Introduction
Global variance reduction is a classification of shielded computational problems. Global problems require not only the statistics of full-space fluxes or flux-related responses but also low statistical errors for all spaces. The global variance reduction problem is common in the design of new reactors, such as the Chinese Fusion Engineering Testing Reactor (CFETR) [1] and the solid fuel thorium molten salt reactor (TMSR-SF1) [2]. Currently, the geometric structures of the new reactors are relatively complex. When designing the shielding, the statistical error of all positions in the entire space must be small and relatively uniform to ensure that the design requirements for radiation protection are satisfied. If only the radiation parameters of the individual locations are calculated, the location of the radioactive leakage can be ignored. Therefore, there are global issues regarding the shielding design of new reactors. In the calculation space, the magnitude of the flux of the particles at different positions differs. Therefore, a corresponding variance reduction method for the global problem must be adopted to reduce the statistical error of the position with low flux. Finally, a more average statistical error distribution in the whole space is obtained, and simultaneously, it can save computing resources.
In the Monte Carlo calculation of a global problem, the MESH virtual grid is typically set to count the calculation results everywhere in the entire space. Therefore, the goal of Monte Carlo calculations of the global problem can be defined as: for a given relative statistical error
In conventional Monte Carlo transport, there are more particles in the region near the source, and the statistical error is small. In other words, the number of particles in the region far from the source is less owing to collisions and other reasons, and the statistical error is large. Although simply increasing the number of simulation particles can reduce the overall variance, the statistical error distribution is not uniform, and it is a waste of resources for particles to continue to be transported near the source, which does not meet the requirements of the global problem. Therefore, a corresponding global variance-reduction technique must be developed.
Principle and Current Situation of Global Variance Reduction
In a study on global variance reduction, Cooper and Larsen et al. [4] noted that a uniform Monte Carlo simulation of particle density can provide a uniform relative statistical error distribution, thus satisfying the goal of global variance reduction. Only particles arriving in the statistical region in the Monte Carlo simulations can contribute to the statistics. The number of Monte Carlo simulation particles in the statistical region determines the magnitude of the relative statistical error. This idea can also be explained by the statistical error calculation Eq. (1) for Monte Carlo simulations. Considering the statistical penetration probability
Relative statistical error is obtained by substituting the statistical error calculation formula:
The relative statistical error in this region is entirely determined by the number of particles
The various global variance reduction techniques that have emerged are also based on this conclusion, using different methods to achieve uniform Monte Carlo-simulated particle density distributions, including the coupling variance-reduction method based on the forward calculation represented by Cooper and Larsen [4] and the coupling variance reduction technique based on adjoint represented by FW-CADIS. The core idea of this method is to first perform one or two auxiliary calculations to generate a reasonable weight window parameter and realize a uniform Monte Carlo simulation of the particle density distribution.
Cooper and Larsen [4] guided the weight window parameter settings based on deterministic forward transport fluxes. For each mesh
Suppose that the central weight of the window or the survival weight
In 2007, Wagner proposed the FW-CADIS method based on CADIS for the global variance reduction of CADIS [5]. The computational goal of the global variance reduction problem is to obtain the calculation results of the global uniform convergence. For the Monte Carlo transport calculations, this can also be understood as obtaining a globally uniform Monte Carlo particle distribution. According to the conjugate transport theory, a conjugate source item
The equation shows that the FW-CADIS method applies the reciprocal of the total corresponding quantity estimate to weigh the conjugate source item. Therefore, the farther away from the physical source item, the greater the enhancement of the conjugate source item, and the conjugate source item increases accordingly. Additionally, the conjugate calculation process of the FW-CADIS method is consistent with that of the CADIS method. The difference between the two methods is that FW-CADIS requires an additional forward deterministic transport calculation before the conjugate calculation to provide the required weighted source term for the conjugate calculation. Therefore, the calculation effect of the FW-CADIS method depends on the accuracy of the conjugate flux provided by the deterministic program.
