Hostname: page-component-74656f9884-rdgjk Total loading time: 0 Render date: 2026-11-09T02:59:42.345Z Has data issue: false hasContentIssue false

Flow instability and scaling transition near strongly polarised surfaces

Published online by Cambridge University Press:  26 November 2025

Wei Liu
Affiliation:
Department of Engineering Mechanics and ASP, Tsinghua University , Beijing 100084, PR China
Yunfan Huang
Affiliation:
Department of Engineering Mechanics and ASP, Tsinghua University , Beijing 100084, PR China
Moran Wang*
Affiliation:
Department of Engineering Mechanics and ASP, Tsinghua University , Beijing 100084, PR China
*
Corresponding author: Moran Wang, moralwang@jhu.edu

Abstract

The electrokinetic and unstable behaviour near strongly polarised surfaces cannot be well captured by the canonical asymptotic theory for induced-charge electro-osmosis, and the intrinsic mechanism remains unclear. Using direct numerical simulations and scaling analysis, this paper reveals that, near the strongly polarised surfaces, the strong electric double layer charging induces a strong local electric field, which drives the cations in the electrical double layer to extend to a finite region and form an extended space-charge (ESC) layer. The ESC triggers flow instability near strongly polarised surfaces, causing a transition of the velocity scaling exponent in the electric field dependence from a 2 to a 4/3 power law. The findings and mechanisms pave the way for designs of energy and biomedical systems.

Information

Type
JFM Papers
Copyright
© The Author(s), 2025. Published by Cambridge University Press
Figure 0

Figure 1. Validation. (a) Ion concentrations. The inset shows the distribution results of cation and anion concentrations from Davidson et al. (2014), demonstrating that the simulation in this study aligns with the existing DNS. (b) Grid independence. The structure of the space-charge layer (obtained by subtracting the cation concentration from the anion concentration) is used to verify grid independence. Here, the parameters are $\tilde{\lambda }_{D}=0.0014$, $\tilde{\kappa }=0.5$ and $E_{0}a/V_{T}=30$.

Figure 1

Figure 2. Strong EDL capacitive charging triggers flow instability. Experimental (Peng et al.2014) and simulation results. The DNS shows an instantaneous snapshot of the dimensionless salt concentration and streamlines. $\Delta \tilde{\varphi}/\tilde{L}=16$ corresponding to $\Delta \tilde{\varphi}=800$. The simulation parameters are $\Delta \tilde{\varphi}/\tilde{L}=16$, $\tilde{\lambda}_{D}=5\boldsymbol{\cdot }10^{-4}$ and $\tilde{\kappa}=0.5$.

Figure 2

Figure 3. The formation mechanism of ESC. (a) The schematic of EDL strong capacitive charging illustrates the subtle processes involved in EDL charging development at the metal–cylinder interface. It highlights the contribution of the electric field to the arrangement of ions. (b) ion concentration, and (c) electric field strength at the cut line (dashed line in figure 2). The EDL structure transitions to an ESC structure, in which a small number of cations are present, while the anion concentration is nearly zero. (d) Ion current induced by EDL capacitive charging. This time current is computed spatially by the radial cation flux on the upper surface of the metal cylinder minus the anion flux. (e) Variation of the cation and anion fluxes with the external electric field. The upper surface EDL exhibits cation selectivity. This ion flux is computed temporally and spatially by the radial cation flux on the upper surface of the metal cylinder minus the anion flux. In (b)–(c), the DNS parameters are $\Delta \tilde{\varphi }/\tilde{L}=16$, $\tilde{\lambda }_{D}=5 \times 10^{-4}$ and $\tilde{\kappa }=0.5$.

Figure 3

Figure 4. The EDL capacitive charging triggers scaling transition of velocity. (a) Fully developed concentration field and streamline distribution. Here, $A_{1}$ and $A_{2}$ are the velocities at two different points in the inflow, and the positions of $A_{1}$ and $A_{2}$ are $\tilde{y}=\sqrt{3}$ and $\tilde{y}=\tilde{\delta }_{\mathrm{esc}}$ + 1, respectively. Also, $B_{1}$ and $B_{2}$ are the velocities at two different points in the outflow, and the positions of $B_{1}$ and $B_{2}$ are $\tilde{x}=-\sqrt{3}$ and $\tilde{x}=-\tilde{\delta }_{\mathrm{esc}}-1$, respectively. Here, we choose $\tilde{\delta }_{\mathrm{esc}}=0.05$. The positions of $A_{1}$ and $B_{1}$ are consistent with those in Davidson et al. (2014). (b) Velocity scaling. To highlight the influence of vortices, the statistics points ($A_{2}$ and $B_{2}$) are considered. The DNS results in this paper are basically consistent with those in Davidson et al. (2014). The simulation parameters are $\Delta \tilde{\varphi }/\tilde{L}=30$, $\tilde{\lambda }_{D}=0.0014$ and $\tilde{\kappa }=0.5$.

