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风沙流中颗粒剪应力分析 被引量:1

Analysis of Particle Shear Stress in Windblown Sand Movement
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摘要 分析了两种颗粒剪应力的定义,一种来自于颗粒黏性阻力,一种来自于颗粒相雷诺应力。通过建立三维风沙流离散颗粒模型,计算分析了这两种颗粒剪应力的差别。结果表明,除了近地面附近,这两种颗粒剪应力基本相等。而在近地面附近,来自于颗粒相雷诺应力的颗粒剪应力小于来自于颗粒黏性阻力的颗粒剪应力,这种差别的主要原因是由于在近地表而附近,颗粒碰撞会产生附加碰撞剪应力。 Two kinds of particle shear stress are analyzed, one is from drag force, the other is from dispersed phase Reynolds stress. The three-dimensional discrete particle model is developed for windblown sand movement to reveal the difference between the two kinds of particle shear stress. The results show that except the region near the sand bed surface, the two kinds of particle shear stress are almost same. While near the sand bed surface, the particle shear stress from dispersed phase Reynolds stress is less than that from drag force. The main reason is that near the sand bed surface, the additional collision shear stress will be produced due to particle collisions.
作者 亢力强
出处 《工程热物理学报》 EI CAS CSCD 北大核心 2011年第9期1516-1518,共3页 Journal of Engineering Thermophysics
基金 国家自然科学基金资助项目(No.11002028)
关键词 风沙流 颗粒剪应力 三维模拟 windblown sand movement particle shear stress three-dimensional simulation
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参考文献5

  • 1KANG L Q,,LIU D Y.Numerical Investigation of Particle Velocity Distributions in Aeolian Sand Transport[].Geomorphology.2010
  • 2Bagnold R A.The Physics of Blown Sand and Desert Dunes[]..1941
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  • 4Crowe C,Sommerfeld M,Tsuji Y.Multiphase Flows with Droplets and Particles[]..1998
  • 5Greeley R,Iversen J D.Wind as a geological process on Earth, Mars, Venus and Titan[]..1985

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