Proton nuclear magnetic resonance measurement of diffusional water permeability in suspended renal proximal tubules.

Diffusional water permeability was measured in renal proximal tubule cell membranes by pulsed nuclear magnetic resonance using proton spin-lattice relaxation times (T1). A suspension of viable proximal tubules was prepared from rabbit renal cortex by Dounce homogenization and differential sieving. T1 measured in a tubule suspension (22% of exchangeable water in the intracellular compartment) containing 20 mM extracellular MnCl2 was biexponential with time constants 1.8 +/- 0.1 ms and 8.3 +/- 0.2 ms (mean +/- SD, n = 8, 37 degrees C, 10 MHz). The slower time constant, representing diffusional exchange of water between intracellular and extracellular compartments, increased to 11.6 +/- 0.6 ms (n = 6) after incubation of tubules with 5 mM parachloromercuribenzene sulfonate (pCMBS) for 60 min at 4 degrees C and was temperature dependent with activation energy Ea = 2.9 +/- 0.4 kcal/mol. To relate T1 data to cell membrane diffusional water permeabilities (Pd), a three-compartment exchange model was developed that included intrinsic decay of proton magnetization in each compartment and apical and basolateral membrane water transport. The model predicted that the slow T1 was relatively insensitive to apical membrane Pd because of low luminal/cell volume ratio. Based on this analysis, basolateral Pd (corrected for basolateral membrane surface convolutions) is 2.0 X 10(-3) cm/s, much lower than corresponding values for basolateral Pf (10-30 X 10(-3) cm/s) measured in the intact tubule and in isolated basolateral membrane vesicles. The measured P,/Pd> 1, low Ea and inhibition of Pd by pCMBS provide strong evidence that water transport in the proximal tubule basolateral membrane is facilitated by a specialized aqueous pore or narrow channel.