JpGU-AGU Joint Meeting 2020

講演情報

[E] ポスター発表

セッション記号 S (固体地球科学) » S-VC 火山学

[S-VC42] 火山噴火のダイナミクスと素過程

コンビーナ:並木 敦子(広島大学 総合科学研究科 環境自然科学講座)、Christian Huber(Brown University)、Michael Manga(University of California Berkeley)、鈴木 雄治郎(東京大学地震研究所)

[SVC42-P06] 風洞実験に基づく火山岩塊の飛行軌道シミュレーション

*常松 佳恵1 (1.山形大学)

キーワード:火山岩塊、風洞実験、抵抗係数、揚力係数

Ballistic projectiles are large (>10 cm) pyroclasts, ejected from erupting volcanoes, that draw parabolic trajectories without being influenced by the flow of the gas and solid mixture (e.g. Taddeucci et al., 2017). Transport dynamics of ballistic projectiles are studied by observing real volcanic eruptions or numerical simulations. The largest unknown factor of ballistic transport is aerial drag, which is hard to estimate by observation.

There are many examples of drag measurements for artificial shapes such as cylinders and cubes, but only a few examples of drag measurements using real volcanic rocks. Therefore, wind tunnel experiments were implemented using a block obtained from Zao volcano, which erupted in 1895 (Kochibe, 1896). In order to clarify the size effect we used blocks of the same shape but different sizes. The results of these experiments were (1) the drag coefficient depends on the Reynolds number (when the block rotates more than three times per second) and the cross-sectional shape, (2) the lift coefficient of the block is very low compared to the drag coefficient when the block is rotating.

Numerical simulations were conducted using the drag and lift coefficients obtained from the wind tunnel experiments. Based on the numerical simulation results we show how the drag and lift coefficients affect the transport of ballistic blocks with and without rotation, and the condition of the blocks that travel furthest, by varying the block size, the ejection angle, and the rotation status.