November 6, 2025
Condensation is the transition of water from a gaseous state (water vapor) to a liquid state (drop of water).
This physical phenomenon is omnipresent in our environment: it occurs in clouds as well as on a cold wall, a window, or even the ceiling of a storage container.
The air always contains a certain amount of water vapor.
When this quantity exceeds a certain threshold, water molecules agglomerate to form small clusters called nuclei: this is the start of the nucleation process.
Two types of nucleation exist:
👉 Example:

Condensation occurs when Relative humidity of the air reaches 100%, in other words when the air can no longer contain more water vapor.
Two situations can then trigger this phenomenon:
This is what happens, for example, when hot, humid air comes into contact with a cold surface: the dew point temperature is reached, and small water droplets form.
In storage containers or rooms with poor ventilation, condensation can quickly become a humidity problem.
When humid air touches cold walls or ceilings, water settles in the form of drops.
Over time, this promotes:
💡 Good control of temperature and relative humidity makes it possible to effectively limit condensation.
Condensation is the transformation of water vapor into liquid water when the air becomes too humid or cools. It occurs everywhere: in nature, but also in enclosed environments such as buildings or containers. Understanding this phenomenon is essential to prevent humidity problems and protect sensitive surfaces.
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