Other scholars conducted in-depth research on the global variance-reduction problem. Van Wijk [6] proposed a method for setting the weight window threshold according to the flux and statistical error. This method is entirely based on the I/O function of the MCNP Monte Carlo radiation transfer code family. Yuan [7] improved it by defining a novel "pseudo-source" based on the flux-based variance reduction method and proposed the PS-GVR method. To improve the efficiency of the source analysis, Qingquan [8] proposed a single-step Monte Carlo criticality method that eliminated the calculation of inactive cycles and achieved the highest computational efficiency through a mathematical optimization analysis. This method was used for the numerical analysis of transplutonium isotope production [9]. Meanwhile, the DeGVR method [10] was proposed to improve the efficiency of the shielding calculations. This method adopts the strategy of “density reduction + density extrapolation,” which can obtain global information quickly and is helpful for global variance reduction. Similar methods include PDMC [11], adaptive variance reduction [12] and SP3-coupled methods [13].
For a single probe, the FOM [14] is often used to measure computational efficiency. However, for global problems, because many detectors are used when obtaining MESH statistics, the formula for calculating the FOM factors is no longer applicable. This is a commonly used method to demonstrate the computational efficiency of counting the relative statistical error of each mesh or the probability distribution of the FOM factor and displaying it in the form of two-dimensional images. However, it is still significant to provide a quantitative number for characterizing computational efficiency. Therefore, researchers have attempted to improve the FOM factor formula to satisfy the requirements of global problems. In this study, the following formula is used to measure the computational efficiency of the global variance reduction method:
Limitations of the AIS Method
To solve the deep-penetration problem, Jiajin proposed the AIS method [15]. This method is based on importance sampling and statistical estimation; it introduces a virtual surface, divides the space into multilayer subspaces, generates virtual particles on the virtual surface to be transported to the next layer of the subspace, and performs automatic particle weight adjustment and quantity control. As shown in Fig. 1, the AIS method is as follows.
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(1)
(2) Virtual particles are generated on the virtual surface at the source event and at each collision event, and the number of virtual particles on the virtual surface is equaled to the number of source particles.
(3) The particles are killed if they reach the current virtual surface during transport.
(4) The virtual particles on the current virtual surface continue to be transported as source particles to the next subspace.
The AIS method uses a statistical estimation to generate virtual particles that continue to be transported as the source term of the subspace in the next layer. In this manner, more particles can be transported to a region far away from the source term, which solves the problem of large statistical errors in the region far away from the source term to a certain extent.
Suppose that the positive particle flow,
The particle current
Substituted into formula (8), then:
In summary, the number of virtual particles on an infinitesimal element is equal to the total number of virtual particles on the virtual surface multiplied by the ratio of the size of the forward particle flow on the infinitesimal element to the size of the total forward particle flow on the virtual surface. Therefore, the number of virtual particles was higher when the level of forward particle flow on the virtual surface was high; thus, the statistical error was smaller. Conversely, at low levels of forward particle flow, the number of virtual particles is lower; thus, the statistical error is larger. The level of the forward particle flow is determined by the problem, independent of the detector location. If the detector is in a region where the horizontal forward particle flow is small, the statistical error of the detector response will be large, and the AIS method will not have a good effect on variance reduction. Therefore, it can be concluded that the AIS method has certain limitations when applied to global problems.
In this study, the grid-AIS method is proposed for the global problem, and the Monte Carlo simulation particle density distribution is made uniform by constructing a corresponding virtual particle number control algorithm.
Grid-AIS Method
Transport Process
The key to achieving global variance reduction is that the Monte Carlo simulation particle density distribution should be uniform. A virtual surface divides an entire space into several subspaces. If the virtual particle density distribution on each virtual plane is uniform, then the Monte Carlo simulation particle density distribution in the entire space is approximately uniform. The grid-AIS method differs from the AIS method. The AIS method only keeps the number of virtual particles on each virtual surface the same, while the grid-AIS method keeps splitting according to the ratio
Based on the analysis, the grid-AIS method achieved a uniform virtual particle density distribution on the virtual surface using a meshing virtual particle number control algorithm. Small meshes of approximately equal areas were evenly divided on the virtual surface, and the number of virtual particles generated by each mesh was maintained. The transport process is as follows.
