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首页> 外文期刊>Journal of Environmental Radioactivity >Automatic plume episode identification and cloud shine reconstruction method for ambient gamma dose rates during nuclear accidents
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Automatic plume episode identification and cloud shine reconstruction method for ambient gamma dose rates during nuclear accidents

机译:核事故期间环境伽马剂量率的自动羽状发作识别和云雾重建方法

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Ambient gamma dose rate (GDR) is the primary observation quantity for nuclear emergency management due to its high acquisition frequency and dense spatial deployment. However, ambient GDR is the sum of both cloud and ground shine, which hinders its effective utilization. In this study, an automatic method is proposed to identify the radioactive plume passage and to separate the cloud and ground shine in the total GDR. The new method is evaluated against a synthetic GDR dataset generated by JRODOS (Real Time On-line Decision Support) System and compared with another method (Hirayama, H. et al., 2014. Estimation of I-131 concentration using time history of pulse height distribution at monitoring post and detector response for radionuclide in plume. Transactions of the Atomic Energy Society of Japan 13:119-126, in Japanese (with English abstract)). The reconstructed cloud shine agrees well with the actual values for the whole synthetic dataset (1451 data points), with a very small absolute fractional bias (FB = 0.02) and normalized mean square error (NMSE = 2.04) as well as a large correlation coefficient (r = 0.95). The new method significantly outperforms the existing one (more than 95% reduction of FB and NMSE, and 61% improvement of the correlation coefficient), mainly due to the modification for high deposition events. The code of the proposed methodology and all the test data are available for academic and non-commercial use. The new approach with the detailed interpretation of the in-situ environment data will help improving the ability of off-site source term inverse estimation for nuclear accidents. (C) 2017 Elsevier Ltd. All rights reserved.
机译:由于环境伽玛剂量率(GDR)的获取频率高且空间部署密集,因此是核应急管理的主要观察量。但是,环境GDR是云层和地面闪耀的总和,这阻碍了其有效利用。在这项研究中,提出了一种自动方法来识别放射性羽流通道并分离总GDR中的云层和地面光泽。该新方法是根据JRODOS(实时在线决策支持)系统生成的合成GDR数据集进行评估的,并与另一种方法进行了比较(Hirayama,H.等,2014。使用脉冲的时间历史估算I-131浓度)监测柱的高度分布和烟羽中放射性核素的检测器响应(日本原子能学会学报,日本,日语:13:119-126)。重建的云层光泽与整个合成数据集的实际值(1451个数据点)非常吻合,绝对分数偏差(FB = 0.02)很小,归一化均方误差(NMSE = 2.04),并且相关系数很大(r = 0.95)。新方法明显优于现有方法(FB和NMSE降低了95%以上,相关系数提高了61%),这主要是由于对高沉积事件进行了修改。拟议方法的代码和所有测试数据可用于学术和非商业用途。带有对现场环境数据的详细解释的新方法将有助于提高核事故的非现场源项逆估计能力。 (C)2017 Elsevier Ltd.保留所有权利。

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