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首页> 外文期刊>Journal of Environmental Radioactivity >Atmospheric discharge and dispersion of radionuclides during the Fukushima Dai-ichi Nuclear Power Plant accident. Part Ⅱ: verification of the source term and analysis of regional-scale atmospheric dispersion
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Atmospheric discharge and dispersion of radionuclides during the Fukushima Dai-ichi Nuclear Power Plant accident. Part Ⅱ: verification of the source term and analysis of regional-scale atmospheric dispersion

机译:福岛第一核电站事故中的放射性核素在大气中的排放和扩散。第二部分:源项的验证和区域尺度大气扩散分析

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Regional-scale atmospheric dispersion simulations were carried out to verify the source term of ~(131)I and ~(137)Cs estimated in our previous studies, and to analyze the atmospheric dispersion and surface deposition during the Fukushima Dai-ichi Nuclear Power Plant accident. The accuracy of the source term was evaluated by comparing the simulation results with measurements of daily and monthly surface depositions (fallout) over land in eastern Japan from March 12 to April 30, 2011. The source term was refined using observed air concentrations of radionuclides for periods when there were significant discrepancies between the calculated and measured daily surface deposition, and when environmental monitoring data, which had not been used in our previous studies, were now available. The daily surface deposition using the refined source term was predicted mostly to within a factor of 10, and without any apparent bias. Considering the errors in the model prediction, the estimated source term is reasonably accurate during the period when the plume flowed over land in Japan. The analysis of regional-scale atmospheric dispersion and deposition suggests that the present distribution of a large amount of ~(137)Cs deposition in eastern Japan was produced primarily by four events that occurred on March 12, 15-16, 20, and 21-23. The ratio of wet deposition to the total varied widely depending on the influence by the particular event.
机译:进行了区域尺度的大气弥散模拟,以验证我们先前研究中估计的〜(131)I和〜(137)Cs的源项,并分析了福岛第一核电站期间的大气弥散和表面沉积事故。通过将模拟结果与2011年3月12日至2011年4月30日日本东部陆地上每日和每月表面沉积(沉降)的测量结果进行比较,评估了源项的准确性。使用观测到的放射性核素的空气浓度对源项进行了改进。现在计算和测量的每日表面沉积之间存在明显差异,并且现在可以获得以前的研究中未使用的环境监测数据的时期。预测使用精制源项的每日表面沉积大部分在10的范围内,并且没有任何明显的偏差。考虑到模型预测中的误差,在日本羽流流过陆地期间,估计的源项相当准确。对区域规模大气扩散和沉积的分析表明,目前日本东部大量〜(137)Cs沉积的分布主要是由3月12日,15日,16日,20日和21日发生的四次事件产生的23。湿沉积物与总沉积物的比率变化很大,具体取决于特定事件的影响。

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