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Crystal Chemistry and Cation Ordering in Zirconolite 2M

Published online by Cambridge University Press:  21 March 2011

G.R. Lumpkin ,
K.R. Whittle ,
C.J. Howard ,
Z. Zhang ,
F.J. Berry ,
G. Oates ,
C.T. Williams  and
A.N. Zaitsev
G.R. Lumpkin
Affiliation:
Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK ANSTO Materials, Private Mail Bag 1, Menai 2234, NSW, Australia
K.R. Whittle
Affiliation:
Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK
C.J. Howard
Affiliation:
ANSTO Materials, Private Mail Bag 1, Menai 2234, NSW, Australia
Z. Zhang
Affiliation:
ANSTO Materials, Private Mail Bag 1, Menai 2234, NSW, Australia
F.J. Berry
Affiliation:
Department of Chemistry, The Open University, Milton Keynes MK7 6AA, UK
G. Oates
Affiliation:
Department of Chemistry, The Open University, Milton Keynes MK7 6AA, UK
C.T. Williams
Affiliation:
Department of Mineralogy, The Natural History Museum, London, SW7 5BD, UK
A.N. Zaitsev
Affiliation:
Department of Mineralogy, The Natural History Museum, London, SW7 5BD, UK
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Abstract

Structural studies of single phase or nearly single phase zirconolite ceramic samples have been conducted using electron microscopy and microanalysis, X-ray diffraction, neutron diffraction, and spectroscopic methods. We show that it is possible to produce a complete series of zirconolite 2M samples with substitution of 2Ti by Nb+Fe in the HTB layer. The samples are single phase up to about 80% Nb +Fe substitution, with the appearance of a minor perovskite phase at higher Nb+Fe levels. Electron probe microanalysis reveals that the samples are homogeneous and close to their nominal compositions, except for those containing perovskite, which have a slight excess of Zr and a deficiency in the Fe content. The lattice parameters and the positions of certain Raman bands are non-linear as a function of composition, suggesting the possibility of cation ordering over the three available Ti sites within the HTB layer. Rietveld refinement of Synchrotron X-ray powder data for the Nb+Fe end-member have been conducted for the disordered case and for six trial models each with a different ordering scheme. Results of this exercise indicate that Fe preferentially occupies the Ti2 (split) site with partial ordering of Nb and the remaining Fe over the Ti1 and Ti2 octahedra. The preference of Fe for the five coordinated Ti2 site has been confirmed by 57Fe Mossbauer spectroscopy.

Type
Research Article
Information
MRS Online Proceedings Library (OPL) , Volume 932: Symposium – Scientific Basis for Nuclear Waste Management XXIX , 2006 , 53.1
Copyright
Copyright © Materials Research Society 2006

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References

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