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CO2 Mobility and Transitions between Co-Current and Counter-Current Flows

机译:CO2流动性和同频和反电流流动之间的过渡

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In this work, we study the modeling of CO2 migration/mobility in two-phase displacements of relevance to sequestration processes in saline aquifers. The main focus of this paper is on accurate modeling and robust numerical implementation of transitions between co-current and counter-current flows in fully implicit simulation of multiphase flow. Several experimental and modeling studies have demonstrated that relative permeability decreases when multiphase flow transitions from co-current to counter-current settings in strongly water-wet porous materials. However, the associated implications in the context of CO2 sequestration design and optimization have not yet been studied or implemented in commonly available reservoir simulation tools. In this study, the relative permeability of each phase is considered to be flow dependent, and a continuous transition between co-current and counter-current relative permeability functions (including hysteresis) has been implemented and tested in a fully implicit reservoir simulator. The transition is represented as a scanning loop between the bounding co- and counter-current relative permeability functions. This allows us to gauge the impact of transitions from co-current to counter- current flow on the vertical movement of CO2 and its impact on sweep efficiency, plume migration and entrapment in sequestration process. Our formulation/implementation of flow dependent relative permeability functions is demonstrated to maintain the numerical stability of conventional fully implicit schemes. However, the total simulation time increases slightly because of the decrease in the vertical mobility and the associated increased travel distance prior to full phase segregation. Furthermore, the footprint of CO2 in the top layers of a reservoir, as predicted by traditional and by our new approach, is shown to be quite different. The results and analysis presented in this paper demonstrate that it is necessary to consider/integrate this effect in numerical calculations whenever transitions between co-current and counter-current flow may occur.
机译:在这项工作中,我们研究了与盐水含水层中螯合过程相关的两相位移中的二氧化碳迁移/移动性的建模。本文的主要重点是在完全隐含多相流模拟中的电流和反电流流动之间的转换的精确建模和稳健的数值实现。几种实验和建模研究已经证明,当多相流动从电流转变为强水湿多孔材料中的逆流设置时相对渗透率降低。然而,尚未在常用的储存器模拟工具中研究或实施在CO2隔离设计和优化的上下文中的相关意义。在该研究中,认为每个相的相对渗透性被认为是依赖性的,并且在完全隐含的储存器模拟器中已经实现和测试了相同电流和逆流相对渗透功能(包括滞后)之间的连续转变。转换表示为边界的共同和反电流相对渗透功能之间的扫描环路。这使我们能够衡量转变从电流的影响到CO2的垂直运动对逆流流动及其对扫描效率的影响,羽流迁移和夹紧在螯合过程中。我们的配方/实施流动依赖性相对渗透功能是为了维持传统完全隐含方案的数值稳定性。然而,由于在全相分离之前垂直移动性和相关的增加的行驶距离,总模拟时间略微增加。此外,如传统和新方法所预测的那样,储层顶层中的CO2的占地面积显示出很大。本文提出的结果和分析表明,只要电流与逆流流程之间的转换,有必要在数值计算中考虑/整合这种效果。

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