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Opposing roles of shear-thinning on successive instabilities in Taylor–Couette flow

Published online by Cambridge University Press:  03 November 2026

Fan Xu
Affiliation:
State Key Laboratory of Mesoscience and Process Engineering, Institute of Process Engineering, Chinese Academy of Sciences , Beijing 100190, PR China
Zifeng Li
Affiliation:
State Key Laboratory of Mesoscience and Process Engineering, Institute of Process Engineering, Chinese Academy of Sciences , Beijing 100190, PR China School of Chemical Engineering, University of Chinese Academy of Sciences, Beijing 100049, PR China
Ning Yang*
Affiliation:
State Key Laboratory of Mesoscience and Process Engineering, Institute of Process Engineering, Chinese Academy of Sciences , Beijing 100190, PR China School of Chemical Engineering, University of Chinese Academy of Sciences, Beijing 100049, PR China
*
Corresponding author: Ning Yang, nyang@ipe.ac.cn

Abstract

Content of image described in text.

The intrinsic effect of shear-thinning on successive instabilities in narrow-gap Taylor–Couette flow is investigated using direct numerical simulation (DNS) with axially periodic boundary conditions, thereby eliminating endwall effects. The Carreau model is employed with three shear-thinning indices ($n = 0.52$, $0.62$, $0.68$), matching the experimental parameters of Cagney and Balabani (Phys. Fluids, 2019, vol. 31, p. 053102). Shear-thinning exerts opposing influences on the two instabilities. For the primary transition from circular Couette flow to Taylor vortex flow, enhanced shear-thinning (decreasing $n$) is destabilising, with the critical Reynolds number $\textit{Re}_{c,1}$ decreasing from $101$ to $94$. In contrast, the secondary transition to wavy vortex flow is strongly stabilised, with $\textit{Re}_{c,2}$ increasing from $115$ to $142$ over the same range of $n$. This opposing behaviour arises from a competition between two consequences of radial viscosity variation: the reduced viscosity near the inner wall promotes centrifugal disturbances (destabilising), while the elevated viscosity in the bulk gap damps inter-vortex oscillations (stabilising). Comparison with the non-monotonic experimental measurements of Cagney and Balabani (Phys. Fluids, 2019, vol. 31, p. 053102) shows that the observed discrepancies originate from endwall-induced wavelength constraints and vortex drift rather than intrinsic rheological effects. These results establish the intrinsic bifurcation structure of shear-thinning Taylor–Couette flow in the narrow-gap configuration and clarify the distinct roles of rheology and confinement in successive flow transitions.

Information

Type
JFM Papers
Copyright
© The Author(s), 2026. Published by Cambridge University Press
Figure 0

Figure 1. Figure 1 long description.(a) Sketch of the TC system. (b–d) Verification of the Carreau model implementation at Re = 40, corresponding to the CCF regime. Symbols denote the viscosity computed from the DNS at various shear rates for n=0.52$n=0.52$, 0.62$0.62$, and 0.68$0.68$; solid lines represent the theoretical Carreau model (2.5) with parameters from table 1.

Figure 1

Table 1. Carreau model parameters for the three shear-thinning fluids investigated (reproduced from Cagney & Balabani (2019)) together with the critical Reynolds numbers Rec,1$\textit{Re}_{c,1}$ and Rec,2$\textit{Re}_{c,2}$ obtained from the present DNS. Here μ0$\mu _0$ and μ∞$\mu _{\infty }$ are the zero- and infinite-shear-rate viscosities, λc$\lambda _c$ is the characteristic relaxation time and n$n$ is the shear-thinning index.Table 1 long description.

