Solving solubility problems often involves calculating the solubility product constant \( K_{sp} \). The \( K_{sp} \) is a specific type of equilibrium constant applied to the dissolution of sparingly soluble salts. For lead(II) iodide, knowing \( K_{sp} \) helps us quantify its solubility in water and predict how much of it will dissolve under equilibrium conditions.
The expression for \( K_{sp} \) of \( \text{PbI}_2 \) is derived from the equilibrium condition set by dissolving \( \text{PbI}_2 \): \( K_{sp} = [\text{Pb}^{2+}][\text{I}^-]^2 \). From earlier calculations, we found:
- \([\text{Pb}^{2+}] = 0.00117 \, \text{M} \)
- \([\text{I}^-] = 2 \, \times\, 0.00117 \, \text{M} = 0.00234 \, \text{M} \)
By substituting these values in, we calculate:
\[ K_{sp} = (0.00117) \times (0.00234)^2 = 6.43 \times 10^{-9} \text{ M}^3 \]
This calculation demonstrates how to derive \( K_{sp} \) from measured solubility data, offering insights into the solubility characteristics of difficult-to-dissolve compounds like lead(II) iodide. Knowing \( K_{sp} \) enables chemists to predict precipitation conditions and understand ionic equilibria in various chemical systems.