The stability of a conducting fluid saturating a porous medium, in the
presence of a uniform magnetic field, is investigated using the Brink
man model. In the first part of the paper constant-flux thermal bounda
ry conditions are considered for which the onset of convection is know
n to correspond to a vanishingly small wave number. The external magne
tic field is assumed to be aligned with gravity. Closed form solutions
are obtained, based on a parallel flow assumption, for a porous layer
with either rigid-rigid, rigid-free or free-free boundaries. In the s
econd part of the paper, the linear stability of a porous layer, heate
d isothermally from below, is investigated using the normal mode techn
ique. The external mag- netic field is applied either vertically or ho
rizontally. Solutions are obtained for the case of a porous layer with
free boundar- ies. Results for a pure viscous fluid and a Darcy (dens
ely packed) porous medium emerge from the present analysis as limiting
cases.