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Field and Laboratory Examination of Uranium Microcrystallization and Its Role in Uranium Transport

Published online by Cambridge University Press:  21 March 2011

Takashi Murakami ,
Toshihiko Ohnuki ,
Hiroshi Isobe  and
Tsutomu Sato
Takashi Murakami
Affiliation:
Dept. of Earth and Planetary Science, Univ. of Tokyo, Bunkyo-ku, Tokyo 113-0033, Japan (e-mail: [email protected])
Toshihiko Ohnuki
Affiliation:
Dept. of Environmental Science, Japan Atomic Energy Res. Inst., Tokai 319-1106, Japan
Hiroshi Isobe
Affiliation:
Dept. of Earth Sciences, Kumamoto Univ., Kumamoto 860-8555, Japan
Tsutomu Sato
Affiliation:
Div. of Global Environmental Science and Engineering, Kanazawa Univ., Kanazawa 920-1192, Japan
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Abstract

Adsorption is believed to be a dominant mechanism of uranium distribution between solid and solution, and thus, to play a major role in uranium transport. Because iron oxides and hydroxides are abundant at the Earth's surface and are great adsorbents of uranium, we have examined natural rocks that contain iron minerals along with uranium, and also carried out Fe-U coprecipitation and aging experiments to find how uranium is distributed between Fe minerals. Transmission and scanning electron microscopy reveals that microcrystals (10-50 nm) of metatorbernite (Cu(UO2)2(PO4)28H2O) are scattered within nodules consisting of fine-grained (2-50 nm) goethite and hematite, where the ground water is undersaturated with respect to metatorbernite, for the natural rocks from the Koongarra ore deposit, Australia. The microscopy also reveals that microcrystals (a few nm) of dehydrated schoepite ((UO2)O0.25(OH)1.5) are formed among fine-grained hematite after aging coprecipitated Fe-U in the laboratory, and the solution is undersaturated with respect to schoepite. The beam size of microscopes is found to be important for the chemical analysis of such microcrystals. We detect a strong signal of uranium for a beam size < 40 nm; whereas a weak uranium signal is obtained for a beam size > 150 nm. Our results indicate that such a weak uranium signal should not be taken as a result of homogeneously distributed uranium over goethite and hematite surfaces by, for instance, adsorption. The micrcrystallization observed in both the field and laboratory suggests that fine grained uranyl minerals play a major role in uranium transport and migration.

Type
Research Article
Information
MRS Online Proceedings Library (OPL) , Volume 663: Symposium – Scientific Basis for Nuclear Waste management XXIV , 2000 , 971
Copyright
Copyright © Materials Research Society 2001

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References

REFERENCES

1. Airey, P. L. and Ivanovich, M., Chemical Geology 55, 203 (1986).Google Scholar
2. Tripathi, V. S., Ph.D. dissertation, Stanford University, Palo Alto, California, 297 p.(1983).Google Scholar
3. Hsi, C.-K. D. and Langmuir, D., Geochimica et Cosmochimica Acta 49, 1931 (1985).Google Scholar
4. Waite, T.D., Davis, J.A., Payne, T.E., Waychunas, G.A., and Xu, N., Geochimica et Cosmochimica Acta, 58, 5465 (1994).Google Scholar
5. Dent, A.J., Ramsay, J.D.F., and Swanton, S.W., Journal of Colloid and Interface Science, 150, 45 (1992).Google Scholar
6. Bruno, J., Pablo, J. De, Duro, L., and Figuerola, E., Geochimica et Cosmochimica Acta, 59, 4113 (1995).Google Scholar
7. Lumpkin, G. R., Payne, T. E., Fenton, B. R., and Waite, T. D., in Scientific Basis for Nuclear Waste Management XXII, edited by Wronkiewicz, D. J. and Lee, J. H. (Mater. Res. Soc. Symp. Proc. 556, Pittsburgh, PA 1999), p. 1067–1074.Google Scholar
8. Fenton, B. R., Lumpkin, G. R., Waite, T. D., and Payne, T. E., this volume.Google Scholar
9.T. E. Payne and Waite, T. D., this volume.Google Scholar
10. Murakami, T., Ohnuki, T., Isobe, H., and Sato, T., American Mineralogist, 82, 888 (1997).Google Scholar
11. Sato, T., Murakami, T., Yanase, Y., Isobe, H., Payne, T. E., Airey, P. L., Environmental Science and Technology, 31, 2854 (1997).Google Scholar
12. Suzuki, Y., Murakami, T., Kogure, T., Isobe, H., Sato, T., in Scientific Basis for Nuclear Waste Management XXI, edited by McKinley, I. G. (Mater. Res. Soc. Symp. Proc. 506, Pittsburgh, PA 1998), p. 839–846.Google Scholar
13. Finch, R. J., Hawthorne, F. C., and Ewing, R. C., in Scientific Basis for Nuclear Waste Management XIX, edited by Murphy, W. M. and Knecht, D. A. (Mater. Res. Soc. Symp. Proc. 412, Pittsburgh, PA 1998), p. 361–368.Google Scholar