Abstract
Microswimmer suspensions self-organize into complex spatio-temporal flow patterns, including vortex lattices and mesoscale turbulence. Here we explore the consequences for the motion of passive tracers, based on a continuum model for the microswimmer velocity field. We observe two qualitatively different regimes distinguished via the dimensionless Kubo number . At advection strengths right above the transition to turbulence, the flow field evolves very slowly () and the spatial vortex structures lead to dominant trapping effects. In contrast, deep in the turbulent state, much faster dynamics () consistent with the so-called sweeping hypothesis leads to transport properties completely determined by the temporal correlations. In between (), we observe a regime of optimal transport, signaled by a maximum of the diffusion coefficient.
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