The particle-in-cell model for ab initio thermodynamics:: implications for the elastic anisotropy of the Earth's inner core

被引:84
作者
Gannarelli, CMS
Alfè, D
Gillan, MJ
机构
[1] UCL, Phys & Astron Dept, London WC1E 6BT, England
[2] UCL, Res Sch Geol & Geophys Sci, London WC1E 6BT, England
关键词
ab initio; anisotropy; core; thermodynamics; TOTAL-ENERGY CALCULATIONS; GRUNEISEN-PARAMETER; IRON; TEMPERATURES; PRESSURES; CONSTANTS; DYNAMICS; CLUSTER; PHYSICS; METALS;
D O I
10.1016/j.pepi.2003.09.001
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 assess the quantitative accuracy of the particle-in-cell (PIC) approximation used in recent ab initio predictions of the thermodynamic properties of hexagonal-close-packed (hcp) iron at the conditions of the Earth's inner core. The assessment is made by comparing PIC predictions for a range of thermodynamic properties with the results of more exact calculations that avoid the PIC approximation. It is shown that PIC gives very accurate results for some properties, but that it gives an unreliable treatment of anharmonic lattice vibrations. In addition, our assessment does not support recent PIC-based predictions that the hexagonal c/a ratio increases strongly with increasing temperature, and we point out that this casts doubt on a proposed re-interpretation of the elastic anisotropy of the inner core. (C) 2003 Elsevier B.V. All rights reserved.
引用
收藏
页码:243 / 253
页数:11
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