Page 137 - Aerodynamics for Engineering Students
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120  Aerodynamics for Engineering Students

                   Method (see Fig. 3.14)
                   (1) Plot the streamlines due to a source at the origin taking the strength of the source
                      equal to 20m2s-'  (say). The streamlines are n/lO apart. It is necessary to take
                      positive values of y only since the pattern is symmetrical about the Ox axis.
                   (2)  Superimpose  on  the  plot  horizontal  lines  to  a  scale  so  that  1c, = -Uy  = -1,
                      -2,  -3,  etc., are lines about 1 unit apart on the paper. Where the lines intersect,
                      add the values of 1c, at the lines of intersection. Connect up all points of constant 1c,
                      (streamlines) by smooth lines.
                     The resulting flow pattern shows that the streamlines can be separated into two
                   distinct groups: (a) the  fluid  from  the  source moves  from the  source to  infinity
                   without mingling with the uniform stream, being constrained within the streamline
                   1c, = 0; (b) the uniform stream is split along the Ox axis, the two resulting streams
                   being deflected in their path towards infinity by 1c, = 0.
                     It is possible to replace any streamline by a solid boundary without interfering with
                   the flow in any way. If 1c, = 0 is replaced by a solid boundary the effects of the source
                   are truly cut off from the horizontal flow and it can be seen that here is a mathem-
                   atical expression that represents the flow round a curved fairing (say) in a uniform
                   flow. The same expression can be used for an approximation to the behaviour of a
                   wind sweeping in off a plain or the sea and up over a cliff. The upward components
                   of velocity of such an airflow are used in soaring.
                     The vertical velocity component at any point in the flow is given by -a$/ax.  Now




                                              -  m atan-lb/x)  ab/.)
                                           &!J
                                         ___--
                                           ax    2n  ab/.)       ax







                                            9 due  to  source  at origin

















                                         9 of combination streamlines

                   Fig. 3.14
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