Hostname: page-component-78c5997874-ndw9j Total loading time: 0 Render date: 2024-11-18T05:57:27.557Z Has data issue: false hasContentIssue false

Solid-Phase Transformation of Cs+- and Sr2+-Bearing Zeolite Sorbents Derived From Cenospheres to Mineral-Like Forms

Published online by Cambridge University Press:  15 February 2011

Sergei N. Vereshchagin
Affiliation:
Institute of Chemistry and Chemical Technology SB RAS, 42 K. Marx Street, Krasnoyarsk, 660036, Russia Siberian Federal University, 79 Svobodnyi Avenue, Krasnoyarsk, 660041, Russia
Tatiana A. Vereshchagina
Affiliation:
Institute of Chemistry and Chemical Technology SB RAS, 42 K. Marx Street, Krasnoyarsk, 660036, Russia
Leonid A. Solovyov
Affiliation:
Institute of Chemistry and Chemical Technology SB RAS, 42 K. Marx Street, Krasnoyarsk, 660036, Russia
Nina N. Shishkina
Affiliation:
Institute of Chemistry and Chemical Technology SB RAS, 42 K. Marx Street, Krasnoyarsk, 660036, Russia
Nataly G. Vasilieva
Affiliation:
Institute of Chemistry and Chemical Technology SB RAS, 42 K. Marx Street, Krasnoyarsk, 660036, Russia
Alexander G. Anshits
Affiliation:
Institute of Chemistry and Chemical Technology SB RAS, 42 K. Marx Street, Krasnoyarsk, 660036, Russia Siberian Federal University, 79 Svobodnyi Avenue, Krasnoyarsk, 660041, Russia
Get access

Abstract

The paper describes the studies of the transformation of Cs+- and Sr2+-containing zeolite sorbents synthesized from fly ash cenospheres to crystalline mineral composition, suitable for the long-term disposal. Series of Cs+- and Sr2+-exchanged NaP1-containing sorbents were subjected to the thermochemical transformation in the temperature range 40-1100°C at atmospheric pressure in air and the progress of reaction was monitored by DSC and XRD analysis. It was shown that initial sodium zeolite undergoes two-step transformation at 736-785°C and 892-982°C forming nepheline as the principle product, with the conversion temperatures being dependant on the heating rate.

The thermal treatment of Cs+-bearing zeolite sorbent led to formation of a complex multiphase system, the principal components of which were nepheline and pollucite. Increasing cesium content in the samples led to a monotonous shift of crystallization peak to the higher temperature range (1005-1006°C). A more complicated behavior was observed for Sr2+-containing samples, for which the crystallization temperature tends to increase (compared with NaP1) at lower Sr contents, but it starts decreasing parallel to the Sr2+ content at Sr2+ loadings >10 mg/g. The principal crystalline phases in Sr-NaP1 sample conversion were nepheline and Sr2+-containing feldspar, the quantity of which increased parallel to the increase of strontium content in zeolite.

Apparent activation energies of thermochemical transformations were calculated and possible approaches to reduce transformation temperature are discussed and experimentally illustrated.

Type
Research Article
Copyright
Copyright © Materials Research Society 2009

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

1 The Strategy of Handling Spent Fuel of the Atomic Energy Ministry of the Russian Federation (http://www.minatom.ru/News/Main/viewPrintVersion?id=696&idChannel=327).Google Scholar
2 Kotel'nikov, A.R., Zyryanov, V.N., and Epel, M.B.'baum, Ocherki fiziko-khimicheskoi petrologii, 18, 3 (1994).Google Scholar
3 Gramenitsky, E.N., Kotelnikov, A.R., Batanova, A.M., Schekina, T.I., Plechov, P.Y.. Eksperimental'naya I nauchnaya petrologiya (Experimental and Technical petrology) (Nauchny Mir, Moscow, 2000), 416 p.Google Scholar
4 Kotel, A.R.'nikov, Akhmedzhanova, G.M., and Suvorova, V.A., Geokhimiya, 2, 192 (1999).Google Scholar
5 Vereshchagina, T.A., Vasil, N.G.'eva, and Anshits, A.G., Khimiya v interesakh ustoichivogo razvitiya (Chemistry for sustainable development), 16, 369 (2008).Google Scholar
6 Laverov, N.P., Omelyanenko, B.I., Velichkin, V.I., Geoekologiya, 6, 3 (1994).Google Scholar
7 Kotel'nikov, A.R., Bychkov, A.M., Zyryanov, V.N., Akhmedzhanova, G.M., and Gavlina, O.T., Geokhimiya, 10, 1527 (1995).Google Scholar
8 Mimura, H., and Kanno, T., J. Atom. Energy Soc. Jap., 18, 518 (1976).Google Scholar
9 Holler, H., and Barth-Wirsching., U. Fortschritte Der Mineralogie, 63, 21(1985).Google Scholar
10 Querol, X., Plana, F., Alastuey, A., Fernandez-Turiel, J.L., and Lopez-Soler, A., Coal Science Series, 24, 1979 (1995).Google Scholar
11 Querol, X., Plana, F., Alastuey, A., and Lopez, A.-Soler, Fuel, 76, 793 (1997).Google Scholar
12 Bosch, P., Caputo, D., Liguori, B., and Collela, C., J. Nucl. Mater., 324, 183 (2004).Google Scholar
13 Penilla, R.P., Bustos, A. G., and Elizalde, S. G., Fuel, 85, 823 (2006).Google Scholar
14 Vereshchagin, S.N., Vereshchagina, T.A., Shishkina, N.N., Salanov, A.N., and Anshits, A.G., Khimiya v interesakh ustoichivogo razvitiya (Chemistry for sustainable development), 16, 519 (2008).Google Scholar
15 Vereshchagina, T.A., Anshits, N.N., Sharonova, O.M., Vasil'eva, N.G., Vereshchagin, S.N., Shishkina, N.N., Fomenko, E.V., and Anshits, A.G., Glass Physics and Chemistry, 34, 547 (2008).Google Scholar
16 Reitveld, H., J. Appl. Cryst., 2, 65 (1969).Google Scholar
17 Solovyov, L.A., J. Appl. Cryst., 37, 743 (2004).Google Scholar
18 Mimura, H., and Akiba, K., J. Nucl. Sci. Techn., 30(5), 436 (1993).Google Scholar