Shock Melting Curve of Iron: A Consensus on the Temperature at the Earth's Inner Core Boundary-Reference-Cited by-同舟云学术

Shock Melting Curve of Iron: A Consensus on the Temperature at the Earth's Inner Core Boundary

Published:2020-08-07 Issue:15 Volume:47 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Li Jun¹,Wu Qiang¹,Li Jiabo¹,Xue Tao¹,Tan Ye¹,Zhou Xianming¹^ORCID,Zhang Youjun²³^ORCID,Xiong Zhengwei⁴,Gao Zhipeng¹⁴,Sekine Toshimori³

Affiliation:

1. National Key Laboratory for Shock Wave and Detonation Physics Institute of Fluid Physics, China Academy of Engineering Physics Mianyang China

2. Institute of Atomic and Molecular Physics Sichuan University Chengdu China

3. Center for High Pressure Science and Technology Advanced Research Shanghai China

4. Joint Laboratory for Extreme Conditions Matter Properties Southwest University of Science and Technology and Research Center of Laser Fusion Mianyang China

Funder

National Key Laboratory of Shockwave and Detonation Physics

National Natural Science Foundation of China

Science Challenge Project

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL087758

Reference66 articles.

1. Temperature of the inner-core boundary of the Earth: Melting of iron at high pressure from first-principles coexistence simulations

2. Iron under Earth’s core conditions: Liquid-state thermodynamics and high-pressure melting curve fromab initiocalculations

3. Another look at the core density deficit of Earth’s outer core

4. Shock temperature and melting in iron sulfides at core pressures

5. Thermal conductivity and heat capacity of single-crystal LiF and CaF2under hydrostatic pressure

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