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Thermal decomposition of hydrotalcite with chromate, molybdate or sulphate in the interlayer

机译:水滑石在夹层中与铬酸盐,钼酸盐或硫酸盐的热分解

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摘要

The thermal decomposition of hydrotalcites with chromate, molybdate and sulphate in the interlayer has been studied using thermogravimetric analysis coupled to a mass spectrometer measuring the gas evolution. X-ray diffraction shows the hydrotalcites have a d(0 0 3) spacing of 7.98 angstrom with very small differences in the d-spacing between the three hydrotalcites. XRD was also used to determine the products of the thermal decomposition. For the sulphate-hydrotalcite decomposition the products were MgO and a spinet MgAl2O4, for the chromate interlayered hydrotalcite MgO, Cr2O3 and spinel. For the molybdate interlayered hydrotalcite the products were MgO, spinet and MgMoO4. EDX analyses enabled the formula of the hydrotalcites to be determined. Two processes are observed in the thermal decomposition namely dehydration and dehydroxylation and for the case of the sulphate interlayered hydrotalcite, a third process is the loss of sulphate. Both the dehydration and dehydroxylation take place in three steps each for each of the hydrotalcites. (c) 2005 Elsevier B.V. All rights reserved.
机译:使用热重分析结合质谱仪测量气体逸出,研究了中间层中水滑石与铬酸盐,钼酸盐和硫酸盐的热分解。 X射线衍射显示水滑石的d(0 0 3)间距为7.98埃,三个水滑石之间的d间距差异很小。 XRD还用于确定热分解产物。对于硫酸盐-水滑石分解,产物为MgO和尖晶石MgAl2O4,对于铬酸盐层间水滑石MgO,Cr2O3和尖晶石。对于钼酸盐层间水滑石,产物为MgO,尖晶石和MgMoO4。 EDX分析可以确定水滑石的配方。在热分解中观察到两个过程,即脱水和脱羟基,对于硫酸盐层间水滑石,第三个过程是硫酸盐的损失。每种水滑石的脱水和脱羟基都分三个步骤进行。 (c)2005 Elsevier B.V.保留所有权利。

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