Water exists in three forms: gaseous (steam), liquid, or solid (ice). In the ambient air, it is present in the form of water vapor, at varying concentrations. We then talk about Humidity in the air, a central concept in many fields: construction, meteorology, well-being, etc.
When the vapour concentration reaches a maximum threshold (called Saturation point), it is transformed into liquid water. That's what we call the condensing. This phenomenon is the cause of many humidity problems in buildings.
The Relative humidity is expressed as a percentage: it indicates the quantity of water vapor present in the air compared to the maximum quantity that the air can contain at a given temperature.
The absolute humidity, on the other hand, measures the real quantity of water vapor (in grams per m³). These two indicators are complementary and make it possible to better understand the humidity level in an environment.
Example: at 20°C, if the air contains 10 g/m³ of water vapor and can contain a maximum of 20 g/m³, the relative humidity is 50%.
When the water vapor condenses, it forms liquid water on cold surfaces: windows, walls, ceilings. This may result in:
This phenomenon is often referred to as “humidity” in everyday speech.
Humidity can be unseen but have important consequences. Here are some tools to measure it:
In case of doubt, it is recommended to measure the humidity level to avoid structural damage.
To prevent the effects of humidity, several solutions exist:
In case of recurrent condensation, it may be useful to calculate the dew point to better anticipate risks.
There are solutions for control humidity effectively.