Force and torque acting on particles in a transitionally rough open channel flow
arXiv:1108.5924 · doi:10.1017/jfm.2011.311
Abstract
Direct numerical simulation of open channel flow over a geometrically rough wall has been performed at a bulk Reynolds number of approximately 2900. The wall consisted of a layer of spheres in a square arrangement. Two cases have been considered. In the first case the spheres are small (with diameter equivalent to 10.7 wall units) and the limit of the hydraulically smooth flow regime is approached. In the second case the spheres are more than three times larger (49.3 wall units) and the flow is in the transitionally rough flow regime. Special emphasis is given on the characterisation of the force and torque acting on a particle due to the turbulent flow. It is found that in both cases the mean drag, lift and spanwise torque are to a large extent produced at the top region of the particle surface. The intensity of the particle force fluctuations is significantly larger in the large-sphere case, while the trend differs for the fluctuations of the individual components of the torque. A simplified model is used to show that the torque fluctuations might be explained by the spheres acting as a filter with respect to the size of the flow scales which can effectively generate torque fluctuations. Fluctuations of both force and torque are found to exhibit strongly non-Gaussian probability density functions with particularly long tails, an effect which is more pronounced in the small-sphere case. Some implications of the present results for sediment erosion are briefly discussed.
accepted for publication in J. Fluid Mech. (2011)
References in corpus (2)
Cited by in corpus (13)
- Sedimentation of a dilute suspension of rigid spheres at intermediate Galileo numbers: the effect of clustering upon the particle motion
- DNS of horizontal open channel flow with finite-size, heavy particles at low solid volume fraction
- Direct numerical simulation of pattern formation in subaqueous sediment
- Interface-resolved direct numerical simulation of the erosion of a sediment bed sheared by laminar channel flow
- Formation of sediment patterns in channel flow: minimal unstable systems and their temporal evolution
- Forcing homogeneous turbulence in DNS of particulate flow with interface resolution and gravity
- DNS-based characterization of pseudo-random roughness in minimal channels
- On the role of turbulent large-scale streaks in generating sediment ridges
- Direct numerical simulation of open-channel flow over a fully-rough wall at moderate relative submergence
- Direct numerical simulations of Taylor--Couette turbulence: the effect of sand grain roughness
- Spatial and temporal scales of force and torque acting on wall-mounted spherical particles in open channel flow
- The effect of spanwise heterogeneous surfaces on mixed convection in turbulent channels
- Results from Particle-Resolved Simulations