The autodissociation of water is another important chemical process impacting
pH
and
pOH
calculations, particularly in very dilute solutions. In pure water, molecules auto-dissociate into hydrogen ions (
H^+
) and hydroxide ions (
OH^-
), even in the absence of other substances. This dissociation constant for water is known as
K_w
and equals
1 imes 10^{-14}
at 25°C.
For very low concentrations of strong bases like
1.2 imes 10^{-8} ext{M}
KOH, the autodissociation of water becomes significant. In low concentrations, the
OH^-
ions from the dissociation of KOH can nearly equal those from water's self-ionization, thus affecting the solution's overall
pH
.
- This effect is sometimes overlooked in concentrated solutions, but it's essential to consider in dilute cases.
- At equilibrium, the relation
pH + pOH = 14
holds, provided we factor in the ions from water itself.
Therefore, when approaching pH calculations in low concentration bases, it is important to remember the potential contribution from pure water.