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1. Measurements of the diffusional permeability, Pd, of tritiated water in isolated frog skin bathed in sulphate Ringer have been made under different stirring conditions.
2. The mean ± S.E. values for Pd were found to be (6·5 ± 0·3), (7·9 ± 0·5), (9·7 ± 0·7) and (11·1 ± 0·8) x 10-5 cm sec-1 at 120, 300, 500 and 1000 rev/min. It is considered that these results indicate the existence of `unstirred layers' associated with frog skin.
3. The hydraulic conductivity, Lp, of the skin in sulphate Ringer was found to be (2·36 ± 0·07) x 10-7 cm sec-1 atm-1 (± S.E. of estimate), and no marked increase in this value for Lp was found when the stirring rate was increased from 0 to 500 rev/min.
4. It is considered that these results show that previous comparisons of the relative magnitudes of LpRT/
w (where
w is the partial molar volume of water) and Pd for frog skin have been in error because of the presence of `unstirred layers'.
5. The bearing of our results and other evidence on the question of pores in cell membranes has been discussed.
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