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Reactivity of kaolinite in ionic liquids:preparation and characterization of a 1-ethyl pyridinium chloride-kaolinite intercalate

机译:高岭石在离子液体中的反应活性:1-乙基吡啶鎓氯化物-高岭石插层酸盐的制备和表征

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摘要

A novel class of organic-inorganic nanohybrid material was prepared by the intercalation in kaolinite of a molten organic salt (1-ethyl pyridinium chloride,EP) above its melting temperature.The intercalation proceeded at 170 deg C under N_2.It did not succeed when kaolinite was used as the starting material,whereas the melt intercalation process was possible when DMSO-kaolinite (DMSO-K) was used as the starting material.The amount of EP loaded in the galleries of kaolinite is 24.3% (0.574 mol of EP per unit-cell) which produces an increase of the basal spacing d_(001) from 1.10 nm in the case of DMSO-K to 1.35 nm.The melt intercalation process could be dramatically improved by the choice of the temperature of reaction as well as of the atmosphere.At lower temperatures (less than 140 deg C),even if the reaction medium is the ionic liquid,the intercalation is not observed.This results from the non-release of DMSO from the interlamellar space of DMSO-K,a step essential for the intercalation of EP to proceed.This work indicates that the intercalation of EP and the displacement of DMSO from the interlamellar spaces of kaolinite take place concurrently,not in a sequential manner.However,the process is initially driven by the thermal removal of DMSO.
机译:在熔融温度以上将熔融的有机盐(1-乙基吡啶鎓氯化物,EP)嵌入高岭石中,制得了一类新型的有机-无机纳米杂化材料。在N_2下于170℃进行嵌入,但当温度升高时,嵌入没有成功。以高岭石为起始原料,而以DMSO-高岭石(DMSO-K)为起始原料,则可以进行熔融插层过程。高岭石画廊中的EP含量为24.3%(0.574 mol EP / g晶胞)可使d_(001)的基本间距从DMSO-K的1.10 nm增加到1.35 nm。通过选择反应温度和反应温度可以显着改善熔体嵌入过程在较低的温度(低于140摄氏度)下,即使反应介质是离子液体,也未观察到嵌入。这是由于DMSO从DMSO-K的层间空间未释放而导致的,插层必不可少的这项工作表明,EP的嵌入和DMSO从高岭石层间空间的置换是同时发生的,而不是以顺序的方式发生的。但是,该过程最初是由DMSO的热去除驱动的。

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