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两相流中二元气体相互作用的改进渗透率模型及其在CO强化煤层气开采中的应用

Improved Permeability Model of the Binary Gas Interaction within a Two-Phase Flow and its Application in CO-Enhanced Coalbed Methane Recovery.

作者信息

Wang Gang, Xu Feng, Xiao Zhiyong, Zhang Lu, Jiang Yujing, Jiang Feng, Zheng Chengcheng

机构信息

Shandong Provincial Key Laboratory of Civil Engineering Disaster Prevention and Mitigation, Shandong University of Science and Technology, Qingdao 266590, China.

College of Civil Engineering, Fujian University of Technology, Fuzhou 350118, China.

出版信息

ACS Omega. 2022 Aug 25;7(35):31167-31182. doi: 10.1021/acsomega.2c03377. eCollection 2022 Sep 6.

Abstract

In this paper, we develop a dual-porosity dual-permeability model for binary gas migration to explore the permeability evolution in the matrix and fracture in the process of a gas-water two-phase flow during CO-enhanced coalbed methane (CO-ECBM) recovery in coal reservoirs. This mechanistic model accommodates the effects of elastic deformation caused by the effective stress change in the matrix and fracture, the swelling/shrinkage deformation of the matrix caused by adsorption/desorption, the convection and diffusion of gas, and the discharge of water. Specifically, the time-dependent matrix swelling, from initially completely reducing the fracture aperture to finally affecting the coal bulk volume, is considered by the invaded volume fraction involving binary gas intrusion. The model is validated through laboratory data and applied to examine the permeability evolution of CO-ECBM recovery for 10 000 days. Furthermore, we analyze the sensitivity of some selected initial parameters to capture the key factors affecting CO-ECBM recovery. Our modeling results show that the permeability evolution can be divided into two stages during the process, where stage I is dominated by effective stress and stage II is dominated by adsorption/desorption. Increasing the injection pressure or initial permeability advances the start of stage II. The decrease in initial water saturation causes the permeability to change more drastically and the time of stage II to appear earlier until a time long enough, after which little effect is seen on the permeability results.

摘要

在本文中,我们开发了一种用于二元气体运移的双孔隙度双渗透率模型,以探究煤层气藏中CO2强化煤层气(CO2-ECBM)开采过程中气水两相流期间基质和裂缝渗透率的演化。该机理模型考虑了基质和裂缝中有效应力变化引起的弹性变形、吸附/解吸引起的基质膨胀/收缩变形、气体的对流和扩散以及水的排出等影响。具体而言,通过涉及二元气体侵入的侵入体积分数来考虑随时间变化的基质膨胀,这种膨胀最初会完全减小裂缝孔径,最终影响煤的总体积。该模型通过实验室数据进行了验证,并应用于考察10000天的CO2-ECBM开采过程中的渗透率演化。此外,我们分析了一些选定初始参数的敏感性,以捕捉影响CO2-ECBM开采的关键因素。我们的模拟结果表明,在此过程中渗透率演化可分为两个阶段,其中阶段I以有效应力为主导,阶段II以吸附/解吸为主导。提高注入压力或初始渗透率会使阶段II提前开始。初始含水饱和度的降低会导致渗透率变化更为剧烈,阶段II出现的时间更早,直到时间足够长后,对渗透率结果的影响才会减小。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8a4b/9453950/f59bfc448ba5/ao2c03377_0002.jpg

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