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Long-term assessment of airborne radiocesium after the Fukushima nuclearaccident: re-suspension from bare soil and forest ecosystems

机译:在福岛核卡卡卡卡卡卡纳卡卡纳卡核查核查后的长期评估:从裸土壤和森林生态系统重新悬浮

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The long-term effect of 137Cs re-suspension from contaminated soil and forests due to the Fukushima nuclear accident has been quantitatively assessed by numerical simulation, a field experiment on dust emission flux in a contaminated area (town of Namie, Fukushima prefecture), and air concentration measurements inside (Namie) and outside (city of Tsukuba, Ibaraki prefecture) the contaminated area. In order to assess the long-term effect, the full year of 2013 was selected to study just after the start of the field experiments. The 137Cs concentrations at Namie and Tsukuba were approximately 10?1–1 and 10?2–10?1?mBq?m?3, respectively. The observed monthly median concentration at Namie was 1 to 2 orders of magnitude larger than that at Tsukuba. This observed difference between the two sites was consistent with the simulated difference, indicating successful modeling of 137Cs re-suspension and atmospheric transport. The estimated re-suspension rate was approximately 10?6?day?1, which was significantly lower than the decreasing rate of the ambient gamma dose rate in Fukushima prefecture (10?4–10?3?day?1) as a result of radioactive decay, migration in the soil and biota, and decontamination. Consequently, re-suspension contributed negligibly in reducing ground radioactivity. The dust emission model could reproduce the air concentration of 137Cs in winter, whereas the summer air concentration was underestimated by 1 to 2 orders of magnitude. Re-suspension from forests at a constant rate of 10?7?h?1, multiplied by the green area fraction, could explain the air concentration of 137Cs at Namie and its seasonal variation. The simulated contribution of dust re-suspension to the air concentration was 0.7–0.9 in the cold season and 0.2–0.4 in the warm season at both sites; the remainder of the contribution was re-suspension from forest. The re-suspension mechanisms, especially through the forest ecosystems, remain unknown. This is the first study that provides a crude estimation of the long-term assessment of radiocesium re-suspension. Additional research activities should investigate the processes/mechanisms governing the re-suspension over the long term. This could be achieved through conducting additional field experiments and numerical simulations.
机译:由于数值模拟,137Cs核事故导致的污染土壤和森林的长期效果已经通过数值模拟,污染区域(Namie,Fukima县)的灰尘排放通量的田间试验内部(NAMIE)和外部的空气浓度测量(Tsukuba市,茨城地区)受污染区域。为了评估长期效应,2013年全年被选中在现场实验开始后立即学习。 Namie和Tsukuba的137Cs浓度约为10?1-1和10?2-10?1?MBQ?M?3。观察到的NAMIE的月度中位数浓度大于Tsukuba的数量级。这两个位点之间的观察到差异与模拟差异一致,表明137CS重新悬架和大气运输的成功建模。估计的重新悬架率约为10?6?日?1,其显着低于福岛县的环境γ剂量率降低(10?4-10?3?日?1)。放射性衰减,土壤和生物群的迁移,以及去污。因此,重新悬浮液在降低地放射性方面可忽略地贡献。粉尘发射模型可以在冬季再现137℃的空气浓度,而夏季空气浓度低估1至2幅度。从森林的恒定速率以10?7?H?1的恒定悬浮率,乘以绿色面积分数,可以解释Namie的137℃的空气浓度及其季节性变化。寒冷季节粉尘的模拟贡献为寒冷季节为0.7-0.9,在两个地方的温暖季节中为0.2-0.4;剩余的贡献是从森林重新暂停。重新悬架机制,特别是通过森林生态系统仍然未知。这是第一项研究,该研究提供了粗估计的卤陶铯再悬浮液的长期评估。其他研究活动应调查长期重新暂停的流程/机制。这可以通过进行额外的现场实验和数值模拟来实现。

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