Mixed Convection Boundary Layer Flow Near the Stagnation Point on a Vertical Surface Embedded in a Porous Medium with Anisotropy Effect

被引:18
|
作者
Bachok, Norfifah [2 ]
Ishak, Anuar [1 ]
Pop, Ioan [3 ]
机构
[1] Univ Kebangsaan Malaysia, Sch Math Sci, Bangi 43600, Selangor, Malaysia
[2] Univ Putra Malaysia, Fac Sci, Dept Math, Serdang 43400, Selangor, Malaysia
[3] Univ Cluj, Fac Math, Cluj Napoca 3400, Romania
关键词
Mixed convection; Stagnation point flow; Porous medium; Dual solutions; Anisotropy; OBLIQUE PRINCIPAL AXES; THERMAL-CONVECTION; NATURAL-CONVECTION; BRINKMAN MODEL; PERMEABILITY;
D O I
10.1007/s11242-009-9431-0
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
The steady boundary-layer flow near the stagnation point on a vertical flat plate embedded in a fluid-saturated porous medium characterized by an anisotropic permeability is investigated. Using appropriate similarity transformation, the governing system of partial differential equations is transformed into a system of ordinary differential equations. This system is then solved numerically. The features of the flow and the heat transfer characteristics for different values of the governing parameters, namely, the modified mixed convection parameter I >, and the anisotropy parameter A are analyzed and discussed. It is found that dual solutions exist for both assisting and opposing flows. Moreover, the range of I > for which the solution exists increases with A.
引用
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页码:363 / 373
页数:11
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