Modeling of Breaching Due to Overtopping Flow and Waves Based on Coupled Flow and Sediment Transport

TL;DR

This paper develops a 2D coupled flow and sediment transport model to analyze dam breach processes caused by overtopping flow and waves, highlighting the significant impact of waves on erosion patterns and breach morphology.

Contribution

It introduces a novel depth-averaged 2D coupled model incorporating sediment transport, bed change, and wave effects, validated against experimental data for simulating overtopping breaching.

Findings

Waves significantly accelerate erosion and alter breach shape.

Flow without waves causes vertical then lateral erosion.

Model accurately simulates flow, bed change, and sediment transport.

Abstract

Breaching of earthen or sandy dams/dunes by overtopping flow and waves is a complicated process with strong, unsteady flow, high sediment transport, and rapid bed changes in which the interactions between flow and morphology should not be ignored. This study presents a depth-averaged two-dimensional (2D) coupled flow and sediment transport model to investigate the flow and breaching processes with and without waves. Bed change and variable flow density are included in the flow continuity and momentum equations to consider the impacts of sediment transport. The model adopts the non-equilibrium approach for total-load sediment transport and specifies different repose angles to handle non-cohesive embankment slope avalanching. The equations are solved using an explicit finite volume method on a rectangular grid with the improved Godunov-type central upwind scheme and the nonnegative reconstruction of the water depth method to handle mixed-regime flows near the breach. The model has been tested against two sets of experimental data which show that it well simulates the flow characteristics, bed changes, and sediment transport. It is then applied to analyze flow and morphologic changes by overtopping flow with and without waves. The simulated bed change and breach cross-section shape show a significant difference if waves are considered. Erosion by flow without waves mainly occurs at the breach and is dominated by vertical erosion at the initial stage followed by the lateral erosion. With waves, the flow overtops the entire length of the dune to cause faster erosion along the entire length. Erosion mainly takes place at the upper layer at the initial stage and gradually accelerates as the height of the dune reduces and flow discharge increases, which indicates the simulated results with waves shall be further verified by physical experimental evidence.