Physics of Fluids · 2024 · 35 citations · 42 references
EngineeringChemical EngineeringMechanical EngineeringDifferential EquationsFluid DynamicsHeat TransferConvection DynamicsDarcy FlowFlow StabilityHeat Transfer In FluidsMass TransferThermal Boundary LayersCasson Fluid FlowConvectionConvective Heat TransferNonlinear StabilityNonlinear Stability TheoryOscillatory FlowOscillatory PatternsThermohaline Convection
In this effort, the consequence of chemical reaction on the thermohaline convection in a permeable layer containing Casson fluid is inspected utilizing both linear and nonlinear stability procedures. To model the momentum equation, the Casson fluid version of Darcy's law is utilized. Applying the linear stability concept, the situation for the start of stationary and oscillatory pattern of convective motion is obtained, whereas the convective heat and mass transferences are determined using nonlinear stability theory. It is found that the oscillatory type of convective flow is probable only if the evaluation of the solutal Rayleigh–Darcy number is less than zero. The effect of the chemical reacting factor, the Casson factor, the Lewis number, and the solutal Rayleigh–Darcy number is to hurry the start of convection toward both stationary and oscillatory styles of convection and also surge the size of the convective cells. The convective heat and mass transfers enhance with increasing the Casson factor, the solutal and thermal Rayleigh–Darcy numbers while both decrease with enhancing the heat capacity quotient. The effect of chemical reacting factor is to increase the mass transmission in the system, while it has no effect on the heat transmission. It is also noted that the convective heat and mass transfers in the system enhance nearly 5.4% and 3.8%, respectively, with a 50% increase in the value of Casson factor.
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Convection Currents in a Porous Medium
C. W. Horton, F. T. Rogers · Journal of Applied Physics · 1945 · 942 citations
Engineering, Earth Sciences, Computational Fluid Dynamics +12
Onset of Thermohaline Convection in a Porous Medium
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