(320b) Sub-Ambient CO2 Flux Measurements and Modeling Using Amino Acid Solvents | AIChE

(320b) Sub-Ambient CO2 Flux Measurements and Modeling Using Amino Acid Solvents

Authors 

Kasturi, A. - Presenter, Georgia Tech
Gabitto, J., PVAMU
Seo, J., Oak Ridge National Lab - Oak Ridge, TN
Sholl, D., Oak Ridge National Laboratory
Custelcean, R., Oak Ridge National Laboratory
Yiacoumi, S., Georgia Institute of Technology
Tsouris, C., Oak Ridge National Laboratory
One of the main advantages of direct air capture (DAC) over point-source capture is the flexibility in plant siting anywhere around the world. In this study, aqueous amino acid solutions, specifically those of potassium sarcosinate (K-SAR), were used to capture CO2 from air. Because plant siting involves areas where the temperature is occasionally below the freezing point of water, termed here as sub-ambient temperatures, there was a need to investigate the physical properties and performance of the solvent at such temperatures. The need for anti-freezing additives, such as triethylene glycol, was determined by comparing the freezing point, CO₂ flux, and mass-transfer coefficient of K-SAR alone and K-SAR with glycol. The solvent viscosity and density were also measured for different temperatures and solvent concentrations. A reactor was set up to reliably measure the CO₂ flux at different temperatures by ensuring a constant, measurable surface area and effective temperature control. The CO₂ flux was measured between -20 and 45 °C for 1 and 3 M K-SAR, and the results were compared to theoretical estimations based on the solvent’s physical properties and operating conditions. For 1 M K-SAR at 25°C, the flux was experimentally determined at 5.9 × 10-5 mol m-2s-1, while the theoretical flux was estimated at 5.4 × 10-5 mol m-2s-1, showing good agreement between experimental data and theoretical results. The results of this study provide the fundamental basis for developing an effective carbon capture technology with amino acid solvents that can be used to effectively capture atmospheric CO₂ at scale in different climates.