1994 Volume 1994 Issue 8 Pages 748-751
Breakthrough curves of NO adsorption on various metal ion-exchanged zeolites have been employed to evaluate the intraparticle effective diffusion coefficient (Di). Di was 0.7×10-3 -29×10-3cm2⋅s-1 and was changed with zeolite structures, metal ions exchanged, and adsorption temperature. On MFI zeolite, Di was dependent on the radius of metal ion, and a maximum Di was observed around 0.09 nm of the radius. With CuZSM-5 and Agmordenite, the maximum Di was observed around 250 K, while the Di of Comordenite was not varied with the adsorption temperature.
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