Vesicle acidification driven by a millionfold proton gradient: a model for acid influx through gastric cell membranes

A delta pH 6 proton (internal pH 7.5, external pH 1.5) was imposed across the bilayer of egg phosphatidylcholine (PC) vesicles. The presence of the gradient was verified by the use of agents that predictably collapsed it. These agents included a detergent (Triton X-100), a pore-forming Na-H+ exchanger (nigericin), and weak acids capable of shuttling protons across the membrane (acetic and acetylsalicylic acids). The magnitude of the proton gradient and the rate of pH gradient collapse were determined by measuring pyranine fluorescence by use of an isosbestic point technique and calculating intravesicular pH from a calibration curve. Acid flux into the vesicles in the presence of chloride was measured directly by a simpler one-wavelength method. p-Xylene-bis-pyridinium bromide (DPX), a pyranine fluorescence quencher, was used to verify that the fluorescence signal originated from within the vesicles and that the observed rates of acidification were not an artifact due to pyranine leakage. Acid flux was found to be dependent on the ionic composition of the buffer. The presence of chloride ion in the external compartment caused a dramatic increase in the rate of acidification. It was demonstrated that the kinetics of acid flux into the vesicle were clearly controlled by the chloride-dependent mechanism at a relatively low chloride concentration of 2.5 mM. The model presented here is a simple and sensitive method for investigating the factors that influence acidification rates across membranes when acidification is driven by extremely large proton gradients, in the presence of chloride; conditions similar to those found in the stomach.