Startseite The influence of Al2O3 on the structural properties of MgSiO3 akimotoite
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The influence of Al2O3 on the structural properties of MgSiO3 akimotoite

  • Nicki C. Siersch , Giacomo Criniti ORCID logo , Alexander Kurnosov , Tiziana Boffa Ballaran , Zhaodong Liu ORCID logo , Takayuki Ishii , Daniel J. Frost ORCID logo , Tony Yu und Yanbin Wang
Veröffentlicht/Copyright: 3. Januar 2023
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Abstract

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 afect 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 difraction 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 stifer 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.

Funding statement: This study was supported by DFG grants FR1555/11 and KU3447/1. Portions of this work were performed at GeoSoilEnviroCARS (The University of Chicago, Sector 13), Advanced Photon Source (APS), Argonne National Laboratory. Geo-SoilEnviroCARS is supported by the National Science Foundation–Earth Sciences (EAR-1634415) and Department of Energy, GeoSciences (DE-FG02-94ER14466). This research used resources of the Advanced Photon Source, a U.S. Department of Energy (DOE) Office of Science User Facility operated for the DOE Office of Science by Argonne National Laboratory under Contract No. DE-AC02-06CH11357.

Acknowledgments

The authors thank Hubert Schulze and Raphael Njul for the preparation of the samples and Leonid Dubrovinsky for his assistance with the Bruker IμS Inside diffractometer. We thank Irene Landi for her help with some aspects of the data collection. We appreciate comments by Masaki Akaogi and Oliver Tschauner that significantly improved the manuscript.

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Received: 2021-08-17
Accepted: 2021-12-22
Published Online: 2023-01-03
Published in Print: 2023-01-27

© 2023 Mineralogical Society of America

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