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Keep the default value, Constant, to define a diffuse gray radiation model. In this case, the surface emissivity has the same definition for all wavelengths. The surface emissivity can still depend on other quantities, in particular on the temperature.
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Select Solar and ambient to define a diffuse spectral radiation model with two spectral bands, one for short wavelengths, [0, λ1], (solar radiation) and one for large wavelengths, [λ1, +∞[, (ambient radiation). It is then possible to define the Intervals endpoint (SI unit: m), λ1, to adjust the wavelength intervals corresponding to the solar and ambient radiation. The surface properties can then be defined for each spectral band. In particular it is possible to define the solar absorptivity for short wavelengths and the surface emissivity for large wavelengths.
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Select Multiple spectral bands and set the Number of wavelength bands value (2 to 5), to define a diffuse spectral radiation model. It is then possible to provide a definition of the surface emissivity for each spectral band. Update Intervals endpoint (SI unit: m), λ1, λ2, ..., to define the wavelength intervals [λi − 1, λi[ for i from 1 to the Number of wavelength bands.
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The first and the last endpoints, λ0 and λN (with N equal to the value selected to define the Number of wavelength bands), are predefined and equal to 0 and +∞, respectively.
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If shadowing is ignored, global energy is not conserved. Control the accuracy by specifying a Radiation integration order. Sharp angles and small gaps between surfaces may require a higher integration order for accuracy but also more time to evaluate the irradiation.
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