Dept of Mathematical Sciences University of Liverpool

Classical work of Jeffery from 1922 established how at low Reynolds number, ellipsoids in steady shear flow undergo periodic motion with non-uniform rotation rate, termed 'Jeffery orbits'.  I will present two problems where Jeffery orbits play a critical role in understanding the transport and aggregation of rod-shaped organisms.  I will discuss the trapping of motile chemotactic bacteria in high shear, and the sedimentation rate of negatively buoyant plankton.