CO 2 –Brine–rock interaction and sequestration capacity in carbonate reservoirs of the Tahe Oilfield, Xinjiang, China

Abstract The characteristics of each carbonate reservoir are greatly different, and current databases are insufficient to support engineering scheme design and optimization of carbon dioxide (CO 2 ) sequestration and enhanced oil recovery. In this paper, the behavior of CO 2 ‐brine‐rock interactions...

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Bibliographic Details
Published in:Greenhouse Gases: Science and Technology
Main Authors: Tan, Yongsheng, Li, Qi, Xu, Liang, Xu, Lifeng, Yu, Tao, Cao, Xiaomin
Other Authors: National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2022
Subjects:
Online Access:http://dx.doi.org/10.1002/ghg.2178
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ghg.2178
https://onlinelibrary.wiley.com/doi/full-xml/10.1002/ghg.2178
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Summary:Abstract The characteristics of each carbonate reservoir are greatly different, and current databases are insufficient to support engineering scheme design and optimization of carbon dioxide (CO 2 ) sequestration and enhanced oil recovery. In this paper, the behavior of CO 2 ‐brine‐rock interactions was investigated under supercritical CO 2 (50°C and 8.5 MPa) conditions. Five experiments were carried out, including CO 2 solubility in brine, mass loss analysis by static reaction of CO 2 –brine–rock, mineralogical composition analysis by X‐ray diffraction (XRD), core surface morphology analysis by scanning electron microscopy (SEM), and wettability alteration by contact angle analysis. The experimental results showed that: (a) the CO 2 solubility in brine increases with increasing pressure, but it increases slowly and gradually reaches equilibrium; (b) the mass loss of carbonate increases with reaction time, but its increments decrease with reaction time; (c) the calcite content gradually decreases and the quartz content slightly increases with reaction time, as evidenced by XRD analysis; (d) based on SEM image analysis, calcite was dissolved into brine by carbonic acid to make the pores larger, and then subsequent precipitation made the pores smaller; and (e) the carbonate rock surface became more water‐wet after CO 2 –brine–rock interaction experiments due to surface corrosion and increased quartz content. Using the experimental results, a mathematical model was developed to predict CO 2 sequestration capacity under reservoir conditions. The results suggest that CO 2 solubility in brine was the main aspect compared with mineral trapping in carbonate reservoirs, and CO 2 sequestration capacity increased with increasing temperature and pressure. © 2022 Society of Chemical Industry and John Wiley & Sons, Ltd.