采用多种实验方法,更好地描述地下水位波动情况下 LNAPL 在土壤中的归宿

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC ACS Applied Electronic Materials Pub Date : 2024-02-09 DOI:10.1016/j.jconhyd.2024.104319
Amélie Cavelan , Pierre Faure , Catherine Lorgeoux , Stéfan Colombano , Jacques Deparis , Dorian Davarzani , Noële Enjelvin , Constantin Oltean , Anne-Julie Tinet , Fabien Domptail , Fabrice Golfier
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引用次数: 0

摘要

轻质非水相液体(LNAPLs)是重要的土壤污染源,地下水的波动可能会严重影响其迁移和释放。然而,由于地下水位的变化会导致三相流体的持续重新分布,因此风险评估仍然十分复杂。因此,必须改进监测方法,以更好地整合与地下水位动态相关的 LNAPL 多化合物和多相。为此,开发了一种溶液模拟污染土壤柱(2 立方米),结合了原位监测(电导率、土壤湿度、温度、pH 值、Eh 值)、直接水和气体采样以及监测井、气体收集室和抽吸探头中的分析(GC/MS-TQD、μGC)。该实验以综合方式评估了受控降雨和地下水位波动模式如何影响 LNAPL 垂直土壤饱和度分布和释放。将这些方法结合起来,可以研究雨水渗透和地下水位波动对受污染土壤氧气周转的影响、LNAPL 污染物在土壤中的分布以及向溶解相和气相的再移动,并估算 LNAPL 源衰减率。因此,在 120 天后,7.5% 的污染物被溶解和气化。在实验过程中,地下水位的变化造成了游离 LNAPL 在土壤中的扩散和滞留,改变了溶解 LNAPL 的浓度。不过,部分溶解的污染物很快被生物降解,只留下水中最耐生物分解的成分。这一结果凸显了开发新实验装置的重要性,这些装置旨在评估与气候有关的参数对受污染场地 LNAPL 最终结果的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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An experimental multi-method approach to better characterize the LNAPL fate in soil under fluctuating groundwater levels

Light-Non-Aqueous phase liquids (LNAPLs) are important soil contamination sources, and groundwater fluctuations may significantly affect their migration and release. However, the risk assessment remains complex due to the continuous three-phase fluid redistribution caused by water table level variations. Hence, monitoring methods must be improved to integrate better the LNAPL multi-compound and multi-phase aspects tied to the groundwater level dynamics. For this purpose, a lysimetric contaminated soil column (2 m3) combining in-situ monitoring (electrical permittivity, soil moisture, temperature, pH, Eh), direct water and gas sampling and analyses (GC/MS-TQD, μGC) in monitoring well, gas collection chambers, and suction probes) were developed. This experiment assesses in an integrated way how controlled rainfalls and water table fluctuation patterns may affect LNAPL vertical soil saturation distribution and release. Coupling these methods permitted the investigation of the effects of rainwater infiltration and water table level fluctuation on contaminated soil oxygen turnover, LNAPL contaminants' soil distribution and remobilization towards the dissolved and the gaseous phase, and the estimate of the LNAPL source attenuation rate. Hence, 7.5% of the contamination was remobilized towards the dissolved and gaseous phase after 120 days. During the experiment, groundwater level variations were responsible for the free LNAPL soil spreading and trapping, modifying dissolved LNAPL concentrations. Nevertheless, part of the dissolved contamination was rapidly biodegraded, leaving only the most bio-resistant components in water. This result highlights the importance of developing new experimental devices designed to assess the effect of climate-related parameters on LNAPL fate at contaminated sites.

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