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    宋学敏, 陆善祥. 镍取代云母蒙脱石的结构表征[J]. 华东理工大学学报(自然科学版), 1994, (4): 528-534.
    引用本文: 宋学敏, 陆善祥. 镍取代云母蒙脱石的结构表征[J]. 华东理工大学学报(自然科学版), 1994, (4): 528-534.
    Structural Charactertization of Nickel-Substituted Mica Montmorillonite[J]. Journal of East China University of Science and Technology, 1994, (4): 528-534.
    Citation: Structural Charactertization of Nickel-Substituted Mica Montmorillonite[J]. Journal of East China University of Science and Technology, 1994, (4): 528-534.

    镍取代云母蒙脱石的结构表征

    Structural Charactertization of Nickel-Substituted Mica Montmorillonite

    • 摘要: 对不同镍含量的镍取代云母蒙脱石(NiSMM)样品,通过XRD分析,阳离子交换容量和比表面积测定,证明随着镍含量的增加,镍越来越多地进入到单元层结构中。NiSMM具有与天然蒙脱石相同的层状结构,其层间填充着可被交换的阳离子。这些阳离子大多数是NH4^+。XRD的d060值和红外光谱的骨架振动吸收带进一步表明,镍是进入到单元层中八面体片的六配位中心离子的位置上。NiSMM的结构稳定性高于天然蒙脱石。

       

      Abstract: The structure of NiSM M(Nickel-Substituted Mica Montmorillonite) samplesprepared under different conditions were characterized by means of XRD analysis,CEC andsurface area measurements,and IR analysis. It was shown that mote nickel enters the layerstructure of NiSM M when more nickel is added to starting matcrials for the synthesis. NIS-MM has the same layer structure as that in natural smectite.There are exchangable cationsbetween the layers, most of which are The d_(060) value of XRD pattern and the skeletalvibration of IR spectra reveal that nickel ions are located at the centers of octahedra inthe unit layer of NiSMM.

       

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