Ab Initio Molecular Dynamic Simulation on the Elasticity of Mg_3Al_2Si_3O_(12) Pyrope
Ab Initio Molecular Dynamic Simulation on the Elasticity of Mg_3Al_2Si_3O_(12) Pyrope作者机构:Mineral Physics Institute Department of Geosciences University of New York at Stony Brook Stony Brook NY 11790 USA Department of Earth Sciences University College London Gower Street London WC1E6BT UK
出 版 物:《Journal of Earth Science》 (地球科学学刊(英文版))
年 卷 期:2011年第22卷第2期
页 面:169-175页
核心收录:
学科分类:081704[工学-应用化学] 07[理学] 070304[理学-物理化学(含∶化学物理)] 070205[理学-凝聚态物理] 08[工学] 0817[工学-化学工程与技术] 0703[理学-化学] 0702[理学-物理学]
基 金:supported by the US NSF (No. EAR0809397) NERC (Nos. NER/T/S/2001/00855, NER/O/S/2001/01227) computer facilities provided by NERC at University College London the UK National Supercomputing Service (Hec-tor)
主 题:AIMD thermo-elasticity pyrope high pressure.
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,K0=159.5 GPa,K0'=4.3,V0=785.89 A3,Grüneisen parameter,γ0=1.15,q=0.80,Anderson Grüneisen parameter δT=3.76 and thermal expansion,α0=2.93×10^-5 K^-*** to room temperature,where V0=750.80 A3,γ0 and α0 become 1.11 and 2.47×10^-5 K^-*** elastic properties of pyrope are found to be nearly isotropic at transition zone conditions.