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首页> 外文期刊>Langmuir: The ACS Journal of Surfaces and Colloids >Solid-State P-31 Nuclear Magnetic Resonance Study of Interlayer Hydroxide Surfaces of Kaolinite Probed with an Interlayer Triethylphosphine Oxide Monolayer
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Solid-State P-31 Nuclear Magnetic Resonance Study of Interlayer Hydroxide Surfaces of Kaolinite Probed with an Interlayer Triethylphosphine Oxide Monolayer

机译:具有层间三乙基膦氧化物单层探测高岭土层间氢氧化物表面的固态P-31核磁共振研究

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摘要

The solid acidity of the interlayer aluminol surfaces of kaolinite was explored by solid-state P-31 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-13 nuclear magnetic resonance with cross polarization and magic angle spinning techniques (C-13 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(-1) in the Fourier-transform infrared spectrum and narrow solid-state P-31 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.
机译:通过使用三乙基膦氧化物(TEPO)的固态P-31核磁共振探索高岭石的层间铝醇表面的固体酸度,其形成具有均匀取向的单层,如Kaolinite层之间的均匀取向探针分子。使用甲氧基改性的高岭石作为中间体实现高岭石层之间的嵌入。通过21和7ppm的两个信号揭示了反应产物中的TEPO的存在,其在TEPO中可将其分配到TEPO中的乙基,其具有交叉极化和魔法角纺纱技术(C. -13 cp / mas nmr)。通过从0.86nm的基础间距的膨胀,甲氧基改性高岭石的层间距为1.16nm的膨胀,表明了高岭石层之间的存在,如X射线衍射图所示,表明TEPO单层的形成在高岭石层之间。通过在傅立叶变换红外光谱中的3598cm(-1)中的另外的OH拉伸带的外观,也揭示了在高岭土中的P = O基团和铝醇基团之间形成氢键。在55-53ppm观察到窄固态P-31 Mas NMR信号,其从物吸收的TEPO(50ppm)的位置移位。这些结果清楚地表明,使用相互作用的长化长单层探测甲氧基改性高岭石的中间层铝醇基团的固体酸度。

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