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

• Published in: Earth, planets, and space planets, and space, 2023-12, Vol.75 (1), p.100-15, Article 100
• Main Authors: Kozono, Tomofumi, Koyaguchi, Takehiro, Ueda, Hideki, Ozawa, Taku, Yamasaki, Tadashi
• Format: Article
• Language: English
• Subjects: 5. Volcanology; Bubble chambers; Chambers; Compressibility; Earth and Environmental Science; Earth Sciences; Environmental aspects; Geodetic observation; Geology; Geophysics/Geodesy; Image analysis; Japan; Lava; Magma; Magma chamber; Magma chambers; Magma dynamics; Magma Migration and Eruptions in a Volcanic Group: Case Studies for the 2017-2018 Activity of the Kirishima Volcano Group and Other Global Examples; Rigidity; Storage; Vapor phases; Volcanic eruption; Volcanic eruptions; Volcanoes
• ISSN: 1880-5981; 1343-8832; 1880-5981
• DOI: 10.1186/s40623-023-01851-2

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. Graphical Abstract