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Numerical simulation of hydraulic fracturing in orthotropic formation based on the extended finite element method

机译:基于扩展有限元法的正交各向异性地层水力压裂数值模拟

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Shale shows remarkable anisotropy in terms of mechanical properties, and it can often be regarded as an orthogonal anisotropic linear elastic body. In this paper, we present a two-dimensional fluid-solid coupled numerical model based on the extended finite element method (XFEM) to simulate the propagation of hydraulic fracture in orthotropic formations. The interaction between rock deformation and fluid flow within fracture is taken into account. Special crack tip enrichment functions of XFEM are used to model fractures in orthotropic formations, and the maximum circumferential tensile stress criterion is modified to determine the fracture propagation direction. The simulation results show that the hydraulic fracture will deviate from its straight-ahead path if there is an angle (defined as the material angle) between the initial fracture direction and the material axes of orthotropy. The initial deviation angle of fracture changes with the variation of the material angle, and the extent of fracture deviation increases with the Young's Modulus ratio. The fracture deviation can be avoided only when the initial fracture is parallel to one of the material axes of orthotropy. In the case where the maximum and minimum horizontal stresses are not equal, the direction of fracture propagation is determined by the combined effects of in-situ stress and orthotropy of the material. These findings offer new insights into the hydraulic fracturing design in orthotropic formations, helping to improve the production rates in shale gas reservoirs. (C) 2016 Elsevier B.V. All rights reserved.
机译:页岩在力学性能方面表现出显着的各向异性,通常被认为是正交各向异性的线性弹性体。在本文中,我们提出了基于扩展有限元方法(XFEM)的二维流固耦合数值模型,以模拟正交各向异性地层中水力压裂的扩展。考虑了岩石变形与裂缝内流体流动之间的相互作用。 XFEM的特殊裂纹尖端富集功能用于模拟正交各向异性地层中的裂缝,并修改了最大周向拉应力准则以确定裂缝的传播方向。仿真结果表明,如果初始裂缝方向与正交各向异性材料轴之间存在一个角度(定义为材料角度),则水力裂缝将偏离其直行路径。断裂的初始偏差角随材料角的变化而变化,断裂偏差的程度随杨氏模量比的增加而增加。仅当初始断裂平行于正交各向异性材料轴之一时,才可以避免断裂偏差。在最大和最小水平应力不相等的情况下,断裂扩展的方向由原位应力和材料的正交各向异性共同决定。这些发现为正交各向异性地层的水力压裂设计提供了新的见解,有助于提高页岩气储层的生产率。 (C)2016 Elsevier B.V.保留所有权利。

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