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  1. 防災科研関係論文

Eruption pattern and a long-term magma discharge rate over the past 100 years at Kelud Volcano, Indonesia

https://nied-repo.bosai.go.jp/records/5469
https://nied-repo.bosai.go.jp/records/5469
fc630bf9-470a-408f-9d42-0f56a9500357
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Eruption pattern and a long-term magma discharge rate over the past 100 years at Kelud Volcano, Indonesia
言語
言語 eng
著者 Fukashi Maeno

× Fukashi Maeno

en Fukashi Maeno

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Setsuya Nakada

× Setsuya Nakada

en Setsuya Nakada

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Mitsuhiro Yoshimoto

× Mitsuhiro Yoshimoto

en Mitsuhiro Yoshimoto

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Taketo Shimano

× Taketo Shimano

en Taketo Shimano

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Natsumi Hokanishi

× Natsumi Hokanishi

en Natsumi Hokanishi

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Akhmad Zaennudin

× Akhmad Zaennudin

en Akhmad Zaennudin

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Masato Iguchi

× Masato Iguchi

en Masato Iguchi

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抄録
内容記述タイプ Other
内容記述 © 2019, Fuji Technology Press. All rights reserved. Kelud Volcano is among the most active volcanoes in Indonesia, with repeated explosive eruptions throughout its history. Here, we reconstructed the relationship between the repose period and the cumulative volume of erupted material over the past 100 years and estimated the long-term magma discharge rate and future eruptive potential and hazards. Tephra data and eruption sequences described in historical documents were used to estimate the volume and mass discharge rate. The volumes of the 1901, 1919, 1951, 1966, 1990, and 2014 eruptions were estimated as 51–296 × 106 m3 . The mass discharge rates were estimated to be on the order of 107 kg/s for the 1919, 1951, and 2014 eruptions and the order of 106 kg/s for the 1966 and 1990 eruptions. Based on a linear relationship between the repose period and cumulative erupted mass, the long-term mass discharge rate was estimated as ∼ 1.5 × 1010 kg/year, explaining the features of the larger eruptions (1919, 1951, and 2014) but not those of the smaller eruptions (1966 and 1990). This estimate is relatively high compared to other typical basaltic-andesitic subduction-zone volcanoes. This result provides important insights into the evolution of magmatic systems and prediction of future eruptions at Kelud Volcano.
言語 en
書誌情報 en : Journal of Disaster Research

巻 14, 号 1, p. 27-39
ISSN
収録物識別子タイプ EISSN
収録物識別子 1883-8030
DOI
関連識別子 10.20965/JDR.2019.P0027
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