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Thermal decomposition of the rare earth sulfates of cerium(III), cerium(IV), lanthanum(III) and samarium(III)

机译:铈(III),铈(IV),镧(III)和sa(III)的稀土硫酸盐的热分解

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Surface and bulk chemical and elemental composition of the rare earth sulfates of cerium(III), cerium(IV), lanthanum(III) and samarium(III) were characterized during various stages of thermal decomposition. Decomposition was conducted under both vacuum and atmospheric conditions. In situ analysis was conducted on samples decomposed in vacuum. As identified by X-ray diffraction, the bulk decomposition of all the rare earth sulfate samples to their corresponding oxide, in atmosphere, proceeded via the formation of an oxysulfate. For the exception of cerium(III) sulfate, similar results were obtained in thermogravimetric analysis. The thermal decomposition profile, as determined by X-ray microanalysis was similar to that observed in thermogravimetric analysis and X-ray diffraction. Elemental maps revealed no observable concentration gradients of sulfur. Surface composition was not necessarily representative of the bulk composition. Thermal decomposition of sulfates to an oxide initiated at a lower temperature in vacuum than that observed at atmospheric pressure. (C) 2003 Elsevier Science B.V All rights reserved. [References: 30]
机译:在热分解的各个阶段,对铈(III),铈(IV),镧(III)和s(III)的稀土硫酸盐的表面和本体化学及元素组成进行了表征。在真空和大气条件下均进行分解。对在真空中分解的样品进行原位分析。如通过X射线衍射所鉴定的,在大气中,所有稀土硫酸盐样品通过形成氧硫酸盐而大量分解成其相应的氧化物。除硫酸铈(III)外,在热重分析中获得了相似的结果。通过X射线微分析确定的热分解曲线与在热重分析和X射线衍射中观察到的相似。元素图显示没有可观察到的硫浓度梯度。表面组成不一定代表整体组成。在真空中比在大气压下观察到的温度低的温度下,硫酸盐热分解为氧化物。 (C)2003 Elsevier Science B.V保留所有权利。 [参考:30]

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