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Study of sedimentation of non-cohesive particles via CFD-DEM simulations

机译:通过CFD-DEM模拟研究非粘性颗粒的沉降

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摘要

The sedimentation process of granular materials exists ubiquitously in nature and many fields which involve the solid-liquid separation. This paper employs the coupled computational fluid dynamics and discrete element method (CFD-DEM) to investigate the sedimentation process of non-cohesive particles, including the hindered settling stage and the deposition stage. Firstly, the coupled CFD-DEM model for sedimentation is validated by the hindered settling velocity at different solid volume concentrations of suspension phi(0), i.e., phi(0) = 0.05-0.6. Two typical modes of sedimentation are also presented by the concentration profiles and the equal-concentration lines. Then, the comparisons between mono-and poly-dispersed particle system are detailed. In the sedimentation of the poly-dispersed particle system, the segregation phenomenon is simulated. Furthermore, this segregation effect reduces with the increase of the initial solid concentration of suspension. From the simulations, the contact force between every pair of particles can be obtained, hence we demonstrate the "effective stress principle" from the view of the particle contact force by giving the correspondence between the particle contact force and the "effective stress", which is a critical concept of soil mechanics. Moreover, the deposition stage can be simulated by CFD-DEM method, therefore the solid concentrations of sediment bed phi(max) on different conditions are studied. Based on the simulation results of phi(max) and the theory of sedimentation, this paper also discusses a method to calculate the critical time when sedimentation ends of two typical modes of sedimentation.
机译:颗粒状物质的沉降过程在自然界普遍存在,涉及固液分离的许多领域。本文采用耦合流体动力学和离散元方法(CFD-DEM)研究非粘性颗粒的沉降过程,包括受阻沉降阶段和沉降阶段。首先,通过在悬浮液phi(0)的不同固体体积浓度(即phi(0)= 0.05-0.6)下的受阻沉降速度验证了耦合的CFD-DEM沉降模型。浓度分布图和等浓度线也显示了两种典型的沉积模式。然后,详细介绍了单分散和多分散颗粒体系之间的比较。在多分散颗粒系统的沉降过程中,模拟了偏析现象。此外,这种分离作用随悬浮液的初始固体浓度的增加而降低。从模拟中,可以获得每对颗粒之间的接触力,因此,通过给出颗粒接触力和“有效应力”之间的对应关系,我们从颗粒接触力的角度证明了“有效应力原理”。是土壤力学的一个重要概念。此外,沉积阶段可以通过CFD-DEM方法进行模拟,因此研究了不同条件下沉积床phi(max)的固体浓度。基于phi(max)的模拟结果和沉降理论,本文还讨论了一种计算两种典型沉降模式沉降结束时的临界时间的方法。

著录项

  • 来源
    《Granular matter》 |2018年第1期|4.1-4.17|共17页
  • 作者单位

    Zhejiang Univ, Coll Civil Engn & Architecture, Res Ctr Coastal & Urban Geotech Engn, Anzhong Bldg A404, Hangzhou 310058, Zhejiang, Peoples R China;

    Virginia Tech, Dept Aerosp & Ocean Engn, 311-A Randolph Hall 0203, Blacksburg, VA 24061 USA;

    Zhejiang Univ, Coll Civil Engn & Architecture, Res Ctr Coastal & Urban Geotech Engn, Anzhong Bldg A404, Hangzhou 310058, Zhejiang, Peoples R China;

    Zhejiang Univ, Coll Civil Engn & Architecture, Inst Disaster Prevent Engn, Anzhong Bldg B832, Hangzhou 310058, Zhejiang, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Sedimentation; Hindered settling; CFD-DEM; Effective stress; Sediment bed density; Critical time;

    机译:泥沙;沉降;CFD-DEM;有效应力;泥床密度;临界时间;

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