Supercritical, liquid, and gas CO2 reactive transport and carbonate formation in portland cement mortar

• Published in: International journal of greenhouse gas control 2022-05, Vol.116 (103632), Article 103632
• Main Authors: Dalton, Laura E., Crandall, Dustin, Pour-Ghaz, M.
• Format: Article
• Language: English
• Subjects: Carbonates; ENGINEERING; Supercritical carbon dioxide; Transport; X-ray CT
• ISSN: 1750-5836; 1878-0148
• DOI: 10.1016/j.ijggc.2022.103632

•The rate of carbonation in cement-based materials depends on degree of saturation.•Carbonates first form in small pores (i.e., gel and capillary pores).•Phases other than Ca(OH)2 contribute to carbonate formation.•Carbonate formation may lead to inhomogeneous microstructure. In this study, we investigate carbonate formation and reactive transport rate in variably saturated portland cement mortars when high concentrations of gas, liquid, or supercritical CO2 flow through their pore network. X-ray computed tomography completed during CO2 flow is used to quantify the microstructural evolution as the mortar carbonates. After in situ tests, higher resolution scans, thermogravimetric analysis, and desorption isotherm analysis are performed to further quantify microstructural changes. We found that at dry conditions supercritical CO2 moves more rapidly through the pore space and precipitates more carbonates than liquid or gas CO2. However, at 50% degree of saturation (DOS) the CO2 state did not affect the rate of transport in that each specimen exposed to a different CO2 state carbonated within the first hour of CO2 exposure. When the pore space is at 50 or 100% DOS, supercritical CO2 did not react with hydration products more rapidly nor did it result in more carbonate formation during exposure compared to gas or liquid CO2. The amount of Ca(OH)2 that contributes to CaCO3 formation is correlated to the DOS. For the mortar composition analyzed, Ca(OH)2 contributes to approximately 40% of the carbonates formed in the 50% DOS specimens and 15% in the 100% DOS specimens. In other words, as the amount of moisture in the pore space increases, phases other than Ca(OH)2 contribute to more than 50% of the total CaCO3 formed.