Difficulty: Easy
Correct Answer: p_v = φ * p_ws(T) (relative humidity × saturation vapour pressure at the same temperature)
Explanation:
Introduction / Context:In air-conditioning and refrigeration engineering, we frequently need the partial pressure of water vapour in moist air. This quantity underpins calculations of humidity ratio, dew-point temperature, and wet-bulb temperature and is central to psychrometric analysis.
Given Data / Assumptions:
Concept / Approach:Dalton’s law states that the total pressure equals the sum of the partial pressures of the constituents. For water vapour in moist air, the driving concept is that relative humidity is the ratio of actual water vapour partial pressure to the saturation vapour pressure at the same temperature, i.e., φ = p_v / p_ws(T). Rearranging immediately gives p_v.
Step-by-Step Solution:
Start from the definition: φ = p_v / p_ws(T).Rearrange to isolate p_v: p_v = φ * p_ws(T).Use tables or equations (e.g., Antoine) to find p_ws(T) at the air temperature, then multiply by the measured or specified relative humidity φ.With p_v known, other properties follow: w = 0.622 * p_v / (p_atm − p_v), and dew point via inversion of p_ws(T_dp) = p_v.Verification / Alternative check:Cross-check by computing humidity ratio from the obtained p_v and then reconstructing p_v = p_atm * w / (0.622 + w); both routes should match within rounding error.
Why Other Options Are Wrong:
Common Pitfalls:Confusing saturation vapour pressure at dry-bulb vs. wet-bulb; p_ws must be evaluated at the relevant temperature indicated in φ's definition (usually the same temperature at which φ is stated).
Final Answer:p_v = φ * p_ws(T)
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