A flow of moist air at 100 kPa, 35C, 40% relative humidity is cooled by adiabatic evaporation

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A flow of moist air at 100 kPa, 35◦C, 40% relative humidity is cooled by adiabatic evaporation of liquid 20◦C water to reach a saturated state. Find the amount of water added per kg dry air and the exit temperature.

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Fundamentals Of Thermodynamics

ISBN: 9781118131992

8th Edition

Authors: Claus Borgnakke, Richard E. Sonntag

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