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Salt-water coupling in leaky epithelia

Summary

This study examines how fluids move through leaky epithelial tissues. It challenges a long-standing theory that relies on cellular osmosis to explain transport. The authors argue that the osmotic permeability of epithelial membranes is too low to support this theory. They show that unstirred-layer effects cannot fully explain the observed discrepancies. Instead, fluid movement may occur through junctional pathways rather than cellular ones. The study suggests that junctional pores cannot support both osmotic and diffusive transport simultaneously. Non-osmotic mechanisms like electro-kinetic or peristaltic flow may better explain fluid transport. The authors conclude that current evidence supports junctional transport over traditional osmotic models. This work contributes to resolving a long-standing debate in epithelial physiology.

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