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TG DTA studies of dehydration behaviors for montmorillonites

机译:蒙脱石脱水行为的TG DTA研究

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The dehydration properties for Na{sup}+-, K{sup}+-, Cu{sup}(2+)- and Co{sup}(2+)- saturated montmorillonites in the temperature range up to 1200°C with TG-DTA were examined. The changes of the dehydration behaviors on the specimens were measured by TG-DTA. From the results of TG analysis, it was recognized that the amounts of water dehydrated for the water adsorbed in the interlayer until 200°C were 8.10% (Na-mont.), 6.99% (K-mont.), 10.1% (Cu-mont.), 12.9% (Co-mont.), respectively. And the amounts of weight losses till 1200°C were 13.7%(Na-mont.), 13.0%(K-mont.), 16.8%(Cu-mont.), 19.5% (Co-mont.), respectively. From the DTA curves, the endothermic peak causing by the water co-ordinated the divalent cations was observed around 172°C for Cu-mont and the peak for Co-mont. was shifted to higher temperature around 200°C That endothermic peaks by dehydration due to the water co-ordinated metal ions were not recognized for Na-mont., K-mont. These results was indicated that the valence number or the sorts of the cations in the interlayer the play an important role in its dehydration properties.
机译:Na {sup} + - ,k {sup} + - ,cu {sup}(2 +) - 和co {sup}(2 +) - 饱和蒙脱石的脱水性能在温度范围内高达1200°C,Tg -DTA被检查。通过TG-DTA测量样品上的脱水行为的变化。从TG分析的结果中,认识到,在中间蛋白中吸附的水脱水的水量为200℃,为8.10%(Na-Mont。),6.99%(K-MONT。),10.1%(Cu - 声。)分别为12.9%(Co-Mont)。并且重量损失的量直至1200℃为13.7%(Na-Mont。),13.0%(K-Mont。),16.8%(Cu-Mont。),19.5%(Co-Mont。)。从DTA曲线,通过水协调的冷热峰被统一阳离子约为172℃,用于Cu-Mont和Co-Mont的峰。在200℃的较高温度下向较高的温度转移到200℃,通过由于水协调金属离子而通过脱水吸热峰被Na-Mont识别。,K-Mont。这些结果表明,中间层中的阳离子中的价值或各种阳离子在其脱水性质中起重要作用。

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