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Forced convection heat transfer phenomena

Heat is transferred from or to a region by the motion of fluids and the phenomenon of convection. In natural convection, the movement is caused by buoyancy forces induced by variations in the density of the fluid these variations are caused by differences in temperature. In forced convection, movement is created by an external agency such as a pump. [Pg.3869]

Convection. When a current or macroscopic particle of fluid crosses a specific surface, such as the boundary of a control volume, it carries with it a definite quantity of enthalpy. Such a flow of enthalpy is called a convective flow of heat or simply convection. Since convection is a macroscopic phenomenon, it can occur only when forces act on the particle or stream of fluid and maintain its motion against the forces of friction. Convection is closely associated with fluid mechanics. In fact, thermodynamically, convection is not considered as heat flow but as flux of enthalpy. The identification of convection with heat flow is a matter of convenience, because in practice it is difficult to separate convection from true conduction when both are lumped together under the name convection. Examples of convection are the transfer of enthalpy by the eddies of turbulent flow and by the current of warm air from a household furnace flowing across a room. [Pg.286]


See other pages where Forced convection heat transfer phenomena is mentioned: [Pg.142]    [Pg.203]    [Pg.223]    [Pg.329]    [Pg.196]    [Pg.1071]    [Pg.43]    [Pg.206]    [Pg.82]    [Pg.115]   
See also in sourсe #XX -- [ Pg.802 , Pg.804 ]




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