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Single- and two-phase flow simulation based on equivalent pore network extracted from micro-CT images of sandstone core

机译:基于等效孔隙网络的砂岩岩心微观CT图像提取的单相和两相流模拟

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摘要

Due to the intricate structure of porous rocks, relationships between porosity or saturation and petrophysical transport properties classically used for reservoir evaluation and recovery strategies are either very complex or nonexistent. Thus, the pore network model extracted from the natural porous media is emphasized as a breakthrough to predict the fluid transport properties in the complex micro pore structure. This paper presents a modified method of extracting the equivalent pore network model from the three-dimensional micro computed tomography images based on the maximum ball algorithm. The partition of pore and throat are improved to avoid tremendous memory usage when extracting the equivalent pore network model. The porosity calculated by the extracted pore network model agrees well with the original sandstone sample. Instead of the Poiseuille’s law used in the original work, the Lattice-Boltzmann method is employed to simulate the single- and two- phase flow in the extracted pore network. Good agreements are acquired on relative permeability saturation curves of the simulation against the experiment results.
机译:由于多孔岩石的复杂结构,孔隙度或饱和度与岩石物理输运特性之间的关系通常用于储层评价和采收策略,要么非常复杂要么不存在。因此,强调了从天然多孔介质中提取的孔隙网络模型是预测复杂的微孔结构中流体输运特性的突破。本文提出了一种改进的方法,该方法基于最大球算法从三维计算机断层扫描图像中提取等效孔隙网络模型。在提取等效的孔网络模型时,改善了孔和喉部的分配,以避免大量内存使用。提取的孔隙网络模型计算出的孔隙度与原始砂岩样品非常吻合。 Lattice-Boltzmann方法代替了原始工作中使用的Poiseuille定律,而是模拟了提取的孔隙网络中的单相和两相流动。在模拟相对实验结果的相对渗透率饱和曲线上取得了良好的一致性。

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