Mg2SiO4 liquid under high pressure from molecular dynamics

被引:48
作者
Adjaoud, Omar [1 ]
Steinle-Neumann, G. [1 ]
Jahn, Sandro [2 ]
机构
[1] Univ Bayreuth, Bayer Geoinst, D-95440 Bayreuth, Germany
[2] Geoforschungszentrum Potsdam, Dept 4, D-14473 Potsdam, Germany
关键词
Mg2SiO4; Melt structure; High pressure; High temperature; Thermodynamics; Diffusivity; Viscosity;
D O I
10.1016/j.chemgeo.2008.06.031
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We use a flexible potential model to perform large-scale molecular dynamics simulations of Mg2SiO4 melt up to pressures of 24GPa and at temperatures between 2390K and 3200K. We find that thermal pressure and the Gruneisen parameter gamma increase linearly with density, independent on temperature. gamma increases from 0.5 at ambient pressure to 0.75 at 24CPa. While Si stays overwhelmingly in tetrahedral coordination, the coordination of Mg increases significantly under compression, from an average 5-fold coordination at room pressure to 7-fold Coordination at 24GPa. Medium range order in Mg2SiO4 as expressed by X-ray and neutron structure factors change considerably with pressure, with features at low wave-vectors q sharpening considerably and shifting to higher q. Diffusivity of the atomic species in Mg2SiO4 decrease uniformly with pressure and are well described by an Arrhenius law. For viscosity eta we find good agreement with experiments at room pressure, and predict a rapid increase with pressure. (c) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:185 / 192
页数:8
相关论文
共 57 条
[1]   Thermal and chemical evolution of the terrestrial magma ocean [J].
Abe, Y .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1997, 100 (1-4) :27-39
[2]   Anomalous size dependence in the melting temperatures of free sodium clusters:: An explanation for the calorimetry experiments -: art. no. 233401 [J].
Aguado, A ;
López, JM .
PHYSICAL REVIEW LETTERS, 2005, 94 (23)
[3]   Multipoles and interaction potentials in ionic materials from planewave-DFT calculations [J].
Aguado, A ;
Bernasconi, L ;
Jahn, S ;
Madden, PA .
FARADAY DISCUSSIONS, 2003, 124 :171-184
[4]  
Allen M. P., 2009, Computer Simulation of Liquids
[5]   Effect of structural transitions on properties of high-pressure silicate melts:: 27Al NMR, glass densities, and melt viscosities [J].
Allwardt, Jeffrey R. ;
Stebbins, Jonathan F. ;
Terasaki, Hidenori ;
Du, Lin-Shu ;
Frost, Daniel J. ;
Withers, Anthony C. ;
Hirschmann, Marc M. ;
Suzuki, Akio ;
Ohtani, Eiji .
AMERICAN MINERALOGIST, 2007, 92 (07) :1093-1104
[6]   SELF-DIFFUSION IN MG2SIO4 (FORSTERITE) AT HIGH-TEMPERATURE - A MODEL CASE-STUDY FOR SIMS ANALYSES ON CERAMIC SURFACES [J].
ANDERSSON, K ;
BORCHARDT, G ;
SCHERRER, S ;
WEBER, S .
FRESENIUS ZEITSCHRIFT FUR ANALYTISCHE CHEMIE, 1989, 333 (4-5) :383-385
[7]   High-pressure melting of MgSiO3 -: art. no. 195701 [J].
Belonoshko, AB ;
Skorodumova, NV ;
Rosengren, A ;
Ahuja, R ;
Johansson, B ;
Burakovsky, L ;
Preston, DL .
PHYSICAL REVIEW LETTERS, 2005, 94 (19)
[8]   ELASTICITY AND CONSTITUTION OF THE EARTH INTERIOR [J].
BIRCH, F .
JOURNAL OF GEOPHYSICAL RESEARCH, 1952, 57 (02) :227-286
[9]   ON THE ISOTHERMAL COMPRESSIBILITY OF SILICATE LIQUIDS AT HIGH-PRESSURE [J].
BOTTINGA, Y .
EARTH AND PLANETARY SCIENCE LETTERS, 1985, 74 (04) :350-360
[10]  
Bowen NL, 1914, AM J SCI, V37, P487