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Simulation of Flow in Discrete Deformable Fractured Porous Media

机译:离散可变形骨折多孔介质流动的模拟

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We investigate the coupled flow/geomechanics behavior of naturally fractured permeable rocks. Model and simulation of these processes is very challenging due to the multi-scale nature of the problems and the strong coupling that exists between flow and mechanical behaviors. We present a numerical procedure for the simulation of two-phase immiscible and compressible flow coupled to mechanical deformation in two-dimensional discrete-fractured porous media. To achive this coupling, we implemented an iterative procedure between the flow and the mechanical deformation simulations in which the fluid pressure in the fracture is used as boundary condition at fracture walls. The deformation problem is solved by discretizing the poroelastic equilibrium equations following a Galerkin Finite Element approach, while the flow part was solved using the discrete fracture control volume method. For the flow simulation fractures are assumed to be n-1 dimensional elements where n is the dimension of the overall problem. We considered continuity in capillary pressure and the implied discontinuityin saturation. The model introduces a coupling between mechanical behavior and flow properties by relating absolute permeabilities to the fracture deformation. This approach allows us to study the effects of the coupling on the oil recoveryin stress sensitive fractured porous media. We present results for the simulation of synthetic cases to illustrate some of the geomechanical effects that mayarise during oil recoveryin fractured reservoirs.
机译:我们研究了天然骨折渗透岩石的耦合流动/地质力学行为。由于问题的多尺度性质和流动行为之间存在的强耦合,这些过程的模型和模拟是非常具有挑战性的。我们提出了一种模拟两相混合和可压缩流动的数值过程,其耦合到二维离散骨折多孔介质中的机械变形。为了实现这种耦合,我们在流动和机械变形模拟之间实现了迭代过程,其中裂缝中的流体压力用作裂缝壁的边界条件。通过离散化伴随有限元接种之后通过离散化的平衡方程来解决变形问题,而使用离散断裂控制体积法解决了流动部分。对于流动模拟裂缝被假设是N-1尺寸元件,其中N是整体问题的尺寸。我们认为毛细管压力的连续性和隐含的不连续性饱和度。该模型通过将绝对渗透率与裂缝变形相关的绝对渗透来引入机械行为和流动性能之间的耦合。这种方法使我们能够研究偶联对油回收率敏感裂缝多孔介质的效果。我们展示了综合案例模拟的结果,以说明在油回收额储层期间莫里斯明的一些地质力学效果。

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