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多孔介质中两相和三相流的三维混合湿润随机孔隙尺度网络建模。I. 模型描述。

Three-dimensional mixed-wet random pore-scale network modeling of two- and three-phase flow in porous media. I. Model description.

作者信息

Piri Mohammad, Blunt Martin J

机构信息

Department of Earth Science and Engineering, Imperial College, London SW7 2AZ, United Kingdom.

出版信息

Phys Rev E Stat Nonlin Soft Matter Phys. 2005 Feb;71(2 Pt 2):026301. doi: 10.1103/PhysRevE.71.026301. Epub 2005 Feb 4.

Abstract

We present a three-dimensional network model to simulate two- and three-phase capillary dominated processes at the pore level. The displacement mechanisms incorporated in the model are based on the physics of multiphase flow observed in micromodel experiments. All the important features of immiscible fluid flow at the pore scale, such as wetting layers, spreading layers of the intermediate-wet phase, hysteresis, and wettability alteration are implemented in the model. Wettability alteration allows any values for the advancing and receding oil-water, gas-water, and gas-oil contact angles to be assigned. Multiple phases can be present in each pore or throat (element), in wetting and spreading layers, as well as occupying the center of the pore space. In all, some 30 different generic fluid configurations for two- and three-phase flow are analyzed. Double displacement and layer formation are implemented as well as direct two-phase displacement and layer collapse events. Every element has a circular, square, or triangular cross section. A random network that represents the pore space in Berea sandstone is used in this study. The model computes relative permeabilities, saturation paths, and capillary pressures for any displacement sequence. A methodology to track a given three-phase saturation path is presented that enables us to compare predicted and measured relative permeabilities on a point-by-point basis. A robust displacement-based clustering algorithm is also presented.

摘要

我们提出了一种三维网络模型,用于在孔隙尺度上模拟两相和三相毛细管主导的过程。该模型中纳入的驱替机制基于在微观模型实验中观察到的多相流物理原理。孔隙尺度上不混溶流体流动的所有重要特征,如润湿层、中间润湿相的铺展层、滞后现象和润湿性改变,都在模型中得以实现。润湿性改变允许指定前进和后退的油水、气水和气油接触角的任意值。每个孔隙或喉道(单元)中都可以存在多个相,存在于润湿层和铺展层中,也占据孔隙空间的中心。总共分析了约30种不同的两相和三相流通用流体构型。实现了双重驱替和层形成,以及直接的两相驱替和层坍塌事件。每个单元都有圆形、方形或三角形横截面。本研究使用了一个代表 Berea 砂岩孔隙空间的随机网络。该模型可计算任何驱替序列的相对渗透率、饱和度路径和毛细管压力。提出了一种追踪给定三相饱和度路径的方法,使我们能够逐点比较预测和测量的相对渗透率。还提出了一种基于驱替的稳健聚类算法。

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