Migration and Distribution Characteristics of Proppant at the Corner of Horizontal Fracture Network in Coal Seam

Frontiers in Earth Science

Qingying Cheng¹  Heng Li²  Xinglong Zhao²  Zheng Sun²  Xuejie Jiao²  Bingxiang Huang²  Haoze Li² 

[1] Jiangsu Key Laboratory of Fire Safety in Urban Underground Space, China University of Mining and Technology, Xuzhou, China;State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Xuzhou, China;

关键词: coal seam;    fracture network;    corner;    proppant migration;    distribution characteristics;   

DOI  :  10.3389/feart.2021.792232

来源: DOAJ

【 摘 要 】

A complex fracture network is composed of many similar structures. The migration law of proppant at each structure is the core and basic content of the migration law of proppant in complex fracture network, and there is little research. In this study, the EulerianEulerian method (TEM) is used to analyze the migration and distribution characteristics of solid–liquid two phases at the fracture corner according to different corner types of the fracture network. The results show that the migration characteristics of proppant in the corner area can be divided into the corner anomaly area, buffer area, and stability area; the influence of the turning angle on proppant migration is mainly concentrated at the corner and in the range of 4 times the fracture width after turning. The probability of sand plugging at the corner of the “Y → T” fracture is lower than that of “L → l”, higher than that of the “X → +” wing branch fracture, and lower than that of the main fracture. At the corner of the fracture network, after the solid flow turns, the proppant will form a high sand area on the side of the impact fracture surface, then rebound back to the fracture, form a sand-free area on the other side, and form a high-velocity core in the refraction interval. At the corner of the “L → l” fracture, there are one high sand area, one non-sand area, two low-velocity areas, and one high-velocity area; there are three low-velocity areas, two sand-free areas, and one high sand area at the corner of the “Y → T” fracture; at the corner of the “X → +” fracture, there is a high sand area and no sand-free area, and the flow velocity of the main fracture is much greater than that of the wing branch fracture.

【 授权许可】

Unknown