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An experimental study on the flow within two disks

机译:两个磁盘内流量的实验研究

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摘要

The present experimental study concerns the flows generated within the gap of two parallel disks. For the sink-flow the reduction of the cross-sectional area along the flow direction drives the average velocity to increase which is accompanied by a static pressure drop. Due to the non-slip requirement on the upper and lower disks, a boundary layer forms. Increase of the local inertia to viscous forces ratio forces the radial velocity profile to flatten mid-channel. As the radius becomes smaller, the plateau progressively expands towards the wall. The source-flow in comparison to sink-flow, exhibits a reverse behavior of the pressure along the flow direction. However, there is a special phenomenon associated with this type of flow field, which is absent in the previous case. Fluid particles near the walls, moving within an adverse pressure gradient, experience a flow reversal. The later produces a vortex that is clearly evident in the pressure profile. The experimental pressure profiles for sink- and source-flows with swirl indicate a pressure variation qualitatively similar to that without swirl, but the generated strong vortex makes the drop more dramatic. Reasonable correlation for the inflow with the previously developed theory is apparent.
机译:本实验研究涉及在两个平行磁盘的间隙内产生的流动。对于汇流流动,沿着流动方向的横截面积的减小驱动了伴随静压下降的平均速度。由于上磁盘和下盘上的防滑要求,边界层形式。局部惯性增加到粘性力的比例迫使径向速度曲线变平频道。随着半径变小,平台逐渐向墙壁膨胀。与下沉流相比,源流程,沿着流动方向表现出压力的反向行为。然而,存在与这种类型的流场相关的特殊现象,这在前面的情况下不存在。在墙壁附近的流体颗粒,在不利的压力梯度内移动,经历流动反转。后来产生一种在压力曲线中清楚明显的漩涡。用于涡旋的下沉和源流的实验压力曲线表明压力变化与没有涡流的情况相似,但产生的强涡流使下降更加戏剧性。与先前开发的理论的流入的合理相关性是显而易见的。

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