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Elasticity of (Mg,Fe)SiO3-Perovskite at high pressures

Kiefer, B; Stixrude, L; Wentzcovitch, RM; (2002) Elasticity of (Mg,Fe)SiO3-Perovskite at high pressures. Geophysical Research Letters , 29 (11) , Article 1539. 10.1029/2002GL014683. Green open access

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Abstract

[1] We calculated the elasticity of (Mg,Fe)SiO3-perovskite, using the plane-wave pseudopotential method for a pressure range that encompasses the earth's lower mantle. Adding 25 mol% FeSiO3 to the Mg endmember decreases the shear modulus by 6% at zero pressure and by 8% at core mantle boundary pressures. The bulk modulus is less affected by iron, increasing by 2% at zero pressure and by 1% at the base of the mantle. For the isotropically averaged wave velocities we find that the compressional wave velocity decreases by 4% independent of pressure and the shear wave velocity decreases by 6% and 7% at zero pressure and at 136 GPa, repectively. For the relative variation of shear to compressional velocities at constant pressure due to variations in Fe-content we find R = 1.6 at 136 GPa and for the relative variation of shear to bulk sound velocities we find xi = 2.6 at 136 GPa.

Type: Article
Title: Elasticity of (Mg,Fe)SiO3-Perovskite at high pressures
Open access status: An open access version is available from UCL Discovery
DOI: 10.1029/2002GL014683
Publisher version: http://dx.doi.org/10.1029/2002GL014683
Language: English
Additional information: Copyright 2002 by the American Geophysical Union
Keywords: Total-energy calculations, Wave basis-set, MgSiO3 perovskite, Lower mantle, Earths mantle, Crystal-structure, Silicate perovskite, Seismic velocities, Thermal-expansion, State
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
URI: https://discovery.ucl.ac.uk/id/eprint/112632
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