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MHD natural convection in a square porous cavity filled with a water-based magnetic fluid in the presence of geothermal viscosity

Mikhail A. Sheremet (Laboratory on Convective Heat and Mass Transfer, Tomsk State University, Tomsk, Russia)
Marina S. Astanina (Laboratory on Convective Heat and Mass Transfer, Tomsk State University, Tomsk, Russia)
Ioan Pop (Department of Applied Mathematics, Babeş-Bolyai University, Cluj-Napoca, Romania)

International Journal of Numerical Methods for Heat & Fluid Flow

ISSN: 0961-5539

Article publication date: 28 September 2018

Issue publication date: 19 October 2018

116

Abstract

Purpose

The purpose of this paper is a numerical analysis of natural convection in a square porous cavity filled with a water-based magnetic fluid of geothermal viscosity under the effect of inclined uniform magnetic field.

Design/methodology/approach

The domain of interest includes the square porous cavity filled with a water-based magnetic fluid (W40). Horizontal walls are supposed to be adiabatic, while right vertical wall is kept at constant low temperature and left vertical wall is kept at constant high temperature. An inclined uniform magnetic field affects the fluid flow and heat transfer inside the cavity. The viscosity of the working fluid is proportional to the linearly decreasing function of depth (vertical coordinate) and inversely proportional to the linear function of temperature. It is assumed in the analysis that the flow is laminar. The fluid is Newtonian and the Boussinesq approximation is valid. The governing equations have been discretized using the finite difference method with the uniform grid. Simulations have been carried out for different values of the Rayleigh number, Hartmann number, Darcy number, magnetic field inclination angle and viscosity variation parameters.

Findings

It has been revealed that an increase in the viscosity parameters leads to the heat transfer enhancement and convective flow intensification. At the same time, this intensification is more essential for high values of the Rayleigh number.

Originality/value

The originality of this work is to analyze MHD natural convection in a square porous cavity filled with a water-based magnetic fluid of geothermal viscosity. The results would benefit scientists and engineers to become familiar with the analysis of convective heat and mass transfer in nanofluids, and the way to predict the properties of nanofluid convective flow in advanced technical systems, in industrial sectors including transportation, power generation, chemical sectors and electronics.

Keywords

Citation

Sheremet, M.A., Astanina, M.S. and Pop, I. (2018), "MHD natural convection in a square porous cavity filled with a water-based magnetic fluid in the presence of geothermal viscosity", International Journal of Numerical Methods for Heat & Fluid Flow, Vol. 28 No. 9, pp. 2111-2131. https://doi.org/10.1108/HFF-12-2017-0503

Publisher

:

Emerald Publishing Limited

Copyright © 2018, Emerald Publishing Limited

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