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Storage in deep geological formations is also known as 'geo-sequestration'. In this technique, CO2 is converted into a high pressure, liquid-like form known as 'supercritical CO2'. Supercritical CO2 behaves like a runny liquid, a bit like WD40, and is injected directly into sedimentary rocks.
CO2 can be captured using a liquid solvent or other separation methods. In an absorption-based approach, once absorbed by the solvent, the CO2 is released by heating to form a high purity CO2 stream.
CO2 is transported, stored and handled in liquid form, either at ambient temperature (in cylinders or non-insulated storage tanks at a pressure of 45-65 bar) or refrigerated (in insulated tankers and storage tanks) at temperatures between -35 °C and -15 °C and pressures of 12 to 25 bar.
Carbon sequestration is the process of capturing and storing atmospheric carbon dioxide. It is one method of reducing the amount of carbon dioxide in the atmosphere with the goal of reducing global climate change. The USGS is conducting assessments on two major types of carbon sequestration: geologic and biologic.
How can CO2 be stored underground? Compressed CO2 can be injected into porous rock formations below the Earth's surface using many of the same methods already used by the oil and gas industry. The three main types of geological storage are oil and gas reservoirs, deep saline formations, and un-minable coal beds.
The main methods for capturing CO2 are: post-combustion; pre-combustion; and oxy-fuel combustion? . Post-combustion technology separates CO2 from the flue gas, by using a chemical solvent for instance, after the fuel is burnt.