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Molecular streaming in a charged angstrom channel: a toy model

Published online by Cambridge University Press:  03 June 2025

Shuyong Luan
Affiliation:
Key Laboratory of Aircraft Configuration Design, School of Aeronautics and Institute of Extreme Mechanics, Northwestern Polytechnical University, Xi’an 710072, PR China
Jiajia Lu
Affiliation:
School of Physical Science and Technology, Northwestern Polytechnical University, Xi’an 710072, PR China
Yanbo Xie*
Affiliation:
Key Laboratory of Aircraft Configuration Design, School of Aeronautics and Institute of Extreme Mechanics, Northwestern Polytechnical University, Xi’an 710072, PR China
*
Corresponding author: Yanbo Xie, ybxie@nwpu.edu.cn

Abstract

Numerous studies showed that the flow and transport phenomena in angstrom channels are different from existing understandings. In this work, we investigate the electrokinetic phenomena in a charged angstrom channel, including homogeneous and heterogeneous charge distributions at the wall to mimic the charging mechanisms of electrified metal-like surfaces and deprotonated dielectric surfaces, respectively. Our results show that both the streaming current and the flow velocity linearly increase as the applied pressure increases in a homogeneously charged system. However, in a heterogeneously charged system, the streaming current is activated only when the applied pressure exceeds a critical threshold. This behaviour arises from the strong Coulomb interactions between counterions and the surface charge, manifesting as an obvious nonlinear feature. The dissociation of counterions from the surface charge may not only cause pressure-dependent streaming conductance but also reduce the friction coefficient of the system, thus the flow resistance, when the system friction is governed by the bound ions. We found that such pressure-dependent streaming conductance gradually weakens as the channel size increases and reaches the regime of classical nanofluidic theories. Taking one-dimensional non-equilibrium statistics and Markov chains for the sequence evolution of bound-ion dissociation, our theory can well explain the pressure-dependent streaming conductance and water permeability in angstrom charged channels. Voltage-driven nonlinear ionic transport and electro-osmosis were also observed in heterogeneously charged systems. Our findings will be helpful for understanding the ionic transport in angstrom-scale channels and possibly useful in ion separations.

Information

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

Figure 1. (a) Schematic of the homogeneously charged system, where each wall atom carries a charge of $-20e/N_c$ with $N_c$ being the number of atoms on the nanotube wall. The green line schematically represents a smooth free energy drop of a free cation under pressure-driven flow. (b) Schematic of a heterogeneously charged system, where a wall atom (green) is periodically charged with $-e$ at intervals of 25 Å. The green line illustrates the potential well due to Coulomb interaction between cation and surface charge under hydrodynamic friction.

Figure 1

Table 1. The LJ force fields and charges of homonuclear atoms. Heteronuclear LJ parameters are computed with Lorentz–Berthelot mixing rules.

Figure 2

Figure 2. (a) The trajectory of three identical $\rm Na^+$ cations (red) and a water molecule (blue) under a pressure gradient of 0.93 bar Å−1 moving with an identical velocity in the homogeneously charged system. (b) The streaming current and (c) water fluxes in the homogeneously charged system (red) and heterogeneously system (blue). The symbols are derived from simulation, while the solid lines denote the theoretical results for ions by (4.5) and water flow rate $Q=\pi R^2v_w$ by (4.4).

Figure 3

Figure 3. (a) An example of the counterion trajectories under a pressure gradient of 28.71 bar Å−1 in a heterogeneously charged system with a low-friction wall. All cations were initially adsorbed at the charged sites on the wall but have a certain probability of dissociating from the binding sites, thus forming a current. The statistics of (b) the streaming current and (c) water fluxes as functions of the pressure gradient for three monovalent cations: $\rm K^+, Na^+, Li^+$. The symbols represent the simulation results, while the solid lines denote the theoretical predictions derived from (4.14) in (b) and $Q=\pi R^2 v_w$ by (4.3) in (c). Both ionic and water fluxes exhibit a strong nonlinear increase with the pressure gradient.

Figure 4

Figure 4. (a) Ionic fluxes and (b) water fluxes as functions of the pressure gradient in channels with radii ranging from 5.48 to 7.05 Å. The green circular dots and the green dashed line represent the streaming current and flow rate in a 7.05 Å channel with a surface charge density of –0.019 $\rm C\, m^{-2}$. The rest of the channels have a fixed number of surface-charged sites of –20$e$ at the wall. We found that the threshold pressure required to activate the streaming current decreased with increasing nanotube radius. The theoretical value (solid lines) derived from (4.14) and water flow rate $Q=\pi R^2 v_w$ by (4.3) matched well with the simulation results. (c) An example of the flow profile in a heterogeneously charged channel under a pressure gradient of 33.51 bar Å−1. The average atomic velocity is computed every 1 ns over a total duration of 10 ns and radially averaged with a 0.01 Å interval. The red dots represent the velocities of water molecules (oxygen atoms), which exhibit plug flow, while the blue dots represent the velocities of sodium ions. The dashed line serves as a guide to the eye.

Figure 5

Figure 5. (a) The probability distribution of dissociated cation number $n$ under a range of pressure gradients. (b) The expected value of the number of dissociated ions as a function of the pressure gradient, where the symbols represent the averaged value of $\langle n \rangle$ from simulation that matched well with the values from (4.13) (solid line).

Figure 6

Figure 6. The normalised permeability $(Z/Z_0)^{-1}$ and surface potential $\zeta /\zeta _0$ as functions of $Da$. Both permeability and surface potential increase with $Da$ and approach 1 when $Da$ is large and close to the homogeneously charged system.

Figure 7

Figure 7. (a) The $I{-}E$ curve in the homogeneously charged system, where red symbols denote simulation results and the solid line represents the theoretical value from (5.5). The inset shows that the average velocity of ions is nearly the same as the electro-osmotic velocity. (b) The conduction current (green symbols) and electro-osmotic flow rate (magenta symbols) as functions of $E$ in the heterogeneously charged system, where the green and magenta solid lines are calculated using (5.7) and $Q=\pi R^2 v_{eo}$, respectively. Both current and electro-osmosis exhibit nonlinear features. The inset shows that the average velocity of ions is higher than the electro-osmotic velocity, where their discrepancy is more obvious than in the homogeneously charged system.

Figure 8

Figure 8. The number of water molecules inside the CNT increases over time.

Figure 9

Figure 9. (a) Autocorrelation function and (b) integrated friction coefficient for a four-charge-site system. (c) Autocorrelation function and (d) integrated friction coefficient of a charge-free nanotube.

Figure 10

Figure 10. The friction coefficient of the system linearly increases with the number of charged sites. The solid line is a linear fitted line to derive the friction coefficient per charged site.

Figure 11

Figure 11. The fitted curve of potential of surface charge.