Floating drift on a vibrofluidized relaxing granular slope

For floating on water, low density is the sole necessary factor. However, it has not been clarified how to floatingly drift on fluidized granular matter. Although this problem relates to various natural phenomena such as debris flow and lunar boulder-fall traces, fundamental aspects of the floating drift on granular flow have not been revealed. Therefore, the motion of a sphere on a vibrated granular slope is experimentally investigated in this study. As a result, we find that the sinking depth of the floating sphere can be explained by a modified buoyancy model. In addition, the downstream velocity of the drifting sphere can be understood by a force balance between flow-induced pushing force and frictional resistance force. This force balance results in a nonsteady but stable floating drift on the relaxing granular slope. Published by the American Physical Society 2024

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Publication Details

Journal
Physical Review Research
Published
2024-11-20
DOI
https://doi.org/10.1103/physrevresearch.6.043178
Primary Topic
Granular flow and fluidized beds
Type
article
Field-Weighted Citation Impact
0.00

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article

Floating drift on a vibrofluidized relaxing granular slope

Hiroaki Katsuragi, Yuki Yamamoto
Physical Review Research
Granular flow and fluidized beds
article

Floating drift on a vibrofluidized relaxing granular slope

Hiroaki Katsuragi, Yuki Yamamoto
article en

Abstract

For floating on water, low density is the sole necessary factor. However, it has not been clarified how to floatingly drift on fluidized granular matter. Although this problem relates to various natural phenomena such as debris flow and lunar boulder-fall traces, fundamental aspects of the floating drift on granular flow have not been revealed. Therefore, the motion of a sphere on a vibrated granular slope is experimentally investigated in this study. As a result, we find that the sinking depth of the floating sphere can be explained by a modified buoyancy model. In addition, the downstream velocity of the drifting sphere can be understood by a force balance between flow-induced pushing force and frictional resistance force. This force balance results in a nonsteady but stable floating drift on the relaxing granular slope. Published by the American Physical Society 2024

Physical Review ResearchVol. 6(4)
The University of Osaka (JP)
Japan Society for the Promotion of Science
Openalex Percentile: Top 77%
Granular flow and fluidized beds
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