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NUMERICAL MODELING OF HYDRAULIC FRACTURE PROPAGATION FROM HORIZONTAL WELLS IN ANISOTROPIC SHALE

机译:各向异性井水平井液压断裂繁殖的数值模拟

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The purpose of this paper is to study the growth of hydraulic fractures in anisotropic rocks such as shale. The boundary value problems of anisotropic materials often are difficult to solve due to the mathematical complexity, therefore such problems are treated numerically under the assumption of isotropy even though such assumption rarely holds in reality. This paper uses the constant element anisotropic displacement discontinuity method (ADDM) for fracture deformation with square root elements at crack tips to calculate stress intensity factors accurately. 3D correction factor G is also developed for anisotropic DDM to include height effect in 2D problems using the analytical solution for stress distribution around a line crack in orthotropic material. The crack propagation is modeled according to the normal stress ratio criterion which accounts elliptically varying fracture toughness while calculating crack trajectory. Crack extension occurs when mode-1 stress intensity factor at tips reaches a critical value K_(IC) (Φ). The fracture deformation is fully coupled with fluid flow inside the fracture by solving all the unknowns simultaneously using globally convergent Newton-Raphson method. The simulation results show significant difference in fracture geometries and apertures between isotropic and anisotropic materials. In anisotropic rock, the direction of plane of elastic symmetry w.r.t fracture influences the fracture geometry. Simulations of multi-stage single lateral fracturing, multi-lateral zipper fracturing in anisotropic shale are included.
机译:本文的目的是研究诸如页岩等各向异性岩石中液压骨折的生长。由于数学复杂性,各向异性材料的边值问题通常难以解决,因此在各向同性的假设下,这些问题也在数值上进行处理,即使这种假设很少存在于现实。本文采用恒定元素各向异性位移不连续方法(ADDM)在裂缝尖端处用方形根元素进行断裂变形,以准确计算应力强度因子。 3D校正因子G还开发用于各向异性DDM,包括使用分析溶液在正交材料中的线裂纹周围的应力分布中的2D问题中的高度效应。根据正常应力比标准进行建模裂纹传播,其在计算裂纹轨迹时忽略椭圆形裂缝韧性。当尖端的模式-1应力强度因子达到临界值K_(IC)(φ)时,会发生裂缝延伸。通过同时使用全球会聚的牛顿 - Raphson方法,通过解决所有未知,与骨折内部的裂缝变形完全耦合。仿真结果显示出各向同性和各向异性材料之间的断裂几何形状和孔的显着差异。在各向异性岩石中,弹性对称的平面方向W.R.T断裂影响断裂几何形状。包括多级单侧压裂的模拟,各向异性页岩中的多侧拉链压裂。

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