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Small-angle x-ray scattering characterization of self-irradiated zircon

Published online by Cambridge University Press:  01 February 2011

Susana Ríos
Affiliation:
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, United Kingdom
Ekhard K. H. Salje
Affiliation:
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, United Kingdom
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Abstract

Small-angle x-ray scattering (SAXS) measurements were performed on two natural zircons: one with an amorphous content close to 85 %, and the second one x-ray amorphous. Electron density fluctuations were observed in the untreated samples, and studied as a function of various heat-treatments. In the starting material, density fluctuations were found to have a characteristic length-scale of approximately 1 nanometer diameter. Below 800 °C, the SAXS contribution (Q<10 nm-1) showed only a small variation as a function of temperature. Above 800 °C, a strong increase in intensity is observed, accompanied by the precipitation of 2–3 nm zirconia domains. At high enough temperatures, >1000 °C, when the amorphous phase recrystallizes into the starting zircon structure, characteristics of surface-scattering are observed, associated to large zircon regions.

Type
Research Article
Copyright
Copyright © Materials Research Society 2004

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References

REFERENCES

[1] Holland, H.D. and Gottfried, D., Acta Cryst., 8, 291, (1955).Google Scholar
[2] Weber, W.J., Ewing, R.C. and Wang, L.M., J. Mater. Res., 9, 688, (1994).Google Scholar
[3] Radlinski, A.P., Claoué-Long, J., Hinde, A.L., Radlinska, E.Z. and Lin, J.-S., Phys. Chem. Minerals, 30, 631, (2003).Google Scholar
[4] Geisler, T., Trachenko, K., Ríos, S., Dove, M.T., and Salje, E.K.H., J. Physics: Condens. Matter 15, L597, (2003).Google Scholar
[5] Ríos, S. and Salje, E.K.H., Appl. Phys. Lett., in press.Google Scholar
[6] Farges, F., Phys. Chem. Minerals, 20, 504, (1994).Google Scholar
[7] Carrez, P., Forterre, C., Braga, D., and Leroux, H., Nucl. Instr. Meth.Phys. Res. B, in pressGoogle Scholar
[8] Meldrum, A., Zinkle, S.J., Boatner, L.A. and Ewing, R.C., Nature, 395, 56, (1998).Google Scholar
[9] Ríos, S. and Boffa-Ballaran, T., J. Appl. Cryst., 36, 1006, (2003).Google Scholar
[10] Woodhead, J.A., Rossman, G.R. and Silver, L.T., Am. Min., 76, 74, (1991).Google Scholar
[11] Zhang, M., Salje, E.K.H., Ewing, R.C., Farnan, I., Ríos, S., Schluter, J. and Leggo, P., J. Physics: Condens. Matter, 12, 5189, (2000).Google Scholar
[12] Capitani, G.C., Leroux, H., Doukhan, J.C., Ríos, S., Zhang, M. and Salje, E.K.H., Phys. Chem. Minerals, 27, 545556, (2000).Google Scholar
[13] Geisler, T., Phys. Chem. Minerals, 29, 420, (2002), and references therein.Google Scholar
[14] Colombo, M. and Chrosch, J., Rad. Phys. and Chem., 53, 555, (1998).Google Scholar