| • | κ is the absorption coefficient (SI unit: m–1 ). | 
      
     
    
      
        
          | • | G is the incident radiation (SI unit: W/m2 ). | 
      
     
    
      
        
          | • | Ib(T) is the blackbody radiative intensity (SI unit: W/(m2 ·sr)), defined as | 
      
     
    
    
      
        
          | • |   nr is the refractive index (dimensionless). | 
      
     
    
      
        
          | • |  σ is the Stefan-Boltzmann constant (SI unit: W/(m2 ·K4 )). | 
      
     
    
      
        
          | • |  T is the temperature (SI unit: K) | 
      
     
    
    
    
    
      
        
          | • |  I(Ω) is the radiative intensity (SI unit: W/(m2 ·sr)) at a given position following the Ω direction, that satisfies the radiative transfer equation | 
      
     
    
    
      
        
          | • |  β = κ + σs is the extinction coefficient (SI unit: 1/m). | 
      
     
    
      
        
          | • |  σs is the scattering coefficient (SI unit: 1/m). | 
      
     
    
      
        
          | • |  ϕ(Ω', Ω) is the scattering phase function (dimensionless) | 
      
     
    If the Radiation discretization method is 
Discrete ordinates method, 
G is defined by
 
    
       (6-10)
 
    
    
       (6-11) 
  
    
    
      
        
          | • |  Si is the ith  discrete ordinate. | 
      
     
    
      
        
          | • |  Ii is the ith  component of the radiative intensity. | 
      
     
    
      
        
          | • |  ωj is the ith  quadrature weight. | 
      
     
    If the Radiation discretization method is 
P1 approximation, 
G is the solution of the following equation
 
    
       (6-12)
 
    where DP1 is the P1 diffusion coefficient.
 
    When Wavelength dependence of radiative properties is 
Solar and ambient or 
Multiple spectral bands in the 
Participating Media Settings section of the interface, 
Equation 6-10 and 
Equation 6-11 are solved for each spectral band 
k: 
Ii,k is the 
ith component of the radiative intensity for spectral band 
k, and 
Gk is the incident radiation for spectral band 
k.
 
    
    
    If radiative emission may be neglected, the Absorbing-Scattering Medium (Radiation in Absorbing-Scattering Media Interface) node may be used instead. The table below describes the different effects accounted for by the interfaces found under the 
Heat Transfer>Radiation branch (

).
 
    
    
    
    
    This section is available when temperature-dependent material properties are used. The default Temperature is 
User defined. When additional physics interfaces are added to the model, the temperature variables defined by these physics interfaces can also be selected from the list. The 
Common model input option corresponds to the 
minput.T variable, set to 293.15 K by default) and all temperature variables from the physics interfaces included in the model. To edit the 
minput.T variable, click the 
Go to Source button (

), and in the 
Default Model Inputs node under 
Global Definitions, set a value for the 
Temperature in the 
Expression for remaining selection section.
 
    
    This section is available when the Wavelength dependence of radiative properties is defined as 
Solar and ambient or 
Multiple spectral bands for the physics interface (see 
Participating Media Settings).
 
    When the Fractional emissive power is 
Blackbody/Graybody, the fractional emissive power is automatically calculated for each spectral band as a function of the band endpoints and temperature.
 
    When the Fractional emissive power is 
User defined on each band, define the 
Fractional emissive power, 
FEPk for each spectral band. All fractional emissive powers are expected to be in [0,1] and their sum is expected to be equal to 1.
 
    
    The Absorption coefficient κ should be specified. It defines the amount of radiation, 
κI(Ω), that is absorbed by the medium.
 
    The Absorption coefficient κ (SI unit: 1/m) uses values 
From material by default.
 
    For User defined, set a value or expression. You can define a temperature-dependent absorption coefficient using the variable 
rpm.T.
 
    If Wavelength dependence of radiative properties is 
Solar and ambient or 
Multiple spectral bands, the wavelength may be accessed through the 
rpm.lambda variable. Any expression set for the absorption coefficient is then averaged on each spectral band to obtain a piecewise constant absorption coefficient. If the average value of the absorption coefficient on each band is known, you may use instead the 
User defined for each band option to avoid the evaluation of the average.
 
    When Absorption coefficient is set to 
User defined for each band, enter a value for the 
Absorption coefficient for each spectral band in the table displayed underneath. Within a spectral band, each value is assumed to be independent of wavelength.
 
    
    
    The Scattering coefficient σs (SI unit: 1/m) uses values 
From material by default.
 
    For User defined, set a value or expression. You can define a temperature-dependent scattering coefficient using the variable 
rpm.T.
 
    If Wavelength dependence of radiative properties is 
Solar and ambient or 
Multiple spectral bands, the wavelength may be accessed through the 
rpm.lambda variable. Any expression set for the scattering coefficient is then averaged on each spectral band to obtain a piecewise constant scattering coefficient. If the average value of the scattering coefficient on each band is known, you may use instead the 
User defined for each band option to avoid the evaluation of the average.
 
    When Scattering coefficient is set to 
User defined for each band, enter a value for the 
Scattering coefficient for each spectral band in the table displayed underneath. Within a spectral band, each value is assumed to be independent of wavelength.
 
    Choose in addition the Scattering type: 
Isotropic, 
Linear anisotropic, 
Polynomial anisotropic (only with 
Discrete ordinates method), or 
Henyey-Greenstein (only with 
Discrete ordinates method). If the 
Radiation discretization method is 
Discrete ordinates method, only 
Isotropic is available for 2D axisymmetric components.
 
    
    
      
        
          | • | Isotropic (default) corresponds to the scattering phase function ϕ(μ0) = 1 . | 
      
     
    
      
        
          | • | For Linear anisotropic it defines the scattering phase function as ϕ(μ0) = 1 + a1μ0 . Enter the Legendre coefficient a1 . | 
      
     
    
      
        
          | • | For Polynomial anisotropic it defines the scattering phase function as | 
      
     
    
    Enter each Legendre coefficient a1, …, 
a12 as required.
 
    
      
        
          | • | For Henyey-Greenstein it defines the scattering phase function as | 
      
     
    
    where −1 < η < 1 is the anisotropy parameter and 
K is defined as follows to produce a normalized phase function:
 
    
    For Linear anisotropic and 
Polynomial anisotropic, select the 
Normalize phase function check box to define a phase function such as
 
    
    
    For Linear anisotropic, 
Polynomial anisotropic, and 
Henyey-Greenstein, select the 
Wavelength-dependent scattering type check box to average each 
Legendre coefficient a1, …, 
a12 or the 
Anisotropy parameter μ to obtain piecewise constant coefficients on each spectral band.
 
    
    
    
    
    
    
    Physics tab with Radiation in Participating Media selected: