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A saturated solution contains the maximum concentration of dissolved solute at equilibrium, where dissolution and recrystallization rates are equal. An unsaturated solution has less solute than needed to reach saturation and can dissolve more solute. The concentration limit of a saturated solution is determined by the relative strengths of solute-solute, solute-solvent, and solvent-solvent attractive forces.

Heating a saturated solution increases its capacity to dissolve more solute. When the heated solution is cooled slowly and left undisturbed, it can form a supersaturated solution, which holds more solute than the equilibrium amount. Supersaturated solutions are unstable and the excess solute often precipitates out.

As a solid solute dissolves, the concentration of dissolved molecules increases, raising the chance of recrystallization. Initially, dissolution occurs faster than recrystallization. When the rate of dissolution equals the rate of recrystallization, dynamic equilibrium is established, creating a saturated solution where both processes continue at equal rates.

A supersaturated solution contains more dissolved solute than the equilibrium amount, making it a nonequilibrium state. These solutions are unstable because the excess solute tends to precipitate. Adding a small amount of solute or disturbing the solution provides a template for crystallization, allowing the excess solute to rearrange and form crystals.

Solubility is determined primarily by the relative strengths of solute-solute, solute-solvent, and solvent-solvent attractive forces. These intermolecular forces govern the maximum concentration achievable when the dissolution process reaches equilibrium. The solubility represents the limit at which no more solute can dissolve under given conditions.

As dissolved solute concentration increases, the probability of solute molecules colliding and recombining to form crystals increases. Higher concentration means more solute particles in solution, raising collision frequency. This increased recrystallization rate eventually matches the dissolution rate, establishing the dynamic equilibrium characteristic of a saturated solution.

Adding a seed crystal to a supersaturated solution provides a template for crystallization. The excess solute rearranges around the crystalline solid and forms new crystals. Once the crystals settle, the solution returns to saturation and dynamic equilibrium is reestablished, stabilizing the solution.