首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Estimation of errors in the inverse modeling of accidental release of atmospheric pollutant: Application to the reconstruction of the cesium-137 and iodine-131 source terms from the Fukushima Daiichi power plant
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Estimation of errors in the inverse modeling of accidental release of atmospheric pollutant: Application to the reconstruction of the cesium-137 and iodine-131 source terms from the Fukushima Daiichi power plant

机译:大气污染物意外释放的逆模型反演中的误差估计:在福岛第一核电站的铯137和碘131来源项的重建中的应用

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A major difficulty when inverting the source term of an atmospheric tracer dispersion problem is the estimation of the prior errors: those of the atmospheric transport model, -those ascribed to the representativity of the measurements, those that are instrumental, and those attached to the prior knowledge on the variables one seeks to retrieve. In the case of an accidental release of pollutant, the reconstructed source is sensitive to these assumptions. This sensitivity makes the quality of the retrieval dependent on the methods used to model and estimate the prior errors of the inverse modeling scheme. We propose to use an estimation method for the errors' amplitude based on the maximum likelihood principle. Under semi-Gaussian assumptions, it takes into account, without approximation, the positivity assumption on the source. We apply the method to the estimation of the Fukushima Daiichi source term using activity concentrations in the air. The results are compared to an L-curve estimation technique and to Desroziers's scheme. The total reconstructed activities significantly depend on the chosen method. Because of the poor observability of the Fukushima Daiichi emissions, these methods provide lower bounds for cesium-137 and iodine-131 reconstructed activities. These lower bound estimates, 1.2 x 10~(16) Bq for cesium-137, with an estimated standard deviation range of 15%-20%, and 1.9 — 3.8 x 1017 Bq for iodine-131, with an estimated standard deviation range of 5%-10%, are of the same order of magnitude as those provided by the Japanese Nuclear and Industrial Safety Agency and about 5 to 10 times less than the Chernobyl atmospheric releases.
机译:逆转大气示踪剂扩散问题的源项时的主要困难是对先验误差的估计:大气传输模型的误差,归因于测量结果代表性的误差,有仪器意义的误差以及与先前误差有关的误差。关于变量的知识。在意外释放污染物的情况下,重构源对这些假设很敏感。这种敏感性使检索的质量取决于用于建模和估计逆建模方案的先验误差的方法。我们建议使用基于最大似然原理的误差幅度估计方法。在半高斯假设下,它近似地考虑了源的正假设。我们使用空气中的活动浓度将该方法应用于福岛第一核电站源项的估算。将结果与L曲线估计技术和Desroziers的方案进行比较。重建的活动总数很大程度上取决于所选的方法。由于福岛第一核电站排放的可观察性差,这些方法为铯137和碘131的重建活动提供了下限。这些下界估计值是铯137的1.2 x 10〜(16)Bq,估计标准偏差范围为15%-20%;碘131的下限估计值为1.9 — 3.8 x 1017 Bq,估计标准偏差范围为5%-10%的数量级与日本核工业安全局提供的数量级相同,比切尔诺贝利大气排放量低约5至10倍。

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