DURABLE SEQUESTRATION OF CO2 BY CARBONATION
When dissolved in water, carbon dioxide forms carbonic acid (H2O + CO2 → H2CO3). The hydrogen cations are readily replaced with metals such as Ca, Mg, or Fe through a process called carbonation to form carbonate minerals such as calcite (CaCO3), magnesite (MgCO3) or siderite (FeCO3). This process has occurred naturally on Earth for billions of years and permanently sequestered large volumes of CO2 from the Earth’s primitive atmosphere. Once carbon is stored as carbonate, it requires no MVA because it is immobile.
As a geologic process, there are of course concerns that carbonation could take too long to be helpful in the current climate crisis. However, researchers in Iceland found that carbonic acid solutions injected into basalt reacted with the rock and formed substantial amounts of carbonate in as little as two years. Other researchers are investigating the use of microbes to potentially speed up carbonation in both surface and downhole environments. In depleted oil fields, carbonates precipitating in subsurface pore space will immobilize CO2 while occluding the pores. The minerals will also block fluid movement and halt fugitive emissions from abandoned wells. Carbonate is a valuable building material, and creating slabs, blocks, and bricks from captured CO2 could provide a saleable product to help improve the economics of DAC. Converting CO2 into solid, stable carbonate minerals offers a simple and elegant solution for carbon dioxide sequestration.