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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Ab initio calculations of the elasticity of iron and iron alloys at inner core conditions: Evidence for a partially molten inner core?
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Ab initio calculations of the elasticity of iron and iron alloys at inner core conditions: Evidence for a partially molten inner core?

机译:内芯条件下铁和铁合金的弹性从头算:内芯部分熔融的证据?

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摘要

Ab initio finite temperature molecular dynamics simulations have been used to calculate the elasticity of hcp-Fe, bcc-Fe, FeS and FeSi at core conditions. The calculated compressional wave velocities are in excellent agreement with the most recent experimental data. However, the calculated shear wave velocities of all phases studied are significantly higher than those inferred from seismology. This discrepancy can only be explained if the inner core is partially molten containing more than similar to 8% liquid. (c) 12006 Elsevier B.V. All rights reserved.
机译:从头开始进行有限温度分子动力学模拟,以计算核心条件下hcp-Fe,bcc-Fe,FeS和FeSi的弹性。计算出的压缩波速度与最新的实验数据非常吻合。然而,所研究的所有相的计算的剪切波速度都显着高于地震学推断的剪切波速度。仅当内芯部分熔融且包含的液体含量超过8%时,才能解释这种差异。 (c)12006 Elsevier B.V.保留所有权利。

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