Abstract
The production of ikaite, a metastable calcium carbonate hydrate, offers a promising pathway for atmospheric CO2 removal through ocean alkalinity enhancement. This study explores the feasibility of ikaite production through a three-step process, involving calcite (CaCO3) dissolution under elevated CO2 pressure, CO2 degassing from the calcium carbonate rich solution, and subsequent crystallisation. Here, a mathematical model was developed and validated against experimental data, and the effect of key operational parameters was examined. The calcite loading/dosage, particle size and CO2 pressure for dissolution, seed loading and particle size for crystallisation, and degassing pressure as critical factors have significant impact on process efficiencies. Under optimal conditions, involving CO2 pressures of 2 bar for dissolution, 0.01 bar for degassing, and 0.001 bar for crystallisation, with seed loading of 5 kg/m³ and seed particle sizes of 3 μm, the process achieved steady state ikaite production of 1.64 kg/m³ from a calcite feed of 0.83 kg/m³. This investigation demonstrates the technical viability of ikaite production through CO2 pressure swing and informs its future development as a potential contributor to climate change mitigation.
| Original language | English |
|---|---|
| Pages (from-to) | 399-410 |
| Number of pages | 12 |
| Journal | Chemical Engineering Research and Design |
| Volume | 225 |
| Early online date | 13 Dec 2025 |
| DOIs | |
| Publication status | Published - Jan 2026 |
Keywords
- Calcite dissolution
- Crystallisation
- Degassing
- Direct atmospheric CO capture
- Ikaite
- Ocean alkalinity enhancement
ASJC Scopus subject areas
- General Chemistry
- General Chemical Engineering