2015
DOI: 10.4208/aamm.2013.m379
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Abstract: Abstract. An analysis is carried out to study the magnetohydrodynamic (MHD) flow and heat transfer characteristics of an electrically conducting dusty non-Newtonian fluid, namely, the upper convected Maxwell (UCM) fluid over a stretching sheet. The stretching velocity and the temperature at the surface are assumed to vary linearly with the distance from the origin. Using a similarity transformation, the governing nonlinear partial differential equations of the model problem are transformed into coupled non-lin… Show more

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Cited by 5 publications
(1 citation statement)
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“…In recent times, these fluid models are being used to study the viscoelastic fluid flow over a stretching /non-stretching sheet with/without heat transfer (Hayat et al [16], Aliakbar et al [17], Vajravelu et al [18], Hayat and Qasim [19], Prasad et al [20], Vajravelu et al [21]). Recently, Vajravelu et al [22] investigated the MHD flow and heat transfer of a dusty non-Newtonian UCM fluid over a stretching sheet numerically and established that the Maxwell fluid reduces the wall-shear stress. In view of the above studies, in the present paper, we analyze MHD flow of a UCM fluid in a parallel plate channel permeated by a uniform, transverse magnetic field where the surface velocity of the channel varies linearly with distance from the origin.…”
mentioning
confidence: 99%
“…In recent times, these fluid models are being used to study the viscoelastic fluid flow over a stretching /non-stretching sheet with/without heat transfer (Hayat et al [16], Aliakbar et al [17], Vajravelu et al [18], Hayat and Qasim [19], Prasad et al [20], Vajravelu et al [21]). Recently, Vajravelu et al [22] investigated the MHD flow and heat transfer of a dusty non-Newtonian UCM fluid over a stretching sheet numerically and established that the Maxwell fluid reduces the wall-shear stress. In view of the above studies, in the present paper, we analyze MHD flow of a UCM fluid in a parallel plate channel permeated by a uniform, transverse magnetic field where the surface velocity of the channel varies linearly with distance from the origin.…”
mentioning
confidence: 99%