A fully coupled model for predicting geomechanical and multiphase flow behaviour in fractured rocks

Haval Kukha Hawez , Taimoor Asim , Marco Fazio
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Abstract

Geomechanical and multiphase flow characteristics are essential in recovering oil from naturally fractured rocks during hydrocarbon production because of changes in pore pressure and tension within the rock. It is a well-established fact that the geomechanical and multiphase flow characteristics of fractured rocks are interdependent on each other. Evaluation of these characteristics, for hydrocarbons displaced by water in fractured rocks under external stress loading, is severely lacking in published literature. This study aims to develop a novel numerical framework for a fully coupled model of fractured rocks, taking into consideration the pore pressure and porous media discontinuity at the fracture-matrix interface, along with an expanded Darcy's equation. The fully coupled Finite Element Method (FEM) and Computational Fluid Dynamics (CFD) model developed in this study is shown to accurately predict geomechanical and multiphase flow behaviour at the fracture-matrix interface. The results show that as external stress loading on the fractured rock increases, the porosity and permeability of the rock matrix decrease, capillary pressure at the fracture-matrix interface decreases, and the relative permeability curves shift to the right, indicating a water-soaked fracture-matrix interface. The findings of this study can be used to develop innovative strategies for enhanced oil recovery from fractured rocks.

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预测断裂岩石中地质力学和多相流行为的完全耦合模型
在碳氢化合物生产过程中,由于岩石内部孔隙压力和张力的变化,地质力学和多相流特性对于从天然断裂岩石中采油至关重要。一个公认的事实是,断裂岩石的地质力学和多相流特性是相互依存的。在已发表的文献中,严重缺乏对外部应力加载下断裂岩石中被水置换的碳氢化合物的这些特征的评估。本研究旨在为裂隙岩的全耦合模型开发一种新的数值框架,考虑到裂隙-基质界面上的孔隙压力和多孔介质不连续性,以及扩展的达西方程。该研究开发的有限元法(FEM)和计算流体动力学(CFD)全耦合模型能够准确预测断裂-基质界面的地质力学和多相流行为。结果表明,随着断裂岩石上的外应力负荷增加,岩石基质的孔隙度和渗透率降低,断裂基质界面上的毛细管压力减小,相对渗透率曲线向右移动,表明断裂基质界面被水浸泡。这项研究的结果可用于开发创新战略,提高裂缝岩石的石油采收率。
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