The solubility product constant is the equilibrium constant for the dissolution of a sparingly soluble ionic solid in water. It is represented by the symbol Ksp and applies to an equilibrium between a pure solid ionic compound and its saturated aqueous solution.
Ksp is a type of equilibrium constant and its numerical value depends on temperature. For most salts, Ksp increases with rising temperature because solubility usually increases with temperature.
Solubility is the property of a solute to dissolve in a given solvent to form a homogeneous solution. For ionic compounds, solubility in water depends on a balance between the lattice enthalpy of the solid and the solvation (hydration) enthalpy of its ions.

Classification of salts on the basis of solubility

Consider the sparingly soluble salt barium sulphate, BaSO4, in contact with its saturated aqueous solution. The dissolution equilibrium is:

The equilibrium constant expression for this reaction is:

Because the activity (or concentration) of a pure solid is constant, it is incorporated into the equilibrium constant. The remaining measurable equilibrium constant is called the solubility product:

Thus, at equilibrium between solid BaSO4 and its saturated solution, the product of the molar concentrations of Ba2+ and SO42- (each raised to the power of its stoichiometric coefficient) is constant at a given temperature. This constant is the Ksp of BaSO4.
For a salt that dissolves according to the stoichiometry:
MX(s) ⇌ M+(aq) + X-(aq)
let the molar solubility of MX be s mol L-1 (i.e., the concentration of M+ and X- produced in a saturated solution). Then:
[M+] = s
[X-] = s
Ksp = [M+][X-] = s × s = s2
For a salt of the type M2X (dissociating to 2 M+ + X2-), if molar solubility is s then:
[M+] = 2s
[X2-] = s
Ksp = (2s)2(s) = 4s3
The common-ion effect is the suppression of the dissociation of a weak electrolyte when a strong electrolyte containing a common ion is added. This is a direct application of Le Châtelier's principle to equilibria involving ionization.
In general, if a salt with equilibrium MaXb ⇌ a Mm+ + b Xn- is in contact with its saturated solution, adding a soluble salt that provides either Mm+ or Xn- will shift the equilibrium to the left and decrease the solubility of the original salt.
Example (qualitative): When hydrogen chloride gas is passed into a saturated sodium chloride solution, the extra chloride ions push the equilibrium NaCl(s) ⇌ Na+ + Cl- to the left, favouring precipitation of NaCl. This is the common-ion effect acting on a saturated solution.

Some compounds of transition metals do not show simple common-ion behaviour because transition metal ions often form complex ions with ligands such as Cl-. For example, cuprous chloride, CuCl, is sparingly soluble in water, but on addition of excess chloride ions it dissolves due to formation of a soluble complex ion (for example [CuCl2]-), increasing the apparent solubility.
Consider MX(s) ⇌ M+ + X- with Ksp = [M+][X-] and molar solubility in pure water equal to s.
[M+] = s
[X-] = s
Ksp = s2
Now suppose a soluble salt that supplies X- is present and its concentration of X- from that source is c (c ≫ s). In the new equilibrium:
[M+] = s'
[X-] = c + s'
Ksp = s'(c + s')
If c ≫ s', then s' ≈ Ksp/c.
Thus the solubility of MX in the presence of a large concentration of the common ion X- is approximately inversely proportional to the common-ion concentration.
Salts containing anions that are the conjugate bases of weak acids (for example CO32-, PO43-, F-, OH-) exhibit solubility that depends strongly on pH.
These pH effects are exploited in processes such as removing carbonate hardness from water by precipitation or dissolving carbonate deposits by acid treatment.
When a metal ion forms a stable complex with a ligand present in solution, the free metal ion concentration decreases and the dissolution equilibrium of the sparingly soluble salt shifts to the right, increasing solubility.
For example, for AgCl(s):
AgCl(s) ⇌ Ag+ + Cl-, Ksp = [Ag+][Cl-]
In the presence of excess Cl-, complex ions such as [AgCl2]- can form:
Ag+ + 2 Cl- ⇌ [AgCl2]-
Formation constant of the complex reduces free [Ag+], so more AgCl dissolves to re-establish Ksp. Thus complex formation increases apparent solubility.
The ionic product or reaction quotient Q for a dissolution is defined exactly like Ksp but for the instantaneous concentrations (not necessarily at equilibrium):
Q = [M+]a[X-]b (where a and b are stoichiometric numbers)
Consider AgCl(s) ⇌ Ag+ + Cl- with Ksp = [Ag+][Cl-] and molar solubility in pure water equal to s.
[Ag+] = s
[Cl-] = s
Ksp = s2
If the solution already contains chloride ions at concentration c (for example from NaCl), then at the new equilibrium:
[Ag+] = s'
[Cl-] = c + s'
Ksp = s'(c + s')
If c ≫ s', then s' ≈ Ksp / c, showing that the solubility of AgCl is reduced when a common ion Cl- is present.
The solubility product constant (Ksp) is a central concept for understanding the solubility of sparingly soluble salts. Solubility depends on lattice and solvation enthalpies, temperature, presence of common ions, pH, complex formation and ionic interactions. The common-ion effect reduces solubility and is routinely used in water treatment, precipitation techniques and analytical chemistry. Comparing the instantaneous ionic product (Q) with Ksp allows prediction of precipitation, while formation of complexes or changes in pH can greatly alter solubility in ways that can be exploited in laboratory and industrial processes.
| 1. What is solubility equilibrium? | ![]() |
| 2. How does temperature affect the solubility equilibrium of sparingly soluble salts? | ![]() |
| 3. What factors determine the solubility of sparingly soluble salts? | ![]() |
| 4. How can we calculate the solubility product constant (Ksp) for sparingly soluble salts? | ![]() |
| 5. What are some common applications of solubility equilibria for sparingly soluble salts? | ![]() |