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Diffusion of Cs$$^{+}$$, I$$^{-}$$ and HDO onto pre-Neogene sedimentary rocks

Hou, L.*; Fukatsu, Yuta  ; Okamoto, Shunichi*; Toda, Kanako*; Nakata, Kotaro*; Nohara, Shintaro*; Ishidera, Takamitsu ; Saito, Takumi*

This study investigates the diffusion behaviors of Cs$$^{+}$$, I$$^{-}$$, and HDO in a pre-Neogene sedimentary rock as a potential host rock for high-level radioactive waste (HLW) disposal in Japan. Through-diffusion experiments were conducted to reveal distinct patterns in their breakthrough curves. Cs$$^{+}$$ exhibited the fastest diffusion among the tracers, significantly influenced by fractures, surface diffusion mechanisms, and aragonite formation. In contrast, the anion exclusion effect notably hindered the diffusion behavior of I$$^{-}$$. The results highlight the diverse diffusion and retardation properties of pre-Neogene sedimentary rocks, showing that the effective diffusion coefficient of HDO is more similar to that of crystalline rocks. These findings contribute to the understanding of the suitability of pre-Neogene sedimentary rocks as a potential natural barrier for HLW repositories.

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Category:Nuclear Science & Technology

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