|
Once concentrated CO2 has been captured, the next step is to store it somewhere. Here are some options.

Storage in geological formations is currently the most promising solution for widespread, long-term sequestration of CO2. Some projects are already under way. In order to reduce greenhouse gases and global warming, stored CO2 must be kept out of the atmosphere for hundreds or thousands of years. Oil and natural-gas reservoirs, deep saltwater aquifers, and coal seams have existed for millions of years with only very gradual changes. There is strong evidence that if properly managed, these formations could provide for long-term storage of CO2.

Many people believe that oil and natural gas are found in big underground caves. This is not the case. Rather, these hydrocarbons are in permeable and porous rocks such as sandstone. These rocks contain microscopic spaces, called pores, which fill with fluids. The fluids may be water, oil, or natural gas. An oil or natural-gas reservoir is more like a sponge than a bottle. Once an oil or natural-gas field has been productive for a period of time, a good portion of the hydrocarbons has been removed. There is space available to store CO2. The porous and permeable rock layer that contains these fluids is covered by an impermeable cap rock—often salt or shale—that does not let them pass through. Normally, oil and natural gas will tend to migrate upward through permeable rock because they are lighter than the water that is also found in such rock formations. The cap rock traps them. Since oil and natural gas have been sequestered in such formations for millions of years, there is good reason to believe that CO2 will remain there as well.
Much of the technology needed to store CO2 in oil fields is already being used for a process known as enhanced oil recovery (EOR). When a reservoir is newly tapped, the oil is typically under pressure and flows freely to the surface. As oil is removed, pressure drops and pumping is needed to recover more. At some point recovery becomes uneconomical and is stopped, or additional techniques are used to extract more oil. One approach is to pump CO2 into the reservoir. This increases pressure so the oil flows more readily. Also, the CO2 dissolves in the oil and causes it to become less viscous and flow more easily. It expands in volume as well, further increasing pressure. CO2 is pumped into the reservoir through an “injection well.” This forces the oil toward a “production well,” where it rises to the surface.

In enhanced oil recovery, CO2 is pumped into the reservoir through an injection well. It mixes with the remaining oil, forming a “miscible zone.” The pressure from the CO2 and expanding oil pushes an oil bank toward the production well, where it rises to the surface. Then the CO2 is separated from the oil and may be added to the stream of CO2 going into the injection well. A side effect of enhanced oil recovery is that the CO2 that was used to force oil out of the formation is now sequestered.
There are many EOR projects using CO2 injection around the world. A good example is the Weyburn field in Canada. |
A side effect of enhanced oil recovery is that CO2 becomes sequestered in the rock formation. If the goal is CO2 storage rather than oil recovery, then depleted or nearly depleted oil fields may be used for sequestration even if they are not good candidates for enhanced oil recovery.
What are potential problems with CO2 sequestration? The big question is whether or not the CO2 will leak out of the reservoir. Leakage would be a problem because it would return the sequestered CO2 to the atmosphere. This would defeat the purpose of the project.
| |
Well Casing 
When an oil well is drilled, the final step in the process is to insert steel pipe in the borehole and to fill the space between the outside of the pipe and the borehole with cement. The pipe, called a casing, is later perforated to allow oil to flow into the pipe and up to the surface. When the well is no longer productive, it may be sealed at the top. |
|
If the leakage was sudden, it could kill people. CO2 is not poisonous, but if it substitutes for available oxygen, people can suffocate. Since CO2 is heavier than air, it can accumulate in low places such as cellars and valleys. There have been natural releases of CO2 that have caused death. One such disaster occurred at Lake Nyos in Cameroon. The lake is in a volcanically active area with carbon dioxide leaking into the waters of the lake from below. On August 21, 1986, there was a sudden release of CO2, which flowed into valleys around the lake and killed 1,800 people in nearby villages. There is no reason to expect CO2 sequestered in an old oil field to suddenly escape, but there are possibilities for slower leakage. Ironically, the wells themselves are a potential problem.
There may be hundreds of such wells in an oil field. If the field is old, the cement around the well casings may have deteriorated. This may provide a pathway for CO2 to escape. There are ways of recementing wells so that they provide a reliable seal for sequestered CO2.
Another possible pathway for CO2 to leak would be cracks in the cap rock. CO2 sequestration is proposed for regions that are geologically stable, where earthquakes are not likely to occur. However, the sequestering of CO2 itself could result in increased pressure under the cap rock that could result in cracks. The solution is to monitor pressure and take care not to exceed the limits of the formation.
There are many underground sealed geological “traps” that have never contained oil or natural gas. Their pores are filled with water. These are called aquifers. The aquifers that are most suitable for CO2 storage are deep underground. They are filled with salt water, so they are unsuitable for supplying or storing fresh water for human use. CO2 would partially dissolve in the water in the aquifer. In some rock types, it might react with minerals to form stable carbonate deposits. This would permanently lock up the CO2. Geological studies would need to be made, as is routinely done for oil and natural-gas reservoirs, to confirm that the aquifer would not leak CO2.
The world’s first CO2 injection program performed for climate-change considerations is offshore Norway in a deep saline aquifer in the North Sea known as the Sleipner field.
Another potential storage medium is in coal deposits that are too deep to be mined. Coal is mostly carbon. It will absorb CO2 and lock it up permanently. Coal deposits usually contain methane. When CO2 is pumped into the coal, it is absorbed in preference to the methane, which is released. As with enhanced oil recovery, useful fuel is produced while sequestering CO2.
A problem with this approach is that coal swells when it absorbs CO2. This can result in reducing the pathways through which the gas flows. The result is more limited storage capacity.
Capture-and-Storage Case Studies
Two CO2 capture-and-storage projects currently under way are in the Sleipner field in the North Sea and in the Weyburn field in Canada. |