Air - Maximum Moisture Carrying Capacity

Maximum water content in humid air vs. temperature. Shows how the maximum moisture content possible in air at saturation varies with temperature.

Temperature (°C)Temperature (°F)Max Water Content (g/m³)Max Water Content (lb/ft³)
-25-130.640.04
-20-41.050.066
-1551.580.099
-10142.310.14
-5233.370.21
0324.890.31
5416.820.43
10509.390.59
155912.80.8
206817.31.07
308630.41.9
4010451.13.2
50122835.2
601401308.1
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Results

Moisture Carrying Capacity Increase-- %

Key Insights

  • Temperature Effect: The maximum moisture content in air increases significantly with temperature
  • Exponential Relationship: The relationship is not linear; small temperature increases at lower temperatures have less effect than at higher temperatures
  • Practical Application: This explains why heated air is far more effective than cold air in drying processes
  • Example: Air heated from 20°C to 50°C increases its moisture carrying capacity by approximately 380%

Note

  • Values are given in g/m³ (grams per cubic meter), which equals 10⁻³ kg/m³
  • Alternative unit: lb/ft³ (pounds per cubic foot)
Air - Maximum Moisture Carrying Capacity | MEPKit Engineering Tools | MEPKit