Using the model
Symbols, assumptions and limitations
The model assumes ideal dilute-solution behavior and complete dissociation of the amount that dissolves. Pure solid is omitted from Ksp. Added common-ion concentrations are treated as fixed initial concentrations; activities, complex formation, acid–base reactions, and competing equilibria are excluded. Tabulated Ksp values depend on temperature and may vary by source.
Worked examples
See the method in practice
Silver chloride
For AgCl(s) ⇌ Ag⁺ + Cl⁻ in pure water, Ksp = s² because both equilibrium ion concentrations equal the molar solubility s.
Calcium fluoride
For CaF₂(s) ⇌ Ca²⁺ + 2F⁻, Ksp = s(2s)² = 4s³ in pure water. Added fluoride lowers the calculated solubility.
Questions
Frequently asked
Why is molar solubility not always the square root of Ksp?
The ion concentrations depend on dissolution coefficients. Only a 1:1 solid in pure water gives Ksp = s².
What is the common-ion effect?
An ion already present shifts dissolution equilibrium toward the solid, usually reducing molar solubility.
Can I use Ksp to predict precipitation directly?
Compare the ion product Qsp with Ksp: Qsp greater than Ksp indicates supersaturation and possible precipitation. This calculator focuses on saturated dissolution states.
Sources & review
Equations and examples are checked against the references below. Results are educational and should be independently verified for safety-critical work.
OpenStax Chemistry — Precipitation and DissolutionWritten by the STEM Hub editorial team · Reviewed August 11, 2026 · Review methodology