the Basics of Sequestration of CO2Although not directly petroleum related this short essay does address subsurface sequestration of CO2 and it's effects; Comments are welcome!Apart from the techniques were CO2 is kept in it’s place by seals, pressure gradient or buoyancy other ways to store CO2 is by causing it to bond to minerals and become part of the hard subsurface rock. This greatly reduces the risk of CO2 escaping and in some cases will produce useful by products.
There are several techniques for sequestration of CO2 and most research in this field is done by geologists. All techniques rely on either increasing natural weathering processes or by biologically fixating CO2.
Increased weathering can be accomplished by chemical reactions, high-temperature pre-treatments or via biological processes, causing the break up of mineral particles. This creates more reactive surface for CO2 to bond with increasing the overall reaction speed. Geologists will need to assess which chemicals and micro-organisms affect certain minerals without causing damage to an entire system. So micro-organism will need to act very specifically in key locations to break apart a mineral structure, eq. by producing acid. Furthermore, studies must be done on how to get the chemicals and micro-organism into deep rock and where suitable formations are located.
Biological fixation of CO2 relies on certain bacteria that generate small quantities of calcium carbonate, thereby catching free CO2. The potential benefits of this technique is that the microbial organisms increase carbonate reactions and produce chemical factors that could solubilise the carbonate after formation. This causes the carbonate to be removed from an subsurface system in solution while new carbonate can precipitate on the free surface of silicate minerals. Again rock characteristics will need to be known for this technique but biologists will need to select the right organisms for the job.
Another alternative is the sequestration of CO2 in unminable coal seams. CO2 can be pumped into a coal seam and because the CO2 absorbs to the surface of coal faster than Methane (CH4). The storage of CO2 in coal therefore has the potential of generating CH4. In Poland a small plant has been build to experiment with this technique, RECOPOL [1]. Geologists are at work in finding the effects of CO2 on the coal, the paths CO2 and CH4 travel by, the decrease and porosity and permeability due to CO2 injection.
Primarily the later could cause great problems for large scale projects of this kind as this process could cause clogging of the coal seam and thereby lower storage capacity and CH4 production.
Also mid-ocean ridges show potential for storing CO2. Due to their unique geohydrologic activity CO2 can be fixed in many minerals: magnesium, magnesium carbonate, dolomite and calcite. Because heat and pressure are high the reaction kinematics are fast a system were CO2 is pumped into a geohydrologic flow near a mid-ocean ridge has great potential in storing CO2. Unfortunately not a lot of research has been done in this area, leaving a lot of room for future studies.
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