Until now, we have assumed that the pH of an aqueous solution of acid or base is determined only by the dissociation of the acid or base itself. However, as described in earlier sections, there is always another acid or base present in the solution- water. Since water dissociates to form H+ and OH-, it affects the pH of the solution. Usually we ignore this effect because water is only very weakly acidic and basic, allowing us to assume that its contribution to the pH of the solution is negligible compared to that of other acids or bases present. However, this assumption is not valid when the concentrations of H+ or OH- due to the dissociation of water are comparable to those due to the dissociation of other acids or bases in solution.

Here we consider the case where water produces a [H+] comparable to that produced by an acid in solution. However, an exactly equivalent case exists for the [OH-] and bases.

At 25oC, pure water dissociates to give a [H+] of 1.0x10-7M. Thus, whenever the [H+] due to the acid in solution is low enough to be close to 1.0x10-7M, the dissociation of water will significantly affect the pH of the solution. This means that we must discard the assumption that water makes a negligible contribution to the pH in order to accurately calculate the pH of the solution. (We will see later how to tell whether or not the [H+] is low enough for water to contribute to the pH.)

Consider a dilute acid solution. The pH will be determined by following two equilibria:

HA H+ + A-

H2O H+ + OH-

We can easily predict what would happen if each of these equilibria was the only source of of H+ in the solution: