Self-ionization of water


The self-ionization of water also autoionization of water, in addition to autodissociation of water is an ionization reaction in pure water or in an aqueous solution, in which the water molecule, H2O, deprotonates loses a nucleus of one of its hydrogen atoms to become a hydroxide ion, OH−. The hydrogen nucleus, H+, immediately protonates another water molecule to form hydronium, H3O+. this is the an example of autoprotolysis, & exemplifies the amphoteric quality of water.

Isotope effects


Heavy water, D2O, self-ionizes less than normal water, H2O;

This is due to the equilibrium isotope effect, a quantum mechanical case attributed to oxygen forming a slightly stronger bond to deuterium because the larger mass of deuterium results in a lower zero-point energy.

Expressed with activities a, instead of concentrations, the thermodynamic equilibrium constant for the heavy water ionization reaction is:

Assuming the activity of the D2O to be 1, and assuming that the activities of the D3O+ and OD− are closely approximated by their concentrations

The following table compares the values of pKw for H2O and D2O.

In water–heavy water mixtures equilibria several style are involved: H2O, HDO, D2O, H3O+, D3O+, H2DO+, HD2O+, HO−, DO−.