Partial slip effect on heat and mass transfer of MHD peristaltic transport in a porous medium
This research looks at the effects of partial slip on heat and mass transfer of peristaltic transport. The magnetohydrodynamic (MHD) flow of viscous fluid in a porous asymmetric channel has been considered. The exact solutions for the stream function, longitudinal pressure gradient, longitudinal vel...
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Universiti Kebangsaan Malaysia
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ukm-72702016-12-14T06:43:35Z http://journalarticle.ukm.my/7270/ Partial slip effect on heat and mass transfer of MHD peristaltic transport in a porous medium Obaid Ullah Mehmood, Norzieha Mustapha, Sharidan Shafie, T. Hayat, This research looks at the effects of partial slip on heat and mass transfer of peristaltic transport. The magnetohydrodynamic (MHD) flow of viscous fluid in a porous asymmetric channel has been considered. The exact solutions for the stream function, longitudinal pressure gradient, longitudinal velocity, shear stress, temperature and concentration fields are derived by adopting long wavelength and small Reynolds number approximations. The results showed that peristaltic pumping and trapping are reduced with increasing velocity slip parameter. Furthermore, temperature increases with increasing thermal slip parameter. Moreover, the concentration profile decreases with increasing porosity parameter, Schmidt number and concentration slip parameter. Comparisons with published results are found to be in good agreement. Universiti Kebangsaan Malaysia 2014-07 Article PeerReviewed application/pdf en http://journalarticle.ukm.my/7270/1/21_Obaid_Ullah.pdf Obaid Ullah Mehmood, and Norzieha Mustapha, and Sharidan Shafie, and T. Hayat, (2014) Partial slip effect on heat and mass transfer of MHD peristaltic transport in a porous medium. Sains Malaysiana, 43 (7). pp. 1109-1118. ISSN 0126-6039 http://www.ukm.my/jsm/ |
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Universiti Kebangasaan Malaysia |
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Online Access |
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English |
description |
This research looks at the effects of partial slip on heat and mass transfer of peristaltic transport. The magnetohydrodynamic (MHD) flow of viscous fluid in a porous asymmetric channel has been considered. The exact solutions for the stream function, longitudinal pressure gradient, longitudinal velocity, shear stress, temperature and concentration fields are derived by adopting long wavelength and small Reynolds number approximations. The results showed that peristaltic pumping and trapping are reduced with increasing velocity slip parameter. Furthermore, temperature increases with increasing thermal slip parameter. Moreover, the concentration profile decreases with increasing porosity parameter, Schmidt number and concentration slip parameter. Comparisons with published results are found to be in good agreement. |
format |
Article |
author |
Obaid Ullah Mehmood, Norzieha Mustapha, Sharidan Shafie, T. Hayat, |
spellingShingle |
Obaid Ullah Mehmood, Norzieha Mustapha, Sharidan Shafie, T. Hayat, Partial slip effect on heat and mass transfer of MHD peristaltic transport in a porous medium |
author_facet |
Obaid Ullah Mehmood, Norzieha Mustapha, Sharidan Shafie, T. Hayat, |
author_sort |
Obaid Ullah Mehmood, |
title |
Partial slip effect on heat and mass transfer of MHD
peristaltic transport in a porous medium |
title_short |
Partial slip effect on heat and mass transfer of MHD
peristaltic transport in a porous medium |
title_full |
Partial slip effect on heat and mass transfer of MHD
peristaltic transport in a porous medium |
title_fullStr |
Partial slip effect on heat and mass transfer of MHD
peristaltic transport in a porous medium |
title_full_unstemmed |
Partial slip effect on heat and mass transfer of MHD
peristaltic transport in a porous medium |
title_sort |
partial slip effect on heat and mass transfer of mhd
peristaltic transport in a porous medium |
publisher |
Universiti Kebangsaan Malaysia |
publishDate |
2014 |
url |
http://journalarticle.ukm.my/7270/ http://journalarticle.ukm.my/7270/ http://journalarticle.ukm.my/7270/1/21_Obaid_Ullah.pdf |
first_indexed |
2023-09-18T19:49:15Z |
last_indexed |
2023-09-18T19:49:15Z |
_version_ |
1777406108475850752 |