Kinetic model for moisture-controlled CO2 sorption
Yuta Kaneko1, Klaus S Lackner1
1School of Sustainable Engineering & The Built Environment, Arizona State University, Tempe, AZ 85287, USA. Klaus.Lackner@asu.edu.
A new model explains carbon dioxide (CO2) sorption kinetics in materials. It shows that slow reaction or diffusion rates limit CO2 capture, a key challenge for practical applications.
Area of Science:
- Materials Science
- Chemical Engineering
- Physical Chemistry
Background:
- Understanding sorption/desorption kinetics is crucial for effective moisture-controlled CO2 capture.
- Existing models may not fully capture the complex interplay of reaction and diffusion in sorbent materials.
Purpose of the Study:
- To develop and validate an analytic model for moisture-controlled CO2 sorption kinetics.
- To differentiate between surface reaction kinetics and interior diffusive transport as rate-limiting steps.
- To establish a generalized effective diffusivity (DM) that unifies these kinetic contributions.
Main Methods:
- Development of an analytic kinetic model for CO2 sorption.
- Analysis of two limiting cases: surface reaction dominance and interior diffusion dominance.
- Mathematical formulation combining carbon species and simplifying diffusion equations.
- Experimental validation using transient CO2 flux measurements in a commercial anion exchange membrane.
Main Results:
- The model accurately describes reaction kinetics as a combination of 1st and 2nd order processes.
- Interior transport kinetics are governed by non-linear diffusion equations.
- A generalized effective diffusivity (DM) was introduced, combining surface reaction and diffusion.
- Experimental data fit the 1st order model, with DM values indicating slow kinetics (6.6-7.1 × 10^-14 m²/s at 35°C).
Conclusions:
- The developed model provides a unified framework for understanding CO2 sorption kinetics.
- Slow kinetics, particularly diffusion and reaction rates, represent a significant barrier to practical CO2 capture applications.
- The model's predictions of CO2 pumping flux in active membranes highlight potential for CO2 transport against concentration gradients, driven by water flux.
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