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寻找微孔强碱性催化剂:高氮掺杂Y型沸石的实验和计算29Si核磁共振谱

Searching for microporous, strongly basic catalysts: experimental and calculated 29Si NMR spectra of heavily nitrogen-doped Y zeolites.

作者信息

Dogan Fulya, Hammond Karl D, Tompsett Geoffrey A, Huo Hua, Conner W Curtis, Auerbach Scott M, Grey Clare P

机构信息

Department of Chemistry, State University of New York at Stony Brook, Stony Brook, New York 11794-3400, USA.

出版信息

J Am Chem Soc. 2009 Aug 12;131(31):11062-79. doi: 10.1021/ja9031133.

Abstract

Nitrogen substituted zeolites with high crystallinity and microporosity are obtained by nitrogen substitution for oxygen in zeolite Y. The substitution reaction is performed under ammonia flow by varying the temperature and reaction time. We examine the effect of aluminum content and charge-compensating cation (H(+)/Na(+)/NH(4)(+)) on the degree of nitrogen substitution and on the preference for substitution of Si-O-Al vs Si-O-Si linkages in the FAU zeolite structure. Silicon-29 magic angle spinning (MAS) nuclear magnetic resonance (NMR) and (1)H/(29)Si cross-polarization MAS NMR spectroscopy have been used to probe the different local environments of the nitrogen-substituted zeolites. Experimental data are compared to simulated NMR spectra obtained by constructing a compendium (>100) of zeolite clusters with and without nitrogen, and by performing quantum calculations of chemical shifts for the NMR-active nuclei in each cluster. The simulated NMR spectra, which assume peak intensities predicted by statistical analysis, agree remarkably well with the experimental data. The results show that high levels of nitrogen substitution can be achieved while maintaining porosity, particularly for NaY and low-aluminum HY materials, without significant loss in crystallinity. Experiments performed at lower temperatures (750-800 degrees C) show a preference for substitution at Si-OH-Al sites. No preference is seen for reactions performed at higher temperatures and longer reaction times (e.g., 850 degrees C and 48 h).

摘要

通过在Y型沸石中用氮取代氧,可获得具有高结晶度和微孔率的氮取代沸石。取代反应在氨气流下通过改变温度和反应时间来进行。我们研究了铝含量和电荷补偿阳离子(H⁺/Na⁺/NH₄⁺)对氮取代程度以及对FAU沸石结构中Si-O-Al与Si-O-Si键取代偏好的影响。硅-29魔角旋转(MAS)核磁共振(NMR)和¹H/²⁹Si交叉极化MAS NMR光谱已被用于探测氮取代沸石的不同局部环境。将实验数据与通过构建包含和不包含氮的沸石簇的汇编(>100个)以及对每个簇中NMR活性核进行化学位移的量子计算而获得的模拟NMR光谱进行比较。假设由统计分析预测的峰强度的模拟NMR光谱与实验数据非常吻合。结果表明,在保持孔隙率的同时可以实现高水平的氮取代,特别是对于NaY和低铝HY材料,结晶度没有显著损失。在较低温度(750 - 800℃)下进行的实验表明,在Si-OH-Al位点有取代偏好。对于在较高温度和较长反应时间(例如850℃和48小时)下进行的反应,没有观察到偏好。

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