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Experimental Study of Uranium(6+) Sorption on the Zeolite Mineral Clinoptilolite

Published online by Cambridge University Press:  01 January 1992

Roberto T. Pabalan
Affiliation:
Center for Nuclear Waste Regulatory Analyses, Southwest Research Institute, 6220 Culebra Road, San Antonio, TX 78238-5166
J. D. Prikryl
Affiliation:
Center for Nuclear Waste Regulatory Analyses, Southwest Research Institute, 6220 Culebra Road, San Antonio, TX 78238-5166
P. M. Muller
Affiliation:
Center for Nuclear Waste Regulatory Analyses, Southwest Research Institute, 6220 Culebra Road, San Antonio, TX 78238-5166
T. B. Dietrich
Affiliation:
Center for Nuclear Waste Regulatory Analyses, Southwest Research Institute, 6220 Culebra Road, San Antonio, TX 78238-5166
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Abstract

Experiments on the sorption of uranium(6+) on clinoptilolite from solutions in equilibrium with atmospheric CO2(g) were conducted to understand the fundamental controls on uranium sorption on zeolite minerals, including the effects of pH, aqueous uranium speciation, and uranium concentration in solution. The results indicate that uranium(6+) species are strongly sorbed on the zeolite mineral clinoptilolite at near-neutral pH. The amount of uranium sorbed is strongly dependent on pH and, to some extent, on the total concentration of uranium. Uranium sorption on clinoptilolite is important in the pH range where UO2(OH)2°(aq) is the predominant uranium aqueous species, whereas sorption is inhibited at pH's where carbonateand hydroxy-carbonate-complexes are the primary uranyl species. Surface adsorption appearsto be the main sorption mechanism, although at pH<4 the results suggest ion exchange may occur between the UO2+2 ions in solution and the cations in the intracrystalline cation exchange sites of clinoptilolite.

The effectiveness of zeolite-rich horizons underneath Yucca Mountain, Nevada, as barriers to actinide transport through sorption processes will depend strongly on groundwater chemistry. Reliable predictions of radionuclide transport through these horizons will need to properly account for changes in solution chemistry.

Type
Research Article
Copyright
Copyright © Materials Research Society 1993

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References

REFERENCES

1. Ames, L.L., Jr., Amer. Mineral. 45, 689 (1960); 49, 127 (1964); 49, 1099 (1964).Google Scholar
2. Chelischev, N.F., Berenschtein, B.G., Berenschtein, T.A., Grebanova, H.K. and Martynova, H.C., Doki. Akad. Nauk SSSR 210, 1110 (1973).Google Scholar
3. Mumpton, F.A., in Natural Zeolites: Occurrence, Properties, Use, edited by Sand, L.B. and Mumpton, F.A., (Pergamon, New York, 1978), pp. 327.Google Scholar
4. Howden, M. and Pilot, J., in Ion Exch. Technol., edited by Naden, D. and Streat, M. (Horwood, Chichester U.K., 1984) pp. 6673.Google Scholar
5. Vavrova, M., Musatovova, O., and Bartha, S., Isotopenpraxis 27, 325 (1991).Google Scholar
6. Daniels, W.R., Wolfsberg, K., Rundberg, R.S., Ogard, A.E., Kerrisk, J.F., Duffy, C.J., Newton, T.W., Knight, S.D., Lawrence, F.O., Rundberg, V.L., Sykes, M., Thompson, G., Travis, B., Treher, E., Vidale, R., Walter, G., Aguilar, R., Cisneros, M., Maestas, S., Mitchell, A., Oliver, P., Oliver, P., Raybold, N., and Wanek, P., Summary Report on the Geochemistry of Yucca Mountain and Environs LA-9328-MS, Los Alamos Nat. Lab., Los Alamos, NM (1982).Google Scholar
7. Meyer, R.E., Arnold, W.D., Case, F.I., O'Kelley, G.D., and Land, J.F., in Scientific Basis for Nuclear Waste Management XIV edited by Abrajano, T.A. Jr., and Johnson, L.H., (Mater. Res. Soc. Proc. 212, Pittsburgh, PA, 1991) pp. 569576.Google Scholar
8. Katayama, N., Kubo, K., and Hirono, S., in Symposium on the Formation of Uranium Ore Deposits (International Atomic Energy Agency, Vienna, 1974), no. IAEA-SM-183/11.Google Scholar
9. Doi, K.S., Hirono, S., and Sakamaki, Y., Econ. Geol. 70, 628 (1975).Google Scholar
10. Pabalan, R.T., in Scientific Basis for Nuclear Waste Management XIV, edited by Abrajano, T.A. Jr., and Johnson, L.H., (Mater. Res. Soc. Proc. 212, Pittsburgh, PA, 1991) pp. 559567.Google Scholar
11. Mehra, O.P. and Jackson, M.L., in Clays and Clay Minerals, 7th Conf. (Pergamon, New York, 1960) pp. 317327.Google Scholar
12. Tripathi, V.S., PhD thesis, Stanford University, 1984.Google Scholar
13. Hsi, C.-K. D. and Langmuir, D., Geochim. Cosmochim. Acta 49, 1931 (1985).Google Scholar
14. Wolery, T.J., Jackson, K.J., Bourcier, W.L., Bruton, C.J., Viani, B.E., Knauss, K.G. and Delany, J.M., in Chemical Modeling in Aqueous Systems 11 edited by Melchior, D.C. and Bassett, R.L., (Amer. Chem. Soc., Washington D.C., 1990), pp. 104116.Google Scholar
15. Payne, T.E., Sekine, K., Davis, J.A. and Waite, T.D., in Alligator Rivers Analogue Proiect Annual Report 1990-1991, edited by Duerden, P. (Aust. Nucl. Sci. Tech. Org., Menai, NSW, 1992) pp. 5785.Google Scholar
16. Grenthe, I., Fuger, J., Konings, R., Lemire, R., Muller, A., Nguyen-Trung, C., Wanner, H., Chemical Thermodynamics of Uranium (North-Holland, Amsterdam, 1992).Google Scholar
17. Siegel, M.D., Leckie, J.O., Park, S.W., Phillips, S.L. and Sewards, T., Sandia National Laboratories Report No. SAND89-2387, 1990.Google Scholar
18. Cotton, F.A. and Wilkinson, G., Advanced Inoreanic Chemistry (John Wiley, New York, 1980), p. 1016.Google Scholar
19. Meier, W.M. and Olson, D.H., Atlas of Zeolite Structure Types. (Polycrystal Book Service, Pittsburgh, 1978).Google Scholar
20. Andreeva, N.R. and Chernyavskaya, N.B., Radiokhimiya 24, 9 (1982).Google Scholar