Interstratified Clay Minerals

Interstratified Clay Minerals
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DOI:
10.1007/978-3-642-65917-1_8
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发表时间:
1975
期刊:
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影响因子:
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通讯作者:
D. Macewan;A. Ruiz-Amil
D. Macewan;A. Ruiz-Amil
中科院分区:
其他
文献类型:
--
作者:
D. Macewan;A. Ruiz-Amil

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层间化是通过 X 射线衍射研究粘土矿物时首次观察到的现象。值得注意的是,其中大多数都有基础反射(001),但没有形成规则的系列。经证实,这种不规则性是由于不同类型的结晶层的层间化造成的。
Interstratification is a phenomenon that was first observed on studying clay minerals by X-ray diffraction. It was noted that the majority of them had basal reflections (001), which did not form a regular series. It was verified that this irregularity was due to the interstratification of different types of crystalline layers.