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首页> 外文期刊>Journal of Materials Science >Thermal decomposition products of hydrotalcite-like compounds: low-temperature metaphases
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Thermal decomposition products of hydrotalcite-like compounds: low-temperature metaphases

机译:类水滑石化合物的热分解产物:低温中期

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摘要

Synthetic hydrotalcite-like samples withcomposition [M1-x2+Alx3+(OH)2] (CO3)x/2·nH2O, whereM=Mg,Ni,x=0.25 and 0.33,n=2x and 1.5x,are studied by XRD,DTA,TG and IR spectroscopy after heating in the temperatureinterval 120-260℃and rehydration in air and water. Structuralmodels of the two metaphases obtained are proposed.Metahydrotalcite-D(HT-D) is formed at 140-180℃by thereversible dehydration of the interlayer. Metahydrotacite-B(HT-B)is formed at temperatures 240-260℃as a result of thedehydroxilation of a part f OH groups of the brucite-like layer andinclusion of two oxygenes from the CO3-group in the same layer.The HT-B has a specific crystal structure. Rehydration does notrestore the initial structural state but leads to the formation of aphase (HT-B-r) charactrized with increased thickness of theinterlayer, high content of water and a low temperature ofdehydration. The properties of HT-B depend on the ratio M2+:Al ofthe initial sample.The substitution Mg?Ni does not influence theproperties of the metaphases in the low temperature region.
机译:用XRD研究了组成为[M1-x2 + Alx3 +(OH)2](CO3)x / 2·nH2O的合成类水滑石样品,其中M = Mg,Ni,x = 0.25和0.33,n = 2x和1.5x,在120-260℃的温度范围内加热并在空气和水中复水后的DTA,TG和IR光谱。提出了两个过渡相的结构模型。中间层可逆脱水在140-180℃形成了水滑石-D(HT-D)。由于水镁石样层的一部分f OH基团的脱氢氧化作用以及在同一层中包含来自CO3-基团的两个氧,因此在240-260℃的温度下生成了偏氢水滑石-B(HT-B)。 B具有特定的晶体结构。再水合不能恢复初始结构状态,而是导致形成无相(HT-B-r),其特征在于中间层厚度增加,水含量高和脱水温度低。 HT-B的性质取决于初始样品的M2 +:Al比率。取代Mg?Ni不会影响低温区的中间相的性质。

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