EQUATIONS OF STATE OF CLOSE-PACKED PHASES OF IRON AND THEIR IMPLICATIONS FOR THE EARTHS CORE

被引：7

作者：

MULARGIA, F ^{[1
]}

BOSCHI, E ^{[1
]}

机构：

[1] UNIV BOLOGNA,IST GEOFIS,I-40126 BOLOGNA,ITALY

来源：

PHYSICS OF THE EARTH AND PLANETARY INTERIORS | 1979年 / 18卷 / 01期

关键词：

D O I：

10.1016/0031-9201(79)90151-1

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：

Theoretical equations of state for Fe at high pressures and temperatures are derived from the expression of the free energy written as a sum of the static energy, the harmonic, the anharmonic and the electronic contributions. All the calculations have been performed for the various crystal structures of Fe using different intermolecular potentials, and namely: Lennard-Jones, Morse and Rydberg functions. The available experimental data do not allow a definite choice between them thus leaving open the problem of the composition of the earth's core. © 1979.

引用

页码：13 / 19

页数：7

共 26 条

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[2] EARTH MODEL BASED ON FREE OSCILLATIONS AND BODY WAVES [J].