Three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip
In this paper, the problem of a steady laminar three-dimensional stagnation point boundary layer flow on a permeable moving surface with anisotropic slip in a viscous fluid is investigated. A similarity transformation reduces the governing system of nonlinear partial differential equations into the...
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AIP Publishing LLC
2015
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my.upm.eprints.576412017-10-24T08:44:34Z http://psasir.upm.edu.my/id/eprint/57641/ Three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip Hafidzuddin, Mohd Ezad Hafidz Mohd Nazar, Roslinda Md. Arifin, Norihan Pop, Ioan In this paper, the problem of a steady laminar three-dimensional stagnation point boundary layer flow on a permeable moving surface with anisotropic slip in a viscous fluid is investigated. A similarity transformation reduces the governing system of nonlinear partial differential equations into the ordinary (similarity) differential equations. The resulting equations are then solved numerically by using the bvp4c function in Matlab. The effects of surface mass transfer parameter, slip parameter, ratio of slip factors and moving parameter on the fluid flow characteristics are presented in the forms of tables and figures and are discussed in details. AIP Publishing LLC 2015 Conference or Workshop Item PeerReviewed application/pdf en http://psasir.upm.edu.my/id/eprint/57641/1/Three-dimensional%20stagnation%20point%20viscous%20flow%20on%20a%20permeable%20moving%20surface%20with%20anisotropic%20slip.pdf Hafidzuddin, Mohd Ezad Hafidz and Mohd Nazar, Roslinda and Md. Arifin, Norihan and Pop, Ioan (2015) Three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip. In: 2015 UKM FST Postgraduate Colloquium, 15-16 Apr. 2015, Faculty of Science and Technology, Universiti Kebangsaan Malaysia. (pp. 1-7). 10.1063/1.4931347 |
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In this paper, the problem of a steady laminar three-dimensional stagnation point boundary layer flow on a permeable moving surface with anisotropic slip in a viscous fluid is investigated. A similarity transformation reduces the governing system of nonlinear partial differential equations into the ordinary (similarity) differential equations. The resulting equations are then solved numerically by using the bvp4c function in Matlab. The effects of surface mass transfer parameter, slip parameter, ratio of slip factors and moving parameter on the fluid flow characteristics are presented in the forms of tables and figures and are discussed in details. |
format |
Conference or Workshop Item |
author |
Hafidzuddin, Mohd Ezad Hafidz Mohd Nazar, Roslinda Md. Arifin, Norihan Pop, Ioan |
spellingShingle |
Hafidzuddin, Mohd Ezad Hafidz Mohd Nazar, Roslinda Md. Arifin, Norihan Pop, Ioan Three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip |
author_facet |
Hafidzuddin, Mohd Ezad Hafidz Mohd Nazar, Roslinda Md. Arifin, Norihan Pop, Ioan |
author_sort |
Hafidzuddin, Mohd Ezad Hafidz |
title |
Three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip |
title_short |
Three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip |
title_full |
Three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip |
title_fullStr |
Three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip |
title_full_unstemmed |
Three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip |
title_sort |
three-dimensional stagnation point viscous flow on a permeable moving surface with anisotropic slip |
publisher |
AIP Publishing LLC |
publishDate |
2015 |
url |
http://psasir.upm.edu.my/id/eprint/57641/1/Three-dimensional%20stagnation%20point%20viscous%20flow%20on%20a%20permeable%20moving%20surface%20with%20anisotropic%20slip.pdf http://psasir.upm.edu.my/id/eprint/57641/ |
_version_ |
1643836547820158976 |
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13.251813 |