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应力通过无摩擦颗粒材料的传播。

Stress propagation through frictionless granular material.

作者信息

Tkachenko A V, Witten T A

机构信息

The James Franck Institute, The University of Chicago, Chicago, Illinois 60637, USA.

出版信息

Phys Rev E Stat Phys Plasmas Fluids Relat Interdiscip Topics. 1999 Jul;60(1):687-96. doi: 10.1103/physreve.60.687.

Abstract

We examine the network of forces to be expected in a static assembly of hard, frictionless spherical beads of random sizes, such as a colloidal glass. Such an assembly is minimally connected: the ratio of constraint equations to contact forces approaches unity for a large assembly. However, the bead positions in a finite subregion of the assembly are underdetermined. Thus to maintain equilibrium, half of the exterior contact forces are determined by the other half. We argue that the transmission of force may be regarded as unidirectional, in contrast to the transmission of force in an elastic material. Specializing to sequentially deposited beads, we show that forces on a given buried bead can be uniquely specified in terms of forces involving more recently added beads. We derive equations for the transmission of stress averaged over scales much larger than a single bead. This derivation requires the ansatz that statistical fluctuations of the forces are independent of fluctuations of the contact geometry. Under this ansatz, the d(d+1)/2-component stress field can be expressed in terms of a d-component vector field. The procedure may be generalized to nonsequential packings. In two dimensions, the stress propagates according to a wave equation, as postulated in recent work elsewhere. We demonstrate similar wave-like propagation in higher dimensions, assuming that the packing geometry has uniaxial symmetry. In macroscopic granular materials we argue that our approach may be useful even though grains have friction and are not packed sequentially.

摘要

我们研究了由随机大小的硬的、无摩擦球形珠子组成的静态集合体(如胶体玻璃)中预期的力网络。这样的集合体连接最少:对于大型集合体,约束方程与接触力的比率接近1。然而,集合体有限子区域内珠子的位置是不确定的。因此,为了保持平衡,一半的外部接触力由另一半确定。我们认为,与弹性材料中的力传递不同,力的传递可以被视为单向的。专门针对顺序沉积的珠子,我们表明,给定埋入珠子上的力可以根据涉及最近添加珠子的力唯一确定。我们推导了在比单个珠子大得多的尺度上平均的应力传递方程。这种推导需要假设力的统计涨落与接触几何形状的涨落无关。在这个假设下,d(d + 1)/2 分量的应力场可以用一个d分量的矢量场来表示。该过程可以推广到非顺序堆积。在二维中,应力根据波动方程传播,正如其他地方最近的工作所假设的那样。假设堆积几何形状具有单轴对称性,我们在更高维度上证明了类似的波动传播。在宏观颗粒材料中,我们认为即使颗粒有摩擦力且不是顺序堆积的,我们的方法也可能有用。

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