Ferroconvection in an Anisotropic Porous Medium with Variable Gravity

Authors

  • Nor Halawati Senin Laboratory of Computational Sciences and Mathematical Physics, Institute for Mathematical Research (INSPEM), Universiti Putra Malaysia, Malaysia
  • Nor Fadzillah Mohd Mokhtar Centre of Foundation Studies for Agricultural Science, Universiti Putra Malaysia, Malaysia
  • Mohamad Hasan Abdul Sathar Centre of Foundation Studies for Agricultural Science, Universiti Putra Malaysia, Malaysia

Keywords:

Ferrofluid, Anisotropic, Variable Gravity

Abstract

A linear stability assessment was performed to study the impact of internal heating and variable gravity in an anisotropic porous medium of a ferrofluid layer system on the onset of Benard-Marangoni convection. The system is heated from below with both the lower and upper limits are considered as completely insulated to the disturbance of the temperature. The eigenvalue problem is solved by using regular perturbation technique to obtain the critical Marangoni number and also the critical thermal Rayleigh number. It is noted that the increase of value anisotropic permeability, Darcy number and also magnetic number will enhance the convection of the system while the increasing values of anisotropic thermal diffusivity will help to stabilize the system.

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Published

2024-03-28

How to Cite

Nor Halawati Senin, Nor Fadzillah Mohd Mokhtar, & Mohamad Hasan Abdul Sathar. (2024). Ferroconvection in an Anisotropic Porous Medium with Variable Gravity. Journal of Advanced Research in Fluid Mechanics and Thermal Sciences, 71(2), 56–68. Retrieved from https://semarakilmu.com.my/journals/index.php/fluid_mechanics_thermal_sciences/article/view/6283

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