Abstract

Kinetical parameters of monovalent cation uptake in yeast are calculated according to a model for mutual interaction of membrane potential and cation uptake. Apparent K m values for monovalent cation uptake obtained from uptake studies are 3–5-times lower than the K m values expected when the membrane potential remains constant at increasing cation concentrations instead of being reduced. The model accounts for varius phenomena as (i) the increase in apparent K m of Rb + uptake accompanying the decrease in maximum rate of uptake found on increasing the cellular K + content, (ii) the decrease in maximum uptake rate and increase in K m in case of simultaneous transport of phosphate and Rb +, (iii) the change in the maximum uptake rate without a change in K m under conditions that the proton pump is effected and (iv) the absence of an increase in K + efflux at high depolarizing external cation concentrations.

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