Unified Reservoir And Seismic Simulation With Explicit Representation Of Fractures And Faults

Z. Han, G. Ren, R. Younis
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引用次数: 2

Abstract

In the context of remote sensing, the vast disparity in characteristic scales between seismic deformation (e.g. milliseconds) and transient flow (e.g. hours) allows a "two-model paradigm" for geophysics and reservoir simulation. In the context of flow-induced geohazard risk mitigation and micro-seismic data integration, this paradigm breaks down. Under micro-seismic deformation, events occur with high-frequency, and over sustained duration during which the rock-fluid coupling is significant. In risk mitigation scenarios, the onset of seismic deformation is directly tied to quasi-static coupling periods. This work develops an approach to reservoir simulation modeling that allows simultaneous resolution of transient (inertial) poromechanics and multiphase fluid flow in the presence of fracture. A mixed discretization scheme combining the extended finite element method (XFEM) and the embedded discrete fracture model (EDFM) is extended using a second-order implicit Newmark time integration scheme for the inertial mechanics. A Lagrange multiplier method is developed to model pressure-dependent contact traction in fractures. The contact constraints are adapted to accommodate fracture opening. Slip-weakening fracture friction models are incorporated. Finally, a time-step controller is proposed to combine local discretization error with contact traction and slip-rate control along the fractures. This strategy allows automatic adaptation to resolve quasi-static, inter-seismic triggering, and co-seismic spontaneous rupture periods within one model. The model is verified to simulate complete induced earthquake sequences, including inter-seismic and dynamic rupture phases. The performance of the adaptive model is illustrated for cases with various set-ups of production and injection periods in a fractured reservoir with explicit fracture representation.
裂缝和断层明确表示的统一储层和地震模拟
在遥感的背景下,地震变形(例如毫秒)和瞬态流动(例如小时)之间的特征尺度的巨大差异允许地球物理和油藏模拟的“双模型范式”。在流动诱发的地质灾害风险缓解和微地震数据整合的背景下,这种模式被打破了。在微震变形下,事件发生频率高,持续时间长,岩石-流体耦合显著。在风险缓解情景中,地震变形的发生与准静态耦合期直接相关。这项工作开发了一种储层模拟建模方法,可以同时解析裂缝存在时的瞬态(惯性)孔隙力学和多相流体流动。采用二阶隐式Newmark时间积分格式,将扩展有限元法(XFEM)与嵌入式离散断裂模型(EDFM)相结合的混合离散化方案扩展到惯性力学中。建立了拉格朗日乘数法来模拟裂缝中压力相关的接触牵引力。接触约束被调整以适应裂缝开口。引入滑移弱化断裂摩擦模型。最后,提出了一种结合局部离散误差、接触牵引力和沿裂缝滑移率控制的时间步长控制器。该策略允许在一个模型内自动适应解决准静态、地震间触发和同震自发破裂期。经验证,该模型可以模拟完整的诱发地震序列,包括震间阶段和动态破裂阶段。在具有明确裂缝表示的裂缝性油藏中,采用不同的生产和注入周期,说明了自适应模型的性能。
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