石墨材料对水吸附的实验与计算相结合的1H NMR研究

Alan R. Ambrozio , Thierry R. Lopes , Daniel F. Cipriano , Fábio A.L. de Souza , Wanderlã L. Scopel , Jair C.C. Freitas
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引用次数: 1

摘要

采用密度泛函理论(DFT)和1H NMR实验相结合的屏蔽计算方法,研究了类石墨烯层相互作用对吸附在多孔碳材料上的水分子1H NMR谱的影响。实验记录了不同含水碳材料(活性炭和磨粒石墨样品)的1H NMR谱;类石墨烯层中存在的电子电流导致材料中吸附的水产生的1H NMR信号具有较强的屏蔽效应。在高热处理温度下制备的活性炭和研磨时间较短的石墨样品中,这种效应得到了增强,这表明石墨烯类层的结构组织是决定被分析材料吸附的水分子中1H核屏蔽程度的关键特征。由这些1H核感知的屏蔽的DFT计算表明,随着这些层之间的距离(代表孔径)的减小,与石墨层的相互作用增加。然后预测较小尺寸孔隙的1H NMR化学位移持续减小,与实验结果很好地一致。这些计算还表明,由于分子间相互作用和孔隙内的屏蔽变化,水簇中几个1H核的化学位移有很大的分散。这种分散,加上类石墨晶体局部各向异性抗磁化率的影响,是导致水吸附在多孔碳材料上的1H NMR信号变宽的主要原因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Combined experimental and computational 1H NMR study of water adsorption onto graphenic materials

The effects caused by the interaction with graphene-like layers on the 1H NMR spectra of water molecules adsorbed onto porous carbon materials were investigated by a combination of shielding calculations using density functional theory (DFT) and 1H NMR experiments. Experimental 1H NMR spectra were recorded for different water-containing carbon materials (activated carbons and milled graphite samples); the 1H NMR signals due to adsorbed water in these materials showed a strong shielding effect caused by the electron currents present in the graphene-like layers. This effect was enhanced for activated carbons prepared at high heat treatment temperatures and for milled graphite samples with short milling times, evidencing that the structural organization of the graphene-like layers was the key feature defining the magnitude of the shielding on the 1H nuclei in the water molecules adsorbed by the analyzed materials. The DFT calculations of the shielding sensed by these 1H nuclei showed an increased interaction with the graphitic layers as the distance between these layers (representing the pore size) was reduced. A continuous decrease of the 1H NMR chemical shift was then predicted for pores of smaller sizes, in good agreement with the experimental findings. These calculations also showed a large dispersion of chemical shifts for the several 1H nuclei in the water clusters, attributed to intermolecular interactions and to shielding variations within the pores. This dispersion, combined with the effects due to the locally anisotropic diamagnetic susceptibility of graphite-like crystallites, are the main contributions to the broadening of the 1H NMR signals associated with water adsorbed onto porous carbon materials.

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