Thermogravitational Convection in a Controlled Rotating Darcy-Brinkman Nanofluids Layer Saturated in an Anisotropic Porous Medium Subjected to Internal Heat Source

Thermogravitational convection in a controlled rotating Darcy-Brinkman nanofluids layer saturated in an anisotropic porous medium heated from below is investigated. The presence of a uniformly distributed internal heat source and considers the Brinkman model for different boundary conditions: rigid-...

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Bibliographic Details
Published in:Journal of Advanced Research in Numerical Heat Transfer
Main Author: Khalid I.K.; Mohd Mokhtar N.F.; Zainal Abidin N.H.
Format: Article
Language:English
Published: Penerbit Akademia Baru 2023
Online Access:https://www.scopus.com/inward/record.uri?eid=2-s2.0-85186895371&doi=10.37934%2farnht.14.1.7090&partnerID=40&md5=9bb979ace9b916cddf4d8a1345bc616e
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Summary:Thermogravitational convection in a controlled rotating Darcy-Brinkman nanofluids layer saturated in an anisotropic porous medium heated from below is investigated. The presence of a uniformly distributed internal heat source and considers the Brinkman model for different boundary conditions: rigid-rigid, free-free, and lower-rigid and upper-free are considered. The effect of a control strategy involving sensors located at the top plate and actuators positioned at the bottom plate of the nanofluids layer is analysed. Linear stability analysis based on normal mode technique is employed. The resulting eigenvalue problem is solved numerically using the Galerkin method implemented with Maple software. The model used for the nanofluids associates with the mechanisms of Brownian motion and thermophoresis. The influences of the internal heat source strength, mechanical anisotropy parameter, modified diffusivity ratio, nanoparticles concentration Darcy-Rayleigh number and nanofluids Lewis number are found to advance the onset of convection. Conversely, the Darcy number, thermal anisotropy parameter, porosity, rotation, and controller effects are observed to slow down the process of convective instability. © 2023, Penerbit Akademia Baru. All rights reserved.
ISSN:27350142
DOI:10.37934/arnht.14.1.7090