Forced convection


Forced convection is a mechanism, or type of transport in which fluid motion is generated by an external source. Alongside natural convection, thermal radiation and thermal conduction it is one of the methods of heat transfer and allows significant amounts of heat energy to be transported very efficiently.

Applications

This mechanism is found very commonly in everyday life, including central heating, air conditioning, steam turbines and in many other machines. Forced convection is often encountered by engineers designing or analyzing heat exchangers, pipe flow, and flow over a plate at a different temperature than the stream.

Mixed convection

In any forced convection situation, some amount of natural convection is always present whenever there is gravitational forces present. When the natural convection is not negligible, such flows are typically referred to as mixed convection..

Mathematical analysis

When analyzing potentially mixed convection, a parameter called the Archimedes number parametrizes the relative strength of free and forced convection. The Archimedes number is the ratio of Grashof number and the square of Reynolds number, which represents the ratio of buoyancy force and inertia force, and which stands in for the contribution of natural convection. When Ar >> 1, natural convection dominates and when Ar << 1, forced convection dominates.
When natural convection isn't a significant factor, mathematical analysis with forced convection theories typically yields accurate results. The parameter of importance in forced convection is the Péclet number, which is the ratio of advection and diffusion of heat.
When the Peclet number is much greater than unity, advection dominates diffusion. Similarly, much smaller ratios indicate a higher rate of diffusion relative to advection.