Helium isotope anomaly in groundwater prior to the 2024 Noto Peninsula earthquake

Intense earthquake swarms had been observed on the Noto Peninsula in north-central Japan since December 2020. We report data obtained by periodical groundwater sampling and helium isotope measurements in the epicentre area starting July 2022 for investigating the cause of this swarm. The data show mantle-derived helium reaching a maximum of 5 R<sub>a</sub> where R<sub>a</sub> is the atmospheric <sup>3</sup>He/<sup>4</sup>He ratio of 1.39 × 10<sup>-6</sup>. This value indicates that the swarm was caused by fluids rising from the mantle. Time-series analysis show an anomalous drop in helium isotopic ratio prior to the 1 January 2024 Noto earthquake (M7.6), which seriously damaged the region. This decrease in helium isotopic ratio is possibly due to the degassing of radiogenic helium via the deformation of the rocks constituting the groundwater aquifer, which is fundamental and valuable data for predicting inland earthquakes in subduction zones. Periodical observation of helium isotopic ratios in deep groundwater is desirable in regions where a large earthquake is expected.

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Journal
Nature Communications
Published
2025-11-26
DOI
https://doi.org/10.1038/s41467-025-65717-9
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
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article

Helium isotope anomaly in groundwater prior to the 2024 Noto Peninsula earthquake

Yasuyuki Kawamoto, Tomo Shibata, Takanori Kagoshima, Yuji Sano et al.
Nature Communications
Groundwater and Isotope Geochemistry
article

Helium isotope anomaly in groundwater prior to the 2024 Noto Peninsula earthquake

Yasuyuki Kawamoto, Tomo Shibata, Takanori Kagoshima, Yuji Sano, Tomoaki Morishita, Naoto Takahata, Junichi Nakajima, Yoshihiro Hiramatsu, Ying Li
article en

Abstract

Intense earthquake swarms had been observed on the Noto Peninsula in north-central Japan since December 2020. We report data obtained by periodical groundwater sampling and helium isotope measurements in the epicentre area starting July 2022 for investigating the cause of this swarm. The data show mantle-derived helium reaching a maximum of 5 R<sub>a</sub> where R<sub>a</sub> is the atmospheric <sup>3</sup>He/<sup>4</sup>He ratio of 1.39 × 10<sup>-6</sup>. This value indicates that the swarm was caused by fluids rising from the mantle. Time-series analysis show an anomalous drop in helium isotopic ratio prior to the 1 January 2024 Noto earthquake (M7.6), which seriously damaged the region. This decrease in helium isotopic ratio is possibly due to the degassing of radiogenic helium via the deformation of the rocks constituting the groundwater aquifer, which is fundamental and valuable data for predicting inland earthquakes in subduction zones. Periodical observation of helium isotopic ratios in deep groundwater is desirable in regions where a large earthquake is expected.

Nature CommunicationsVol. 16(1)
Kanazawa University (JP), Tokyo Institute of Technology (JP), Planetary Science Institute (US), Japan Agency for Marine-Earth Science and Technology (JP), University of Kochi (JP), Fukuoka University (JP), ASKA Pharmaceutical (Japan) (JP), Sphere Institute (US), University of Toyama (JP), The University of Tokyo (JP), Kōchi University (JP), China Earthquake Administration (CN)
Japan Society for the Promotion of Science
Openalex Percentile: Top 68%
Groundwater and Isotope Geochemistry
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