Hydraulic Fracturing In Unconventional Reservoirs: The Impact of Layering and Permeable Frictional Interfaces

G. Qian, Ghassemi Ahmad
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Abstract

The hydraulic fracture containment and the impact of layering on pumping energy are critical factors in a successful stimulation treatment. Height confinement is needed to ensure effective stimulation of target zones and to maintain the fractures in the target zones. Also, the existence of beds with different ductility can impact the net pressure and pumping requirements. Layered rock properties, in-situ stress, and formations interfaces influence the lateral and height growth of hydraulic fractures. Conventionally, it is considered that the in-situ stress is the dominant factor controlling the fracture height. The influence of mechanical properties on fracture height growth is often ignored or is limited to consideration of different Young's modulus. Also, it is commonly assumed that the interfaces between different layers are perfectly bounded without slippage, and interface permeability is not considered. In-situ experiments have demonstrated that variation of modulus and in-situ stress alone cannot explain the containment of hydraulic fractures observed in field (SPE39950). Enhanced toughness, in-situ stress, interface slip and energy dissipation in the layered rocks should be combined to contribute to the fracture containment. In this study, we consider these factors in a fully coupled 3D hydraulic fracture simulator developed based on finite element method. We use laboratory and numerical simulations to investigate the above factors and how they impact hydraulic fracture propagation, height growth, and injection pressure. In this work a 3D fully coupled hydro-mechanical model is developed and utilized. The model uses a special zero-thickness interface element and the cohesive zone model (CZM) to model fracture propagation, interface slippage, and fluid flow in fractures. The nonlinear mechanical behavior of frictional sliding along interface surfaces is considered. The hydro-mechanical model has been successfully verified through benchmarked analytical solutions. The influence of layered Young's modulus on fracture height growth in layered formations is analyzed. The formation interfaces between different layers are explicitly simulated through the usage of the hydro-mechanical interface element. The impacts of mechanical and hydraulic properties of the formation interfaces on preventing hydraulic fracture growth are studied. Hydraulic fractures tend to propagate in the layer with lower Young's modulus so that soft layers could potentially act as barriers to limit the height growth of hydraulic fractures. Depending on the mechanical properties and the conductivity of the interfaces, the shear-slippage and/or opening along the formation interfaces could result in flow along the interface surfaces and terminate the fracture growth. The frictional slippage along the interfaces could be an effective mechanism that contributes to the containment of hydraulic fractures in layered formations. It is suggested that whether a hydraulic fracture would cross a discontinuity depends not only on the mechanical properties but also on the hydraulic properties of the discontinuity; both the frictional slippage and fluid pressure along horizontal formation interfaces contribute to the reinitiation of a hydraulic fracture from a pre-existing flaw along the interfaces, producing an offset from the interception point to the reinitiation point.
非常规油藏水力压裂:分层和渗透摩擦界面的影响
水力裂缝控制和分层对泵送能量的影响是成功增产的关键因素。为了确保目标层的有效增产,并维持目标层的裂缝,需要高度限制。此外,不同延展性地层的存在也会影响净压力和泵送要求。层状岩石性质、地应力和地层界面影响水力裂缝的横向和高度增长。传统上认为地应力是控制裂缝高度的主导因素。力学性能对断裂高度增长的影响往往被忽略或局限于考虑不同的杨氏模量。此外,通常假设不同层之间的界面是完美结合的,没有滑移,并且不考虑界面渗透率。现场试验表明,单靠模量和地应力的变化不能解释现场观察到的水力裂缝的封闭性(SPE39950)。层状岩石的韧性增强、地应力、界面滑移和能量耗散应结合在一起,以促进裂缝的遏制。在本研究中,我们在基于有限元法开发的全耦合三维水力压裂模拟器中考虑了这些因素。我们使用实验室和数值模拟来研究上述因素,以及它们如何影响水力裂缝扩展、高度增长和注入压力。本文建立并应用了三维全耦合流体力学模型。该模型采用特殊的零厚度界面单元和黏合带模型(CZM)来模拟裂缝扩展、界面滑移和裂缝内流体流动。考虑了沿界面表面摩擦滑动的非线性力学行为。流体力学模型已通过基准解析解成功验证。分析了层状地层中层状杨氏模量对裂缝高度增长的影响。利用水-力学界面元,明确模拟了不同层间的地层界面。研究了地层界面力学性能和水力性能对防止水力裂缝扩大的影响。水力裂缝倾向于在杨氏模量较低的地层中扩展,因此软层可能会成为限制水力裂缝高度增长的屏障。根据界面的力学性能和导电性,沿地层界面的剪切滑移和/或张开可能导致沿界面表面的流动并终止裂缝的扩展。在层状地层中,沿界面的摩擦滑移可能是一种有效的机制,有助于封堵水力裂缝。水力裂缝能否跨越不连续面不仅取决于其力学性能,还取决于其水力性能;沿水平地层界面的摩擦滑移和流体压力都有助于沿界面从先前存在的裂缝重新启动水力裂缝,从而产生从拦截点到重新启动点的偏移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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