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镍取代云母蒙脱石的结构表征
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, 20(4): 528-534
作者姓名:宋学敏 陆善祥
作者单位:Laval大学,华东理工大学联合化学反应工程研究所,华东理工大学化学系,华东理工大学石油加工研究所
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。

关 键 词:镍 催化剂 蒙脱石 云母蒙脱石 XRD

Structural Charactertization of Nickel-Substituted Mica Montmorillonite
Song Xuemin, Lu Shanxiang, Xu Zhige,Li Chenglie and Liu Fuyjng. Structural Charactertization of Nickel-Substituted Mica Montmorillonite[J]. Journal of East China University of Science and Technology, 1994, 20(4): 528-534
Authors:Song Xuemin   Lu Shanxiang   Xu Zhige  Li Chenglie  Liu Fuyjng
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.
Keywords:clay mineral  Nickel  X-ray diffraction analysis  IR spectra  catalyst  mont-morillonite
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