ISOTOPE-EXCHANGE TECHNIQUE FOR MEASUREMENT OF GAS-ADSORPTION EQUILIBRIA AND KINETICS

Citation
Rm. Rynders et al., ISOTOPE-EXCHANGE TECHNIQUE FOR MEASUREMENT OF GAS-ADSORPTION EQUILIBRIA AND KINETICS, AIChE journal, 43(10), 1997, pp. 2456-2470
Citations number
45
Categorie Soggetti
Engineering, Chemical
Journal title
ISSN journal
00011541
Volume
43
Issue
10
Year of publication
1997
Pages
2456 - 2470
Database
ISI
SICI code
0001-1541(1997)43:10<2456:ITFMOG>2.0.ZU;2-9
Abstract
The isotope exchange technique (IET) can be used to simultaneously mea sure multicomponent gas adsorption equilibria and self-diffusivities o f the components in a single isothermal experiment without disturbing the overall adsorbed phase. An experimental protocol for the IET and c orresponding data analysis procedures is described. Isotherms and self -diffusivities for adsorption of N-2 as a pure gas were measured on co mmercial samples of a carbon molecular sieve and a 4-Angstrom zeolite using IET, as well as those of O-2 and N-2 from their binary mixtures. The carbon molecular sieve did not exhibit thermodynamic selectivity for air separation, but had a kinetic selectivity of O-2 over N-2. Mas s-transfer resistances for self-diffusion of N-2 and O-2 on the carbon molecular sieve were controlled by pore mouth restrictions in the car bon, but those for adsorption of N, into the 4-Angstrom zeolite by Fic kian diffusion inside the adsorbent. A linear driving force model desc ribed the uptakes of N-2 and O-2 in the carbon molecular sieve. The Fi ckian diffusion model described the N-2 uptake in the 4-Angstrom zeoli te. Mass-transfer coefficients for both O-2 and N-2 on the carbon mole cular sieve increased linearly with increasing gasphase partial pressu re of these gases, and the pressure of O-2 did nor affect mass-transfe r coefficients for N-2. The self-diffusivity of N-2 in the 4-Angstrom zeolite decreased with increasing adsorbate loading.