Conceptualizing Controlling Factors for PFAS Salting Out in Groundwater Discharge Zones Along Sandy Beaches.

Ground water Pub Date : 2024-11-01 Epub Date: 2024-06-28 DOI:10.1111/gwat.13428
Hiroko M Hort, Clare E Robinson, Audrey H Sawyer, Yue Li, Rebecca Cardoso, Sophia A Lee, Douglas Roff, David T Adamson, Charles J Newell
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Abstract

Understanding fate and transport processes for per- and poly-fluoroalkyl substances (PFAS) is critical for managing impacted sites. "PFAS Salting Out" in groundwater, defined herein, is an understudied process where PFAS in fresh groundwater mixes with saline groundwater near marine shorelines, which increases sorption of PFAS to aquifer solids. While sorption reduces PFAS mass discharge to marine surface water, the fraction that sorbs to beach sediments may be mobilized under future salinity changes. The objective of this study was to conceptually explore the potential for PFAS Salting Out in sandy beach environments and to perform a preliminary broad-scale characterization of sandy shoreline areas in the continental U.S. While no site-specific PFAS data were collected, our conceptual approach involved developing a multivariate regression model that assessed how tidal amplitude and freshwater submarine groundwater discharge affect the mixing of fresh and saline groundwater in sandy coastal aquifers. We then applied this model to 143 U.S. shoreline areas with sandy beaches (21% of total beaches in the USA), indirectly mapping potential salinity increases in shallow freshwater PFAS plumes as low (<10 ppt), medium (10-20 ppt), or high (>20 ppt) along groundwater flow paths before reaching the ocean. Higher potential salinity increases were observed in West Coast bays and the North Atlantic coastline, due to the combination of moderate to large tides and large fresh groundwater discharge rates, while lower increases occurred along the Gulf of Mexico and the southern Florida Atlantic coast. The salinity increases were used to estimate potential perfluorooctane sulfonic acid (PFOS) sorption in groundwater due to salting out processes. Low-category shorelines may see a 1- to 2.5-fold increase in sorption of PFOS, medium-category a 2.0- to 6.4-fold increase, and high-category a 3.8- to 25-fold increase in PFOS sorption. The analysis presented provides a first critical step in developing a large-scale approach to classify the PFAS Salting Out potential along shorelines and the limitations of the approach adopted highlights important areas for further research.

沙质海滩地下水排放区 PFAS 盐化控制因素的概念化。
了解全氟烷基和多氟烷基物质 (PFAS) 的归宿和迁移过程对于管理受影响的场地至关重要。本文所定义的地下水中的 "PFAS 盐化 "是一个未被充分研究的过程,即淡水中的 PFAS 与海洋海岸线附近的含盐地下水混合,从而增加 PFAS 对含水层固体的吸附。虽然吸附作用减少了 PFAS 向海洋地表水的大量排放,但吸附在海滩沉积物上的部分可能会在未来盐度变化的情况下被移动。虽然没有收集具体地点的 PFAS 数据,但我们的概念方法包括建立一个多变量回归模型,以评估潮汐幅度和淡水海底地下水排 放量如何影响沙质沿海含水层中淡水和含盐地下水的混合。然后,我们将该模型应用于美国 143 个有沙滩的海岸线地区(占美国沙滩总数的 21%),间接绘制了浅层淡水全氟辛烷磺酸羽流在到达海洋之前沿地下水流动路径的潜在盐度升高图,最低为 20 ppt。在西海岸海湾和北大西洋海岸线观察到的潜在盐度增加较高,这是由于中到大潮汐和大量地下淡水排放率的共同作用,而在墨西哥湾和佛罗里达州南部大西洋海岸线观察到的潜在盐度增加较低。盐度的增加被用来估算地下水中因盐化过程而可能吸附的全氟辛烷磺酸(PFOS)。低类别海岸线的全氟辛烷磺酸吸附量可能会增加 1 到 2.5 倍,中类别增加 2.0 到 6.4 倍,高类别增加 3.8 到 25 倍。所做的分析为开发一种大规模方法来对海岸线的全氟辛烷磺酸盐化潜力进行分类迈出了关键的第一步,所采用方法的局限性突出了有待进一步研究的重要领域。
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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