A 2D numerical model for simulating landslide dam failure and induced morphological changes considering multi-layer and non-uniform sediments

Jiangtao Yang, S. Soares-Frazão, Zhenming Shi, Danyi Shen
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Abstract

Landslide dams are formed by the blockage of rivers with landslides, or any debris flows. Such dams are prone to failure and therefore, simulation of their failure and induced morphological changes is of great importance for hazard mitigation. Multi-layer and non-uniform sediments are usually observed in landslide dam materials, but these are rarely considered in simulations. In this paper, a two-dimensional numerical model considering multi-layered and non-uniform sediments is proposed. The model solves the shallow water equations, the Exner equation considering the different size fractions and Hirano's active layer equation based on a finite volume scheme in a weakly coupled approach. Two experimental tests are used to assess the applicability and accuracy of the model. The results show that it can well simulate the flow and morphological changes, as well as the surface coarsening and fining phenomena related to multi-layer and non-uniform sediments. The numerical results of dam failure process and morphological changes are in overall good agreement with the experiments, but the peak discharge and bed elevation tend to be underestimated when finer material is considered. Finally, the influence of sediments fractions and active layer depth on numerical results, as well as the limitations of the model are discussed.
考虑到多层和非均匀沉积物的滑坡溃坝和诱发形态变化的二维数值模拟模型
滑坡坝是由山体滑坡或任何泥石流堵塞河流而形成的。这种坝很容易垮塌,因此,模拟其垮塌和诱发的形态变化对减轻危害非常重要。在滑坡坝体材料中通常会观察到多层和不均匀沉积物,但在模拟中却很少考虑这些因素。本文提出了一种考虑多层和非均匀沉积物的二维数值模型。该模型以弱耦合方法求解了浅水方程、考虑了不同粒径分数的 Exner 方程以及基于有限体积方案的平野活动层方程。两个实验测试用于评估模型的适用性和准确性。结果表明,该模型可以很好地模拟与多层和非均匀沉积物有关的流动和形态变化,以及表面粗化和细化现象。溃坝过程和形态变化的数值结果与试验结果总体吻合,但当考虑更细的材料时,峰值排水量和河床高程有被低估的趋势。最后,讨论了沉积物比例和活动层深度对数值结果的影响以及模型的局限性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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