How are fine sediments described in sediment sheet flow?
Stony debris flow transits to sediment sheet flow when the river bed gradient becomes gentle. The sediment sheet flow consists of a water flow layer and a sediment moving layer. Fine sediments are expected to behave as a part of the fluid rather than a solid phase in the sediment moving layer. Furth...
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Published in | E3S web of conferences Vol. 415; p. 1027 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
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EDP Sciences
01.01.2023
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Abstract | Stony debris flow transits to sediment sheet flow when the river bed gradient becomes gentle. The sediment sheet flow consists of a water flow layer and a sediment moving layer. Fine sediments are expected to behave as a part of the fluid rather than a solid phase in the sediment moving layer. Further, it can be thought that a part of fine sediment can be suspended in the water flow layer. However, it was not possible to physically express whether the fine sediment behaves as a solid phase or a fluid phase in the numerical simulation model. Here we physically modeled fine sediment behavior in sediment sheet flow. We confirmed the applicability of the new model to describe the longitudinal deposited sediment gradient in flume experiments. |
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AbstractList | Stony debris flow transits to sediment sheet flow when the river bed gradient becomes gentle. The sediment sheet flow consists of a water flow layer and a sediment moving layer. Fine sediments are expected to behave as a part of the fluid rather than a solid phase in the sediment moving layer. Further, it can be thought that a part of fine sediment can be suspended in the water flow layer. However, it was not possible to physically express whether the fine sediment behaves as a solid phase or a fluid phase in the numerical simulation model. Here we physically modeled fine sediment behavior in sediment sheet flow. We confirmed the applicability of the new model to describe the longitudinal deposited sediment gradient in flume experiments. |
Author | Satofuka, Yoshifumi Nishiguchi, Yuki Niwa, Satoshi Uchida, Taro Kubo, Takeshi Gonda, Yutaka |
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Cites_doi | 10.1139/cgj-2019-0452 10.1061/(ASCE)HY.1943-7900.0001586 10.1029/2021JF006452 10.1002/2015JF003725 10.2208/prohe.41.759 10.1201/9780203946282 10.20965/jdr.2011.p0313 10.1029/97RG00426 10.1016/j.earscirev.2022.104135 |
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