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ZEOLITE TYPESA,X,AND Y  161

            7.1.3. Examples of Molecular Sieving
            Separation and purification can be accomplished by molecular sieving, that is, by
            size exclusion. An example is drying or dehydration of gases or alcohols by 3A
            zeolite, which excludes all hydrocarbons, O 2 ,N 2 , and essentially all permanent
            gases except ammonia. It is particularly useful for drying gases under reactive
            conditions. Isotherms of water on 3A are given in Figure 7.2, which also shows
            the approximate minimum condition for dehydration of zeolites. Another example
            is the large-scale commercial use of 5A zeolite in processes for the separation
            of normal paraffins from branched-chain (e.g., iso-) paraffins and cyclic hydro-
            carbons, and the Union Carbide isoSiv process is a prime example (Yang, 1987).
            The free aperture size of 5A zeolite is 4.3 ˚ A, which admits only linear paraffins
            but not branched-chain paraffins and cyclic hydrocarbons. The branched-chain
            paraffins have higher octane numbers than their n-paraffin homologs as a gaso-
            line product. It is known that temperature has a sizable effect on molecular
            sieving. The aperture size decreases with temperature. Thus, for some molecules,
            molecular sieving occurs only below certain temperatures. The temperature effect
            may be illustrated by the sieving of N 2 /O 2 with 4A zeolite (Breck, 1974). The
            kinetic diameter of N 2 is approximately 0.2 ˚ A larger than O 2 . At temperatures
                      ◦
            below −100 C, N 2 becomes essentially excluded, while Ar becomes excluded at
                       ◦
            below −150 C. A schematic is given in Figure 7.3 that shows the relationship

                 24


                 20

                                       −20 °C  25°    60°
               Capacity, lbs H 2 O/100 lbs, 3Å  12  40°  80°
                 16
                                        0°






                  8

                                                        100 °C
                  4



                  0
                  10 −5  10 −4  10 −3  10 −2  10 −1  1.0    10    100    1000
                                    H O Partial pressure, mm Hg
                                     2
            Figure 7.2. Equilibrium isotherms of water on 3A zeolite (taken from undated brochure of
            Grace Davison Division).
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