2023 AIChE Annual Meeting
(569f) Kinetics of CO2 Sorption on Binderless Pellets of Different Cationic Forms of Y-Type Zeolites
Authors
The technoeconomic feasibility of using such materials for adsorption-based carbon capture processes is typically assessed by optimizing detailed numerical process models6 for which the key properties that need to be parametrized are the adsorption equilibria and kinetics. While experimental techniques for measuring adsorption equilibrium are widely available, accurate kinetic measurements remain challenging to perform and their outcomes can significantly impact the overall separation performance. Therefore, the aims of this work were three-fold: (1) To characterize the textural (porosity) and CO2 adsorption equilibrium properties, (2) to accurately quantify the kinetics and determine the mass-transfer mechanisms involved in the sorption of CO2, and (3) to relate these mechanisms to the textural and equilibrium properties of three different cationic forms of Y.type zeolites (Si/Al = 2.6), namely hydrogen (H-Y), sodium (Na-Y), and tetramethylammonium (TMA-Y).
To this end, we produced binderless pellets for each cationic form using a manual hydraulic press. We used nitrogen sorption isotherms at 77 K to determine their micro- and mesoporosity and mercury intrusion porosimetry to evaluate the macroporosity. The results from the combined pore size distribution obtained from these measurements indicate the samples are microporous with additional macroporosity introduced during the pelletization process. For the equilibrium sorption measurements, we obtained CO2 sorption isotherms at 288, 298, and 308 K up to a pressure of 101 kPa. The isotherms exhibit an increase in both CO2 capacity and concave non-linearity in the order H-Y < TMA-Y < Na-Y, which suggests an increase in strength of attraction between the zeolite and the CO2 molecules due to increasing basicity of the zeolite framework7. We used the parameters (i.e. skeletal density, porosity, and equilibrium isotherm models) resulting from these characterization steps as model inputs to extract kinetic parameters for CO2 sorption from the subsequent dynamic desorption experiments.
We carried out dynamic sorption experiments on individual zeolite pellets using the experimental technique described in our previous works8,9. The experiments were carried out at 288, 298, and 308 K by saturating the adsorbent to a CO2 partial pressure of up to 95 kPa, followed by desorption at two different flowrates of carrier gas. Helium and argon were used separately as carrier gases to elucidate the impact of macropore resistance to mass transfer within the adsorbent pellets which can be introduced due to the packing of the zeolite crystals during the shaping process10. We then fit the time-resolved desorption profiles obtained from the experiments using a parameter estimation routine with the isotherm models fitted to the volumetric CO2 sorption isotherms as inputs. We used the resulting two-parameter rate expressions obtained for the two cases with different carrier gases, along with the findings from textural characterization to determine the controlling resistance to mass transfer for each zeolite pellet11. Ultimately, the rate expression obtained can be readily adapted in numerical models for adsorption-based processes and used for design and optimization of these separations.
References
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