“…This, however, is often difficult or even impossible to achieve, for example, in random porous media with a broad range of length scales. In addition, deviations from fluid flow lines due to inertial effects can occur even for small particles, as recently shown for time-periodic and chaotic flows (Ouellette et al 2008;Pushkin 2011). Consequently, the impact of particle size within inhomogeneous flow fields has to be considered, which leads to relevant hydrodynamic effects even in simple geometries (Segre and Silberberg 1962;Staben et al 2003).…”