In any aqueous solution, water self-ionizes to a tiny extent into hydrogen ions (\(\text{H}^+\)) and hydroxide ions (\(\text{OH}^-\)). This self-ionization is described by the ion product of water, \(\text{K}_w\). At 25°C, \(\text{K}_w\) has a constant value of \(1.0 \times 10^{-14}\). This means:\[\text{K}_w = [\text{H}_3\text{O}^+] \times [\text{OH}^-] = 1.0 \times 10^{-14}\]Using this relationship, if you know the concentration of \(\text{H}_3\text{O}^+\), you can easily find \(\text{OH}^-\) by rearranging the equation:
- \([\text{OH}^-] = \frac{\text{K}_w}{[\text{H}_3\text{O}^+]}\)
For example, using our previously found \(\text{H}_3\text{O}^+\) concentration of 2.5 M:
- \([\text{OH}^-] = \frac{1.0 \times 10^{-14}}{2.5} \approx 4.0 \times 10^{-15}\)
This value shows how the presence of a strong acid like \(\text{HNO}_3\) shifts the balance, reducing the concentration of hydroxide ions significantly, thereby affecting the acidity of the solution.