Consider the classical adiabatic saturation process

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Consider the classical adiabatic saturation process in which a stream of is mixed adiabatically and isobarically (T1)with a stream of liquid water in order (T2) to become a saturated air +water vapor mixture . Show that the adiabatic saturation temperature T3 is a function of the of the inlet humidity ratio.

Reference no: EM13713273

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