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Global flow equations for membrane transport from local equations of motion—II. The case of a single nonelectrolyte solute plus water

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Abstract

The global flow equations of nonequilibrium thermodynamics for a single nonelectrolyte solute and water passing through a membrane are obtained by solving the local equations of motion. The method follows that developed for the general,n-solute case in the previous paper (Mikulecky, 1978). It is easily seen in this simple case that the passage from local interactions, formulated as position dependent frictional interactions in the equations of motion, to ghe global result involves a loss of any simple way of identifying particulars about local information. Two particular cases are analyzed in further detail: the case of no interaction within the pore and the case of constant interaction for both solute and solvent across the pore. In the former case, Onsager reciprocity survives in the global result if a self-consistent definition of the partial viscosity coefficients is used, while in the latter case, reciprocity is lost. Since, in many biologically interesting cases, the presence of interaction of the type considered here is likely to occur, the reciprocity condition should not automatically be assumed to hold.

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Mikulecky, D.C. Global flow equations for membrane transport from local equations of motion—II. The case of a single nonelectrolyte solute plus water. Bltn Mathcal Biology 41, 629–640 (1979). https://doi.org/10.1007/BF02462419

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  • DOI: https://doi.org/10.1007/BF02462419

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