Pillaring Processes of Smectites with and Without Tetrahedral Substitution
Pillaring Processes of Smectites with and Without Tetrahedral Substitution
复制标题
有和没有四面体取代的蒙皂石的柱撑过程
DOI:
10.1346/ccmn.1987.0350201
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发表时间:
1987
影响因子:
2.2
通讯作者:
J. Fripiat
中科院分区:
文献类型:
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作者:
D. Plée;L. Gatineau;J. Fripiat
Pillaring of montmorillonite and beidellite with aluminum polyhydroxypolymer takes place first by the saturation of the cation-exchange capacity by monomeric and/or dimeric aluminum hydroxide species and then the intercalation of the so-called Al13-polyhydroxypolymer. The clay slurry must have a solid concentration greater than 0.01% (w/w) to produce a basal spacing of about 18 Å. Sizeable clay tactoids must therefore exist in the slurry in order to produce a turbostratic structure ordered along the c axis. The main difference between pillared montmorillonite and pillared beidellite seems to be a more ordered distribution of pillars within the interlamellar space of the clays that are rich in tetrahedral substitutions. Recent 27Al and 21Si high-resolution nuclear magnetic resonance data suggest that this higher degree of ordering results from the reaction of the aluminic pillars and the clay sheet near the sites of the tetrahedral substitutions.
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