Page 111 - Aerodynamics for Engineering Students
P. 111

94  Aerodynamics for Engineering  Students

                  becomes important (see Section 2.3.4), Mach number becomes a second dimension-
                  less quantity characterizing the flow field.
                    The Navier-Stokes  equations are deceptively simple in form, but at high Reynolds
                  numbers the resulting flow fields can be exceedingly complex even for simple geo-
                  metries. This is basically a consequence of the behaviour of the regions of vortical
                  flow at high Reynolds number. Vorticity can only be created in a viscous flow and
                  can be regarded as a marker for regions where the effects of viscosity are important in
                  some sense.
                    For  engineering applications of  aerodynamics the  Reynolds numbers are  very
                  large, values well in excess of lo6 are commonplace. Accordingly, one would expect
                  that to a good approximation one could drop the viscous terms on the right-hand
                  side of the dimensionless Navier-Stokes  Eqns (2.100). In general, however, this view
                  would be mistaken and one never achieves a flow field similar to the inviscid one no
                  matter how high the Reynolds number. The reason is that the regions of non-zero
                  vorticity where viscous effects cannot be neglected become confined to exceedingly
                  thin boundary layers adjacent to the body surface. As Re + oc the boundary-layer
                  thickness, 6 + 0. If the boundary layers remained attached to the surface they would
                  have little effect beyond giving rise to skin-friction drag. But in all real flows the
                  boundary layers separate from the surface of the body, either because of the effects of
                  an adverse pressure gradient or because they reach the rear of the body or its trailing
                  edge. When these thin regions of vortical flow separate they form complex unsteady
                  vortex-like structures in the wake. These take their most extreme form in turbulent
                  flow which is characterized by vortical structures with a wide range of length and
                  time scales.
                    As we have seen from the discussion given above, it is not necessary to solve the
                  Navier-Stokes  equations in order to obtain useful information from them. This is
                  also illustrated by following example:
                  Example 2.3  Aerodynamic modelling
                  Let us suppose that we are interested carrying out tests on a model in a wind-tunnel in order to
                  study and determine the aerodynamic forces exerted on a motor vehicle travelling at normal
                  motorway speeds. In this case the speeds are sufficiently  low to ensure that  the effects  of
                  compressibility are negligible. Thus for a fixed geometry the flow field will be characterized
                  only by Reynolds number.* In this case we can use U,,  the speed at which the vehicle travels
                  (the air speed in the wind-tunnel working section for the model) as the reference flow speed,
                  and L can be the width or length of the vehicle. So the Reynolds number Re   pU,L/p.  For
                  a  fixed  geometry it  is  clear  from Eqns  (2.99)  and  (2.100) that the  non-dimensional flow
                  variables, U, V, W, and P are functions only of the dimensionless coordinates X: Y, 2: T,
                  and the dimensionless quantity, Re. In a steady flow the aerodynamic force, being an overall
                  characteristic of the flow field, will not depend on X, Y, Z, or T. It will, in fact, depend only
                  on Re. Thus if we make an aerodynamic force, drag (0) say, dimensionless, by introducing
                  a force (i.e. drag) coefficient defined as

                                                                                     (2.102)

                  (see Section 1.5.2 and noting that here we have used Lz in place of area S) it should be clear
                  that
                                       Co = F(Re)  i.e. a function of Re only        (2.103)


                  * In fact, this statement is somewhat of an over-simplification. Technically the turbulence characteristics of
                  the oncoming flow also influence the details of the flow field.
   106   107   108   109   110   111   112   113   114   115   116