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Convective roll patterns in vertically vibrated beds of granules

机译:垂直振动颗粒床中的对流辊型

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This paper describes dynamic transition of convection motions of granules under vertical vibrations. The granule motion of one convection mode, which has been studied by many authors, is downward along the vertical side walls and upward in the middle forming a heap. Tile present study focuses on the granule motion of the other convection mode that occurs in rectangular containers: granules move upward along the vertical side walls, anti downwards in the middle forming a valley. This latter convection mode is stable enough to yield multiple pairs of convection rolls, The number of convection rolls is strongly dependent on the vibrational acceleration, granular size, and tu a lesser extent on frequency, given the bed height and width. The critical vibrational acceleration, where a transition occurs between the two convection modes, is dependent on the bed height but not on the bed width in the range investigated (100-200 mm). In the case of large granules (mean diameter (d) over bar greater than or equal to 0.78 mm) a chaotic state (where convective motion of granules ceases to exist) is found to appear in between the two convection modes mentioned above.
机译:本文描述了颗粒在垂直振动条件下对流运动的动态转变。许多作者已经研究了一种对流模式的颗粒运动,该运动沿竖直侧壁向下,在中间沿向上形成堆。目前的研究集中在矩形容器中另一种对流模式下的颗粒运动:颗粒沿垂直侧壁向上移动,中间沿向下移动形成山谷。后一种对流模式足够稳定,可以产生多对对流辊。给定床的高度和宽度,对流辊的数量在很大程度上取决于振动加速度,颗粒尺寸,并且在频率上的影响程度较小。在两个对流模式之间发生过渡的临界振动加速度取决于床高,而不取决于床宽(100-200 mm)。在大颗粒的情况下(棒上的平均直径(d)大于或等于0.78mm),发现在上述两种对流模式之间出现混沌状态(颗粒的对流运动不再存在)。

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