Page 41 - Materials Chemistry, Second Edition
P. 41

28                                              2 Solid-State Chemistry

                a
                       crystallization solution


                                                      volatile "nonsolvent"





                b



                                                         "Nonsolvent" layered
                                                         on top of crystallization
                                                         solvent



                c
                  "Cold finger", filled with ice
                  water, dry ice/acetone mixture, etc.  To vacuum



                                                      Side arm valve, controls
                                                      dynamic or static vacuum
                        Oil bath, or
                        heating mantle
                                                       Solid mixture


           Figure 2.6. Schematic of three common methods used to grow single crystals. Shown is (a) diffusion
           where vapors from a volatile “nonsolvent” meet the crystallization solvent; (b) interfacial where the non-
           solvent is layered on top of the crystallization solvent; (c) sublimation where the solid mixture is heated
           and the vapors form crystallites on the surface of a cold finger. For this latter technique, the crystallization
           flask may be opened to vacuum throughout the sublimation process (dynamic vacuum), or closed after
           maintaining initial vacuum to allow slower crystal growth (static vacuum).


           melt, there is extension of the crystal due to preferred alignment of other silicon
           atoms present in the melt (see Chapter 4). The empirical use of seed crystals is
           frequently used for crystal growth at all temperature regimes. Scratching the inside
           of the flask, or even using boiling stones has been successful at inducing crystal
           formation, through the introduction of sites for nucleation. It must be noted that pH
           is often not an important factor for inorganic or organic crystals; however, for
           protein crystallization, which is beyond the scope of this book, many such atypical
           conditions must also be considered.
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