Page 334 - Bird R.B. Transport phenomena
P. 334

318  Chapter 10  Shell Energy  Balances and Temperature Distributions in Solids and Laminar Flow

                           This  equation  describes  the  balance  among  thejyiscous  force,  the  pressure  force,  the
                           gravity  force,  and  the  buoyant  force  -~pgf3(T  -  T)  (all  per  unit  volume).  Into  this  we
                           now  substitute  the  temperature distribution  given  in  Eq.  10.9-4  to  get  the  differential
                           equation                   2

                                                                                                 -
                                                   ^ d v 7  (dp  1   ш * т   у                (m9 9)
                                                           {£
                           which  is to be solved  with  the boundary conditions
                           B.C. 1:                      at у  = -В,  v  = 0                    (10.9-10)
                                                                     z
                           B.C. 2:                      at у  = +B,  v  = 0                    (10.9-11)
                                                                     z
                           The  solution  is

                                        v z  =

                           We now require that the net mass flow in the z direction be zero, that is,

                                                              pv dy  = 0                       (10.9-13)
                                                           J -в  z
                           Substitution  of  v z  from  Eq. 10.9-12  and p from  Eqs. 10.9-6 and 4 into this integral  leads to
                           the  conclusion that
                                                            dp
                                                            -^  =  -pg                         (10.9-14)

                           when  terms containing the square  of the small  quantity  AT are neglected. Equation  10.9-
                           14 states  that the pressure  gradient  in the system  is due solely  to the weight  of  the  fluid,
                           and  the usual  hydrostatic  pressure  distribution  prevails.  Therefore  the second  term  on
                           the  right  side  of  Eq.  10.9-12  drops  out and  the  final expression  for  the velocity  distribu-
                           tion  is


                                                                                               (10.9-15)
                                                                          D
                                                                         \ /A
                           The  average  velocity  in the upward-moving  stream  is
                                                                      D2
                                                                                               (10.9-16)

                           The  motion of  the  fluid  is thus a direct result  of  the buoyant  force  term in Eq. 10.9-8, as-
                           sociated  with  the  temperature gradient  in  the  system.  The  velocity  distribution  of  Eq.
                            10.9-15  is shown  in Fig.  10.9-1. It is  this sort  of  velocity  distribution  that occurs  in the air
                           space in a double-pane window  or in double-wall  panels in buildings.  It is also  this kind
                           of  flow  that occurs in the operation  of  a Clusius-Dickel  column used  for  separating  iso-
                           topes  or  organic  liquid  mixtures  by  the combined  effects  of  thermal  diffusion  and  free
                           convection. 1






                               1  Thermal diffusion  is the diffusion  resulting  from a temperature gradient. For a lucid  discussion
                           of the Clusius-Dickel column see K. E. Grew and T. L. Ibbs, Thermal Diffusion in Gases, Cambridge
                            University  Press  (1952), pp. 94-106.
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