Is there a coupling between rotational and translational motion of methane in silicalite-1 and AlPO4-5?

被引:3
作者
Fritzsche, S
Osotchan, T
Schüring, A
Hannongbua, S
Kärger, J
机构
[1] Univ Leipzig, Fac Phys & Geosci, Inst Theoret Phys, D-04109 Leipzig, Germany
[2] Mahidol Univ, Fac Sci, Dept Phys, Bangkok 10700, Thailand
[3] Chulalongkorn Univ, Fac Sci, Dept Chem, Bangkok, Thailand
[4] Univ Leipzig, Fac Phys & Geosci, Inst Expt Phys 1, D-04109 Leipzig, Germany
关键词
D O I
10.1016/j.cplett.2005.06.067
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Methane, although often treated approximately as a spherical Lennard-Jones particle, has merely a tetrahedral shape. While moving in zeolites, the interaction of the molecule with the walls will cause a fluctuating angular momentum of this guest molecule. In zeolites containing channels, as it is the case with silicalite-1 or AlPO4-5, adsorbed guest molecules move along channels and change to other channel types at channel intersections. The question arises whether or not the corrugation of the zeolite channels leads to a coupling of rotational and translational motions. It shall be shown, however, that for methane in silicalite-1 and AlPO4-5 the two kinds of motion are uncoupled. The relaxation behavior of translational and angular momentum shows different patterns, although in both cases the relaxation time is on the same order of magnitude. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:423 / 428
页数:6
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