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Engineering ToolBox > Changing Air Conditions by Heating, Cooling, Mixing, Humidifying or Dehumidifying the Air
The most common changes of air conditions are
The process of heating of air can be expressed in the Mollier diagram as:

Heating of air moves the air condition from A to B along a constant specific humidity - x - line. The supplied heat - dH - can be read in the diagram as shown.
The heating process of air expressed can also be expressed in the psychrometric chart as:

When mixing air of a condition A and air of a condition C, the mixing point will be on the straight line in point B.
The position of point B depends on air volume A and air volume C.

The heat balance for the mix can be expressed as:
mA hA + mC hC = (mA + mC) hB (1)
where
m = mass of the air
h = heat of the air
The moisture balance for the mix can be expressed as:
mA xA + mC xC = (mA + mC) xB (1)
where
x = water content in the air
When hot air is mixed with cold air the result may be fog. When the mixing point is below the saturation line, parts of the moisture in the air condensates as small droplets floating in the air. The fog process can be expressed in the Mollier diagram as:

With a cold surface in the air, the air may be cooled and even dehumidified.
If the temperature on the cooling surface is higher than the dew point temperature - tDP, the air cools along the constant specific humidity - x - line.
The cooling process of air can be expressed in the Mollier diagram as:

It the temperature on the cold surface is lower than the dew point temperature - tDP, the air cools in the direction of a point C as shown below.

Vapor in the air condensates on the surface, and the the amount of water condensated will be xA - xB.
If water is added to air without any heat supply, the air condition will change adiabatic along a constant enthalpy line - h. The dry temperature of the air will decrease as shown in the Mollier diagram below.

If steam is added to the air, the air condition will change along a constant dh/dx line as shown above.