Page 604 - Bird R.B. Transport phenomena
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584  Chapter  19  Equations  of Change for  Multicomponent Systems

                            where  R Q  is  the  molar  rate  of  production  of  a  per  unit  volume.  This  equation  can  be
                            rewritten by use  of  Eq. (V)  of  Table  17.8-1  to give

                                          дс  _
                                           а   -(V  •  c v* >-(v-j;) +  K  a  = ,2,3,  . . . , N  (19.1-11)
                                                                             1
                                          dt          a             a
                                         rate of  net rate of  rate of  rate of
                                         increase  addition  addition  production
                                         in moles  in moles  of  of moles  of  of moles  of
                                         of A per  A per unit  A per unit  A per unit
                                         unit  volume  by  volume  by  volume  by
                                         volume  convection  diffusion  reaction
                            When  all N equations in Eq. 19.1-10 or  11 are added  we  get

                                                                                               (19.1-12)

                            for  the equation  of continuity  for  the mixture. To get  this we  used  Eq. (M) of Table  17.8-1.
                            We  also  note that the  chemical  reaction  term  does  not drop  out  because  the number  of
                            moles  is not necessarily  conserved  in a chemical reaction. Finally we  note that

                                                         (V  • v*) = £  £  R a                  (19.1-13)

                            for  a fluid mixture  of constant molar density  с
                               We  have  thus  seen  that  the equation  of  continuity  for  species  a  may  be  written  in
                            two  forms,  Eq.  19.1-7 and  Eq.  19.1-11.  Using  the continuity  relations  in  Eqs.  19.1-8 and
                            19.1-12 the reader may  verify  that the equation  of continuity for  species  a  can be put into
                            two  additional, equivalent  forms:


                                      { dt  +  ( , 7  '  *o)-  -( и     a  = ..2 ,3,.          (19.1-14)


                                  <dx a  + (v* • Vx  =  -(V  + R -  x  N     a =  1/ 2, 3,..   (19.1-15)
                                             v  л с•')        a    Q  1                 •  ,N
                                                                    /3 = 1
                            These  two  equations  express  exactly  the same  physical  content, but  they  are  written  in
                            two  different  sets  of notation—the first  in mass  quantities and  the second  in molar quan-
                            tities. To use  these equations we  have  to insert  the appropriate expressions  for  the fluxes
                            and  the chemical  reaction  terms.  In this  chapter  we  give  only  the  results  for  binary sys-
                            tems with  constant рЯЬ  with  constant сЯЬ , or with  zero  velocity.
                                               АВ/
                                                                АВ

      Binary  Systems with  Constant рЯЬ АВ
                            For this assumption,  Eq. 19.1-14 becomes, after  inserting  Fick's law  from  Eq. (A)  of  Table
                            17.8-2,

                                                     f   ( V                                   (19.1-16)

                            with  a corresponding  equation  for  species  B. This equation  is appropriate  for  describing
                            the diffusion  in dilute liquid solutions at constant temperature and pressure.  The left  side
                            can be  written  as  pDo) /Dt.  Equation  9.1-16 without  the  v A  term  is  of  the same  form  as
                                               a
                            Eq.  11.2-8 or  9. This  similarity  is  quite  important, since  it  is  the basis  for  the  analogies
                            that  are  frequently  drawn  between  heat and  mass  transport  in  flowing  fluids  with  con-
                            stant physical  properties.
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