In order to clarify the interaction between CO
2 diffusion and HCO
3- shift in the red blood cell (RBC), HCO
3- shift was measured by using a stopped flow method combined with fluorometry. When HCO
3- entered the RBC, the intracellular
PCO2 increased, causing a secondary outflow of CO
2. Conversely, when HCO
3- ions flowed out of the RBC, the resulting decrease of
PCO2 caused an inward CO
2 diffusion. The
PCO2 change caused by the inward HCO
3- shift was about 3- to 4-fold that of the outward shift. During the respective in- and outward-shifts, the mean half times of the extracellular pH changes were 0.15 and 0.13sec. These were approximately twice as long as those of the primary CO
2 diffusion. The permeability of HCO
3- across the RBC membrane was obtained by comparing the experimental extracellular pH curve with a numerical solution for CO
2 and HCO
3- diffusions accompanied by the hydration and dehydration reactions. Thus the HCO
3- permeability was determined to be 5×10
-4 and 7×10
-4cm/sec, in the in- and outward-HCO
3- shifts, respectively. The influence of Cl
- concentration on HCO
3- permeability was tested by reducing the initial Cl
- gradient across the RBC membrane. In a physiological Cl
- concentration range the HCO
3- permeability was not affected by the Cl
- gradient.
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