Interfacial area measurements for unsaturated flow through a porous medium

被引:178
作者
Culligan, KA [1 ]
Wildenschild, D
Christensen, BSB
Gray, WG
Rivers, ML
Tompson, AFB
机构
[1] Univ Notre Dame, Dept Civil Engn & Geol Sci, Notre Dame, IN 46556 USA
[2] Oregon State Univ, Dept Geosci, Corvallis, OR 97331 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, Dept Geophys Sci, Chicago, IL 60637 USA
[6] Univ Chicago, Consortium Adv Radiat Sources, Chicago, IL 60637 USA
[7] Lawrence Livermore Natl Lab, Geosci & Environm Technol Div, Livermore, CA 94551 USA
关键词
interfacial area; porous media; unsaturated flow;
D O I
10.1029/2004WR003278
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Multiphase flow and contaminant transport in porous media are strongly influenced by the presence of fluid-fluid interfaces. Recent theoretical work based on conservation laws and the second law of thermodynamics has demonstrated the need for quantitative interfacial area information to be incorporated into multiphase flow models. We have used synchrotron based X-ray microtomography to investigate unsaturated flow through a glass bead column. Fully three-dimensional images were collected at points on the primary drainage curve and on the secondary imbibition and drainage loops. Analysis of the high-resolution images (17 micron voxels) allows for computation of interfacial areas and saturation. Corresponding pressure measurements are made during the course of the experiments. Results show the fluid-fluid interfacial area increasing as saturation decreases, reaching a maximum at saturations ranging from 20 to 35% and then decreasing as the saturation continues to zero. The findings support results of numerical studies reported in the literature.
引用
收藏
页码:1 / 12
页数:12
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