Page 405 - Bird R.B. Transport phenomena
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§12.4  Boundary  Layer Theory  for Nonisothermal Flow  387

                              From Eq. 12.3-6 the heat flux through the base  of the wall may be obtained:
                                                               2ksecTTx/b _                      _
                                                             =            (h  To)              ( ] 2 3  7 )




            BOUNDARY      LAYER   THEORY FOR
                                        1
            NONISOTHERMAL        FLOW -  23
                          In  §4.4  the  use  of boundary  layer  approximations  for steady,  laminar  flow  of incom-
                          pressible  fluids  at constant  temperature  was  discussed.  We  saw  that, in the  neighbor-
                          hood of a solid  surface,  the equations of continuity and  motion could  be  simplified,  and
                          that  these equations  may  be  solved  to get  "exact  boundary  layer  solutions"  and  that an
                          integrated  form  of these equations  (the von  Karman momentum balance) enables  one to
                          get  "approximate boundary  layer  solutions."  In this  section we  extend  the previous  de-
                          velopment by including  the boundary  layer  equation  for  energy  transport, so that  the
                          temperature profiles  near solid  surfaces  can be obtained.
                              As  in §4.4 we  consider the steady  two-dimensional  flow around a submerged  object
                          such as that  shown  in Fig.  4.4-1.  In  the  vicinity  of the  solid  surface  the  equations of
                          change may be written  (omitting the bars  over p and  /3) as:
                                                          dV Y  dv .
                                                                x
                                                                 1
                                                            1
                          Continuity                      -ТГ  + -г  = О                      (12.4-1)
                                                          oX  dy
                          Motion         p ^ , ^ +  o , ^ J -  ^  +   ^  + p^ff-T,)           (12.4-2)
                                                            w     M
                                                                                                -
                                               ^-g^fb^Mt)                                    <i24 3)

                          Here p,  /x, k, and C  are regarded as constants, and  fi(dv /dy) 2  is the viscous  heating ef-
                                                                          x
                                           p
                          fect, which is henceforth disregarded.  Solutions  of  these equations are asymptotically  ac-
                          curate  for small  momentum  diffusivity  v = /x/p in Eq.  12.4-2,  and  for small  thermal
                          diffusivity  a = k/pC  in Eq. 12.4-3.
                                           p
                              Equation  12.4-1 is the  same as Eq. 4.4-1. Equation  12.4-2  differs  from  Eq.  4.4-2  be-
                          cause  of the inclusion  of the buoyant  force  term (see §11.3), which  can be significant  even
                          when  fractional  changes  in density  are small. Equation  12.4-3 is obtained from  Eq. 11.2-9
                          by  neglecting  the heat conduction in the x direction. More complete forms  of the bound-
                          ary  layer  equations may be found  elsewhere. ' 2 3
                              The usual boundary  conditions for  Eqs.  12.4-1 and 2 are that v  = v  = 0 at the  solid
                                                                                       y
                                                                                  x
                          surface, and that the velocity  merges  into the potential flow at the outer edge  of  the veloc-
                          ity  boundary layer, so that v x  —» v (x). For Eq. 12.4-3 the temperature T is  specified  to be T o
                                                     e
                          at the solid  surface  and  Т  at the outer edge of the thermal boundary layer. That is, the ve-
                                               ж
                          locity  and temperature are  different  from  v {x) and  Т  only  in thin layers  near the  solid
                                                                       ж
                                                               e
                          surface.  However,  the  velocity  and  temperature  boundary  layers  will be of  different
                          thicknesses  corresponding  to the relative  ease  of the diffusion  of momentum and  heat.
                          Since Pr  =  v/a,  for  Pr > 1 the temperature boundary  layer  usually  lies inside  the  veloc-

                              1
                               H. Schlichting, Boundary-Layer  Theory, 7th edition, McGraw-Hill, New  York  (1979), Chapter 12.
                               K. Stewartson, The Theory of Laminar Boundary  Layers in Compressible Fluids, Oxford  University
                              2
                          Press  (1964).
                               E. R. G. Eckert and  R. M. Drake, Jr., Analysis  of Heat and Mass  Transfer, McGraw-Hill, New  York,
                              3
                          (1972), Chapters 6 and 7.
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