天然裂缝介质中两相流体流动的全耦合THM配方

Yarlong Wang
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引用次数: 0

摘要

基于双孔隙度模型,建立了一个耦合公式,用于模拟非等温两相流体流动条件下的天然裂缝含水层。研究了双孔隙型介质中变形耦合的两相流,以及两流体相之间和两多孔固相之间能量传递的非局部平衡条件。沿着和通过它们,导电和对流机制可能占主导地位。更重要的是,不同的物理参数反映了不同的岩石类型,并定义和解释了裂缝特征,从而可以表示相应的岩石行为。模型和物理解释发展和提出了不同的研究人员进行了回顾和比较。该模型适用于两相渗流天然裂缝储层模拟、注固co2安全设计、油气储层注入能力评价、采热设计等。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fully Coupled THM Formulations with two-phase fluid flow in naturally fractured media
A coupled formulation is developed, based on a dual-porosity model to simulate a naturally fractured aquifer under non-isothermal and two-phase fluid flow conditions.  Two-phase flow coupled to the deformation in a dual-porosity type media, and non-local equilibrium conditions are imposed for the energy transport between and among, respectively, two fluid and porous solid phases. Along and through them conductive and convective mechanisms may dominate. More importantly different physical parameters reflect different rock types and fracture characteristics are defined and interpreted so that the corresponding rock behaviors may be represented. Models and physical interpretations developed and proposed by different researchers are reviewed and compared. The model is applicable in reservoir simulation of naturally fractured formations with two-phase fluid flow,  safety design of co2 injection and sequestration, oil/gas storage injectivity or capacity evaluation, and heat extraction design in geothermal reservoir.
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