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166   ZEOLITES AND MOLECULAR SIEVES

                                                    SiO 2




                                                      +Y
                                                  B   +B
                                                      +X
                                                      +A
                                          Y
                                               X
                                                 A


                                              HS
                                     Na O                         Al O 3
                                       2
                                                                   2
                                                     (a)
                                                     SiO
                                                        2



                                               Y      +S,Y
                                              S       +R
                                                    R  +X
                                                      +A
                                                X
                                                   A





                                     Na O                          Al O 3
                                       2
                                                                     2
                                                      (b)
                     Figure 7.5. Compositional ‘‘synthesis windows’’ for the Na 2 O-Al 2 O 3 -SiO 2 -H 2 O system at
                        ◦
                     100 C and 90–98 mol% H 2 O. Source of SiO 2 is (a) sodium silicate and (b) colloidal silica.
                     The area enclosing a letter represents the composition that yields the corresponding phase,
                     while the + marks the typical composition of the product. A, X, and Y = zeolites types A, X,
                     and Y; B = zeolite P; R = chabazite; S = gmelinite; and HS = hydroxysodalite (from Breck and
                     Flanigen, 1968, with permission).


                       Tetramethylammonium (TMA) cation was investigated as an additive in the
                     synthesis of type A zeolite (LTA or Linde Type A) in 1961 (Barrer and Denny,
                     1961; Kerr and Kokotailo, 1961). Many new crystalline phases were found by the
                     addition of TMA. It was soon found that the Si/Al ratio in LTA could be increased
                     up to 2.5 by the use of TMA. An analog of these crystals is named ZK-4 (Kerr,
                     1966). The size of the TMA cation is approximately 6 ˚ A, which is about the same
                     size as that of hydrated Na . These cations fit well in the beta or sodalite cage.
                                           +
                     A typical composition of ZK-4 is Na 8 (TMA) 1.2 [(AlO 2 ) 9.2 (SiO 2 ) 14.8 ] · 28H 2 O.
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