Abstract

Cells of the rabbit renal cortical collecting tubule possess significant regulatory volume decrease (RVD) capabilities. After a 100-mosmol/kg reduction in peritubular osmolality, principal and intercalated cells swell 40-45 and 30-35%, respectively, and immediately activate RVD mechanisms. Both cell types downregulate their volume to within 5-6% of control volume at initial rates of 3-6%/min. Return to isotonic saline causes both cell types to shrink (isotonic shrinkage) 25-35% below control volume due to the loss of osmotically active intracellular solutes during RVD. In most mammalian cells studied to date, RVD is mediated largely by passive KCl efflux via KCl cotransport, parallel K+ and Cl- channels, or parallel K+-H+ and Cl- -HCO3- exchange mechanisms. Peritubular application of 0.1 mM ouabain (0 Na+ lumen), bilateral CO2-HCO3- removal, or bilateral application of 0.02 mM bumetanide, 2.0 mM Ba2+, 2.0 mM anthracene-9-carboxylic acid, or 0.5 mM SITS had no significant effect on rates or magnitudes of RVD and isotonic shrinkage in either cell type. Bilateral elevation of K+ from 5 to 52.5 mM reverses or reduces the electrochemical gradient for K+ movement, causing accumulation of this ion in the cytoplasm, but had no effect on the rates or magnitude of principal and intercalated cell RVD. Principal and intercalated cells from K+- or Cl- -depleted tubules (1 h bilateral perfusion with K+- or Cl- -free saline at 37 degrees C) showed normal rates and magnitudes of RVD in K+- or Cl- -free hypotonic saline. Taken together, these results argue against a significant role of passive KCl efflux pathways in mediating principal and intercalated cell RVD.

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