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

IF 4.4 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Journal of contaminant hydrology 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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Abstract

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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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
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。
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来源期刊
Journal of contaminant hydrology
Journal of contaminant hydrology 环境科学-地球科学综合
CiteScore
6.80
自引率
2.80%
发文量
129
审稿时长
68 days
期刊介绍: The Journal of Contaminant Hydrology is an international journal publishing scientific articles pertaining to the contamination of subsurface water resources. Emphasis is placed on investigations of the physical, chemical, and biological processes influencing the behavior and fate of organic and inorganic contaminants in the unsaturated (vadose) and saturated (groundwater) zones, as well as at groundwater-surface water interfaces. The ecological impacts of contaminants transported both from and to aquifers are of interest. Articles on contamination of surface water only, without a link to groundwater, are out of the scope. Broad latitude is allowed in identifying contaminants of interest, and include legacy and emerging pollutants, nutrients, nanoparticles, pathogenic microorganisms (e.g., bacteria, viruses, protozoa), microplastics, and various constituents associated with energy production (e.g., methane, carbon dioxide, hydrogen sulfide). The journal''s scope embraces a wide range of topics including: experimental investigations of contaminant sorption, diffusion, transformation, volatilization and transport in the surface and subsurface; characterization of soil and aquifer properties only as they influence contaminant behavior; development and testing of mathematical models of contaminant behaviour; innovative techniques for restoration of contaminated sites; development of new tools or techniques for monitoring the extent of soil and groundwater contamination; transformation of contaminants in the hyporheic zone; effects of contaminants traversing the hyporheic zone on surface water and groundwater ecosystems; subsurface carbon sequestration and/or turnover; and migration of fluids associated with energy production into groundwater.
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