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arXiv 1306.6037cond-mat.softphysics.flu-dyn
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高速穿越静水颗粒介质的入侵体的升力和阻力

Lift and drag in intruders moving through hydrostatic granular media at high speeds

Fabricio Q. Potiguar, Yang Ding

摘要:

最近,实验表明,入侵者水平拖动通过密集,流体静力学颗粒填料的力主要取决于当地的表面取向,可以看作是施加在小表面元素的力的总和。为了更深入地理解这种力,我们进行了二维软球分子动力学模拟,在类似的设置,入侵者通过50-50双分散颗粒填料,直径为0.30和0.34厘米。我们测量,对于圆形和半圆形,平行(阻力)和垂直(升力)的阻力方向的阻力速度的函数,与V=10.3-309厘米/秒,和入侵者的深度,与D=3.75-37.5厘米。作用在入侵者上的阻力随V和D单调增加,并且在圆上更大。然而,升力并不单调地依赖于V和D,这种关系受入侵者形状的影响。垂直力对于半圆是负的,但对于V和D的小范围,我们测量到正升力。我们没有发现圆上升力的符号变化,它总是正的。的非单调依赖的解释是有关的减少接触的入侵者V的增加。这在性质上类似于超音速气流从障碍物上脱离。分离的图片支持的模拟测量的速度场周围的入侵者和力剖面上测得的表面。

英文摘要:

Recently, experiments showed that forces on intruders dragged horizontally through dense, hydrostatic granular packings mainly depend on the local surface orientation and can be seen as the sum of the forces exerted on small surface elements. In order to understand such forces more deeply, we perform 2D soft-sphere molecular dynamics simulation, on similar set up, of an intruder dragged through a 50-50 bi-disperse granular packing, with diameters 0.30 and 0.34 cm. We measure, for both circular and half-circle shapes, the forces parallel (drag) and perpendicular (lift) to the drag direction as functions of the drag speed, with V=10.3-309 cm/s, and intruder depths, with D=3.75-37.5 cm. The drag forces on an intruder monotonically increase with V and D, and are larger for the circle. However, the lift force does not depend monotonically on V and D, and this relationship is affected by the shape of the intruder. The vertical force was negative for the half-circle, but for a small range of V and D, we measure positive lift. We find no sign change for the lift on the circle, which is always positive. The explanation for the nonmonotonic dependence is related to the decrease in contacts on the intruder as V increases. This is qualitatively similar to supersonic flow detachment from an obstacle. The detachment picture is supported by simulation measurements of the velocity field around the intruder and force profiles measured on its surface.

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