(1) In the initialization stage,
(2) During the source-term sampling and each collision event, the particle produces a virtual particle on the virtual surface. Mesh
(3) If a particle reaches the current virtual plane during transport, the source particle is eliminated.
(4) The virtual particle on the current virtual surface is returned as the source particle of the next subspace, and (2) continues to be transported.
For virtual surface
This differs from the rule in which the number of virtual particles on each virtual surface is the same as that in the traditional AIS method. The traditional AIS method considers the total flux of the space between virtual surfaces and requires only the same number of particles between the virtual surfaces to ensure that the statistical error of each virtual surface is as similar as possible. Global variance reduction must ensure that the statistical error of each mesh flux is as consistent as possible; therefore, the number of virtual particles on the virtual face must be adjusted according to the size of the virtual face.
This distinction is evident in the calculation of item-source global problems. The virtual polygon is generally divided into a series of spheres centered on the point source with radii ranging from small to large. The number of virtual particles in each layer in the traditional AIS method was the same. Although the total number of particles remains the same when the particles are transported to outer space, the number of particles per unit volume is insufficient owing to the increase in the area of the virtual surface. The virtual surface area of the grid-AIS method gradually increased from the inside to the outside, and the number of virtual particles also increased. When particles are transported to outer space, the number of particles per unit volume is consistent with that of the inner layer, which increases the statistical error.
When meshing, this paper requires that the mesh area of each virtual polygon is approximately the same, so if
Meshing and Virtual Particle Adjustment
In the grid-AIS method, virtual particles must be generated on the virtual plane during source item sampling and each collision event, and mesh
The commonly used planes, cylindrical surfaces, and spherical surfaces must be strictly meshed by area. Figure 2 shows the meshing of the cylindrical virtual surfaces.
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(1) The mesh division of the virtual plane surface was relatively simple. Suppose that its length in the
(2) The division of the cylindrical surface was similar to that of the plane. Divide evenly in the two directions of the azimuth
(3) For the spherical case, if the mesh is divided uniformly in two directions according to the polar angle
In summary, this paper adopts the way that the polar angle
For the polar angle mesh
Then,
Thus, the area of each mesh was approximately the same and the shape of the mesh was closer to a square, which further reduced the flux difference within the mesh.
When mesh
After determining the mesh
For other cases of nonplanar, cylindrical, and spherical surfaces, the modeling of virtual surfaces may include intersection, concatenation, and complementary cases, which are more complex and make it difficult to divide the mesh strictly into equal areas. In this study, an approximate division method was adopted, and statistical MESH was used to divide the virtual surface. The MESH number where the virtual particle is located is used as the virtual face mesh number, and the number of virtual particles per virtual face mesh is maintained in proportion to the volume of the MESH. Here, the volume of the MESH is considered to be approximately proportional to the area of the virtual surface contained in it.
Table 1 shows the comparison between the AIS and grid-AIS methods.
Method | Virtual particle generation | Virtual particle number control | Variance reduction parameter |
---|---|---|---|
AIS Method | Generate virtual particles on the virtual surface along the direction of particle motion during source sampling and each collision event | Maintain an equal number of particles on each virtual surface | Only need to set virtual surface position parameters |
Grid-AIS Method | Maintain an equal number of virtual particles per mesh on each virtual surface | Need to set virtual surface position parameters and grid size parameters |
Currently, the grid-AIS method is implemented in the MCShield program. MCShield is a neutron/photon/electron-coupled transport Monte Carlo program for radiation shielding calculations independently developed by the Radiation Protection and Environmental Protection Laboratory of Tsinghua University. The MCShield program can simulate neutron, photon, and electron coupled transport with massively parallel computation functions and can efficiently and accurately solve the deep penetration problem and the complex shielding problem of the Monte Carlo variance reduction technique. At the same time, the software also contains a variety of powerful pre- processing and post-processing modules, such as CAD geometry conversion, parametric geometry modeling, visualization parameter setting, particle trajectory display and three-dimensional dose display. The program was validated against dozens of international benchmarks [21].
