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HEATINC VENTILATINC AIR CONDITIONING CUIDE 1941
Temp
F
t
-96 -64 -32
0
Table 2. Specific Volume of Dry Air3 at 29.921 In. Hg
Cu Ft per Lb 1 fa 1
9.1488
9.9597 10.7699 11.5796
D I
|
Temp
F
t
32 64 96 128
|Cu Ft per d Lb
12.3888
13.1977 14.0063 14.8147
j I
I
Temp
F
t
160 192 224 256
Cu Ft per Lb Pa
15.6229 16.4310 17.2389 19.0467
Prepared by John A. Goff.
great accuracy, the effect of intermolecular forces may be ignored and Equation 2 simplified to
pv = BT
(1)
Example 8. Calculate an approximate value for the specific volume of drv air at 64 F, 29.921 in. Hg.
0 7 ,-
53.351 X 523.70
.
Solutton. v = 29-92i x q.49115 X 144 = 13'200 cu ft per Pund-
Note: This answer may be compared with the value in Table 2. The difference is due to intermolecular forces. It should not be concluded, however, that because the effect of intermolecular forces on the volume is so small these forces can be ignored entirely.
The relationship of Equation 1 expresses certain familiar laws approxi mately true for gases at not too high pressures. Thus, with temperature constant, the volume of a given weight of gas is inversely proportional to its absolute pressure is a statement of Boyle's Law. If m denotes the specific volume at absolute pressure Pi, then at the same temperature, the specific volume Vt at absolute pressure pt is approximately,
*= 1,1 ()
Also, with pressure constant the volume of a given weight of gas is directly proportional to its absolute temperature is a statement of Charles' Law. If t>i denotes the specific volume at absolute temperature Tx, then at the same pressure, the specific volume Vi at absolute temperature Ti is approxi mately,
Absolute Temperature
For the range 0 to 660 C, the standard temperature scale is the Inter national Centigrade Scale, namely, the readings of a platinum resistance thermometer standardized at the ice-point (0 C), the steam-point (100 C) and the sulphur-point (444.60 C). The corresponding Fahrenheit scale t used in scientific work is derived from the International Centigrade Scale by means of the relation,
t = 1.8 (Int. Cent. Temp.) + 32
(3) -
Temperatures on the absolute Fahrenheit scale are then obtained by adding 459.70 according to the equation
T = l + 459.70 4
(4)
CHAPTER 1. THERMODYNAMICS OF AIR AND WATER MIXTURES
Absolute temperatures computed from Equations 3 and 4 are practically identical with the fundamental thermodynamic temperatures to which the zero-pressure values of the product pv for gases are proportional in accordance with Equation 2.
Specific Enthalpy
Most air conditioning processes are of the steady-flow type. In steady flow the energy ^onvected with the fluid crossing a given section is the
sum of (a) kinetic energy due to velocity, (b) gravitational energy due to elevation, (c) enthalpy due to the condition of temperature, pressure and
composition at a given section. It is clear, therefore, that in order to apply the Law of Conservation of Energy to steady-flow processes,
information regarding the enthalpy is needed.
Recent developments in quantum mechanics have made it possible to calculate the zero-pressure specific enthalpy of a gas from spectroscopic
measurements, and with a degree of accuracy exceeding that with which
this property can be inferred from direct calorimetric measurements.
Available data for each gas listed in Table 1 have been assembled and
critically examined; and from them have been calculated best values
for the specific enthalpy of dry air at zero pressure. These are listed in Table 3. The unit of energy is the Btu which is related to the foot
pound as follows:
1 Btu = 778.26 ft-lb
(5)
In Table 3 are also listed values of mean zero-pressure specific heat for the range 0 to t F. This is simply the increase of specific enthalpy from 0 to l F, divided by the increase of temperature or, with 0 F as the reference point, by the temperature itself. The numerical values indicate that a rounded figure of 0.24 Btu per pound can be used in ordinary calculations.
Applying well known identical relations of thermodynamics to Equation 2, the following expression for specific enthalpy, valid at not too high pressures, is obtained
-+
(6)
where h denotes specific enthalpy at zero pressure. This equation emphasizes that the effect of pressure on specific enthalpy is not so much due to the second virial coefficient A itself as to its variation with tempera ture. In other words, the pressure effect may be much more important than the corresponding effect on specific volume. Values of the specific
Table 3. Specific Enthalpy of Dry Air at Zero Pressure3
Temp
F
t
Specific Enthalpy Btu per Lb
*:
MRan Specific
Heat K)o
-96 -64 -32
0
-22.839 -15.186
-7.529
-0.131
0.2393
0.2393 0.2394 0.2394
Temp
F
t
Specific Enthalpy Btu per Lb
<
Mean Specific
Heat
K)l
32 7.796 0.2395
64 15.466 0.2396
96 23.145 0.2397128 30.831 0.2398
Temp
F
t
Specific Enthalpy Btu per Lb
Mean Specific
Heat
Klo
160 38.529 0.2400 192 46.238 0.2401 224 53.962 0.2403 256 61.702 0.2405
Prepared by John A. Goff from published data computed from spectroscopic measurements.
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