Fracture Propagation Behavior of Jointed Rocks in Hydraulic Fracturing

Jointed rocks are typical examples of heterogeneous materials with joints. The existence of joints influences the physical properties of rock mass and propagation of fractures, which can affect production operations in engineering. A series of simulations is performed to understand the failure patte...

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Main Authors: Xiaoxi Men, Jiren Li, Zhihui Han
Format: Article
Language:English
Published: Hindawi Limited 2018-01-01
Series:Advances in Materials Science and Engineering
Online Access:http://dx.doi.org/10.1155/2018/9461284
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spelling doaj-61532c4e259a4adab2ea5ebc6555a8042020-11-25T01:58:31ZengHindawi LimitedAdvances in Materials Science and Engineering1687-84341687-84422018-01-01201810.1155/2018/94612849461284Fracture Propagation Behavior of Jointed Rocks in Hydraulic FracturingXiaoxi Men0Jiren Li1Zhihui Han2College of Civil Engineering, University of Science and Technology Liaoning, An Shan 114051, ChinaCollege of Civil Engineering, University of Science and Technology Liaoning, An Shan 114051, ChinaACRE Coking and Refractory Engineering Consulting Corporation, MCC, Dalian 116085, ChinaJointed rocks are typical examples of heterogeneous materials with joints. The existence of joints influences the physical properties of rock mass and propagation of fractures, which can affect production operations in engineering. A series of simulations is performed to understand the failure patterns and fracture propagation behavior of jointed rocks in hydraulic fracturing. Three points, that is, dip-angle joint, joint strength, and complex joints, are considered in the simulations. Results demonstrate three basic kinds of hydraulic fractures on jointed rock, namely, along the joint, across the joint, and partly along the joint and partly across the joint. The maximum principal stress is the control factor of fracture propagation in global scale, and the joint plane is the control factor of fracture propagation in local scale. In the propagation path, when the dip angle is small or the joint is weak, the fracture propagates along the joint; otherwise, the fracture propagates across the joint. In the multijoint interconnection models, hydraulic fractures propagate along joints in the tensile stress regions near the propagating fracture tip without dip angle limitation. Subsequently, the fractures connect with one another to form a complex fracture network based on the joint morphology.http://dx.doi.org/10.1155/2018/9461284
collection DOAJ
language English
format Article
sources DOAJ
author Xiaoxi Men
Jiren Li
Zhihui Han
spellingShingle Xiaoxi Men
Jiren Li
Zhihui Han
Fracture Propagation Behavior of Jointed Rocks in Hydraulic Fracturing
Advances in Materials Science and Engineering
author_facet Xiaoxi Men
Jiren Li
Zhihui Han
author_sort Xiaoxi Men
title Fracture Propagation Behavior of Jointed Rocks in Hydraulic Fracturing
title_short Fracture Propagation Behavior of Jointed Rocks in Hydraulic Fracturing
title_full Fracture Propagation Behavior of Jointed Rocks in Hydraulic Fracturing
title_fullStr Fracture Propagation Behavior of Jointed Rocks in Hydraulic Fracturing
title_full_unstemmed Fracture Propagation Behavior of Jointed Rocks in Hydraulic Fracturing
title_sort fracture propagation behavior of jointed rocks in hydraulic fracturing
publisher Hindawi Limited
series Advances in Materials Science and Engineering
issn 1687-8434
1687-8442
publishDate 2018-01-01
description Jointed rocks are typical examples of heterogeneous materials with joints. The existence of joints influences the physical properties of rock mass and propagation of fractures, which can affect production operations in engineering. A series of simulations is performed to understand the failure patterns and fracture propagation behavior of jointed rocks in hydraulic fracturing. Three points, that is, dip-angle joint, joint strength, and complex joints, are considered in the simulations. Results demonstrate three basic kinds of hydraulic fractures on jointed rock, namely, along the joint, across the joint, and partly along the joint and partly across the joint. The maximum principal stress is the control factor of fracture propagation in global scale, and the joint plane is the control factor of fracture propagation in local scale. In the propagation path, when the dip angle is small or the joint is weak, the fracture propagates along the joint; otherwise, the fracture propagates across the joint. In the multijoint interconnection models, hydraulic fractures propagate along joints in the tensile stress regions near the propagating fracture tip without dip angle limitation. Subsequently, the fractures connect with one another to form a complex fracture network based on the joint morphology.
url http://dx.doi.org/10.1155/2018/9461284
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