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Redox properties of MX-80 and Montigel bentonite-water systems

Published online by Cambridge University Press:  11 February 2011

Cecilia Lazo
Affiliation:
Dept. Inorg. Chem., Royal Institute of Technology, Stockholm, Sweden.
Ola Karnland
Affiliation:
Clay Technology AB, IDEON Research Center, Lund, Sweden.
Eva-Lena Tullborg
Affiliation:
Terralogica AB, Gråbo, Sweden.
Ignasi Puigdomenech
Affiliation:
Swedish Nuclear Fuel and Waste Management Co. (SKB), Stockholm, Sweden.
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Abstract

The uptake of dissolved oxygen (O2) has been studied in bentonite suspensions in 0.1 M NaCl media at (25±2)°C. MX-80 and Montigel bentonites were used in concentrations varying from 18 to 73 g/L. The experiments were performed in a magnetically stirred closed glass vessel, in an N2-glove box. Redox potentials where measured with Pt-wires, and dissolved O2 was measured both with a membrane electrode and with an optode. The experiments with MX-80 show that dissolved O2 disappears in ∼5 days under these conditions. Redox potentials decreased from ∼ +500 to ∼ +125 mVSHE (versus Standard Hydrogen Electrode). The data for the Montigel bentonite show similar time scales for O2 uptake but lower redox potentials at the end of the experiments ∼ −175 mVSHE. Pyrite oxidation is perhaps not the main process for O2 uptake, as MX-80 contains 0.3% FeS2 while Montigel bentonite only has a negligible amount.

Type
Research Article
Copyright
Copyright © Materials Research Society 2003

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References

REFERENCES

1. Wersin, P., Spahiu, K., and Bruno, J., Report No. SKB-TR-94–02, 1994.Google Scholar
2. Müller-vonMoos, M. and Kahr, G., Report No. NAGRA-TB-83–12, 1983.Google Scholar
3. Lazo, C., Karnland, O., Tullborg, E.-L., and Puigdomenech, I., Report No. SKB-TR-(in print), 2003.Google Scholar
4. King, F., Litke, C.D., Quinn, M.J., and LeNeveu, D.M., Corros. Sci. 37, 833 (1995).Google Scholar
5. Williamson, M.A. and Rimstidt, J.D., Geochim. Cosmochim. Acta 58, 5443 (1994).Google Scholar
6. Nicholson, R.V., Gillham, R.W., and Reardon, E.J., Geochim. Cosmochim. Acta 52, 1077 (1988);Google Scholar
Moses, C.O. and Herman, J.S., Geochim. Cosmochim. Acta 55, 471 (1991);Google Scholar
Kamei, G. and Ohmoto, H., Geochim. Cosmochim. Acta 64, 2585 (2000);Google Scholar
McGuire, M.M., Edwards, K.J., Banfield, J.F., and Hamers, R.J., Geochim. Cosmochim. Acta 65, 12431258 (2001).Google Scholar
7. Evangelou, V.P., Seta, A.K., and Holt, A., Environ. Sci. Technol. 32, 2084 (1998);Google Scholar
Domènech, C., de Pablo, J., and Ayora, C., Chem. Geol. 190, 339– 353 (2002).Google Scholar