In summary, compared with other methods, the grid-AIS method proposed in this paper for global problems has the following main innovations. (1) For the global variance reduction problem, the weight window method is currently widely used. The weight window method usually divides the grid in the entire space and sets the weight window parameters of each grid. Furthermore, the effect of variance subtraction computation was highly correlated with the quality of the weight window parameters. In contrast to the weight window method, the grid-AIS method must only set a few variance reduction parameters, such as the virtual surface position and grid size, which is convenient for users. (2) In the CADIS method, a deterministic method must be used for the adjoint calculation in a single calculation to calculate the parameters of the weight window. Therefore, the entire calculation process requires two sets of geometric models, Monte Carlo programs, and determinism, which makes the shielding calculation very difficult. The grid-AIS method does not require adjoint calculations and only requires one Monte Carlo forward calculation to obtain the result, which is convenient for users.
Unbiased Description
The general transport architecture of the grid-AIS method was the same as that of the AIS method, whereas the unbiased nature of the AIS method was demonstrated and is not repeated here. The number of virtual particles in the virtual surface mesh was controlled using roulette and splitting, and the process was unbiased. The amount of particle transport between virtual surfaces varies with the virtual surface area, which is different from the AIS method. However, this process is achieved by gambling splitting, the weights are adjusted accordingly, and the overall process is unbiased. Overall, the Grid-AIS method was unbiased.
VENUS-III International Benchmark Problem
Description of Benchmark
The VENUS-III [22] experimental reactor is a low-flux thermal neutron reactor that was built in 1964 to study reactor core designs and the irradiation damage of nuclear materials. This provides benchmark experiments for numerical simulation programs. The 1/4 core model of the VENUS-III reactor is shown in Fig. 3, and it consists of 639 fuel rods and 11 control rods, with dimensions of 73.65 cm length, 37.80 cm width, and 37.80 cm height. In the figure, the light-grey area represents the control rods, whereas the other parts are fuel rods. The grey parts represent fuel rods enriched to 4% burnable poison, the white parts represent fuel rods enriched to 3% burnable poison, and the dark grey parts represent fuel rods enriched to 3% burnable poison.
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The VENUS-III reactor plane diagram is shown in Fig. 3. It is divided into nine horizontal regions from the center to the left as follows: (1) the central water channel outside the core; (2) the inner layer baffle outside the core (stainless steel thickness of 2.858 cm); (3) the core fuel area (4% fuel rods and 3.3% fuel rods); (4) the outer layer baffle outside the core (stainless steel thickness of 2.858 cm); (5) the water reflector outside the core (minimum water thickness of 2.169 cm); (6) the outer core basket (stainless steel thickness of 4.99 cm); (7) the cooling water layer outside the basket (water thickness of 5.80 cm); (8) the thermal shield (stainless steel thickness of 6.72 cm); and (9) the reactor pressure vessel (stainless steel). From the center, it was divided into eight regions, from bottom to top, as follows: (1) the lower water region inside the pressure vessel, (2) the lower core support structure, (3) the outer bottom support frame of the core, (4) the lower internal reflector of the core, (5) the core fuel area, (6) the upper internal reflector of the core, (7) the outer upper support frame of the core, and (8) the upper water region inside the pressure vessel.
Calculation Results
The source term in the core region consists of fission neutrons with a Watt spectrum and isotropic distribution. The source term is distributed within the cylindrical fuel rods, and the sampling probabilities for different positions within each fuel rod vary. In this case, the neutron flux in the computational region was calculated using MESH tallies. The MESH grid size is 20.00 mm × 20.00 mm × 20.00 mm, with 46, 46, and 85 MESH grids in the X, Y, and Z directions, respectively. In this study, three methods were compared: AIS, grid-AIS, and traditional Monte Carlo methods. Nine cylindrical virtual surfaces were set up for the grid-AIS and AIS methods. The center of the virtual surface of the cylinder moved down from the center of the core (0, 0, 0) to (0, 0, -400 mm), and the radius of the virtual surface of the cylinder increased from 500 to 900 mm. Virtual particles were generated on the top, bottom, and lateral surfaces of the cylinder. In the Grid-AIS method, grid size parameter d=40, 80, and 160 mm. Table 2 shows the calculation results of the VENUS-III international benchmark.
