EGU23-17368
https://doi.org/10.5194/egusphere-egu23-17368
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Novel method of ocean alkalinity enhancement using ikaite and other hydratedcarbonate minerals

Laura Bastianini, Kristina Peterson, and Phil Renforth
Laura Bastianini et al.
  • Research Centre for Carbon Solutions, Heriot-Watt University, Edinburgh EH14 4AS, UK

Removing large volumes of CO2 from the atmosphere, as well as rapid and deep emission reductions, may be required to meet the goals of the Paris Agreement. This has catalyzed recent attention on carbon dioxide removal (CDR) approaches that can remove more CO2 from the atmosphere than they emit. The oceans absorb approximately 25% of the CO2 that is emitted to the atmosphere, which causes acidification and adds to the stress experienced by some shell-forming organisms. A relatively inexpensive process for creating a hydrated calcium carbonate, ikaite, could be used to mimic the effect of natural carbonate weathering. This process uses high pressure CO2 (~15 bar) in an aqueous reactor to dissolve crushed limestone within minutes. The calcium rich water is passed to a low-pressure reactor (~0.1 bar) that evolves and recycles gaseous CO2 and forces the precipitation of ikaite over 30 – 80 minutes at temperatures <15°C. Experimental results suggest complete dissolution of ikaite can increase seawater alkalinity and thus potentially ameliorate the effects of ocean acidification. The focus of this study is on material characterisation and geochemical kinetics. In particular, we are using Raman spectroscopy coupled with X-Ray Diffraction for identification of the materials synthetically formed and we are exploring experimentally the precipitation and dissolution kinetics of ikaite and other hydrated carbonate minerals such as amorphous calcium carbonate (ACC). Preliminary results show that ikaite might be a precursor of ACC and synthetic can be stable for days at low temperature (sufficient time to be added to the ocean) and that it dissolves in seawater and stoichiometrically increases alkalinity.

            This technology could be scaled up to have a meaningful impact on climate change, and the costs could be comparable to other CO2 removal approaches. That is possible within the next 20 to 30 years, particularly as the raw materials are abundant.

How to cite: Bastianini, L., Peterson, K., and Renforth, P.: Novel method of ocean alkalinity enhancement using ikaite and other hydratedcarbonate minerals, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-17368, https://doi.org/10.5194/egusphere-egu23-17368, 2023.