用本构方程模拟泥石流的修正颗粒法的发展

Takuro Suzuki, N. Hotta
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引用次数: 5

摘要

本文提出了一种计算泥石流流速和含沙量垂直分布的数值模拟方法。该方法基于运动粒子半隐式(MPS)方法。将Egashira等人的本构方程引入到MPS方法中。利用现有的基于浅水方程的模型和基于MPS方法的模型对泥石流进行了数值模拟。在河床坡度减小的条件下,与实验结果吻合较好,包括在初始沉积过程中形成凸向上的沉积形状。现有的基于浅水方程的模拟方法无法得到初始沉积过程的模拟结果。此外,该模型还可以在上、下两层水流方向不同的情况下进行自然溃坝的数值模拟。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Development of Modified Particles Method for Simulation of Debris Flow Using Constitutive Equations
We propose a numerical simulation method for calculating the vertical distributions of the flow velocity and the sediment concentration in debris flows. Our method is based on the moving particle semi-implicit (MPS) method. We introduce the constitutive equations of Egashira et al. to the MPS method. Numerical simulations of the debris flow are performed by using an existing model based on a shallow water equation, along with our model based on the MPS method. In the condition where the riverbed gradient becomes less steep, there is good agreement with experimental results, including those involving the formation of a convex upward deposition shape in the initial deposition process. Results for the initial deposition process are not produced with existing simulation method based on a shallow water equation. Further, our model can yield clear results when the upper and lower layers have different flow directions in a numerical simulation of the collapse of a natural dam by overtopping.
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