Cooling and dehumidification requirement: To cool and dehumidify a moist air stream across a coil, the coil surface temperature must be set __________ the incoming air’s dew-point temperature.

Difficulty: Easy

Correct Answer: lower than the incoming dew-point temperature

Explanation:


Introduction / Context:
Dehumidification requires condensing moisture from air. The condition for condensation is governed by the dew-point temperature of the incoming stream and the coil surface (or apparatus dew-point).



Given Data / Assumptions:

  • Uniform coil surface temperature.
  • Well-mixed outlet air leaving the coil.
  • Steady operation near atmospheric pressure.


Concept / Approach:
Condensation begins when a surface is at or below the dew-point temperature of the adjacent moist air. For continuous cooling and dehumidification, the coil must be colder than the incoming air’s dew-point so that water vapour condenses on the fins/tubes.



Step-by-Step Solution:

Find the incoming dew-point T_dp from the psychrometric state.Set coil surface temperature T_s < T_dp to initiate condensation.Result: both sensible cooling and latent removal occur.If T_s > T_dp, only sensible cooling occurs and humidity ratio remains unchanged.


Verification / Alternative check:
On the chart, cooling and dehumidification follows a line trending down and left toward the saturation curve, which only happens when the coil is below T_dp.



Why Other Options Are Wrong:
Temperatures between DBT and WBT may not be low enough to reach dew-point; adiabatic saturation temperature is unrelated to coil surface requirement.



Common Pitfalls:
Assuming any cooling causes dehumidification; unless T_s ≤ T_dp, no condensation occurs.



Final Answer:
lower than the incoming dew-point temperature

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