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Research Highlight | Open Access

Characterization of mineral and pore evolution under CO2-brine-rock interaction at in-situ conditions

Songtao Wu1,2,3( )Cong Yu1,2,3Xiaolin Hu1Zhichao Yu1,2,3Xiaohua Jiang1,2,3
Research Institute of Petroleum Exploration and Development, CNPC, Beijing 100083, P. R. China
National Energy Tight Oil and Gas R&D Center, Beijing 100083, P. R. China
CNPC Key Laboratory of Oil and Gas Reservoirs, Beijing 100083, P. R. China
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Abstract

Herein, a method of physical modeling of CO2-brine-rock interaction and characterization of mineral and pore evolution at in-situ conditions is established. The nested preparation and installation of the same sample with different sizes could protect and keep the integrality of the millimeter-size sample in conventional high-temperature and high-pressure reactors. This paper establishes a procedure to obtain the three-dimensional comparison of minerals and pores before and after the reaction at in-situ conditions. The resolution is updated from 5-10 μm to 10 nm, which could be helpful for modeling CO2-brine-rock interaction in unconventional tight reservoirs. This method could be applied to CO2-enhanced oil recovery as well as CO2 capture, utilization, and storage scientific research. Furthermore, it may shed light on the carbon sequestration schemes in the Chinese petroleum industry.

References

 
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Wu, S., Zou, C., Ma, D., et al. Reservoir property changes during CO2-brine flow-through experiments in tight sandstone: Implications for CO2 enhanced oil recovery in the Triassic Chang 7 Member tight sandstone, Ordos Basin, China. Journal of Asian Earth Sciences, 2019, 179: 200-210.
 
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Advances in Geo-Energy Research
Pages 177-178
Cite this article:
Wu S, Yu C, Hu X, et al. Characterization of mineral and pore evolution under CO2-brine-rock interaction at in-situ conditions. Advances in Geo-Energy Research, 2022, 6(2): 177-178. https://doi.org/10.46690/ager.2022.02.09

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Received: 28 March 2022
Revised: 05 April 2022
Accepted: 09 April 2022
Published: 11 April 2022
© The Author(s) 2022.

Open Access This article is distributed under the terms and conditions of the Creative Commons Attribution (CC BY-NC-ND) license, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

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