Modeling PFAS Subsurface Transport in the Presence of Groundwater Table Fluctuations: The Impact on Source-Zone Leaching and Exploration of Model Simplifications

IF 4.6 1区 地球科学 Q2 ENVIRONMENTAL SCIENCES Water Resources Research Pub Date : 2024-11-05 DOI:10.1029/2024wr037707
Jicai Zeng, Mark L. Brusseau, Bo Guo
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Abstract

Air–water interfacial adsorption represents a major source of retention for many per- and poly-fluoroalkyl substances (PFAS). Therefore, transient hydrological fluxes that dynamically change the amount of air–water interfaces are expected to strongly influence PFAS retention in their source zones in the vadose zone. We employ mathematical modeling to study how seasonal groundwater table (GWT) fluctuations affect PFAS source-zone leaching. The results suggest that, by periodically collapsing air–water interfaces, seasonal GWT fluctuations can lead to strong temporal variations in groundwater concentration and significantly enhance PFAS leaching in the vadose zone. The enhanced leaching is more pronounced for longer-chain PFAS, coarser-textured porous media, drier climates, and greater amplitudes of fluctuations. GWT fluctuations and lateral migration above the GWT introduce a downgradient persistent secondary source zone for longer-chain PFAS. However, the enhanced leaching and the secondary source zone are greatly reduced when subsurface heterogeneity is present. In highly heterogeneous source zones, GWT fluctuations may even lead to overall slower leaching due to lateral flow (in the GWT fluctuation zone and above the GWT) moving PFAS into local regions with greater retention capacities. Model simplification analyses suggest that the enhanced source-zone leaching due to GWT fluctuations may be approximated using a static but shallower GWT. Additionally, while vertical 1D models underestimate source-zone leaching due to not representing lateral migration, they can be revised to account for lateral migration and provide lower- and upper-bound estimates of PFAS source-zone leaching under GWT fluctuations. Overall, our study suggests that representing GWT fluctuations is critical for quantifying source-zone leaching of PFAS, especially the more interfacially active longer-chain compounds.
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地下水位波动情况下的 PFAS 地下迁移建模:对源区沥滤的影响以及对模型简化的探讨
空气-水界面吸附是许多全氟和多氟烷基物质(PFAS)滞留的主要来源。因此,动态改变空气-水界面数量的瞬态水文通量预计会强烈影响全氟辛烷磺酸(PFAS)在其源区内的滞留。我们采用数学模型研究了季节性地下水位(GWT)波动如何影响 PFAS 源区沥滤。研究结果表明,通过周期性地塌陷空气-水界面,季节性地下水位波动会导致地下水浓度的强烈时间变化,并显著增强渗透带中 PFAS 的沥滤作用。对于长链全氟辛烷磺酸、质地较粗的多孔介质、较干燥的气候以及波动幅度较大的地区,沥滤作用的增强更为明显。GWT 波动和 GWT 上部的横向迁移为长链全氟辛烷磺酸引入了一个向下的持久性二级来源区。然而,当存在地下异质性时,沥滤增强和二级源区的作用就会大大减弱。在高度异质源区,由于横向流(在 GWT 波动区和 GWT 上方)将 PFAS 转移到滞留能力更强的局部区域,GWT 波动甚至可能导致整体沥滤速度减慢。模型简化分析表明,可以使用静态但较浅的 GWT 来近似估算由于 GWT 波动而导致的源区沥滤增强。此外,虽然垂直一维模型由于没有反映横向迁移而低估了源区沥滤,但可以对其进行修正,以考虑横向迁移,并提供 GWT 波动下 PFAS 源区沥滤的下限和上限估计值。总之,我们的研究表明,表示 GWT 波动对于量化 PFAS(尤其是界面活性更强的长链化合物)的源区沥滤至关重要。
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来源期刊
Water Resources Research
Water Resources Research 环境科学-湖沼学
CiteScore
8.80
自引率
13.00%
发文量
599
审稿时长
3.5 months
期刊介绍: Water Resources Research (WRR) is an interdisciplinary journal that focuses on hydrology and water resources. It publishes original research in the natural and social sciences of water. It emphasizes the role of water in the Earth system, including physical, chemical, biological, and ecological processes in water resources research and management, including social, policy, and public health implications. It encompasses observational, experimental, theoretical, analytical, numerical, and data-driven approaches that advance the science of water and its management. Submissions are evaluated for their novelty, accuracy, significance, and broader implications of the findings.
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