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An Interesting Look at Multiple Fractures: Stress Shadowing andPropagation

机译:一个有趣的看起来多重骨折:压力阴影和提高

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The objectives of this paper are twofold.First to evaluate the extent,or shadowing,of the stresses anddisplacements resulting from an internally pressurized crack and second to show how a creative testingapparatus can model the interaction of multiple fractures and display the influence of stress shadowing.The solution for 2-D planar crack in elliptical-cylindrical coordinates was used to evaluate the stressand displacement shadowing.This analysis indicated that the compressive stresses for a pressurized crackof length H,will dissipate by 100% within a distance d/H = 3/4.The analysis also showed that the shearstresses and displacements are concentrated in a small area around the crack tip of radial distance equalto d/H = 0.05.H is crack length and d is distance from the crack.Following this analysis,the mechanicalapparatus was used to visualize the influence of the stress and displacement shadows in the propagationof multiple fractures.The example that validated the application of the apparatus consisted of modeling the merging of twofractures observed in the 2017 Puebla,Mexico earthquake.In this case,both the testing apparatus andthe numerical results given by a two dimensional Finite Element(FE)code closely reproduced the fieldobservations.Following this validation,the application of the testing apparatus was extended to model thepropagation and interaction of multiple fractures.Three cases were considered.Case 1,consisted of a mainfracture propagating between pre-existing fracture-pockets filled with fluid(pressurized pockets).Case 2,included the propagation of multiple parallel fractures.Case 3,considered hydraulic fractures propagatingthrough zones populated with micro-fissures.Case 1,showed how a hydraulic fracture can activate and propagate pre-existing frac-pockets.Thisexample could explain how some frac-hits occur.Case 2,illustrated that from a cluster of several parallelfractures that are close to each other(D/H < 1),only one or two dominant fractures will propagate.D isdistance between parallel fractures.The experimental results for Case 3 indicated that the micro-fissuresdiverted the direction of fracture propagation and also increased the tortuosity.The extent of departure anddegree of tortuosity depended on the orientation of the micro-fissures.Micro-fissures normal to the crackresulted in more diversion and more tortuosity compared to the diversion and tortuosity resulting frommicro-fissures parallel to the crack.Further the tests also showed that the micro-fissures not aligned withthe fracture also suffered significant dilation.
机译:本文的目标是twofold.First评估的范围内,或遮蔽从内部加压裂纹产生的应力anddisplacements的,和第二显示一个创造性的testingapparatus如何建模多个裂缝的相互作用,并显示应力遮蔽的影响。在椭圆圆柱坐标系2-d平面裂纹将溶液用于评价应激和位移shadowing.This分析表明,对于加压crackof长度H中的压缩应力,将通过100%的距离d内消散/ H = 3 / 4.分析还表明,shearstresses和位移都集中在围绕径向距离的裂纹尖端的小区域equalto d / H = 0.05.H是裂纹长度,d是从crack.Following该分析,mechanicalapparatus是距离用于可视化在propagationof多个fractures.The示例的应力和位移的阴影的影响,审定的申请装置由在2017布拉,墨西哥earthquake.In这种情况下观察到的twofractures的合并建模的,无论是测试装置由二维有限元(FE)代码以及所述给定的数值结果密切再现的fieldobservations.Following此验证,应用程序的测试装置被扩展到多个fractures.Three例considered.Case 1模型thepropagation和相互作用,包括一个mainfracture填充有流体(加压袋)预先存在的断裂的口袋之间传播。病例2的,包含的传播多个并行fractures.Case 3,考虑水力裂缝propagatingthrough填充micro-fissures.Case 1区,显示出水力压裂可如何激活和预先存在的繁殖压裂pockets.Thisexample可以解释一些压裂命中如何occur.Case 2,示出的是从几个parallelfractures是彼此接近的(d / H <1)中,只有一个或两个主导性骨折将集群对于情况3平行fractures.The实验结果之间propagate.D isdistance表明微fissuresdiverted断裂传播方向并且还增加了扭曲的出发anddegree的tortuosity.The程度依赖于的取向微fissures.Micro-裂缝垂直于crackresulted在更导流多迂曲相比的转移和扭曲所得frommicro-裂缝平行于crack.Further测试还表明,微裂缝不对齐的任意不等阶骨折也遭受显著扩张。

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