Simulation of hydraulic fracturing in quasi-brittle shale formations using characterized cohesive layer: Stimulation controlling factors

Mahdi Haddad, Kamy Sepehrnoori
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引用次数: 102

Abstract

Economic production from shale gas cannot be achieved by natural mechanisms alone; it requires technologies such as hydraulic fracturing in multiple stages along a horizontal wellbore. Developing numerical models for hydraulic fracturing is essential since a successful fracturing job in a shale formation cannot be generalized to another due to different shale characteristics, and restricted access to the field data acquisition. The cohesive zone model (CZM) identifies the plastic zone and softening effects at the fracture tip in a quasi-brittle rock such as shale, which leads to a more precise fracture geometry and injection pressure compared to those from linear elastic fracture mechanics. The incorporation of CZM in a fully coupled pore pressure–stress, finite element analysis provides a rigorous tool to include also the significant effect of in situ stresses in large matrix deformations on the fracturing fluid flow components, for instance leak-off. In this work, we modeled single and double-stage fracturing in a quasi-brittle shale layer using an improved CZM for porous media besides including the material softening effect and a new boundary condition treatment, using infinite elements connecting the domain of interest to the surrounding rock layers. Due to the lack of experimental data for the cohesive layer properties, we characterized the cohesive layer by sensitivity study on the stiffness, fracture initiation stress, and energy release rate. We demonstrated the significance of rock mechanical properties, pumping rate, viscosity, and leak-off in the pumping pressure, and fracture aperture. Moreover, we concluded that the stress shadowing effects of hydraulic fractures on each other majorly affects not only fractures’ length, height, aperture, and the required injection pressure, but also their connection to the injection spot. Also, we investigated two scenarios in the sequence of fracturing stages, simultaneous and sequential, with various fracture spacing and recommended the best scenario among them.

Abstract Image

基于特征黏结层的准脆性页岩水力压裂模拟:增产控制因素
仅靠自然机制无法实现页岩气的经济生产;它需要一些技术,比如沿水平井筒进行多级水力压裂。开发水力压裂的数值模型至关重要,因为由于页岩的不同特征,成功的压裂作业不能推广到另一个页岩地层,并且限制了现场数据采集的获取。内聚区模型(CZM)识别准脆性岩石(如页岩)裂缝尖端的塑性区和软化效应,与线弹性断裂力学相比,可以获得更精确的裂缝几何形状和注入压力。将CZM整合到完全耦合的孔隙压力-应力有限元分析中,提供了一个严格的工具,还包括大基质变形时的原位应力对压裂液流动成分(例如泄漏)的显著影响。在这项工作中,我们使用改进的多孔介质CZM模型模拟了准脆性页岩层的单段和双段压裂,除了考虑材料软化效应和新的边界条件处理外,还使用无限单元将感兴趣的域连接到围岩。由于缺乏关于黏结层性能的实验数据,我们通过对黏结层刚度、断裂起裂应力和能量释放率的敏感性研究来表征黏结层。我们证明了岩石力学特性、泵送速率、粘度和泄漏对泵送压力和裂缝孔径的重要性。水力裂缝之间的应力阴影效应不仅影响裂缝的长度、高度、孔径和所需的注入压力,还影响裂缝与注入点的连接。此外,我们还研究了同时压裂和顺序压裂两种不同裂缝间距的压裂方案,并推荐了其中的最佳方案。
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