Abstract
A simple method of measuring proton/hydroxide conductance (G H/OH) through planar lipid bilayer membranes is described. First the total conductance (G m ) is measured electrically. Then the H+/OH transference number (T H/OH) is estimated from the diffusion potential (V m ) produced by a transmembrane pH gradient. The pH gradient is produced by a pair of buffered solutions which have identical concentrations of all ions except H+ and OH. Thus,V m is due entirely to H+/OH diffusion andG H/OH can be calculated from the relations,V m =T H/OH E H/OH andG H/OH=T H/OH G m , whereE H/OH is the equilibrium potential for H+ and OH. In bilayers made from bacterial phosphatidylethanolamine (PE) inn-decane,G H/OH is nearly independent of pH, ranging from about 10−9 S cm−2 at pH 1.6 to 10−8 S cm−2 at pH 10.5. BecauseG H/OH is nearly independent of pH, the calculated permeability coefficients to H+ and/or OH are extremely pH dependent, which partly explains the wide range of values reported for phospholipid vesicles and biological membranes.G H/OH appears to be independent of the membrane surface charge, because titrating either the phosphate or the amino group of PE has little effect onG H/OH.G H/OH is reduced about 10-fold when the water activity is reduced 33% by replacement with glycerol. Although the mechanism of H+/OH conductance is not known, the relation betweenG H/OH and water activity suggests that several water molecules are involved in the H+/OH transport process.