TY - JOUR
T1 - Solving the carbon-dioxide buoyancy challenge
T2 - The design and field testing of a dissolved CO2 injection system
AU - Sigfusson, Bergur
AU - Gislason, Sigurdur R.
AU - Matter, Juerg M.
AU - Stute, Martin
AU - Gunnlaugsson, Einar
AU - Gunnarsson, Ingvi
AU - Aradottir, Edda S.
AU - Sigurdardottir, Holmfridur
AU - Mesfin, Kiflom
AU - Alfredsson, Helgi A.
AU - Wolff-Boenisch, Domenik
AU - Arnarsson, Magnus T.
AU - Oelkers, Eric H.
N1 - Publisher Copyright: © 2015 Elsevier Ltd.
PY - 2015/6/1
Y1 - 2015/6/1
N2 - Long-term security is critical to the success and public acceptance of geologic carbon storage. Much of the security risk associated with geologic carbon storage stems from CO2 buoyancy. Gaseous and supercritical CO2 are less dense than formation waters providing a driving force for it to escape back to the surface via fractures, or abandoned wells. This buoyancy can be eradicated by the dissolution of CO2 into water prior to, or during its injection into the subsurface. Here we demonstrate the dissolution of CO2 into water during its injection into basalts leading directly to its geologic solubility storage. This process was verified via the successful injection of over 175t of CO2 dissolved in 5000t of water into porous rocks located 400-800m below the surface at the Hellisheidi, Iceland CarbFix injection site. Although larger volumes are required for CO2 storage via this method, because the dissolved CO2 is no longer buoyant, the storage formation does not have to be as deep as for supercritical CO2 and the cap rock integrity is less important. This increases the potential storage resource substantially compared to the current estimated storage potential of supercritical CO2.
AB - Long-term security is critical to the success and public acceptance of geologic carbon storage. Much of the security risk associated with geologic carbon storage stems from CO2 buoyancy. Gaseous and supercritical CO2 are less dense than formation waters providing a driving force for it to escape back to the surface via fractures, or abandoned wells. This buoyancy can be eradicated by the dissolution of CO2 into water prior to, or during its injection into the subsurface. Here we demonstrate the dissolution of CO2 into water during its injection into basalts leading directly to its geologic solubility storage. This process was verified via the successful injection of over 175t of CO2 dissolved in 5000t of water into porous rocks located 400-800m below the surface at the Hellisheidi, Iceland CarbFix injection site. Although larger volumes are required for CO2 storage via this method, because the dissolved CO2 is no longer buoyant, the storage formation does not have to be as deep as for supercritical CO2 and the cap rock integrity is less important. This increases the potential storage resource substantially compared to the current estimated storage potential of supercritical CO2.
KW - CO
KW - Carbon injection
KW - Geological storage
KW - Solubility trapping
KW - Storage security
UR - https://www.scopus.com/pages/publications/84925735544
U2 - 10.1016/j.ijggc.2015.02.022
DO - 10.1016/j.ijggc.2015.02.022
M3 - Article
SN - 1750-5836
VL - 37
SP - 213
EP - 219
JO - International Journal of Greenhouse Gas Control
JF - International Journal of Greenhouse Gas Control
ER -