Dynamics of convective dissolution from a migrating current of carbon dioxide
During geologic storage of carbon dioxide (CO[subscript 2]), trapping of the buoyant CO[subscript 2] after injection is essential in order to minimize the risk of leakage into shallower formations through a fracture or abandoned well. Models for the subsurface behavior of the CO[subscript 2] are use...
Main Authors: | , , |
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Other Authors: | |
Format: | Article |
Language: | en_US |
Published: |
Elsevier
2016
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Online Access: | http://hdl.handle.net/1721.1/101652 https://orcid.org/0000-0002-7370-2332 |