Abstract

Spillway excavation is often adopted as a precautionary engineering measure for disaster mitigation before landslide dam breaching. Based on the landslide dam breach mechanisms, this paper focuses on developing a numerical model to comprehensively discuss the issue based on three documented landslide dam failures, such as Tangjiashan, Xiaogangjian, and Baige landslide dams. The spillway cross section morphologies were modeled with different sizes under common shape (i.e., an inverted trapezoid) and slope conditions. The influence of cross section on dam breach processes was analyzed under conditions of different depth, bottom width, slope ratio in the cross and longitudinal sections, with/without spillway. The following conclusions can be drawn: 1) excavation of a spillway can effectively reduce the peak breach flow, therefore delay the time to peak; 2) the peak breach flow dramatically decreases and the time to peak delays as the spillway depth increases; 3) the peak breach flow changes little and the time to peak occurs earlier with the increment in spillway bottom width; 4) the peak breach flow decreases and the time to peak delays with the decrease of slope ratio in cross section in the spillway; 5) the slope ratio in the longitudinal section has little influence on the breach process. Hence, if conditions permit, the spillway with large spillway depth, small bottom width, and gentle slope ratio in the cross section is the preferable section morphology for the emergency disposal of the landslide dam.

Highlights

  • Landslide dam is formed by mass movements of rock and debris blocking the river channel due to earthquakes and intense rainfall (Costa and Schuster, 1988); Figure 1 presents the Hongshiyan landslide dam that occurred on August 3rd, 2014 in China

  • The following section utilizes the numerical model to study the influence of spillway section morphologies on landslide dam breaching

  • Considering the morphological, structural, and material characteristics of the landslide dams and the hydrodynamic conditions of dammed lakes, a numerical model was developed by the authors

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Summary

INTRODUCTION

Landslide dam is formed by mass movements of rock and debris blocking the river channel due to earthquakes and intense rainfall (Costa and Schuster, 1988); Figure 1 presents the Hongshiyan landslide dam that occurred on August 3rd, 2014 in China. It is vital to completely consider the rate of rising of the water level in the dammed lake, the limitations of the construction conditions, and the discharge capacity of the downstream river channel, and to optimize the design of the spillway section morphology. Zhao et al (2018) conducted the centrifugal model tests under the condition of the same cross section area and found that the compound section is a relatively safer morphology for the spillway considering the higher initial discharge efficiency and lower peak breach flow. Based on the breach process, a numerical model that can consider the hydrodynamic conditions of the dammed lake, the morphological, structural, and material characteristics of the landslide dam was proposed by Zhong et al (2020a). Y. et al, 2015), Xiaogangjian (Chen et al, 2018), and Baige (Cai et al, 2020; Zhong et al, 2020b) in China with documented information on the breach process are chosen as the representatives

Introduction of the Three Landslide Dams
Calculated Results
CONCLUSION
DATA AVAILABILITY STATEMENT
Full Text
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