Humid Air   

Humid Air

Humid air always contains dry air and steam. Once the saturation is exceeded water droplets and ice occur. The calculations presented are limited to relative saturation up to 100%.
In good approximation dry air and steam can be regarded as ideal gases. The calculations are valid for humid air at ambient pressure and temperatures between 5 - 70 [°C].
The dew point of a humid air is the temperature at which its realive humidity reaches 100%.
Relative humidity equals 100%, if the partial pressure of steam equals its saturation pressure.

Theory Humid Air

Feuchte Luft
C. Meyer
humid air
C. Meyer

You like that explanation? Feel invited to contribute a translation to any other language. If you like your name will be mentioned in the table and the document. Contact us: About

Home | Calculation Programs | Download | Upload | Physical properties and Theory | Literature | Links | Converter | Terms of use | About