Evaluating four-dimensional time-lapse electrical resistivity tomography for monitoring DNAPL source zone remediation

被引:47
|
作者
Power, Christopher [1 ]
Gerhard, Jason I. [1 ]
Karaoulis, Marios [2 ]
Tsourlos, Panagiotis [3 ]
Giannopoulos, Antonios [4 ]
机构
[1] Univ Western Ontario, Dept Civil & Environm Engn, London, ON N6A 3K7, Canada
[2] Colorado Sch Mines, Dept Geophys, Golden, CO 80401 USA
[3] Aristotle Univ Thessaloniki, Dept Geophys, Thessaloniki 54124, Greece
[4] Univ Edinburgh, Sch Engn, Edinburgh EH9 3JL, Midlothian, Scotland
关键词
DNAPL; Remediation; 4D time-lapse monitoring; Geophysics; Electrical resistivity tomography; HETEROGENEOUS POROUS-MEDIA; INDUCED POLARIZATION TOMOGRAPHY; LEAST-SQUARES INVERSION; 3D ERT; MIGRATION; MODEL; TRANSPORT; CONDUCTIVITY; REDISTRIBUTION; IMMOBILIZATION;
D O I
10.1016/j.jconhyd.2014.04.004
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Practical, non-invasive tools do not currently exist for mapping the remediation of dense non-aqueous phase liquids (DNAPLs). Electrical resistivity tomography (ERT) exhibits significant potential but has not yet become a practitioner's tool due to challenges in interpreting the survey results at real sites. This study explores the effectiveness of recently developed four-dimensional (4D, i.e., 3D space plus time) time-lapse surface ERT to monitor DNAPL source zone remediation. A laboratory experiment demonstrated the approach for mapping a changing NAPL distribution over time. A recently developed DNAPL-ERT numerical model was then employed to independently simulate the experiment, providing confidence that the DNAPL-ERT model is a reliable tool for simulating real systems. The numerical model was then used to evaluate the potential for this approach at the field scale. Four DNAPL source zones, exhibiting a range of complexity, were initially simulated, followed by modeled time-lapse ERT monitoring of complete DNAPL remediation by enhanced dissolution. 4D ERT inversion provided estimates of the regions of the source zone experiencing mass reduction with time. Results show that 4D time-lapse ERT has significant potential to map both the outline and the center of mass of the evolving treated portion of the source zone to within a few meters in each direction. In addition, the technique can provide a reasonable, albeit conservative, estimate of the DNAPL volume remediated with time: 25% underestimation in the upper 2 m and up to 50% underestimation at late time between 2 and 4 m depth. The technique is less reliable for identifying cleanup of DNAPL stringers outside the main DNAPL body. Overall, this study demonstrates that 4D time-lapse ERT has potential for mapping where and how quickly DNAPL mass changes in real time during site remediation. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:27 / 46
页数:20
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