Crystal structure study of new lanthanide silicates with silico-carnotite structure
The crystal structures of new rare earth-based silicate compounds (Ca{sub 3}Eu{sub 2}Si{sub 3}O{sub 12}, Ca{sub 3}Gd{sub 2}Si{sub 3}O{sub 12}, Ca{sub 3}Dy{sub 2}Si{sub 3}O{sub 12}, Ca{sub 3}Er{sub 2}Si{sub 3}O{sub 12} and Ca{sub 3}Lu{sub 2}Si{sub 3}O{sub 12}) have been determined using powder X-ray diffraction. From Rietveld refinement calculations on the collected powder patterns we observe a different distribution of the rare earth ions on the three available crystal sites characterized by different coordination numbers, depending on the ionic radius of the rare earth ion. The reasons of the instability of the silico-carnotite structure for lanthanide ions larger than Eu{sup 3+} have been deduced. In addition, in order to detect crystal phase transitions, the powder patterns of Ca{sub 3}Eu{sub 2}Si{sub 3}O{sub 12} and Ca{sub 3}Sm{sub 2}Si{sub 3}O{sub 12} samples have been collected as a function of the temperature (RT-1000 Degree-Sign C range), but no phase transitions have been observed. - Graphical abstract: Synchrotron X-ray diffraction allows us the accurate determination of the RE{sup 3+} ions distribution on the three available crystal sites of the silico-carnotite structure. Highlights: Black-Right-Pointing-Pointer The structure of the Ca{sub 3}M{sub 2}Si{sub 3}O{sub 12} (M=Eu, Gd, Dy, Er and Lu) was determined. Black-Right-Pointing-Pointer Different distribution of RE{sup 3+} ions on the three available crystal sites was observed. Black-Right-Pointing-Pointer The instability of the silico-carnotite structure for RE=La{yields}Sm was discussed.