GAS MIXTURES AND PSYCHROMETRICS:SPECIFIC AND RELATIVE HUMIDITY OF AIR

SPECIFIC AND RELATIVE HUMIDITY OF AIR

The amount of water vapor in the air can be specified in various ways. Probably the most logical way is to specify directly the mass of water vapor present in a unit mass of dry air. This is called absolute or specific humidity (also called humidity ratio) and is denoted by :

GAS MIXTURES AND PSYCHROMETRICS-0027

where P is the total pressure.

Consider 1 kg of dry air. By definition, dry air contains no water vapor, and thus its specific humidity is zero. Now let us add some water vapor to this dry air. The specific humidity will increase. As more vapor or moisture is added, the specific humidity will keep increasing until the air can hold no more moisture. At this point, the air is said to be saturated with moisture, and it is called saturated air. Any moisture introduced into saturated air will condense. The amount of water vapor in saturated air at a specified temperature and pressure can be determined from Eq. 9–29 by replacing Pυ by Pg, the saturation pressure of water at that temperature (Fig. 9–15).

The amount of moisture in the air has a definite effect on how comfortable we feel in an environment. However, the comfort level depends more on the amount of moisture the air holds (mυ) relative to the maximum amount of moisture the air can hold at the same temperature (mg). The ratio of these two quantities is called the relative humidity f (Fig. 9–16)

GAS MIXTURES AND PSYCHROMETRICS-0028GAS MIXTURES AND PSYCHROMETRICS-0029

The relative humidity ranges from 0 for dry air to 1 for saturated air. Note that the amount of moisture air can hold depends on its temperature. Therefore, the relative humidity of air changes with temperature even when its specific humidity remains constant.

Atmospheric air is a mixture of dry air and water vapor, and thus the enthalpy of air is expressed in terms of the enthalpies of the dry air and the water vapor. In most practical applications, the amount of dry air in the air–water-vapor mixture remains constant, but the amount of water vapor changes. Therefore, the enthalpy of atmospheric air is expressed per unit mass of dry air instead of per unit mass of the air–water-vapor mixture.

The total enthalpy (an extensive property) of atmospheric air is the sum of the enthalpies of dry air and the water vapor:

GAS MIXTURES AND PSYCHROMETRICS-0030

Also note that the ordinary temperature of atmospheric air is frequently referred to as the dry-bulb temperature to differentiate it from other forms of temperatures that shall be discussed.

GAS MIXTURES AND PSYCHROMETRICS-0031GAS MIXTURES AND PSYCHROMETRICS-0032GAS MIXTURES AND PSYCHROMETRICS-0033

Related posts:

Case studies:VSD installation and commissioning Borehole pump
Engineering Data:Graphical symbols for pneumatic systems and components
Design procedures:The use of test data in system design
Material property influences:Fly ash
ROUBLESHOOTING PNEUMA TIC CIRCUITS:TROUBLESHOOTING PNEUMATIC CIRCUITS
RESERVOIRS, STRAINERS, FILTERS, AND ACCUMULATORS:Full-Flow Filters.
HYDRAULIC FLUIDS:Control of Contamination
HYDRAULIC PUMPS:Gear Pumps and External Gear Pumps
CONTROL VALVES:Rotary Spool Four- Way Valves
Air Compressors, Air Treatment and Pressure Regulation:dynamic compressors
Actuators:mounting arrangements
BASICCONCEPTS OF THE RMODYNAMICS:ENERGY AND ENVIRONMENT
POWER AND REFRIGER A TION CYCLES:ACTUAL VAPOR-COMPRESSION REFRIGERATION CYCLE
SUMMARY OF GAS MIXTURES AND PSYCHROMETRICS
FORCED CONVECTION:FLOW ACROSS CYLINDERS AND SPHERES

Leave a comment

Your email address will not be published. Required fields are marked *