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Simulation of Water-Soil-Structure Interactions Using Incompressible Smoothed Particle Hydrodynamics

机译:使用不可压缩平滑粒子动力学模拟水土结构相互作用

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摘要

In the present work, an incompressible smoothed particle hydrodynamic (SPH) method is introduced to simulate water-soil-structure interactions. In the current calculation, the water is modelled as a Newtonian fluid. The soil is modelled in two different cases. In the first case, the granular material is considered as a fluid where a Bingham type constitutive model is proposed based on Mohr-Coulomb yield-stress criterion, and the viscosity is derived from the cohesion and friction angle. In addition, the fictitious suspension layers between water and soil depending on the concentration of soil are introduced. In the second case, Hooke's law introduces elastic soil. In ISPH, the pressure is evaluated by solving the pressure Poisson equation using a semi-implicit algorithm based on the projection method and an eddy viscosity for water is modelled by a large eddy simulation with the Smagorinsky model. In the proposed ISPH method, the pressure is stabilized to simulate the multiphase flow between soil and water. Numerical experiments for water-soil suspension flow of Louvain erosional dam break with flat soil foundation, is simulated and validated using 3D-ISPH method. Coupling between water-soil interactions with different solid structures are simulated. The results revealed that, the suspension layers with the Bingham model of soil gives more accurate results in the experiment as compared to the case of the Bingham model without suspension layers. In addition, the elastic soil model by the Hooke's law can simulate soil hump accurately as compared to the Bingham model. From the simulations, avoiding erosion behind the structure for preventing the structure break during flood are investigated by using an extended structure or a wedge structure.
机译:在本作工作中,引入了不可压缩的平滑颗粒流体动力学(SPH)方法以模拟水土结构相互作用。在目前的计算中,水被建模为牛顿液。土壤模拟两种不同的情况。在第一种情况下,粒状材料被认为是基于MoHR-Coulomb屈服 - 应力标准提出弯曲型本构模型的流体,并且粘度源自粘性和摩擦角。此外,引入了根据土壤浓度的水和土壤之间的虚拟悬浮层。在第二种情况下,胡克的法律介绍了弹性土壤。在ISPH中,通过使用基于投影方法的半隐式算法求解压力泊松方程来评估压力,并通过用SMAGORINSKY模型进行大型涡流模拟模拟水的涡流粘度。在所提出的ISPH方法中,压力稳定以模拟土壤和水之间的多相流。利用3D-ISPH方法模拟和验证了Louvain腐蚀坝突破水土悬架流量的数值实验。模拟与不同固体结构的水土相互作用之间的耦合。结果表明,与无悬浮层的弯曲模型的情况相比,具有宾果型土壤模型的悬浮层在实验中提供了更准确的结果。此外,与宾厄姆型号相比,胡克定律的弹性土壤模型可以确定地模拟土壤驼峰。从模拟中,通过使用延伸的结构或楔形结构来研究防止防洪过程中的结构破裂的结构背后的侵蚀。

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  • 来源
    《Computers, Materials & Continua》 |2020年第1期|205-224|共20页
  • 作者单位

    Department of Mathematics College of Science King Khalid University Abha 62529 Saudi Arabia Department of Mathematics Faculty of Science South Valley University Qena 83523 Egypt;

    Civil Engineering Department Kyushu University Fukuoka 819-0395 Japan;

    Electrical Engineering Department College of Engineering Prince Sattam Bin Abdulaziz University Wadi Addwasir 11991 Saudi Arabia Electrical Engineering Department Faculty of Engineering Aswan University Aswan 81542 Egypt;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Bingham model; ISPH method; rigid body; water-soil interactions;

    机译:宾厄姆模特;ISPH方法;刚体;水土互动;

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