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.
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)