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首页> 外文期刊>International Journal of Quantum Chemistry >High-temperature transformations of Cu-rich hydrotalcites
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High-temperature transformations of Cu-rich hydrotalcites

机译:富铜水滑石的高温转变

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CuM(II)Al ternary hydrotalcites (M(II) = Ni, Co and Mg) with a (Cu + M(II))/Al atomic ratio of 3.0 and Cu/M(II) atomic ratio of 5.0 were synthesized by coprecipitation under low supersaturation. Powder X-ray diffraction of the as-synthesized samples showed a pattern characteristic of hydrotalcite-like (HT-like) structure (JCPDS: 41-1428). Thermal analyses of these samples showed four stages of weight loss/heat change when recorded in nitrogen. Analysis of the evolved gases characterized the nature of these transformations. The thermoanalytical effects differed significantly especially for the high-temperature transformations, when the treatment was performed in oxygen. In situ powder X-ray diffraction of the samples was carried out to elucidate the phase evolution of these compounds. Surprisingly formation of CuO was noted at temperatures around 200degreesC well below the destruction of the layered network. The nature of the resulting phases varied with both the nature of the co-bivalent metal ion and the heating atmosphere. FT-IR spectroscopy confirmed the retention of carbonate ions at higher temperatures (above 700degreesC), although the concentration of carbonate anion (most likely unidentate) varied with the calcination temperature. The crystallinity of CuO increased significantly above 600degreesC, probably through dissociation of copper oxycarbonate. Significant differences in the thermal transformation temperatures (for the third and the fourth transformations) of these samples containing different co-bivalent metal ions were not observed. This suggests that an association of the co-bivalent metal ions and/or trivalent metal ion in this phase is unlikely. A plausible thermal evolution scheme of these hydrotalcites is proposed. (C) 2003 Elsevier Inc. All rights reserved. [References: 35]
机译:通过共沉淀合成CuM(II)Al三元水滑石(M(II)= Ni,Co和Mg)(Cu + M(II))/ Al原子比为3.0和Cu / M(II)原子比为5.0在低过饱和度下。所合成样品的粉末X射线衍射显示出水滑石样(HT样)结构的图案特征(JCPDS:41-1428)。这些样品的热分析表明,在氮气中记录时,失重/热变化分为四个阶段。对逸出气体的分析表征了这些转变的性质。当在氧气中进行处理时,尤其是对于高温转变,热分析效果差异很大。对样品进行原位粉末X射线衍射,以阐明这些化合物的相演变。令人惊讶的是,在大约200摄氏度的温度下,远低于分层网络的破坏,形成了CuO。所得相的性质随共二价金属离子的性质和加热气氛而变化。 FT-IR光谱法证实了碳酸根离子在较高温度(高于700℃)下的保留,尽管碳酸根阴离子的浓度(极有可能是未知的)随煅烧温度而变化。 CuO的结晶度在600℃以上显着增加,这可能是由于碳酸氧铜的解离所致。在这些包含不同共价二价金属离子的样品中,未观察到热转变温度(第三次和第四次转变)的显着差异。这表明在该相中共二价金属离子和/或三价金属离子的缔合是不可能的。提出了这些水滑石的合理的热演化方案。 (C)2003 Elsevier Inc.保留所有权利。 [参考:35]

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