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首页> 外文期刊>Journal of Solid State Chemistry >Crystal chemistry of the divalent cation in alluaudite-type phosphates: A structural and infrared spectral study of the Na-1.5(Mn1-xMx2+)(1.5)Fe-1.5(PO4)(3) solid solutions (x = 0 to 1, M2+ = Cd2+, Zn2+)
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Crystal chemistry of the divalent cation in alluaudite-type phosphates: A structural and infrared spectral study of the Na-1.5(Mn1-xMx2+)(1.5)Fe-1.5(PO4)(3) solid solutions (x = 0 to 1, M2+ = Cd2+, Zn2+)

机译:钙铝石型磷酸盐中二价阳离子的晶体化学:Na-1.5(Mn1-xMx2 +)(1.5)Fe-1.5(PO4)(3)固溶体(x = 0至1,M2 + = Cd2 +,Zn2 +)

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摘要

Compounds of the Na-1.5(Mn1-xMx2+)(1.5)Fe-1.5(PO4)(3) (M2+ = Cd2+, Zn2+) alluaudite-type solid solutions were synthesized by solid-state reactions in air, between 800 and 900 degrees C, and were investigated by X-ray powder diffraction and infrared spectroscopy. The site occupancy factors of the Na-1.5(Mn1-xCdx2+),,, x Fe-1.5(PO4)(3) compounds, obtained from the Rietveld refinements of the X-ray powder patterns, indicate that the replacement of Mn2+ by CA(2+) takes place on the M(1) site for x = 0.25 and 0.50, and then on the M(1) and M(2) sites for x = 0.75 and 1.00. Small amounts of Cd2+ were also detected on the A(1) site, compensated by small amounts of Na+ occurring on M(1). This partially disordered distribution is probably due to the similar effective ionic radii of Cd2+ and Na+. The cationic distributions in the Na-1.5(Mn1-x,Zn-x(2+))(1.5)Fe-1.5(PO4)(3) solid solution indicate that Zn2+ was first introduced in the M(2) site, before to replace Mn2+ in the M(1) site. The unit-cell parameters show a significant increase when Mn2+ is replaced by Cd2+, and a significant decrease when it is replaced by Zn2+. The variations of the beta angle were also correlated with the M(1)-M(2) distances. The infrared spectra show the displacement of an absorption band at ca. 400-425 cm(-1), which is assigned to the vibrations of the M2+ cations localized on the M(1) site. This assignment is confirmed by the excellent correlations between the M(1)-O bond distances and the energy of the absorption band.
机译:Na-1.5(Mn1-xMx2 +)(1.5)Fe-1.5(PO4)(3)(M2 + = Cd2 +,Zn2 +)钙铝石型固溶体的化合物是通过在800至900度的空气中通过固态反应合成的C,并通过X射线粉末衍射和红外光谱研究。从X射线粉末图的Rietveld精炼获得的Na-1.5(Mn1-xCdx2 +),x Fe-1.5(PO4)(3)化合物的位点占据因子表明,CA替代了Mn2 + (2+)在x = 0.25和0.50的M(1)站点上发生,然后在x = 0.75和1.00的M(1)和M(2)站点上发生。在A(1)站点上也检测到少量Cd2 +,由在M(1)上发生的少量Na +补偿。这种部分无序的分布可能是由于Cd2 +和Na +的有效离子半径相似。 Na-1.5(Mn1-x,Zn-x(2 +))(1.5)Fe-1.5(PO4)(3)固溶体中的阳离子分布表明Zn2 +首先被引入M(2)位替换M(1)站点中的Mn2 +。当Mn2 +被Cd2 +取代时,晶胞参数显示出显着增加,而当Zn2 +替代时,晶胞参数则显着下降。 β角的变化也与M(1)-M(2)距离相关。红外光谱显示吸收带的位移约为。 400-425 cm(-1),分配给位于M(1)位置的M2 +阳离子的振动。 M(1)-O键距与吸收带能量之间的良好相关性证实了这种分配。

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