Numerical simulation of the generalized maxwell-stefan model for multicomponent diffusion in microporous sorbents
Numerical simulation of the generalized maxwell-stefan model for multicomponent diffusion in microporous sorbents
复制标题
微孔吸附剂中多组分扩散的广义 Maxwell-Stefan 模型的数值模拟
DOI:
10.1135/cccc19920687
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发表时间:
1992
影响因子:
--
通讯作者:
J. Moulijn
中科院分区:
文献类型:
--
作者:
J. Loos;Peter JT Verheijen;J. Moulijn
The results of simulations of transient multicomponent surface diffusion in a microporous adsorbent are given for various conditions. The generalized Maxwell-Stefan theory was applied to describe the diffusion phenomena. The diffusion equations were solved numerically. The tranqient uptake of a binary mixture and the counterdiffusion of two sorbate species in a slab were simulated. Some striking phenomena of multicomponent diffusion are presented. The relation to the approximate solution obtained by the linearized theory of multicomponent mass transfer is discussed. The simulations are compared with various results found in the literature. Separation and conversion processes taking place on solid sorbents, e.g. zeolites often proceed under non-equilibrium conditions. The understanding and modelling of the diffusion behaviour of mixtures in these materials has practical importance because of its influence on the selectivity of these separations and reactions. Surface diffusion is also of fundamental interest in physical chemistry. In principle, a molecule moving over a surface can be seen as a probe of the interactions with the surface and with the other molecules in its vicinity. Diffusion in micropores (size smaller than 2 nni) is strongly temperature and concentration dependent. The diffusing molecules neker really leave the force field of the surface. In zeolites the intracrystalline pores or openings are of molecular dimensions and the diffusing molecules are likely to hinder each other at high surface occupancies. Multicomponent diffusion behaviour is of special interest. The transient uptake of a mixture of a fast diffusing-weakly adsorbing species and a slow diffusing-strongly adsorbing species in zeolites is typical: the uptake of the fast diffusing species exceeds the equilibrium value in the approach to the equilibrium situation (see e.g. refs*-4). The transient uptake of mixture components in microporous sorbents has been