How Water Content Controls Carbon Capture in Mine Tailings: New Research on Calcite vs Crust Formation
bioengineer.orgNew research from Results in Engineering shows that water content, not just chemistry, determines whether carbon dioxide mineralized in mine tailings forms stable calcite or a reactive-blocking crust. The team tested cemented paste backfill from a copper mine across five moisture levels, from dry paste to dilute slurry, all under the same CO2 flow. Dry samples produced amorphous, impurity-locked carbonate that stalled quickly. Water-rich samples grew clean, micron-scale calcite crystals, while total carbonate uptake stayed nearly constant across all conditions. The practical angle for carbon removal projects: the amount of water at the reaction front controls the quality and durability of stored carbon, not necessarily the total quantity captured. Too little water creates a passivation layer that stops the reaction. Too much water slows CO2 diffusion and adds handling costs. The authors suggest an optimal window near the minimum water needed to trigger dissolution and reprecipitation, which also flushes magnesium and other impurities out of the calcite lattice. This matters for anyone sizing mineral carbonation facilities at mine sites. Moisture control could be a low-cost lever to produce cleaner, more stable carbonate products from a waste stream that already exists.
