2022
DOI: 10.1007/s00603-022-02994-6
|View full text |Cite
|
Sign up to set email alerts
|

Thermo-Poromechanical Properties of Pierre II Shale

Abstract: During the injection of carbon dioxide (CO2) for CO2 capture and storage (CCS) operations, the near-well (including casing, cement, and rock around it) can undergo several thermal loadings. These loadings can significantly increase or decrease the pore pressure and can thus lead to mechanical failure of the cement sheath and rock formation. When these failures appear in the caprock, they can compromise the integrity of the storage site. The understanding of thermo-mechanical behaviour of a potential caprock sh… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2023
2023
2023
2023

Publication Types

Select...
4

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(1 citation statement)
references
References 43 publications
(57 reference statements)
0
1
0
Order By: Relevance
“…In the current research, the length of the investigated geological profile was 150 m. The ground temperature along this profile was approximately equal to 130 • C. If the investigated profile was much longer, it would be expected that the V s showed a better correlation with temperature variation. This is due to the fact that the temperature variation changes the rheological characteristic of the rocks containing pore fluids as well as the poroelastic properties of the rocks [73,74]. Hence, for future works, investigations are suggested to be carried out to unveil the link between the ground temperature and V s variation.…”
Section: Discussionmentioning
confidence: 99%
“…In the current research, the length of the investigated geological profile was 150 m. The ground temperature along this profile was approximately equal to 130 • C. If the investigated profile was much longer, it would be expected that the V s showed a better correlation with temperature variation. This is due to the fact that the temperature variation changes the rheological characteristic of the rocks containing pore fluids as well as the poroelastic properties of the rocks [73,74]. Hence, for future works, investigations are suggested to be carried out to unveil the link between the ground temperature and V s variation.…”
Section: Discussionmentioning
confidence: 99%