Double-Diffusive Convection in Bidispersive Porous Medium with Chemical Reaction and Magnetic Field Effects

This study features a model for double-diffusive convection in a bidisperse porous medium where a vertical magnetic field chemical reaction’s effects are present. Double-diffusive convection is the convective motion of fluid resulting from temperature and salt gradient effects. A bidisperse porous medium is one in which there exist pores known as macropores. Furthermore, the solid skeleton has cracks or fissures which give rise to a porosity within the skeleton, called microporosity. The emphasis here is on the situation of a single temperature field where the layer is heated from below and simultaneously salted from above to below.