简介概要

Spectroscopic studies and Rietveld refinement of strontium-britholites

来源期刊:Journal of Rare Earths2008年第4期

论文作者:Khaled Boughzala Ezzedine Ben Salem Fethi Kooli Pierre Gravereau Khaled Bouzouita

文章页码:483 - 489

摘    要:Strontium-britholites whose chemical formula was Sr10–xLax(PO4)6–x(SiO4)xF2, where x=0, 1, 2, and 4 were prepared by solid state reaction. The structural refinement carried out using the Rietveld method indicated that La3+ ions were located into the two sites with a strong preference for metal (2) sites especially for low contents. A progressive shift of the F- position along the c-axis outside the centre of the triangle formed by metal (2)-atoms was observed with the increase of x. The infrared and Raman spectra exhibited the characteristic vibration modes of PO4 and SiO4 groups confirming the incorporation of this last group into the apatite structure. The 29Si MAS-NMR spectra exhibited one reso- nance peak confirming the data obtained by X-ray diffraction, indicating that P and Si were located in the same crystallographic site.

详情信息展示

Spectroscopic studies and Rietveld refinement of strontium-britholites

Khaled Boughzala,Ezzedine Ben Salem,Fethi Kooli,Pierre Gravereau,Khaled Bouzouita

摘 要:Strontium-britholites whose chemical formula was Sr10–xLax(PO4)6–x(SiO4)xF2, where x=0, 1, 2, and 4 were prepared by solid state reaction. The structural refinement carried out using the Rietveld method indicated that La3+ ions were located into the two sites with a strong preference for metal (2) sites especially for low contents. A progressive shift of the F- position along the c-axis outside the centre of the triangle formed by metal (2)-atoms was observed with the increase of x. The infrared and Raman spectra exhibited the characteristic vibration modes of PO4 and SiO4 groups confirming the incorporation of this last group into the apatite structure. The 29Si MAS-NMR spectra exhibited one reso- nance peak confirming the data obtained by X-ray diffraction, indicating that P and Si were located in the same crystallographic site.

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