Abstract
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.
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A.J. Harfash proposed the model, carried out the computations and drafted the introduction and the stability analysis results sections; A.J. Badday contributed to the sections namely Governing equations, linear instability and nonlinear stability. Both authors gave final approval for publication.
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Badday, A.J., Harfash, A.J. Double-Diffusive Convection in Bidispersive Porous Medium with Chemical Reaction and Magnetic Field Effects. Transp Porous Med 139, 45–66 (2021). https://doi.org/10.1007/s11242-021-01642-x
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DOI: https://doi.org/10.1007/s11242-021-01642-x