Parabolic velocity profile causes drift of inertial prolate spheroids -- but gravity is stronger

Abstract

Motion of elongated particles in shear is studied. In applications where particles are much heavier than the carrying fluid, e.g. aerosols, the influence of particle inertia dominates the particle dynamics. Assuming that the particle only experiences a local linear velocity profile, its rotational and translational motion are independent. However, we show that quadratic terms of the local velocity profile combined with particle inertia cause a lateral drift of prolate spheroidal particles. We find that this drift is maximal when particle inertial forces are of the same order of magnitude as viscous forces, and that both extremely light and extremely heavy particles have negligible drift. In the non-inertial case, the particle rotates according to the local linear velocity profile, with each instantaneous orientation corresponding to a velocity that gives zero force on the particle. This results in a translational motion in the flow direction with periodic velocity fluctuations. With added particle inertia, the particle is slow to react to the surrounding fluid motion and the particle will switch between slower and faster rotation compared to the zero-force solution. The final motion that gives zero integrated force over a rotational period, is a motion with a lateral drift. We show that this drift is purely an effect of the non-sphericity of the particle and its translational inertia, while rotational inertia is negligible. Finally, although this inertial drift will contribute to the lateral motion of heavy elongated particles in channel flow, sedimentation due to gravity will dominate in any practical application on earth.