Method | NPS | CPU Time (min) | Mean absolute error | MESH average statistical error (%) |
---|---|---|---|---|
Conventional Monte Carlo | 1.00 ×108 | 460 | 6.29×10-8 | 24.00 |
1.00×107 | 42 | 2.50×10-7 | 36.89 | |
AIS | 1.00×107 | 330 | 1.41×10-7 | 7.58 |
Grid-AIS | 1.00×107 | 352 | 1.42×10-7 | 6.80 |
Table 3 and Fig. 4 show that both the grid-AIS and AIS methods showed significant improvements in computational results, compared to the traditional Monte Carlo algorithm. The average statistical error of the MESH grid decreased from 0.24 to 0.07, demonstrating the effectiveness of the AIS method. Compared to the AIS method, the Grid-AIS method showed the following improvements in the computational results: the percentage of MESH grids with a statistical error greater than 0.80 decreased from 0.31% to 0.02%; the percentage of MESH grids with a statistical error greater than 0.50 decreased from 1.56% to 0.33%; the percentage of MESH grids with a statistical error less than 0.30 increased from 95.98% to 98.40%; and the percentage of MESH grids with a statistical error less than 0.10 increased from 83.14% to 87.58%. Furthermore, the variance in the statistical errors for the MESH grids in the grid-AIS method decreased from 1.08% to 0.38%, representing a 64.00% reduction. This indicates that the grid-AIS method reduced the global variance problem. In addition, by comparing the calculation results for different grid size parameters, we found that the calculation results for d=80 and 160 mm were better than those for d=40 mm. Generally, the grid size parameter should match the size of the MESH grid and the number of simulated particles. A grid-size parameter that is either too large or too small affects the effectiveness of the grid-AIS method.
Method | Variance of MESH statistical error (%) | Proportion of grids with statistical error > 30% | Proportion of grids with statistical error < 10% |
---|---|---|---|
Conventional Monte Carlo | 4.36 | 30.67% | 27.43% |
5.98 | 62.55% | 20.65% | |
AIS | 1.08 | 4.02% | 83.14% |
Grid-AIS | 0.38 | 1.60% | 87.58% |
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In this section, the effectiveness of the grid-AIS method is validated using the VENUS-III international benchmark problem. However, in this benchmark problem, the radius of the computational region was relatively small compared to the core radius, resulting in minimal differences in the surface areas of the different cylindrical virtual surfaces. In addition, because of the relatively uniform distribution of geometry and materials in the VENUS-III international benchmark questions, the calculation results of the AIS method were already good, with little room for improvement. Therefore, based on an actual reactor structure, this study proposes a self-designed reactor shielding example in which pipes and other structures are added to increase the geometric anisotropy, and the grid-AIS method is further verified.
Self-Design Reactor Shielding Example
Example Description
In this section, the grid-AIS method is validated using a self-designed reactor-shielding algorithm. The geometric model is shown in Fig. 5. The core is a cylinder with a radius of 0.50 m and height of 1 m, and its lower surface is flush with the bottom of the water layer. Outside the core is a water layer with a radius of 1.50 m and height of 4.00 m. Outside of the water layer is a concrete layer with a thickness of 0.50 m, and outside the vacuum boundary. Radial and axial air pipes with a radius of 0.10 m pass through the water layer and concrete. The source was uniformly distributed in the core area, the energy distribution was a Watt fission spectrum, and the direction was isotropic. The calculation example has a thick shielding body, pipes, and other structures with strong anisotropy, which is a typical shielding calculation problem with difficult convergence of global counting, and can be used to test the computational capability of the Monte Carlo method under a more anisotropic geometry.
