Archaeological analogues for the lifetime prediction of the canister for spent nuclear fuel in the deep geological repository: Part I. Composition of pore water and corrosion products

Kateřina Kolomá, Václava Havlová, Anna Pecková, Šárka Šachlová, Vlastislav Kašpar, Diana Tkachenok, Alžběta Danielisová, Drahomíra Malyková, Helena Březinová, Ludmila Barčáková, Saqib Mukhtar, Richard Bureš, Jan Stoulil
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Abstract

This work focuses on archaeological analogues as a way of obtaining long‐term data for assessing the lifetime of a spent nuclear fuel canister. An analysis of the environment around the excavated artefacts is presented, followed by geochemical modelling of the likely corrosion products and subsequent comparison with real phases in the corrosion layer estimated by X‐ray diffraction. A total of 16 archaeological sites with fine clay soils and the potential for long‐term flooding were evaluated. Although the soil pore solution contained high levels of silicates, no such phases with iron in the corrosion products were confirmed. Carbonate corrosion products, typical of bentonite environments, were also not observed. Although oxygen access is very limited in the environments of all sites, even low concentrations shifted the equilibrium of corrosion products formed in favour of (hydroxy)oxides.
用于预测深层地质处置库乏核燃料罐寿命的考古类比:第一部分:孔隙水和腐蚀产物的成分
这项工作的重点是通过考古模拟来获取评估乏核燃料罐寿命的长期数据。对出土文物周围的环境进行了分析,随后对可能的腐蚀产物进行了地球化学建模,并与通过 X 射线衍射估算的腐蚀层中的实际相进行了比较。共对 16 个考古遗址进行了评估,这些遗址的土壤为细粘土,有可能长期被水淹没。虽然土壤孔隙溶液中含有大量硅酸盐,但没有在腐蚀产物中发现铁相。也没有观察到膨润土环境中典型的碳酸盐腐蚀产物。虽然在所有地点的环境中氧气的获取都非常有限,但即使是低浓度的氧气也会使形成的腐蚀产物的平衡向(羟基)氧化物倾斜。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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