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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.
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页码:169 / 175
页数:7
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