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Journal Articles

Impact of uncertainty reduction on lead-bismuth coolant in accelerator-driven system using sample reactivity experiments

Katano, Ryota; Oizumi, Akito; Fukushima, Masahiro; Pyeon, C. H.*; Yamamoto, Akio*; Endo, Tomohiro*

Nuclear Science and Engineering, 198(6), p.1215 - 1234, 2024/06

 Times Cited Count:0 Percentile:0.01(Nuclear Science & Technology)

In this study, we have demonstrated that data assimilation using lead and bismuth sample reactivities measured in the Kyoto University Critical Assembly A-core can successfully reduce the uncertainty of the coolant void reactivity in accelerator-driven systems derived from inelastic-scattering cross-sections of lead and bismuth. We re-evaluated and highlighted the experimental uncertainties and correlations of the sample reactivities for the data assimilation formula. We used the MCNP6.2 code to evaluate the sample reactivities and their uncertainties, and performed data assimilation using the reactor analysis code system MARBLE. The high-sensitivity coefficients of the sample reactivities to lead and bismuth allowed us to reduce the cross-section-induced uncertainty of the void reactivity of the accelerator-driven system from 6.3% to 4.8%, achieving a provisional target accuracy of 5% in this study. Furthermore, we demonstrated that the uncertainties arising from other dominant factors, such as minor actinides and steel, can be effectively reduced by using integral experimental data sets for the unified cross-section dataset ADJ2017.

Journal Articles

An Estimation method for an unknown covariance in cross-section adjustment based on unbiased and consistent estimator

Maruyama, Shuhei; Endo, Tomohiro*; Yamamoto, Akio*

Journal of Nuclear Science and Technology, 60(11), p.1372 - 1385, 2023/11

 Times Cited Count:1 Percentile:63.33(Nuclear Science & Technology)

Journal Articles

GPU optimization of lattice Boltzmann method with local ensemble transform Kalman filter

Hasegawa, Yuta; Imamura, Toshiyuki*; Ina, Takuya; Onodera, Naoyuki; Asahi, Yuichi; Idomura, Yasuhiro

Proceedings of 13th Workshop on Latest Advances in Scalable Algorithms for Large-Scale Heterogeneous Systems (ScalAH22) (Internet), p.10 - 17, 2022/00

The ensemble data assimilation of computational fluid dynamics simulations based on the lattice Boltzmann method (LBM) and the local ensemble transform Kalman filter (LETKF) is implemented and optimized on a GPU supercomputer based on NVIDIA A100 GPUs. To connect the LBM and LETKF parts, data transpose communication is optimized by overlapping computation, file I/O, and communication based on data dependency in each LETKF kernel. In two dimensional forced isotropic turbulence simulations with the ensemble size of $$M=64$$ and the number of grid points of $$N_x=128^2$$, the optimized implementation achieved $$times3.85$$ speedup from the naive implementation, in which the LETKF part is not parallelized. The main computing kernel of the local problem is the eigenvalue decomposition (EVD) of $$Mtimes M$$ real symmetric dense matrices, which is computed by a newly developed batched EVD in EigenG. The batched EVD in EigenG outperforms that in cuSolver, and $$times64$$ speedup was achieved.

Journal Articles

Modeling the drift of Japan Tsunami Marine Debris (JTMD); An Application of high computing simulation and data assimilation

Kamachi, Masafumi*; Ishikawa, Yoichi*; Kawamura, Hideyuki; Maximenko, N.*; Hafner, J.*; MacFadyen, A.*

Techno-Ocean 2016 (Techno-Ocean), p.599 - 602, 2016/10

The tsunami that followed the Great East Japan Earthquake in March 2011 caused a large amount of debris to flow out into the North Pacific, mainly from the Tohoku district, Japan. We conducted drift simulations to monitor and predict the trajectory of the tsunami debris. The results suggested that the tsunami debris was mainly transported eastward by the Kuroshio Extension and prevailing westerly winds, spreading in a north-south direction by ocean eddies and storms. As for the tsunami debris with high buoyancy, it was shown to be strongly influenced by ocean surface winds as well as ocean currents, reaching the west coast of the North American continent around the fall of 2011.

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