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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Flow in the unsaturated zone around a shallow subsurface radioactive waste trench: Interpretation of an infiltration-drainage test at the Chernobyl Pilot Site
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Flow in the unsaturated zone around a shallow subsurface radioactive waste trench: Interpretation of an infiltration-drainage test at the Chernobyl Pilot Site

机译:浅层地下放射性废料沟周围非饱和带中的流体:切尔诺贝利试验场的渗透排水试验的解释

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This article describes an infiltration-drainage test carried out in the unsaturated zone (UZ) at the Chernobyl Pilot Site during October 2008; this is an international radioecology study site and is the subject of several papers in this special issue. The test has to be seen in the larger context of radionuclide transport from a waste trench. The conducted experiment consisted of infiltrating a layer of 9.5cm of water in a circular area of 5.51m ~2 over 5h. Its main objective was to create a larger range of water content values (and hence suction pressure values), not only at the top of the soil profile but also at greater depths, in this case up to 1.50m. Observations of water content and suction pressure were carried out continuously at seven different depths during infiltration, drainage and during the return to natural conditions over a period of several months. This allowed deriving UZ parameter values with greater confidence than those derived from monitoring small natural water content changes over periods of years.The experiment also shows that a 1D model was incapable of correctly reproducing the observed water balance established on the central axis. A 2D axi-symmetric model was needed showing that lateral boundary effects have to be accounted for. This implies that small scale infiltrometer tests should be analysed in more than one dimension. It further became clear from the drainage curves that soil layering played a significant role and that in the present case hysteresis did not play a major role; i.e. the infiltration and drainage event can be reproduced with the same set of parameters and subsequent natural rain events can be reproduced well enough with two numerical models used for test interpretation, one is module oriented for reactive transfer, and the second with an automatic optimisation procedure. The robustness of the estimated parameter values, of the model discretisation and layer identification was tested over a 2-month period with natural infiltration using a 1D model. The results validated the test outcome.
机译:本文介绍了在2008年10月在切尔诺贝利试验场的非饱和带(UZ)中进行的渗透排水试验;这是一个国际放射生态研究站点,也是本期特刊中几篇论文的主题。必须从更大范围的放射性核素从废物沟中运输来进行测试。进行的实验包括在5小时内以5.51m〜2的圆形区域渗透9.5cm的水层。它的主要目的是创建一个更大范围的水含量值(以及吸水压力值),不仅在土壤剖面的顶部,而且在更大的深度(在这种情况下,最大深度为1.50m)。在渗透,排水和恢复自然状态的几个月中,在七个不同的深度连续进行了水含量和吸气压力的观测。与多年以来监测较小的自然水含量变化得出的参数相比,这可以更可靠地得出UZ参数值。实验还表明,一维模型无法正确再现在中心轴上建立的观察到的水平衡。需要一个二维轴对称模型,该模型表明必须考虑横向边界效应。这意味着应该在一个以上的维度上分析小规模的渗透计测试。从排水曲线还可以清楚地看出,土壤分层起着重要作用,而在当前情况下,滞后作用并不重要。也就是说,可以使用相同的参数集来再现入渗和排水事件,并且可以使用两个用于测试解释的数值模型来很好地再现随后的自然降雨事件,一个用于反应转移的模块,第二个具有自动优化程序。使用一维模型在2个月的自然渗透下测试了估计参数值,模型离散化和层识别的稳健性。结果验证了测试结果。

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