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246                                               8.  Stability  and  Transition

         Table  8.1.  Critical  Reynolds  number
         for  Falkner-Skan  flows  [3].

         %             0            H
         12490         1.0          2.216
         10920         0.8          2.240
          8890         0.6          2.274
          7680         0.5          2.297
          6230         0.4          2.325
          4550         0.3          2.362
          2830         0.2          2.411
          1380         0.1          2.481
          865          0.05         2.529
          520          0.0          2.591
          318        -0.05          2.676
           199       -0.10          2.801
           138       -0.14          2.963
           67        -0.1988        4.029


         Falkner-Skan  flows  given  by  Eq.  (7.3.11).  Note  that  in  this  figure  the  critical
         Reynolds  number  is  based  on  displacement  thickness  <5*, and  local  velocity  u e.
        In  terms  of  Falkner-Skan  variables  it  can  be  expressed  as

                                      Rs*  =  \fRx6\                       (8.1.8)
        with  8\  denoting  a  dimensionless  displacement  thickness  parameter  expressed
        in  terms  of  Falkner-Skan  variables  by


                               *i=   r{l-f')dri   = rie-fe                 (8-1.9)
                                    JO
           From  Fig.  8.2  it  is  seen  that  accelerating  flows  can  tolerate  larger  Reynolds
        numbers than  decelerating  flows and,  as  a result,  have  a higher  critical  Reynolds
        number.  On  the  other  hand,  decelerating  flows  have  less  tolerance  to  higher
        Reynolds  numbers,  indicating  that  R$*  becomes  smaller  as  H  becomes  bigger
        which  corresponds  to  smaller  values  of (3.


         8.2  Solution  of  the  Orr-Sommerfeld     Equation

        There  are  several  numerical  methods  for  obtaining  solutions  of  the  stability
        equations  for  two-  and  three-dimensional  flows.  In  general,  finite-difference
        methods  are  more  efficient  and  flexible  than  the  initial-value  schemes  which
        may  have  problems  associated  with  parasitic  error  growth  as  discussed  in  [3].
        An  efficient  and  accurate  finite-difference  method  is  the  box-scheme  discussed
        in  subsection  4.4.3  for  the  unsteady  heat  conduction  equation  and  in  Chap-
        ter  7  for  the  boundary  layer  equations.  Here  we  discuss  its  application  to  the
         Orr-Sommerfeld  equation.
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