Figure 4

Figure 5. Velocity scaling in a broad parameter space. (a) The effect of dimensionless Debye length, hydrodynamic coupling coefficient and electric field on the velocity. Under the action of strong electric field, the velocity satisfies the 4/3 power law. (b) Universal scaling laws of velocity. The experimental setup described in Peng et al. (2014) involves an Au sphere with a diameter of $50\,{\unicode{x03BC}} \mathrm{m}$, placed between two metal plates spaced $10\,\mathrm{mm}$ apart. The solution concentration is $0.1\mathrm{mM}$, corresponding to a dimensionless Debye length of $\tilde{\lambda }_{D}\approx 0.005$. To normalise the experimental data, we adopt the dimensionless reference values used in this study: a reference length of $10\,{\unicode{x03BC}} \mathrm{m}$, a reference voltage of $25.6\mathrm{mV}$ and a diffusion velocity of $2 \times 10^{-4}\,\mathrm{ms}^{-1}$. In the scaling factor $S(\omega )=1/(1+\omega ^{2}\tau _{c}^{2})$, where $\omega$ is the electric field frequency which is set to $1\mathrm{kHZ}$ in the experiment. The characteristic resistance–capacitance charging time $\tau _{c}$ can be calculated using $\tau _{c}=\varepsilon _{w}(\pi | x_{e}| )\sigma \lambda _{D}$ (Pascall & Squires 2010), with $x_{e}$ being the position where velocity is statistically measured–$20\,{\unicode{x03BC}} \mathrm{m}$ in the experiment (Peng et al.2014). Here, $\sigma$ is the conductivity of the aqueous solution, and $\lambda _{D}$ is the Debye length. Note that we do not consider the non-monotonic effects of frequency on velocity, as studied in Davidson et al. (2014) and Peng et al. (2014).

Figure 5

Figure 6. Flow pattern. Effect of electric field on (a) flow pattern and (d) velocity distribution at the cutline. Here, the parameters are set to $\tilde{\lambda }_{D}=0.005$ and $\tilde{\kappa }=0.5$. Effect of the hydrodynamic coupling coefficient on (b) flow pattern and (e) velocity distribution. Here, the parameters are set to $\Delta \tilde{\varphi }/\tilde{L}=20$ and $\tilde{\lambda }_{D}=10^{-3}$. Effect of the dimensionless Debye layer thickness on (c) flow pattern and (f) velocity distribution. In the diffuse layer, the radial velocity and distance satisfy the decay power law of −3. Here, $\Delta \tilde{\varphi }/\tilde{L}=30$ and $\tilde{\kappa }=0.5$.

Figure 6

Figure 7. The spatio-temporal evolution of salt concentration ($\tilde{c}_{1}$+$\tilde{c}_{2}$)/2. At the cutline ($\tilde{x}=1.1$, $-0.5\leq \tilde{y}\leq 0.5$), the spatio-temporal evolution of salt concentration is shown in (a) case 1 ($\tilde{\lambda}_{D}=0.0005$, $\Delta \tilde{\varphi}/\tilde{L}=16$ and $\tilde{\kappa}=0.5$) and (b) case 2 ($\tilde{\lambda}_{D}=0.0014$, $\Delta \tilde{\varphi}/\tilde{L}=22$ and $\tilde{\kappa}=0.5$). (c) The velocity fluctuation ($\tilde{u}^{\prime}$) curves. For case 1, the flow is unstable, which is consistent with our theoretical analysis. Local small-scale vortices erupt, forming a fascinating feather texture structure and irregular fluctuations in velocity. However, for case 2, the flow is stable, forming a long band-like salt-jet structure. Case 1 and case 2 correspond to point 1 (unstable) and point 2 (stable) in figure 8, respectively.

Figure 7

Figure 8. The EDL capacitive charging triggers flow state transition. When the dimensionless parameters exceed the critical stability curve, the flow is in an unstable state; otherwise, it remains stable. The flow state is identified through the spatio-temporal evolution of salt concentration. Physically, a decrease in $\tilde{\lambda }_{D}$ corresponds to the volumetric force of the ESC layer becoming stronger, triggering small-scale vortex bursts.