1994
DOI: 10.1016/0142-727x(94)90053-1
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Natural-convection boundary-layer flow on a vertical surface with Newtonian heating

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Cited by 248 publications
(156 citation statements)
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“…The convective forced flow is assumed to be moving upward, while the gravity vector g acts downward in the opposite direction, where the coordinates x and y are chosen such that x measures the distance along the surface of the sphere from the lower stagnation point and y measures the distance normal to the surface of the sphere. We assume that the equations are subjected to a Newtonian heating of the form proposed by Merkin [10]. Under the Boussinesq and boundary layer approximations, the basic equations are (Nazar et al [6,8])…”
Section: Discussionmentioning
confidence: 99%
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“…The convective forced flow is assumed to be moving upward, while the gravity vector g acts downward in the opposite direction, where the coordinates x and y are chosen such that x measures the distance along the surface of the sphere from the lower stagnation point and y measures the distance normal to the surface of the sphere. We assume that the equations are subjected to a Newtonian heating of the form proposed by Merkin [10]. Under the Boussinesq and boundary layer approximations, the basic equations are (Nazar et al [6,8])…”
Section: Discussionmentioning
confidence: 99%
“…This situation arises in conjugate heat transfer problems (see, e.g., Merkin and Pop [9]), and also when there is Newtonian heating of the convective fluid from the surface. The latter case has been first discussed in detail by Merkin [10]. The situation with Newtonian heating arises in what are usually termed conjugate convective flows, where the heat is supplied to the convecting fluid through a bounding surface with a finite heat capacity.…”
Section: Introductionmentioning
confidence: 99%
“…Similarly, heat transfer is concerned with the exchange of thermal energy from one physical system to another. Merkin (1994) presented the most recent heating phenomenon, namely Newtonian heating (NH), in which the heat transfer rate from the bounding surface with a finite heat capacity is proportional to the local surface temperature and which is usually termed conjugate convective flow. Various authors have analyzed the simultaneous effects of heat and mass transport phenomena for the flows of nonNewtonian fluids under these conditions.…”
Section: Introductionmentioning
confidence: 99%
“…The distinct feature of this type of convection is that it does not depend on local surface temperature to act as heat sink (Chaudhary and Jain, 2006) and hence Newtonian heating conditions enhances the heat transfer application to a relatively wider range. Merkin (1994) practically demonstrated the phenomenon of free-convection boundary layer for the first time followed by overwhelming number of studies where Newtonian heating applications were investigated (Lesnic et al, 2000;Lesnic et al, 2004;Salleh et al, 2011). Initial studies pertaining to convective heat transfer revealed that Newtonian conditions were first simply analyzed for vertical flat plate immersed in a viscous fluid (Merkin (1994) later on complex conditions where vertical and horizontal surfaces embedded in a porous medium were also considered (Lesnic et al, 2004).…”
Section: Introductionmentioning
confidence: 99%