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7.3  Numerical  Method  for  the  Standard  Problem                   217



                          rj =  yju e/ux  y,  ij)(x, y)  =  y/u evx  /(x,  7?)  (7.3.4)

         Noting  the  chain  rule  relations  (subsection  2.2.4),  it  can  be  shown  that,  with  a
         prime  denoting  differentiation  with  respect  to  77, and  with

                                    £ =  £   u e =  ^                       (7.3.5)
                                        Li         UQQ
         Eq.  (7.3.3)  and  its  boundary  conditions,  Eq.  (7.3.1),  can  be  written  as
                                               2
                (bf'Y +  ^ / / "   +  m[l -  (/') ] = £ [f^  - " | 0         (7.3.6)
                                                               /

                                          /
                77  =  0,  / '  =  0,  /(£,0)  = „(£)  =  -  ^  /  ?  —  d?  (7.3.7a)
                                     »?  =  %,  / '  =  1                  (7.3.7b)
         Here  r? e corresponds  to  a  transformed  boundary-layer  thickness,  yju e/vx8,  or
         y/u eRL/t;8/L;  RL  is  a  Reynolds  number  based  on  reference  velocity  UOQ and
         length  L\  m  is  a  dimensionless  pressure-gradient  parameter  defined  by

                                       ra=  —  — -                          (7.3.8)

         The  velocity  components  u  and  v  are  related  to  the  dimensionless  stream  func-
         tion  /(£,/7)  by
                                         u  =  u e / '                     (7.3.9a)

                        ?J  =  —yJU eVX        /u ex +  —- + /  —         (7.3.9b)
                                       /w ex  dx      dx     dx  \
         For  laminar  flows  with  the  external  velocity  of  the  form

                                           =  Cx m                        (7.3.10)
                                        u e
        with  C  and  m  constants,  and with boundary  conditions  on  /  and '  independent
                                                                    /
        of  x,  the  left-hand  side  of  Eq.  (7.3.6)  reduces  to
                             r+rn   +  \ ffH  +  m[1_ {fl)2]=Q             ( 7 3 n )

         which  is  called  the  Falkner-Skan  equation.  Its  solutions,  which  are  limited  to
         —0.0904  <  m  <  00, are  independent  of  £ and  can  be  used to  generate  the  initial
         conditions  needed  for  the  solution  of  the  boundary-layer  equations,  as  shall  be
         shown  later.
            There are several numerical methods that  can be used to  solve the  boundary-
         layer equations. Finite-difference  methods  offer  the greatest  flexibility,  and  those
         of  Crank-Nicolson  and  Keller,  discussed  in  Section  4.4,  have  been  widely  used.
         The  latter  method  provides  significant  advantages  over  the  former  method  and
         will  be  used  to  solve  the  boundary-layer  equations  in  this  chapter,  as  well  as
         the  stability  equation  to  be  discussed  in  Chapter  8.
           To  solve  Eqs.  (7.3.6)  and  (7.3.7)  with  Keller's  box  method,  we  follow  the
         four  steps  discussed  in  subsection  4.4.3.
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