Agudo José R, Han Jiwon, Park Jinyoung, Kwon Sinyoung, Loekman Soebiakto, Luzi Giovanni, Linderberger Christoph, Delgado Antonio, Wierschem Andreas
Institute of Fluid Mechanics, FAU Busan Campus, University of Erlangen-Nuremberg;
Institute of Fluid Mechanics, FAU Busan Campus, University of Erlangen-Nuremberg.
J Vis Exp. 2018 Feb 22(132):57238. doi: 10.3791/57238.
Two different experimental methods for determining the threshold of particle motion as a function of geometrical properties of the bed from laminar to turbulent flow conditions are presented. For that purpose, the incipient motion of a single bead is studied on regular substrates that consist of a monolayer of fixed spheres of uniform size that are regularly arranged in triangular and quadratic symmetries. The threshold is characterized by the critical Shields number. The criterion for the onset of motion is defined as the displacement from the original equilibrium position to the neighboring one. The displacement and the mode of motion are identified with an imaging system. The laminar flow is induced using a rotational rheometer with a parallel disk configuration. The shear Reynolds number remains below 1. The turbulent flow is induced in a low-speed wind tunnel with open jet test section. The air velocity is regulated with a frequency converter on the blower fan. The velocity profile is measured with a hot wire probe connected to a hot film anemometer. The shear Reynolds number ranges between 40 and 150. The logarithmic velocity law and the modified wall law presented by Rotta are used to infer the shear velocity from the experimental data. The latter is of special interest when the mobile bead is partially exposed to the turbulent flow in the so-called hydraulically transitional flow regime. The shear stress is estimated at onset of motion. Some illustrative results showing the strong impact of the angle of repose, and the exposure of the bead to shear flow are represented in both regimes.
本文介绍了两种不同的实验方法,用于确定从层流到湍流条件下,颗粒运动阈值与床层几何特性之间的函数关系。为此,在由单层大小均匀的固定球体组成的规则基底上研究单个珠子的初始运动,这些球体以三角形和正方形对称规则排列。阈值由临界希尔兹数表征。运动开始的判据定义为从原始平衡位置到相邻平衡位置的位移。位移和运动模式通过成像系统识别。层流由具有平行盘配置的旋转流变仪产生。剪切雷诺数保持在1以下。湍流在具有开放式试验段的低速风洞中产生。通过鼓风机上的变频器调节风速。用连接到热膜风速仪的热线探头测量速度剖面。剪切雷诺数在40到150之间。利用对数速度定律和罗塔提出的修正壁面定律,从实验数据中推断剪切速度。当移动珠子在所谓的水力过渡流态下部分暴露于湍流时,后者特别重要。在运动开始时估计剪切应力。在两种流态下都给出了一些说明性结果,显示了休止角和珠子暴露于剪切流的强烈影响。