Heating and humidification of air: The final relative humidity of the leaving air (after adding heat and moisture) is generally:

Difficulty: Medium

Correct Answer: can be lower or higher than that of the entering air

Explanation:


Introduction / Context:
Heating and humidification is common in winter air-conditioning, where dry cold air is warmed and moisture is added. Predicting the final relative humidity (RH) requires understanding of how both dry-bulb temperature and absolute moisture content change simultaneously.



Given Data / Assumptions:

  • Humidifier adds water vapour (steam or evaporative), while a heater raises dry-bulb temperature.
  • Process may be simultaneous (e.g., spray washer with heating) or sequential (heater then humidifier).
  • Pressure remains near constant.


Concept / Approach:
RH is defined as p_w / p_ws(T). Adding moisture increases p_w; heating increases p_ws(T). Depending on the relative magnitudes of these changes, RH can rise or fall. On a psychrometric chart, heating shifts right; humidification shifts up; combined, the path can approach or recede from the saturation curve depending on rates of heat and moisture addition.



Step-by-Step Solution:

Consider strong heating with little humidification: T increases substantially, p_ws(T) rises, p_w rises only slightly → RH may decrease.Consider modest heating with strong humidification: p_w increases markedly while T rises a little → RH may increase.General outcome: RH can be higher or lower than at inlet; it is not fixed.Exact result requires mass and energy balances across the equipment.


Verification / Alternative check:
Plotting initial and final states on the chart confirms that different heater/humidifier capacities produce different RH results for the same inlet state.



Why Other Options Are Wrong:

  • Always higher / always lower: Over-generalizations; outcome depends on process intensity.
  • Always 100%: Only occurs if the process reaches saturation, which is not guaranteed.
  • Always unchanged: RH is sensitive to both T and moisture changes.


Common Pitfalls:
Assuming RH tracks moisture addition alone; ignoring the strong influence of temperature on saturation pressure.



Final Answer:
can be lower or higher than that of the entering air

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