Department of Applied Chemistry, School of Advanced Science and Engineering , Waseda University , 3-4-1 Okubo, Shinjuku-ku , Tokyo 169-8555 , Japan.
Department of Earth Sciences, School of Education , Waseda University , Nishiwaseda 1-6-1, Shinjuku-ku , Tokyo 169-8050 , Japan.
Langmuir. 2018 Oct 30;34(43):12694-12701. doi: 10.1021/acs.langmuir.8b01728. Epub 2018 Oct 22.
The solid acidity of the interlayer aluminol surfaces of kaolinite was explored by solid-state P nuclear magnetic resonance with magic angle spinning (MAS) using triethylphosphine oxide (TEPO), which formed a monolayer with a uniform orientation between the layers of kaolinite as a probe molecule. Intercalation of TEPO between the layers of kaolinite was achieved using methoxy-modified kaolinite as an intermediate. The presence of TEPO in the reaction products was revealed by the two signals at 21 and 7 ppm, which were assignable to ethyl groups in TEPO, in the solid-state C nuclear magnetic resonance with cross polarization and magic angle spinning techniques (C CP/MAS NMR). The presence of TEPO between the layers of kaolinite was demonstrated by the expansion of basal spacing from 0.86 nm, the interlayer distance of methoxy-modified kaolinite to 1.16 nm, as shown by the X-ray diffraction patterns, suggesting the formation of a TEPO monolayer between the layers of kaolinite. The formation of hydrogen bonds between the P═O groups of TEPO and the aluminol groups on the interlayer surfaces of kaolinite was also revealed by the appearance of an additional OH stretching band at 3598 cm in the Fourier-transform infrared spectrum and narrow solid-state P MAS NMR signals observed at 55-53 ppm which were shifted from the position of the physisorbed TEPO (50 ppm). These results clearly indicate that the solid acidity of interlayer aluminol groups of methoxy-modified kaolinite was probed using an interacted TEPO monolayer.
采用固体核磁共振中的魔角旋转(MAS)技术,利用三乙氧基氧化膦(TEPO)作为探针分子,研究了高岭石层间羟铝表面的固体酸度。通过甲氧基改性高岭石作为中间产物,实现了 TEPO 在高岭石层间的插层。在固体 C 核磁共振的交叉极化和魔角旋转技术(C CP/MAS NMR)中,反应产物中存在 TEPO 可通过在 21 和 7 ppm 处的两个信号来揭示,这两个信号可归属为 TEPO 中的乙基基团。高岭石层间存在 TEPO 可通过 X 射线衍射图谱显示的层间间距从甲氧基改性高岭石的 0.86nm 扩展到 1.16nm 来证明,表明在高岭石层间形成了 TEPO 单层。此外,通过在傅里叶变换红外光谱中出现另外的 3598cm 的 OH 伸缩带,以及在 55-53ppm 处观察到的窄的固体 P MAS NMR 信号,表明在 TEPO 的物理吸附位置(50ppm)发生了位移,这表明在 TEPO 和高岭石层间表面的羟铝基团之间形成了氢键。这些结果清楚地表明,使用相互作用的 TEPO 单层探测了甲氧基改性高岭石层间羟铝基团的固体酸度。