Abstract

The transport of potassium, sodium and various anions in rat-liver mitochondria was studied mainly by analysis of ion content and water compartmentation of the mitochondrial pellet. A comparison of spontaneous transport with valinomycin- or gramicidin-stimulated transport is made. The rate or extent of uptake, the internal concentrations and the concentration ratio (Cin/Cout) are calculated and compared to test existing models for ion transport in mitochondria. Several models of ion transport in mitochondria are based on a cation-pump which is directed inward. This hypothesis is rejected because of the following findings: (1) Valinomycin stimulates the rate of potassium uptake but does not increase the potassium concentration ratio that can be actively maintained in a steady state (in which there is no potassium flow). (2) Valinomycin greatly stimulates the efflux of42K from mitochondria during the process of potassium accumulation. When potassium accumulation is stimulated the flux ratio, i.e. influx/efflux, decreases; in the presence of valinomycin this ratio approaches 1. (3) In the presence of gramicidin, the concentration ratios of potassium and sodium are about the same under a variety of conditions. These findings indicate that potassium and sodium transport are passive processes of relaxation towards electro-chemical equilibrium (of the potassium and sodium). In high external potassium concentrations the extent of potassium uptake is limited by the permeation of anions; of the permeating anions multivalent acids support a higher extent than monovalent acids. It was found that succinate, acetate and oxalate which are transported together with potassium are distributed in accordance with the ΔpH and without any relation to the potassium concentration ratio. These findings are compatible with the hypothesis that an outward-directed proton pump creates an electrical potential gradient, which shifts the equilibrium state for the cations and drives sodium and potassium inward, and also creates proton gradient that is the driving force for anion transport.

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