Figure 2

Figure 2. (a) Critical Reynolds numbers for the onset of TVF (Rec,1$\textit{Re}_{c,1}$) and WVF (Rec,2$\textit{Re}_{c,2}$) as functions of the shear-thinning index n$n$. The DNS results are shown as open symbols connected by lines, while the open symbols denote the experimental data of Cagney & Balabani (2019). The regimes CCF, TVF and WVF are denoted by text labels in the diagram. (b) Instantaneous contours of the azimuthal vorticity (normalised by the rotating angular velocity of inner cylinder) in the meridional (r−z$r{-}z$) plane at two azimuthal positions (θ=0$\theta =0$ and θ=π$\theta =\pi$) for TVF (Rec,1=94$\textit{Re}_{c,1}=94$) and WVF (Rec,2=142$\textit{Re}_{c,2}=142$) at n=0.52$n=0.52$. The steady axisymmetric TVF structure and the symmetry breaking in WVF are clearly visible. Three triangular markers at z=L/4$z = L/4$, L/2$L/2$ and 3L/4$3L/4$ are superimposed on the WVF contour at θ=0$\theta =0$, indicating the locations of the three monitor points used in (c); all three probes are at the mid-gap r∗=0.5$r^*=0.5$. (c) Time evolution of the axial velocity uz/ui$u_z/u_i$ at the mid-gap (r∗=0.5$r^*=0.5$) for n=0.52$n=0.52$, recorded at three axial monitor points (z=L/4,L/2,3L/4$z=L/4, L/2, 3L/4$). Dashed lines denote the steady state at the primary instability threshold (Rec,1=94$\textit{Re}_{c,1}=94$), while solid lines illustrate the quasi-periodic oscillations at the secondary instability threshold (Rec,2=142$\textit{Re}_{c,2}=142$). The overlapping traces confirm the existence of an axially coherent, global travelling wave in the WVF regime. (d) Circumferential profile of uz/ui$u_z/u_i$ at the mid-gap (r∗=0.5$r^*=0.5$) for n=0.52$n=0.52$ (the corresponding profiles for other n$n$ values are provided in the Appendix C). The profile exhibits three complete wave periods, corresponding to a dominant azimuthal mode m = 3.

Figure 3

Figure 3. Figure 3 long description.Radial profiles of the time-, azimuthally- and axially-averaged dimensionless viscosity μ(γ˙)/μ0$\mu (\dot \gamma )/\mu _0$ (a,c) and its radial gradient dμ(γ˙)/dr$\text{d}\mu (\dot \gamma )/\text{d}r$ (b,d) for three shear-thinning fluids with n=0.52$n = 0.52$, 0.62$0.62$ and 0.68$0.68$. Panels (a,b) correspond to the primary instability threshold (Re=Rec,1$\textit{Re} = \textit{Re}_{c,1}$); panels (c,d) correspond to the secondary instability threshold (Re=Rec,2$\textit{Re} = \textit{Re}_{c,2}$). The dashed lines in (a,c) represent the average values of dimensionless viscosity at different n, and the dashed lines in (b,d) represent the radial gradient where dμ(γ˙)/dr=0$\text{d}\mu (\dot \gamma )/\text{d}r = 0$.

Figure 4

Figure 4. Contours of the instantaneous (left) shear rate λcγ˙$\lambda _c\dot \gamma$, (middle) dimensionless viscosity μ/μ0$\mu /\mu _0$ and (right) azimuthal velocity uθ/ui$u_\theta /u_i$ superposed velocity vectors (the radial and axial components) in the meridional (r$r$–z$z$) plane for the most shear-thinning fluid (n=0.52$n = 0.52$): (a) at the primary instability threshold (Rec,1=94$\textit{Re}_{c,1} = 94$) and (b) at the secondary instability threshold (Rec,2=142$\textit{Re}_{c,2} = 142$).

Figure 5

Table 2. Critical Reynolds numbers obtained from controlled simulations, where only the shear-thinning index n$n$ is varied, while μ0,μ∞$\mu _0, \mu _\infty$ and λc$\lambda _c$ are fixed at the values of the original n=0.52$n=0.52$ fluid.Table 2 long description.

Figure 6

Table 3. Comparison of the primary instability threshold Rec,1$\textit{Re}_{c,1}$ between the linear stability results of Alibenyahia et al. (2012) using the power-law model and the present DNS using the Carreau model. Both sets exhibit the same physical trend, where decreasing n$n$ leads to a lower Rec,1$\textit{Re}_{c,1}$, confirming the reliability of our numerical framework.Table 3 long description.

Figure 7

Figure 5. Circumferential profiles of uz/ui$u_z/u_i$ at the mid-gap (r∗=0.5$r^* = 0.5$) for n=0.52$n = 0.52$, 0.62$0.62$ and 0.68$0.68$, evaluated at their respective secondary instability thresholds (Re=Rec,2$\textit{Re} = \textit{Re}_{c,2}$). All three profiles exhibit three complete wave periods, indicating a dominant azimuthal mode m=3$m = 3$ that is independent of n$n$.

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