Page 649 - Bird R.B. Transport phenomena
P. 649

§20.2  Steady-State Transport in Binary  Boundary  Layers  629

                From the last three equations we  conclude that the profiles  will be expressible  in terms  of the
                single coordinate  77, if and only  if the interfacial  velocity  v (x) is  of the form
                                                              o
                                                                                    (20.2-37)

                Any  other functional  form  for v (x) would  cause the left  side  of  Eq. 20.2-34  to depend on both
                                         Q
                x  and  17, so that a combination  of  variables  would  not be possible.  The boundary  layer  equa-
                tions would  then require integration  in two  dimensions, and  the calculations  would  become
                more difficult.  Equation 20.2-37 specifies  that v (x) vary as  1/Vx,  and thus, inversely  with the
                                                     o
                boundary  layer  thickness  8  of  Eq. 4.4-17.This  equation has  the same  range  of  validity  as  Eq.
                20.2-34, that is, 1  < <  (v^x/v)  <  (i> */i>)  (see Fig. 20.2-2).
                                            x   cril
                    Fortunately the condition in Eq. 20.3-37  is a useful  one. It corresponds to a direct propor-
                tionality  of pv  to the interfacial  fluxes  т , q , and j .  Conditions of  this type arise naturally in
                           0                    0  0    AQ
                diffusion-controlled  surface  reactions, and  also  in  certain  cases  of  drying  and  transpiration
                cooling. The determination of  К for  these situations  is considered  at the end  of  this  example.
                Until then we treat К as given.
                    With  the  specification  of  v (x)  according  to  Eq.  20.2-37,  the  problem  statement  is  com-
                                          o
                plete, and we are ready  to discuss  the calculation  of the profiles.  This is best done by numeri-
                cal integration, with  specified  values  of the parameters Л and K.
                    The  first  step  in the solution  is  to evaluate  the velocity  profile  П,. For this  purpose  it  is
                                                                        г
                convenient to introduce the function

                                              f=  -K+  P I M T J                    (20.2-38)
                                                      Jo
                which  is a generalization  of  the dimensionless  stream  function / used  in Example  4.4-2. Then
                                                                                    2
                setting  Л  =  1 in  Eq. 20.2-34  and  making  the substitutions /'  = df/d-q =  U  f"  = d f/dr) 2  =
                                                                             v/
                dU /drj, and so on, gives the equation of motion in the form
                   v
                                                  -ff"=f'"                          (20.2-39)
                and  Eqs. 20.2-35, 36, and 38 give the boundary conditions

                                             at  r/ =  oo,  /' = i                  (20.2-40)
                                             at7j  = 0,  f'  = 0                    (20.2-41)
                                             at  7) = 0,  f  = -K                   (20.2-42)

                Equation  20.2-39 can be  solved  numerically  with  these boundary  conditions  to obtain / as a
                function  of  г] for various  values  of  X.
                    Once  the  function  /(ту,  К)  has  been  evaluated,  we  can  integrate  Eq.  20.2-34  with  the
                boundary conditions in Eqs. 20.2-35 and 36 to obtain

                                               J  expl-Aj  fi^
                                                         j
                                               J
                                               — )
                                    IKTJ, Л, Ю = —   )             {                (20.2-43)
                                               f
                                               f    I    f         \
                                                  exp  -Л
                                                     \
                Some profiles  calculated  from  this equation by  numerical integration are given  in Fig. 20.2-
                3.  The velocity  profiles  are given by  the curves  for  Л = 1. The temperature and composition
                profiles  for  various  Prandtl and  Schmidt  numbers  are  given  by  the  curves  for  the corre-
                sponding  values  of  Л. Note that the velocity,  temperature, and  composition boundary  lay-
                ers  get  thicker when  К is  positive  (as in evaporation) and  thinner when  К is  negative  (as in
                condensation).
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