The Darcy model with the Boussinesq approximation is used to study double-diffusive natural convection in a shallow porous cavity. The horizontal walls are subject to uniform fluxes of heat and mass, while the side vertical walls are exposed to a constant heat flux of intensity aq ', where a is a real number. Results are presented for -20 less than or equal to R-T less than or equal to 50, -20 less than or equal to R-S less than or equal to 20, 5 less than or equal to Le less than or equal to 10, 4 less than or equal to A less than or equal to 8 and -0.7 less than or equal to a less than or equal to 0.7, where RT, Rs, Le and A correspond to thermal Rayleigh number, solutal Rayleigh number, Lewis number and aspect ratio of the enclosure, respectively. In the limit of a shallow enclosure (A much greater than 1) an asymptotic analytical solution for the stream function and temperature and concentration fields is obtained by using a parallel flow assumption in the core region of the cavity and an integral form of the energy and the constituent equations. In the absence of side heating (a = 0), the solution takes the form of a standard Benard bifurcation. The asymmetry brought by the side heating (a not equal 0) to the bifurcation is investigated. For high enough Rayleigh numbers, multiple steady states near the threshold of convection are found. These states represent flows in opposite directions. In the range of the governing parameters considered in the present study, a good agreement is observed between the analytical predictions and the numerical simulations of the full governing equations.