Abstract
The onset of thermal convection in an Ellis fluid-saturated porous medium in the presence of a horizontal pressure gradient yielding a basic throughflow and subject to a lack of thermal equilibrium between the fluid and solid phases is investigated. The eigenvalue problem is solved analytically and the condition for the onset of convection is obtained. It is found that the instability sets in as oscillatory mode contrary to the manifestation of stationary convection in a Newtonian fluid-saturated porous layer. The effects of local thermal nonequilibrium and Ellis fluid parameters are discussed on the onset of convection. It is found that an increase in the Ellis power-law index and the scaled interphase heat transfer coefficient is to delay the onset of convection, while an opposite behaviour is observed with an increase in the Darcy–Ellis number and the porosity-modified conductivities ratio. The pressure lines and isotherms are presented at the critical state. The results delineated under the limiting cases are shown to be in excellent agreement with those published previously.
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Shivakumara, I.S., Raghunatha, K.R., Dhananjaya, M. et al. Lack of Thermal Equilibrium Effects on Convection in a Porous Medium saturated with an Ellis Fluid. Transp Porous Med 146, 703–720 (2023). https://doi.org/10.1007/s11242-022-01881-6
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DOI: https://doi.org/10.1007/s11242-022-01881-6