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Granular wave patterns in a horizontal rotating cylinder.

机译:水平旋转圆柱体中的粒状波型。

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摘要

It is well known that the front of a fluid sheet flowing over an inclined surface is unstable to spanwise perturbations. This instability, which manifests itself in the formation of fingers of fairly constant wavelength, is thought to reflect a competition between bulk viscosity and surface tension.;Recent experiments have shown that the front of a granular layer flowing over an inclined surface may also develop fingers. Because the materials used in these experiments are cohesionless and, thus, unable to sustain surface tension, this instability is surprising. As an explanation, it has been suggested that frontal finger formation in granular materials is induced by the segregation of coarse, irregularly shaped grains.;We present the results of an experiment involving a thin granular layer flowing within a horizontal cylinder that is rotated about its axis. We uncover an assortment of stationary and temporally varying spatial patterns, patterns that bear close resemblance to aeolian ripples and sand dunes. In particular, we find that, even when the medium is well sieved and consists of nearly uniform spherical grains, its front may develop fingers, suggesting that, in general flow configurations, mechanisms other than grain segregation may drive the instability of a straight front.;As a step toward understanding these mechanisms, we develop a system of evolution equations that accounts for the steady motion of grains with the cylinder and for the motion of saltating and reptating grains. We develop a numerical algorithm for the solution of these equations and use this algorithm to determine a dispersion relation for the growth rate in terms of the wave number of frontal disturbances. We find that the model is able to predict some of the qualitative features observed from our rotating cylinder experiment.;Our long-term objective is to combine our experimental and computational results to determine the values of the critical constitutive parameters that appear in our theory.
机译:众所周知,在倾斜表面上流动的流体板的前部对于翼展方向的扰动是不稳定的。这种不稳定性表现为波长相当恒定的指状物的形成,据认为反映了本体粘度和表面张力之间的竞争。最近的实验表明,在倾斜表面上流动的颗粒层的前端也可能形成指状物。 。由于这些实验中使用的材料无内聚力,因此无法维持表面张力,因此这种不稳定性令人惊讶。作为解释,有人提出颗粒状材料中的前指形成是由于粗大,不规则形状的晶粒的偏析引起的。我们给出了一个实验结果,该实验涉及在水平圆柱体内旋转的薄颗粒层,该水平圆柱体绕其旋转轴。我们发现了各种固定的,随时间变化的空间模式,这些模式与风沙和沙丘非常相似。尤其是,我们发现,即使对介质进行充分筛分并由几乎均匀的球形颗粒组成,其前端也可能会出现指状现象,这表明,在一般的流动配置中,除颗粒偏析以外的其他机制都可能导致直线前端的不稳定性。 ;为进一步了解这些机制,我们开发了一个演化方程系统,该方程组负责谷物随着圆柱体的稳定运动以及谷物盐析和沉淀的运动。我们为这些方程式的求解开发了一种数值算法,并使用该算法根据正面扰动的波数确定了增长率的色散关系。我们发现该模型能够预测从我们的旋转圆筒实验中观察到的一些定性特征。;我们的长期目标是将我们的实验结果和计算结果相结合,以确定出现在理论中的关键本构参数的值。

著录项

  • 作者

    Shen, Qing Amy.;

  • 作者单位

    University of Illinois at Urbana-Champaign.;

  • 授予单位 University of Illinois at Urbana-Champaign.;
  • 学科 Applied Mechanics.;Geophysics.;Engineering Civil.
  • 学位 Ph.D.
  • 年度 2000
  • 页码 135 p.
  • 总页数 135
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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