日本地球惑星科学連合2024年大会

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[J] ポスター発表

セッション記号 M (領域外・複数領域) » M-AG 応用地球科学

[M-AG34] ラジオアイソトープ移行:福島原発事故環境動態研究の新展開

2024年5月31日(金) 17:15 〜 18:45 ポスター会場 (幕張メッセ国際展示場 6ホール)

コンビーナ:津旨 大輔(筑波大学)、高橋 嘉夫(東京大学大学院理学系研究科地球惑星科学専攻)、桐島 陽(東北大学)、加藤 弘亮(筑波大学アイソトープ環境動態研究センター)

17:15 〜 18:45

[MAG34-P09] 高分解能化海洋拡散モデルを用いた福島第一原子力発電所事故による直接放出率の推定の改善

*津旨 大輔1、坪野 考樹2三角 和弘2 (1.筑波大学、2.電力中央研究所)

キーワード:福島第一原子力発電所事故、直接漏洩、放射性セシウム137、領域海洋モデル

A series of accidents at the Fukushima Daiichi Nuclear Power Station (F1NPS) following the 11 March 2011 earthquake and tsunami resulted in the release of radioactive substances into the ocean. In particular, the large amount of radioactive caesium released caused damage to the fishing industry, including voluntary restraints on fishing and restrictions on shipments. For environmental impact assessments and the formulation of measures to contain the effects of the accident, oceanic dispersion simulations are useful, based on the estimation of the supply routes and fluxes of radioactive materials. For direct release rate from the F1 NPS site, an estimation method was proposed using the results of nearby monitoring and the estimated seawater exchange rate by numerical simulation. However, the influence of the volume for setting the seawater exchange rate as not considered. Appropriate volumes need to be considered for use in estimating future accidents. In addition, underestimation of coastal directional transport was observed in the reproduction simulations for the F1NPS accident due to lack of resolution. A study using a higher resolution model was carried out to estimate the pathways and fluxes of radioactive material supply to the ocean and to understand the concentration distribution based on the ocean dispersion simulation. The conventional ocean dispersion model ROMS with a horizontal resolution of 1 km was increased to a horizontal resolution of 200 m. The optimal setting of the seawater exchange rate was investigated and the transport process of radiocesium in the coastal direction was improved. It was found that the conventional volume for determining the seawater exchange rate, including the locations of release sources and observation points, is optimal. This validity was confirmed by experimental equations from previous oceanic tracer-release experiments. In the estimation of future release rates, it was found necessary to establish an appropriate volume, e.g. depending on the distance between the locations of release sources and the observation point. In addition, improvements were observed in the transport process in the coastal direction due to the higher resolution, which improved the reproducibility. However, with a horizontal resolution of 200 m, there were problems with repeatability near ports, and it was found that a higher resolution using nesting or other methods would be desirable to deal with smaller-scale release than the F1NPS accident.