Page 58 - Bird R.B. Transport phenomena
P. 58

§2.2  Flow  of a Falling  Film  43

                                                                  a
                                                                               c
                obtained by neglecting  such  disturbances,  particularly  if  W nd L are large ompared to
                                                                t
                the  film  thickness  8. For small  flow  rates  we expect  that he viscous  forces  will  prevent
                continued  acceleration  of he liquid  down he wall, so that  v z  will  become ndependent
                                                    t
                                      t
                                                                               i
                of  z in a  short  distance  down  the plate.  Therefore  it  seems  reasonable  to postulate  that
                    v
                                                               F
                17, = (x),  v x  = 0, nd v y  = 0, nd further  that p  = p(x). rom Table  B.I it is seen  that he
                               a
                                         a
                                                                                       t
                     z
                                              a
                only onvanishing omponents of т re  then T  = T  =  -fi(clv /dx).
                                c
                    n
                                                       XZ
                                                           ZX
                                                                     z
                                      "
                   We  now select  as he system"  a thin shell  perpendicular to the x direction  (see Fig.
                                   t
                                    2
                2.2-2).  Then  we set p a -momentum balance  over  this  shell,  which  is a region  of  thick-
                                u
                                                a
                                  t
                ness  Ax, ounded  by he planes  2  = 0 nd z  = L, nd extending  a distance  W in he у di-
                                                                                   t
                       b
                                                         a
                                                  m
                                               t
                rection. The various  contributions to he omentum balance are  then  obtained  with he
                                                                                       t
                                     t
                help  of the quantities  in he z-component"  columns  of Tables  1.2-1 nd 1.7-1.  By  using
                                                                          a
                                        "
                                t
                the omponents  of he combined  momentum-flux  tensor"  ф  defined  in  1.7-1 to 3,  we
                                    "
                   c
                can  include all he possible  mechanisms  for  momentum  transport at once:
                             t
                      2
                rate  of -momentum in
                across  surface  at z  = 0      (WAx)</> |                           (2.2-1)
                                                       22 2=0
                                 o
                rate of -momentum ut
                      2
                across  surface  at z  = L      (WAx)<£ 22| 2=L                      (2.2-2)
                      z
                rate  of -momentum in
                across  surface  at x            (L №)(ф )\                          (2.2-3)
                                                      Х2  х
                      2
                rate of -momentum ut
                                 o
                across  surface  at x  + Ax    (L 1Л/)(ф )|  .                       (2.2-4)
                                                      Х2 х+Дд
                gravity  force  acting
                         t
                on  fluid  in he z direction  (L W Ax)(pg cos /3)                    (2.2-5)
                By  using  the  quantities  ф хг  and  ф гг  we  account  for  the  z-momentum  transport  by  all
                mechanisms, convective  and  molecular. Note that we  take the "in"  and  "out"  directions
                in  the  direction  of  the  positive  x- and  z-axes  (in  this  problem  these  happen  to  coincide
                with  the  directions  of  z-momentum  transport). The  notation  \ x+lx  means  "evaluated  at
                x  + Ax,"  and g  is the gravitational  acceleration.
                    When  these terms are substituted  into the z-momentum balance  of  Eq. 2.1-1, we  get
                                -  ФХдх)  +  WAx(4> |  "  ФЛг-i)  +  0 ^  Ax)(pg cos  j8)  = 0  (2.2-6)
                                                  22 2=0
                                             gravity
                Fig. 2.2-2  Shell  of thickness  Ax over  which  a 2-momentum balance is made. Arrows show  the
                momentum fluxes associated  with  the surfaces  of the shell. Since v x  and v y  are both zero, pv v
                                                                                        x z
                and  pv v  are zero. Since v z  does not depend on у and z, it follows  from  Table  B.I that r yz  = 0
                     y z
                and  r Z2  = 0. Therefore, the dashed-underlined fluxes do not need to be considered.  Both p
                and  pv v  are the same at z  = 0 and z  — L, and therefore  do not appear  in the final  equation
                     z z
                for  the balance  of z-momentum, Eq. 2.2-10.
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