Melting phase relation of seifertite and pyrite-type SiO2 determined by machine learning potentials

Fuente: arXiv
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Autori principali: Park, Doyoon, Deng, Xin, Deng, Jie
Natura: Preprint
Pubblicazione: 2025
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author Park, Doyoon
Deng, Xin
Deng, Jie
author_facet Park, Doyoon
Deng, Xin
Deng, Jie
contents Silica (SiO2) is fundamental to both industrial technology and planetary science, yet the phase relations of its high-pressure polymorphs remain poorly constrained. Here, we develop two machine learning potentials (MLPs) for SiO2 that faithfully represent the SCAN and PBEsol exchange-correlation functionals over a wide temperature (1000-10000 K) and pressure (100-400 GPa) range using deep neural networks. With large-scale two-phase simulations powered by these potentials, we determine the melting curves of seifertite and pyrite-type SiO2 and infer the solid-solid phase boundary between these two phases. The SCAN functional, which captures intermediate-range van der Waals interactions, reproduces structural and thermodynamic properties with high fidelity, predicting melting temperatures 6-10 % higher and a seifertite to pyrite-type transition pressure 22 % higher than the PBEsol. The strongly negative Clapeyron slope (-6.1 MPa/K) of this transition suggests that mantle convection could be highly layered in super-Earth exoplanets, potentially affecting their long-term thermal evolution and habitability.
format Preprint
id arxiv_https___arxiv_org_abs_2510_13119
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Melting phase relation of seifertite and pyrite-type SiO2 determined by machine learning potentials
Park, Doyoon
Deng, Xin
Deng, Jie
Materials Science
Geophysics
Silica (SiO2) is fundamental to both industrial technology and planetary science, yet the phase relations of its high-pressure polymorphs remain poorly constrained. Here, we develop two machine learning potentials (MLPs) for SiO2 that faithfully represent the SCAN and PBEsol exchange-correlation functionals over a wide temperature (1000-10000 K) and pressure (100-400 GPa) range using deep neural networks. With large-scale two-phase simulations powered by these potentials, we determine the melting curves of seifertite and pyrite-type SiO2 and infer the solid-solid phase boundary between these two phases. The SCAN functional, which captures intermediate-range van der Waals interactions, reproduces structural and thermodynamic properties with high fidelity, predicting melting temperatures 6-10 % higher and a seifertite to pyrite-type transition pressure 22 % higher than the PBEsol. The strongly negative Clapeyron slope (-6.1 MPa/K) of this transition suggests that mantle convection could be highly layered in super-Earth exoplanets, potentially affecting their long-term thermal evolution and habitability.
title Melting phase relation of seifertite and pyrite-type SiO2 determined by machine learning potentials
topic Materials Science
Geophysics
url https://arxiv.org/abs/2510.13119