A team led by the University of Oslo in Norway, in collaboration with the University of Maryland in USA, is investigating how to massively store carbon dioxide (CO2) underground by copying nature. Through a chemical reaction, carbon dioxide can be trapped naturally inside the Earth’s subsurface and stored as solid minerals, called carbonates. The researchers are now carrying out experiments at the ESRF with the aim to accelerate such a process.
Carbon dioxide levels in the atmosphere are higher than ever, mainly due to the burning of fossil fuels and other anthropogenic activities. This, in turn, increases global temperatures and impacts sea levels and the ocean ecosystems.
A potential solution to this crisis would be to trap and store CO2 underground as solid minerals, which is a natural process that occurs over long periods thanks to the reaction of CO2 with rocks in the Earth’s crust and mantle.
Scientists have been studying the injection of CO2 in the subsurface for years. For example, in Sleipner, in the North Sea, millions of tons of carbon dioxide have been injected into a sandstone geological reservoir in the past fifteen years, where CO2 is stored in liquid form. CO2 can also be stored in solid form through mineralization processes, minimising the risk of leakage. Small-scale ongoing projects, such as Carbfix in Iceland, show promising results but questions of efficiency remain.
“The natural process is very effective but too slow, so we wonder whether we could somehow accelerate it so that large quantities of CO2 could be injected underground, without leakage”, explains François Renard, director of the Njord Centre at the University of Oslo and ESRF user.
The natural process
Atmospheric CO2 and water from precipitations naturally react with rocks present at the Earth’s surface – this process is called weathering. Some of these rocks have been produced by volcanic activity (basalts in Iceland) or were exhumed to the Earth’s surface from the mantle (peridotites). When reacting with CO2 and water, they may dissolve partially over geological time scales, liberating magnesium, iron, and calcium ions that can bind with carbon dioxide, in a process called mineral carbonation, which converts CO2 into minerals. The end product is a calcium, iron or magnesium carbonate, which are stable minerals that effectively trap carbon dioxide into a solid form.
Renard and his team are focusing on storing CO2 in basaltic and peridotite rocks, rich in magnesium and calcium, as they are the most efficient environments for it due to their high reactivity. They make up about 70% of the Earth’s surface and are responsible for 1/3 of the trapping of CO2 from the atmosphere through weathering. Estimates suggest that mid-ocean ridges worldwide can store up to 100,000 Gt of CO2. This is more than 2000 times the annual global emissions of CO2.
Once in the basaltic or peridotite rocks, the CO2 quickly reacts with the divalent cations (Ca2+, Mg2+, and Fe2+) from dissolving minerals in the rock and form carbonate minerals. In comparison, it might take several tens of thousands of years for significant amounts of CO2 to mineralize in a sandstone reservoir. After it becomes a mineral, the carbon will not move over geological timescales.
Carbonation at the ESRF
The team is focused on studying how basalts and peridotites can host large quantities of flows of carbon dioxide mixed with water, which will react with the rock to produce carbonate minerals.
Read more on ESRF website