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Surface structure and intercalative polymerization studies of smectite clay thin films

机译:绿土粘土薄膜的表面结构和插层聚合研究

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The microstructure of the clay minerals Cu~(2+) exchanged hectorite, Na~+ exchanged hectorite, Na~+ exchanged montmorillonite and Ca~(2+) exchanged montmorillonite were studied using scanning force microscopy (SFM), electron spin resonance (ESR), and x-ray diffraction. The montmorillonite films displayed the rough clay fabric commonly associated with these materials. Ca~(2+) montmorillonite films consisted of a porous web-like grain structure, while Na~+ montmorillonite films were composed of clumps of smaller discrete grains. The lesser studied hectorite films, however, revealed many large, flat regions suitable for further SFM examination and polymerization studies. The chemical reactivity fot he hectorite clays was studied by examining polymerization reactions occurring when the clays were exposed to benzene and aniline. In the case of standard Na~+ exchanged hectorite, little or no reactivity was observed upon exposure to the various monomers. For the Cu~(2+) exchanged hectorite, large scale intergallery and surface polymerization were observed upon exposure to aniline, with intergallery polymerization observed in the case of benzene.
机译:利用扫描力显微镜(SFM),电子自旋共振(ESR)研究了Cu〜(2+)交换锂蒙脱石,Na〜+交换锂蒙脱石,Na〜+交换蒙脱石和Ca〜(2+)交换蒙脱石等粘土矿物的微观结构。 )和X射线衍射。蒙脱石薄膜显示出通常与这些材料相关的粗糙粘土织物。 Ca〜(2+)蒙脱土薄膜由多孔网状晶粒结构组成,而Na〜+蒙脱土薄膜由较小的离散晶粒团块组成。然而,研究较少的锂蒙脱石膜显示出许多大的平坦区域,适合于进一步的SFM检查和聚合研究。通过检查当粘土暴露于苯和苯胺时发生的聚合反应,研究了锂蒙脱石粘土的化学反应性。在标准的Na +交换锂蒙脱石的情况下,暴露于各种单体后几乎没有观察到反应性。对于Cu〜(2+)交换的锂蒙脱石,在暴露于苯胺时观察到大规模的族间和表面聚合,在苯的情况下观察到族间聚合。

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