In Figure 4.1 the boundary conditions are varied to determine how the index of the refraction of the medium affects fluence calculations. The delta-Eddington approximation works best for index matched conditions, because no approximation must be made to account for total internal reflection of light at the boundary.
The total fluence is the sum of collimated and diffuse fluences. The
collimated fluence dominates when the albedo is small. This explains
Figure 4.2 in which the delta-Eddington approximation is
better for low than for high albedos. Figure 4.3
illustrates that the delta-Eddington approximation is better for isotropic
scattering than anisotropic scattering. In this graph, the
Henyey-Greenstein phase function is used with
gHG=0.875. The
equivalent delta-Eddington parameters (g'=0.47, f=0.77) can be
calculated using Equations (1.4) and (1.5). The effective
thickness
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