首页> 外文会议>9th International Conference on Environmental Remediation and Radioactive Waste Management >NATURAL AND ENGINEERED BARRIERS IN A ROMANIAN DISPOSAL SITE FOR LOW AND INTERMEDIATE LEVEL WASTE
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NATURAL AND ENGINEERED BARRIERS IN A ROMANIAN DISPOSAL SITE FOR LOW AND INTERMEDIATE LEVEL WASTE

机译:中低水平废物在罗马尼亚处置场中的自然屏障和工程屏障

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The operational waste generated by the Cernavoda Nuclear Power Plant will be disposed in a near-surface facility. The low and intermediate level wastes, containing particularly large concentrations of C-14 and H-3, are treated and conditioned in steel drums, which will be placed in the disposal cells and then immobilized in concrete. The Saligny site has been proposed for LIL waste disposal. Geologically, the main components of this site are the quaternary loess, the Precambrian and pre-quaternary clays, and the Eocene and Barremian limestones. Hydrologically, the site can be divided into a vadose zone down to 45-50m and three distinct aquifers, two of them in the limestone beds and the third into the lenses of sand and limestone existing in the pre-quatemary clay layer. Preliminary performance assessments, presented in this paper, indicate that the geologic layers are efficient natural barriers against water flow and radionuclide migration from the vadose zone to the Barremian aquifer. The semi-arid climate and the low precipitation rate prevent contaminant transport from the disposal site to the Eocene aquifer. FEHM simulations of transient groundwater flow showed that seasonal variations influence the moisture content profile in the top of the vadose zone, but the influence over the long term is not significant for contaminant transport. The Danube River level variations control water movement in the Barremian aquifer, especially in the upper part where the limestone is highly fractured and water moves toward the river when its level is low and toward the site when the river level is high. The disposal concept tries to combine the natural and engineered barriers in order to ensure the safety of the environment and population. Therefore, the concrete filling the disposal cells surrounds the waste with a medium that facilitates C-14 retention by precipitation, thus reducing the C-14 releases in the atmosphere and geosphere.
机译:切尔纳沃达核电站产生的运行废物将被处置在近地表设施中。含有特别高浓度的C-14和H-3的中低水平废物在钢桶中进行处理和调理,然后将其放置在处置室中,然后固定在混凝土中。已提议在Saligny场地处置LIL废物。从地质学上讲,该站点的主要成分是第四纪黄土,前寒武纪和第四纪前粘土以及始新世和巴雷米亚的石灰岩。在水文方面,该地点可分为一个低渗层带(低至45-50m)和三个不同的含水层,其中两个在石灰岩层中,第三个在早古季粘土层中存在的沙和石灰岩的晶状体中。本文提出的初步性能评估表明,地质层是阻止水流和放射性核素从渗流带向巴雷米亚含水层迁移的有效天然屏障。半干旱气候和低降水率阻止了污染物从处置场向始新世含水层的迁移。瞬态地下水流动的FEHM模拟表明,季节性变化会影响渗流带顶部的水分含量分布,但从长远来看,对污染物的迁移影响并不显着。多瑙河水位变化控制着巴雷米亚含水层中的水运动,特别是在石灰岩高度破裂,水位低时向河水运动和水位高时向场地运动的上部。处置概念试图将自然屏障和工程屏障结合起来,以确保环境和人口的安全。因此,填充处理单元的混凝土将废物包围在介质中,该介质通过沉淀促进C-14的保留,从而减少了C-14在大气和地球大气中的释放。

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