Melting Temperature of Iron Under the Earth's Inner Core Condition from Deep Machine Learning

Fuente: arXiv
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Main Authors: Wu, Fulun, Wang, Cai-Zhuang, Ho, Kai-Ming, Wu, Shunqing, Wentzcovitch, Renata M., Sun, Yang
Format: Preprint
Published: 2024
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author Wu, Fulun
Wang, Cai-Zhuang
Ho, Kai-Ming
Wu, Shunqing
Wentzcovitch, Renata M.
Sun, Yang
author_facet Wu, Fulun
Wang, Cai-Zhuang
Ho, Kai-Ming
Wu, Shunqing
Wentzcovitch, Renata M.
Sun, Yang
contents Constraining the melting temperature of iron under Earth's inner core conditions is crucial for understanding core dynamics and planetary evolution. Here, we develop a deep potential (DP) model for iron that explicitly incorporates electronic entropy contributions governing thermodynamics under Earth's core conditions. Extensive benchmarking demonstrates the DP's high fidelity across relevant iron phases and extreme pressure and temperature conditions. Through thermodynamic integration and direct solid-liquid coexistence simulations, the DP predicts melting temperatures for iron at the inner core boundary, consistent with previous \textit{ab initio} results. This resolves the previous discrepancy of iron's melting temperature at ICB between the DP model and \textit{ab initio} calculation and suggests the crucial contribution of electronic entropy. Our work provides insights into machine learning melting behavior of iron under core conditions and provides the basis for future development of binary or ternary DP models for iron and other elements in the core.
format Preprint
id arxiv_https___arxiv_org_abs_2404_17852
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Melting Temperature of Iron Under the Earth's Inner Core Condition from Deep Machine Learning
Wu, Fulun
Wang, Cai-Zhuang
Ho, Kai-Ming
Wu, Shunqing
Wentzcovitch, Renata M.
Sun, Yang
Geophysics
Materials Science
Constraining the melting temperature of iron under Earth's inner core conditions is crucial for understanding core dynamics and planetary evolution. Here, we develop a deep potential (DP) model for iron that explicitly incorporates electronic entropy contributions governing thermodynamics under Earth's core conditions. Extensive benchmarking demonstrates the DP's high fidelity across relevant iron phases and extreme pressure and temperature conditions. Through thermodynamic integration and direct solid-liquid coexistence simulations, the DP predicts melting temperatures for iron at the inner core boundary, consistent with previous \textit{ab initio} results. This resolves the previous discrepancy of iron's melting temperature at ICB between the DP model and \textit{ab initio} calculation and suggests the crucial contribution of electronic entropy. Our work provides insights into machine learning melting behavior of iron under core conditions and provides the basis for future development of binary or ternary DP models for iron and other elements in the core.
title Melting Temperature of Iron Under the Earth's Inner Core Condition from Deep Machine Learning
topic Geophysics
Materials Science
url https://arxiv.org/abs/2404.17852