Percentage humidity φ=y/y
s and relative humidity ψ=H/H
s have both been very popularized for us. But their physical meanings are limited to the lower temperature range than the temperature at which the saturated vapor pressure is equal to the total pressure of the system. For example, in the case of air-water system at 760mmHg total pressure above 100°C, φ must be given a suspicious value as the quotient of p divided by a greater pressure than 760mmHg which is the total pressure of the system, and therefore it may happen that the value of p is greater than the total pressure 760mmHg. In that case, ψ may become a negative and meaningless value. The fact that the value of H is infinity having no relation to the value of ψ at 100°C, is disagreeable for us.
The authers propose a new definition to represent the humidity % as follows: then
above 100°C and they name ε "Specific humidity, " temporarily.
The advantages obtained by using this specific humidity ε in place of ψ or φ are as follows:
(1) We can represent and treat numerically any condition of humidity % without limitation of temperature range, rationally.
(2) The condition of ε=100% is correspond to ψ=100%, and the replacement of or ψ by in Carrier's type humidity chart brings no obstacle to other relations.
(3) It is possible to convert the value of humidity % between dry basis H and wet basis ε=H/(1+H), on th ordinate H scale of the Carrier's type chart.
Fig. 1 & 3 are the skeleton of such a humidity chart, and Fig. 2 & 4 shows the relation between ε and ψ at various temperatures.
The matter in this report will hold in any other system of gas-vapor mixture.
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