2024 Volume 80 Issue 16 Article ID: 23-16110
In the gravel bed rivers, levee disasters caused by erosion occur frequently, regardless of over-flow. Particularly in curved sections of the river channel, we observe disasters where erosion of the backside of the low-water revetment leads to levee erosion. This study focuses on the levee eroison occurring on the outer side of the curved sections of the river channel, where the risk of that is high. We reproduced the levee erosion during flooding through large-scale hydraulic experiments, elucidated the process of erosion disaster progression, and verified the effectiveness of countermeasures based on that disaster process.