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96 2. Introductory applications



          and this is completely determined, as is (2.106), so matching is used only to confirm
          the correctness of these results (and this is left as an exercise).
            The boundary layer near x = 0 is written in terms  of    with
                      again); equation (2.105) now becomes





          The boundary layer is, not surprisingly, the same size at this end of the domain:
          and then  with          we obtain




          A bounded solution, as    requires the choice   and       will ensure
          that the boundary  condition    is satisfied i.e.      The next  term
          in the asymptotic expansion                satisfies





          with       (for boundedness) and   (because        i.e.




          it is left as another exercise to confirm that this matches with (2.106).


          In our examples so far  (and see also  Q2.21,  2.22), the  character and position of the
          boundary layer (or its interior counterpart, the transition layer) have been controlled
          by the  known function a (x), as in   (or a (x) y in  our most  recent  example).
          We will now investigate how  the same  approach can be adopted when  the  relevant
          coefficient is a function of y. In this situation, we do not know, a priori, the sign of
          y—and this is usually critical. Typically, we make an appropriate assumption, seek a
          solution and then  test the  assumption. For example, if the  two boundary values for
          y—we are thinking here of two-point boundary value problems—have the same sign,
          then we may reasonably suppose that y retains this  sign  throughout the  domain. On
          the other  hand,  if the boundary  values are of opposite sign,  then the  solution must
          have at least one zero somewhere on the domain (and this indicates the existence of a
          transition layer).

          E2.18  A problem which exhibits either a boundary layer or a transition
                layer: I
          (An example similar to this one is discussed in great detail in Kevorkian & Cole,  1981
          & 1996; see Q2.23.)
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