13-18 May 2018
Casino Conference Centre
Europe/Prague timezone

Spectroscopic and batch studies of technetium uptake by siderite

15 May 2018, 09:30
Marble Hall (Casino Conference Centre)

Marble Hall

Casino Conference Centre

Reitenbergerova 4/95, Mariánské Lázně, Czech Republic
Verbal Chemistry of Nuclear Fuel Cycle, Radiochemical Problems in Nuclear Waste Management NFC 2


Dr Katja Schmeide (Helmholtz-Zentrum Dresden - Rossendorf, Institute of Resource Ecology)


99Tc is a long-lived (t1/2 = 2.1 x 105 years) β-emitter formed during the fission of U and is of major concern for radioactive waste disposal. Its environmental mobility is primarily governed by the oxidation states VII and IV, with TcVII forming the highly mobile TcO4 aquo anion, whereas TcIV is rather immobile due to the low solubility of its hydrolysis products [1]. Redox processes, which are able to convert TcVII into TcIV, are hence of paramount importance for the safety of radioactive waste repositories. FeII-bearing minerals, ubiquitous in nature but also forming as corrosion products of the steel canisters foreseen as a possible first enclosure of radioactive waste, play a vital role in these redox reactions due to their high redox reactivity and high sorption capacity, as has been shown not only for Tc, but also for Se, U, Np and Pu.
We studied the TcVII uptake by siderite (FeCO3), a typical FeII mineral in carbonate-rich environments, in the relevant pH range 7 – 12.6 under anoxic conditions by means of batch sorption experiments and by X-ray absorption spectroscopy. Sorption experiments showed that Tc retention by siderite is fast and efficient (log Rd ~5) across the investigated pH range and independent of ionic strength (0.1 – 1 M NaCl). Tc K-edge X-ray absorption near-edge structure (XANES) data confirmed that the Tc immobilization is due to the surface-mediated reduction of TcVII to TcIV. The local structure of TcIV in Tc siderite sorption samples and Tc siderite coprecipitates probed by extended X-ray absorption fine-structure (EXAFS) spectroscopy revealed three different species: In the pH range 7.8 to 11.8, TcO2-dimers form inner-sphere sorption complexes at the surface of the initial siderite phase as well as on secondary magnetite or green rust formed during the redox reaction. Between pH 11.9 and 12.6, a mixed Fe/Tc hydroxocarbonate precipitate (chukanovite-like) is formed.
The results showed that siderite contributes effectively to the retention of Tc under repository conditions through formation of strong sorption complexes and precipitation of hydroxocarbonate phases with low solubility.
[1] Eriksen, T.E., Ndalamba, P., Bruno, J., Caceci, M.: The solubility of TcO2xnH2O in neutral to alkaline solutions under constant pCO2. Radiochim. Acta 58-9, 67 (1992).

Primary author

Dr Katja Schmeide (Helmholtz-Zentrum Dresden - Rossendorf, Institute of Resource Ecology)


Dr Andre Rossberg (The Rossendorf Beamline at ESRF) Mr Stephan Weiss (Helmholtz-Zentrum Dresden - Rossendorf, Institute of Resource Ecology) Dr Andreas C. Scheinost (The Rossendorf Beamline at ESRF)

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