日本地球惑星科学連合2022年大会

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[J] 口頭発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS21] 地球流体力学:地球惑星現象への分野横断的アプローチ

2022年5月24日(火) 15:30 〜 17:00 104 (幕張メッセ国際会議場)

コンビーナ:伊賀 啓太(東京大学大気海洋研究所)、コンビーナ:吉田 茂生(九州大学大学院理学研究院地球惑星科学部門)、柳澤 孝寿(国立研究開発法人海洋研究開発機構 海域地震火山部門)、コンビーナ:相木 秀則(名古屋大学)、座長:伊賀 啓太(東京大学大気海洋研究所)、吉田 茂生(九州大学大学院理学研究院地球惑星科学部門)

15:45 〜 16:00

[MIS21-02] Experimental investigation of Rayleigh-Benard convection in a fluid
layer with quasi-two-dimensional confinement

*髙野 奏汰1能登 大輔2田坂 裕司2柳澤 孝寿3,2宮腰 剛広3、村井 祐一2 (1.北海道大学大学院工学院、2.北海道大学大学院工学研究院、3.海洋研究開発機構)


Geometric confinement has a large influence on flow structures in Rayleigh-Bénard convection. For example, large scale circulation reverses its flow direction more frequently in thinner convection cells. Confinement also have great effects on convective heat transfer efficiency. Heat flux increases significantly in quasi-two-dimensional geometries, even though the flow is strongly suppressed by the surrounding walls. Geometric confinement brings about great changes in the behavior of convection. We performed experimental study in quasi-two-dimensional Rayleigh-Bénard convection to examine the confinement effects on thermal convective flow.

We conducted visualization experiments using Xanthan-Gum aqueous solution with small temperature dependence of viscosity as the test fluid and highly confined convection cells with rectangular shape as a container. Geometric confinement is characterized by thickness-to-height aspect ratio Γ. We set Γabout 1/8, where the quasi-two dimensional convective flow is realized. Velocity profiles measured by particle image velocimetry to quantify the spatiotemporal dynamics. We observed quasi-two-dimensional roll near the onset of convection. As convection developed with increasing thermal buoyancy, time-periodic oscillations occurred near the side walls. This oscillation coincides with the emergence of vortex structures at the corner. Once the vortex structure appears, the size of the roll structures increases. This fact implies that the vortex structure may play an important role in heat transport in quasi-two-dimensional convection.