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MAGNETO-CONVECTION OF ALUMINA - WATER NANOFLUID WITHIN THIN HORIZONTAL LAYERS USING THE REVISED GENERALIZED BUONGIORNO'S MODEL

A.Wakifa,* , Z. Boulahiaa, A. Amineb , I.L. Animasaunc , M. I. Afridid, M. Qasimd , R. Sehaquia

a Hassan II University, Faculty of Sciences Aïn Chock, Laboratory of Mechanics, B.P.5366 Mâarif, 20100 Casablanca, Morocco.
b Hassan II University, Faculty of Sciences and Technology, Laboratory of Condensed Matter and Renewable Energy, Mohammedia, Morocco.
c Department of Mathematical Sciences, Federal University of Technology, Akure, Nigeria.
d Department of Mathematics, COMSATS University Islamabad (CUI), Park Road, Tarlai Kalan, Islamabad-455000, Pakistan.

* Corresponding Author: Email: email

Frontiers in Heat and Mass Transfer 2019, 12, 1-15. https://doi.org/10.5098/hmt.12.3

Abstract

The significance of an externally applied magnetic field and an imposed negative temperature gradient on the onset of natural convection in a thin horizontal layer of alumina-water nanofluid for various sizes of spherical alumina nanoparticles (e.g., 30

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, A., Amine, A., Qasim, M. (2019). MAGNETO-CONVECTION OF ALUMINA - WATER NANOFLUID WITHIN THIN HORIZONTAL LAYERS USING THE REVISED GENERALIZED BUONGIORNO'S MODEL. Frontiers in Heat and Mass Transfer, 12(1), 1–15.



cc This work is licensed under a Creative Commons Attribution 4.0 International License , which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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