2019
DOI: 10.1007/s11053-019-09604-3
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Impact of Reservoir Permeability, Permeability Anisotropy and Designed Injection Rate on CO2 Gas Behavior in the Shallow Saline Aquifer at the CaMI Field Research Station, Brooks, Alberta

Abstract: This document is the author's post-print version, incorporating any revisions agreed during the peer-review process. Some differences between the published version and this version may remain and you are advised to consult the published version if you wish to cite from it.

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Cited by 11 publications
(3 citation statements)
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“…As can be seen, the permeability anisotropy ( ) of sand has no effects on the vertical migration of CO plume ( and CM / H ), which is yet highly controlled by the correlation length ( ) and density ( NTG ) of capillary barriers. Although buoyancy-driven migration of CO in homogeneous reservoir models has been shown to be highly influenced by the permeability anisotropy in previous studies 39 , our results delineate that the lateral extension and density of capillary barriers have more influential impact on retarding the upward migration of CO . According to the tornado chart, it was observed that has minimal impacts on the configuration of CO plume (i.e., , , and CM / H ) and pressure buidlup (i.e., , and ).…”
Section: Resultscontrasting
confidence: 42%
“…As can be seen, the permeability anisotropy ( ) of sand has no effects on the vertical migration of CO plume ( and CM / H ), which is yet highly controlled by the correlation length ( ) and density ( NTG ) of capillary barriers. Although buoyancy-driven migration of CO in homogeneous reservoir models has been shown to be highly influenced by the permeability anisotropy in previous studies 39 , our results delineate that the lateral extension and density of capillary barriers have more influential impact on retarding the upward migration of CO . According to the tornado chart, it was observed that has minimal impacts on the configuration of CO plume (i.e., , , and CM / H ) and pressure buidlup (i.e., , and ).…”
Section: Resultscontrasting
confidence: 42%
“…According to statistics, large-scale site projects will enter the explosive period after 2020 [3]. Most of the current research on the geological storage of CO 2 in deep saline aquifers focuses on the exploration of CO 2 migration law, storage mechanisms, and risk assessment of leakage [10][11][12][13][14]. e monitoring data from the site project show that the salt precipitation near the well is part of the low permeability zone, which causes the accumulation of injection pressure and reduces the CO 2 injectivity [15].…”
Section: Introductionmentioning
confidence: 99%
“…Moreover, the fluid composition within and above the storage formation needs to be determined where the characterisation of noble gas distributions (He, Ne, Ar, Kr, Xe) may be an additional asset. 71 Besides the large scale commercial scale, various monitoring methods have also been used for smaller CO 2 pilot injection studies around the world, such as the CaMI Field Research Station project in Alberta (Canada), 72 the Otway project in Victoria (Australia), [73][74][75] the German Ketzin project, 76 the Frio Brine Pilot project in Texas (USA) 77 and in the K-COSEM storage site (South Korea). 78 After the injection phase ceases, a portion of CO 2 will be securely stored as a result of various processes including dissolution, residual and mineral trapping.…”
mentioning
confidence: 99%