Derivation of the adding-doubling method
This derivation follows Plass et al. [47] with the terms representing internal
sources omitted for clarity. Define Tnm and Rnm as the transmission and reflection
operators for light incident on side n and exiting side .
Homogeneous tissues
have no preferred direction and so the matrices are equal
Tnm=Tmn and Rnm=Rmn
(The matrices are also symmetric.) Let the vector
denote the radiance incident
from on side 0 of the slab 01, and
denote the radiance incident on side 1.
Similarly define L0- and L1+ as the radiance exiting the slab from sides 0 and 1
respectively (Figure 3.1B). The downward radiance from side 1 is the sum of the
transmitted incident radiance from side 0 and the reflected radiance from side 1,
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L1+=T01L0+ +R10L1-
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(3.10) |
The upward radiance from side 0 is the transmitted radiance from side 1 and the
reflected radiance from side 0
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L1-=R01L0+ +T10L1-
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(3.11) |
Analogous formulas apply to a layer 12
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L2+ =T12L1+ +R21L2-
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(3.12) |
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L1- =R12L1+ + T21L2-
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(3.13) |
Juxtaposition of layers 01 and 12 yields a combined layer 02. The equations relating
the radiances exiting from the top and bottom of this slab are
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L2+ =T 02L0+ +R20L2-
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(3.14) |
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L0- =R02L0+ + T20L2-
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(3.15) |
Presumably, the reflection and transmission operators for the 01 and 12 layers are
known. The reflection and transmission operators for the 02 layer are needed in
terms of those for the 01 and 12 layers. To do this Equation (3.10) is multiplied by
R12 from the left and added to Equation (3.13). Since the terms containing L1+
cancel
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(E-R12R10) L1- =R12T01L0+ + T21L2-
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(3.16) |
Multiplying Equation (3.16) on the left by
(E-R12R10)-1 yields
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L1- = (E-R12R10)-1 (R12T01L0+ + T21L2-)
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(3.17) |
This equation expresses the upward radiance at the interface between two layers. An
equation for the downward mid-layer radiance can be obtained similarly using
Equations (3.13) and (3.10)
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L1+ = (E-R10R12)-1 (T01L0+ + R10T21L2-)
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(3.18) |
Substituting Equation (3.18) into Equation (3.12) yields
![\begin{displaymath}
L_2^+ = \left[T_{12}(E-R_{10}R_{12})^{-1}T_{01} \right]L_0^+...
...ft[T_{12}(E-R_{10}R_{12})^{-1}R_{10}T_{21}+R_{21} \right]L_2^-
\end{displaymath}](img152.gif) |
(3.19) |
Comparing this equation with Equation (3.14) indicates that
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T02 = T12(E-R10R12)-1T01
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(3.20) |
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R20 = T12(E-R10R12)-1 R10T21+R21
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(3.21) |
Similarly Equation (3.11) can be substituted into Equation (3.13) to obtain
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T20 = T10(E-R12R10)-1T21
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(3.22) |
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R02 = T10(E-R12R10)-1 R12T01+R01
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(3.23) |
Equations (3.20)-(3.23) define the reflection and
transmission operators for a layer
comprised of two individual layers in terms of reflection and transmission operators
for each layer.
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