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:
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:
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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