马天辉

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副研究员

博士生导师

硕士生导师

性别:男

毕业院校:东北大学

学位:博士

所在单位:土木工程系

学科:岩土工程

办公地点:土木4#楼330

联系方式:QQ: 19928600 wechat: tianhuima

电子邮箱:tianhuima@dlut.edu.cn

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出版著作和论文

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Effect of discontinuity stress shadows on hydraulic fracture re-orientation

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论文类型:期刊论文

发表时间:2017-01-01

发表刊物:INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES

收录刊物:SCIE、EI

卷号:91

页面范围:179-194

ISSN号:1365-1609

关键字:Hydraulic fracture re-orientation; Stress shadow effect; Differential stress; Rock mass homogeneity, Numerical modelling

摘要:Hydraulic fracturing has been applied to the cave mining industry as a pre-conditioning method to improve rock mass caveability and fragmentation sizes. In theory, the hydraulic fracture orientation is dictated by and is perpendicular to the minimum in-situ stress orientation. Such orientations will not always result in the creation of a blocky rock mass to aid caveability. The understanding of hydraulic fracture re-orientation induced by the stress shadow effect is important for either avoiding the undesirable interaction between multiple transverse hydraulic fractures or taking advantage of this phenomenon to Create prescribed hydraulic fractures that result in the creation of blocky rock masses. In this paper, the existing knowledge of the stress shadow effect around a pre-existing discontinuity is reviewed. A 3D numerical modelling code, Rock Failure Process Analysis (RFPA) is used to investigate factors influencing hydraulic fracture re-orientation. It is established that hydraulic fractures can be forced to propagate in desired directions if advantage is taken of the stress shadow effect in combination with knowledge of rock mass homogeneity and site far field stress conditions. Both the differential stresses between sigma(2) and sigma(3) and between sigma(1) and sigma(3) affect the hydraulic fracture re-orientation geometry. The minimum far field stress magnitude has no direct impact on hydraulic fracture re-orientation. Rock mass homogeneity significantly influences how far a hydraulic fracture propagates along its predefined orientation from its initiation point before re-orientation.