An analysis is made of the unsteady mixed convection from a vertical flat p
late embedded in a fluid-saturated porous medium. For time t < 0 a uniform
free stream velocity U exists parallel to the plate surface and the tempera
ture T-infinity throughout the porous medium is uniform. Then at time t = 0
the temperature on the surface is instantaneously changed from the ambient
fluid temperature T-infinity to T-w. At small times the transport effects
are confined within a narrow layer adjacent to the plate. As this inner bou
ndary layer evolves, a steady boundary layer is approached but far from the
plate the ambient conditions remain. A complete analysis is made of the go
verning equations at t = 0, the steady state at large times and a series so
lution valid at small times is derived. A numerical solution of the full bo
undary-layer equations is then obtained for the whole transient from t = 0
to the steady state. Results are presented to illustrate the occurrence of
transients when the buoyancy parameter is positive (buoyancy and free strea
m forces in the same direction) and negative (buoyancy and free stream forc
es in opposing directions). The uniqueness of this problem lies in the fact
that we have been able to match significantly different profiles at the ti
me when the forward integration approach breaks down and the solution at la
rge times and establish a smooth evolution around the transition time. (C)
1998 Elsevier Science Ltd. All rights reserved.