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Chemistry and Mineralogy of Earth’s Mantle. Hexagonal Na0.41[Na0.125Mg0.79Al0.085]2[Al0.79Si0.21]6O12 (NAL phase): Crystal structure refinement and elasticity
-
Martha G. Pamato
,
Alexander Kurnosov
Veröffentlicht/Copyright:
12. August 2014
Abstract
At lower mantle conditions, subducted mid oceanic ridge basalts (MORB) will crystallize more than 20 vol% of an aluminum-rich phase, which is referred to generally as the new aluminum (NAL) phase. Given that a significant proportion of the lower mantle may be comprised of subducted crust, the NAL phase may contribute to the bulk elastic properties of the lower mantle. In this study we report for the first time the structure, Raman spectrum and elasticity of single crystals of Na0.41 [Na0.125Mg0.79Al0.085]2[Al0.79 Si0.21]6O12 NAL phase, synthesized at 2260 °C and 20 GPa. The single-crystal structure refinement of NAL, which is consistent with the space group P63/m, reveals dynamic disorder of Na atoms along channels within the structure. The elastic tensor was experimentally determined at ambient conditions by Brillouin scattering spectroscopy. The elastic modulii obtained from the Voigt- Reuss-Hill approximation using the elastic constants determined in this study are KS = 206 GPa and μ = 129 GPa, whereas the isotropic compressional and shear sound velocities are vP = 9.9 km/s and vS = 5.8 km/s. The NAL phase is elastically anisotropic, displaying 13.9% compressional and shear wave anisotropy. Elastic constants as well as Raman active modes of NAL have also been calculated using density-functional theory and density-functional perturbation theory.
Keywords: NAL phase; Brillouin spectroscopy; single-crystal X-ray diffraction; lower mantle; elasticity
Published Online: 2014-8-12
Published in Print: 2014-8-1
© 2014 by Walter de Gruyter Berlin/Boston
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Schlagwörter für diesen Artikel
NAL phase;
Brillouin spectroscopy;
single-crystal X-ray diffraction;
lower mantle;
elasticity
Artikel in diesem Heft
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- Chemistry and Mineralogy of Earth’s Mantle. Evidence for multiple diamondite-forming events in the mantle
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