Parameters affecting maximum fluid transport in large aperture fractures

被引:35
作者
Dragila, MI
Weisbrod, N
机构
[1] Oregon State Univ, Dept Crop & Soil Sci, Corvallis, OR 97331 USA
[2] Ben Gurion Univ Negev, Desert Res Inst, Inst Water Sci & Technol, Dept Environm Hydrol & Microbiol, IL-84990 Sede Boqer, Israel
关键词
fractured rock; unsaturated; vadose zone; contact angle; fracture intersection; film flow; capillary flow; fluid transport; fracture flow;
D O I
10.1016/j.advwatres.2003.09.002
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
We present results of laboratory experiments to study the behavior of liquids moving in unsaturated wide-aperture fractures. A 5-mm-thick glass plate cut with a similar to1.7-mm aperture was used as a fractured rock analog to study behavior of film and capillary droplet flow modes. Flow rates ranged between 0.6 and 6.0 ml/min. Variability in the ambient barometric pressure, resulting from weather conditions, seemed to play a role in the natural selection of flow mode. For droplet mode, constant input conditions resulted in highly variable transport properties within the fracture. The advancing meniscus exhibited a dynamic contact angle that was a function of the droplet speed and much larger than the static contact angle. Flow rate was reduced due to the larger contact angle. Analytical expressions for droplet velocity and flow capacity are presented as a function of the dynamic rather than the static contact angle. (C) 2003 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1219 / 1228
页数:10
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