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          as measured in terms  of   then the flow away from the wall is t =  1, with only
          exponentially small corrections. The  boundary  layer  remains  thin   along
          the full  length  of the pipe,  but note  that  lines of constant temperature, emanating
          from the  neighbourhood of the wall, are  the lines     i.e.
          Thus, defining the boundary-layer thickness in terms of a particular temperature, this
          thickness increases as x increases, although it remains    However,
          if the pipe is so long that    then  the  exponential  term in  (3.59)  becomes
          O(1), and the temperature now has an O(1) correction. In other words, the O(1)
          temperature at the pipe  wall has  caused heat to be  conducted  through the  fluid to
          affect the whole pipe flow,   Indeed, we see that the scaling  in our
          original equation, (3.53), balances dominant terms from both sides of the equation for
                   there is no longer a boundary layer at the wall; this is shown schematically
          in figure  5.



          The two  examples  presented  above have  shown how the  notion  of a  boundary
          layer, as developed for ordinary differential equations, is relevant to partial differen-
          tial  equations—and essentially without any adjustment to  the method;  some similar
          examples can  be  found in  exercises Q3.12–3.14. We  have  now  seen the two  basic
          types of problem (breakdown and rescale; select a scaling relevant to a layer), although
          the equations that we have introduced as the vehicles for these demonstrations—quite
          deliberately—have been relatively uncomplicated. We conclude this section with an
          example that,  ultimately, possesses a simple perturbation structure  (as in §3.2), but
          which involves a set of four,  coupled, nonlinear partial differential equations. As be-
          fore, the purpose of the example is to exhibit the power (and inherent simplicity) of
          the singular perturbation approach.

          E3.5  Unsteady, one-dimensional flow of a viscous, compressible gas
          The flow of a compressible gas, with temperature variations and viscosity, is described
          by the equations













          which are the equations of momentum, mass conservation,  energy and state, respec-
          tively. Here,  is  the  coefficient of (Newtonian) viscosity,  the  thermal conductivity,
             the gas constant and   is associated with the isentropic-gas model (see E3.2); we
          shall take all these parameters to be  constant.  Any movement of the gas is in  the
          direction—we use primes here to denote physical variables—with no variation in other
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