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海洋生物群对放射性核素摄取的动态建模:应用于福岛核电站事故

Dynamic modelling of radionuclide uptake by marine biota: application to the Fukushima nuclear power plant accident.

作者信息

Vives i Batlle Jordi

机构信息

Belgian Nuclear Research Centre (SCK•CEN), Boeretang 200, 2400 Mol, Belgium.

出版信息

J Environ Radioact. 2016 Jan;151 Pt 2:502-11. doi: 10.1016/j.jenvrad.2015.02.023. Epub 2015 Mar 13.

Abstract

The dynamic model D-DAT was developed to study the dynamics of radionuclide uptake and turnover in biota and sediments in the immediate aftermath of the Fukushima accident. This dynamics is determined by the interplay between the residence time of radionuclides in seawater/sediments and the biological half-lives of elimination by the biota. The model calculates time-variable activity concentration of (131)I, (134)Cs, (137)Cs and (90)Sr in seabed sediment, fish, crustaceans, molluscs and macroalgae from surrounding activity concentrations in seawater, with which to derive internal and external dose rates. A central element of the model is the inclusion of dynamic transfer of radionuclides to/from sediments by factorising the depletion of radionuclides adsorbed onto suspended particulates, molecular diffusion, pore water mixing and bioturbation, represented by a simple set of differential equations coupled with the biological uptake/turnover processes. In this way, the model is capable of reproducing activity concentration in sediment more realistically. The model was used to assess the radiological impact of the Fukushima accident on marine biota in the acute phase of the accident. Sediment and biota activity concentrations are within the wide range of actual monitoring data. Activity concentrations in marine biota are thus shown to be better calculated by a dynamic model than with the simpler equilibrium approach based on concentration factors, which tends to overestimate for the acute accident period. Modelled dose rates from external exposure from sediment are also significantly below equilibrium predictions. The model calculations confirm previous studies showing that radioactivity levels in marine biota have been generally below the levels necessary to cause a measurable effect on populations. The model was used in mass-balance mode to calculate total integrated releases of 103, 30 and 3 PBq for (131)I, (137)Cs and (90)Sr, reasonably in line with previous estimates.

摘要

动态模型D-DAT是为研究福岛事故刚发生后生物群和沉积物中放射性核素的摄取和周转动力学而开发的。这种动力学由放射性核素在海水/沉积物中的停留时间与生物群消除的生物半衰期之间的相互作用决定。该模型根据海水中的周围活度浓度计算海底沉积物、鱼类、甲壳类动物、软体动物和大型藻类中(131)I、(134)Cs、(137)Cs和(90)Sr随时间变化的活度浓度,据此得出内照射和外照射剂量率。该模型的一个核心要素是通过对吸附在悬浮颗粒上的放射性核素的消耗、分子扩散、孔隙水混合和生物扰动进行因式分解,纳入放射性核素在沉积物中的动态转移,这由一组简单的微分方程与生物摄取/周转过程相结合来表示。通过这种方式,该模型能够更真实地再现沉积物中的活度浓度。该模型用于评估福岛事故急性期对海洋生物群的辐射影响。沉积物和生物群的活度浓度在实际监测数据的广泛范围内。因此,与基于浓度因子的更简单的平衡方法相比,动态模型能更好地计算海洋生物群中的活度浓度,平衡方法在急性事故期间往往会高估。沉积物外照射的模拟剂量率也明显低于平衡预测值。模型计算证实了先前的研究,即海洋生物群中的放射性水平通常低于对种群产生可测量影响所需的水平。该模型以质量平衡模式用于计算(131)I、(137)Cs和(90)Sr的总综合释放量分别为103、30和3 PBq,与先前的估计合理相符。

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