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Updated: Jun 3, 2025

Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography
Published on: February 21, 2017
Moisture-driven carbonation kinetics for ultrafast CO2 mineralization.
Yining Gao1,2, Yong Tao1,2, Gen Li1,2
1Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Hong Kong 999077, China.
Water content critically influences CO2 mineralization efficiency. Optimal moisture levels enhance CO2 uptake via capillary condensation, while excessive water shifts reactions to mineral surfaces for ultrafast carbonation.
Area of Science:
- Earth and Environmental Sciences
- Materials Science
- Chemical Engineering
Background:
- CO2 mineralization is key for carbon sequestration and mitigating global warming.
- Water's role in CO2 mineralization is vital but not fully understood.
- Calcium-bearing minerals are crucial for this process.
Purpose of the Study:
- To elucidate the mechanisms of moisture-driven carbonation kinetics in calcium-bearing minerals.
- To understand how water content affects CO2 uptake and reaction pathways.
- To optimize CO2 mineralization strategies for decarbonization.
Main Methods:
- Combined experimental and atomistic simulation approach.
- Utilized a self-designed carbonation reactor with an ultrasonic atomizer for precise water control.
- Employed Grand Canonical Monte Carlo and metadynamics simulations.
Main Results:
- Maximum CO2 uptake occurs at optimal moisture (0.1-0.2 g/g) due to capillary condensation enhancing CO2 adsorption.
- Higher moisture content hinders CO2 diffusion into mineral pores.
- Very high moisture levels shift carbonation to the mineral surface, driven by dissolution.
Conclusions:
- Water plays a multifaceted role in mineral carbonation kinetics.
- Optimal moisture levels enable ultrafast adsorption-driven carbonation.
- Surface dissolution-driven carbonation occurs at high moisture levels, offering another ultrafast pathway.
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