Correction of the Buckingham-Darcy Law for flow of high strength salts in variably saturated porous media

被引:2
|
作者
Burns, Erick R.
Dragila, Maria I.
Selker, John S.
Guenther, Ronald B.
Parlange, Jean-Yves
Weisbrod, Noam
机构
[1] Univ Calgary, Dept Geol & Geophys, Calgary, AB T2N 1N4, Canada
[2] Oregon State Univ, Dept Crop & Soil Sci, Corvallis, OR 97331 USA
[3] Oregon State Univ, Dept Bioengn, Corvallis, OR 97331 USA
[4] Oregon State Univ, Dept Math, Corvallis, OR 97331 USA
[5] Cornell Univ, Dept Biol & Environm Engn, Ithaca, NY 14853 USA
[6] Ben Gurion Univ Negev, Jacob Blaustein Inst Desert Res, Zuckerberg Inst Water Res, Dept Environm Hydrol & Microbiol, IL-84990 Sede Boqer, Israel
关键词
process thermodynamics; Darcy; Buckingham; salt; saline; unsaturated;
D O I
10.1016/j.advwatres.2006.04.010
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The Buckingham-Darcy Law is used to describe fluid flow in unsaturated porous media at low Reynolds number. In order to provide a priori corrections to this law, a process thermodynamic approach is utilized to ascertain the functional dependence. Using this knowledge, corrections to the hydraulic conductivity coefficient are proposed and compared with available data. The proposed corrections substantially predict the observed behavior of flow of high concentration (saturated) sodium chloride solutions in porous media. During the derivation, physical principles consistent with the thermodynamics of the system were utilized. A review of these principles and their results provides an alternative form of the generalized Gibbs-Duhem Relation for continuous processes, indicating that the identical equivalence to zero is unlikely to occur for dissipative processes. Further, the postulated Gibbs and Gibbs-Duhem Relations indicate that special differential operators need to be used for continuous processes rather than the usual use of a generic differential. (C) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:469 / 482
页数:14
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