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The influence of Al₂O₃ on the structural properties of MgSiO₃ akimotoite

Title data

Siersch, Nicki C. ; Criniti, Giacomo ; Kurnosov, Alexander ; Boffa Ballaran, Tiziana ; Liu, Zhaodong ; Ishii, Takayuki ; Frost, Daniel J. ; Yu, Tony ; Wang, Yanbin:
The influence of Al₂O₃ on the structural properties of MgSiO₃ akimotoite.
In: American Mineralogist. Vol. 108 (2023) Issue 1 . - pp. 100-109.
ISSN 1945-3027
DOI: https://doi.org/10.2138/am-2022-8257

Official URL: Volltext

Abstract in another language

Akimotoite, a MgSiO3 polymorph present in the lower transition zone within ultramafic portions of subducting slabs and potentially also in the ambient mantle, will partition some amount of Al, raising the question of how this will affect its crystal structure and properties. In this study, a series of samples along the MgSiO3-Al2O3 (akimotoite-corundum) solid solution have been investigated by means of single-crystal X-ray diffraction to examine their crystal chemistry. Results show a strong nonlinear behavior of the a- and c-axes as a function of Al content, which arises from fundamentally different accommodation mechanisms in the akimotoite and corundum structures. Furthermore, two Al2O3-bearing akimotoite samples were investigated at high pressure to determine the different compression mechanisms associated with Al substitution. Al2O3-bearing akimotoite becomes more compressible at least up to 20 mol% Al2O3, due likely to an increase in compressibility as the Al cation is incorporated into the SiO6 octahedron. This observation is in strong contrast to the stiffer corundum end-member having a KT = 250 GPa, which is larger than that of the akimotoite end-member KT = 205(1) GPa. These findings have implications for mineral physics models of elastic properties, which have in the past assumed linear mixing behavior between the MgSiO3 akimotoite and Al2O3 corundum end-members to calculate sound wave velocities for Al-bearing akimotoite at high pressure and temperature.

Further data

Item Type: Article in a journal
Refereed: Yes
Institutions of the University: Research Institutions > Central research institutes > Bavarian Research Institute of Experimental Geochemistry and Geophysics - BGI
Result of work at the UBT: Yes
DDC Subjects: 500 Science > 550 Earth sciences, geology
Date Deposited: 17 Oct 2024 07:44
Last Modified: 17 Oct 2024 07:44
URI: https://eref.uni-bayreuth.de/id/eprint/90727