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Organic and inorganic complex of dolinite in coal-bearing strata

机译:含煤地层中白云石的有机和无机配合物

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摘要

A detailed study on intercalation of some organic and inorganic compounds in kaolinite that have volcanic origin in coal-bearing strata is made in this paper. The C-axis spacing in kaolinite expends to a largest value 1.14 nm by the intercalation of polar compound dimethylsulphoxide (DMSO) into kaolinite. The expansion value is relatively stable, and the rather strong perturbation of the OH stretching on the intercalation is observed in IR spectra.
机译:本文对含煤地层中火山成因的高岭石中某些有机和无机化合物的插层进行了详细研究。通过将极性化合物二甲亚砜(DMSO)插入高岭石中,高岭石中的C轴间距最大扩展到1.14 nm。膨胀值相对稳定,并且在IR光谱中观察到插层上的OH拉伸的相当强的扰动。

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