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On velocity profiles and stresses in sheared and vibrated granular systems under variable gravity

机译:重力作用下的剪切和振动颗粒系统的速度分布和应力

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We employ discrete element three-dimensional simulations that include realistic modeling of physical system boundaries to determine the influence of gravity on velocity profiles and stresses for frictional inelastic particles that are confined in an angular Couette cell, and sheared by a rotated upper wall. In addition to Earth gravity, we consider other gravitational fields, in particular those of the Moon and Mars. The computational techniques are based on hard-sphere simulations of polydisperse particles at relatively high volume fraction (50-55%). We find that the presence of gravity induces significant changes of the velocity profiles and stresses. One important nondimensional parameter in the problem is shown to be I-Omega=gamma d/root P-g/rho(s), where gamma is the imposed shear rate, P-g is the weight of the system per unit area due to gravity, and rho(s) is the solid density. We also consider systems that are vibrated in addition to being sheared, since vibrations are one of several important methods for agitating (e.g., fluidizing and/or unjamming) granular systems. We find that the introduction of nondimensional acceleration Gamma=a(2 pi f)(2)/g, where a,f,g are the amplitude and frequency of oscillations, and the acceleration of gravity, explains novel features that develop in these complex granular systems.(c) 2006 American Institute of Physics.
机译:我们采用离散元三维模拟,其中包括物理系统边界的逼真的建模,以确定重力对速度分布和应力的影响,这些摩擦和非弹性摩擦粒子被限制在成角的Couette单元中,并被旋转的上壁剪断。除地球重力外,我们还考虑其他重力场,特别是月球和火星的重力场。计算技术基于相对较高的体积分数(50-55%)的多分散颗粒的硬球模拟。我们发现重力的存在会引起速度分布和应力的显着变化。问题中一个重要的无量纲参数显示为I-Omega = gamma d /根Pg / rho(s),其中gamma是施加的剪切速率,Pg是由于重力引起的每单位面积系统的重量,rho (s)是固体密度。我们还考虑除了剪切之外还振动的系统,因为振动是搅动(例如,流化和/或堵塞)颗粒系统的几种重要方法之一。我们发现,引入无量纲加速度Gamma = a(2 pi f)(2)/ g,其中a,f,g是振荡的振幅和频率以及重力加速度,解释了这些复杂现象中发展起来的新颖特征(c)2006美国物理研究所。

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