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Keep the default value, Constant, to define a gray radiation model. In this case, the radiative properties (emissivity, absorption and scattering coefficients) have the same definition for all wavelengths. These properties can still depend on other quantities, in particular on the temperature.
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Select Solar and ambient to define a spectral radiation model with two spectral bands, one for short wavelengths, [0, λsol/amb], (solar radiation) and one for large wavelengths, [λsol/amb, +∞[, (ambient radiation). It is then possible to define the Separation point between spectral bands (SI unit: m), λsol/amb, to adjust the wavelength intervals corresponding to the solar and ambient radiation. The radiative properties can then be defined for each spectral band.
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Select Multiple spectral bands and set the value of the Right endpoint for each spectral band in the table, to define a spectral radiation model. The value of the Right endpoint must be entered without unit. Modify the Wavelength unit to set the unit of all the endpoints. Right endpoint values should be set in an ascending order. The values of the Left endpoint for the next spectral band are updated automatically. It is possible to provide a definition of the surface properties for each spectral band.
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The first Left endpoint and the last Right endpoint are predefined and equal to 0 and +∞, respectively.
Parameters can be used to set the value of the Right endpoint.
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The wavelengths λ set in Solar and ambient and Multiple spectral bands are the wavelengths in vacuum.
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When Discrete ordinates method is selected, Opaque Surface (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces) and Continuity on Interior Boundary (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces) are automatically added as default boundary features. The Incident Intensity (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces) and Periodic Condition (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces) features are made available from the Physics ribbon toolbar (Windows users), Physics context menu (Mac or Linux users), or the context menu (all users).
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When P1 approximation is selected, Opaque Surface (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces) is automatically added as a default boundary feature. The Incident Intensity (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces), Periodic Condition (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces), and Symmetry (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces) features are made available from the Physics ribbon toolbar (Windows users), Physics context menu (Mac or Linux users), or the context menu (all users). Continuity on Interior Boundary (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces) is not available.
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The choice of Radiation discretization method also offers different settings for the Absorbing-Scattering Medium (Radiation in Absorbing-Scattering Media Interface), Opaque Surface (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces), and Incident Intensity (Radiation in Participating Media and Radiation in Absorbing-Scattering Media Interfaces) nodes.
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The Level Symmetric Even (the default), Level Symmetric Hybrid, and Equal Weight Odd sets are SN approximations. Depending on the set and the order selected in the Discrete ordinates method list, different moment conditions are satisfied. In 3D, S2, S4, S6, and S8 generate 8, 24, 48, and 80 directions, respectively. In 2D and 2D axisymmetric, S2, S4, S6, and S8 generate 4, 12, 24, and 40 directions, respectively.
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The Quasi-uniform weight approximation discretizes the angular space by using a reference octahedron with 8 triangular faces, further discretized in function of the order of the method. This corresponds to a TN approximation, for which 8N2 weights are computed at order N in 3D and 4N2 in 2D and 2D axisymmetric.
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