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Some Studies on Dehydroxylation-Rehydration Phenomenon of Kaolin of Indian Origin

机译:印度高岭土脱羟基复水现象的一些研究

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Dehydroxylated kaolin has widespread application in the synthesis of mullite ceramics. In the present study, a new source of highly pure kaolin from western part of India was used as a raw material to investigate the dehydroxylation-rehydroxylation behavior utilizing DTA/TGA and FTIR technique. The results showed that kaolin used in this study possesses high degree of crystalinity and retained its structure up to some extent even after dehydroxylation at 700℃ with a tendency to rehydrate. The DTA peak at 1000℃ supports the high reactivity of dehydroxylated kaolin and the peak is associated with the formation of mullite. The SEM study does not reveal any major microstructural changes after dehydroxylation. However, the XRD pattern of raw clay shown kaolin as major phase which converted to amorphous nature after dehydroxylation and subsequent grinding.
机译:脱羟基高岭土在莫来石陶瓷的合成中具有广泛的应用。在本研究中,使用了来自印度西部的高纯高岭土的新来源作为原料,利用DTA / TGA和FTIR技术研究了脱羟基-再羟基化行为。结果表明,本研究中所用的高岭土具有较高的结晶度,即使在700℃脱羟基后也能在一定程度上保留其结构,并具有再水化的趋势。在1000℃的DTA峰支持脱羟基高岭土的高反应性,并且该峰与莫来石的形成有关。 SEM研究没有揭示脱羟基后的任何主要微观结构变化。然而,未加工粘土的XRD图谱显示高岭土为主要相,其在脱羟基和随后的研磨后转变为无定形性质。

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