The broken link between space and time in elastic turbulence
Giulio Foggi Rota, Rahul K. Singh, Alessandro Chiarini, Christian Amor, Giovanni Soligo, Dhrubaditya Mitra, Marco Edoardo Rosti
TL;DR
Elastic turbulence in viscoelastic flows at low inertia exhibits $E(k) \sim k^{-α}$ and $E(ω) \sim ω^{-β}$, with $α$ clustering near 4 while $β$ varies widely, challenging a universal space–time relation. Using direct numerical simulations in a triperiodic box, a channel, and a planar jet with Oldroyd–B dynamics, the authors demonstrate that $α \approx 4$ is robust across configurations but $β$ is not universal due to breakdown of Taylor’s hypothesis. A phenomenological analysis reveals multiple competing timescales and shows that, despite $u(r) \sim r^1$, a single dynamic exponent linking space and time does not exist in ET. The work reframes the problem by emphasizing the spatial scaling and suggests broader relevance to smooth chaotic flows and active turbulence.
Abstract
Elastic turbulence (ET), observed in flows of sufficiently elastic polymer solution at small inertia, is characterized by chaotic motions and power-law scaling of energy spectrum ($E$) in both wavenumber ($k$) and frequency ($ω$): $E(k) \sim k^{-α}$ and $E(ω) \sim ω^{-β}$. Experiments of ET have obtained a vast range of values for the exponent $β$. In inertial turbulence, Taylor's frozen-flow hypothesis implies $α= β$, i.e., spatial and temporal scales are linearly related to each other. In contrast, from high-resolution simulation in three different setups, a tri-periodic box, a channel, and a planar jet, we show that in ET $α\approx 4$ while $β$ varies significantly. Our analysis shows that in general Taylor's hypothesis does not hold in ET as there is no universal relation, linear or otherwise, between space and time. Thus, we clear the confusion of the different scaling exponents found in ET, and focus the attention of future research on understanding $α$. We introduce a fundamentally new way of looking not only at polymeric turbulence, but also at smooth chaotic flows in general, e.g., active turbulence.
