science behind the humification processes which refers mainly to the systematized knowledge of the properties of air and water
Psychrometry
Psychrometry
The mass of vapor carried by a unit mass of vapor-free gas
Saturation/Humidity
Saturation Equation
S= (M_a/M_b) * p_a/(P-p_a)
Where,
* PA – the partial pressure of the vapor in the mixture
* P - the total pressure (usually atmospheric unless otherwise specified)
* MA, MB – the molecular weights of components A and B, respectively
A gas in which the vapor is in equilibrium with the liquid at the gas temperature and pressure
Saturated Gas
—– temp, —– capacity to hold vapor
higher, higher
—– pressure, —- capacity for vapor
higher, lesser
in this condition, there would be higher tendency for vapor to condense
at this point the partial pressure of that vapor in the gas mixture is equal to the saturation pressure of that vapor at a particular pressure and temperature.
Saturated Gas
A gas in which the water vapor is in equilibrium with the liquid water at the gas temperature and pressure.
Saturated Air
Relative Saturation, RS
Relative Saturation formula
%RS = (Pa/P*sat) x 100%
Saturated Gas Formula
Psat*=pa
Ratio of the actual saturation S (actual humidity, H) to the maximum saturation Smax (saturation humidity, HS) at the gas temperature and pressure.
Percentage Saturation
%S =
%S=S/S_max ×100%
=(pa/(P-pa ))/((Psat)/(P-Psat ))×100%
=%RS (P-Psat)/(P-pa )
Dew Point
Dew point
Dew Point Formula
ln(P_sat^* )=A-B/(C+T)
Dew pt for air-water system
ln〖P_sat^* (mmHg)〗=18.3036-3816.44/(T(K)-46.13)
Humid volume (vH)
υ_H
υ_H=(RT/P) (1/M_B +S/M_A )
B
gas
A
vapor
Humid heat (Cs)
Humid Heat SI Formula
C_s=1.005+1.88H kJ/(kg dry air ∙K) (SI)