Superdiffusion and antidiffusion in an aligned active suspension
arXiv:2510.00740 · doi:10.1103/d61l-1tyh
Abstract
We show theoretically that an imposed uniaxial anisotropy leads to new universality classes for the dynamics of active particles suspended in a viscous fluid. In the homogeneous state, their concentration relaxes superdiffusively, stirred by the long-ranged flows generated by its own fluctuations, as confirmed by our numerical simulations. Increasing activity leads to an anisotropic diffusive instability, and thus an original phase-separation mechanism, driven by the interplay of active stresses with a particle current proportional to the local curvature of the suspension velocity profile.
Physics of the origin of certain terms clarified, numerical estimates improved, key references added
References in corpus (20)
- The Mechanics and Statistics of Active Matter
- Living Liquid Crystals
- Scalar field theory for active-particle phase separation
- Active nematics on a substrate: giant number fluctuations and long-time tails
- Cluster phases and bubbly phase separation in active fluids: Reversal of the Ostwald process
- Flow-induced phase separation of active particles is controlled by boundary conditions
- Active Model H: Scalar Active Matter in a Momentum-Conserving Fluid
- Origins and diagnostics of the nonequilibrium character of active systems
- Activating membranes
- Hydrodynamically interrupted droplet growth in scalar active matter
- A two-sphere model for bacteria swimming near solid surfaces
- Active phase separation: new phenomenology from non-equilibrium physics
- Screening, Hyperuniformity, and Instability in the Sedimentation of Irregular Objects
- Long-range fluctuation-induced forces in driven electrolytes
- Controlling cell motion and microscale flow with polarized light fields
- Re-enterant efficiency of phototaxis in Chlamydomonas reinhardtii cells
- Universal properties of repulsive self-propelled particles and attractive driven particles
- The effect of inter-particle hydrodynamic and magnetic interactions in a magnetorheological fluid
- Current fluctuations across a nanopore
- Anomalous Diffusion in Driven Electrolytes due to Hydrodynamic Fluctuations