Title
First-principles determination of elastic anisotropy and wave velocities of MgO at lower mantle conditions
Document Type
Article
Publication Date
11-26-1999
Abstract
The individual elastic constants of magnesium oxide (MgO) have been determined throughout Earth's lower mantle (LM) pressure-temperature regime with density functional perturbation theory. It is shown that temperature effects on seismic observables (density, velocities, and anisotropy) are monotonically suppressed with increasing pressure. Therefore, at realistic LM conditions, the isotropic wave velocities of MgO remain comparable to seismic velocities, as previously noticed in a thermal high-pressure calculations. Also, the predicted strong pressure-induced anisotropy is preserved toward the bottom of the LM, so lattice-preferred orientations in MgO may contribute substantially to the observed seismic anisotropy in the D'' layer.
Publication Source (Journal or Book title)
Science
First Page
1705
Last Page
1707
Recommended Citation
Karki, B., Wentzcovitch, R., De Gironcoli, S., & Baroni, S. (1999). First-principles determination of elastic anisotropy and wave velocities of MgO at lower mantle conditions. Science, 286 (5445), 1705-1707. https://doi.org/10.1126/science.286.5445.1705