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Impacts of stratum dip angle on CO 2 geological storage amount and security

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  • Fugang Wang
  • Jing Jing
  • Tianfu Xu
  • Yanlin Yang
  • Guangrong Jin

Abstract

Storage strata are usually generalized as horizontal when using numerical simulation methods to analyze CO 2 geological storage in saline aquifers. However, horizontal strata are not common in nature. Most strata have gradients, because of the effects of geological structure and diagenesis. Based on the actual strata dip angle variation range of two CO 2 injection demonstration projects in China, five modeling schemes were designed to investigate the impact of formation dip on CO 2 storage amount and space migration of gas‐phase CO 2 in reservoir formation. The results show that the total CO 2 storage amount is inversely proportional to formation dip, and after injection is halted, storage amounts of upper and lower parts of the same stratum reservoir have a reverse trend. Formation dip has a significant impact on the migration of CO 2 . The greater the formation dip, the more significant the effect on CO 2 migration distance. Given the low porosity and permeability of the Shiqianfeng formation reservoir in the case study, when the stratum dip angle is 16°, at centennial time scale, CO 2 migration distance is 47.06% greater than that in the horizontal reservoir. We expect that for storage reservoirs with high porosity and permeability, the influence of formation dip on CO 2 migration will be more significant. Because non‐horizontal strata are predominant in deep saline aquifers in nature, regardless of the influence of formation dip, CO 2 leakage risks in geological storage will be greatly underestimated. Therefore, in research related to CO 2 geological storage, the stratum dip angle must be considered. © 2016 Society of Chemical Industry and John Wiley & Sons, Ltd

Suggested Citation

  • Fugang Wang & Jing Jing & Tianfu Xu & Yanlin Yang & Guangrong Jin, 2016. "Impacts of stratum dip angle on CO 2 geological storage amount and security," Greenhouse Gases: Science and Technology, Blackwell Publishing, vol. 6(5), pages 682-694, October.
    • Handle: RePEc:wly:greenh:v:6:y:2016:i:5:p:682-694
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    File URL: http://hdl.handle.net/10.1002/ghg.1594
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    1. Pruess, Karsten & García, Julio & Kovscek, Tony & Oldenburg, Curt & Rutqvist, Jonny & Steefel, Carl & Xu, Tianfu, 2004. "Code intercomparison builds confidence in numerical simulation models for geologic disposal of CO2," Energy, Elsevier, vol. 29(9), pages 1431-1444.
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    Cited by:

    1. Kim, Min & Kwon, Seoyoon & Ji, Minsoo & Shin, Hyundon & Min, Baehyun, 2023. "Multi-lateral horizontal well with dual-tubing system to improve CO2 storage security and reduce CCS cost," Applied Energy, Elsevier, vol. 330(PB).
    2. Jing, Jing & Yang, Yanlin & Cheng, Jianmei & Ding, Zhaojing & Wang, Dandan & Jing, Xianwen, 2023. "Analysis of the effect of formation dip angle and injection pressure on the injectivity and migration of CO2 during storage," Energy, Elsevier, vol. 280(C).
    3. Emad A. Al†Khdheeawi & Stephanie Vialle & Ahmed Barifcani & Mohammad Sarmadivaleh & Yihuai Zhang & Stefan Iglauer, 2018. "Impact of salinity on CO2 containment security in highly heterogeneous reservoirs," Greenhouse Gases: Science and Technology, Blackwell Publishing, vol. 8(1), pages 93-105, February.
    4. Jing, Jing & Yang, Yanlin & Tang, Zhonghua, 2021. "Assessing the influence of injection temperature on CO2 storage efficiency and capacity in the sloping formation with fault," Energy, Elsevier, vol. 215(PA).
    5. Masoud Ahmadinia & Seyed M. Shariatipour, 2020. "Analysing the role of caprock morphology on history matching of Sleipner CO2 plume using an optimisation method," Greenhouse Gases: Science and Technology, Blackwell Publishing, vol. 10(5), pages 1077-1097, October.
    6. Masoud Ahmadinia & Seyed M. Shariatipour, 2021. "A study on the impact of storage boundary and caprock morphology on carbon sequestration in saline aquifers," Greenhouse Gases: Science and Technology, Blackwell Publishing, vol. 11(1), pages 183-205, February.

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