Ab initio molecular dynamic simulation on the elasticity of Mg3Al2Si3O12 pyrope

被引:11
作者
Li, Li [1 ]
Weidner, Donald J. [1 ]
Brodholt, John [2 ]
Alfe, Dario [2 ]
Price, G. David [2 ]
机构
[1] SUNY Stony Brook, Dept Geosci, Inst Mineral Phys, Stony Brook, NY 11790 USA
[2] UCL, Dept Earth Sci, London WC1E 6BT, England
基金
英国工程与自然科学研究理事会; 美国国家科学基金会;
关键词
AIMD; thermo-elasticity; pyrope; high pressure; SINGLE-CRYSTAL ELASTICITY; TOTAL-ENERGY CALCULATIONS; EQUATION-OF-STATE; HIGH-PRESSURE; THERMAL EQUATION; WAVE VELOCITIES; PEROVSKITE; GARNET; EARTH; GPA;
D O I
10.1007/s12583-011-0169-6
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We calculated thermo-elastic properties of pyrope (Mg3Al2Si3O12) at mantle pressures and temperatures using Ab initio molecular dynamic simulation. A third-order Birch-Murnaghan equation at a reference temperature of 2 000 K fits the calculations with bulk modulus, K (0)=159.5 GPa, K (0)'=4.3, V (0)=785.89 (3), Gruneisen parameter, gamma (0)=1.15, q=0.80, Anderson Gruneisen parameter delta (T) =3.76 and thermal expansion, alpha (0)=2.93x10(-5) K-1. Referenced to room temperature, where V (0)=750.80 (3), gamma (0) and alpha (0) become 1.11 and 2.47x10(-5) K-1. The elastic properties of pyrope are found to be nearly isotropic at transition zone conditions.
引用
收藏
页码:169 / 175
页数:7
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