首页> 外文期刊>Journal of oceanography >134Cs and 137Cs in the North Pacific Ocean derived from the March 2011 TEPCO Fukushima Dai-ichi Nuclear Power Plant accident, Japan. Part two: estimation of 134Cs and 137Cs inventories in the North Pacific Ocean
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134Cs and 137Cs in the North Pacific Ocean derived from the March 2011 TEPCO Fukushima Dai-ichi Nuclear Power Plant accident, Japan. Part two: estimation of 134Cs and 137Cs inventories in the North Pacific Ocean

机译:北太平洋的134C和137C来自2011年3月日本东京电力公司福岛第一核电站事故。第二部分:北太平洋134C和137C清单的估算

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We estimated the inventories of radiocaesium released by the Tokyo Electric Power Company Fukushima Dai-ichi Nuclear Power Plant (FNPP1) accident to the North Pacific Ocean by using compiled data and model simulations. By comparing the observed inventories with model-simulated results, we obtained 12–15 PBq of 137Cs for the atmospheric deposition released by the FNPP1 accident in the North Pacific Ocean. Before the Fukushima accident, 137Cs activity in the North Pacific Ocean was about 69 PBq. Therefore, the 12–15 PBq of 137Cs newly added by atmospheric deposition together with the 3.5?±?0.7 PBq added by direct discharge increased the total 137Cs inventory in the North Pacific Ocean by 22–27?%. We also estimated the total amount of 137Cs released to the atmosphere to be 15–20?PBq, and the total amount of 137Cs released to the environment to be 19–24 PBq, respectively. Observed 134Cs to 137Cs activity ratio at the time of accident was close to 1 and extremely uniform, therefore, the total amount of 134Cs deposition in the North Pacific Ocean, that of released to the atmosphere, that of direct discharge to the ocean and that of released to the environment were the same amounts as those of 137Cs.
机译:通过使用汇总数据和模型模拟,我们估算了东京电力公司福岛第一核电站事故(FNPP1)泄漏到北太平洋的放射性铯的存量。通过将观测到的清单与模型模拟的结果进行比较,我们得出了FNPP1事故在北太平洋释放的137Cs的12-15 PBq。福岛事故之前,北太平洋的137Cs活度约为69 PBq。因此,大气沉积新增加的137Cs的12-15 PBq和直接排放增加的3.5?±?0.7 PBq一起使北太平洋137Cs的总库存增加了22-27%。我们还估计释放到大气中的137Cs总量为15–20?PBq,释放到环境中的137Cs总量分别为19-24PBq。事故发生时观察到的134Cs与137Cs活度比接近于1,并且非常均匀,因此,北太平洋中134Cs的沉积总量,释放到大气中的总量,直接排放到海洋的总量和释放到环境中的数量与137Cs的数量相同。

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