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The three main types of geological storage are oil and gas reservoirs, deep saline formations, and un-minable coal beds. CO2 can for instance be physically trapped under a well-sealed rock layer or in the pore spaces within the rock.

Once the carbon dioxide has been transported, it is stored in porous geological formations that are typically located several kilometers under the earth's surface, with pressure and temperatures such that carbon dioxide will be in the liquid or supercritical phase. Suitable storage sites include former gas and oil

One major concern with CCS is that CO2 could leak out of these underground reservoirs into the surrounding air and contribute to climate change, or taint nearby water supplies. Another is the risk of human-made tremors caused by the build-up of pressure underground, known as induced seismicity.

In the case of saline aquifers, as well as structural and mineral storage, the CO2 can dissolve into the salty water in a process called 'dissolution storage'. Here, the dissolved CO2 slowly descends to the bottom of the aquifer. In any given reservoir, each (or all) of these processes work to store CO2 indefinitely.

By studying a natural reservoir in Utah, USA, where CO2 released from deeper formations has been trapped for around 100,000 years, a Cambridge-led research team has now shown that CO2 can be securely stored underground for far longer than the 10,000 years needed to avoid climatic impacts.

Carbon dioxide is first dissolved into a beaker containing an electrolyte liquid, then a small amount of the liquid metal catalyst is added. When an electrical current is applied, the catalyst chemically activates the surface of the mixture, which slowly converts the CO2 into solid flakes of carbon.

Carbon sequestration refers in UFORE to the removal of carbon (in the form of carbon dioxide) from the atmosphere through the process of photosynthesis. carbon storage refers to the amount of carbon bound up in woody material above and below ground.

The most well-developed approach to storing CO2 is injecting it underground into naturally occurring, porous rock formations such as former natural gas or oil reservoirs, coal beds that can't be mined, or saline aquifers.

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