Uniqueness of inverse procedure
The iteration method implicitly assumes that a unique combination
of the albedo a, the optical depth ,
and the anisotropy
gHG
will be determined by a specified set of reflection and transmission
measurements. Consider the case when
the optical thickness is held constant. Increasing the albedo
increases reflection and decreases transmission. Decreasing
the anisotropy also increases the reflection and decreases the
transmission, and so the anisotropy and the albedo are not obviously
independent functions of the reflection and transmission.
Figure 6.1:
Flowchart for inversion process. The method involves
guessing the optical properties of a tissue, calculating the
reflection and transmission for these properties, comparing the
calculated with the measured reflection and transmission, and
repeating this process until the calculated and measured transmission
match.
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In Figure 6.2 the dependence of the total transmission and the
diffuse reflection on the anisotropy and albedo is shown. The
grid was computed with the collimated transmission fixed at ten
percent (
Tcollmathrmmeas=0.1) and the boundaries of the sample are matched with
the outside. The intersection of the appropriate measured diffuse
reflection and measured total transmission grid lines determines
a unique albedo and anisotropy. Diffuse reflectances above about
0.5 are physically impossible for the assumed boundary conditions
and assumed collimated transmission. The albedo and anisotropy
are most sensitive to errors in the magnitudes of the diffuse
reflection and total transmission measurements when the magnitudes
of both these measurements are small (e.g., R=0.1, T=0.2).
Now let
gHG be held constant: in this case the two parameters
which may be varied are the albedo a and the optical depth .
Increasing the albedo increases the reflection and decreases
transmission. Since increasing the optical depth also increases
reflection and decreases transmission, the optical depth is again
not clearly independent of the albedo. Figure 6.3 shows how
T (total transmission) and R+T (diffuse reflection plus total
transmission) depend on the albedo and optical thickness for
the case when
gHG=0 and the sample boundaries are matched with
the environment. This graph is typical of other anisotropies
and boundary conditions. Measured values for R and T (or equivalently,
T and R+T) determine a unique
intersection point whose ordinate is a simple function of the
albedo a and whose abscissa is the optical depth .
The axes
in Figure 6.3 were chosen to linearize the T and the R+T contour
curves.
Figure:
Typical diffuse reflectance (R) and total transmission
(T) grid for a fixed collimated transmission (Tc=0.1). For every
pair of measurements R and T, the R-T grid intersection defines
a unique pair of optical properties for the albedo a and the
anisotropy
for that tissue.
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Figure:
Typical diffuse reflectance (R) and total transmission
plus diffuse reflectance (R+T) grid for a fixed anisotropy
.
For every pair of measurements R and T, the T/R+T grid intersection
defines a unique pair of optical properties for the albedo a
and the optical depth
for that tissue.
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