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Fully compositional multi-scale reservoir simulation of various CO2 sequestration mechanisms

•Large-scale simulation of multi-phase flow using the ADGPRS/GFLASH software is presented.•Aqueous electrolyte solutions are modeled using the GHC equation.•Salt precipitation/dissolution are modeled using combined chemical/phase equilibrium.•Sequestration by residual, dissolution and mineral trappi...

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Bibliographic Details
Published in:Computers & chemical engineering 2017-01, Vol.96, p.183-195
Main Authors: Voskov, Denis V., Henley, Heath, Lucia, Angelo
Format: Article
Language:English
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Summary:•Large-scale simulation of multi-phase flow using the ADGPRS/GFLASH software is presented.•Aqueous electrolyte solutions are modeled using the GHC equation.•Salt precipitation/dissolution are modeled using combined chemical/phase equilibrium.•Sequestration by residual, dissolution and mineral trapping are illustrated.•Three examples demonstrate that ADGPRS/GFLASH captures key physics of CO2 sequestration. A multi-scale reservoir simulation framework for large-scale, multiphase flow with mineral precipitation in CO2-brine systems is proposed. The novel aspects of this reservoir modeling and simulation framework are centered around the seminal coupling of rigorous reactive transport with full compositional modeling and consist of (1) thermal, multi-phase flow tightly coupled to complex phase behavior, (2) the use of the Gibbs-Helmholtz Constrained (GHC) equation of state, (3) the presence of multiple homogeneous/heterogeneous chemical reactions, (4) the inclusion of mineral precipitation/dissolution, and (5) the presence of homogeneous/heterogeneous formations. The proposed modeling and simulation framework is implemented using the ADGPRS/GFLASH system. A number of examples relevant to CO2 sequestration including salt precipitation and solubility/mineral trapping are presented and geometric illustrations are used to elucidate key attributes of the proposed modeling framework.
ISSN:0098-1354
1873-4375
DOI:10.1016/j.compchemeng.2016.09.021