Direct measurement of thermal conductivity in solid iron at planetary core conditions

被引：0

作者：

Zuzana Konôpková

R. Stewart McWilliams

Natalia Gómez-Pérez

Alexander F. Goncharov

机构：

[1] DESY Photon Science,Departamento de Geociencias

[2] School of Physics and Astronomy and Centre for Science at Extreme Conditions,undefined

[3] University of Edinburgh,undefined

[4] Universidad de Los Andes,undefined

[5] Key Laboratory of Materials Physics,undefined

[6] Institute of Solid State Physics,undefined

[7] Chinese Academy of Sciences,undefined

[8] Geophysical Laboratory,undefined

[9] Carnegie Institution of Washington,undefined

[10] †Present address: European XFEL GmbH,undefined

[11] Notkestrasse 85,undefined

[12] DE-22607 Hamburg,undefined

[13] Germany.,undefined

来源：

Nature | 2016年 / 534卷

关键词：

D O I：

暂无

中图分类号：

学科分类号：

摘要：

The thermal conductivity of solid iron at the pressure and temperature conditions that prevail in the cores of planets is measured directly using a dynamically laser-heated diamond-anvil cell, yielding values that support findings from ancient magnetized rocks that suggest Earth’s magnetic field has persisted since the Earth’s earliest history.

引用

页码：99 / 101

页数：2

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