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Summary:

Switzerland’s path to achieving net zero emissions by 2050 requires not only reducing CO2 output but also finding ways to store unavoidable emissions permanently. Researchers at ETH Zurich have conducted the first nationwide study assessing whether underground CO2 storage through in-situ mineralization is feasible in Switzerland. The study1 was published in the Swiss Journal of Geosciences.

Their research identifies key geological requirements for CO2 storage, including the presence of calcium-, magnesium-, and iron-rich rocks such as basalt and peridotite. While suitable rock formations exist in regions like the Zermatt-Saas zone and the Arosa zone, significant technical challenges arise due to Switzerland’s complex geology. The heavily folded rock layers, limited porosity, and past natural mineralization make large-scale storage difficult. Additionally, the immense water requirements for in-situ mineralization and societal concerns over environmental impacts add further complications.

Given these obstacles, researchers suggest alternative CO2 storage solutions, such as injection into deep saline aquifers. A separate study2 explored this method, finding promising results in Zurich’s subsurface. Projects like DemoUpCARMA, which transports Swiss CO2 to Iceland for underground storage, also demonstrate viable approaches. The findings highlight the need for continued exploration of practical CO2 sequestration methods.

Image: CO2 is dissolved in water and pumped 350 metres underground where it is stored permanently (s. zero emissions)
CO2 is dissolved in water and pumped 350 metres underground where it is stored permanently. Credit: Image adapted from Campbell, J. S. et. al. (2022) | DOI: 10.3389/fclim.2022.879133 | Frontiers in Climate

Storing CO2 underground in Switzerland

For Switzerland to achieve its net zero climate target, not only must it reduce its CO2 emissions, it must also find a way to store the greenhouse gas permanently. Researchers at ETH Zurich have investigated whether, and under what conditions, CO2 could be stored underground in Switzerland.

To achieve its net zero climate target by 2050, Switzerland must press forward with the energy transition – whether in electricity, heating or mobility. The permanent storage of CO2 is another important challenge. In particular, Switzerland must find a permanent solution for emissions that are difficult or impossible to avoid, such as those produced by waste incinerators.

Researchers at ETH Zurich have conducted the first ever study1 to investigate whether CO2 can be permanently stored underground in Switzerland in the form of carbonate rock, and what criteria would need to be met for this to happen. They present their findings in a study that was recently published in the Swiss Journal of Geosciences.

How rock can be used to store CO2

To begin with, ETH researchers want to find out whether there are any zones in Switzerland where CO2 can be permanently stored in the rocky underground. Permanent storage of CO2 underground requires that the rock be rich in calcium, magnesium and iron, while at the same time containing as little silicon dioxide as possible. Potential candidates include basalt, peridotite and serpentinite.

For ideal storage capacity, the rock in the subsurface must also be of a certain volume and located at a depth of at least 350 metres in order for the pressure to be high enough to keep the CO2 in the water. An optimal temperature of between 90 and 185 degrees Celsius, plus the age, alteration condition, porosity and permeability of the rock all play an important role as well.

“These are some of the criteria that have to be met before an area can even be considered as a reservoir,” says Adrian Martin, whose master’s thesis forms the basis for this study.

To store the CO2 underground, it is dissolved in water and pumped underground as carbonic acid. The water used is initially acidic, i.e. it has a low pH value. It penetrates and dissolves the porous rock, releasing iron, magnesium and calcium ions. This causes the pH of the injected water to increase, and at a certain point a reverse reaction occurs: the CO2 combines with calcium and magnesium to form white carbonate rock, e.g. limestone. “This process is called in-situ mineralisation,” says Martin.

Potential recognised, but feasibility questionable

Thanushika Gunatilake, a former postdoc with Stefan Wiemer, a professor in the Department of Earth and Planetary Sciences and head of the Swiss Seismological Service, also worked on the study. She is now an assistant professor at the Vrije Universiteit Amsterdam and emphasises that this nationwide search for suitable rock types is the first of its kind in Switzerland.

