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76  Aerodynamics for Engineering Students
















                   Fig. 2.17


                    All other points Pz, P3, etc. which have a stream function equal in value to that of P
                   have, by definition, the same flow across any lines joining them to 0, so by the same
                   argument the velocity of the flow in the region of PI, Pz, P3, etc. must be along PP1,
                   Pz,  P3,  etc.,  and  no  fluid  crosses  the  line  PP1, P2,. . .,P,.  Since  $pl  = h2 =
                   1clp3 = +p  = constant, the line PP1, Pz, . . . P,,  etc. is a line of constant $ and is called
                   a streamline. It follows further that since no flow can cross the line PP,  the velocity
                   along the line must always be in the direction tangential to it. This leads to the two
                   common definitions of a streamline, each of which indirectly has the other’s meaning.
                   They are:

                       A streamline is a line of constant $

                   and/or
                       A streamline  is  a  line  of  fluid  particles,  the  velocity  of  each  particle being
                       tangential to the line (see also Section 2.1.2).
                   It should be noted that the velocity can change in magnitude along a streamline but
                   by definition the direction is always that of the tangent to the line.
                   2.5.3  Velocity components in terms of w

                   (a) In Cartesian coordinates Let point P(x, y) be on the streamline AB in Fig. 2.18a
                   of  constant $ and point  Q(x + Sx, y + Sy) be  on  the  streamline CD  of  constant
                   $ + S$. Then from the definition of  stream function, the amount of  fluid flowing
                   across any path  between  P  and Q = S$,  the change of  stream function between
                   P and Q.
                     The most convenient path along which to integrate in this case is PRQ, point R
                   being given by  the coordinates (x + Sx, y). Then the flow across PR = -vSx  (since
                   the flow is from right  to left and thus by  convention negative), and that across
                   RQ = uSy. Therefore, total flow across the line PRQ is

                                                S$ = uSy - VSX                        (2.55)
                     Now $ is a function of two independent variables x and y in steady motion, and thus
                                                   a$     a$
                                              S$ = -Sx  + -Sy                         (2.56)
                                                   ax      ay
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