Power Christopher, Gerhard Jason I, Karaoulis Marios, Tsourlos Panagiotis, Giannopoulos Antonios
Department of Civil and Environmental Engineering, University of Western Ontario, London, Ontario, N6A 3K7, Canada.
Department of Geophysics, Colorado School of Mines, Golden, CO, 80401, USA.
J Contam Hydrol. 2014 Jul;162-163:27-46. doi: 10.1016/j.jconhyd.2014.04.004. Epub 2014 May 5.
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 2m and up to 50% underestimation at late time between 2 and 4m 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.
目前还不存在用于绘制致密非水相液体(DNAPL)修复情况的实用、非侵入性工具。电阻层析成像(ERT)显示出巨大潜力,但由于在实际场地解释测量结果存在挑战,尚未成为从业者的工具。本研究探讨了最近开发的四维(4D,即三维空间加时间)时移地表ERT监测DNAPL源区修复的有效性。一项实验室实验展示了随时间绘制变化的NAPL分布的方法。然后采用最近开发的DNAPL-ERT数值模型独立模拟该实验,证实DNAPL-ERT模型是模拟实际系统的可靠工具。接着使用该数值模型评估该方法在现场尺度的潜力。最初模拟了四个具有不同复杂程度的DNAPL源区,随后通过增强溶解对完全的DNAPL修复进行时移ERT监测模拟。4D ERT反演提供了源区随时间质量减少区域的估计。结果表明,4D时移ERT有很大潜力在每个方向几米范围内绘制源区不断演变的处理部分的轮廓和质心。此外,该技术可以提供随时间修复的DNAPL体积的合理估计,尽管较为保守:在地表以下2米范围内低估25%,在2至4米深度的后期低估高达50%。该技术在识别主DNAPL主体外部的DNAPL细脉清理方面可靠性较低。总体而言,本研究表明4D时移ERT有潜力绘制场地修复期间DNAPL质量实时变化的位置和速度。