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Title: Pressure effect on elastic anisotropy of crystals from ab initio simulations: The case of silicate garnets

Journal Article · · Journal of Chemical Physics
DOI:https://doi.org/10.1063/1.4882699· OSTI ID:22420127
;  [1];  [2]
  1. Dipartimento di Chimica and Centre of Excellence NIS (Nanostructured Interfaces and Surfaces), Università di Torino, via Giuria 5, IT-10125 Torino (Italy)
  2. Institut für Elektrochemie, Universität Ulm, D-89081 Ulm (Germany)

A general methodology has been devised and implemented into the solid-state ab initio quantum-mechanical CRYSTAL program for studying the evolution under geophysical pressure of the elastic anisotropy of crystalline materials. This scheme, which fully exploits both translational and point symmetry of the crystal, is developed within the formal frame of one-electron Hamiltonians and atom-centered basis functions. Six silicate garnet end-members, among the most important rock-forming minerals of the Earth's mantle, are considered, whose elastic anisotropy is fully characterized under high hydrostatic compressions, up to 60 GPa. The pressure dependence of azimuthal anisotropy and shear-wave birefringence of seismic wave velocities for these minerals are accurately simulated and compared with available single-crystal measurements.

OSTI ID:
22420127
Journal Information:
Journal of Chemical Physics, Vol. 140, Issue 23; Other Information: (c) 2014 AIP Publishing LLC; Country of input: International Atomic Energy Agency (IAEA); ISSN 0021-9606
Country of Publication:
United States
Language:
English