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Assessment of the evolution of the redox conditions in the SKB ILW-LLW SFR-1 repository (Sweden)

机译:评估SKB ILW-LLW SFR-1存储库中氧化还原条件的演变(瑞典)

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The evaluation of the redox conditions in the Swedish ILW-LLW repository, SFR-1, is of high relevance in the performance assessment. The SFR-1 repository contains heterogeneous types of wastes, of different activity levels and with different materials in the waste and in the matrices and packaging. Steel and concrete-based materials are ubiquitous in the repository. The assessment presented in this work is based on the evaluation of the redox conditions and of the reducing capacity in 15 individual and representative waste package types in SFR-1. A combination of the individual models is used to determine the redox evolution of the different vaults in the repository. The results of the model indicate that in the initial time after repository closure, O_2 is consumed through degradation of organic matter and metal corrosion during the initial time after repository closure. Afterwards, the system is kept under reducing conditions for long time periods, and H_2(g) is generated due to the anoxic corrosion of steel forming magnetite as main corrosion product. The time at which steel is depleted varies with the amount and characteristics of steel and ranges from 5,000 to over 60,000 years. After complete steel corrosion, the reducing capacity of the system is mainly given by magnetite. The calculated redox potential under the chemical conditions imposed by the massive amounts of cements in the repository is in the order of -0.75 V (at pH 12.5). In case of assuming that the Eh of the system is controlled by the interaction between Fe(III)/Magnetite as a result of groundwater/magnetite interactions, redox potentials in the range -0.7 to -0.01 V are calculated, considering the uncertainty in the pH prevalent in the system If the absence of oxic disturbances the Eh of the repository system would be kept reducing. In the event of oxidising and diluted glacial meltwater intrusion, magnetite would gradually convert into Fe(III) oxides, buffering the redox potential of the system and preventing it from oxidation for long time periods.
机译:在瑞典ILW-LLW储存库中的氧化还原条件,SFR-1的评估在性能评估中具有高相关性。 SFR-1储存库含有异质类型的废物,不同的活性水平,以及废物中的不同材料以及矩阵和包装。钢和混凝土材料在储存库中无处不在。本作工作中提出的评估是基于氧化还原条件的评估和在SFR-1中的15个个体和代表性废物包装类型中的降低能力。各个模型的组合用于确定存储库中不同拱顶的氧化还原演化。该模型的结果表明,在储存库闭合后的初始时间,通过在储存库闭合后的初始时间期间通过有机物质和金属腐蚀的降解消耗O_2。然后,系统保持在减小条件下,长时间的条件,并且由于钢形成磁铁矿的缺氧腐蚀而产生H_2(G)作为主要腐蚀产物。钢耗尽的时间随钢的量和特点而且范围为5,000至超过60,000多年。经过完全钢腐蚀,系统的降低能力主要由磁铁矿给出。在储存库中大量水泥施加的化学条件下计算的氧化还原电位为-0.75V(pH 12.5)。如果假设系统EH的EH通过地下水/磁铁矿相互作用的FE(III)/磁铁矿之间的相互作用来控制,则考虑到不确定性,计算-0.7至-0.01V范围内的氧化还原电位系统中的pH普遍存在,如果没有氧化库扰动的储存系统的EH将保持减少。在氧化和稀释的冰醋水侵犯的情况下,磁铁矿将逐渐转化为Fe(III)氧化物,缓冲系统的氧化还原电位并防止其长时间氧化。

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