Got the low hanging fruit for implementing MG theory in the theory manual. The majority of work will be in the physics.rst and cross_sections.rst files which I have not attacked yet. I also noticed that the theory wasnt updated for the new secondary particle bank (Ive only seen one place where it needed to be mentioned so far) and for the polar/azimuthal/mu filters. Both have been incorporated.

This commit is contained in:
Adam Nelson 2016-02-26 04:57:12 -05:00
parent 446262f709
commit f9146abeea
3 changed files with 36 additions and 18 deletions

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@ -8,7 +8,7 @@ The physical process by which a population of particles evolves over time is
governed by a number of `probability distributions`_. For instance, given a
particle traveling through some material, there is a probability distribution
for the distance it will travel until its next collision (an exponential
distribution). Then, when it collides with a nucleus, there is associated
distribution). Then, when it collides with a nucleus, there is an associated
probability of undergoing each possible reaction with that nucleus. While the
behavior of any single particle is unpredictable, the average behavior of a
large population of particles originating from the same source is well defined.
@ -45,10 +45,15 @@ following steps:
- Initialize the pseudorandom number generator.
- Read ACE format cross sections specified in the problem.
- Read the contiuous-energy or multi-group cross section data specified in
the problem.
- If using a special energy grid treatment such as a union energy grid or
lethargy bins, that must be initialized as well.
lethargy bins, that must be initialized as well in a continuous-energy
problem.
- In a multi-group problem, individual nuclide cross section information is
combined to produce material-specific cross section data.
- In a fixed source problem, source sites are sampled from the specified
source. In an eigenvalue problem, source sites are sampled from some initial
@ -95,6 +100,10 @@ proceed. The life of a single particle will proceed as follows:
P(i) = \frac{\Sigma_{t,i}}{\Sigma_t}.
Note that the above selection of collided nuclide only applies to
continuous-energy simulations as multi-group simulations use nuclide
data which has already been combined in to material-specific data.
8. Once the specific nuclide is sampled, the random samples a reaction for
that nuclide based on the microscopic cross sections. If the microscopic
cross section for some reaction :math:`x` is :math:`\sigma_x` and the total
@ -105,13 +114,20 @@ proceed. The life of a single particle will proceed as follows:
P(x) = \frac{\sigma_x}{\sigma_t}.
Since multi-group simulations use material-specific data, the above is
performed with those material multi-group cross sections (i.e.,
macroscopic cross sections for the material) instead of microscopic
cross sections for the nuclide).
9. If the sampled reaction is elastic or inelastic scattering, the outgoing
energy and angle is sampled from the appropriate distribution. Reactions
of type :math:`(n,xn)` are treated as scattering and the weight of the
particle is increased by the multiplicity of the reaction. The particle
then continues from step 3. If the reaction is absorption or fission, the
particle dies and if necessary, fission sites are created and stored in the
fission bank.
energy and angle is sampled from the appropriate distribution. In
continuous-energy simulation, reactions of type :math:`(n,xn)` are treated
as scattering and any additional particles which may be created are added
to a secondary particle bank to be tracked later. In a multi-group
simulation, this secondary bank is ont used but the particle weight is
increased accordingly. The original particle then continues from step 3.
If the reaction is absorption or fission, the particle dies and if
necessary, fission sites are created and stored in the fission bank.
After all particles have been simulated, there are a few final tasks that must
be performed before the run is finished. This include the following:

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@ -32,8 +32,9 @@ OpenMC: flux, total reaction rate, scattering reaction rate, neutron production
from scattering, higher scattering moments, :math:`(n,xn)` reaction rates,
absorption reaction rate, fission reaction rate, neutron production rate from
fission, and surface currents. The following variables can be used as filters:
universe, material, cell, birth cell, surface, mesh, pre-collision energy, and
post-collision energy.
universe, material, cell, birth cell, surface, mesh, pre-collision energy,
post-collision energy, polar angle, azimuthal angle, and the cosine of the
change-in-angle due to a scattering event.
With filters for pre- and post-collision energy and scoring functions for
scattering and fission production, it is possible to use OpenMC to generate
@ -55,9 +56,9 @@ be scored to for each value of the filter variable. If a particle is in cell
:math:`n`, the mapping would identify what tally/bin combinations specify cell
:math:`n` for the cell filter variable. In this manner, it is not necessary to
check the phase space variables against each tally. Note that this technique
only applies to discrete filter variables and cannot be applied to energy
bins. For energy filters, it is necessary to perform a binary search on the
specified energy grid.
only applies to discrete filter variables and cannot be applied to energy,
angle, or change-in-angle bins. For these filters, it is necessary to perform
a binary search on the specified energy grid.
-----------------------------------------
Volume-Integrated Flux and Reaction Rates
@ -196,8 +197,9 @@ One important fact to take into consideration is that the use of a track-length
estimator precludes us from using any filter that requires knowledge of the
particle's state following a collision because by definition, it will not have
had a collision at every event. Thus, for tallies with outgoing-energy filters
(which require the post-collision energy) or for tallies of scattering moments
(which require the scattering cosine), we must use an analog estimator.
(which require the post-collision energy), scattering change-in-angle filters,
or for tallies of scattering moments (which require the scattering cosine of
the change-in-angle), we must use an analog estimator.
.. TODO: Add description of surface current tallies
@ -430,7 +432,7 @@ analytically. For one degree of freedom, the t-distribution becomes a standard
.. math::
:label: cauchy-cdf
c(x) = \frac{1}{\pi} \arctan x + \frac{1}{2}.
c(x) = \frac{1}{\pi} \arctan x + \frac{1}{2}.
Thus, inverting the cumulative distribution function, we find the :math:`x`
percentile of the standard Cauchy distribution to be

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@ -65,7 +65,7 @@ Now let's look at the pros and cons of Monte Carlo methods:
- **Pro**: Running simulations in parallel is conceptually very simple.
- **Con**: Because they related on repeated random sampling, they are
- **Con**: Because they rely on repeated random sampling, they are
computationally very expensive.
- **Con**: A simulation doesn't automatically give you the global solution