Page 175 - Bird R.B. Transport phenomena
P. 175

§5.3  The Time-Smoothed Velocity  Profile  near a Wall  159

                            Equation  5.2-11 is an extra  equation obtained by  subtracting  Eq. 5.2-10 from  the original
                            equation  of continuity.
                               The  principal  result  of  this  section  is  that  the  equation  of  motion  in  terms  of  the
                            stress  tensor, summarized  in Appendix  Table  B.5, can be adapted  for  time-smoothed tur-
                           bulent flow by  changing  all  v  to v  and p to p as well  as  r  to ~r  = rf  + rf  in any  of  the
                                                    {   {                  /y    i}
                            coordinate systems  given.
                               We  have  now  arrived  at  the  main  stumbling  block  in  the  theory  of  turbulence.
                            The  Reynolds  stresses  rf  above  are  not  related  to  the  velocity  gradients  in  a  simple
                            way  as  are the time-smoothed viscous  stresses  r ^  in  Eq. 5.2-9. They are, instead, com-
                            plicated  functions  of  the  position  and  the  turbulence  intensity.  To  solve  flow  prob-
                            lems  we  must  have  experimental  information  about  the  Reynolds  stresses  or  else
                            resort  to some  empirical  expression.  In §5.4  we  discuss  some  of  the empiricisms  that
                            are  available.
                               Actually  one can also obtain equations of change for the Reynolds stresses  (see Prob-
                            lem  5D.1). However,  these  equations  contain quantities  like  v'jVJvl.  Similarly,  the  equa-
                            tions  of  change  for  the v\v v  contain the next  higher-order  correlation  v-vjvlvi,  and  so
                                                  } k
                            on. That is, there is  a never-ending  hierarchy  of  equations that must be solved.  To solve
                            flow  problems  one  has  to  "truncate" this  hierarchy  by  introducing  empiricisms.  If  we
                            use  empiricisms  for  the Reynolds  stresses,  we  then have  a  "first-order"  theory.  If we  in-
                            troduce  empiricisms  for  the  v'jVJvl,  we  then  have  a  "second-order  theory,"  and  so  on.
                            The  problem  of  introducing  empiricisms  to  get  a  closed  set  of  equations  that  can  be
                            solved  for  the velocity  and pressure  distributions  is referred  to as the "closure  problem."
                            The discussion  in  §5.4 deals  with  closure  at the first  order. At  the second  order  the  "k-E
                            empiricism"  has  been  extensively  studied  and  widely  used  in  computational  fluid
                            mechanics. 2


      §5.3  THE  TIME-SMOOTHED        VELOCITY    PROFILE   NEAR   A  WALL
                            Before  we  discuss  the various  empirical  expressions  used  for  the Reynolds  stresses,  we
                            present here several  developments  that do not depend  on any empiricisms.  We  are con-
                            cerned  here with  the fully  developed,  time-smoothed velocity  distribution  in the neigh-
                            borhood  of  a wall. We  discuss  several  results: a Taylor  expansion  of the velocity  near the
                            wall, and  the universal  logarithmic  and power  law  velocity  distributions  a little  further
                            out from  the wall.
                               The  flow  near  a  flat  surface  is  depicted  in  Fig.  5.3-1. It is  convenient  to  distinguish
                            four  regions  of  flow:

                               •  the viscous sublayer very near the wall, in which viscosity plays  a key  role
                               •  the  buffer layer  in  which  the  transition  occurs  between  the  viscous  and  inertial
                                 sublayers
                               •  the inertial sublayer at the beginning  of  the main turbulent stream, in which  viscos-
                                 ity plays  at most a minor role
                               •  the  main  turbulent  stream, in  which  the  time-smoothed  velocity  distribution  is
                                 nearly flat and viscosity is unimportant
                            It must be emphasized  that this classification  into regions  is somewhat  arbitrary.




                                 J. L. Lumley, Adv.  Appl. Mech., 18,123-176  (1978); С  G. Speziale, Ann.  Revs. Fluid Mech., 23,
                               2
                            107-157  (1991); H. Schlichting and  K. Gersten, Boundary-Layer Theory, Springer, Berlin, 8th edition (2000),
                            pp.  560-563.
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