Understanding Water Self-ionisation and Equilibrium Constants
Expert reviewed •22 November 2024• 5 minute read
Introduction
Water molecules can transfer protons between themselves in a process called self-ionization. This fundamental concept in chemistry helps us understand acid-base equilibria and forms the foundation for calculating pH and pOH in aqueous solutions.
The Self-ionization Process
In pure water, molecules continuously undergo a reversible reaction where a proton transfers from one water molecule to another. This process produces hydronium (H3O+) and hydroxide (OH−) ions:
2H2O(l)⇌H3O+(aq)+OH−(aq)
At 25°C, this equilibrium is characterized by the water ionization constant (Kw):
Kw=[H3O+][OH−]=1.0×10−14
Temperature Effects on Water Self-ionization
The self-ionization of water is an endothermic process (ΔH>0). Temperature changes affect the equilibrium in the following ways:
Above 25°C: Kw increases as the equilibrium shifts toward products
Below 25°C: Kw decreases as the equilibrium shifts toward reactants
Despite these changes in Kw, pure water remains neutral at all temperatures because [H3O+]=[OH−].
The Ka-Kb Relationship
The water ionization constant connects the acid dissociation constant (Ka) and base dissociation constant (Kb) through the relationship:
Kw=Ka×Kb=1.0×10−14 (at 25°C)
For a weak acid HA and its conjugate base A⁻, we can write: