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Uncertainty assessment method for the Cs-137 fallout inventory and penetration depth

机译:Cs-137尘埃清单和穿透深度的不确定度评估方法

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Within the presented study, soil samples were collected in year 2007 at 20 different locations of the Greek terrain, both from the surface and also from depths down to 26 cm. Sampling locations were selected primarily from areas where high levels of Cs-137 deposition after the Chernobyl accident had already been identified by the Nuclear Engineering Laboratory of the National Technical University of Athens during and after the year of 1986. At one location of relatively higher deposition, soil core samples were collected following a 60 m by 60 m Cartesian grid with a 20 m node-to-node distance. Single or pair core samples were also collected from the remaining 19 locations. Sample measurements and analysis were used to estimate Cs-137 inventory and the corresponding depth migration, twenty years after the deposition on Greek terrain. Based on these data, the uncertainty components of the whole sampling-to-results procedure were investigated. A cause-and-effect assessment process was used to apply the law of error propagation and demonstrate that the dominating significant component of the combined uncertainty is that due to the spatial variability of the contemporary (2007) Cs-137 inventory. A secondary, yet also significant component was identified to be the activity measurement process itself. Other less significant uncertainty parameters were sampling methods, the variation in the soil field density with depth and the preparation of samples for measurement. The sampling grid experiment allowed for the quantitative evaluation of the uncertainty due to spatial variability, also by the assistance of the semi variance analysis. Denser, optimized grid could return more accurate values for this component but with a significantly elevated laboratory cost, in terms of both, human and material resources. Using the hereby collected data and for the case of a single core soil sampling using a well-defined sampling methodology quality assurance, the uncertainty component due to spatial variability was evaluated to about 19% for the Cs-137 inventory and up to 34% for the Cs-137 penetration depth. Based on the presented results and also on related literature, it is argued that such high uncertainties should be anticipated for single core samplings conducted using similar methodology and employed as Cs-137 inventory and penetration depth estimators. (C) 2017 Elsevier Ltd. All rights reserved.
机译:在提出的研究中,土壤样本于2007年在希腊地形的20个不同位置收集,无论是从表面还是从深至26厘米的深度。采样地点的选择主要是从1986年及之后的雅典国立技术大学核工程实验室识别出切尔诺贝利事故后高Cs-137沉积的地区开始的。 ,按照60 m x 60 m的笛卡尔网格并以20 m的节点到节点的距离收集土壤核心样本。还从其余19个地点收集了单核或双核样品。在希腊地形上沉积20年后,通过样本测量和分析来估算Cs-137存量和相应的深度迁移。基于这些数据,对整个抽样到结果过程的不确定性成分进行了研究。因果评估过程用于应用误差传播定律,并证明组合不确定性的主要重要组成部分是由于当代(2007年)Cs-137清单的空间变异性。确定了次要的也是重要的部分是活动测量过程本身。其他不太重要的不确定性参数包括采样方法,土壤田间密度随深度的变化以及准备用于测量的样品。采样网格实验还可以借助半方差分析对由于空间变异性引起的不确定性进行定量评估。 Denser优化网格可以返回该组件的更准确值,但在人力和物力方面都显着提高了实验室成本。使用据此收集的数据,以及对于使用明确定义的抽样方法进行质量保证的单芯土壤抽样的情况,由于空间变异性导致的不确定性分量在Cs-137清单中评估为约19%,在Cs-137清单中高达34%。 Cs-137穿透深度。根据给出的结果以及相关文献,有人认为使用类似方法进行单核取样并用作Cs-137清单和渗透深度估算器时,应预期会有如此高的不确定性。 (C)2017 Elsevier Ltd.保留所有权利。

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