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Updated: Aug 6, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
Radial gradient of superionic hydrogen in the Earth's inner core
Zepeng Wu1, Liangrui Wei1, Chen Gao1
1Department of Physics, Xiamen University, Xiamen 361005, China.
Hydrogen
Area of Science:
- Geophysics and geochemistry
- Materials science
- Computational physics
Background:
- Hydrogen is a crucial light element in Earth's core.
- The thermodynamics of hydrogen's superionic phase and its distribution in the inner core are not well understood.
Purpose of the Study:
- To compute ab initio Gibbs free energies for liquid and superionic hcp and bcc Fe-H phases.
- To construct the superionic-liquid phase diagram under Earth's inner core conditions.
- To investigate the distribution and thermodynamic behavior of hydrogen in the inner core.
Main Methods:
- Ab initio calculations of Gibbs free energies for Fe-H phases.
- Construction of the superionic-liquid phase diagram.
- Application of thermochemical constraints.
Main Results:
- Phase diagrams collapse when temperatures are scaled by iron's melting point, indicating pressure-weak sensitivity.
- A scaling relation reconciles theoretical discrepancies and matches low-pressure experimental data.
- A radial hydrogen gradient within the inner core was revealed.
Conclusions:
- Compositional gradients of superionic hydrogen arise naturally from equilibrium thermodynamics.
- A general mechanism for depth-dependent light element distribution in Earth's inner core is suggested.
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