Formation of dry granular fronts and watery tails in debris flows
Debris flows are particle–fluid mixtures that pose a significant hazard to many communities throughout the world. Bouldery debris flows are often characterised by a deep dry granular flow front, which is followed by a progressively thinner and increasingly watery tail. The formation of highly destru...
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Veröffentlicht in: | Journal of fluid mechanics 2022-07, Vol.943, Article A19 |
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Format: | Artikel |
Sprache: | eng |
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