TY - JOUR
T1 - The use of supercritical CO2 in deep geothermal reservoirs as a working fluid
T2 - Insights from coupled THMC modeling
AU - Gan, Quan
AU - Candela, Thibault
AU - Wassing, Brecht
AU - Wasch, Laura
AU - Liu, Jun
AU - Elsworth, Derek
N1 - Funding Information:
This project was partly subsidized through the ERANET Cofund GEOTHERMICA (Project no. 731117 ), from the European Commission , Topsector Energy subsidy from the Ministry of Economic Affairs of the Netherlands, Federal Ministry for Economic Affairs and Energy of Germany and EUDP, and the Science and Technology Department of Sichuan Province (Grant No. 21YFH0048 ).
Publisher Copyright:
© 2021 Elsevier Ltd
PY - 2021/11
Y1 - 2021/11
N2 - A coupled THMC (thermal-hydrological-mechanical-chemical) model is developed and applied to explore the potential feasibility of using scCO2 (supercritical carbon dioxide) as a working fluid in geothermal reservoirs. This is achieved by examining the evolution of the kinetics of mineral precipitation-dissolution and its associated impact on the evolution of the rock permeability and porosity. The pH of the reservoir rapidly reduces from 7 to ∼4.5–5 due to the fast dissolution of calcite. Chemical reactions and mineral dissolution and precipitation near the injector are suppressed by the plug-flow penetration of anhydrous scCO2 displacing the original pore fluid. A conceptual three-zone model is proposed to illustrate the kinetic process of feldspar dissolution and precipitation depending on timing. The initial high concentration of K+ prompts feldspar to precipitate in the first stage by consuming K+ until 1y, Feldspar were dissolved into precipitations of illite, smectite, and siderite at 1-6y, with albite, muscovite and kaolinite mostly precipitated in the last stage 6–10y. The precipitations of secondary clay minerals and quartz serve to maintain the integrity of caprock sealing. Continuous scCO2 injection under fully coupled THMC model shows a 1.4-times enhancement of fracture permeability and 1.2-times enhancement of matrix permeability dominated by chemical dissolution and thermal unloading process. The pronounced thermal drawdown is the principal factor in enhancing permeability and porosity near injection well. Furthermore, the expansive capability of CO2 provides extra benefits in enhancing formation pressure to ensure consistent high flow rates, while achieving a higher thermal energy extraction efficiency and preventing scaling issues in wellbore. The mass concentration of scCO2 in the production well increased to 0.82 after 1.2 × 108s also leads to the enhancement of fluid enthalpy up to 6.5 × 105 J/kg, due to the high heat capacity of scCO2. The injected CO2 are sequestered at ∼2 × 107 kg at t = 2 × 108s (6.34y) as the solubility trapping mechanism.
AB - A coupled THMC (thermal-hydrological-mechanical-chemical) model is developed and applied to explore the potential feasibility of using scCO2 (supercritical carbon dioxide) as a working fluid in geothermal reservoirs. This is achieved by examining the evolution of the kinetics of mineral precipitation-dissolution and its associated impact on the evolution of the rock permeability and porosity. The pH of the reservoir rapidly reduces from 7 to ∼4.5–5 due to the fast dissolution of calcite. Chemical reactions and mineral dissolution and precipitation near the injector are suppressed by the plug-flow penetration of anhydrous scCO2 displacing the original pore fluid. A conceptual three-zone model is proposed to illustrate the kinetic process of feldspar dissolution and precipitation depending on timing. The initial high concentration of K+ prompts feldspar to precipitate in the first stage by consuming K+ until 1y, Feldspar were dissolved into precipitations of illite, smectite, and siderite at 1-6y, with albite, muscovite and kaolinite mostly precipitated in the last stage 6–10y. The precipitations of secondary clay minerals and quartz serve to maintain the integrity of caprock sealing. Continuous scCO2 injection under fully coupled THMC model shows a 1.4-times enhancement of fracture permeability and 1.2-times enhancement of matrix permeability dominated by chemical dissolution and thermal unloading process. The pronounced thermal drawdown is the principal factor in enhancing permeability and porosity near injection well. Furthermore, the expansive capability of CO2 provides extra benefits in enhancing formation pressure to ensure consistent high flow rates, while achieving a higher thermal energy extraction efficiency and preventing scaling issues in wellbore. The mass concentration of scCO2 in the production well increased to 0.82 after 1.2 × 108s also leads to the enhancement of fluid enthalpy up to 6.5 × 105 J/kg, due to the high heat capacity of scCO2. The injected CO2 are sequestered at ∼2 × 107 kg at t = 2 × 108s (6.34y) as the solubility trapping mechanism.
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U2 - 10.1016/j.ijrmms.2021.104872
DO - 10.1016/j.ijrmms.2021.104872
M3 - Article
AN - SCOPUS:85114663129
SN - 1365-1609
VL - 147
JO - International Journal of Rock Mechanics and Mining Sciences
JF - International Journal of Rock Mechanics and Mining Sciences
M1 - 104872
ER -