Effect of In-Situ Stress on Hydraulic Fracturing of Tight Sandstone Based on Discrete Element Method

被引:2
|
作者
Wang, Hongjian [1 ,2 ]
Gong, Wanlin [1 ]
Yuan, Guangxiang [1 ]
Wang, Xiaodong [1 ]
Zhao, Jitao [3 ]
Su, Yujie [1 ,2 ]
Wang, Yuchen [1 ,2 ]
机构
[1] North China Univ Water Resources & Elect Power, Zhengzhou 450045, Peoples R China
[2] Key Lab Geol Environm Intelligent Monitoring & Di, Zhengzhou 450045, Peoples R China
[3] SCIVIC Engn Corp, Luoyang 471000, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
tight sandstone; hydraulic fracturing; fracture network evolution; discrete element method; fractal dimension; PROPAGATION; ROCK; TOUGHNESS; MODEL;
D O I
10.3390/en15155620
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The tight sandstone reservoir in the Qianfoya formation of well PL-3 of the Puguang gas field in Sichuan, China, obtained a high-yield gas flow after a volume fracturing treatment. However, the stimulated reservoir volume (SRV), fracture morphology, scale and formation law still remain unclear. Based on particle flow discrete-element theory in this paper, we carried out a few trials of the Brazilian splitting test, uniaxial compression and triaxial compression of rock mechanics. Meanwhile, the research also testified to the conversion relationship between macroparameters and microparameters, established the numerical simulation on hydraulic fracturing through PFC2D discrete element software, and finally analyzed the influence of difference coefficients on the fracturing effect, in terms of different in-situ stresses. The conclusions are as follows: firstly, the influence of in-situ stress is essential for the direction, shape and quantity of fracture propagation, and the fractures generated by hydraulic fracturing are mainly tension fractures, accounting for over 90% of the total longitudinal fractures. Secondly, it is indicated that when the difference coefficient is small in the in-situ stress, the fractures formed by hydraulic fracturing expand randomly around the wellbore. When the difference coefficient K-h of in-situ stress is above 0.6, the development of hydraulic fractures is mainly controlled by in-situ stress; as a result, the fractures tend to expand in the vertical direction of the minimum horizontal principal stress and the fracture shape is relatively singular. When the difference coefficient of in-situ stress was 0.3, in total, 3121 fractures were generated by fracturing, and the fractal dimension D value of the fracture network complexity was 1.60. In this case, this fracturing effect was the best and it is the easiest to achieve for the purpose of economical and effective development on large-scale volume fracturing.
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页数:13
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