Effect of partial slip on an unsteady MHD mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet

The objective of the present study was to investigate the partial slip effect on an unsteady two-dimensional mixed convection stagnation point flow towards a permeable shrinking sheet. The governing equations are reduced to a system of non-dimensional partial differential equations using a semi-simi...

Full description

Saved in:
Bibliographic Details
Main Authors: Aurangzaib, Aurangzaib, Bhattacharyya, Krishnendu, Shafie, Sharidan
Format: Article
Published: Elsevier 2016
Subjects:
Online Access:http://eprints.utm.my/id/eprint/69292/
http://dx.doi.org/10.1016/j.aej.2016.04.018
Tags: Add Tag
No Tags, Be the first to tag this record!
Institution: Universiti Teknologi Malaysia
id my.utm.69292
record_format eprints
spelling my.utm.692922017-11-22T00:45:09Z http://eprints.utm.my/id/eprint/69292/ Effect of partial slip on an unsteady MHD mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet Aurangzaib, Aurangzaib Bhattacharyya, Krishnendu Shafie, Sharidan QA Mathematics The objective of the present study was to investigate the partial slip effect on an unsteady two-dimensional mixed convection stagnation point flow towards a permeable shrinking sheet. The governing equations are reduced to a system of non-dimensional partial differential equations using a semi-similarity transformation, before being solved numerically by using Keller-box method. The features of the flow characteristics for different values of the governing parameters are analysed and discussed. The results indicate that the momentum, thermal and concentration boundary layer thicknesses increase with increasing mixed convection parameter for opposing flow, whereas the opposite effect is observed for assisting flow. The results also show that the surface velocity is higher when there is slip at a sheet compared to its absent. Further, the study indicates that the boundary layer thicknesses become thicker and thicker with increasing shrinking parameter, while the opposite effect is observed with increasing Hartmann number. Comparison with previously published work for special cases is performed and found to be in excellent agreement. Elsevier 2016 Article PeerReviewed Aurangzaib, Aurangzaib and Bhattacharyya, Krishnendu and Shafie, Sharidan (2016) Effect of partial slip on an unsteady MHD mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet. Alexandria Engineering Journal, 55 (2). pp. 1285-1293. ISSN 1110-0168 http://dx.doi.org/10.1016/j.aej.2016.04.018 DOI:10.1016/j.aej.2016.04.018
institution Universiti Teknologi Malaysia
building UTM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Malaysia
content_source UTM Institutional Repository
url_provider http://eprints.utm.my/
topic QA Mathematics
spellingShingle QA Mathematics
Aurangzaib, Aurangzaib
Bhattacharyya, Krishnendu
Shafie, Sharidan
Effect of partial slip on an unsteady MHD mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet
description The objective of the present study was to investigate the partial slip effect on an unsteady two-dimensional mixed convection stagnation point flow towards a permeable shrinking sheet. The governing equations are reduced to a system of non-dimensional partial differential equations using a semi-similarity transformation, before being solved numerically by using Keller-box method. The features of the flow characteristics for different values of the governing parameters are analysed and discussed. The results indicate that the momentum, thermal and concentration boundary layer thicknesses increase with increasing mixed convection parameter for opposing flow, whereas the opposite effect is observed for assisting flow. The results also show that the surface velocity is higher when there is slip at a sheet compared to its absent. Further, the study indicates that the boundary layer thicknesses become thicker and thicker with increasing shrinking parameter, while the opposite effect is observed with increasing Hartmann number. Comparison with previously published work for special cases is performed and found to be in excellent agreement.
format Article
author Aurangzaib, Aurangzaib
Bhattacharyya, Krishnendu
Shafie, Sharidan
author_facet Aurangzaib, Aurangzaib
Bhattacharyya, Krishnendu
Shafie, Sharidan
author_sort Aurangzaib, Aurangzaib
title Effect of partial slip on an unsteady MHD mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet
title_short Effect of partial slip on an unsteady MHD mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet
title_full Effect of partial slip on an unsteady MHD mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet
title_fullStr Effect of partial slip on an unsteady MHD mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet
title_full_unstemmed Effect of partial slip on an unsteady MHD mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet
title_sort effect of partial slip on an unsteady mhd mixed convection stagnation-point flow of a micropolar fluid towards a permeable shrinking sheet
publisher Elsevier
publishDate 2016
url http://eprints.utm.my/id/eprint/69292/
http://dx.doi.org/10.1016/j.aej.2016.04.018
_version_ 1643656050594807808