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Sepsci*21*TSK*Venkatachala=BG
                                                                                I / CHROMATOGRAPHY    47


           is given by:                                    minimized by using particles of small diameter with
                                                           a narrow particle size distribution in columns with
                             u"  E/4                  [2]  a high and homogeneous packing density. For open-
                                                           tubular columns, Sow anisotropy is not a contribu-
           where   is the solution dielectric constant,   is the zeta  ting factor since the streamlines have no obstacles in
           potential (potential at the boundary between the  their way to cause disruption of the sample proRle.
           charged surface and the start of the diffuse part  Axial diffusion is the natural tendency of sol-
           of the double layer), and E is the electric Reld  ute molecules in the mobile phase to redistribute
           strength. Note that there is no explicit dependence on  themselves by diffusion from a region of high con-
           the particle size and column length, which limit the  centration to one of lower concentration. Its contri-
           total efRciency of columns when the Sow is pneu-  bution to zone broadening depends on the solute
           matically driven. The column length and column in-  diffusion coefRcient in the mobile phase and
           ternal diameter, however, cannot be treated as inde-  the column residence time. Diffusion of solute
           pendent variables in MEKC and CEC, but are related  molecules occurs in all directions but only the compo-
           through Joule heating of the electrolyte and its ef-  nents in the plane of mobile-phase migration contrib-
           fect on the mobile-phase Sow proRle. Heat is gener-  utes to the peak proRle observed in the chromatogram.
           ated homogeneously throughout the electrolyte but  Resistance to mass transfer in either the stationary
           the temperature variation across the column diameter  or mobile phases is a consequence of the fact that
           is parabolic. Radial temperature gradients between  mass transfer in the chromatographic system is not
           the centre of the tube and the column wall cause  instantaneous and equilibrium may not be achieved
           zone broadening resulting from sample diffusion  under normal separation conditions. Consequently,
           and solvent density and viscosity differences in  the solute concentration proRle in the stationary
           the direction of Sow.                           phase is always slightly behind the equilibrium posi-
                                                           tion and the mobile-phase proRle is similarly slightly
                                                           in advance of the equilibrium position (Figure 9). The
           Zone Broadening
           Rate theory attempts to explain the kinetic contribu-
           tion to zone broadening in column chromatography
           as the sum of three main contributions: Sow ani-
           sotropy (eddy diffusion), axial diffusion (longi-
           tudinal diffusion), and resistance to mass trans-
           fer. Flow anisotropy is illustrated in Figure 8. When
           a sample band migrates through a packed bed, the
           individual Sow paths must diverge to navigate
           around the particles such that individual Sow streams
           are of unequal lengths. These variations in Sow
           direction and rate lead to zone broadening that
           should depend only on the particle size and homogen-
           eity of the column packing. Flow anisotropy can be



















                                                           Figure 9 Representation of resistance to mass transfer in the
                                                           mobile and stationary phases. The dashed line represents the
           Figure 8 Representation of flow anisotropy in a packed col-  equilibrium position and the solid line the actual position of
           umn.                                            the solute zones.
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