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首页> 外文期刊>International Journal of Quantum Chemistry >Rare earth phosphate powders RePO4 center dot nH(2)O (Re = La, Ce or Y) II. Thermal behavior
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Rare earth phosphate powders RePO4 center dot nH(2)O (Re = La, Ce or Y) II. Thermal behavior

机译:稀土磷酸盐粉末RePO4中心点nH(2)O(Re = La,Ce或Y)II。热行为

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摘要

The thermal behavior, thermostructural and morphological changes, of rare earth phosphate powders RePO4 (.) nH,0 (Re La, Ce or Y) was investigated up to 1500degreesC using high temperature X-ray diffraction, FT-infrared and Raman spectroscopies and thermogravimetry coupled with differential thermal analysis. The hydration water of the compounds was zeolitic (for Re = La or Ce) or coordinated (for Re = Y) and was associated with a divariant or a monovariant equilibrium of dehydration, respectively. The high temperature anhydrous monoclinic phase LaPO4 or CePO4 formed irreversibly at about 750degreesC after the total dehydration of the hexagonal hydrated structure while the dehydration of the monoclinic YPO4 (.) 2H(2)O phase began from about 190degreesC with its simultaneous decomposition into tetragonal YPO4. A polytrioxophosphate secondary minor phase Re(PO3)(3) resulting from adsorbed H3PO4 was formed at 950degreesC and decomposed at 1350degreesC. The particle morphology did not change with the temperature but grain coalescence occurred below 1000degreesC. (C) 2003 Elsevier Inc. All rights reserved.
机译:使用高温X射线衍射,傅立叶变换红外光谱和拉曼光谱以及热重分析法研究了稀土磷酸盐粉末RePO4(。)nH,0(Re La,Ce或Y)的热行为,热结构和形貌变化,直至1500°C。结合差热分析。化合物的水合水是沸石的(对于Re = La或Ce)或配位的(对于Re = Y),分别与脱水的单变量或单变量平衡有关。六方水合结构完全脱水后,高温无水单斜晶相LaPO4或CePO4在约750°C不可逆地形成,而单斜晶YPO4(。)2H(2)O相的脱水从约190°C开始,同时分解为四方YPO4 。由H 3 PO 4吸附而形成的聚三氧磷酸盐次级次要相Re(PO 3)(3)在950℃形成并在1350℃分解。颗粒的形貌没有随温度变化,但在低于1000℃时发生了颗粒聚结。 (C)2003 Elsevier Inc.保留所有权利。

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