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Air handling, in AHU or in drying operations, requires the heating of humid air. It is then important to be able to calculate the energy required to bring air from a temperature \(T_1\) to a temperature \(T_2\).
Humid air is heated up, without change of state of the water, at constant specific humidity, but not at constant relative humidity, as the relative humidity decreases if the temperature increases.
The 1st step is to define the enthalpy of humid air:
With:
In practice, at 273.15 K (0°C):
Considering a temperature \(T_A\) (starting temperature) and a temperature \(T_B\) (end temperature), the energy required to heat up humid air, at constant absolute humidity is then:
Example of humid air heating calculation: Step by Step calculation
Air at 25°C and 50% RH is to be heated up until 35°C, what is the energy required?
STEP 1: determine the absolute humidity of the air
It can be determined on a Mollier diagram or psychrometric chart: the absolute humidity is ~0.010 kg water / kg of dry air.
STEP 2: calculate the difference in enthalpy in between states
\[ \Delta H = (1005 + 1884 \cdot 0.010) \cdot (35 - 25) = 10238 \text{ J/kg of dry air} \]
It is possible to calculate the energy required to heat up humid air by using a psychrometric chart, which illustrates the thermodynamic properties of moist air for drying applications. Knowing the starting conditions, it is possible to determine the final conditions by moving along the lines of constant specific humidity.
The value obtained graphically is close to the calculated value; the difference comes from the chart resolution and reading precision.
Q: Does absolute humidity change during heating?
A: No, unless water is added or removed, \(\omega\) remains constant during sensible heating.
Q: Why does Relative Humidity drop?
A: Warmer air has a higher capacity to hold water vapor (higher saturation pressure), so the same amount of water represents a smaller percentage of the maximum possible.