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Interface pinning of CO₂ gravity currents

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dc.contributor.advisor Ruben Juanes. en_US
dc.contributor.author Zhao, Benzhong en_US
dc.contributor.other Massachusetts Institute of Technology. Dept. of Civil and Environmental Engineering. en_US
dc.date.accessioned 2012-10-26T19:02:03Z
dc.date.available 2012-10-26T19:02:03Z
dc.date.copyright 2012 en_US
dc.date.issued 2012 en_US
dc.identifier.uri http://hdl.handle.net/1721.1/74498
dc.description Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2012. en_US
dc.description Cataloged from PDF version of thesis. en_US
dc.description Includes bibliographical references (p. 41-43). en_US
dc.description.abstract Carbon capture and storage (CCS) is widely regarded as a promising tool for reducing global atmospheric carbon dioxide (CO₂) emissions, while allowing continued use of fossil fuels in the 21st century. In CCS, CO₂ is captured at point sources such as coal power plants and injected deep underground in geological formations like saline aquifers for long-term storage. Given the large scale of CCS required to significantly reduce anthropogenic CO₂ emissions into the atmosphere, it is critical to understand the migration of CO₂ after injection, so that we can design effective injection strategies to minimize the leakage risks of CO₂ . Recent studies have demonstrated that simple models that incorporate the essential physics involved in CO₂ storage are able to make significant contributions in addressing important questions such as storage capacity and leakage risks in large scale CO₂ sequestration projects. Here, we study the impact of capillarity on the migration of CO₂ plume through exchange flow experiments of immiscible fluids. We show that capillarity leads to the development of striking features not present in miscible exchange flows, including a vertical pinned interface and sharp corners. We show that interface pinning is caused by capillary pressure hysteresis, and the amount of pinning scales with the relative strength of capillarity relative to gravity, as measured by the inverse of the Bond number. We demonstrate that capillary pressure hysteresis in porous media is caused by the fundamental difference in pore-scale invasion patterns between drainage and imbibition. In addition, we propose a sharp interface gravity current model that incorporates capillary pressure hysteresis and quantitatively explains the experimental observations, including the x ~ t1/2 spreading behavior at intermediate times and the fact that capillarity stops the spreading of a finite release current. These results suggest that interface pinning has important implications in the migration of CO₂ plume in deep saline aquifers. en_US
dc.description.statementofresponsibility by Benzhong Zhao. en_US
dc.format.extent 43 p. en_US
dc.language.iso eng en_US
dc.publisher Massachusetts Institute of Technology en_US
dc.rights M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. en_US
dc.rights.uri http://dspace.mit.edu/handle/1721.1/7582 en_US
dc.subject Civil and Environmental Engineering. en_US
dc.title Interface pinning of CO₂ gravity currents en_US
dc.type Thesis en_US
dc.description.degree S.M. en_US
dc.contributor.department Massachusetts Institute of Technology. Dept. of Civil and Environmental Engineering. en_US
dc.identifier.oclc 813844793 en_US


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