Difficulty: Medium
Correct Answer: wet-bulb temperature
Explanation:
Introduction / Context:
Adiabatic humidification and cooling are central to air–water psychrometrics, evaporative coolers, and packed-tower humidifiers. When unsaturated air contacts liquid water in an adiabatic device at essentially constant pressure, the air warms or cools and its humidity changes in a coupled way along lines closely tied to the wet-bulb temperature.
Given Data / Assumptions:
Concept / Approach:
The wet-bulb temperature (T_wb) is the temperature a water-wetted thermometer reaches due to evaporative cooling under adiabatic conditions. In adiabatic saturation of air with water at constant pressure, the air state moves along a path of nearly constant T_wb: the reduction in sensible heat balances the gain in latent heat. The dry-bulb temperature (T_db) decreases as evaporation proceeds, while absolute humidity increases until an approach to the adiabatic saturation state is reached.
Step-by-Step Solution:
Verification / Alternative check:
On a standard psychrometric chart, adiabatic humidification trajectories are nearly lines of constant wet-bulb temperature, confirming the invariance of T_wb, while T_db shifts downward and humidity ratio increases toward saturation at the adiabatic saturation temperature.
Why Other Options Are Wrong:
Common Pitfalls:
Confusing isothermal humidification (contact with a very large water reservoir at fixed temperature) with adiabatic humidification; in the latter, the key invariant is the wet-bulb temperature, not dry-bulb or dew point.
Final Answer:
wet-bulb temperature
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