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Interplay of ion availability and mobility in the loss of cation selectivity for CaCl\textsubscript{2} in negatively charged nanopores: molecular dynamics using scaled-charge models

Salman Shabbir, Dezső Boda, Zoltán Ható

TL;DR

This work probes how confinement and interfacial chemistry reshape ion transport in negatively charged silica nanopores for NaCl and CaCl$_2$ solutions using atomistic MD with scaled-charge ECCR2 ions and TIP4P/2005 water. By decomposing local transport into $\mathbf{j}_{i}(\mathbf{r})=\mathbf{v}_{i}(\mathbf{r})c_{i}(\mathbf{r})$, the authors connect static interfacial adsorption to dynamic perm-selectivity, revealing that Ca$^{2+}$ adsorption and charge inversion erode cation selectivity and promote interior Cl$^{-}$ conduction, while Na$^{+}$ remains the mobile counterion near the wall. The results depend sensitively on force-field choices, including ion model and water model, but the qualitative mechanism—surface immobilization of Ca$^{2+}$ and bulk-like interior conduction after charge inversion—persists across tested models. The findings highlight the need for careful force-field validation in confined electrokinetics and suggest that reduced or implicit models can still capture the essential physics of nanopore perm-selectivity.

Abstract

Ion transport through charged nanopores is commonly interpreted in terms of electrical double layer structure, leading to the expectation of cation-selective conduction in negatively charged pores. This picture can break down for multivalent electrolytes, where strong ion-urface correlations and charge inversion modify transport behavior. Here, we study NaCl and CaCl$_2$ conduction through negatively charged silica nanopores using atomistic molecular dynamics simulations with scaled-charge ion models. By separating concentration and velocity contributions to the radial particle current density, we connect static adsorption to dynamic perm-selectivity. While NaCl exhibits conventional cation selectivity, CaCl$_2$ shows nearly bulk-like or even anion-favored transport due to Ca$^{2+}$ immobilization near the surface and dominant Cl$^-$ conduction in the pore interior following charge inversion. Although this qualitative mechanism is robust, its detailed manifestation depends sensitively on the balance of ion-surface and ion-water interactions encoded in the force field.

Interplay of ion availability and mobility in the loss of cation selectivity for CaCl\textsubscript{2} in negatively charged nanopores: molecular dynamics using scaled-charge models

TL;DR

This work probes how confinement and interfacial chemistry reshape ion transport in negatively charged silica nanopores for NaCl and CaCl solutions using atomistic MD with scaled-charge ECCR2 ions and TIP4P/2005 water. By decomposing local transport into , the authors connect static interfacial adsorption to dynamic perm-selectivity, revealing that Ca adsorption and charge inversion erode cation selectivity and promote interior Cl conduction, while Na remains the mobile counterion near the wall. The results depend sensitively on force-field choices, including ion model and water model, but the qualitative mechanism—surface immobilization of Ca and bulk-like interior conduction after charge inversion—persists across tested models. The findings highlight the need for careful force-field validation in confined electrokinetics and suggest that reduced or implicit models can still capture the essential physics of nanopore perm-selectivity.

Abstract

Ion transport through charged nanopores is commonly interpreted in terms of electrical double layer structure, leading to the expectation of cation-selective conduction in negatively charged pores. This picture can break down for multivalent electrolytes, where strong ion-urface correlations and charge inversion modify transport behavior. Here, we study NaCl and CaCl conduction through negatively charged silica nanopores using atomistic molecular dynamics simulations with scaled-charge ion models. By separating concentration and velocity contributions to the radial particle current density, we connect static adsorption to dynamic perm-selectivity. While NaCl exhibits conventional cation selectivity, CaCl shows nearly bulk-like or even anion-favored transport due to Ca immobilization near the surface and dominant Cl conduction in the pore interior following charge inversion. Although this qualitative mechanism is robust, its detailed manifestation depends sensitively on the balance of ion-surface and ion-water interactions encoded in the force field.
Paper Structure (13 sections, 8 equations, 9 figures, 2 tables)

This paper contains 13 sections, 8 equations, 9 figures, 2 tables.

Figures (9)

  • Figure 1: From left to right: axial ($z$) components of particle current density (in 1/ps$\;$nm$^{2}$), velocity (in nm/ps), and concentration (in mol/dm$^{3}$). Red and blue curves refer to full-charge and scaled-charge silanol oxygen (O$_{\mathrm{S}}$) models, respectively. Full and open symbols refer to cations and Cl$^{-}$ ions, respectively. Top row (A) refers to simulations for a scaled-charge model for NaCl with TIP4P/2005 water model kohagen_jpcb_2015, while the bottom row (B) refers to simulations for the ECCR2 model for CaCl$_{2}$ with TIP4P/2005 water model. martinek_jcp_2018
  • Figure 2: Radial distribution functions (RDF) for pairs of O$_{\mathrm{S}}$ and Ca$^{2+}$ (left panel) as well as O$_{\mathrm{S}}$ and O$_{\mathrm{w}}$ (right panel), where O$_{\mathrm{S}}$ stands for the oxygen of the deprotonated silanol group and O$_{\mathrm{w}}$ stands for the oxygen atom of the water molecule modeled by the TIP4P/2005 FF. The inset of the left panel zooms in on the depletion zone between the 1st and 2nd peaks. The figure shows results for the ECCR2 model with TIP4P/2005 water. Red and blue curves refer to full-charge and scaled-charge silanol oxygen (O$_{\mathrm{S}}$) models, respectively.
  • Figure 3: From top to bottom: axial ($z$) components of particle current density (in 1/ps$\;$nm$^{2}$), velocity (in nm/ps), and concentration (in mol/dm$^{3}$). Black, blue, red, and green curves refer to pore radii $R^{\mathrm{P}}\approx 1$, $1.3$, $2$, and $3$ nm, respectively. Full and open symbols refer to Ca$^{2+}$ and Cl$^{-}$ ions, respectively. The figure refers to simulations for the scaled-charge silanol oxygen (O$_{\mathrm{S}}$) model and the ECCR2 model of ions with TIP4P/2005 water.
  • Figure 4: From left to right: axial ($z$) components of particle current density (in 1/ps$\;$nm$^{2}$), velocity (in nm/ps), and concentration (in mol/dm$^{3}$). Red and blue curves refer to the FULL and ECCR2 models of Ca$^{2+}$ and Cl$^{-}$, respectively. Full and open symbols refer to Ca$^{2+}$ and Cl$^{-}$ ions, respectively. The figure refers to simulations for the scaled-charge silanol oxygen (O$_{\mathrm{S}}$) model and the TIP4P/2005 model of water.
  • Figure 5: From left to right: axial ($z$) components of particle current density (in 1/ps$\;$nm$^{2}$), velocity (in nm/ps), and concentration (in mol/dm$^{3}$). Black, blue, and red curves refer to the ECC, ECCR2, and ECCR models of Ca$^{2+}$ and Cl$^{-}$, respectively. Full and open symbols refer to Ca$^{2+}$ and Cl$^{-}$ ions, respectively. The figure refers to simulations for the scaled-charge silanol oxygen (O$_{\mathrm{S}}$) model and the TIP4P/2005 model of water.
  • ...and 4 more figures