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For a two-level system in slab geometry that includes collisional pumping between atomic levels,
the radiation transport equation is
+ c = A21 - cK12n1-K21n2f,
|
(1) |
where c is the speed of light, x is the position in the slab, is the direction
cosine of the radiation, is the frequency of the radiation,
f (,, x, t) is
the photon number density distribution per unit atom density,
n2(x, t) is the upper
level population fraction,
n1(x, t) is the lower level population fraction, A21
is the spontaneous emission rate,
(a,) is the Voigt line profile normalized to
unit integral [7], and
K12 = N where is the lower state
absorption cross section and N is the atom number density. The coefficient K21
is defined by
K21 = K12,
|
(2) |
where g1 and g2 are the statistical weights for levels 1 and 2, respectively. As in
[3], we consider the problem in the regime of complete redistribution and
no physical scattering of photons.
The equations governing the atomic population fractions n1 and n2 are
|
= |
C12n1 - C21n2 - A21n2 + cK12n1-K21n2 |
|
|
|
x dd()f (,) |
(3) |
and
where C12 and C21 are rate constants for the collisional transitions
1 2 and
2 1, respectively. One must also add in appropriate boundary conditions
and initial state to the above equations.
Using (4), equations (1) and (3) may be rewritten as
+ c = A21 - cK12-K21+K12nf
|
(5) |
and
|
= |
C12 - C12+C21+A21n + cK12-K21+K12n |
|
|
|
x ddf, |
(6) |
respectively, where n is the upper level population fraction.
We can generate a finite differencing scheme in time for (6) by using the standard IMC
technique [3]. We integrate (6) from t0 to
t0 + t.
In the spontaneous emission and collision terms, we approximate n(t) by
n(t0 + t).
In the absorption term, we substitute n(t0) for n(t) and obtain
n(t0 + t) |
= |
n(t0) + C12-C12+C21+A21nt0+tt |
|
|
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+ cK12-K21+K12nt0 |
|
|
|
x dtddf,, t. |
(7) |
In the standard IMC technique [3], we substitute
n(t0 + t) from (7) into the spontaneous
emission term of (5) while using n(t0) in the absorption term.
After some algebra, we obtain
+ c |
= |
nt0+tC12 + |
|
|
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x K12-K21+K12nt0ddf, |
|
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- cK12-K21+K12nt0f, |
(8) |
where is defined as
= .
|
(9) |
Equation (8) can be interpreted as a transport equation with a net absorption, , and effective
scattering, , contribution as given by
() = ()K12-K21+K12n(t0)
|
(10) |
and
() = 1-()K12-K21+K12n(t0)
|
(11) |
where the fraction, , is given by
= .
|
(12) |
The fraction, , determines how much effective scattering the problem contains. As approaches
unity, effective scattering vanishes. The disadvantage of this method is that the effective scattering
term dominates the execution time in optically thick problems, resulting in very long problem runs. Reducing the
effective scattering by making approach 1 requires a smaller time step which also increases execution time
and may reduce accurracy (see Sec. 2.5).
Symbolic Implicit Monte Carlo [4] achieves implicit time integration using a different point of view.
Photons produced by spontaneous emission are given a symbolic weight that remains undetermined until the end of the
time step. The Monte Carlo procedure is the same as for IMC, except there is no effective scattering term. Particle scoring results
in a linear system of equations that are solved for the upper atomic population fraction at the end of a time step.
After spatial discretization (see Sec. 2.3), the upper atomic population is updated with
nt0+t |
= |
n(t0)i + C12-C12+C21+A21nt0+tt |
|
|
|
+ cK12-K21+K12n(t0)i |
|
|
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x FNi+FSijnt0+t/Vi. |
(13) |
The quantities in the square brackets are short hand for the following integral
In Eq. (13), the term containing FNi is the contribution to the change in upper state population within zone i
from photons that were present at the
beginning of the time step. They have therefore explicit, numerical weights. The term containing
FSijn(t0 + t)j is
a similar contribution coming from bundles with symbolic weights that were born in
zone j during the time step; n(t0)i is the upper level atomic population fraction in zone i at start of
time step;
n(t0 + t)i is the unknown upper atomic population fraction in zone i at the end
of the time step; and Vi is the thickness of zone i. For further details, we refer to Ref. [4]. Although the problems we present will involve
small numbers of zones, and as a result the solution of small linear systems using a direct solver,
there is some concern that the size of the linear system to be solved will become intractable using
direct solution methods for problems with larger zone counts. Jacobi iteration [8],
or other more sophisticated techniques, do very well at solving the system of equations given
in (13) by using the values in the previous time step for the initial starting point.
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