Pore-scale characteristics of multiphase flow in porous media: A comparison of air-water and oil-water experiments

被引:154
|
作者
Culligan, KA
Wildenschild, D [1 ]
Christensen, BSB
Gray, WG
Rivers, ML
机构
[1] Oregon State Univ, Dept Civil Construct & Environm Engn, Dept Geosci, Corvallis, OR 97331 USA
[2] Univ Notre Dame, Dept Civil Engn & Geol Sci, Notre Dame, IN 46556 USA
[3] Tech Univ Denmark, DK-2800 Lyngby, Denmark
[4] Univ N Carolina, Dept Environm Sci & Engn, Chapel Hill, NC 27599 USA
[5] Univ Chicago, Consortium Adv Radiat Sources, Chicago, IL 60637 USA
[6] Univ Chicago, Dept Geophys Sci, Chicago, IL 60637 USA
基金
美国国家科学基金会;
关键词
multi-phase flow; NAPLs; porous media; microtomography; Interfacial areas; capillary pressure-saturation curves;
D O I
10.1016/j.advwatres.2005.03.021
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Studies of NAPL dissolution in porous media have demonstrated that measurement of saturation alone is insufficient to describe the rate of dissolution. Quantification of the NAPL-water interfacial area provides a measure of the expected area available for mass transfer and will likely be a primary determinant of NAPL removal efficiency. To measure the interfacial area, we have used a synchrotron-based CMT technique to obtain high-resolution 3D images of flow in a Soltrol-water glass bead system. The interfacial area is found to increase as the wetting phase saturation decreases, reach a maximum, and then decrease as the wetting phase saturation goes to zero. These results are compared to previous findings for an air-water-glass bead study; The Soltrol-water interfacial areas were found to peak at similar saturations as those measured for the air-water system (20-35% saturation range), however, the peak values were in some cases almost twice Lis high for the oil-water system. We believe that the observed differences between the air-water and oil-water systems to a large degree can be explained by the differences in interfacial tensions for the two systems. (C) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:227 / 238
页数:12
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