A direct passive method for measuring water and contaminant fluxes in porous media

被引:120
|
作者
Hatfield, K
Annable, M
Cho, JH
Rao, PSC
Klammler, H
机构
[1] Univ Florida, Dept Civil & Coastal Engn, Gainesville, FL 32611 USA
[2] Univ Florida, Interdisciplinary Program Hydrol Sci, Gainesville, FL 32611 USA
[3] Purdue Univ, Dept Environm Engn Sci, W Lafayette, IN 47907 USA
[4] Purdue Univ, Sch Civil Engn, W Lafayette, IN 47907 USA
[5] Graz Univ Technol, Dept Hydraul Engn & Water Resources Management, A-8010 Graz, Austria
关键词
mass flux; groundwater; mass discharge; tracer; passive; flux measurement;
D O I
10.1016/j.jconhyd.2004.06.005
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This paper introduces a new direct method for measuring water and contaminant fluxes in porous media. The method uses a passive flux meter (PFM), which is essentially a self-contained permeable unit properly sized to fit tightly in a screened well or boring. The meter is designed to accommodate a mixed medium of hydrophobic and/or hydrophilic permeable sorbents, which retain dissolved organic/inorganic contaminants present in the groundwater flowing passively through the meter. The contaminant mass intercepted and retained on the sorbent is used to quantify cumulative contaminant mass flux. The sorptive matrix is also impregnated with known amounts of one or more water soluble 'resident tracers'. These tracers are displaced from the sorbent at rates proportional to the groundwater flux; hence, in the current meter design, the resident tracers are used to quantify cumulative groundwater flux. Theory is presented and quantitative tools are developed to interpret the water flux from tracers possessing linear and nonlinear elution profiles. The same theory is extended to derive functional relationships useful for quantifying cumulative contaminant mass flux. To validate theory and demonstrate the passive flux meter, results of multiple box-aquifer experiments are presented and discussed. From these experiments, it is seen that accurate water flux measurements are obtained when the tracer used in calculations resides in the meter at levels representing 20 to 70 percent of the initial condition. 2,4-Dimethyl-3-pentanol (DMP) is used as a surrogate groundwater contaminant in the box aquifer experiments. Cumulative DMP fluxes are measured within 5% of known fluxes. The accuracy of these estimates generally increases with the total volume of water intercepted. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:155 / 181
页数:27
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