Published online by Cambridge University Press: 21 April 2006
A model problem is solved mathematically in order to clarify how an essential singularity, which is an integral part of the boundary-layer solution of a time-dependent convective–diffusive system, is removed by the inclusion of the effect of longitudinal diffusion. The model problem involves a uniform velocity field along a plane boundary at which boundary conditions of a mixed type are prescribed. The problem is solved by means of a method involving the Laplace transform and the Wiener–Hopf technique. An exact solution is presented.
Special attention is given to an asymptotic solution that is valid for large values of the dimensionless time. It is shown that the large-time asymptote and the naïve boundary-layer solution are close approximations of one another, except in the neighbourhood of the location where the latter is singular. Around this point the present solution provides an interlayer which matches smoothly the purely time-dependent Rayleigh-like and the stationary components of the boundary-layer approximation.