Page 27 - Adsorption Technology & Design, Elsevier (1998)
P. 27

24  Adsorbents


            relatively  inexpensive  and  can  be  used  for  re-refining  edible  and  mineral
            oils, adsorbing toxic chemicals, removing pigments, etc. The cationic forms
            are capable of adsorbing a range of polar molecules and non-polar molecules
            if some water is present.
              The  spaces between the natural  layers can be  enlarged  to form pillared
            interlayered  clays.  This  is  carried  out  by  ion  exchanging  the  charge
            compensation  cations  with polynuclear  metal  ion  hydro-complexes  which
            are formed in hydrolysed solutions of polyvalent metal ions such as Al(III)
            or Zr(IV). The polynuclear cations dehydrate on calcination to create metal
            oxide clusters which act as pillars between the clay layers and create spaces
            of molecular  dimensions.  Example  separations  with pillared  clays include
            the separation of oxygen and nitrogen, and the separation of isomers.



            2.9    ZEOLITES

            Zeolites are porous crystalline aluminosilicates which comprise assemblies
            of SiO4 and AIO4 tetrahedra joined together through the sharing of oxygen
            atoms. More than 150 synthetic zeolite types are known, the most important
            commercially being the  synthetic types A  and X, synthetic mordenite  and
            their  ion-exchanged  varieties.  Of  the  40  or  so  mineral  zeolites  the  most
            important commercially are chabazite, faujasite and mordenite. Cavities (or
            cages) are contained within the framework of a zeolite and are connected by
            regular channels (pores) which are of molecular dimensions and into which
            adsorbate  molecules  can  penetrate.  In  crystal  form,  zeolites  are  distinct
            from other adsorbents in that, for each type, there is no distribution of pore
            size because  the  crystal  lattice  into which the  adsorbate  molecules  can  or
            cannot enter is precisely uniform. The internal porosity is high and thus the
            majority  of adsorption  takes  place  internally.  For  this reason  zeolites  are
            capable  of separating  effectively  on  the  basis  of size  and  they have  been
            assigned  the  popular  description  of  molecular  sieves.  The  processes  of
            adsorption and desorption of molecules in zeolites are based on differences
            in molecular size, shape and other properties such as polarity. For physical
            adsorption  the  cavities  fill  and  empty  reversibly  and  the  mechanism  is
            generally  considered  to  be  one  of  pore  filling.  Hence  the  surface  area
            concepts presented for other types of adsorbent strictly do not apply.
              The  channel size is determined by the number of atoms which form the
            apertures (or windows) leading to the cages. For example, apertures may be
            constructed from rings of 6, 8, 10 or 12 oxygen atoms together with the same
            number  of  aluminium  and/or  silicon  atoms.  Cages  formed  with  6  oxygen
            atom  apertures  can  admit  only  the  smallest  molecules  such  as  water  and
            ammonia. Zeolites containing 8, 10 and 12 oxygen atom rings have limiting
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