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FORCED CONVECTION BOUNDARY LAYER STAGNATION-POINT FLOW IN DARCY-FORCHHEIMER POROUS MEDIUM PAST A SHRINKING SHEET

Shahirah Abu Bakara, Norihan Md. Arifina,*, Roslinda Nazarb, Fadzilah Md. Alia, Ioan Popc

a Department of Mathematics & Institute For Mathematical Research, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor, Malaysia.
b Faculty of Science and Technology, Universiti Kebangsaan Malaysia, 43600 UKM Bangi, Selangor, Malaysia.
c Department of Mathematics, Babes-Bolyai University, R-400084 Cluj-Napoca, Romania

* Corresponding Author: Email: email

Frontiers in Heat and Mass Transfer 2016, 7, 1-6. https://doi.org/10.5098/hmt.7.38

Abstract

A mathematical model of forced convection boundary layer stagnation-point slip flow in Darcy-Forchheimer porous medium over a shrinking sheet is presentedin this paper. The governing partial differential equations are transformed into ordinary differential equation using self-similarity transformation which are then solved numerically with shooting method. A parametric study of the physical parameters involved in the problem is conducted and representative set of numerical results are presented through graphs and tables, and are discussed.

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Cite This Article

Bakara, S. A., Arifin, N. M., Nazar, R., Ali, F. M., Pop, I. (2016). FORCED CONVECTION BOUNDARY LAYER STAGNATION-POINT FLOW IN DARCY-FORCHHEIMER POROUS MEDIUM PAST A SHRINKING SHEET. Frontiers in Heat and Mass Transfer, 7(1), 1–6.



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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