(688d) CO2 Separations with KFI Zeolites | AIChE

(688d) CO2 Separations with KFI Zeolites

Authors 

Lorgouilloux, Y. - Presenter, Katholieke Universiteit Leuven
Baron, G. - Presenter, Vrije Universiteit Brussel
Denayer, J. - Presenter, Vrije Universiteit Brussel


T. Remy, S. Van Der Perre, Y. Lorgouilloux, C.E.A.
Kirschhock, J.A. Martens, G.V. Baron, J.F.M. Denayer

CO2 separations with KFI zeolites

Several options exist to separate industrial gas
mixtures: cryogenic distillation, membranes, absorption or selective
adsorption. Selective separation of CO2 plays an important role
within the current issues about global warming and CO2 mitigation.
Typically CO2 is being removed from gas streams, via amine stripping
which is a process with significant drawbacks. Adsorptive or membrane processes
are interesting alternatives for CO2/CH4 and CO2/N2
separations.

The potential of cation-exchanged KFI zeolites
(K-KFI, Li-KFI and Ca-KFI) for these processes has been investigated in this
study. The KFI structure consists of a
three-dimensional network of two larger a-cages (diameter 11.6 ) and six smaller
g-cages (6.6  x10.8 ) per unit cell. The cavities are connected with each other
through eight-membered rings with a diameter of 3.9 .

Adsorption isotherms of CO2, CH4 and N2
were recorded using the gravimetric technique on K-KFI, Li-KFI and Ca-KFI zeolites at 303
K. CO2 adsorption isotherms are of type I, with a capacity amounting
to 4-4.5 mmol/g depending on the cation present. The uptake measurements
indicate much lower affinity for CH4, with a low diffusion through
the small 8-membered windows. Water vapour isotherms measured at 313 K indicate
a large affinity for water, with a capacity of about 8.5 mmol/g.

The dynamic separation potential was assessed via breakthrough
measurement at 308 K for CO2/CH4 and CO2/N2  (P = 1 bar) and different compositions
in order to record the binary isotherm under these conditions. As a result of
the limited diffusion of CH4 and the lower affinity for this component, almost
immediate breakthrough of methane is observed. In these dynamic conditions,
also CO2 uptake is hindered by diffusion, resulting in broadened
breakthrough profiles. The influence of water was investigated by altering the
relative humidity from 0 to 20%.

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