Supercooling is the process of cooling a liquid below its freezing point without it solidifying. This can occur when the liquid is pure and free from any impurities or when it is cooled very slowly, allowing it to remain in a liquid state at temperatures below its freezing point.
When a liquid is cooled below its freezing point, it may not immediately solidify because there are no nucleation sites for crystallization to begin. As a result, the liquid remains in a supercooled state until it is disturbed or a nucleation site is introduced, causing it to rapidly solidify.
Supercooling can be observed in nature, such as when water droplets in clouds remain in a supercooled state until they come into contact with a nucleation site, causing them to freeze and fall as snow or ice pellets.
When studying supercooling, consider the following key points: