Abstract
We report detailed experimental studies of statistical, scaling, and spectral properties of elastic turbulence (ET) in a von Karman swirling flow between rotating and stationary disks of polymer solutions in a wide, from dilute to semidilute entangled, range of polymer concentrations . The main message of the investigation is that the variation of just weakly modifies statistical, scaling, and spectral properties of ET in a swirling flow. The qualitative difference between dilute and semidilute unentangled versus semidilute entangled polymer solutions is found in the dependence of the critical Weissenberg number of the elastic instability threshold on . The control parameter of the problem, the Weissenberg number is defined as the ratio of the nonlinear elastic stress to dissipation via linear stress relaxation and quantifies the degree of polymer stretching. The power-law scaling of the friction coefficient on characterizes the ET regime with the exponent independent of . The torque and pressure power spectra show power-law decays with well-defined exponents, which has values independent of and separately at ppm and ppm ranges. Another unexpected observation is the presence of two types of the boundary layers, horizontal and vertical, distinguished by their role in the energy pumping and dissipation, which has width dependence on and differs drastically. In the case of the vertical boundary layer near the driving disk, is independent of and linearly decreases with , while in the case of the horizontal boundary layer its width is independent of , linearly decreases with , and is about five times smaller than . Moreover, these and dependencies of the vertical and horizontal boundary layer widths are found in accordance with the inverse turbulent intensity calculated inside the boundary layers and , respectively. Specifically, the dependence of in the vertical boundary layer on and agrees with a recent theoretical prediction [S. Belan, A. Chernych, and V. Lebedev, Boundary layer of elastic turbulence (unpublished)].
10 More- Received 8 December 2016
DOI:https://doi.org/10.1103/PhysRevFluids.2.103301
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