Phase functions
When light strikes a particle with an index of refraction different from its
environment, the light is refracted. The angle at which the light is bent is a
function of the size and shape of the particle as well as the wavelength of the
incident light and the incidence angle of the light. In general, each particle will
have a different scattering profile. This scattering profile is called the phase
function. This name is misleading since the scattering profile has no connection
with the phase of the incident light waves and would be more appropriately
called a scattering function.
The phase function
describes the amount of light scattered from
the direction denoted by the unit vector
into the direction
.
There are a number of ways in which the phase function may be normalized, but the
most natural is that used by the astrophysicists. They treat the phase function
as a probability distribution; consequently, their normalization condition
requires the integral of the phase function over all angles to equal unity
 |
(1.1) |
where
is a differential solid angle in the
direction.
This condition does not permit the phase function to describe absorption of light
by the particle, the phase function is a description of only the distribution of
scattering by the particle. Thus
is
the probability that a photon incident from the
direction will
leave in the differential unit of solid angle in the
direction.
The phase function will differ in general from particle to particle. For
simplicity an average phase function which adequately describes the most
important features of the scattering process is used. This average phase
function is further constrained by assuming that the probability of scattering from
one direction into another is a function only of the angle between the two
directions, thus
.
The simplest phase function is the isotropic phase function
 |
(1.2) |
The factor of
results from the normalization condition (1.1) and the fact that
there are
steradians in a complete circle. The phase function has units of sr-1.
If the phase function is not isotropic, then a parameter called the average
cosine of the phase function is used to describe the degree of anisotropy of the
phase function. This parameter is often denoted by g and is defined as the
integral over all angles of the phase function multiplied by the cosine of the angle
 |
(1.3) |
The choice of a single scattering phase function is a compromise between realism
and mathematical tractability. Jacques et al. have shown that a
modified Henyey-Greenstein function describes single particle light scattering in
human dermis quite well [32]. More recently Yoon et al.
have found similar results for human aorta [69]. The modified
Henyey-Greenstein function is
![\begin{displaymath}
p_{\rm m-HG}(\cos\theta) = {1\over4\pi} \left[
\beta + (1-\b...
...hrm{HG}}^2 - 2g_{\mathrm{HG}}\cos\theta\right)^{3/2} }
\right]
\end{displaymath}](img44.gif) |
(1.4) |
In this function, the first term
represents the amount of light scattered
isotropically. The second term is the Henyey-Greenstein function. The function
is normalized such that the integral of the phase function over all solid angles is
unity. When
this phase function reduces to the Henyey-Greenstein phase
function.
A popular phase function is the Eddington phase function
![\begin{displaymath}
p_{\rm Eddington}(\cos\theta) = {1\over4\pi} \left[1+3g'\cos\theta \right]
\end{displaymath}](img46.gif) |
(1.5) |
With this approximation the transport equation may be reduced into a diffusion
equation [31,55]. Such a solution provides
a qualitative picture of radiative transport in media which is not highly forward
scattering. Unfortunately, the anisotropy (the average cosine of the phase
function) for tissue such as dermis [32], aorta [70] and
bladder [9] have values of 0.8-0.9. This suggests
that the Eddington approximation would not be very good for modeling light in
such tissues.
Another possible phase function is the delta-Eddington approximation
[34],
![\begin{displaymath}
p_{\delta-\mathrm{E}}(\cos\theta) = {1\over4\pi} \left[2f\delta(1-\cos\theta)+
(1-f)(1+3g'\cos\theta) \right]
\end{displaymath}](img47.gif) |
(1.6) |
where f is the fraction of light scattered into the forward peak and g' is an
asymmetry factor. As
the phase function becomes exactly a delta
function, and as
the phase function reduces to the Eddington
approximation. This phase function also allows reduction of the transport
equation to a diffusion equation. Consequently, it is desirable to approximate
the modified Henyey-Greenstein function using the delta-Eddington phase
function. Joseph et al. used the delta-Eddington phase function above
to approximate the Henyey-Greenstein phase function [34]. Only slight
modification must be made to their derivation to arrive at an approximation for
the modified Henyey-Greenstein function.
Recalling that the Dirac delta function may be expanded as a sum of
Legendre polynomials [44] allows expansion of the
delta-Eddington phase function
![\begin{displaymath}
p_{\delta-\mathrm{E}}(\cos\theta) = {1\over4\pi}
\left[f\su...
...1)P_n(\cos\theta)+(1-f) \big( 1+3g'P_1(\cos\theta)\big)\right]
\end{displaymath}](img50.gif) |
(1.7) |
collecting like terms
![\begin{displaymath}
p_{\delta-\rm E}(\cos\theta) = {1\over4\pi}
\left[1+3[f+g'(1-f)]P_1(\cos\theta)+5fP_2(\cos\theta) + \cdots \right]
\end{displaymath}](img51.gif) |
(1.8) |
The modified Henyey-Greenstein phase function may also be expanded as a sum
of Legendre polynomials using the expansion from [60] for the
Henyey-Greenstein function
![\begin{displaymath}
p_{\rm m-HG}(\cos\theta) = {1\over4\pi} \left[
\beta P_0(\co...
...um_{n=0}^\infty (2n+1)g_{\mathrm{HG}}^nP_n(\cos\theta)
\right]
\end{displaymath}](img52.gif) |
(1.9) |
and collecting like terms
![\begin{displaymath}
p_{\rm m-HG}(\cos\theta) = {1\over4\pi}
\left[1+3(1-\beta)g...
...)+5(1-\beta)g_{\mathrm{HG}}^2 P_2(\cos\theta) + \cdots \right]
\end{displaymath}](img53.gif) |
(1.10) |
Now the first terms of each series are equated. The very first term (n=0) is
for both series. This results from the normalization of the phase functions. The
next term (n=1) corresponds to three times the average cosine of the phase
function g [31]. Thus for the delta-Eddington approximation, the
average cosine of the phase function is
and for the modified Henyey-Greenstein function the average cosine is
 |
(1.12) |
The average cosine of the phase function g is a measure of how much light is
scattered in the forward direction. The anisotropy can be any value between -1
and 1. If g=-1, then scattering is completely in the backwards direction; if g=1,
then scattering is totally in the forwards direction; and if g=0, then scattering is
isotropic. If Equations (1.11) and (1.12) are equated then a relation between the
parameters of the two phase functions is obtained
 |
(1.13) |
Proceeding in a similar manner, the second moments of the two phase functions
may be equated
 |
(1.14) |
And using Equation (1.13) an expression for g' may be obtained
 |
(1.15) |
Notice that if
then
provided that ,
otherwise
.
For example, measurements of the phase function of dermis at 633nm
yields the modified Henyey-Greenstein parameters
gHG=0.91 and .
Using
Equations (1.14) and (1.15) the corresponding values for the delta-Eddington
phase function may be found, i.e., f=0.75 and g'=0.29. This illustrates the way
that the delta-Eddington approximation accommodates for strongly forward
scattering phase functions by lumping a large portion of the scattering into the
forward directed Dirac delta function and allowing the anisotropy to fall.
Increased accuracy results since it is known that the diffusion approximation is
poor for large values of anisotropy but is relatively good when the scattering is
nearly isotropic.
For completeness, the following equations relate the modified Henyey-
Greenstein parameters to the delta-Eddington parameters
 |
(1.16) |
These are useful as long as f is not zero. If f is zero then no solution is possible,
because the equations relating the first and second moments are no longer
independent.
|