“…The GRTE, developed in Ref. [1,21] for possibly non Beerian phases of this kind of porous media, is directly based on G ext (s − s, θ, ϕ), P sc,ν (s − s, θ, ϕ), n w,ν (θ, ϕ) and the scattering phase function p w (θ i , ϕ i , θ sc , ϕ sc ). For optically thick media, the GRTE rigorously degenerates into a classical RTE, characterized by generalized extinction, absorption and scattering coefficients at equilibrium B w (θ, ϕ), K w,ν (θ, ϕ) and Σ w,ν (θ, ϕ) given by…”