Page 111 - Computational Fluid Dynamics for Engineers
P. 111

4.2  Model  Equations                                                  97



        This  equation  is  still  parabolic  in  time  in  the  (x, t)  space  and  is  called  the
         convection-diffusion  equation  due  to  the  simultaneous  presence  of  convection
        by  the  velocity  u  and  diffusion  through  the  diffusivity  coefficient  a.
           If the  effect  of the pressure gradient  on the momentum  equation  is  neglected,
        Eq.  (4.2.2)  becomes
                                                   2
                                    du     du     d u                      , *  „  ^
                                       +u
                                                                            - -
                                    m e- =^                                (4 2 7)
                                            x
        which  has  the  structure  of  a  convection-diffusion  equation  but  is  nonlinear.  It
        is  known  as  Burger's  equation,  and  it  contains  the  full  nonlinearity  of the  one-
        dimensional  flow  equations.  For  an  inviscid  flow,  it  becomes
                                      du     du                            ,,  ^  ^
                                         +u
                                      m d- =°                              (4 2 8)
                                                                            - -
                                              x
        and  is  known  as  the  "inviscid"  Burger's  equation.  Unlike  Eq.  (4.2.7),  which  is
        parabolic,  this  equation  is hyperbolic.  It  is  also  nonlinear,  as  is Eq.  (4.2.7).
           The discussion on constructing model equations  for simplified  one-dimensional
        flows can  also be extended  to simplified  two-dimensional  flows.  For this  purpose,
        for  two-dimensional  inviscid  flows,  the  Laplace  equation  given  by  Eq.  (2.4.20)
                                              2
                                       2
                                      d 6  + =0                           (429)
                                             d 6
                                     n£ 4                                    -
        which  is  a  typical  elliptic  equation,  describes  an  isotropic  diffusion  in  the  (x,y)
        space.
           A  similar  equation  results  from  Eq.  (2.2.11),  which  is  a  parabolic  in  time  in
        the  (x,y,  £) space.  Assuming  that  the  temperature  field  is  in  a  medium  at  rest,
        then  in the  presence  of the  source  term  q^,  Eq.  (2.2.11)  reduces  to  the  Poisson
        equation
                                           2
                                    2
                                   d T    d T      1  .                  /.  o ^  x
                                                                          ' -
                                   7^   + W   =  -k qh                   (4 2 10a)
        An  equation  similar  to  this  is  obtained  from  Eq.  (2.2.9)  for  a  fully  developed
        laminar  channel  flow  in  a  rectangular  duct.  Noting  that  Du/Dt  is  zero,  and
        neglecting  the  body  force,
                                    2
                                           2
                                   d u    d u     I  dp
                                   dx 2   dy 2    ji  dx
           If  the  temperature  in  Eq.  (4.2.10a)  is  time  dependent,  and  the  medium  is
        again  at  rest,  then  the  unsteady  heat  conduction  equation  in  two  dimensions
        and  with  source  term  becomes





        This  equation  is  parabolic  in  time  in  the  (x,?/,£)  space.  Its  solutions  at  large
        time  values  should  approach  the  solutions  of  Eq.  (4.2.10a).
   106   107   108   109   110   111   112   113   114   115   116