基于前向和后向扩散模拟的数据同化方法在事故核素释放源定位中的应用

Yuhan Xu, Shengjiang Fang, Xinwen Dong, Shuhan Zhuang
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摘要

意外放射性核素释放源定位对核应急和核决策至关重要,特别是在事先无法获得有关可能释放区域的可靠信息的情况下。为了在有限的测量次数下快速准确地确定源位置,本文提出了一种基于RIMPUFF模型中正反向色散模拟的两步数据同化方法。在第一步中,气象变量如风速被逆转,测量值被设置为几次反向RIMPUFF运行的来源。通过识别来自不同测点的反向羽流的重叠,可以大致确定离散到网格中的潜在区域。在第二步中,将第一步选择的网格设置为单位释放率的RIMPUFF正向运行的源,并通过最小化模拟数据和测量数据的基于相关性的函数来细化源位置。通过SCK-CEN 41Ar现场实验验证了该方法的有效性。利用所有测点的伽马剂量率数据,在野外实验的两天内分别以22.36m和30m的误差反演了源位置。与基于直接相关的方法相比,该方法在较短的时间内得到了满意的解。特别是在整个过程中不需要预先确定源释放率,这表明该方法可以方便地与其他源位置已知的源项反演方法相结合。因此,本文提出的两步数据同化方法具有较高的精度和效率,有望为核应急系统的进一步整合提供有用的工具。
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Source Localization of Accidental Radionuclide Release Using a Data Assimilation Method Based on Forward and Backward Dispersion Simulations
Source localization of accidental radionuclide release is crucial to nuclear emergency and decision making, especially when no reliable information about possible release regions can be previously obtained. To rapidly and accurately determine the source location with a limited number of measurements, this paper proposes a two-step data assimilation method based on forward and backward dispersion simulations in the RIMPUFF model. In the first step, meteorological variables such as wind speed are reversed and the measurements are set as sources for several backward RIMPUFF runs. By identifying the overlap of backward plumes originating from different measurement sites, potential regions discretized into grids can be roughly determined. In the second step, the grids selected by the first step are set as sources for forward RIMPUFF runs with unit release rate and the source location will be refined by minimizing a correlation-based function of simulated and measured data. The method is verified by SCK-CEN 41Ar field experiment. Using gamma dose rate data from all measurement sites, source location is retrieved with errors of 22.36m and 30m respectively on the two days of the field experiment. Compared with the direct correlation-based method, the proposed method achieves satisfactory solutions in an obviously shorter time. In particular, there is no need for predetermining the source release rate throughout the process, indicating that the method can conveniently combine with other source term inversion approaches whose source location is viewed as a known quantity. Therefore, the presented two-step data assimilation method here is potentially a useful tool with high accuracy and efficiency for further integration in nuclear emergency response system.
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