Salt-water coupling in leaky epithelia.
The theory of quasi-isotonic transport by cellular osmosis (the standing-gradient theory) has been challenged on the grounds that the osmotic permeabilities of the mucosal and interspace membranes are too low; if they were as high as the theory requires then the osmotic permeability of the whole epithelium would be 2-3 orders of magnitude higher than observed. This objection has basically been accepted for it is now claimed that these enormous permeabilities do exist, but are masked by unstirred-layer effects; I show that this is incorrect because unstirred-layer corrections are small and that the situation has not changed since 1975. The view that the route of fluid transport is junctional is replacing the cellular theory, and trans-junctional water flows seem to account for major fractions of the flow in various epithelia. I argue on grounds of general theory that these are unlikely to be osmotic flows because the junctional pores cannot satisfy both the osmotic and diffusive properties required of them, but the basic osmotic theory is also rather vague here. Non-osmotic theories, if junctional flow is accepted, must be either electro-kinetic or peristaltic.
D000818:Animals; D001693:Biological Transport, Active; D002463:Cell Membrane Permeability; D004848:Epithelium / Q000378:metabolism*; D005544:Forecasting; D007365:Intercellular Junctions / Q000378:metabolism; D008433:Mathematics; D008564:Membrane Potentials; D008954:Models, Biological; D009092:Mucous Membrane / Q000378:metabolism; D009995:Osmosis; D010873:Pinocytosis; D012965:Sodium Chloride / Q000378:metabolism*; D014867:Water / Q000378:metabolism*
D014867:Water; D012965:Sodium Chloride