Modelling of Bottom Shear Stresses in Scoured Hole Formed by Nappe Flow During Levee Overtopping

Increases in flood magnitude due to climate change increase the necessity of resilient river levees to prevent the breaching that can contribute to reduced flood inundation volume even when overtopping from a levee occurs. When a levee is composed of cohesive soil and the levee crest is paved, overtopping can lead to a waterfall-like nappe flow due to the erosion of the downstream slope of a levee. This flow subsequently expands the scour hole and increases the risk of levee failure. Although some models of scour hole expansion due to nappe flow were proposed, flow structures in the scour hole were not adequately taken into account. This study aimed to clarify the flow structure, including formation of vortices in the scour hole, by conducting flow visualization experiments and three-dimensional numerical analyses. After clarifying the flow structure, this study proposed a simplified model to calculate the bottom shear stress in a scour hole on the levee side. The accuracy of the estimated bottom shear stress was verified by comparing the results with a three-dimensional numerical analysis. This proposed method can predict further erosion of a scour hole.

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Publication Details

Journal
GeoHazards
Published
2025-03-01
DOI
https://doi.org/10.3390/geohazards6010011
Citations
2
Primary Topic
Hydrology and Sediment Transport Processes
Type
article
Field-Weighted Citation Impact
3.43
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article

Modelling of Bottom Shear Stresses in Scoured Hole Formed by Nappe Flow During Levee Overtopping

Yoshiya IGARASHI, Norio Tanaka
2 citations
GeoHazards
Hydrology and Sediment Transport Processes
3.43
article

Modelling of Bottom Shear Stresses in Scoured Hole Formed by Nappe Flow During Levee Overtopping

Yoshiya IGARASHI, Norio Tanaka
article en
2 citations

Abstract

Increases in flood magnitude due to climate change increase the necessity of resilient river levees to prevent the breaching that can contribute to reduced flood inundation volume even when overtopping from a levee occurs. When a levee is composed of cohesive soil and the levee crest is paved, overtopping can lead to a waterfall-like nappe flow due to the erosion of the downstream slope of a levee. This flow subsequently expands the scour hole and increases the risk of levee failure. Although some models of scour hole expansion due to nappe flow were proposed, flow structures in the scour hole were not adequately taken into account. This study aimed to clarify the flow structure, including formation of vortices in the scour hole, by conducting flow visualization experiments and three-dimensional numerical analyses. After clarifying the flow structure, this study proposed a simplified model to calculate the bottom shear stress in a scour hole on the levee side. The accuracy of the estimated bottom shear stress was verified by comparing the results with a three-dimensional numerical analysis. This proposed method can predict further erosion of a scour hole.

GeoHazardsVol. 6(1)
Saitama University (JP)
Openalex Percentile: Top 10%
Hydrology and Sediment Transport Processes
3.43
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Modelling of Bottom Shear Stresses in Scoured Hole Formed by Nappe Flow During Levee Overtopping — Yoshiya IGARASHI, Norio Tanaka · GeoHazards (2025) | TGRS Research Map | TGRS