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A novel multi-rate dual-porosity model for improved simulation of fractured and multi-porosity reservoirs

机译:一种新型多速率双孔隙度模型,用于改进裂缝和多孔隙储层模拟

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A major part of the world’s remaining oil reserves is located in fractured carbonate reservoirs, which are dual-porosity (fracture-matrix) or multi-porosity (fracture-vug-matrix) in nature. Fractured reservoirs suffer from poor recovery, high water cut, and generally low performance. They are modelled using a dual-porosity approach, which assumes that the high-permeability fractures are mobile and low-permeability matrix is immobile. A single transfer function models the rate at which hydrocarbons migrate from the matrix into the fractures. As shown in many numerical, laboratory, and field experiments, a wide range of transfer rates occurs between the immobile matrix and mobile fractures. These arise, for example, from the different size of matrix blocks (yielding a distribution of shape factors), different porosity types, or the inhomogeneous distribution of saturations in the matrix blocks. Accurate models are hence needed that capture all the transfer rates between immobile matrix and mobile fracture domains, particularly to predict late-time recovery more reliably when the water cut is already high. In this work we propose a novel multi-rate mass transfer model for two-phase flow, which accounts for viscous dominated flow in the fracture domain and capillary flow in the matrix domain. It extends the classical (i.e., single-rate) dual-porosity model in that it allows us to simulate the wide range of transfer rates occurring in naturally fractured multi-porosity rocks. Using numerical simulations of water-flooding in naturally fractured rock masses at the grid-block scale we demonstrate that our multi-rate mass-transfer model matches the observed recovery curves more accurately compared to the classical dual-porosity model. We further discuss how tracer tests can be used to calibrate our multi-rate dual-porosity model before the water-flood commences and how our model could be employed in commercial reservoir simulation workflows.
机译:世界上剩余的石油储量的主要部分位于骨折碳酸盐储层中,其是自然界的双孔隙率(骨折 - 基质)或多孔隙率(骨折 - Vug-Matrix)。裂缝储层遭受较差的恢复,高污水率,以及一般低的性能。它们使用双孔隙率接近进行建模,这假设高渗透性裂缝是移动的,并且低渗透性基质是不动的。单个传递函数模拟碳氢化合物从基质迁移到骨折中的速率。如在许多数值,实验室和现场实验中所示,在固定基质和移动骨折之间发生宽范围的转移率。这些例如从基质块的不同尺寸(产生形状因子分布),不同的孔隙率类型或饱于饱和度的不均匀分布。因此,需要精确的模型,以捕获固定矩阵和移动骨折结构域之间的所有传输速率,特别是当水切割已经高时更可靠地预测后期恢复。在这项工作中,我们提出了一种用于两相流量的新型多速率传质模型,其考虑了裂缝结构域和基质结构域中的毛细血管流动的粘性主导流动。它延伸了经典(即单速率)双孔隙度模型,因为它允许我们模拟在天然断裂多孔隙岩石中发生的广泛的传输速率。在网格块标度下使用自然裂缝岩体中水洪水的数值模拟,我们证明我们的多速率传感模型与经典双孔隙度模型相比更准确地匹配观察到的恢复曲线。我们进一步讨论了如何使用示踪剂测试,以便在水洪开始之前校准我们的多速率双孔隙度模型以及我们的模型如何在商业储层模拟工作流程中使用。

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