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64                                                  CHAPTER 4 PHYSICAL FUNDAMENTALS
                  Lydersen, A. L., Mass Transfer in Engineering Practice. Wiley, New York, 1983.
                  Nyvlt, J., Industrial Crystallisation from Solutions. Butterworths, London 1971.
                  Oliver, E. D., Diffusional Separation Processes: Theory, Design and Evaluation. Wiley, New York, 1966.
                  Reid, R. C., Prausnitz, J. M., and Sherwood, T. K., The Properties of Gases and Liquids.
                     McGraw-Hill, New York, 1977.
                  Sherwood, T. K., Pigford, R. L., and Wilke, C. R., Mass Transfer. McGraw-Hill, New York, 1975.
                  Sissom, L. E., and Pitts, D. R., Elements of Transport Phenomena. McGraw-Hill New York, 1972.
                  Treybal, R. E., Mass Transfer Operations. McGraw-Hill, New York, 1968.



        4.2 STATE VALUES OF HUMID AIR; MOLLIER DIAGRAMS AND THEIR APPLICATIONS

        4.2.1 Properties of Air and Other Gases
                  The analysis of dry atmospheric air varies with location, altitude, time of year,
                  and other factors. Table 4.4 gives the molecular weights of the constituents
                  and the volumetric and gravimetric analyses.
                     For general engineering work for altitudes up to 1500 m it is sufficiently
                  accurate to use the following:




                  The above values are based on the assumption that argon is combined with n
                  trogen, adjusting the molecular weight to 28.16. Other gases present in the atmc
                  sphere air are normally ignored, as these represent less than 0.003% {by volumi
                  27.99 ppm). Table 4.5 provides some basic information on these trace gases.
                     The gases also have other constituents mixed with them, typical ones beinj
                  dusts, pollens, bacteria, viruses, mold spores, smoke particles, and the produc
                  of industrial activity such as SO 2, H 2, and S. Volcanic activity also adds variou
                  gases and dusts to the atmosphere.


        4.2.2 Fundamentals
                  Air is seldom dry; it normally contains varying amounts of moisture. Humid a;
                  is a mixture of dry air and water vapor. The term dry air denotes the mixture <
                  all gases present in air (nitrogen, oxygen, carbon monoxide, and inert gases), e>
                  cept water vapor.

                  TABLE 4.4 Analysis of Air at Sea Level

                                                           Volumetric  Gravimetric
                  Constituent  Symbol   Molecular weight (M)  analysis %  analysis %

                  Nitrogen     N 2      28.016             78.09      75.55
                  Oxygen                32.00              20.95      23.13
                               0 2
                  Argon        Ar       39.944             0.93       1.27
                  Carbon dioxide  CO 2  44.01              0.03       0.05
                  Total                                    100        100
                     Source: R.B. Keey, Drying Principles and Practice, 1972
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