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               100                                                                                Crystallization Processes


               provide a useful means of correlating nucleation kinetics  Multicrystal-magma studies usually involve examina-
               and using the resulting correlations in process analysis and  tion of the rate of change of a characteristic crystal di-
               control. The correlations generally take the form:  mension or the rate of increase in the mass of crystals in
                                          j
                                       i
                                ◦
                               B = k N σ M N k           (18)    a magma. The characteristic dimension in such analyses
                                          T                      depends upon the method used in the determination of
               where k N , i, j, k are positive parameters obtained from  crystal size; for example, the second largest dimension is
               data correlation, M T is the magma density (mass of solids  measured by sieve analyses, while an equivalent spherical
               per unit volume of slurry or solvent in the magma), and N  diameter is determined by both electronic zone sensing
               is the rotational velocity of the impeller or pump rotor. For  and laser light scattering instruments. A relationship be-
               convenience, either crystal growth rate or mean residence  tween these two measured dimensions and between the
               time, both of which are directly related to supersaturation,  measured quantities and the actual crystal dimensions can
               may be substituted for σ in Eq. (18).             be derived from appropriate shape factors. Volume and
                 If primary nucleation dominates the process, i tends  area shape factors are defined by the equations:
               to larger values (say greater than 3), j and k approach          3                     2
                                                                      v crys = k vol L  and  a crys = k area L  (19)
               zero, and Eq. (18) approaches Eq. (17). Should crystal–
               impeller and/or crystal–crystallizer impacts dominate, j  where v crys and a crys are volume and area of a crystal,
               approaches 1; on the other hand, if crystal–crystal contacts  k vol and k area are volume and area shape factors, and L
               dominate, j approaches 2.                         is the characteristic dimension of the crystal. Suppose an
                 The ease with which nuclei can be produced by con-  equivalent spherical diameter L sphere is obtained from an
               tact nucleation is a clear indication that this mechanism  electronic zone-sensing instrument, and the actual dimen-
               is dominant in many industrial crystallization operations.  sions of the crystal are to be calculated. Assume for the
               Research on this nucleation mechanism is continuing with  sake of this example that the crystals have a cubic shape.
                                                                                                        sphere
               the objective of building an understanding of the phe-  Let L cube be the edge length of the crystal and k vol  and
               nomenon that will allow its successful inclusion in models  k cube  be the volume shape factors for a sphere and a cube,
                                                                  vol
               describing commercial systems.                    respectively. Since the volume of the crystal is the same,
                                                                 regardless of the arbitrarily defined characteristic dimen-
                                                                 sion,
               D. Fundamentals of Crystal Growth
                                                                                  sphere  3    cube  3
                                                                           v crys = k  L   = k   L          (20)
               Crystal growth rates may be expressed as (1) the linear            vol  sphere  vol  cube
               advance rate of an individual crystal face, (2) the change  sphere     cube
                                                                 Since k vol  is π/6 and k vol  is 1.0, the numerical rela-
               in a characteristic dimension of a crystal, or (3) the rate of
                                                                 tionship between L cube and L sphere is given by:
               change in mass of a crystal or population of crystals. These
               different expressions are related through crystal geometry;    k sphere    1/3      1/3
                                                                                              π
                                                                              vol
               it is often convenient to use the method of measurement  L cube =  cube  L sphere =  L sphere  (21)
                                                                             k                 6
               as the basis of the growth rate expression or, in certain      vol
               instances, the method used to analyze a crystallization  The rate of change of a crystal mass dm crys /dt can be
               process will require that growth rate be defined in a spe-  related to the rate of change in the crystal characteristic
               cific way. For example, the use of a population balance  dimension (dL/dt = G) by the equation:
               to describe crystal size distribution requires that growth     d ρk vol L 3

               rate be defined as the rate of change of a characteristic  dm crys  =     = 3ρk vol L 2  dL   (22)
               dimension.                                               dt        dt               dt
                 Single-crystal growth kinetics involve the advance rate  where ρ is crystal density. Since k area = a crys /L ,
                                                                                                       2
               of an individual crystal face normal to itself or the rate of
               change in crystal size associated with exposure to a super-  dm crys  = 3ρ(k vol /k area )a crys G  (23)
               saturated solution. The advance rate of a single crystal face  dt
               can be quantified by observation of the face through a cali-  At least two resistances contribute to the kinetics of
               bratedeyepieceofanopticalmicroscope,whichallowsex-  crystal growth. These resistances apply to (1) integration
               aminationofthestructureoftheadvancingcrystalfaceand  of the crystalline unit (e.g., solute molecules) into the crys-
               isolation of surface-reaction kinetics from mass-transfer  talsurface(i.e.,lattice),and(2)moleculardiffusionorbulk
               kinetics (these phenomena will be discussed later). An  transport of the unit from the surrounding solution to the
               additional advantage of single-crystal systems is that it is  crystalsurface.Asaspectsofmoleculardiffusionandmass
               possible to examine crystal growth kinetics without inter-  transfer are covered elsewhere, the current discussion will
               ference from competing processes such as nucleation.  focus only on surface incorporation.
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