Author
Listed:
- Zhuo Li
(School of Earth Sciences, Northeast Petroleum University, Daqing 163318, China
Office of Academic Research, Northeast Petroleum University, Daqing 163318, China)
- Yanfang Lv
(School of Earth Sciences, Northeast Petroleum University, Daqing 163318, China)
- Bin Liu
(School of Electrical Engineering and Information, Northeast Petroleum University, Daqing 163318, China)
Abstract
CO 2 geological storage, which is an effective way to reduce CO 2 emissions, is of great significance to mitigate the current greenhouse effect. In long-term CO 2 storage, although the chemical reaction rate of CO 2 –brine–rock is slow, it can significantly change the mineral composition of rock and the structure and properties of pores and joints, and then change the transport process and distribution state of CO 2 in porous media. Therefore, a simplified 2D geological model is established based on the geological data of the Shihezi Formation in the Ordos Basin, China. The mechanism of the CO 2 –brine–rock reaction and its effect on mineral transformation and pore permeability are studied. In the early stage of CO 2 geological sequestration, the rate of CO 2 intrusion into the caprock is fast, the CO 2 –brine–rock reaction in the early stage is mainly a dissolution reaction, and the porosity and permeability of the caprock show an increasing trend. During the period from 100 to 1000 years of CO 2 sequestration, the vertical distance of CO 2 intrusion into the caprock does not change much. During this period, the type of CO 2 –brine–rock reaction is mainly a precipitation reaction, which reduces the porosity and permeability of the caprock and increases the sealing ability of the caprock to a certain extent. Our results can not only provide theoretical support for the site selection and risk assessment of CO 2 geological sequestration, but also provide a theoretical basis and practical guidance for large-scale commercial storage in the future.
Suggested Citation
Zhuo Li & Yanfang Lv & Bin Liu, 2022.
"Numerical Simulation of CO 2 Migration and Geochemical Reactions in Shihezi Formation Caprock, China,"
Energies, MDPI, vol. 16(1), pages 1-17, December.
Handle:
RePEc:gam:jeners:v:16:y:2022:i:1:p:92-:d:1010731
Download full text from publisher
Corrections
All material on this site has been provided by the respective publishers and authors. You can help correct errors and omissions. When requesting a correction, please mention this item's handle: RePEc:gam:jeners:v:16:y:2022:i:1:p:92-:d:1010731. See general information about how to correct material in RePEc.
If you have authored this item and are not yet registered with RePEc, we encourage you to do it here. This allows to link your profile to this item. It also allows you to accept potential citations to this item that we are uncertain about.
We have no bibliographic references for this item. You can help adding them by using this form .
If you know of missing items citing this one, you can help us creating those links by adding the relevant references in the same way as above, for each refering item. If you are a registered author of this item, you may also want to check the "citations" tab in your RePEc Author Service profile, as there may be some citations waiting for confirmation.
For technical questions regarding this item, or to correct its authors, title, abstract, bibliographic or download information, contact: MDPI Indexing Manager (email available below). General contact details of provider: https://www.mdpi.com .
Please note that corrections may take a couple of weeks to filter through
the various RePEc services.