Abstract

T84 is an established cell line expressing an enterocyte phenotype whose permeability properties have been widely explored. Osmotic permeability (POSM), hydraulic permeability (PHYDR) and transport-associated net water fluxes (JW-transp), as well as short-circuit current (ISC), transepithelial resistance (RT), and potential difference (deltaVT) were measured in T84 monolayers with the following results: POSM 1.3 +/- 0.1 cm.s-1 x 10-3; PHYDR 0.27 +/- 0.02 cm.s-1; RT 2426 +/- 109 omega.cm2, and deltaVT 1.31 +/- 0.38 mV. The effect of 50 microM 5,6-dichloro-1-ethyl-1,3-dihydro-2H-benzimidazol-2-one (DCEBIO), a "net Cl- secretory agent", on T84 cells was also studied. We confirm the reported important increase in ISC induced by DCEBIO which was associated here with a modest secretory deltaJW-transp. The present results were compared with those reported using the same experimental approach applied to established cell lines originating from intestinal and renal epithelial cells (Caco-2, LLC-PK1 and RCCD-1). No clear association between PHYDR and RT could be demonstrated and high PHYDR values were observed in an electrically tight epithelium, supporting the view that a "water leaky" barrier is not necessarily an "electrically leaky" one. Furthermore, the modest secretory deltaJW-transp was not consistent with previous results obtained with RCCD-1 cells stimulated with vasopressin (absorptive fluxes) or with T84 cells secreting water under the action of Escherichia coli heat stable enterotoxin. We conclude that, while the presence of aquaporins is necessary to dissipate an external osmotic gradient, coupling between water and ion transport cannot be explained by a simple and common underlying mechanism.

Highlights

  • Epithelial barriers are classified as “tight” or “leaky” according to their electrical conductance [1], which in general decreases with barrier tightness

  • It is accepted that fluxes generated by hydrostatic pressure gradients (JW-hydr) move across the intercellular spaces, while the main route for those induced by an external osmotic gradient (JW-osm) is controversial

  • POSM (Table 1) was calculated from the slope of the regression curve obtained from JW values and the applied osmotic gradients

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Summary

Introduction

Epithelial barriers are classified as “tight” or “leaky” according to their electrical conductance [1], which in general decreases with barrier tightness. Two different permeability coefficients of water net fluxes can be measured: osmotic (POSM) and hydrostatic (PHYDR) [2]. Correlation between electric and water permeability properties is especially important when a so-called electrogenic ionic transport is observed, resulting in a net salt transfer across the barrier. A net fluid transfer (JW-transp) is frequently associated with salt movement by a process that is not clearly understood [3,4]. These water movements, driven by a salt transport-generated osmotic gradient, could occur among or across epithelial cells

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