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CONCEPTS. DEFINITIONS AND METHODS                    29

                (f) Turbulent flows
               Due to a three-dimensional instability of laminar flow, the flow  field becomes turbulent:
               the  flow  velocity  and  pressure  are  no  longer  steady but  contain  randomly  fluctuating
               components. Two-dimensional disturbances in the laminar flow field eventually become
               three-dimensional, and this is soon followed by  turbulence. The critical Reynolds number
               for the onset of turbulence is best stated in terms of the width of the flow’  and depends on
               the shape of the laminar velocity profile; it is typically O( lo2) for profiles with inflection
               points  and  6(103) or  more  for  profiles  of  single curvature. Thus,  boundary  layers  in
               falling pressures are a good deal more stable than those that are suffering a pressure rise;
               similarly, jets and wakes are also very unstable.
                 When turbulence appears, as originally observed and described by  Reynolds for pipe
               flow, the flow field may be expressed as V + v and P + p, where the lower-case quantities
               represent the fluctuating components about the mean (with zero average) and V and P are
               the mean components; V = (VI, U2, U3}T and v = (u1, u2, ~  3  in  )an  ~(XI, x2, x3)-frame.
               Substitution into the Navier-Stokes  equations and averaging yields
                     au;     au;     1  ap       v  --E ,,),
                     -+u                  +- a                     i,j=l,2,3,       (2.85)
                      at     ax,     p  ax;  ax,    axj

               where the indicia1 notation is utilized, in  which repeated indices imply summation; e.g.
                                                                 is
                Uj(aUj/axj) = E&, [Uj(aUj/axj)]. The  new  term  -q the  correlation  of  ui  and
               ii,,  obtained  by  multiplying the  two,  integrating over  a  long  time  (appropriate to  the
               flow under investigation), and  then dividing by  the time  interval. The quantity  --pW
               represents  additional  normal  and  shear  stresses due  to  additional momentum  transfer
               associated  with  the  velocity  fluctuations,f the  so-called Reynolds  stresses.  Thus,  in  a
               simple two-dimensional shear flow predominantly in the XI -direction, the viscous shearing
               stress p(aUl/axz) is increased by  -pm, which has the same sign as aUl/ax2  and is
               sometimes written  as p,(aUl/axz), where the subscript t  is for  ‘turbulence’; ut  = pr/p
               is the  so-called kinematic eddy viscosity.  To  differentiate the quantities associated with
               viscous stresses from those related to turbulence, or equivalently the quantities associated
               with velocity fluctuations at the molecular (Brownian) scale from the turbulent ones, the
               subscript m  (for  ‘molecular’) is  introduced, as in  u,  in equation (2.85); v,  here is the
               same as u in equation (2.63).
                 The  Reynolds stresses are generally much  larger than  the  viscous ones, except  near
               walls, in the viscous sublayer (Hinze  1975); on  the wall  itself, all turbulent fluctuations
               vanish. One of  the central problems of  turbulent  flows is  the derivation of  satisfactory
               relations for Reynolds stresses in terms of  the mean flow field (Townsend 1961).
                 The spatial structure of a turbulent flow may be described statistically by  correlation
               functions or by  spectra. The general space-time correlation function between, say, u; at
               point x and uj at point x + r is defined by




                 ‘The  width of  a jet or a wake, or the  thickness of a boundary layer.
                 *This is an essential characteristic of turbulence. As noted by Townsend (1961). ‘a sharp increase in friction,
               or in heat and mass transfer is frequently used to determine the onset of turbulent motion if direct observation
               of  the fluctuations is inconvenient’.
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