首页> 外文会议>ASME international mechanical engineering congress and exposition;IMECE2011 >NUMERICAL SIMULATIONS OF NON-NEWTONIAN GEOPHYSICAL FLOWS USING SMOOTHED PARTICLE HYDRODYNAMICS (SPH) METHOD:A RHEOLOGICAL ANALYSIS
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NUMERICAL SIMULATIONS OF NON-NEWTONIAN GEOPHYSICAL FLOWS USING SMOOTHED PARTICLE HYDRODYNAMICS (SPH) METHOD:A RHEOLOGICAL ANALYSIS

机译:非牛顿地球物理流动的数值模拟:流变分析

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This paper presents computational results for two-dimensional (2-D) simulations of geophysical flows using the Smoothed Particle Hydrodynamics (SPH) method. The basic equations solved are the incompressible mass conservation and Navier-Stokes equations, and the discretization is carried out using the SPH method. The simulations are carried out for two problems. The first problem involved a 2-D dam-break problem with mud flow. The second problem involved non-Newtonian flow of deformable landslide on a mild slope. In both the simulations, the flow is assumed to be incompressible. In the present study, the mud flow materials are represented as non-Newtonian fluids with a Bingham model. The effects of the rheological formulation are assessed for the predicted mudflow shape. The simulation results are compared with the experimental data available in open literature. The velocity profiles and the free surface shape are in good agreement with the experimental data. To distinguish between the non-Newtonian model simulations and the Newtonian model, the dam-break simulations were also carried out using water and Newtonian models. The simulations reveal several distinctive flow features between the Newtonian and non-Newtonian approaches. The results of the simulations are of engineering interest in mitigation of natural hazards such as debris flows.
机译:本文介绍了使用平滑粒子流体动力学(SPH)方法对地球物理流进行二维(2-D)模拟的计算结果。求解的基本方程是不可压缩的质量守恒方程和Navier-Stokes方程,离散化是使用SPH方法进行的。针对两个问题进行了仿真。第一个问题涉及泥浆流的二维溃坝问题。第二个问题涉及在平缓坡度上非牛顿可变形滑坡的流动。在两个模拟中,均假定流动不可压缩。在本研究中,采用宾厄姆模型将泥浆流物质表示为非牛顿流体。针对预计的泥流形状评估流变配方的影响。仿真结果与公开文献中提供的实验数据进行了比较。速度分布和自由表面形状与实验数据非常吻合。为了区分非牛顿模型模拟和牛顿模型,还使用水和牛顿模型进行了溃坝模拟。模拟揭示了牛顿方法和非牛顿方法之间的几个独特的流动特征。模拟的结果对于减轻自然灾害(如泥石流)具有工程意义。

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