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Fully coupled hydromechanical flow simulation of water-induced dynamic fractures in low-permeability reservoirs

机译:低渗透油藏水诱导动态骨折的完全耦合水力力学模拟

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Water-induced dynamic fractures are the new features affecting the reservoir heterogeneity in low-permeability reservoirs. Due to the high injection pressure, water-induced fractures will generate and propagate when the formation pressure exceeds fracturing pressure during water-flood of low-permeability reservoirs. Based on field production data and water-flood behavior analysis in low-permeability reservoirs, propagation mechanism of dynamic fractures is identified and the relationship between fracture aperture and permeability variation with normal and shear stresses is derived. We developed a dynamic fracture model that implicitly coupled fluid flow with the stresses induced by fracture deformation. A crossing criterion is implemented that predicts whether propagating dynamic fracture will cross natural fractures or terminate against them. With dual porosity model, the dynamic fracture model is fully coupled with the fluid flow in matrix and fractures. Simulations were performed of a single propagating fracture to validate the model against classical analytical solutions based on PKN model. Numerical simulation results show that formation pressure controls matrix rock deformation and creation, opening, propagation and closure of dynamic fractures. Unlike the former studies which mainly focus on the normal stress, the study in this paper found that shear stimulation also plays an important role in controlling fracture aperture and permeability. Dynamic fractures increase heterogeneity in low-permeability reservoirs so they significantly affect residual oil distribution after water-flood. The sweep efficiency and ultimate oil recovery can be increased by controlling injection pressure and the range of hydraulic fracturing and optimizing the match between well pattern and dynamic fracture orientation.
机译:水诱导的动态骨折是影响低渗透储层中储层异质性的新特征。由于高注射压力,当在低渗透储层的水洪水洪水期间形成压力超过压裂压力时,水诱导的骨折会产生和传播。基于低渗透储存器的现场生产数据和水洪行为分析,鉴定了动态骨折的传播机制,衍生裂缝孔径与正常和剪切应力的渗透变化之间的关系。我们开发了一种动态骨折模型,其隐含地耦合流体流,裂缝变形引起的应力。实施交叉标准,其预测传播动态骨折是否会交叉自然骨折或终止于它们。具有双孔隙率模型,动态断裂模型与基质和裂缝中的流体流完全耦合。对单一传播骨折进行仿真,以验证基于PKN模型的经典分析解决方案模型。数值仿真结果表明,形成压力控制矩阵岩石变形和创造,打开,传播和闭合动态裂缝。与主要关注正常应激的前一项研究不同,本文的研究发现,剪切刺激也在控制骨折孔径和渗透性方面发挥着重要作用。动态骨折增加了低渗透储层中的异质性,因此它们在洪水后显着影响残留的油分布。通过控制注射压力和液压压裂范围和优化井图案和动态断裂取向之间的匹配,可以增加扫描效率和终极性恢复。

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