首页> 外文会议>Trilateral Meeting on Clays >PREPARATION OF HOMOIONIC EXCHANGED SMECTITES IN BENTONITES: INFLUENCE OF VALENCE OF CATIONS AND INFLUENCE OF IMPURITIES ON THE EXCHANGE PROCEDURE
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PREPARATION OF HOMOIONIC EXCHANGED SMECTITES IN BENTONITES: INFLUENCE OF VALENCE OF CATIONS AND INFLUENCE OF IMPURITIES ON THE EXCHANGE PROCEDURE

机译:膨润土中同性化交换蒙脱石的制备:阳离子价值的影响及杂质对交换程序的影响

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The interlayers of natural smectites store a mixture of sodium and/or calcium and magnesium, respectively, and rarely potassium. Many chemical, mechanical and thermal properties of smectites and smectite-rich materials depend on the interlayer cations. Therefore, homoionic exchanged materials are prepared to investigate reaction mechanism as function of the interlayer cation or as function of the layer structure with uniform interlayer occupation. 54 publications from different journals from 1950 to 2009 were reviewed with respect to the applied homoionic exchange procedure. Only 6 papers reported on the result of homoionic exchange. Up to now there exists no general instruction to prepare homoionic exchanged smectites in dependency of layer charge, cation exchange capacity (CEC) and the obtained level of homoionic interlayers. The aim of the present study was to create a general instruction to prepare homoionic exchanged smectites and smectite-rich materials in dependency of the required cation and impurities of the used materials.
机译:天然壁的中间层分别储存钠和/或钙和镁的混合物,很少钾。许多化学,机械和热性能的蒙脱石和富透明岩材料取决于层间阳离子。因此,制备均匀交换材料以研究反应机制作为层间阳离子的功能或用作均匀层间占用的层结构的功能。 54来自1950年至2009年的不同期刊的出版物是关于应用的同种换部交换程序的审查。只有6篇论文报告了同性量交换的结果。到目前为止,在层电荷,阳离子交换能力(CEC)和所获得的同性夹层水平的依赖性中,没有一般性指示。本研究的目的是创造一般指导,以便在所需材料的所需阳离子和杂质的依赖性中制备均匀交换的麦片和富胶质材料。

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