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Heat and mass transfer on a stretching sheet with suction or blowing

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This article is published in Canadian Journal of Chemical Engineering.The article was published on 1977-12-01. It has received 1408 citations till now. The article focuses on the topics: Suction.

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Citations
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Boundary layer flow of a nanofluid past a stretching sheet with a convective boundary condition

TL;DR: In this article, the boundary layer flow induced in a nanofluid due to a linearly stretching sheet is studied numerically and the transport equations include the effects of Brownian motion and thermophoresis.
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Heat Transfer Characteristics of a Continuous, Stretching Surface With Variable Temperature

TL;DR: Resolution du transfert de chaleur provenant d'une surface en cours d'allongement critique lineaire, avec champ de temperature, en loi de puissance, en termes de fonctions de Kummer as discussed by the authors.
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Viscous flow due to a shrinking sheet

TL;DR: In this paper, the viscous flow induced by a shrinking sheet is studied and its existence and uniqueness are proved. Exact solutions, both numerical and in closed form, are found.
Journal ArticleDOI

Heat transfer of a continuous, stretching surface with suction or blowing

TL;DR: In this paper, an analysis has been carried out to determine the heat transfer occurring in the laminar boundary layer on a linearly stretching, continuous surface subject to suction or blowing.
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Flow of a viscoelastic fluid over a stretching sheet

TL;DR: In this paper, the flow of an incompressible second-order fluid past a stretching sheet is studied, and the authors present a study of the flow in the presence of a stretch sheet.
References
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Boundary‐layer behavior on continuous solid surfaces: I. Boundary‐layer equations for two‐dimensional and axisymmetric flow

B. C. Sakiadis
- 01 Mar 1961 - 
TL;DR: In this article, the boundary-layer behavior on continuous surfaces is examined, and the basic differential and integral momentum equations of boundary layer theory are derived for such surfaces, for both laminar and turbulent flow in the boundary layer.
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The Incomplete Gamma Integral

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