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.
