Supersaturation in gravimetric precipitation is undesirable because it can lead to incomplete precipitation of the desired solid, as excess solute may remain dissolved in the solution. This non-stable state occurs when the concentration of a solute exceeds its solubility at a given temperature, often created by slowly cooling a saturated solution. Without perturbation, precipitation occurs very slowly, and significant crystallization can happen only when a seed crystal is introduced. To mitigate supersaturation, it is recommended to avoid preparing solutions in small volumes and to monitor the solubility of the salt with temperature changes. If solubility increases with temperature, conducting the reaction at lower temperatures or cooling the solution rapidly after adding reactants can help ensure complete precipitation. The discussion also highlights the phenomenon of meta-stable states, where solutions can remain in a liquid state below their freezing point until disturbed, leading to rapid crystallization.