An atomistic model of MgSiO3 perovskite and post-perovskite phases

被引:3
|
作者
Pinilla, C. [1 ,2 ]
Acuna-Rojas, M. [1 ]
Seriani, N. [3 ]
Scandolo, S. [3 ,4 ]
机构
[1] Univ Norte, Dept Fis & Geociencias, Km 5 Via Puerto Colombia, Barranquilla, Colombia
[2] UCL, Dept Earth Sci, Gower St, London WC1E 6BT, England
[3] Abdus Salam Int Ctr Theoret Phys, Str Costiera 11, I-34151 Trieste, Italy
[4] INFM Democritos Natl Simulat Ctr, Via Beirut 2-4, I-34014 Trieste, Italy
关键词
MgSiO3; phases; Force fields; Molecular dynamics; Materials at extreme conditions; MOLECULAR-DYNAMICS; ELASTIC PROPERTIES; PRESSURE; POTENTIALS; TEMPERATURE; TRANSITION; DIFFUSION; DEFECTS; DENSITY; SILICA;
D O I
10.1016/j.commatsci.2016.09.032
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
A classical force field for MgSiO3 polymorphs is presented and tested for the perovskite, post-perovskite and enstatite phases. In this force field each ion has a fixed partial charge and a fixed polarizability and the potential energy is minimised with respect to the ions' dipole moments at each step of molecular dynamics by iterating them to self-consistency. The potential parameters are obtained by fitting to forces, stresses and energies calculated by density functional theory. The phase transition from perovskite to post-perovskite is predicted to take place at a pressure of 60 GPa at zero temperature. The potential reproduces well structural and thermodynamic properties as well as defects formation in a wide range of pressures, and therefore will be useful for the investigation of MgSiO3 based materials in a geophysical context. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:351 / 359
页数:9
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