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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crwiley:10.1002/ghg.2178 2024-10-13T14:06:37+00:00 CO 2 –Brine–rock interaction and sequestration capacity in carbonate reservoirs of the Tahe Oilfield, Xinjiang, China Tan, Yongsheng Li, Qi Xu, Liang Xu, Lifeng Yu, Tao Cao, Xiaomin National Natural Science Foundation of China 2022 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 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Greenhouse Gases: Science and Technology volume 12, issue 5, page 642-660 ISSN 2152-3878 2152-3878 journal-article 2022 crwiley https://doi.org/10.1002/ghg.2178 2024-10-03T04:04:58Z 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. Article in Journal/Newspaper Carbonic acid Wiley Online Library Greenhouse Gases: Science and Technology 12 5 642 660 |
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English |
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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. |
author2 |
National Natural Science Foundation of China |
format |
Article in Journal/Newspaper |
author |
Tan, Yongsheng Li, Qi Xu, Liang Xu, Lifeng Yu, Tao Cao, Xiaomin |
spellingShingle |
Tan, Yongsheng Li, Qi Xu, Liang Xu, Lifeng Yu, Tao Cao, Xiaomin CO 2 –Brine–rock interaction and sequestration capacity in carbonate reservoirs of the Tahe Oilfield, Xinjiang, China |
author_facet |
Tan, Yongsheng Li, Qi Xu, Liang Xu, Lifeng Yu, Tao Cao, Xiaomin |
author_sort |
Tan, Yongsheng |
title |
CO 2 –Brine–rock interaction and sequestration capacity in carbonate reservoirs of the Tahe Oilfield, Xinjiang, China |
title_short |
CO 2 –Brine–rock interaction and sequestration capacity in carbonate reservoirs of the Tahe Oilfield, Xinjiang, China |
title_full |
CO 2 –Brine–rock interaction and sequestration capacity in carbonate reservoirs of the Tahe Oilfield, Xinjiang, China |
title_fullStr |
CO 2 –Brine–rock interaction and sequestration capacity in carbonate reservoirs of the Tahe Oilfield, Xinjiang, China |
title_full_unstemmed |
CO 2 –Brine–rock interaction and sequestration capacity in carbonate reservoirs of the Tahe Oilfield, Xinjiang, China |
title_sort |
co 2 –brine–rock interaction and sequestration capacity in carbonate reservoirs of the tahe oilfield, xinjiang, china |
publisher |
Wiley |
publishDate |
2022 |
url |
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 |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_source |
Greenhouse Gases: Science and Technology volume 12, issue 5, page 642-660 ISSN 2152-3878 2152-3878 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ghg.2178 |
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Greenhouse Gases: Science and Technology |
container_volume |
12 |
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5 |
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642 |
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660 |
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1812812809518448640 |