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  1. 防災科研関係論文

Constraints on magma storage conditions based on geodetic volume change and erupted magma volume and application to the 2011 and 2018 eruptions at Kirishima Shinmoe-dake volcano, Japan

https://nied-repo.bosai.go.jp/records/6327
https://nied-repo.bosai.go.jp/records/6327
7299aea4-cbdc-4ba3-8791-f2a0155a11a5
Item type researchmap(1)
公開日 2024-05-13
タイトル
言語 en
タイトル Constraints on magma storage conditions based on geodetic volume change and erupted magma volume and application to the 2011 and 2018 eruptions at Kirishima Shinmoe-dake volcano, Japan
著者 Tomofumi Kozono

× Tomofumi Kozono

en Tomofumi Kozono

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Takehiro Koyaguchi

× Takehiro Koyaguchi

en Takehiro Koyaguchi

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Hideki Ueda

× Hideki Ueda

en Hideki Ueda

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Taku Ozawa

× Taku Ozawa

en Taku Ozawa

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Tadashi Yamasaki

× Tadashi Yamasaki

en Tadashi Yamasaki

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抄録
内容記述タイプ Other
内容記述 We investigated magma storage conditions prior to the 2011 and 2018 eruptions at Kirishima Shinmoe-dake volcano in Japan based on the relationship between geodetic volume change of magma chamber and erupted magma volume. We derived an analytical expression for the ratio of the erupted magma volume to the geodetic volume change (“volume ratio”), which was formulated as a function of parameters related to the magma storage conditions. This expression shows that the volume ratio is strongly dependent on the effective compressibility of the magma chamber, which in turn depends on the rigidity of surrounding host rocks and shape of the chamber. For the Shinmoe-dake eruptions, the magnitude of the volume change (i.e., deflation) of a spherical magma chamber associated with lava effusion was estimated based on geodetic observations. The erupted magma volume was estimated from a SAR image analysis of the lava accumulation inside the summit crater. Based on these observations, we estimated that the volume ratio in 2011 and 2018 was 2.69 and 2.33, respectively. Substituting the estimated volume ratio into the analytical expression revealed that the observed geodetic data and volume ratio can be explained only when the magma chamber, which was assumed to be spherical, is filled with bubble-free magma. This result suggests that efficient gas segregation from the chamber occurred prior to the eruptions. Our results indicate that combining multi-observation data based on the volume ratio provides valuable information about the magma storage process, such as the behavior of the gas phase in the magma chamber.
言語 en
書誌情報 en : Earth, Planets and Space

巻 75, 号 1, 発行日 2023-06-20
出版者
言語 en
出版者 Springer Science and Business Media LLC
ISSN
収録物識別子タイプ EISSN
収録物識別子 1880-5981
DOI
関連識別子 10.1186/s40623-023-01851-2
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