Document 6BzrQjBm1xqKNk9awQezRG9pm

American Society of Heating and Ventilating Engineers Guide, 1937 W = the weight of the gas, pounds. R = a constant depending on the nature of the gas. is 53134. T = the absolute temperature, degrees Fahrenheit. The average value of R for air This is the characteristic equation for a perfect gas, and while no gases are perfect in this sense, they conform so nearly that Equation 3 will apply to most engineering computations. HUMIDITY Humidity is the water vapor mixed with dry air in the atmosphere. Absolute humidity has a multiplicity of meanings, but usually the term refers to the weight of water vapor per unit volume of space occupied, expressed in grains or pounds per cubic foot. With this meaning, absolute humidity is nothing but the actual density of the water vapor in the mixture and might better be so called. A study of Keenan's Steam Tables* indicates that water vapor, either saturated or super-heated, at partial pressures lower than 4 in. pf mercury may be treated as a gas with a gas constant R of 1.21 in the characteristic equation of the gas pV,= wR (t + 460). Within such limits, the density (d) of water vapor is d = ~ = Y~21 (T+ 460) fPunds f>er cubic foot) (4a) where = (grains per cubic foot) ' (4b) e = actual partial pressure of vapor, inches of mercury. t -- dry-bulb temperature, degrees Fahrenheit. Specific Humidity It simplifies many problems which deal with mixtures of dry air and water vapor to express the weight or the mass of the vapor in terms of the weight or the mass of dry air. If the'weight of the water vapor.in a mixture be divided by the weight of the dry air, and the weight of dry air be made unity, we have an expression of the weight of water vapor carried by a unit weight of dry air. This relation has no generally accepted name. It has been variously called: mixing ratio, proportionate humidity, mass or density ratio, absolute humidity, and specific humidity. Of all these terms specific humidity is the most suggestive of the meaning which it is desired to express and it has found considerable use in this sense even though it is defined in International Critical Tables as the ratio of the mass of vapor to the total mass. It will be understood here that specific humidity refers to the weight of water vapor carried by one pound of dry air. / The gas constant for dry air, when the partial pressure of the air. is expressed in inches of Hg, is 0.753; so that the specific humidity, if represented by W, is --- ------------------- c Published by American Society of Mechanical Engineers, see abstract in Table 8- ,' S Chapter 1--Air, Water and Steam W ~ 1.21 (I + 460) : 0.753 (I + 460) = 0.622 (pounds) (5a) = 4354 (grains) . where e = actual partial pressure of vapor, inches of mercury. B = total pressure of mixture (barometric pressure), inches of mercury. (5b) - Relative Humidity Relative humidity (<!>) is either the ratio of the actual partial pressure, e, of the water vapor in the air to the saturation pressure, et, at the drybulb temperature, or the ratio of the actual density, d, of the vapor to the density of saturated vapor, dt, at the dry-bulb temperature. That is: The relative humidity of a given mixture at a.given temperature is not the same as the specific humidity, W, of the mixture divided by the specific humidity, Wt, of saturated vapor at the same temperature, for from Equations 5a and 6 wt- -622 (fT^hi) -0622 fe) = <7> The specific humidity of an unsaturated air-vapor mixture cannot, therefore, be accurately found by multiplying the specific humidity of saturated vapor by its relative humidity; although the error is usually small especially when the relative humidity is high. With a relative humidity of 100 per cent, the dry-bulb, wet-bulb, and dew-point temperatures are equal. With a relative humidity less than 100 per cent, the dry-bulb exceeds the wet-bulb, and the wet-bulb exceeds the dew-point temperature. RELATION OF DEW POINT TO RELATIVE HUMIDITY A peculiar relationship exists between the dew point and the relative humidity and thfs is found most useful in air conditioning .work. This relationship is, that for a fixed relative humidity there is. substantially a constant difference between- the dew point and the dry-bulb temperature over a considerable temperature range. Table 5, giving the dry-bulb and dew-point temperatures and the dew-point differentials for 50 per cent relative humidity, illustrates this relationship clearly. : Table 5. Temperatures for 50 Per Cent Relative Humidity Dry-bulb temperature.............. -- -............... 65.0 Dew-point temperature.-............................-- 45.8 Difference between dew-point and drybulb temperature..................................... 19.2 70.0 50.5 19.5 75.0 80.0 85.0 90.0 55.25 59.75 64.25 68.75 19.75 20.25 20.75 21.25 9