Chloride flux in bilayer membranes: chloride permeability in aqueous dispersions of single-walled, bilayer vesicles

Abstract

Aqueous dispersions of phosphatidylcholine vesicles were utilized to determine bilayer permeability to 36-Cl as a function of pH and temperature. These dispersions were comprised of single-walled vesicles, homogeneous in size, prepared by sonication of purified egg phosphatidylcholine under argon followed by fractionation on a molecular sieve. Permeability constants calculated from the inward flux of 36-Cl and the geometric parameters of these vesicles proved to be dependent on both pH and temperature. Analysis of these dependences leads to the conclusion that 36-Cl permeation in the presence of KCl is due principally to a carrier mediated exchange process involving a phospholipid-HCL complex. Net permeation by H-36-Cl may make a small contribution to the 36-Cl flux, however, studies carried out at very low chloride concentrations show that this flux is much smaller than the exchange flux. Thus chloride permeability for the exchange process is 1.5 times 10- minus 11 cmsec- minus 1 while the corresponding coefficient for the net flux of H-36-Cl is 1.0 times 10- minus 12 cm sec- minus 1 at pH 7. The activation energy for the 36-Cl exchange flux was found to be 19 plus or minus 2 kcal/mol. This value is similar to that obtained for the transbilayer "flip-flop" of phosphatidylcholine molecules in a similar system (Kornberg and McConnell, 1971). This correspondence together with the fact that the experimentally determined flux of 36-Cl agrees well with that calculated from the "flip-flop" parameters, strongly suggests that the flux of 36-Cl and "flip-flop" of phosphatidylcholine may be the same process.