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The subbody fluxes in full space were counted using MESH with a mesh size of 4.40 cm × 4.40 cm × 4.40 cm and a total of 568,800 meshes. Calculations were performed separately using the original MCShield, AIS, and Grid-AIS methods. The AIS virtual surfaces were 18 spherical surfaces with the center of the core as the center of the sphere, from the inside to the outside, and the radii of the spherical surfaces were spaced 20.00 cm apart. Owing to the limitation of the overall geometric boundary, the spheres are not closed spheres, and the starting and ending polar angles are determined by the spheres and vacuum geometric boundary.
The computing platform used in this study is a multinode computing cluster with two 18-core processors per node: Intel Xeon E5-2699 V3 @2.3 GHz CPU with 64 GB of memory.
The calculation results are listed in Tables 4~5. To facilitate comparison of the statistical errors, the number of simulated particles was controlled for each method. The simulation times of the methods are relatively close; therefore, the magnitude of the statistical error represents the computational efficiency. Using 100 processes for parallel computation, the CPU time listed in Table 1 is the sum of the running times of each process. The computational efficiency was measured using the FOM factor applied to a global problem.
Method | NPS | CPU time (min) | Mean absolute error | Mean relative statistical error (%) | FOM (min-1) |
---|---|---|---|---|---|
Conventional Monte Carlo | 1.00×1010 | 6.54×104 | 8.17×10-10 | 62.20 | 3.95×10-5 |
AIS | 6.00×108 | 7.37×104 | 1.15×10-9 | 11.90 | 9.56×10-4 |
Grid-AIS | 1.00×108 | 7.81×104 | 2.78×10-9 | 3.30 | 1.15×10-2 |
Method | Variance of MESH statistical error (%) | Proportion of grids with statistical error > 30% | Proportion of grids with statistical error < 10% |
---|---|---|---|
Conventional Monte Carlo | 7.13 | 33.99% | 45.09% |
AIS | 3.80 | 14.81% | 69.28% |
Grid-AIS | 1.67 | 5.12% | 86.95% |
It can be seen from the parameter results that the average relative statistical error of the conventional Monte Carlo method was as high as 62.20%, and the results were unreliable. The grid-AIS method has an average statistical error of 3.30%, which is less than 5.00% and is acceptable for shielding calculations. In addition, the FOM factor of the grid-AIS method was approximately 12 times higher than that of the AIS method, and 290 times higher than that of the conventional Monte Carlo method.
Example Results
Sectional views of the statistical MESH flux are shown in Figs. 6, 7, and 8. The top of each figure represents the X-Z plane, which is the plane through the vertical air duct. The figure below shows the YZ-plane perpendicular to the horizontal air duct. The left and right images of the two-dimensional images in Figs. 6, 7, and 8 have the same meaning, and the flux is displayed in logarithmic coordinates. The colors represent the fluxes. Red indicates the highest, blue indicates the lowest, and the span between each contour is one order of magnitude.
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The maximum flux attenuation was approximately 10-19. The flux decreased exponentially with the distance from the core in the range near the core. In the upper area, far away from the core, the flux was higher in the air duct and near the air duct because of the influence of the two air ducts, and the flux was lower in other areas. The conventional Monte Carlo method has many empty meshes at positions far away from the source and only has values near the air pipe, which indicates that the conventional Monte Carlo method cannot transport particles to positions far away from the core. By contrast, the AIS and grid-AIS methods essentially have no empty meshes.
The relative statistical errors of the MESH fluxes are shown in the cross-sectional plots in Figs. 9, 10, and 11, and the relative statistical errors are displayed in linear coordinates. For display purposes, the width of each color was 2.50%, from 0.00 to 20.00%, and colors above 20.00% were red, for a total of nine colors. As shown in the illustration, the conventional Monte Carlo method yields poor results in the upper part of the space away from the core, where the statistical error is lower than 20.00% only near the vertical air duct and higher than 20.00% everywhere else. The AIS method has a smaller statistical error near the air ducts in the upper part of the space away from the core, and a larger statistical error at a location away from the ducts. Combined with the flux cut diagram, the statistical error changes in size with the same pattern of change in the flux size. The statistical error was smaller when the flux level was high on the virtual surface, and vice versa. This is consistent with the results of a previous analysis conducted using the AIS method. As shown in Fig. 11, the statistical errors of the Grid-AIS method were smaller and more uniformly distributed than those of the AIS method, and the statistical errors were also smaller at locations far from the air ducts. This indicates the strategy of the grid-AIS method to ensure that the virtual particles are uniformly distributed on the virtual surface.
