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. 1978 Apr;234(4):F340-8.
doi: 10.1152/ajprenal.1978.234.4.F340.

Volume absorption in the pars recta. II. Hydraulic conductivity coefficient

Volume absorption in the pars recta. II. Hydraulic conductivity coefficient

J A Schafer et al. Am J Physiol. 1978 Apr.

Abstract

We evaluated the hydraulic conductivity (Pf, micron s-1) of superficial proximal straight tubules isolated from rabbit kidney. Tubules were perfused with hypotonic (270 mosmol/kg H2O) and bathed with isotonic (290 mosmol/kg H2O) NaCl buffers at 25 degrees C. Due to the tendency of transepithelial osmosis plus solute entry to produce osmotic equilibrium along the perfused length, we observed that the total net volume absorption ('JV, nl min-1) increased from 0.64 to 2.21 when the perfusion rate (VO, nl min-1) was increased from 11 to 45 in a group of tubules with an average length of 0.86 mm. From a 'JV of 2.21 nl min-1 at VO = 45 nl min-1 we computed a minimum Pf of 2,200 micron s-1. And extrapolation of the data to VO leads to infinity gave a Pf value of 5,200-7,600 micron s-1. The same perfusion rate dependence of 'JV in a group of tubules with an average length of 3.29 mm gave quantitatively similar results. A theoretical analysis of radial osmosis occurring simultaneously with axial osmotic equilibration showed that Pf values in the range of 3,000-4,000 micron s-1 accurately predicted the observed relations between VO, 'JV, and tubule length.

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