Local atomic environments reveal structural controls on MgSiO3 liquid-crystal similarity
- 1Department of Geosciences, Princeton University , 11 Ivy Lane, 08540, New Jersey ,
- 2Department of Earth and Planetary Sciences, Harvard University , 20 Oxford Street, 02138, Massachusetts ,
Abstract
MgSiO3 is a fundamental silicate system in Earth and rocky planetary interiors, where its structures control crystallization, differentiation, and evolution of host planets. Yet, silicate structure has usually been analyzed through aggregate structural observables that do not place individual local atomic environments from crystals and liquids into a common similarity space. Here we compare local environments across eight MgSiO3 polymorphs and the liquid up to 700 GPa and 12,000 K generated via a machine-learning potential and first-principles calculations. We use the Smooth Overlap of Atomic Positions (SOAP) descriptor, principal component analysis (PCA), and k-nearest-neighbor distances in the full descriptor space. PCA shows that the dominant variation largely follows density-driven packing, whereas full-space distances reveal pronounced differences in structural similarity among MgSiO3 polymorphs and the liquid. Pyroxene-family phases, majorite, and akimotoite remain comparatively close to the liquid, but bridgmanite and post-perovskite are systematically less liquid-like. This separation is not explained by the SiO4-to-SiO6 coordination change alone, and instead stems from a coupled variation in multiple structural features. These results show that local atomic descriptors expose structural distinctions hidden by conventional averaged metrics and suggest that high-pressure liquid thermodynamics, including the non-monotonic pressure dependence of liquid Grüneisen parameters, need not be interpreted simply as progressive convergence toward the stable lower-mantle crystal structures.
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BibTeX
@article{acquadro2026local,
title = {{Local atomic environments reveal structural controls on MgSiO3 liquid-crystal similarity}},
author = {Jake Acquadro and Xiyuan Bao and Jie Deng},
journal = {PNAS Nexus},
year = {2026},
month = oct,
doi = {10.1093/pnasnexus/pgag347},
url = {https://academic.oup.com/pnasnexus/advance-article/doi/10.1093/pnasnexus/pgag347/8868851},
note = {CC BY 4.0},
}
RIS
TY - JOUR
TI - Local atomic environments reveal structural controls on MgSiO3 liquid-crystal similarity
AU - Jake Acquadro
AU - Xiyuan Bao
AU - Jie Deng
PY - 2026
DA - 2026/10/06
JO - PNAS Nexus
DO - 10.1093/pnasnexus/pgag347
UR - https://academic.oup.com/pnasnexus/advance-article/doi/10.1093/pnasnexus/pgag347/8868851
AB - MgSiO3 is a fundamental silicate system in Earth and rocky planetary interiors, where its structures control crystallization, differentiation, and evolution of host planets. Yet, silicate structure has usually been analyzed through aggregate structural observables that do not place individual local atomic environments from crystals and liquids into a common similarity space. Here we compare local environments across eight MgSiO3 polymorphs and the liquid up to 700 GPa and 12,000 K generated via a machine-learning potential and first-principles calculations. We use the Smooth Overlap of Atomic Positions (SOAP) descriptor, principal component analysis (PCA), and k-nearest-neighbor distances in the full descriptor space. PCA shows that the dominant variation largely follows density-driven packing, whereas full-space distances reveal pronounced differences in structural similarity among MgSiO3 polymorphs and the liquid. Pyroxene-family phases, majorite, and akimotoite remain comparatively close to the liquid, but bridgmanite and post-perovskite are systematically less liquid-like. This separation is not explained by the SiO4-to-SiO6 coordination change alone, and instead stems from a coupled variation in multiple structural features. These results show that local atomic descriptors expose structural distinctions hidden by conventional averaged metrics and suggest that high-pressure liquid thermodynamics, including the non-monotonic pressure dependence of liquid Grüneisen parameters, need not be interpreted simply as progressive convergence toward the stable lower-mantle crystal structures.
SN - 2752-6542
ER -