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Multiphase Modeling of Geologic Carbon Sequestration in Saline Aquifers
Author(s) -
Bandilla Karl W.,
Celia Michael A.,
Birkholzer Jens T.,
Cihan Abdullah,
Leister Evan C.
Publication year - 2015
Publication title -
groundwater
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.84
H-Index - 94
eISSN - 1745-6584
pISSN - 0017-467X
DOI - 10.1111/gwat.12315
Subject(s) - geomechanics , carbon sequestration , percolation theory , multiphase flow , aquifer , petroleum engineering , percolation (cognitive psychology) , permeability (electromagnetism) , geology , environmental science , soil science , geotechnical engineering , mechanics , engineering , groundwater , carbon dioxide , chemistry , topology (electrical circuits) , biochemistry , physics , organic chemistry , neuroscience , membrane , electrical engineering , biology
Geologic carbon sequestration ( GCS ) is being considered as a climate change mitigation option in many future energy scenarios. Mathematical modeling is routinely used to predict subsurface CO 2 and resident brine migration for the design of injection operations, to demonstrate the permanence of CO 2 storage, and to show that other subsurface resources will not be degraded. Many processes impact the migration of CO 2 and brine, including multiphase flow dynamics, geochemistry, and geomechanics, along with the spatial distribution of parameters such as porosity and permeability. In this article, we review a set of multiphase modeling approaches with different levels of conceptual complexity that have been used to model GCS . Model complexity ranges from coupled multiprocess models to simplified vertical equilibrium (VE) models and macroscopic invasion percolation models. The goal of this article is to give a framework of conceptual model complexity, and to show the types of modeling approaches that have been used to address specific GCS questions. Application of the modeling approaches is shown using five ongoing or proposed CO 2 injection sites. For the selected sites, the majority of GCS models follow a simplified multiphase approach, especially for questions related to injection and local‐scale heterogeneity. Coupled multiprocess models are only applied in one case where geomechanics have a strong impact on the flow. Owing to their computational efficiency, VE models tend to be applied at large scales. A macroscopic invasion percolation approach was used to predict the CO 2 migration at one site to examine details of CO 2 migration under the caprock.