Page 216 - Process Modelling and Simulation With Finite Element Methods
P. 216

Simulation and Nonlinear Dynamics         203



                                                                      (5.18)


         Equation  (5.17)  can be  viewed  as the  vorticity  generation equation by  direct
         comparison to (3.3). Any y-variation in concentration c or finite vertical velocity
         v creates vorticity  on the RHS of  (5.17), which  then convects concentration in
         (5.18), potentially  reinforcing the voriticity  generation mechanisms  on the RHS
         of  (5.17),  if diffusion is not strong enough to dissipate out the disturbance or if
         the nonlinear coupling parameter R is too strong for diffusion to overcome.  The
         linear  stability  theory  [13]  quantifies  for  a  given  wavenumber  of  vertical
         disturbance, whether  the relative opposing forces (R for instability  by  vorticity
          generation,  1Pe  for  stability  by  diffusion)  result  in  stabilization  or
          destabilization in tandem.  In general, there is a longwave instability that cuts-off
          at a given short length scale, smaller than which diffusion dominates and causes
          disturbances to  decay.  This longwave unstable packet is expected to manifest
          itself with the mode corresponding to fastest growth dominating.
             Because of the change of variables and coordinate transform, we now expect
          that far enough away horizontally  from the mixing zone, c becomes uniform and
          u=0, i.e. periodic boundary conditions can be used for c and y, if we apply a well
          known trick for c  - domain doubling.  If we use the mirror  image of the initial
          condition for c, which  was taken  as a modification of the complementary error
          function on the positive x-axis, erfc(x)*(  1 .+0.05*sin(3 1.4159*y)), then c decays
          from unity at the origin in both directions, i.e. periodic at infinity, but effectively
          zero after a short distance, then both c and u can be approximated as periodic
          horizontally.  The upper  and  lower  bounding  surfaces can be  taken  as either
          periodic  (as  in  [14])  or  no  fludno penetration.  The latter  pair  of  boundary
          conditions are adopted here.  The FEMLAB model is specified as follows.
          Launch FEMLAB and bring up the Model Navigator.  Select the  Multiphysics
          tab.
            Model Navigator
                   Select 2-D dimension
                   Select PDE modes =xoefficient*mode   name mom, variable si>>
                   Select PDE modes =xoefficient*mode   name condiff, variable c>>
                   Select solver time dependent


          Pull down the Options menu  and set the grid to (-1.1,l.l) x  (-0.1,l.l) and the
          grid spacing to 0.5,O.l. Pull down the Draw menu and select Rectangle/Square
          and place it with vertices  [-1,1] x [0,1].
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