Global CO2 emissions can only be reduced if policies are widely and intensively used. These policies include major technological breakthroughs, increasing the share of non-fossil forms of energy production, and carbon capture and storage (IEA, 2004). For the second, carbon dioxide CO2 storage must be collected from significant, stationary sources, shipped to a place out of the way, and sealed up for extended periods (centuries to millennia).
How many ways are there to store CO2?
The three main places where CO2 can be stored are the oceans, deep geological media, and surface mineral carbonation (IPCC, 2005). Mineral carbonation is the most expensive and significantly impacts the environment of the three ways to store CO2. CO2 storage in the ocean is an untested method that will change the local chemical environment, put some ocean species at risk, and affect ecosystems (IPCC, 2005). In contrast, carbon dioxide (CO2) capture and geological storage (CCGS) is a technology that: 1) can used right away thanks to lessons learned mainly in the oil and gas industry, deep waste disposal, and groundwater protection; 2) has a large capacity, even if it is not evenly spread around the world; and 3) has retention times of hundreds of thousands to millions of years (IPCC, 2005).
Taking into account what was going on at the time
The near-well environment has been used to study how well the CO2 storage system works in infection. From this setting, we can pick out the following themes:
There are only a few recent articles on this topic, and during the injection stage, SC-CO2 will dominate the environment close to the well. Because of this, it is essential to learn more about how pure SC-CO2 or H2O dissolved in SC-CO2 might interact with cement or host rock.
Acknowledgments
Statoil Hydro paid for this research in Trondheim, Norway. It was done at the Research Centre there.
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