High-pressure mercury intrusion analysis of pore structure in typical lithofacies shale

被引:7
|
作者
Wei, Jianguang [1 ,2 ,3 ]
Zhou, Xiaofeng [1 ,2 ,3 ]
Shamil, Sultanov [4 ]
Yuriy, Kotenev [4 ]
Yang, Erlong [1 ,5 ]
Yang, Ying [1 ,2 ,3 ]
Wang, Anlun [1 ,2 ,3 ]
机构
[1] Northeast Petr Univ, Natl Key Lab Continental Shale Oil, Daqing 163318, Heilongjiang, Peoples R China
[2] Northeast Petr Univ, Key Lab Continental Shale Hydrocarbon Accumulat &, Minist Educ, Daqing 163318, Heilongjiang, Peoples R China
[3] Northeast Petr Univ, Inst Unconvent Oil & Gas, Daqing 163318, Peoples R China
[4] Ufa State Petr Technol Univ, World Class Res Ctr Efficient Dev Global Liquid Hy, Ufa 450064, Russia
[5] Northeast Petr Univ, Sch Petr Engn, Daqing 163318, Heilongjiang, Peoples R China
关键词
Shale reservoirs; Pore throat structure; Cross scale; Coupling parameters; Mercury intrusion method; REAL-GAS MIXTURE; TRANSPORT; POROSITY; MODEL; INJECTION; NANOPORES; RESERVOIR; BARNETT; AREA;
D O I
10.1016/j.energy.2024.130879
中图分类号
O414.1 [热力学];
学科分类号
摘要
In this paper, statistical research on the characterization of pore and fracture structures is systematically conducted on shale reservoirs in different blocks and under different lithofacies conditions. The impact of lithological characteristics on shale pore fracture structures is revealed, and the coupling mechanism of "high-pressure mercury injection, pore fracture structure, and lithofacies" is clarified. Results show that: (a). When the capillary force is equal to 0.0035 MPa, the pore throat radius is equal to 209.661 mu m. (b). There exist turning pressures both in injection curve and removal curve. When the capillary pressure is lower than 100 MPa, the slope of injection curve is high, while when the capillary pressure is higher than 100 MPa, the slope of injection curve becomes lower. (c). The majority of pores is distributed in the pore size interval range from 0.063 mu m to 0.004 mu m. (d). There are also a certain amount of regular pores in inorganic pores. Part of the pores are secondary intergranular dissolved pores formed by later dissolution.
引用
收藏
页数:10
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