Pattern formation and coarsening dynamics in three-dimensional convective mixing in porous media

Geological carbon dioxide (CO[subscript 2]) sequestration entails capturing and injecting CO[subscript 2][subscript 2]into deep saline aquifers for long-term storage. The injected CO[subscript 2] partially dissolves in groundwater to form a mixture that is denser than the initial groundwater. The lo...

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Bibliographic Details
Main Authors: Fu, Xiaojing (Contributor), Cueto-Felgueroso, Luis (Contributor), Juanes, Ruben (Contributor)
Other Authors: Massachusetts Institute of Technology. Department of Civil and Environmental Engineering (Contributor)
Format: Article
Language:English
Published: Royal Society, The, 2015-01-07T16:00:51Z.
Subjects:
Online Access:Get fulltext
LEADER 01994 am a22002293u 4500
001 92724
042 |a dc 
100 1 0 |a Fu, Xiaojing  |e author 
100 1 0 |a Massachusetts Institute of Technology. Department of Civil and Environmental Engineering  |e contributor 
100 1 0 |a Juanes, Ruben  |e contributor 
100 1 0 |a Fu, Xiaojing  |e contributor 
100 1 0 |a Cueto-Felgueroso, Luis  |e contributor 
100 1 0 |a Juanes, Ruben  |e contributor 
700 1 0 |a Cueto-Felgueroso, Luis  |e author 
700 1 0 |a Juanes, Ruben  |e author 
245 0 0 |a Pattern formation and coarsening dynamics in three-dimensional convective mixing in porous media 
260 |b Royal Society, The,   |c 2015-01-07T16:00:51Z. 
856 |z Get fulltext  |u http://hdl.handle.net/1721.1/92724 
520 |a Geological carbon dioxide (CO[subscript 2]) sequestration entails capturing and injecting CO[subscript 2][subscript 2]into deep saline aquifers for long-term storage. The injected CO[subscript 2] partially dissolves in groundwater to form a mixture that is denser than the initial groundwater. The local increase in density triggers a gravitational instability at the boundary layer that further develops into columnar plumes of CO[subscript 2]-rich brine, a process that greatly accelerates solubility trapping of the CO[subscript 2]. Here, we investigate the pattern-formation aspects of convective mixing during geological CO[subscript 2] sequestration by means of high-resolution three-dimensional simulation. We find that the CO[subscript 2] concentration field self-organizes as a cellular network structure in the diffusive boundary layer at the top boundary. By studying the statistics of the cellular network, we identify various regimes of finger coarsening over time, the existence of a non-equilibrium stationary state, and a universal scaling of three-dimensional convective mixing. 
546 |a en_US 
655 7 |a Article 
773 |t Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences