EGU25-14834, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-14834
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 28 Apr, 14:00–15:45 (CEST), Display time Monday, 28 Apr, 14:00–18:00
 
Hall X4, X4.122
Simulation of the impact assessment of the discharge of ALPS treated water into the ocean
Daisuke Tsumune1, Takaki Tsubono2, Kazuhiro Misumi2, Tomomi Okamura3, Hiroshi Abe3, Hiroaki Kato1, and Yuichi Onda1
Daisuke Tsumune et al.
  • 1Center for Research in Radiation, Isotopes, and Earth System Sciences, University of Tsukuba, Tsukuba, Japan (tsumune.daisuke.gw@u.tsukuba.ac.jp)
  • 2Central Research Institute of Electric Power Industry, Abiko, Japan
  • 3Decommissioning Archive Center, Tokyo Electric Power Company Holdings, Inc.

As part of the decommissioning work at the Fukushima Daiichi Nuclear Power Plant, the discharge of ALPS-treated water began in August 2023. ALPS-treated water contains not only H-3, but also other nuclides, albeit at extremely low concentrations. ALPS-treated water is treated so that the total of the concentration ratios of the 30 target nuclides is less than 1, and then diluted so that the H-3 concentration is less than 1500 Bq/L before being discharged. Prior to discharge, a radiation impact assessment was carried out by TEPCO. This assessment used a marine dispersion model that had been verified using observation results for Cs-137 that had leaked out as a result of the Fukushima Daiichi Nuclear Power Plant accident.

The ocean dispersion model was a 1 km x 1 km ROMS model with a variable mesh that was refined to 200 m x 200 m in the vicinity. It was driven by meteorological reanalysis data from the Japan Meteorological Agency, and data assimilation was performed using JCOPE2M ocean reanalysis data to reproduce the Kuroshio and mesoscale eddies.

In this assessment, a H-3 concentration of 0.1 Bq/L was used as the background concentration from atmospheric nuclear testing. However, a concentration of 1 Bq/L of H-3 was observed even before the release, and this is thought to be due to the influence of the supply from the power plant site or surrounding areas, or from rivers. After taking into account the influence of these background concentrations, the results of the model simulations were verified against the results of the monitoring of H-3 concentrations. Because the rate of release of the ALPS processed water was small, the range of influence of the monitoring of H-3 concentrations was limited, but the verification results were consistent. It is necessary to determine the average distribution by continuing to monitor in the future.

How to cite: Tsumune, D., Tsubono, T., Misumi, K., Okamura, T., Abe, H., Kato, H., and Onda, Y.: Simulation of the impact assessment of the discharge of ALPS treated water into the ocean, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-14834, https://doi.org/10.5194/egusphere-egu25-14834, 2025.