Worked example 1
The molar solubility of CaF₂ is 2.1 × 10⁻⁴ M. Calculate Ksp.
Try it first: Write out the dissociation and express each ion in terms of s.
0 of 4 steps revealed.
What you'll be able to do: Convert between Ksp and molar solubility and explain quantitatively why a common ion reduces solubility.
Insoluble is a useful lie. Even chalk and limestone dissolve a little, and the equilibrium constant for that tiny amount explains kidney stones, hard water and cave formation.
These are recommended, not required. You can start this lesson at any time.
In a saturated solution, ions leave the crystal surface at the same rate that they rejoin it. Writing that as an equation gives, for example, AgCl(s) ⇌ Ag⁺(aq) + Cl⁻(aq), and the solid drops out of the expression.
Ksp = [Ag⁺][Cl⁻]
Molar solubility s is the number of moles of the salt that dissolve per litre of saturated solution. Each formula unit that dissolves releases ions in the ratio of the formula, so for CaF₂ dissolving to a level s the concentrations are [Ca²⁺] = s and [F⁻] = 2s.
Substituting the ion concentrations gives a fixed relationship for each salt type. For AB salts Ksp = s², for AB₂ or A₂B salts Ksp = 4s³, and for AB₃ salts Ksp = 27s⁴. Going backwards means taking the corresponding root.
CaF₂: Ksp = (s)(2s)² = 4s³
A smaller Ksp only means a less soluble salt when the salts have the same ion ratio. AgCl with Ksp = 1.8 × 10⁻¹⁰ has s = 1.3 × 10⁻⁵ M, whereas Ag₂CrO₄ with a larger Ksp of 1.1 × 10⁻¹² still works out at s = 6.5 × 10⁻⁵ M, five times more soluble. Convert to molar solubility before ranking salts of different types.
Dissolving AgCl in 0.10 M NaCl means starting with chloride already present. That extra product pushes the dissolution equilibrium back toward the solid, so far less AgCl dissolves. In the ICE table the common ion goes in the initial row, and since Ksp is small the approximation 0.10 + s is about 0.10 is almost always safe.
To decide whether mixing two solutions produces a solid, calculate Q from the diluted ion concentrations and compare with Ksp. Q greater than Ksp means a precipitate forms until Q falls back to Ksp.
The equilibrium constant for a solid dissolving into its ions, with the solid omitted.
Moles of salt that dissolve per litre of saturated solution.
AB gives Ksp = s², AB₂ gives 4s³, AB₃ gives 27s⁴.
A shared ion suppresses dissolution and lowers solubility.
Like any K, Ksp changes only with temperature, not with a common ion.
Ksp = s²
Ksp = 4s³
Q > Ksp means a precipitate forms
The molar solubility of CaF₂ is 2.1 × 10⁻⁴ M. Calculate Ksp.
Try it first: Write out the dissociation and express each ion in terms of s.
0 of 4 steps revealed.
Ksp for AgCl is 1.8 × 10⁻¹⁰. Find its molar solubility in pure water.
Try it first: Decide which of the s formulas applies to a 1:1 salt.
0 of 3 steps revealed.
Find the molar solubility of AgCl (Ksp = 1.8 × 10⁻¹⁰ in 0.10 M NaCl.
Try it first: Put the chloride already present into the initial row of the ICE table.
0 of 5 steps revealed.
Why it's wrong: Pure solids are omitted from every equilibrium expression.
Check instead: Write only the aqueous ion terms.
Why it's wrong: The coefficient acts twice, once as a multiplier of s and once as an exponent.
Check instead: Write (2s)², not 2s².
Why it's wrong: The relationship between Ksp and s depends on the ion ratio.
Check instead: Convert each Ksp to a molar solubility first.
Why it's wrong: Ksp changes only with temperature; it is the solubility that falls.
Check instead: State that the equilibrium shifts toward the solid.
Why it's wrong: For AB₂ salts the anion concentration is 2s, not s.
Check instead: Identify s explicitly at the end.
No practice questions are available for this topic yet. You can still practice the whole unit.
A saturated solution of a sparingly soluble salt is an equilibrium between the undissolved solid and its ions, described by the solubility product Ksp. Because the solid is a pure phase it does not appear in the expression, so Ksp is simply the product of ion concentrations raised to their coefficients. Molar solubility s is the moles of salt that dissolve per litre, and the relationship between s and Ksp depends on the formula: AB gives Ksp = s² while AB₂ gives Ksp = 4s³. Comparing Ksp values directly only ranks solubility fairly for salts with the same ion ratio. Adding an ion the salt already contains shifts the dissolution equilibrium back toward the solid, so solubility drops sharply, which is the common ion effect.
This lesson is original Chem Help content. No external sources were adapted.