Martin has not only analysed numerous scientific studies; he has also examined geological maps area by area and identified those locations that meet the criteria and could therefore be suitable for in-situ CO2 mineralisation. These areas include the Zermatt-Saas zone and the Tsaté nappe in Valais, as well as the Arosa zone in Graubünden.

The areas identified by Martin are not currently suitable for permanent underground storage of CO2. “Although we do have suitable rock types in Switzerland, we face major technical challenges,” says Martin. The geological structure is very complex due to the heavily folded rock strata and tectonic faults. At the Tsaté nappe in Valais, the layers in suitable rocks in areas such as the one between Gouille and Mont des Ritses can have a thickness of over 500 metres, while at Les Diablons thickness is only around 150 metres.

Other factors compound the issue: the rocks in the Zermatt-Saas zone, for example, were transformed in the past by high pressures and temperatures and now already contain many carbonate minerals, indicating that natural CO2 absorption (i.e. previous mineralisation) has already occurred. Furthermore, the Zermatt rocks are packed very close together underground and contain few open cavities or cracks, into which the CO2 could penetrate.

Additionally, the volume of water required for in-situ mineralisation is enormous – close to 25 tonnes of water would be needed to store one tonne of CO2. Martin adds: “On top of that, there are economic and societal hurdles: Who will bear the costs? How do you overcome the scepticism of local residents who are concerned about water pollution, for example? What would be the legal regulations?”

Alternative methods of CO2 storage

The researchers conclude that permanent storage of CO2 through in-situ mineralisation in Switzerland is not feasible in the short term and appears unsuitable in the long term. They therefore recommend investigating alternative storage methods. Gunatilake has recently published another study2, this time focussing on storing CO2 in saline aquifers.

Image: Lithological stratigraphy of Triemli, Switzerland and Geological Profile from NW to SE crossing city Zurich
a) Lithological stratigraphy of Triemli, Switzerland and b) Geological Profile from NW to SE crossing city Zurich. Modified after (Sommaruga et al., 2012). The target formation for CO2 injection is the Upper Muschelkalk at 2250m depth. c) A depiction of Switzerland featuring wells penetrating the Upper Muschelkalk (indicated by blue circles), with emphasis on the study area outlined by a red box. Credit: Gunatilake T et al. (2025) | DOI: DOI: 10.1016/j.ccst.2024.100360 | Carbon Capture Science & Technology

For this project, researchers used numerical simulations to analyse data from the area around Triemli in Zurich. They succeeded in injecting CO2 into the geological unit, the lower Muschelkalk, to a depth of over 2,000 metres without water. “This method of CO2 storage is promising,” emphasises Gunatilake.

There are also projects that successfully demonstrate permanent storage of CO2 underground. “One example is the DemoUpCARMA project, where CO2 from Switzerland was transported to Iceland where it is now stored underground in the form of carbonate rock,” says Martin.

It is important to raise public awareness of the issue and to dispel myths and rumours. “Many people think we’re creating a bubble underground and that it could even explode at some point,” explains Martin. “But the risk to the public from underground CO2 storage is minimal and the methods are scientifically well proven.”

Journal References:
1
. Martin A, Becattini V, Marieni C, Kolbeinsdóttir S, Mazzotti M, Gunatilake T, ‘Potential and challenges of underground CO2 storage via in-situ mineralization in Switzerland’, Swiss Journal of Geosciences 118, 1 (2025). DOI: 10.1186/s00015-024-00473-4

2. Gunatilake T, Zappone A, Zhang Y, Zbinden D, Mazzotti M, Wiemer S., ‘Quantitative modeling and assessment of CO2 storage in saline aquifers: A case study in Switzerland’, Carbon Capture Science & Technology 14, 100360 (2025). DOI: 10.1016/j.ccst.2024.100360

Article Source:
Press Release/Material by Deborah Kyburz | ETH Zurich
Featured image: Suitable rock types for storing CO2 can be found all around the iconic Matterhorn. Credit: Pixabay | Pexels

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