Odd viscosity suppresses intermittency in direct turbulent cascades
Sihan Chen, Xander M. de Wit, Michel Fruchart, Federico Toschi, Vincenzo Vitelli
TL;DR
The paper investigates how odd viscosity, a non-dissipative parity-breaking term, affects intermittency in direct turbulent cascades. Using DNS and a two-channel helical shell model, it shows that odd viscosity suppresses intermittency at small scales by breaking multiple scale invariances via parity-breaking waves with frequencies $\omega_\pm(\bm k)=\pm \nu_{\rm odd} k_z |\bm k|$. It develops a generalized framework with generalized odd viscosity ($\omega_{\pm}(\bm k)=\pm c_{\rm odd} k_z |\bm k|^{\alpha-1}$), predicting a wave-affected cascade with crossover scale $k_{\rm odd}$ and dissipation scale $k_c$, and demonstrates pattern formation and extended inertial ranges. The results indicate a route to designing turbulent flows with tunable intermittency by controlling parity-breaking wave dynamics.
Abstract
Intermittency refers to the broken self-similarity of turbulent flows caused by anomalous spatio-temporal fluctuations. In this Letter, we ask how intermittency is affected by a non-dissipative viscosity, known as odd viscosity (also Hall or gyro-viscosity), which appears in parity-breaking fluids such as magnetized polyatomic gases, electron fluids under magnetic field and spinning colloids or grains. Using a combination of Navier-Stokes simulations and theory, we show that intermittency is suppressed by odd viscosity at small scales. This effect is caused by parity-breaking waves, induced by odd viscosity, that break the multiple scale invariances of the Navier-Stokes equations. Building on this insight, we construct a two-channel helical shell model that reproduces the basic phenomenology of turbulent odd-viscous fluids including the suppression of anomalous scaling. Our findings illustrate how a fully developed direct cascade that is entirely self-similar can emerge below a tunable length scale, paving the way for designing turbulent flows with adjustable levels of intermittency.
