The water dissociation constant, often referred to as \( K_w \), is a fundamental concept when discussing the ionization of water. This constant gives us insights into the extent to which water naturally breaks down into hydronium and hydroxide ions at a particular temperature.At the standard temperature of \( 25^{\circ} \text{C} \), the value of \( K_w \) is \( 1.0 \times 10^{-14} \). This means at this temperature, the product of the concentrations of \( \text{H}_3\text{O}^+ \) and \( \text{OH}^- \) ions in pure water is always equal to \( 1.0 \times 10^{-14} \).This constant value is crucial for calculating ion concentrations in aqueous solutions and helps us understand the nature of acidic or basic solutions.
- \( K_w \) at \( 25^{\circ} \text{C} \) = \( 1.0 \times 10^{-14} \)
- Indicates equilibrium between hydronium and hydroxide ions
- Basis for pH and pOH calculations