Page 137 - Bird R.B. Transport phenomena
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122  Chapter 4  Velocity Distributions with  More Than One Independent Variable

                           pressure  by  taking  the  curl  of  the  equation  of  motion,  after  making  use  of  the  vector
                           identity  [v  •  Vv]  =  ^V(v  •  v)  -  [v  X  [V  X  v]], which  is  given  in  Eq. A.4-23.  For fluids  of
                           constant viscosity and density,  this operation gives

                                             4  [V  X v]  -  [V  X  [v  X  [V  X v]]]  =  X  v]  (4.2-1)
                                             ot
                           This  is  the  equation of  change for  the vorticity  [V  X  v];  two  other  ways  of  writing  it  are
                           given in Problem 3D.2.
                               For  viscous  flow  problems  one  can  then  solve  the  vorticity  equation  (a  third-order
                           vector  equation)  together  with  the  equation  of  continuity  and  the  relevant  initial  and
                           boundary  conditions  to  get  the  velocity  distribution.  Once  that  is  known,  the  pressure
                           distribution  can be  obtained  from  the Navier-Stokes  equation  in  Eq. 3.5-6. This  method
                           of  solving  flow  problems  is  sometimes  convenient  even  for  the  one-dimensional  flows
                           previously  discussed  (see, for  example, Problem  4B.4).
                               For  planar  or  axisymmetric  flows  the vorticity  equation  can be  reformulated  by  in-
                           troducing  the  stream function  ф. То  do  this, we  express  the  two  nonvanishing  compo-
                           nents  of  the velocity  as  derivatives  of  ф in  such  a way  that the equation  of  continuity  is
                           automatically  satisfied  (see  Table  4.2-1).  The component  of  the vorticity  equation  corre-
                           sponding  to the  direction  in  which  there  is  no  flow  then becomes  a  fourth-order  scalar
                           equation  for  ф. The  two  nonvanishing  velocity  components  can  then be  obtained  after
                           the  equation  for  the scalar  ф has  been  found.  The most  important problems  that can  be
                           treated in this way  are given in Table  4.1-I. 1
                               The stream  function  itself  is  not without  interest.  Surfaces  of  constant  ф contain the
                                     2
                           streamlines,  which  in  steady-state  flow  are  the paths  of  fluid  elements.  The  volumetric
                           rate  of  flow between  the surfaces  ф = ф  and  ф = ф  is proportional to ф  —  ф\.
                                                            х
                                                                      2
                                                                                       2
                               In  this  section  we  consider,  as  an example,  the steady,  creeping  flow  past  a  station-
                           ary  sphere, which  is described  by  the Stokes  equation  of  Eq. 3.5-8, valid  for  Re  < <  1  (see
                           the  discussion  right  after  Eq. 3.7-9).  For creeping  flow  the second  term on the left  side  of
                           Eq.  4.2-1  is  set  equal  to zero.  The equation  is  then linear,  and  therefore  there are  many
                           methods  available  for  solving  the problem.  3  We  use  the  stream  function  method  based
                           on  Eq. 4.2-1.

       EXAMPLE   4.2-1     Use  Table  4.2-1  to  set  up  the  differential  equation  for  the  stream  function  for  the  flow  of  a
                           Newtonian  fluid  around  a stationary  sphere  of  radius  R at  Re  <<  1. Obtain the velocity  and
      Creeping Flow  around  pressure  distributions  when  the fluid  approaches  the sphere  in the positive  z direction, as  in
      a Sphere             Fig. 2.6-1.



                               1  For a technique applicable to more general flows, see J. M. Robertson, Hydrodynamics in Theory and
                           Application, Prentice-Hall, Englewood  Cliffs,  N.J. (1965), p. 77; for examples  of three-dimensional flows
                           using two stream functions, see Problem 4D.5 and also J. P. Sorensen and W. E. Stewart, Chem.  Eng. Sci.,
                           29, 819-825  (1974). A. Lahbabi and H.-C. Chang, Chem. Eng. Sci., 40, 434^47  (1985) dealt with high-Re
                           flow through cubic arrays  of spheres, including steady-state  solutions and transition to turbulence.
                           W. E. Stewart and M. A. McClelland, AIChE Journal, 29, 947-956 (1983) gave matched asymptotic
                           solutions  for forced  convection in three-dimensional flows with viscous  heating.
                                See, for example, G. K. Batchelor, An Introduction to Fluid Dynamics, Cambridge University  Press
                               2
                           (1967), §2.2. Chapter 2 of this book is an extensive  discussion  of the kinematics  of fluid motion.
                                The solution given here follows that given by L. M. Milne-Thomson, Theoretical Hydrodynamics,
                               3
                           Macmillan, New York, 3rd edition (1955), pp. 555-557.  For other approaches, see H. Lamb, Hydrodynamics,
                           Dover, New York (1945), §§337, 338. For a discussion  of unsteady flow around a sphere, see R. Berker, in
                           Handbuch der Physik, Volume  VIII-2, Springer, Berlin  (1963), §69; or H. Villat and J. Kravtchenko,
                           Leqons sur les Fluides Visqueux, Gauthier-Villars, Paris (1943), Chapter VII. The problem of finding the
                           forces and torques on objects  of arbitrary  shapes is discussed  thoroughly by S. Kim and S. J. Karrila,
                           Microhydrodynamics: Principles and Selected Applications, Butterworth-Heinemann, Boston (1991), Chapter II.
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