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A Study of the Hydrothermal Stability of Copper for Use as a Container Material for Nuclear Waste

Published online by Cambridge University Press:  28 February 2011

Paul I. Lazaar
Affiliation:
Dept. of Geology, Temple University, Philadelphia, Pa. 19122
G. C. Ulmer
Affiliation:
Dept. of Geology, Temple University, Philadelphia, Pa. 19122
D. E. Grandstaff
Affiliation:
Dept. of Geology, Temple University, Philadelphia, Pa. 19122
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Abstract

The hydrothermal stability of copper has been studied to assess its suitability as a container material for disposal of nuclear waste in the proposed repository site at Hanford, Wa. The experiments (Cohassett basalt, synthetic Grande Ronde #4 groundwater, and copper powder with a water:rock:Cu-powder mass ratio of 20:1:1) were conducted at 300°C, 30 MPa, using Dickson rocking autoclaves for periods up to 3000 hours. Redox was calculated from dissolved H2 measured by gas chromatograph and He-ionization detector.

After ca. 100 hours the solution Cu concentration stabilized at 2–3 ppm, near Cu saturation, and did not vary significantly during the remainder of the experiment. The in situ solution pH was slightly alkaline. The copper powder showed little evidence of etching. The Cu concentration did not reflect oxide-coating spallation effects such as those described by Johnston et al.[15]. Within 48 hours, the log fO2 values decreased rapidly toward the magnetite-hematite phase boundary (−31 at 300°C); this is well within the stability field of native copper. SEM and EDX analysis of the reaction products revealed a copper-iron sulfide. One experiment used copper powder containing ca. 5% cuprite. Oxygen released by the cuprite overwhelmed the buffering capacity of the basalt. The resulting log fO2 values stabilized near the copper-cuprite phase boundary (−23.1 at 300°C) with the solution remaining within the copper stability field. Copper purity is important as oxygen contamination or oxidation of the copper containers may strongly affect the repository redox and mobility of radionuclides.

Type
Research Article
Copyright
Copyright © Materials Research Society 1988

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References

1. Anantatmula, R.P., Delegard, C.H., and Fish, R.L., in Scientific Basis for Nuclear Waste Management VII, edited by McVay, G.L. (Elsevier Science Publishers, New York, 1984) pp.113120.Google Scholar
2. Brown, A.C., Econ. Geol. 48 543573 (1971).CrossRefGoogle Scholar
3. Crisman, D.P. and Jacobs, G.K., Native Copper Deposits of the Portage Lake Volcanics, Michigan: Their Implications with Respect to Canister Stability for Nuclear Waste Isolation in the Columbia River Basalts Beneath the Hanford Site, Washington, RHO-BW-ST-26P, Rockwell Hanford Operations, Richland, WA (1982).Google Scholar
4. Seyfried, W.E. Jr., Janecky, D.R., and Berndt, M.E., in Hydrothermal Experimental Techniques, edited by Ulmer, G.C. and Barnes, H.L. (John Wiley & Sons, New York, 1987) pp. 216239.Google Scholar
5. Dickson, F.W., Blount, C.W., and Tunnell, G., Am. J. Sci. 26 (1), 6178 (1983).Google Scholar
6. Moore, E.L., Ulmer, G.C., and Grandstaff, D.E., Chem. Geol. 49 5371 (1985).Google Scholar
7. Allen, C.C. and Strope, M.B., Microcharacterization of Basalt. Considerations for a Nuclear-Waste Repository, Rockwell Document RHO-BW-SA-924P, (1983).Google Scholar
8. Long, P.E., ”Stratigraphy of the Grande Ronde Basalt,” in Myers, C.W. and Price, S.M., eds., Subsurface Geology of the Cold Creek Syncline, RHO-BWI-ST-14, Rockwell Hanford Operations, Richland, WA (1981).Google Scholar
9. Jones, T.E., ”Recipe for Grande Ronde #4 Solution,” Rockwell Hanford Letter Report, No. 103011–83–001 (1983).Google Scholar
10. Van Der Plas, L. and Tobi, A.C., Amer. J. Sci. 263 97–90 (1965).Google Scholar
11. Kishima, N. and Sakai, H., Geochem. J. 18 1929 (1984).Google Scholar
12. Grandstaff, D.E., Korn, R., Foster, R., and Ulmer, G.C. in Second International Symposium on Hydrothermal Reactions p.10 (1985).Google Scholar
13. Kacandes, G.H., personal comm. (1987).Google Scholar
14. Korn, R., Ulmer, G.C., and Grandstaff, D.E. in Fifth International Symposium on Water-Rock Interaction: Extended Abstracts (Orkustofnun, Reykjavik, Iceland, 1986) p. 333.Google Scholar
15. Johnston, R.G., Anantatmula, R.P., Lutton, J.M., and Rivera, C.L., 88th Annual Meeting Abstracts, The American Ceramic Society, Inc. (Columbus, Ohio, 1986) p.503.Google Scholar
16. McKeon, G.L., personal comm. (1987).Google Scholar
17. Helgeson, H.C., Delaney, J.M., Nesbitt, W.H., and Bird, D.K., Amer. J. Sci. 278–A, 1229 pp. (1978).Google Scholar
18. Sangameshwar, S.R. and Barnes, H.L., Econ. Geol. 78 13791397 (1983).Google Scholar