Critical Dynamics of Gravito-Convective Mixing in Geological Carbon Sequestration

When CO(2) is injected in saline aquifers, dissolution causes a local increase in brine density that can cause Rayleigh-Taylor-type gravitational instabilities. Depending on the Rayleigh number, density-driven flow may mix dissolved CO(2) throughout the aquifer at fast advective time-scales through...

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Detalles Bibliográficos
Autores principales: Soltanian, Mohamad Reza, Amooie, Mohammad Amin, Dai, Zhenxue, Cole, David, Moortgat, Joachim
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5093900/
https://www.ncbi.nlm.nih.gov/pubmed/27808178
http://dx.doi.org/10.1038/srep35921

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5093900/
https://www.ncbi.nlm.nih.gov/pubmed/27808178
http://dx.doi.org/10.1038/srep35921

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