The flow method of reaction rate measurement has been adapted to the determination of the rate of diffusion of water into the human red cell. In seven experiments the half-time for diffusion exchange has been found to be 4.2 4-1.1 reset., which is equivalent to a diffusion flow of 8.6 × 10 -9 ml. H20/(see., red cell). This figure has been compared with the rate of water entrance under an osmotic pressure gradient, and has been found to be smaller by a factor of 2.5. The difference between these two rates of water entrance has been interpreted as indicating the presence of water-filled channels in the membrane. An estimate of the equivalent radius of these channels (on the assumption of uniform right cylindrical pores) leads to a value of 3.5 ,~., which is viewed as an operational description of the resistance offered by the membrane to the passage of water.The present experiments were undertaken to measure the in vitro exchange rate of water across the human red cell membrane under isotonic conditions, using tritiated water (THO) as a tracer. To determine the time course of this rapid exchange, a flow method was devised, based on the principles developed by Hartridge and Roughton (1), Dirken and Mook (2), and Chance (3). Freshly drawn, heparinized, whole blood or fresh red cell suspensions were mixed with an isotonic red cell buffer containing THO, and the rate of uptake of the T H O by the cells was followed. The rates of entrance of water by diffusion and by osmosis were then used to calculate an equivalent pore size for the red cell membrane.
Experimental MethodPrinciples. m A suspension of ceils and tritiated, isotonic buffer is mixed and forced down an observation tube. As the mixture flows down the tube, the non-labelled intracellular