中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Combined Effect of In Situ Stress Level and Bedding Anisotropy on Hydraulic Fracture Vertical Growth in Deep Marine Shale Revealed via CT Scans and Acoustic Emission

文献类型:期刊论文

作者Guo, Peng2; Li, Xiao1,2; Li, Shouding1; Mao, Tianqiao1
刊名ENERGIES
出版日期2023-11-01
卷号16期号:21页码:14
关键词in situ stress level bedding anisotropy hydraulic fracture growth CT scans acoustic emission
DOI10.3390/en16217270
英文摘要The economic exploitation of unconventional gas and oil in deep shale relies closely on effective hydraulic fracturing stimulations. However, the fracturing operations of deep shale reservoirs face challenges of insufficient fracture growth and a rapid decline in productivity due to the increasing in situ stress level. In addition, the shale strata on the margin of the Sichuan Basin are frequently folded and faulted, and the change in bedding inclinations significantly complicates the process of hydraulic fracturing. The investigation of the combined effect of the in situ stress level and bedding anisotropy on the hydraulic fracture configuration is vital for fracturing engineering design. To analyze this, we conducted hydraulic fracturing tests on shale cores to simulate the hydraulic fracture initiation and growth from a horizontally positioned perforation. By using acoustic emission detection and CT scans, the influence of natural stress levels and the angle of the shale's bedding on the process of hydraulic fracturing in shale and the resulting fracture geometry were analyzed. The results showed that the area of hydraulic fracture under a higher stress level (sigma(1) = 50 MPa, sigma(3) = 40 MPa) was about 13%similar to 23% smaller than that created under the lower stress level (sigma(1) = 30 MPa, sigma(3) = 20 MPa) when the bedding angle was smaller than 60 degrees. With the increase in bedding angle, the curves of the fracture area and fracture network index under two different stress levels presented similar decreasing trends. Also, the time from micro-crack generation to sample breakdown was significantly reduced when the bedding orientation changed from the horizontal to vertical position. The increasing stress level significantly increased the breakdown pressure. In particular, the fracturing of shale samples with bedding angles of 0 degrees and 30 degrees required a higher fluid pressure and released more energy than samples with larger bedding inclinations. Additionally, the measurement of the sample radial deformation indicated that the hydraulic fracture opening extent was reduced by about 46%similar to 81% with the increasing stress level.
WOS关键词UNCONVENTIONAL RESERVOIRS ; PROPAGATION ; INITIATION ; MORPHOLOGY
资助项目National Natural Science Foundation of China[42090023] ; National Key R&D Program of China[2020YFA0710504]
WOS研究方向Energy & Fuels
语种英语
出版者MDPI
WOS记录号WOS:001103344800001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/110660]  
专题地质与地球物理研究所_中国科学院页岩气与地质工程重点实验室
通讯作者Guo, Peng; Li, Xiao
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, Beijing 100029, Peoples R China
2.Peking Univ, Inst Energy, Sch Earth & Space Sci, Beijing 100871, Peoples R China
推荐引用方式
GB/T 7714
Guo, Peng,Li, Xiao,Li, Shouding,et al. Combined Effect of In Situ Stress Level and Bedding Anisotropy on Hydraulic Fracture Vertical Growth in Deep Marine Shale Revealed via CT Scans and Acoustic Emission[J]. ENERGIES,2023,16(21):14.
APA Guo, Peng,Li, Xiao,Li, Shouding,&Mao, Tianqiao.(2023).Combined Effect of In Situ Stress Level and Bedding Anisotropy on Hydraulic Fracture Vertical Growth in Deep Marine Shale Revealed via CT Scans and Acoustic Emission.ENERGIES,16(21),14.
MLA Guo, Peng,et al."Combined Effect of In Situ Stress Level and Bedding Anisotropy on Hydraulic Fracture Vertical Growth in Deep Marine Shale Revealed via CT Scans and Acoustic Emission".ENERGIES 16.21(2023):14.

入库方式: OAI收割

来源:地质与地球物理研究所

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