Solubility Product Calculator — calculate solubility product using standard chemistry formulas. Worked example with units.
The solubility product, Ksp, describes the equilibrium between a sparingly soluble ionic solid and its dissolved ions. For a simple 1:1 salt, the ion concentrations at saturation determine Ksp and allow an approximate molar solubility to be estimated. The result is intended as a transparent educational estimate: keep the substance, temperature, pressure, concentration basis, and unit convention beside any number you reuse.
These calculations are useful for chemistry study, laboratory planning, process troubleshooting, and comparing scenarios. They are not a substitute for a measured phase diagram, validated equilibrium model, certified method, or engineering design. Compare Common Ion Calculator and Molarity Calculator when a problem crosses between gas, phase-change, or solution behaviour.
Unit discipline matters as much as the algebra. Pressure may be reported in pascals, kilopascals, atmospheres, or millimetres of mercury; concentration may be molar, molal, or expressed as a mole fraction; and an equilibrium constant may carry a convention that differs between references. Convert before substituting, retain a few guard digits during intermediate steps, and round only the displayed result.
Temperature and composition are part of the definition of the problem, not optional notes. A vapour pressure at 20 °C cannot be transferred unchanged to 60 °C, and a solvent mass cannot be replaced by solution volume in a molality calculation. For equilibrium or separation work, state whether the mixture is dilute, ideal, binary, saturated, or at steady state so a reader can judge whether the model is appropriate carefully.
When comparing two scenarios, change one assumption at a time where possible. That simple practice makes it easier to explain whether a difference came from concentration, temperature, pressure, solvent choice, or an equilibrium constant, and it gives a useful audit trail for later laboratory work.
For MX ⇌ M⁺ + X⁻, Ksp = [M⁺][X⁻]; in pure water s = √Ksp, while a common ion gives approximately s = Ksp ÷ [common ion].
The formula is deliberately shown next to the inputs so that units can be audited. A result with a plausible number can still be wrong if a mass fraction was entered as a mole fraction, Celsius was used as kelvin, or a concentration was based on solution volume instead of solvent mass.
The result applies the 1:1 salt model and treats activities as concentrations. Different stoichiometries require the correct powers in the equilibrium expression, and pH, complexation, ionic strength, and temperature can all change the apparent solubility.
Use the result to compare like-for-like scenarios rather than presenting extra decimal places as extra certainty. If the calculation is near a phase boundary, saturation limit, precipitation threshold, or material-balance constraint, small changes in temperature and composition can matter more than rounding.
A good validation check asks whether the direction of change makes chemical sense. Adding non-volatile solute should lower solvent vapour pressure and freezing temperature, while it should raise boiling temperature; increasing reflux should increase internal liquid flow; and a material balance should conserve both total feed and the tracked component. These checks catch swapped fields and sign errors before they reach a lab notebook or process decision.
This is an educational chemistry calculator. Chemical handling, pressurised equipment, heating, distillation, solvent selection, product release, and laboratory or process safety require qualified supervision, current safety data, validated methods, and applicable local regulations.