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Material Parameters and Experiments - Corrosion Behavior of Spent Fuel in Non-saline Solutions Experimental Studies at FZK/INE

机译:材料参数与实验 - 富含盐水溶液在FZK / INE实验研究中的腐蚀性的腐蚀行为

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With respect to the assessment of the long-term behavior of the waste form spent fuel it is of high importance to understand in particular the UO_(2) matrix dissolution behavior and the associated release or retention of mobilized radionuclides during an assumed contact with groundwater. Due to the radionuclide inventory of the fuel radiolysis of the groundwater will start, followed by oxidation and subsequent dissolution of the fuel. Additionally, the overall corrosion behavior of the fuel is governed by the geochemical constraints in the near field. Related to this objective we studied experimentally the impact of geochemical conditions possibly encountered in close vicinity to the spent fuel on fuel matrix dissolution under anoxic conditions. Special attention was focused on (1) the nature of solution contacting the matrix (5 M NaCl brine, granite water [low ionic strength, SiO_(2)-rich], granite bentonite water [high ionic strength, low in SiO_(2)]), the (2) presence/absence of CO_(2), and (3) the presence or absence of corroding container material (Fe and Fe corrosion products). Pre washed powdered fuel samples (grain size > 3 (mu)m) were used for these studies to achieve a faster reaction progress and to mask contributions from the grain boundary inventories. The fuel matrix dissolution rates were found to be within the same range in 5 M NaCl-brine, granite and granite bentonite water (about 10-4/d). In the presence of iron and its corrosion products considerable amounts of H_(2) were generated due to the corrosion of the added iron. In these cases, the matrix dissolution rates have been slowed down by a factor of 10 - 20, associated with strong retention effects for various radioelements. Studies upon spent fuel corrosion behavior in a clay environment are presently in the planning stage.
机译:对于废物体乏燃料的长期行为的评估是非常重要的,特别要了解UO_(2)基体溶解行为,并与地下水的假定接触过程中相关的发行或动员的放射性核素的保留。由于地下水将启动的燃料辐的放射性核素库存,其次是氧化和燃料的后续溶解。此外,燃料的整体腐蚀性行为是由在近场地球化学约束管理。相关实验研究的缺氧条件下密切附近可能遇到的燃料基质溶解乏燃料地球化学条件的影响,这个目标我们。特别注意力都集中在(1)的溶液中的基质(5M的NaCl盐水洗涤,花岗岩水接触的性质[低离子强度,SiO_(2)富含],花岗岩膨润土水[高离子强度,低SiO_(2) ]),(2)存在/不存在的CO_(2),和(3)腐蚀容器材料的存在或不存在(Fe和铁腐蚀产物)。预洗涤的粉末状燃料样品(粒度> 3(亩)M)用于这些研究,以实现更快的反应进展,并屏蔽从晶界库存贡献。燃料基质的溶解速率被认为是在相同范围内的5M的NaCl盐水,花岗岩和花岗岩膨润土水(约10-4 / d)。在的铁及其腐蚀产物相当量H_(2)的存在下产生的,由于添加的铁的腐蚀。在这些情况下,基质溶解率已经由10倍放缓 - 20,与各种放射性元素强滞留效应有关。在粘土环境在乏燃料腐蚀行为的研究目前正处于规划阶段。

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