Modeling Heat Transfer by Radiation
This section summarizes the functionalities available within the Heat Transfer Module for the modeling of heat transfer by radiation.
Radiation is a heat transfer mode that should be considered in addition to conduction and convection in the following cases:
As an example, consider a plate of concrete with a cold bottom wall at temperature T0, placed in a hot environment with an air flux at temperature Tamb:
The figures below illustrate the relative importance of heat transfer by radiation and by convection (due to the air flux), when the emissivity ε is 0.1 (left) and 0.9 (right).
Figure 3-12: Integral of convective and radiative heat fluxes (W/m) along the top boundary, for two values of emissivity, as a function of the temperature difference.
Whereas the boundary radiative and convective heat fluxes are of the same order for temperature difference up to 500K when the emissivity is low (ε=0.1), radiation becomes the dominant mode of heat transfer even for a small temperature difference when the emissivity is high (ε=0.9). Note that the convective heat flux decrease observed for high temperature gradients is related to the fact that the velocity, not the mass flow rate, is prescribed at the air inlet.
See Heat Transfer Variables for the definition of the variables q0 and rflux giving access to the convective and radiative heat fluxes on boundaries.
Two configurations are considered regarding the functionalities available for the modeling of radiative heat transfer: