Multiscale Fractal Characterization of Pore-Fracture Structure of Tectonically Deformed Coal Compared to Primary Undeformed Coal: Implications for CO2 Geological Sequestration in Coal Seams

被引:4
|
作者
Zhang, Kun [1 ,2 ]
Liu, Huihu [2 ,3 ]
Ma, Mengya [4 ]
Xu, Hongjie [3 ]
Fang, Huihuang [3 ]
机构
[1] Anhui Univ Sci & Technol, State Key Lab Min Response & Disaster Prevent & Co, Huainan 232000, Peoples R China
[2] Hefei Comprehens Natl Sci Ctr, Inst Energy, Hefei 230031, Peoples R China
[3] Anhui Univ Sci & Technol, Sch Earth & Environm, Huainan 232001, Peoples R China
[4] Anhui Univ Sci & Technol, Joint Natl Local Engn Res Ctr Safe & Precise Coal, Huainan 232001, Peoples R China
关键词
CO2 geological sequestration; tectonically deformed coal reservoirs; multiscale pore-fracture structure; fractal characterization; geological potential; CH4 ADSORPTION CAPACITY; SICHUAN BASIN; SUPERCRITICAL CO2; DIFFUSION; METHANE; PERMEABILITY; DIMENSION; SHALES; ANTHRACITE; DESORPTION;
D O I
10.3390/pr11102934
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
The tectonically deformed coal (TDC) reservoirs with abundant gas resources and low permeability are expected to become one of the target coal seams for carbon dioxide geological storage-enhanced coalbed methane recovery (CO2-ECBM). The pore-fracture structure plays a crucial role in determining the effectiveness of CO2 storage. Fractal analysis provides a valuable approach to quantitatively describe the complex and heterogeneous pore-fracture structures across various scales in coal matrixes. Accordingly, the TDC samples in the Huainan-Huaibei coalfield and primary-undeformed coal (PUC) samples in the Qinshui Basin were selected for pore-fracture structure parameter tests using the mercury intrusion porosimetry (MIP) and low-temperature nitrogen adsorption (LNA) methods. Their multiscale pore-fracture parameters were analyzed using different fractal methods based on pore diameter. According to the fractal results, a multiscale classification standard for pore-fracture structures was devised in this study that is suitable for the controlling gas migration process. A parameter of 8 nm is set as the separating pore diameter for gas migration and storage. It was observed that the connectivity of migration pores (>8 nm) in TDC samples was stronger compared to PUC samples, reflected in larger pore volumes and smaller fractal dimensions. However, its complex development of seepage pores (150-300 nm) may hinder the flow of CO2 injection. As for the storage pores (<8 nm), the fractal dimension of the 2-8 nm pores in TDC was found to be similar to that of PUC but with larger pore volumes. The fractal dimension of the filling pores (<2 nm) in TDC samples was relatively lower, which facilitates efficient gas volume filling. Therefore, the pore-fracture structure of the TDC samples is found to be more advantages for CO2 injection and storage compared to the PUC. This suggests that TDC reservoirs holds promising geological potential for CO2-ECBM implementation.
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页数:23
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