TEM Observation of Interstratified Ni-Serpentine/Smectite Compounds
TEM Observation of Interstratified Ni-Serpentine/Smectite Compounds
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层间镍蛇纹石/蒙皂石化合物的 TEM 观察
DOI：
10.1246/cl.2000.344
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发表时间：
2000
影响因子：
1.6
通讯作者：
M. Chatterjee
中科院分区：
文献类型：
--
作者：
T. Nagase;T. Ebina;K. Torii;T. Iwasaki;H. Hayashi;Y. Onodera;M. Chatterjee
首次用透射电镜（TEM）描述了镍-蛇纹石/蒙皂石= 2/1的层间化合物。晶格条纹的图像与模拟结果相吻合，与X射线衍射图中具有相似周期性的蒙脱石/蒙脱石= 1/1矿物的晶格条纹图像明显不同。微畴的形貌向其蛇形部分的方向弯曲，表明颗粒表面主要由Si-O片层组成。
Interstratified Ni-serpentine/smectite = 2/1 compound was described by transmission electron microscopy (TEM) for the first time. The image of the lattice fringe coincided with the result of simulation, and it is clearly different from that of chlorite/smectite = 1/1 mineral which has a similar periodicity in X-ray diffraction pattern. The image of domains curving to the direction of their serpentine-part, suggested that the surface of the particle was mainly consisting of Si-O sheets.