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To verify the correctness of the grid-AIS method, the relative deviation results of the grid-AIS method and results of the conventional Monte Carlo and AIS methods are plotted separately, as shown in Figs. 12-13; the colors used in the plots have the same meaning as in the statistical error plots. The figure shows that the relative deviation of the Grid-AIS method results from the conventional Monte Carlo and AIS method results near the core and inside the vertical air ducts is low, below 2.50%, which further verifies the correctness of the Grid-AIS method. By contrast, regions with higher relative deviations also have higher statistical errors and are therefore not meaningful for comparison.
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The cumulative probability distribution functions with frequency histograms of the statistical errors for each MESH for the three methods are shown in Fig. 14. The horizontal coordinates represent the relative statistical error, which ranged from 0.00% to 100.00%. The vertical coordinate is the cumulative probability distribution function of the relative error, representing the proportion of MESH below a certain relative statistical error relative to the total mesh. As shown in Fig. 14a, the statistical error of the grid-AIS method increases most steeply, and the meshes with statistical errors below 10.00% account for approximately 94.00%. The AIS method, on the other hand, has approximately 77.00% of the meshes with statistical errors below 10.00%. The conventional Monte method was even lower, accounting for approximately 20.00%. In addition, the statistical errors of the conventional Monte Carlo and AIS methods show a step increase of approximately 100.00% because these two methods have partially empty meshes.
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Figure 14b presents the frequency histograms of the relative statistical errors for each MESH. Relative statistical errors were divided into 1.00% intervals, and the number of MESHs within each relative statistical error segment was counted as a percentage of the total number of MESH. To make the graph more concise, the vertical boundaries of each statistical error segment in the histogram are hidden. As shown in Fig. 14b, the statistical errors of the Grid-AIS method were relatively concentrated, and the proportion of higher statistical errors was much lower than those of the conventional Monte Carlo and AIS methods. The spatial distribution of the Monte Carlo simulation particle density in the grid-AIS method is more uniform; therefore, the statistical error is more uniform in the whole space and is reflected in the frequency histogram, and the statistical error distribution shows a trend of being more concentrated.
In addition, it can be found from the data that the statistical error distribution of the conventional Monte Carlo and AIS methods has a more consistent trend in the areas with larger relative statistical errors. Although the AIS method reduces the overall statistical error by introducing a virtual surface, it does not change the Monte Carlo simulation particle density distribution on the virtual surface; therefore, the error change trend is close to that of the conventional Monte Carlo method. A relative statistical error of 100.00% represents no statistical value, that is, an empty mesh. In the figure, the vertical coordinate at a 100.00% relative statistical error represent the ratio of the number of empty meshes to the total number of meshes. This ratio was approximately 50.00% for the conventional Monte Carlo method, approximately 2.00% for the AIS, and 0.00% for the grid-AIS, representing no empty mesh.
Conclusion
Based on the basic AIS method, a Grid-AIS method applicable to global variance reduction is proposed in this paper and implemented in the Monte Carlo program MCShield.
In this study, the grid-AIS method was validated using the VENUS-III international benchmark problem and a self-shielding reactor calculation. The results demonstrated that the grid-AIS method produced accurate computational results for addressing the global variance reduction problem, thereby confirming the correctness of the grid-based AIS method. In both validation cases, there was a reduction of approximately 60.00% in the variance of the statistical errors of the computed results. The grid-AIS method also exhibited a computational efficiency approximately one order of magnitude higher than that of the AIS method and approximately two orders of magnitude higher than that of the conventional Monte Carlo method. These results validate the effectiveness of the grid-AIS method.
In summary, the Grid-AIS method can better solve the global problem in shielding calculations and is an extension and supplement to the AIS method.
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.The authors declare that they have no competing interests.