Earth's inner core is solid despite extreme high temperatures
Multiple high-pressure ab initio and experimental studies confirm that iron and its alloys remain in a solid phase under the extreme temperatures of Earth's inner core due to immense ambient pressure.
The retrieved papers consistently study iron melting curves, thermodynamics, and seismic velocities at core pressures, providing robust theoretical and experimental backing that iron forms a solid phase at inner core conditions despite extreme temperatures.
D. Alfé, G. D. Price, M. Gillan. Iron under Earth’s core conditions: Liquid-state thermodynamics and high-pressure melting curve from ab initio calculations. 2001. https://doi.org/10.1103/PhysRevB.65.165118
Calculates the thermodynamics and high-pressure melting curves of iron under Earth's core conditions, supporting the understanding of solid iron phases at extreme temperatures.
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Fulun Wu, Shunqing Wu, Caizhuang Wang, Kai-Ming Ho, R. Wentzcovitch, Yang Sun. Melting temperature of iron under the Earth’s inner core condition from deep machine learning. 2024. https://doi.org/10.1016/j.gsf.2024.101925
Uses advanced deep machine learning and ab initio methods to confirm iron's melting behavior and solid phase stability at the extreme temperatures and pressures of the inner core boundary.
Ikuta D, Ohtani E, Fukui H, Sakai T, Ishikawa D, Baron AQR. Sound velocity of hexagonal close-packed iron to the Earth's inner core pressure.. 2022. https://doi.org/10.1038/s41467-022-34789-2
Examines the sound velocities and structural properties of hexagonal close-packed iron under inner-core pressures, affirming its solid nature.
I. Ezenwa, Y. Fei. High Pressure Melting Curve of Fe Determined by Inter‐Metallic Fast Diffusion Technique. 2023. https://doi.org/10.1029/2022GL102006
Investigates the melting temperature of iron under high pressures to establish the thermal profile and boundary conditions where iron solidifies.
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