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An Examination of the Evidence for Membrane Pores in Frog Skin

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Journal J Physiol
Specialty Physiology
Date 1966 Jul 1
PMID 5965891
Citations 22
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Abstract

1. Measurements of the diffusional permeability, P(d), 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 P(d) 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, L(p), 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 L(p) 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 L(p)RT/V(w) (where V(w) is the partial molar volume of water) and P(d) 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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From membrane pores to aquaporins: 50 years measuring water fluxes.

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Extracellular Ca2+ and the effect of antidiuretic hormone on the water permeability of the toad urinary bladder: an example of flow-induced alteration of flow.

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References
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HOSHIKO T, LINDLEY B . THE RELATIONSHIP OF USSING'S FLUX-RATIO EQUATION TO THE THERMODYNAMIC DESCRIPTION OF MEMBRANE PERMEABILITY. Biochim Biophys Acta. 1964; 79:301-17. View