High‐pressure elastic properties of major materials of Earth's mantle from first principles
By Bijaya B. Karki, L. Stixrude, Renata M. Wentzcovitch. 2001
276 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/4d9a3d46c6b3063a2ccbaaffd632809bda68df55
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In Geophysics
- S. Karato
- L. Stixrude
- C. Lithgow‐Bertelloni
- T. Tsuchiya
- K. Umemoto
- J. Tsuchiya
- Renata M. Wentzcovitch
- K. Hirose
Citations in the corpus
- Rheology of the Earth's mantle: A historical review (2010, methodology): “In particular, so-called first-principle calculation has been applied to many properties including Gibbs free energy (stability of various phases) and elastic constants with great success (e.g., Karki et al., 2001; Stixrude et al., 1998; Tsuchiya et al., 2004).”
- Geophysics of Chemical Heterogeneity in the Mantle (2012, background): “The Voigt and Reuss bounds place limits on the maximum amount of shape-preferred anisotropy in subsolidus mantle to values that are small compared with that expected from lattice-preferred orientation (Karki et al. 2001).”
- Quantum‐mechanical condensed matter simulations with CRYSTAL (2018, methodology): “The three acoustic wave velocities can be labeled as quasi-longitudinal vp (P mode), slow quasi-transverse vs1 (slow S mode) and fast quasi-transverse vs2 (fast S mode), depending on the polarization direction û with respect to wave-vector q̂ (Karki et al., 2001).”
- Thermodynamics of mantle minerals – I. Physical properties (2005, background): “The convergence of the Eulerian expansion for the elastic constants may be understood in a similar way (Karki et al. 2001).”
- Thermodynamics, structure, dynamics, and freezing of Mg2SiO4 liquid at high pressure (2008, unknown): “where PS is the static pressure of the fully relaxed structure of forsterite computed with a 2 � 2 � 2 Monkhorst Pack kpoint mesh, and 600 eV as has been found in previous studies to yield fully converged results ( Karki et al., 2001 ).”
- Elasticity of post‐perovskite MgSiO3 (2004, methodology): “The full elastic constant tensor of this orthorhombic structure with nine independent components was calculated using stress-strain relations [Karki et al., 2001].”