The effect of pH on the kinetics of iron release from diferric ovotransferrin induced by pyrophosphate.

Pyrophosphate-induced iron release from diferric ovotransferrin follows biphasic kinetics in the pH range from 6.6 to 8.6 except at pH 8.0 where the kinetics become monophasic. The rates of formation of the four molecular species, Fe2OT, FeOTN, FeOTC, and ApoOT, were studied by urea gel electrophoresis and the four microscopic rate constants were calculated at various pH values. Below pH 8.0, these intrinsic rate constants for iron release from Fe2OT follow the order k2N greater than k1N greater than k2C greater than k1C. Each constant diminishes almost proportionally with an increase in pH with the faster rate constants being affected more by the fall in hydrogen ions than the slower ones. Around pH 8.0 the four rates are approximately equal, resulting in monophasic kinetics. However, the rate constants from the C-site become faster than that from the N-site at pH above 8.2. At low pH, there is a marked preference for iron to be released from the N-site rather than from the C-site and such preference becomes less distinct as pH increases. A rather weak positive cooperativity between the two sites is demonstrated in pH between 6.8 and 7.8. The ligand responsible for the transition from biphasic to monophasic kinetics at pH 8.0 is not known. It is possible that there are different anions such as [CO3(2-)] and [HCO3-] at the two iron-binding sites, which might explain the preferential rates of iron release from these sites during protonation.