Simulation Study on the Mechanical Effect of CO2 Geological Storage in Ordos Demonstration Area

Author:

Li Chang12,Hao Shuren34,Zhang Shengjie3,Jiang Yongqing3,Yi Zhidong5

Affiliation:

1. Harbin Center for General Survey of Natural Resources, CGS, Harbin 150081, China

2. Observation and Research Station of Earth Critical Zone on Black Soil in Harbin, Harbin 150081, China

3. School of Civil and Architectural Engineering, East China University of Technology, Nanchang 330013, China

4. Engineering Research Center for Geological Environment and Underground Space of Jiangxi Province, East China University of Technology, Nanchang 330013, China

5. Department of Natural Resources of Jiangxi Province, Nanchang 330002, China

Abstract

In order to understand the long-term process of CO2 storage and demonstrate its safety, multi-field coupled numerical simulation is considered a crucial technology in the field of geological CO2 storage. This study establishes a site-specific homogeneous thermo-hydro-mechanical coupling model based on TOUGH-FLAC3D coupling program using actual stratigraphic data from the Ordos demonstration area. The analysis investigates the transport behavior of CO2 within the formation considering pore permeability homogeneity, incorporates redistribution of effective stress and rock deformation, and provides a mechanical evaluation of the effectiveness of CO2 sequestration at this specific site. The findings indicate that: (1) the sealing effect of the cap rock depends on the difference of permeability between the reservoirs. The greater the permeability difference, the better the sealing effect. (2) High pore fluid pressure can lead to a decrease in the effective stress of rocks, causing deformation. After simulation calculations, the maximum deformation of rocks can reach 7.79 mm within a decade of CO2 injection. (3) Under the condition of continuous CO2 injection, the pore pressure will not be able to dissipate quickly and will continue to rise, and eventually shear failure will occur in the rock layer, but it is mainly concentrated in the lower part of the cap rock.

Funder

Natural Science Foundation of China

Jiangxi Geological Environment and Underground Space Engineering Research Center

China Geological Survey Project “Hydrogeological survey of Key Areas of the Upper Reaches of Hutuo River”

Publisher

MDPI AG

Subject

Water Science and Technology,Aquatic Science,Geography, Planning and Development,Biochemistry

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