Gland N, Wang P, Makse H A
Levich Institute and Physics Department, City College of New York, New York, NY 10031, USA.
Eur Phys J E Soft Matter. 2006 Jun;20(2):179-84. doi: 10.1140/epje/i2006-10012-6. Epub 2006 Jun 23.
We investigate the Green function of two-dimensional dense random packings of grains in order to discriminate between the different theories of stress transmission in granular materials. Our computer simulations allow for a detailed quantitative investigation of the dynamics which is difficult to obtain experimentally. We show that both hyperbolic and parabolic models of stress transmission fail to predict the correct stress distribution in the studied region of the parameters space. We demonstrate that the compressional and shear components of the stress compare very well with the predictions of isotropic elasticity for a wide range of pressures and porosities and for both frictional and frictionless packings. However, the states used in this study do not include the critical isostatic point for frictional particles, so that our results do not preclude the fact that corrections to elasticity may appear at the critical point of jamming, or for other sample preparation protocols, as discussed in the main text. We show that the agreement holds in the bulk of the packings as well as at the boundaries and we validate the linear dependence of the stress profile width with depth.
我们研究了颗粒二维密集随机堆积的格林函数,以便区分颗粒材料中应力传递的不同理论。我们的计算机模拟允许对动力学进行详细的定量研究,而这很难通过实验获得。我们表明,应力传递的双曲线模型和抛物线模型都无法预测参数空间研究区域内的正确应力分布。我们证明,在广泛的压力和孔隙率范围内,以及对于有摩擦和无摩擦的堆积,应力的压缩分量和剪切分量与各向同性弹性的预测非常吻合。然而,本研究中使用的状态不包括有摩擦颗粒的临界等静点,因此我们的结果并不排除这样一个事实,即如正文所讨论的,在堵塞临界点或其他样品制备方案中可能会出现对弹性的修正。我们表明,这种一致性在堆积体的主体以及边界处都成立,并且我们验证了应力分布宽度与深度的线性关系。