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Avalanches on a conical bead pile: scaling with tuning parameters

机译:圆锥形珠堆上的雪崩:使用调整参数缩放

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Uniform spherical beads were used to explore the scaling behavior of a granular system near its critical angle of repose on a conical 3D bead pile. We found two tuning parameters that could take the system to a critical point. The existence of those tuning parameters violates the fundamental assumption of self-organized criticality, which proposed that complex dynamical systems self-organize to a critical point without need for tuning. Our avalanche size distributions were well described by a simple power-law, as is characteristic of a critical point, with the power r = 1.5 when dropping beads slowly onto the apex of a bead pile from a small height. However, we could also move the system from the critical point using either of two tuning parameters: the height from which the beads fell onto the top of the pile or the region over which the beads struck the pile. As the drop height increased, the system did not reach the critical point yet the resulting distributions were independent of the bead mass, coefficient of friction, or coefficient of restitution. All our apex-dropping distributions for any type of bead (glass, stainless steel, zirconium) showed universality by scaling onto a common curve with x = 1.5 and σ = 1.0, where 1 /σ is the power of the tuning parameter. From independent calculations using the moments of the distribution, we find values for t = 1.6±0.1and σ =0.91 ±0.15. When beads were dropped across the surface of the pile instead of solely on the apex, then the system also moved from the critical point and again the avalanche size distributions fell on a common curve when scaled similarly using the same values of r and a. We also observed that an hep structure on the base of the pile caused an emergent structure in the pile that had six faces with some fcc or hcp structure; this structure did not affect the distribution of avalanche sizes.
机译:使用均匀的球形珠子来探索颗粒系统在圆锥形3D珠子堆上的临界休止角附近的缩放行为。我们发现了两个调整参数,它们可能会使系统达到临界点。这些调整参数的存在违反了自组织关键性的基本假设,即假设复杂的动力学系统无需调整即可自组织至临界点。我们的雪崩尺寸分布可以通过简单的幂定律很好地描述,这是临界点的特征,当从很小的高度缓慢将珠子滴到珠子堆的顶点时,功率r = 1.5。但是,我们还可以使用以下两个调整参数之一将系统从临界点移开:珠子掉落到绒头顶部的高度或珠子撞到绒头的区域。随着下落高度的增加,系统尚未达到临界点,但最终的分布与珠子质量,摩擦系数或恢复系数无关。我们对任何类型的珠子(玻璃,不锈钢,锆)的所有下降点分布都显示出通用性,方法是缩放到x = 1.5和σ= 1.0的共同曲线上,其中1 /σ是调整参数的幂。从使用分布矩的独立计算中,我们得出t = 1.6±0.1和σ= 0.91±0.15的值。当珠子滴落在绒头表面而不是仅滴在顶点上时,系统也从临界点移开,当使用相同的r和a值进行类似缩放时,雪崩尺寸分布再次落在一条公共曲线上。我们还观察到,桩基上的一个麻结构会在桩中产生一个具有六个面的带有fcc或hcp结构的突出结构。这种结构不会影响雪崩尺寸的分布。

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