Kinetics of K-Cl Cotransport in Frog Erythrocyte Membrane: Effect of External Sodium

Abstract.

In frog red blood cells, K-Cl cotransport (i.e., the difference between ouabain-resistant K fluxes in Cl and NO₃) has been shown to mediate a large fraction of the total K⁺ transport. In the present study, Cl⁻-dependent and Cl⁻-independent K⁺ fluxes via frog erythrocyte membranes were investigated as a function of external and internal K⁺ ([K⁺] _e and [K⁺] _i ) concentration. The dependence of ouabain-resistant Cl⁻-dependent K⁺ (⁸⁶Rb) influx on [K⁺] _e over the range 0–20 mm fitted the Michaelis-Menten equation, with an apparent affinity (K _m ) of 8.2 ± 1.3 mm and maximal velocity (V _max ) of 10.4 ± 1.6 mmol/l cells/hr under isotonic conditions. Hypotonic stimulation of the Cl⁻-dependent K⁺ influx increased both K _m (12.8 ± 1.7 mm, P < 0.05) and V _max (20.2 ± 2.9 mmol/l/hr, P < 0.001). Raising [K⁺] _e above 20 mm in isotonic media significantly reduced the Cl⁻-dependent K⁺ influx due to a reciprocal decrease of the external Na⁺ ([Na⁺] _e ) concentration below 50 mm. Replacing [Na⁺] _e by NMDG⁺ markedly decreased V _max (3.2 ± 0.7 mmol/l/hr, P < 0.001) and increased K _m (15.7 ± 2.1 mm, P < 0.03) of Cl⁻-dependent K⁺ influx. Moreover, NMDG⁺ Cl substitution for NaCl in isotonic and hypotonic media containing 10 mm RbCl significantly reduced both Rb⁺ uptake and K⁺ loss from red cells. Cell swelling did not affect the Na⁺-dependent changes in Rb⁺ uptake and K⁺ loss. In a nominally K⁺(Rb⁺)-free medium, net K⁺ loss was reduced after lowering [Na⁺] _e below 50 mm. These results indicate that over 50 mm [Na⁺] _e is required for complete activation of the K-Cl cotransporter. In nystatin-pretreated cells with various intracellular K⁺, Cl⁻-dependent K⁺ loss in K⁺-free media was a linear function of [K⁺] _i , with a rate constant of 0.11 ± 0.01 and 0.18 ± 0.008 hr⁻¹ (P < 0.001) in isotonic and hypotonic media, respectively. Thus K-Cl cotransport in frog erythrocytes exhibits a strong asymmetry with respect to transported K⁺ ions. The residual, ouabain-resistant K⁺ fluxes in NO₃ were only 5–10% of the total and were well fitted to linear regressions. The rate constants for the residual influxes were not different from those for K⁺ effluxes in isotonic (∼0.014 hr⁻¹) and hypotonic (∼0.022 hr⁻¹) media, but cell swelling resulted in a significant increase in the rate constants.