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A model of mudflow propagation downstream from the Grohovo landslide near the city of Rijeka (Croatia)

机译:里耶卡(克罗地亚)附近格罗霍沃滑坡下游的泥石流传播模型

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摘要

Mudflows regularly generate significant human and property losses. Analyzing mudflows is important to assess the risks and to delimit vulnerable areas where mitigation measures are required. The smoothed-particle hydrodynamics (SPH) model adopted here considers, in two phases, a granular skeleton with voids filled with either water or mud. The SPH depth-integrated numerical model (Pastor et al., 2009a) used for the present simulations is a 2-D model capable of predicting the runout distance, flow velocity, deposition pattern and the final volume of mudflows. It is based on mathematical and rheological models.
机译:泥流经常会造成重大的人员和财产损失。分析泥石流对于评估风险和划定需要采取缓解措施的脆弱区域很重要。此处采用的平滑粒子流体动力学(SPH)模型分两个阶段考虑了一个具有填充水或泥浆的空隙的粒状骨架。用于本模拟的SPH深度积分数值模型(Pastor等,2009a)是一种能够预测跳动距离,流速,沉积模式和泥浆最终体积的二维模型。它基于数学和流变模型。

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