Naturally occurring surface water foams as a PFAS sampling matrix.

IF 11.3
Journal of hazardous materials Pub Date : 2025-09-15 Epub Date: 2025-08-05 DOI:10.1016/j.jhazmat.2025.139456
Donovan S Vitale, Donald M Reeves, Ethan S Coffin, Daniel P Cassidy
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Abstract

Surface Water Foam (SWF) and underlying Surface Water (SW) were collected from six distinct sites across Michigan using a novel sampling device. PFAS were detected in all SWF samples (Σ41 compounds, n = 14; Avg total PFAS=54,895 ng/L). SWF samples were enriched in high and intermediate molecular volume PFAS relative to SW samples (n = 10) which were dominated by low molecular volume, short-chain PFAS (Avg total PFAS=21 ng/L). Ultra-long-chain and rarely detected PFAS were quantified in SWF that were not detected in SW. Wet and dry SWFs were distinguished by appearance, liquid content, and PFAS composition. Dry SWFs had higher total PFAS concentrations than wet SWFs (Avg total PFAS difference =158,330 ng/L). Intermediate molecular volume PFAS constituted a greater percentage of total PFAS concentrations in wet SWFs, whereas dry SWFs were dominated by high molecular volume PFAS. Principal component and cluster analyses show distinct compositional differences between SW, wet SWF, and dry SWF. A conceptual model is proposed to describe changes in PFAS composition during the evolution and aging of SWFs. Bubbles created from turbulence in surface waters initially accumulate to form wet SWFs. Liquid drains as wet SWFs evolve towards dry SWFs and lower molecular weight PFAS with lower air-water interface (AWI) adsorption drain with the liquid. This enriches dry SWFs with higher molecular volume PFAS that have higher AWI adsorption (up to five orders of magnitude). This study demonstrates the value of SWFs as a complementary sampling matrix for quantifying high and intermediate volume PFAS in natural surface water systems.

自然产生的地表水泡沫作为PFAS采样矩阵。
地表水泡沫(SWF)和底层地表水(SW)使用一种新型采样设备从密歇根州的六个不同地点收集。所有SWF样品中均检测到PFAS (Σ41化合物,n = 14;平均总PFAS=54,895 ng/L)。相对于SW样品(n = 10),SWF样品富含高、中分子体积PFAS,而SW样品以低分子体积、短链PFAS为主(平均总PFAS=21 ng/L)。超长链和很少检测到的PFAS在SWF中被量化,而在SW中没有检测到。通过外观、液体含量和PFAS组成来区分干湿SWFs。干SWFs的总PFAS浓度高于湿SWFs(平均总PFAS差异=158,330 ng/L)。在湿性主权财富基金中,中等分子体积的PFAS占总PFAS浓度的比例较大,而干性主权财富基金则以高分子体积的PFAS为主。主成分分析和聚类分析表明,湿性SWF和干性SWF在成分上存在明显差异。提出了一个描述主权财富基金演化和老化过程中PFAS组成变化的概念模型。由地表水湍流产生的气泡最初积聚形成湿的主权财富基金。液体随湿SWFs向干SWFs和低分子量PFAS演变而排出,具有较低的空气-水界面(AWI)吸附。这使干SWFs具有更高分子体积的PFAS,具有更高的AWI吸附(高达五个数量级)。这项研究证明了SWFs作为一种补充采样矩阵的价值,可以量化天然地表水系统中高体积和中体积的PFAS。
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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