New Mexico Subsurface Underground Carbon Dioxide Storage Lease and Agreement (with Landowner, Long Form)
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FAQ
Keeping the lid on CO2 stored underground Over time, the CO2 trapped in reservoirs will often begin to chemically react with the minerals of the surrounding rock. The elements bind to create solid, chalky minerals, essentially locking the CO2 into the rock in a process called 'mineral storage'.
WHAT ARE THE DIFFERENT STORAGE TYPES FOR GEOLOGIC CO2 STORAGE? Saline formations. Oil and natural gas reservoirs. Unmineable coal seams. Basalt formations. Organic-rich shales.
The longer the CO2 remains underground, the more securely it is stored. When the CO2 is pumped deep underground, it is initially more buoyant than water and will rise up through the porous rocks until it reaches the top of the formation where it can become trapped by an impermeable layer of cap-rock, such as shale.
Geological storage involves injecting CO2 captured from industrial processes into rock formations deep underground, thereby permanently removing it from the atmosphere. an extensive cap rock or barrier at the top of the formation to contain the CO2 permanently.
Deep saline aquifers and depleted and existing hydrocarbon reservoir rocks are considered major potential CO2 storage media.
Carbon Probably Won't Stay in the Ground Shoving CO2 underground creates a lot of pressure. It can also cause chemical reactions with the minerals underground. As a result, many storage sites have seen the surrounding geology do things scientists were never expecting, jeopardizing the projects.
Storage of CO 2 can be undertaken in a variety of geological settings in sedimentary basins. Within these basins, oil fields, depleted gas fields, deep coal seams and saline formations are all possible storage formations (Figure 2).
