Modeling tracer counter-permeation through anisotropic zeolite membranes: from mean field theory to single-file diffusion

被引:42
作者
Nelson, PH
Auerbach, SM [1 ]
机构
[1] Univ Massachusetts, Dept Chem, Amherst, MA 01003 USA
[2] Univ Massachusetts, Dept Chem Engn, Amherst, MA 01003 USA
基金
美国国家科学基金会;
关键词
counter-permeation; anisotropic zeolite membranes; mean field theory; single-file diffusion; kinetic Monte-Carlo;
D O I
10.1016/S1385-8947(99)00052-2
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Diffusion in anisotropic host-guest systems exhibiting a Langmuir-type adsorption isotherm is investigated using a tracer counter-permeation (TCP) simulation technique. In the TCP simulations, tagged and untagged molecules counter-diffuse through zeolite membranes of finite thickness. Fick's law is used to measure the diffusivities at high equilibrium occupancy, as a function of the membrane thickness, L, and anisotropy, eta. For values of eta much greater than 1, sorbate motion in the plane of the membrane is very rapid and washes out any correlations in the transmembrane direction, so that diffusion is well modeled by mean field theory. As eta is reduced, correlations between the motion of nearby molecules decrease the counter-diffusivity, but diffusion remains "normal" in the sense that the diffusivity is independent of thickness for sufficiently thick membranes. For membranes with eta=0, a single-file mode of diffusion occurs for all membrane thicknesses, and the counter-diffusivity becomes inversely proportional to thickness for thick membranes. Membranes with eta much less than 1 exhibit a single-file diffusion mode for thin membranes that changes over to a normal diffusion mode as the thickness is increased. We have also determined that the rate of transmembrane permeation is controlled by the ratio of the diffusion time to the sorption time, which is given by k(d)L/D where D is the counter-diffusivity and kd is the desorption coefficient. When permeation is diffusion limited, an assumption of local thermodynamic equilibrium is appropriate at the edges, and the permeability coefficient is independent of membrane thickness. On the other hand, when permeation is sorption limited, the edge concentrations are not determined by the isotherm, and the permeability coefficient depends on thickness so that the permeance is itself independent of membrane thickness. (C) 1999 Elsevier Science S.A. All rights reserved.
引用
收藏
页码:43 / 56
页数:14
相关论文
共 44 条
[1]  
ADAMSON AW, 1990, PHYSICAL CHEM SURFAC
[2]   TRANSPORT-THEORY FOR CATIONIC ZEOLITES - DIFFUSION OF BENZENE IN NA-Y [J].
AUERBACH, SM ;
HENSON, NJ ;
CHEETHAM, AK ;
METIU, HI .
JOURNAL OF PHYSICAL CHEMISTRY, 1995, 99 (26) :10600-10608
[3]   Permeation of aromatic hydrocarbon vapors through silicalite-zeolite membranes [J].
Baertsch, CD ;
Funke, HH ;
Falconer, JL ;
Noble, RD .
JOURNAL OF PHYSICAL CHEMISTRY, 1996, 100 (18) :7676-7679
[4]   Permeation characteristics of a metal-supported silicalite-1 zeolite membrane [J].
Bakker, WJW ;
Kapteijn, F ;
Poppe, J ;
Moulijn, JA .
JOURNAL OF MEMBRANE SCIENCE, 1996, 117 (1-2) :57-78
[5]   Applications of Monte Carlo methods to statistical physics [J].
Binder, K .
REPORTS ON PROGRESS IN PHYSICS, 1997, 60 (05) :487-559
[6]   Transport diffusion and self-diffusion of benzene in NaX and CaX zeolite crystals studied by ZLC and tracer ZLC methods [J].
Brandani, S ;
Xu, Z ;
Ruthven, D .
MICROPOROUS MATERIALS, 1996, 7 (06) :323-331
[7]   Permeation of single gases in thin zeolite MFI membranes [J].
Burggraaf, AJ ;
Vroon, ZAEP ;
Keizer, K ;
Verweij, H .
JOURNAL OF MEMBRANE SCIENCE, 1998, 144 (1-2) :77-86
[8]  
Chen N. Y., 1994, MOL TRANSPORT REACTI
[9]  
CRANK J, 1978, MATH DIFFUSION
[10]   Structure and dynamics of zeolites investigated by molecular dynamics [J].
Demontis, P ;
Suffritti, GB .
CHEMICAL REVIEWS, 1997, 97 (08) :2845-2878