Least squares fit
Once the experimental data has been converted into an equivalent
phase function measurement
pmeas using Equation (5.13), it must
be fit to a phase function. It was found that a modified Henyey-Greenstein
phase function
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(5.14) |
accurately represented the phase function for human dermis.
If the albedo for a tissue is unknown, or a correction factor
in Equation (5.13) is not known precisely, then it is convenient
to include an arbitrary multiplicative factor in the expression
for the phase function. If this is done then
The second equality
is useful only when all factors
in Equation (5.13) are known. This is a poor way to measure
the albedo of a material because it requires excellent absolute
accuracy in the goniometric measurement rather than good relative
accuracy. To fit the modified Henyey-Greenstein phase function
to the measured phase function three parameters must be determined:
the multiplicative factor g, the amount of light scattered isotropically
,
and the anisotropy factor
gHG.
Figure 5.4:
Raw goniophotometer data from 100 m sample of
human dermis. Error bars are constant in magnitude and equal
to the resolution of the A/D converter in the computer (0.005V).
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Figure 5.5:
Corrected goniophotometer data from a 100 m sample
of human dermis. Error bars have also been corrected and no
longer have a constant magnitude.
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One of the assumptions in the modified Henyey-Greenstein phase
function is that light scattered in the backwards direction (reflected
light) is scattered isotropically. Figure 5.5 shows a plot of
the corrected data. The light reflected is not absolutely isotropic
(a flat response) but increases slightly around 180
due to internal reflectance of the forward peak. Subtraction
of this reflected light yields a nearly constant value in the
backwards direction. The fraction of light scattered isotropically
( )
is determined by averaging values for
in the
backwards direction.
Figure 5.6:
Linearized phase function data from 100 m sample
of human dermis showing increasing error for grazing angles (small
).
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The reflected data provides information for
and the transmitted
data is used to find two more parameters
gHG and .
The transformation
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(5.15) |
reduces the modified Henyey-Greenstein equation into a linear
equation of the form y=mx+b. The slope and intercept are given
by
![\begin{displaymath}
m=-{2g_{\mathrm{HG}}\over[\gamma(1-\beta)(1-g_{\mathrm{HG}}^...
...athrm{HG}}^2\over[\gamma(1-\beta)(1-g_{\mathrm{HG}}^2)]^{2/3}}
\end{displaymath}](img525.gif) |
(5.16) |
If Equation (5.15) is used to transform the data then a graph
similar to Figure 5.4 is obtained. The error values were calculated
with a fixed photometric error of 0.005V in the goniophotometer.
The errors in
are roughly proportional to the correction
factor shown in Figure 5.2. A weighted least squares fit must
be used to find the slope and intercept of the best-fit line
because of the widely varying errors between data points. The
error in the slope ( )
and intercept ( )
may also be calculated
[4].
The phase function parameters
and
gHG may be recovered from
the slope and intercept by solving Equations (5.16). This results
in the following physical expressions for
gHG and
in terms
of the calculated intercept b, slope m, and product
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(5.17) |
The errors in the values calculated for
gHG and
are found using
the standard error propagation formula,
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(5.18) |
Inserting Equations (5.17) leads to the following equation for
the error in the anisotropic value of
gHG
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(5.19) |
The error in
is
![\begin{displaymath}
\Delta\gamma = \gamma\left[{(9\Delta m)^2\over 4m^2}+\left( ...
...Delta g_{\mathrm{HG}})^2\over g_{\mathrm{HG}}^2} \right]^{1/2}
\end{displaymath}](img533.gif) |
(5.20) |
The error in
is
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(5.21) |
where
is the standard deviation of the average of the backwards
scattered light used to find .
Intra-sample variation of
gHG
and
was much greater than the errors arising from the fitting
process.
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