Ralf Heidler, Geert O.A. Janssens, Wilfried J. Mortier, Robert A. Schoonheydt
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引用次数: 9
Abstract
The interaction of pyrrole with alkali cation exchanged FAU-type zeolites is studied using a combination of the electronegativity equalization method (EEM) and the Monte Carlo technique. Pyrrole adsorbs at SII cations, the NH-group pointing to the most basic oxygen O4. The NH-bond polarization and the pyrrole framework interaction energy reflect the fundamental and well established trends of the intrinsic framework basicity: an increasing basicity with an increasing Al-content and, at a given Si:Al-ratio, an increasing basicity with increasing size of the exchangeable cations. In contrast to a recent interpretation of the IR-spectra of the NH-stretching vibration of pyrrole (D. Murphy, P. Massiani, R. Franck, D. Barthomeuf, J. Phys. Chem., 100 (1996) 6731; D. Murphy, P. Massiani, R. Franck, D. Barthomeuf, Stud. Surf. Sci. Catal., 105 (1997) 639). our Monte Carlo calculations show that there is only one adsorption site for pyrrole in the FAU-structure at low loadings. An alternative explanation for the observed heterogeneity of the IR-spectra of pyrrole is discussed on the basis of our calculations: the orientation of the pyrrole molecule with respect to the six-ring depends on the Si:Al-ratio of the tetrahedra forming the six-rings.
采用电负性平衡法(EEM)和蒙特卡罗技术相结合的方法研究了吡咯与碱性阳离子交换的fu型沸石的相互作用。吡咯吸附在SII阳离子上,nh基团指向最碱性的氧O4。nh键极化和吡咯骨架相互作用能反映了固有骨架碱度的基本趋势:碱度随al含量的增加而增加,在一定的Si: al比下,碱度随交换阳离子尺寸的增加而增加。与最近对pyrrole的nh拉伸振动的红外光谱的解释(D. Murphy, P. Massiani, R. Franck, D. Barthomeuf, J. Phys。化学。, 100 (1996) 6731;D. Murphy, P. Massiani, R. Franck, D. Barthomeuf, Stud。冲浪。科学。Catal。, 105(1997) 639)。我们的蒙特卡罗计算表明,在低负荷下,fau结构中只有一个吸附位点。对观察到的吡咯红外光谱不均匀性的另一种解释在我们的计算的基础上进行了讨论:吡咯分子相对于六环的取向取决于形成六环的四面体的Si: al比。