Protonic thermoelectric effect of Superionic H2O and magnetic field generation in Uranus and Neptune

Fuente: arXiv
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Autori principali: Liu, Daohong, Zhang, Wei, He, Yu, Guo, Xinzhuan, Zhang, Chuanyu, Sun, Yang
Natura: Preprint
Pubblicazione: 2026
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author Liu, Daohong
Zhang, Wei
He, Yu
Guo, Xinzhuan
Zhang, Chuanyu
Sun, Yang
author_facet Liu, Daohong
Zhang, Wei
He, Yu
Guo, Xinzhuan
Zhang, Chuanyu
Sun, Yang
contents Uranus and Neptune are characterized by anomalously tilted and multi-dipole magnetic fields, which poses substantial challenges for elucidating the internal mechanisms generating magnetic fields. Recent investigations confirmed that superionic H2O is thermodynamically stable and constitutes the dominant H2O phase within their icy mantles. In this study, we demonstrate that the superionic H2O ice exhibits a pronounced protonic thermoelectric effect, in which the maximum Seebeck coefficient within the interior of Uranus can reach approximately 620 uV/K, whereas that of Neptune is lower, within the range of 570-585 uV/K. Consequently, temperature gradients in the icy mantles can induce proton convection, which in turn drives magnetic field generation. Based on this novel mechanism, the disparities in magnetic field strength between Uranus and Neptune can be accounted for exclusively by their differing internal temperature gradients, and the predicted values are in agreement with observations.
format Preprint
id arxiv_https___arxiv_org_abs_2601_03659
institution arXiv
publishDate 2026
record_format arxiv
spellingShingle Protonic thermoelectric effect of Superionic H2O and magnetic field generation in Uranus and Neptune
Liu, Daohong
Zhang, Wei
He, Yu
Guo, Xinzhuan
Zhang, Chuanyu
Sun, Yang
Earth and Planetary Astrophysics
Materials Science
Uranus and Neptune are characterized by anomalously tilted and multi-dipole magnetic fields, which poses substantial challenges for elucidating the internal mechanisms generating magnetic fields. Recent investigations confirmed that superionic H2O is thermodynamically stable and constitutes the dominant H2O phase within their icy mantles. In this study, we demonstrate that the superionic H2O ice exhibits a pronounced protonic thermoelectric effect, in which the maximum Seebeck coefficient within the interior of Uranus can reach approximately 620 uV/K, whereas that of Neptune is lower, within the range of 570-585 uV/K. Consequently, temperature gradients in the icy mantles can induce proton convection, which in turn drives magnetic field generation. Based on this novel mechanism, the disparities in magnetic field strength between Uranus and Neptune can be accounted for exclusively by their differing internal temperature gradients, and the predicted values are in agreement with observations.
title Protonic thermoelectric effect of Superionic H2O and magnetic field generation in Uranus and Neptune
topic Earth and Planetary Astrophysics
Materials Science
url https://arxiv.org/abs/2601.03659