Understanding transport mechanisms in thin-film composite membranes is critical for advancing membrane technology. While the solution-friction model, or more appropriately, the sorption-friction (SF) model, can describe water and salt transport behavior, the contribution of frictional forces towards salt–water selectivity in different membranes has not been explored. In this study, we establish relationships between intrinsic membrane properties and transport parameters based on the SF model, using permeation experiments and molecular dynamics (MD) simulations. Pore sizes of various commercial thin-film composite membranes are quantified by measuring the rejection of neutral organic solutes. Salt partitioning is measured using quartz crystal microbalance, while salt permeance is determined in a stirred dead-end cell. Our results show that as pore size increased from 0.6 to 0.7 nm, salt partitioning increased by 21.2 %, while salt permeance increased more than tenfold. These results suggest that transport within the membrane, rather than salt partitioning at the membrane surface, is more sensitive to changes in membrane structure. Using the SF model, we show that ion-membrane and water-membrane interactions decrease with larger pore sizes, which may explain the observed differences in salt and water permeances. These findings are supported by MD simulations used to determine ion and water self-diffusion coefficients in five distinct membranes. Through these simulations, we confirmed that water and ion mobilities are greater in membranes with larger pores due to weaker frictional interactions between these species and the membrane. This study demonstrates how frictional forces are related to membrane pore size and can be effectively used to model salt and water transport through the membrane.
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