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Radiation Effects in Zircon, Hafnon, and Thorite: Implications for Pu Disposal

Published online by Cambridge University Press:  15 February 2011

A. Meldrum
Affiliation:
Oak Ridge National Laboratory, Oak Ridge, TN 37831
S.J. Zinkle
Affiliation:
Oak Ridge National Laboratory, Oak Ridge, TN 37831
L.A. Boatner
Affiliation:
Oak Ridge National Laboratory, Oak Ridge, TN 37831
M. Wu
Affiliation:
Fisk University, Dept. of Physics, Nashville, TN 37208
R. Mu
Affiliation:
Fisk University, Dept. of Physics, Nashville, TN 37208
A. Ueda
Affiliation:
Fisk University, Dept. of Physics, Nashville, TN 37208
D.O. Henderson
Affiliation:
Fisk University, Dept. of Physics, Nashville, TN 37208
R.C. Ewing
Affiliation:
The University of Michigan, Dept. of Nuclear Engineering and Radiological Sciences, Ann Arbor, MI 48109
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Abstract

Synthetic ZrSiO4, HfSiO4, and ThSiO4 single-crystal specimens were irradiated by 800 keV Kr+ ions, and the microstructural evolution was observed in-situ in a transmission electron microscope. All three compounds were found to become amorphous up to temperatures in excess of 600°C. Using a new model, the activation energies for annealing were found to be in the range of 3.1 to 3.6 eV for these compounds. At temperatures above 600°C, the orthosilicates were observed to decompose into the component oxides (e.g., tetragonal ZrO2 + amorphous SiO2 in the case of zircon). A single-crystal zircon specimen was also irradiated with a pulsed picosecond Nd:YAG laser operated at 355 nm, and the resulting microstructure was investigated by optical absorption, SEM, AFM, and TEM techniques.

Type
Research Article
Copyright
Copyright © Materials Research Society 1999

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References

1 Vance, E.R. and Anderson, B.W., Mineral. Mag. 38, 605(1972).Google Scholar
2 Ewing, R.C., Lutze, W., and Weber, W.J., J. Mater. Res. 10, 243(1995).Google Scholar
3 Weber, W.J., Ewing, R.C., Catlow, C.R.A., Rubia, T. Diaz de la, Hobbs, L.W., Kinoshita, C., Matzke, Hj., Motta, A.T., Nastasi, M.A., Salje, E.H.K., Vance, E.R., and Zinkle, S.J., J. Mater. Res. 13, 1434 (1998).Google Scholar
4 Weber, W.J., Ewing, R.C., and Wang, L.M., J. Mater. Res. 9, 688 (1994).Google Scholar
5 Meldrum, A., Zinkle, S.J., Boatner, L.A., and Ewing, R.C., Phys. Rev. B (in press).Google Scholar
6 Miller, M.L. and Ewing, R.C., Ultramicroscopy 48, 203(1992).Google Scholar
7 Zinkle, S.J. and Kinoshita, C., J. Nucl. Mater. 251, 200 (1997).Google Scholar
8 Virk, H.S., Radiat. Eff. Def. Sol. 133, 87 (1995).Google Scholar
9 Meldrum, A., Boatner, L.A., Weber, W.J., and Ewing, R.C., Geochim. Cosmochim. Acta 62, 2509 (1998)Google Scholar
10 Meldrum, A., Zinkle, S.J., Boatner, L.A., and Ewing, R.C., Nature 395, 56 (1998).Google Scholar
11 Wang, S.X., Wang, L.M., Ewing, R.C., and Doremus, R.H., J. Non-Cryst. Sol. 238, 198 (1998).Google Scholar