Quantitative Visualization of Two‐Phase Flow in a Fractured Porous Medium

Author:

Liao Zhen123ORCID,Detwiler Russell L.4ORCID,Cookson Esther S.4ORCID,Lei Wanjun12,Chen Yi‐Feng12ORCID

Affiliation:

1. State Key Laboratory of Water Resources Engineering and Management Wuhan University Wuhan China

2. Key Laboratory of Rock Mechanics in Hydraulic Structural Engineering of the Ministry of Education Wuhan University Wuhan China

3. Yajiang Clean Energy Science and Technology Research (Beijing) Corporation Limited Beijing China

4. Department of Civil and Environmental Engineering University of California Irvine Irvine CA USA

Abstract

AbstractTwo‐phase fluid flow in fractured porous media impacts many natural and industrial processes but our understanding of flow dynamics in these systems is constrained by difficulties measuring the exchange of water between fracture and adjacent porous matrix. We present a novel experimental system that allows quantitative visualization of the air and water phases in a single analog fractured porous medium. The fracture system consists of a sintered‐glass porous plate in contact with an impermeable glass plate. A reservoir connected to the porous plate allows control of pore pressure within the porous medium. The fracture fills and drains through the porous matrix and flow manifolds along two edges of the fracture. The fracture is mounted in an imaging system that includes a controlled light‐emitting diode panel and a charge‐coupled‐device camera. Flow and pressure are controlled and monitored by a computer during experiments. To demonstrate this system, we carried out a series of cyclic drainage and imbibition experiments in fractures bounded by porous media with different pore‐size distributions in the porous matrix. Images of the drainage process demonstrate that the air‐water distribution within the fracture evolves differently than has been observed in non‐porous fractured systems. Specifically, we observed limited trapping of water within the fracture during drainage. Conversely, during imbibition, because air cannot exit through the porous matrix, significant regions of air became entrapped once pathways to the fracture boundaries became water filled. The differences in phase evolution led to substantial differences in the evolution of estimated relative permeability with saturation.

Publisher

American Geophysical Union (AGU)

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3