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Birnessite-type manganese oxide-alkylamine mesophases obtained by intercalation and their thermal behaviour

机译:通过插层获得的水钠锰矿型氧化锰-烷基胺中间相及其热行为

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摘要

Layered birnessite-type manganese oxide inserts alkylamines (decylamine-octadecylamine) by ion-exchange and intercalation mechanisms and the concomitant expansion is compatible with formation of a head-to-tail layer of interdigitated amine.The structural arrangement of the MnO_2-alkylamine mesophases is sensitive to temperature,and at a temperature dependent on the chain length of the intercalated alkylamine,undergoes a phase transition to a more highly expanded phase.The basal spacing of the more expanded phases formed at higher temperature indicates that de-interdigitation occurs to give a bilayer organisation of neutral and protonated alkylamine species.The phase transition temperature is identified by differential scanning calorimetry.X-Ray absorption spectroscopy shows that while the local structure around manganese is not affected by intercalation,it provides evidence that this transition is accompanied by partial lowering of the oxidation state of manganese and migration of manganese into the interlayer region.This phase transition is reminiscent of some of those observed in phospholipid membranes,but seems to represent a new phenomenon for inorganic intercalates.
机译:层状水钠锰矿型氧化锰通过离子交换和插层机理插入烷基胺(癸胺-十八烷基胺),其伴随膨胀与指叉胺头尾层的形成相容.MnO_2-烷基胺中间相的结构排列为对温度敏感,并且在取决于插入的烷基胺链长的温度下,会发生相转变为更高膨胀的相。在较高温度下形成的更大膨胀相的基础间距表明,脱叉指的产生是为了通过差示扫描量热法确定相变温度。X射线吸收光谱表明,虽然锰周围的局部结构不受插层的影响,但它提供了这种转变伴随部分降低的证据。的氧化态和锰的迁移这种相变使人联想到在磷脂膜中观察到的那些,但似乎代表了无机插层的新现象。

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