How non-spherical particles orient as they settle in a flow has important practical implications in a number of scientific and engineering problems. In a quiescent fluid, a slowly settling particle orients so that it settles with its broad side first. This is an effect of the torque due to convective inertia of the fluid set in motion by the settling particle, which maximises the drag experienced by the particle. Turbulent flows tend to randomise the particle orientation. Recently the settling of non-spherical particles in turbulence was analysed neglecting the effect of convective fluid inertia, but taking into account the effect of the turbulent fluid-velocity gradients on the particle orientation. These studies reached the opposite conclusion, namely that a rod settles preferentially with its tip first, wheras a disk settles with its edge first, therefore minimizing the drag on the particle. Here, we consider both effects, the convective inertial torque as well as the torque due to fluctuating velocity gradients, and ask under which circumstances either one or the other dominate. To this end we estimate the ratio of the magnitudes of the two torques. Our estimates suggest that the fluid-inertia torque prevails in high-Reynolds number flows. In this case non-spherical particles are expected to settle with a maximal drag. But when the Reynolds number is small then the torque due to fluid-velocity gradients may dominate, causing the particle to settle with its broad side first.
I. INTRODUCTIONThe settling of non-spherical particles in a flow is of importance in several scientific and engineering problems [2]. One example is given by deep cumulus clouds. In such clouds, the temperature falls well below 0 o C, inducing the formation of small ice crystals, which play a very significant role in the formation of precipitation [8,37]. The orientation of such small ice crystals also determines how electromagnetic radiation is reflected from clouds [42]. A second example is the sedimentation of organic and anorganic matter in the turbulent ocean [27,38]. The dynamics of motile micro-organisms in turbulence [4,12,16,43], usually slightly heavier than water, has important consequences for the population dynamics and the ecology of the ocean system.More generally, understanding the angular dynamics of non-spherical particles in turbulent flows is a challenging fundamental problem [41]. When the particles are heavier than the surrounding fluid, the problem is significantly complicated. Even in the simplest case of spherical particles suspended in a turbulent flow, a detailed understanding of their settling properties is only beginning to emerge [3,15,20,33,36]. Clearly, understanding the angular dynamics is essential to describe the settling of non-spherical particles.An exact theoretical description of the problem requires the solution of the full Navier-Stokes equations, imposing no-slip boundary conditions at the surface of the solid [7,22,35]. An alternative, much more tractable approach consists in using simplified desc...