No inertia, yet more than ten times the resistance
The 2000 apparatus of Groisman and Steinberg is a cup under a rotating plate: plate radius 38 mm, cup radius 43.6 mm, liquid depth 10 mm. The solvent is a sugar solution of viscosity ; with 80 ppm polyacrylamide added, the relaxation time is . Near a shear rate of the flow changes abruptly, at and a Reynolds number of only about 0.3, and the transition shows hysteresis.
Beyond the transition, the stress needed to keep the plate turning reaches about 12 times that of a laminar flow of the same viscosity, and about 19 times with a 20 mm layer. A Newtonian liquid in the same apparatus needs a Reynolds number of about 20 000 to reach 19 times.
Where does the extra resistance come from? In inertial turbulence it comes from the Reynolds stress. Here the authors estimate from their velocity measurements that the Reynolds stress is less than 0.5% of the resistance, and the averaged viscous stress of the solvent is the same as in laminar flow. The only stress left to carry the increase is the elastic stress of the polymers.
Source: A. Groisman and V. Steinberg
The spectrum says smooth but chaotic
Beyond the transition, the velocity at a point fluctuates irregularly in time. Its power spectrum follows a power law over about one decade, with an exponent of about in the 2000 swirling flow; in the 2001 curved channel, converting time to space with the Taylor hypothesis, the spatial spectrum has an exponent of about .
An exponent steeper than has a direct consequence: the velocity gradients come mainly from the largest scales. The mean-square velocity gradient is the integral of , and with and that integral converges at high wavenumber. The flow is smooth in space and random in time. Groisman and Steinberg (2004) compare it with the part of an inertial turbulent flow below the Kolmogorov dissipation scale.
It also means that elastic turbulence is not a copy of inertial turbulence: there is no cascade of energy from large eddies to small ones, and no spectrum at small scales.
Source: A. Groisman and V. Steinberg · A. Groisman and V. Steinberg · A. Groisman and V. Steinberg
Mixing three orders of magnitude faster than diffusion
The 2001 channel is 3 mm wide and made of 60 half-rings. The solution relaxes in 1.4 s, and the dye diffuses with a coefficient of about . The flow stays steady up to a Weissenberg number of 3.2; at 6.7 the two streams are mixed after about 15 half-rings, about 120 s.
By molecular diffusion alone, mixing across the 3 mm width would take more than a day (see the formula). With a more viscous solvent and slower diffusion at the same Weissenberg number, the mixing is unchanged, so what does the work is the flow the polymers drive, neither inertia nor diffusion.
Source: A. Groisman and V. Steinberg
Criteria give a trend, not a universal threshold
The parameter of Chapter 6 and the Pakdel–McKinley criterion both say that curved streamlines with normal stress drive the instability. The actual transition point depends on the geometry. Groisman and Steinberg (2004) report transitions at Weissenberg numbers of 3.2 and 2 in the flow between two plates for gap-to-radius ratios of 0.26 and 0.52; about 4 in Couette–Taylor flow; and in the curved channel, stationary vortices may appear near 2 while irregular motion starts only at 3.2.
The resistance growth differs too. The paper sums it up as about 20 times between two plates, about 4.2 in Couette–Taylor flow and about 2.8 in the channel. The review of Datta and co-authors gives a local maximum of the criterion of about 4 to 5 in cross-slot simulations, but no critical values for Taylor–Couette or cone-and-plate flow.
So when you read that “the critical Weissenberg number is” some value, first ask: in which geometry, with which definition of the Weissenberg number, and with which solution?
How far the four-roll model goes
Experiments cannot see the polymer stress field; a numerical model can. The four-roll model of Chapter 7 gives the symmetry-breaking threshold and the oscillation periods. Thomases, Shelley and Thiffeault also seeded the oscillating flow at a Weissenberg number of 10 with tracer particles, measured an effective diffusivity of about 0.025 and a finite-time Lyapunov exponent of about 0.014, and in one run with a cycling vortex saw the particles from the four quadrants approach a quarter each after t of about 3000.
This course recomputed the model on a coarser discretisation; the numbers below are numerical results of this route, not experimental data. On a grid with the threshold is 4.86; a grid and half the time step also give 4.86, consistent with the papers’ 4.8 to 4.9. At a Weissenberg number of 10 the symmetry breaks near ; between 1000 and 2000 the probe velocity has two periods of about 288 and 56, against the paper’s 330 and 55; the probe curves of the three discretisations differ by less than a few parts in a thousand before .
Stress diffusion changes the outcome. At the threshold rises to 5.09 and the flow at a Weissenberg number of 10 ends in an asymmetric steady state; at the threshold is 6.64 and the symmetry does not break until . In this range, more diffusion makes breaking harder. That points the opposite way to the conclusion of Gupta and Vincenzi that diffusion creates the breaking, but they compared zero diffusion with a different force, and this course did not test the limit .
One check did not pass. On with , the smallest eigenvalue of the conformation tensor falls to about −4.4 during start-up, a sign that this grid does not resolve the thinnest stress strand; on it stays positive. The mixing is also only partial: after the tracers are released the mixing index settles near 0.66, and particles from the diagonally opposite quadrant make up only about 6% of quadrant one.
Source: B. Thomases · A. Gupta and D. Vincenzi · Sandbox Physics FR26
What is still open
The 2022 review by Datta and co-authors summarises a workshop discussion. Three of its points bear directly on this course.
First, constitutive models. Elastic instabilities usually appear at high Weissenberg number, where Oldroyd-B is almost never quantitative in shear or in extension, and the same holds for extensions such as FENE, Giesekus and PTT. Understanding elastic instability has to go hand in hand with better rheological models.
Second, the eigenvalue spectrum of two-dimensional elastic Taylor–Couette flow has hardly been studied, although the onset of instability has been seen there near a Weissenberg number of 10 at a large gap ratio.
Third, a Lagrangian view. Every purely elastic instability mechanism worked out so far relies on shear, in viscometric flows. Yet a single polymer in extension shows a coil–stretch transition that is sharp, hysteretic and dependent on its history. How the history along a fluid element’s path enters the instability remains to be studied. The stress-diffusion debate of Chapter 7 is another question the numerics have not yet settled.
Source: S. S. Datta et al. · A. Gupta and D. Vincenzi
Worked example: is the channel really free of inertia?
Groisman and Steinberg (2001) use and . Dividing one by the other removes the flow rate: .
With , , and , . At that gives , against the 0.06 the paper reports. The difference comes from shear thinning: the viscosity was measured at a shear rate of 4 per second.
Conclusion: at the transition, inertial forces are a few per cent of viscous forces, so the disorder can only come from elasticity.
Source: A. Groisman and V. Steinberg