宋永臣

个人信息Personal Information

教授

博士生导师

硕士生导师

性别:男

毕业院校:大连理工大学

学位:博士

所在单位:能源与动力学院

学科:能源与环境工程

办公地点:能动大楼810

联系方式:songyc@dlut.edu.cn

电子邮箱:songyc@dlut.edu.cn

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A visualization study on two-phase gravity drainage in porous media by using magnetic resonance imaging

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论文类型:期刊论文

发表时间:2016-09-01

发表刊物:MAGNETIC RESONANCE IMAGING

收录刊物:SCIE、PubMed、Scopus

卷号:34

期号:7

页面范围:855-863

ISSN号:0730-725X

关键字:Wettability; Displacement front velocity; Gravity number; Capillary number; Bond number; Displacing-phase saturation

摘要:Gravity drainage characteristics are important to improve our understanding of gas-liquid or liquid-liquid two-phase flow in porous media. Stable or unstable displacement fronts that controlled by the capillary force, viscous force, gravitational force, etc., are relevant features of immiscible two-phase flow. In this paper, three dimensionless parameters, namely, the gravity number, the capillary number and the Bond number, were used to describe the effect of the above mentioned forces on two-phase drainage features, including the displacement front and final displacing-phase saturation. A series of experiments on the downward displacement of a viscous fluid by a less viscous fluid in a vertical vessel that is filled with quartz beads are performed by using magnetic resonance imaging (MRI). The experimental results indicate that the wetting properties at both high and low capillary numbers exert remarkable control on the fluid displacement. When the contact angle is lower than 90 degrees, i.e., the displaced phase is the wetting phase, the average velocity V-f of the interface of the two phases (displacement front velocity) is observably lower than when the displaced phase is the non-wetting phase (contact angle higher than 90 degrees). The results show that a fingering phenomenon occurs when the gravity number G is less than the critical gravity number G' = Delta mu/mu(g). Moreover, the higher Bond number results in higher final displacing-phase saturation, whereas the capillary number has an opposite effect. (C) 2016 Elsevier Inc. All rights reserved.