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Selenium uptake onto natural pyrite

Curti, E.*; Aimoz, L.*; Kitamura, Akira  

$$^{79}$$Se is a major dose-determining redox-sensitive nuclide in safety analysis of radioactive waste disposal sites. In aqueous solutions, selenium forms soluble anionic species (Se$$^{rm IV}$$O$$_{3}$$$$^{2-}$$ and Se$$^{rm VI}$$O$$_{4}$$$$^{2-}$$) that hardly sorb on negatively charged surfaces of common host-rock minerals. However, Se is known to have a strong affinity with sulphides and interacts with pyrite, a common minor mineral of argillaceous rocks being considered as host rocks for radioactive waste repositories in Switzerland etc. In this study, we present micro- and bulk X-ray spectroscopy data ($$mu$$-XRF, $$mu$$-XANES, and EXAFS) showing that, under nearly anoxic conditions, dissolved Se$$^{rm IV}$$O$$_{3}$$$$^{2-}$$ and Se$$^{rm VI}$$O$$_{4}$$$$^{2-}$$ sorb directly onto the pyrite surface and are subsequently reduced to Se$$^{0}$$ with increasing ageing time (up to 8 months). These results suggest that the mobility of $$^{79}$$Se$$^{rm IV}$$ released from radioactive waste could efficiently be reduced through uptake on the pyrite surface followed by transformation into a sparingly soluble reduced form.

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Category:Chemistry, Analytical

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