In the world of acid-base chemistry, the water dissociation constant, represented as \(K_w\), is a key concept for understanding how water ionizes into hydrogen and hydroxide ions. At standard temperature, which is 25°C, the value of \(K_w\) is given as:\[K_w = [H_3O^+][OH^-] = 1.0 \times 10^{-14}\]This equilibrium constant is a product of the molar concentrations of hydronium ions \([H_3O^+]\) and hydroxide ions \([OH^-]\).
- This means that in pure water at 25°C, both \([H_3O^+]\) and \([OH^-]\) are equal and approximately \(1.0 \times 10^{-7}\; \text{M}\).
- The constant applies to any aqueous solution, not just pure water.
Partial ionization of water can impact the pH level of the solution, affecting whether it is acidic, neutral, or basic. This principle is fundamental for calculating ion concentrations in different solutions.