Calculate the solubility of a salt based on the value of Ksp for the salt.
The dissolution of a salt is a reversible process whose extent is described by Ksp, the solubility-product constant. For a saturated solution:
AgCl(s) ⇌ Ag⁺(aq) + Cl⁻(aq) Ksp = [Ag⁺][Cl⁻]
The solid is excluded, so Ksp is just the product of the ion concentrations, each raised to its coefficient.
Molar solubility (s) is the moles of salt that dissolve per litre to give a saturated solution. Converting between s and Ksp is the core skill, and the relationship depends on the ion ratio:
EK 7.11.A.3 connects back to Unit 4: the solubility rules can be quantitatively related to Ksp, with Ksp values greater than 1 corresponding to soluble salts.
Qsp versus Ksp predicts precipitation:
A critical comparison rule: you may compare Ksp values directly to rank solubility only when the salts have the same ion ratio. Otherwise convert both to molar solubility first.
Ksp for PbI₂ is 7.1 × 10⁻⁹ at 25 °C. (a) Calculate its molar solubility. (b) Calculate its solubility in g/L. (c) Ag₂CrO₄ has Ksp = 1.1 × 10⁻¹², and AgCl has Ksp = 1.8 × 10⁻¹⁰. Which is more soluble?
(a) Molar solubility of PbI₂.
PbI₂(s) ⇌ Pb²⁺(aq) + 2 I⁻(aq)
Let s = molar solubility. Then [Pb²⁺] = s and [I⁻] = 2s.
Ksp = [Pb²⁺][I⁻]² = (s)(2s)² = 4s³
7.1 × 10⁻⁹ = 4s³
s³ = 1.775 × 10⁻⁹
s = 1.2 × 10⁻³ M
(b) In g/L. M(PbI₂) = 207.2 + 2(126.9) = 461.0 g/mol
(1.2 × 10⁻³ mol/L)(461.0 g/mol) = 0.55 g/L
(c) Comparing across different ion ratios — convert both to s.
AgCl (1:1): Ksp = s² → s = √(1.8 × 10⁻¹⁰) = 1.3 × 10⁻⁵ M
Ag₂CrO₄ (2:1): Ksp = (2s)²(s) = 4s³ → s³ = 1.1 × 10⁻¹²/4 = 2.75 × 10⁻¹³ → s = 6.5 × 10⁻⁵ M
Ag₂CrO₄ is about five times more soluble, even though its Ksp is nearly 200 times smaller. This is exactly why Ksp values cannot be compared directly across different ion ratios.