BETWEEN 1.5 AND 270 K Can Mineral, December 1, 2008; 46(6): 1593 - 1622. [Abstract] [Full Text] [PDF] |
||||
![]() |
M. Tribaudino, M. Bruno, G. Iezzi, G. Della Ventura, and I. Margiolaki The thermal behavior of richterite American Mineralogist, October 1, 2008; 93(10): 1659 - 1665. [Abstract] [Full Text] [PDF] |
||||
![]() |
F. Nestola, M. Tribaudino, T. Boffa Ballaran, C. Liebske, and M. Bruno The crystal structure of pyroxenes along the jadeite hedenbergite and jadeite aegirine joins American Mineralogist, August 1, 2007; 92(8-9): 1492 - 1501. [Abstract] [Full Text] [PDF] |
||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |