利用熔融表面和跨钻孔电阻率层析成像技术绘制和监测高密度非水相液源区。

Journal of hazardous materials Pub Date : 2024-10-05 Epub Date: 2024-08-22 DOI:10.1016/j.jhazmat.2024.135618
Fansong Meng, Jinguo Wang, Yongsheng Zhao
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引用次数: 0

摘要

有效确定致密非水相液体(DNAPL)源区的特征对于污染场地的修复至关重要。由于土壤的异质性、重力和毛细管障碍,DNAPL 通常以残留物或油池的形式存在于高渗透透镜内部和不透水层之上。由于钻探成本高昂,电阻率层析成像 (ERT) 技术(包括地表 ERT 和交叉钻孔 ERT)通常用于 DNAPL 源区绘图和监测。然而,ERT 的空间分辨率较低,增加了源区调查的不确定性。本研究提出了一种通过融合地面和跨钻孔 ERT 数据来改进 DNAPL 测绘和监测的方法。通过沙箱实验模拟了一个异质 DNAPL 源区,采用两种 ERT 方法进行静态绘图和动态监测。利用反射光成像(RLM)可视化 DNAPL 迁移并提供饱和度数据,从而量化 ERT 在描述 DNAPL 分布特征方面的有效性。结果表明,由于背景干扰,单个 ERT 方法在绘制 DNAPL 源区图时面临巨大挑战。单靠地表ERT往往会低估深层DNAPL源区的范围。然而,将地表和跨钻孔 ERT 融合在一起,可以互补地提高垂直空间分辨率,从而改善 DNAPL 源区的特征描述。静态和延时 ERT 数据的融合大大提高了 DNAPL 源区的绘图和监测能力。通过使用电阻率变化等值线(5%、10%、15%)计算 ERT 监测区域与实际区域的比率,发现与单独使用地面 ERT 相比,融合地面和跨钻孔 ERT 数据可提高监测分辨率 50.48%,与跨钻孔 ERT 相比,可提高 22.95%。主成分分析法(PCA)在融合延时数据方面很有效,而加权平均法(WAM)在融合静态电阻率数据方面则优于 PCA。
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Mapping and monitoring dense non-aqueous phase liquid source zone by fused surface and cross-borehole electrical resistivity tomography.

Effective characterization of dense non-aqueous phase liquid (DNAPL) source zones is crucial for remediating polluted sites. DNAPL often reside as residuals or pools within high-permeability lenses and above impermeable layers due to soil heterogeneity, gravity, and capillary barriers. Given the high cost of drilling, electrical resistivity tomography (ERT) techniques-including surface ERT and cross-borehole ERT, are commonly used for DNAPL source zone mapping and monitoring. However, the low spatial resolution of ERT increases uncertainty in source zone investigations. This study proposes a method for improving DNAPL mapping and monitoring by fusing surface and cross-borehole ERT data. Sandbox experiments were conducted to simulate a heterogeneous DNAPL source zone, employing both ERT methods for static mapping and dynamic monitoring. Reflective light imaging (RLM) was used to visualize DNAPL migration and provide saturation data, allowing for the quantification of ERT's effectiveness in characterizing DNAPL distribution. The results indicate that individual ERT methods face significant challenges in DNAPL source zone mapping due to background interference. Surface ERT alone tends to underestimate the extent of deeper DNAPL source zones. However, fusing surface and cross-borehole ERT results in a complementary enhancement of vertical spatial resolution, thereby improving the characterization of DNAPL source zones. The fusion of static and time-lapse ERT data substantially enhances DNAPL source zone mapping and monitoring capabilities. By calculating the ratio of the ERT-monitored area to the actual area using resistivity change contours (5 %, 10 %, 15 %), it was found that fusing surface and cross-borehole ERT data improved monitoring resolution by 50.48 % compared to surface ERT alone and by 22.95 % compared to cross-borehole ERT. Principal component analysis (PCA) was effective in fusing time-lapse data, while the weighted average method (WAM) outperformed PCA for static resistivity data fusion.

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