2012
DOI: 10.1007/s12665-012-1689-9
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Numerical analysis of thermal effects during carbon dioxide injection with enhanced gas recovery: a theoretical case study for the Altmark gas field

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Cited by 26 publications
(14 citation statements)
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“…OGS has a built-in random-walk particle tracking method for Euler-Lagrange simulations [97] and can simulate incompressible and compressible flow [98], densitydependent flow [99], unsaturated flow [100], two-phase flow [101,102], and overland flow [103]. All flow model components are available for non-isothermal conditions and for deformable porous media.…”
Section: Opengeosysmentioning
confidence: 99%
“…OGS has a built-in random-walk particle tracking method for Euler-Lagrange simulations [97] and can simulate incompressible and compressible flow [98], densitydependent flow [99], unsaturated flow [100], two-phase flow [101,102], and overland flow [103]. All flow model components are available for non-isothermal conditions and for deformable porous media.…”
Section: Opengeosysmentioning
confidence: 99%
“…The H 2 O is assumed to be residually trapped and immobile such that θ w ρ w is constant (Singh et al 2011(Singh et al , 2012. The volume fraction of the rock is θ r = 1 − φ, where φ [-] is the porosity, and the product θ r ρ r is also constant.…”
Section: The Mathematical Modelmentioning
confidence: 99%
“…Andre et al 2010;Mathias et al 2013a). Exceptions to these include Han et al (2012), who considered a minimum initial pressure of 6.89 MPa, Ziabaksh-Ganji & Kooi (2014), who assumed an initial pressure of 6 MPa, Afanasyev (2013), who assumed a minimum initial pressure of 4.5 MPa, and Singh, Goerke & Kolditz (2011) and Singh et al (2012), who considered an initial pressure of 4 MPa. However, depleted gas reservoirs are often abandoned at pressures lower than 1 MPa.…”
Section: Introductionmentioning
confidence: 99%
“…Thermal effects including changes in in-situ reservoir temperature arising from heat transfer/exchanges between the injected CO 2 and the formation, contribute to the dynamics of underground activities (Hou et al, 2012, Norden et al, 2012, Singh et al, 2012. Changes in reservoir temperature are dependent on the geological structure and variations in rock thermal conductivity (Norden et al, 2012); some aspects of Joule-Thompson cooling (JTC) and viscous heat dissipation (VHD) are illustrated in Singh et al (2012), while in Hou et al (2012) the thermal process is incorporated with hydro-mechanical processes for the prediction of reservoir responses.…”
Section: Introductionmentioning
confidence: 99%
“…Changes in reservoir temperature are dependent on the geological structure and variations in rock thermal conductivity (Norden et al, 2012); some aspects of Joule-Thompson cooling (JTC) and viscous heat dissipation (VHD) are illustrated in Singh et al (2012), while in Hou et al (2012) the thermal process is incorporated with hydro-mechanical processes for the prediction of reservoir responses.…”
Section: Introductionmentioning
confidence: 99%