Intermittency in the not-so-smooth elastic turbulence.
basic_science · Level V
Where this comes from
- Record sourced from PubMed, PMID 38802336.
- Also identified by DOI 10.1038/s41467-024-48460-5 and PMC identifier 11130217.
- Licence recorded as CC BY.
- The licence permits redistribution, so the abstract is shown in full and the full text is available from the publisher.
Abstract
Elastic turbulence is the chaotic fluid motion resulting from elastic instabilities due to the addition of polymers in small concentrations at very small Reynolds ( <math xmlns="http://www.w3.org/1998/Math/MathML"><mi>Re</mi></math> ) numbers. Our direct numerical simulations show that elastic turbulence, though a low <math xmlns="http://www.w3.org/1998/Math/MathML"><mi>Re</mi></math> phenomenon, has more in common with classical, Newtonian turbulence than previously thought. In particular, we find power-law spectra for kinetic energy E(k) ~ k<sup>-4</sup> and polymeric energy E<sub>p</sub>(k) ~ k<sup>-3/2</sup>, independent of the Deborah (De) number. This is further supported by calculation of scale-by-scale energy budget which shows a balance between the viscous term and the polymeric term in the momentum equation. In real space, as expected, the velocity field is smooth, i.e., the velocity difference across a length scale r, δu ~ r but, crucially, with a non-trivial sub-leading contribution r<sup>3/2</sup> which we extract by using the second difference of velocity. The structure functions of second difference of velocity up to order 6 show clear evidence of intermittency/multifractality. We provide additional evidence in support of this intermittent nature by calculating moments of rate of dissipation of kinetic energy averaged over a ball of radius r, ε<sub>r</sub>, from which we compute the multifractal spectrum.