化学
膨润土
肺表面活性物质
分解
水溶液
氢氧化物
阳离子交换容量
甲醇
无机化学
核化学
化学工程
有机化学
土壤水分
地质学
土壤科学
工程类
生物化学
出处
期刊:Clay Minerals
[Cambridge University Press]
日期:2014-12-01
卷期号:49 (5): 683-692
被引量:7
标识
DOI:10.1180/claymin.2014.049.5.05
摘要
Abstract Organo-bentonites were prepared using a bentonite and an aqueous cetyltrimethylammonium hydroxide solution. The ratio of the surfactant (in mmoles) to the cation exchange capacity varied from 0.5 to 20, with 20 being the highest ratio ever reported in the literature. At high surfactant to cation exchange capacity ratios, the interlayer spacing increased to 3.75 nm due to the formation of a paraffin-type bilayer of surfactant cations, which was shown to be mainly in gauche conformations using solid state 13 C CP/NMR. When the exchange reaction was carried out in a methanol-water mixture, the expansion of the organo-bentonites depended on the concentration of methanol (% by volume). The decomposition temperatures of the organic cations depended on the basal spacing of the organo-bentonites, and in situ X-ray diffraction revealed that the basal spacing of our organo-bentonites was stable up to 210°C. Above this temperature, the basal spacing shrunk to 1.47 nm due to decomposition of the surfactants.
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