Isomorphous substitution of europium for strontium in the structure of synthetic hydroxovanadate

Polycrystalline strontium–europium hydroxovanadates Sr 10− x Eu x (VO 4) 6(OH) 2− x O x were synthesized and studied by X-ray powder diffraction, infrared absorption and diffuse-reflectance spectroscopies and also thermogravimetry. The single-phase region of isomorphous substitution of Eu for Sr in...

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Bibliographic Details
Published in:Journal of solid state chemistry Vol. 181; no. 9; pp. 2386 - 2392
Main Authors: Get’man, E.I., Yablochkova, N.V., Loboda, S.N., Prisedsky, V.V., Antonovich, V.P., Chivireva, N.A.
Format: Journal Article
Language:English
Published: Amsterdam Elsevier Inc 01-09-2008
Elsevier
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Summary:Polycrystalline strontium–europium hydroxovanadates Sr 10− x Eu x (VO 4) 6(OH) 2− x O x were synthesized and studied by X-ray powder diffraction, infrared absorption and diffuse-reflectance spectroscopies and also thermogravimetry. The single-phase region of isomorphous substitution of Eu for Sr in hydroxovanadate has been found to lie in the compositional interval 0⩽ x⩽0.18 at 800 °C. Refinement of X-ray diffraction (XRD) patterns by the Rietveld method shows that Eu substitutes for Sr preferentially at the Sr(1) sites of the apatite structure. The substitution results in a more uniform distribution of Sr–O bond lengths in coordination polyhedra both around Sr (1) and Sr (2) sites and also in a slight contraction of the vanadate anion VO 4 3−. Synthetic Sr hydroxovanadates absorb a considerable amount of water in two forms: capillary condensed and chemically combined. The latter form may be absorbed at temperatures as high as 500 °C. The results of this paper contribute to a general picture of substitution effects of the rare-earth (RE) elements in the apatite structure. The dependence of the substitution limit x max in Sr 10− x RE x (VO 4) 6(OH) 2− x O x on the atomic number of the RE element is shown here with the present data marked with red color.
ISSN:0022-4596
1095-726X
DOI:10.1016/j.jssc.2008.06.003