Instability of a Diffusive Boundary Layer beneath a Capillary Transition Zone

Natural convection induced by carbon dioxide (CO<sub>2</sub>) dissolution from a gas cap into the resident formation brine of a deep saline aquifer in the presence of a capillary transition zone is an important phenomenon that can accelerate the dissolution process, reducing the risk of...

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Bibliographic Details
Main Authors: Fengyuan Zhang, Hamid Emami-Meybodi
Format: Article
Language:English
Published: MDPI AG 2018-10-01
Series:Fluids
Subjects:
Online Access:https://www.mdpi.com/2311-5521/3/4/85