Abstract

Sol-gel modification of mesoporous alumina membranes is a very successful technique to improve gas separation performance. Due to the formed microporous top layer, the membranes show activated transport and molecular sieve-like separation factors. This paper concentrates on the mechanism of activated transport (also often referred to as micropore diffusion or molecular sieving). Based on a theoretical analysis, results from permeation and separation experiments with H 2, CO 2, O 2, N 2, CH 4 and iso-C 4H 10 on microporous sol-gel modified supported ceramic membranes are integrated with sorption data. Gas permeation through these membranes is activated, and for defect-free membranes the activation energies are in the order of 13–15 kJ.mol −1 and 5–6 kJ.mol −1 for H 2 and CO 2 respectively. Representative permeation values are in the order of 6×10 −7 mol.m −2.s −1.Pa −1 and 20×10 −7 mol.m −2.s −1.Pa −1 for H 2 at 25°C and 200°C, respectively. Separation factors for H 2 CH 4 and H 2 iso-butane are in the order of 30 and 200 at 200°C, respectively, for high quality membranes. Processes which strongly determine gas transport through microporous materials are sorption and micropore diffusion. Consequently, the activation energy for permeation is an apparent one, consisting of a contribution from the isosteric heat of adsorption and the activation energy for micropore diffusion. An extensive model is given to analyse these contributions. For the experimental conditions studied, the analysis of the gas transport mechanism shows that interface processes are not rate determining. The calculated activation energies for micropore diffusion are 21 kJ.mol −1 and 32 kJ.mol −1 for H 2 and CO 2, respectively. Comparison with zeolite diffusion data shows that these activation energies are higher than for zeolite 4A ( d pore=4Å), indicating that the average pore size of the sol-gel derived membranes is probably smaller.

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