Estimation of Vent Radii From Video Recordings and Infrasound Data Analysis

Implications for Vulcanian Eruptions From Sakurajima Volcano, Japan

Dan Muramatsu, Koki Aizawa, Akihiko Yokoo, Masato Iguchi, Takeshi Tameguri

研究成果: ジャーナルへの寄稿記事

抄録

We estimated the vent radius within Showa Crater of Sakurajima volcano from ejection velocity and flow rate of gas-particle mixtures. The ejection velocity was calculated from video recordings, and the flow rate and volume from infrasound data. Based on the assumption that the vent shape does not change during an explosion, the vent radius was estimated from 201 impulsive Vulcanian eruptions at Showa Crater, yielding values of 6.4–42.3 m (median 23.8 m), which is comparable with the width of fresh lava capping the vent, as photographed from a helicopter. Long-term changes in vent radius (i.e., over several months) show a relationship with magma accumulation within a reservoir 2–5 km beneath the crater. If the top of the conduit is assumed to be cylindrical, then the vertical extent of the gas-rich zone is estimated to be 120 m, which may reflect the depth of gas accumulation and buildup of significant overpressure.

元の言語英語
ページ(範囲)12,829-12,836
ジャーナルGeophysical Research Letters
45
発行部数23
DOI
出版物ステータス出版済み - 12 16 2018

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vents
volcanoes
volcanic eruptions
crater
Japan
volcano
volcanic eruption
recording
radii
craters
gas
ejection
capping
overpressure
long-term change
lava
flow velocity
gases
explosion
magma

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth and Planetary Sciences(all)

これを引用

Estimation of Vent Radii From Video Recordings and Infrasound Data Analysis : Implications for Vulcanian Eruptions From Sakurajima Volcano, Japan. / Muramatsu, Dan; Aizawa, Koki; Yokoo, Akihiko; Iguchi, Masato; Tameguri, Takeshi.

:: Geophysical Research Letters, 巻 45, 番号 23, 16.12.2018, p. 12,829-12,836.

研究成果: ジャーナルへの寄稿記事

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abstract = "We estimated the vent radius within Showa Crater of Sakurajima volcano from ejection velocity and flow rate of gas-particle mixtures. The ejection velocity was calculated from video recordings, and the flow rate and volume from infrasound data. Based on the assumption that the vent shape does not change during an explosion, the vent radius was estimated from 201 impulsive Vulcanian eruptions at Showa Crater, yielding values of 6.4–42.3 m (median 23.8 m), which is comparable with the width of fresh lava capping the vent, as photographed from a helicopter. Long-term changes in vent radius (i.e., over several months) show a relationship with magma accumulation within a reservoir 2–5 km beneath the crater. If the top of the conduit is assumed to be cylindrical, then the vertical extent of the gas-rich zone is estimated to be 120 m, which may reflect the depth of gas accumulation and buildup of significant overpressure.",
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