Amon Daniel L, Niculescu Tatiana, Utter Brian C
Department of Physics and Astronomy, James Madison University, Harrisonburg, Virginia 22807, USA.
Phys Rev E Stat Nonlin Soft Matter Phys. 2013 Jul;88(1):012203. doi: 10.1103/PhysRevE.88.012203. Epub 2013 Jul 11.
We present statistics on granular avalanches in a rotating drum with and without imposed vertical vibration. The experiment consists of a quasi-two-dimensional, vertical drum containing pentagonal particles and rotated at a constant angular velocity. The drum rests on an electromagnetic shaker to allow vibration of the assembly as it rotates. We measure time series of the slope of the interface and find that the critical angle for slope failure θ(c) and the resulting angle of repose θ(r) are broadly distributed with an approximate power-law distribution of avalanches θ(c)-θ(r) for large avalanches. The faceted pentagonal grains used lead to significant interlocking with critical and repose angles (θ(c)≈45° and θ(r)≈39°) larger than experiments using spherical grains, even with vibration, and avalanche magnitudes correlated with the prior build-up and anti-correlated with the prior avalanche. We find that the stability of the assembly increases with small vibrations and is destabilized at vibration amplitudes above a dimensionless acceleration (peak acceleration divided by acceleration due to gravity) of Γ=0.2. We also study history dependence of the avalanches by periodically oscillating the drum to compare the initial avalanche upon reversal of shear to steady-state distributions for avalanches during continuous rotation. We observe history dependence as an initial decrease in critical angle upon reversal of the drum rotation direction, indicating that a texture is induced to resist continued shear such that the surface is weaker to reversals in shear direction. Memory of this history is removed by sufficient external vibration (Γ≥0.8), which leads to compaction and relaxation of the surface layer grains responsible for avalanching dynamics, as initial and steady-state avalanche distributions become indistinguishable.
我们给出了在有和没有垂直振动的旋转鼓中颗粒雪崩的统计数据。实验包括一个准二维的垂直鼓,鼓中装有五边形颗粒,并以恒定角速度旋转。鼓放置在电磁振动台上,以便在旋转时使组件振动。我们测量了界面斜率的时间序列,发现边坡失稳的临界角θ(c)和由此产生的休止角θ(r)分布广泛,对于大型雪崩,雪崩θ(c)-θ(r)大致呈幂律分布。所使用的多面五边形颗粒导致显著的互锁,其临界角和休止角(θ(c)≈45°和θ(r)≈39°)比使用球形颗粒的实验结果更大,即使在有振动的情况下也是如此,并且雪崩大小与先前的堆积相关,与先前的雪崩呈反相关。我们发现,组件的稳定性随着小振动而增加,并且在无量纲加速度(峰值加速度除以重力加速度)Γ=0.2以上的振动幅度下会失稳。我们还通过周期性地振荡鼓来研究雪崩的历史依赖性,并比较剪切反转时的初始雪崩与连续旋转期间雪崩的稳态分布。我们观察到历史依赖性表现为鼓旋转方向反转时临界角的初始减小,这表明诱导了一种纹理来抵抗持续的剪切,使得表面对剪切方向的反转更脆弱。通过足够的外部振动(Γ≥0.8)可以消除这种历史记忆,这会导致负责雪崩动力学的表层颗粒压实和松弛,因为初始和稳态雪崩分布变得无法区分。