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EDDA 2.0: integrated simulation of debris flow initiation and dynamics considering two initiation mechanisms

机译:EDDA 2.0:考虑两种启动机制的泥石流启动和动力学综合模拟

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摘要

Climate change is resulting in more frequent rainstorms and more rain-induced debris flows in mountainous areas. The prediction of likely hazard zones is important for debris flow risk assessment and management. Existing numerical methods for debris flow analysis often require the input of hydrographs at prescribed initiation locations, ignoring the initiation process and leading to large uncertainties in debris flow initiation locations, times, and volumes when applied to regional debris flow analysis. The evolution of the flowing mixture in time and space is also barely addressed. This paper presents a new integrated numerical model, EDDA 2.0, to simulate the whole process of debris flow initiation, motion, entrainment, deposition, and property changes. Two physical initiation mechanisms are modelled: transformation from slope failures and surface erosion. Three numerical tests and field application to a catastrophic debris flow event are conducted to verify the model components and evaluate the model performance. The results indicate that the integrated model is capable of simulating the initiation and subsequent flowing process of rain-induced debris flows, as well as the physical evolution of the flowing mixture. The integrated model provides a powerful tool for analysing multi-hazard processes, hazard interactions, and regional debris flow risk assessment in the future.
机译:气候变化导致山区更频繁的暴雨和更多的降雨引起的泥石流。潜在危险区域的预测对于泥石流风险评估和管理非常重要。现有的泥石流分析数值方法通常要求在指定的起始位置输入水文图,而忽略了起始过程,并导致泥石流起始位置,时间和体积的不确定性,将其应用于区域泥石流分析。流动混合物在时间和空间上的演变也几乎没有得到解决。本文提出了一个新的集成数值模型EDDA 2.0,以模拟泥石流引发,运动,夹带,沉积和性质变化的全过程。对两种物理起爆机制进行了建模:斜坡破坏和地面侵蚀的转化。进行了三个数值测试和对灾难性泥石流事件的现场应用,以验证模型组件并评估模型性能。结果表明,该集成模型能够模拟雨水诱发的泥石流的形成和随后的流动过程,以及流动混合物的物理演化过程。集成模型提供了一个强大的工具,可用于分析未来的多灾种过程,病害间的相互作用以及区域性泥石流风险评估。

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