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高分辨率深度离散分析在受 AFFF 影响场地包气带源中 PFAS 分布和浸出。

High-Resolution Depth-Discrete Analysis of PFAS Distribution and Leaching for a Vadose-Zone Source at an AFFF-Impacted Site.

机构信息

Department of Environmental Science, The University of Arizona Tucson, Arizona 85721, United States.

Hydrology and Atmospheric Sciences Department, The University of Arizona, Tucson, Arizona 85721, United States.

出版信息

Environ Sci Technol. 2024 Jun 4;58(22):9863-9874. doi: 10.1021/acs.est.4c01615. Epub 2024 May 23.

DOI:10.1021/acs.est.4c01615
PMID:38780413
Abstract

The long-term leaching of polyfluoroalkyl substances (PFAS) within the vadose zone of an AFFF application site for which the depth to groundwater is approximately 100 m was investigated by characterizing the vertical distribution of PFAS in a high spatial resolution. The great majority (99%) of PFAS mass resides in the upper 3 m of the vadose zone. The depths to which each PFAS migrated, quantified by moment analysis, is an inverse function of molar volume, demonstrating chromatographic separation. The PFAS were operationally categorized into three chain-length groups based on the three general patterns of retention observed. The longest-chain (>∼335 cm/mol molar volume) PFAS remained within the uppermost section of the core, exhibiting minimal leaching. Conversely, the shortest-chain (<∼220 cm/mol) PFAS accumulated at the bottom of the interval, which coincides with the onset of a calcic horizon. PFAS with intermediate-chain lengths were distributed along the length of the core, exhibiting differential magnitudes of leaching. The minimal or differential leaching observed for the longest- and intermediate-chain-length PFAS, respectively, demonstrates that retention processes significantly impacted migration. The accumulation of shorter-chain PFAS at the bottom of the core is hypothesized to result from limited deep infiltration and potential-enhanced retention associated with the calcic horizon.

摘要

研究了距地下水位约 100 m 的 AFFF 应用场地包气带中聚全氟烷基物质(PFAS)的长期浸出情况,该场地采用高空间分辨率对 PFAS 在包气带中的垂直分布进行了特征描述。绝大多数(99%)PFAS 质量存在于包气带的上部 3 m 内。通过矩分析量化了每种 PFAS 的迁移深度,迁移深度是摩尔体积的反函数,这表明存在色谱分离。根据观察到的三种一般保留模式,PFAS 可操作地分为三组链长。最长链(>∼335 cm/mol 摩尔体积)的 PFAS 保留在岩芯的最上部,浸出最小。相反,最短链(<∼220 cm/mol)的 PFAS 积累在间隔的底部,这与钙质层的出现相吻合。具有中等链长的 PFAS 沿岩芯长度分布,表现出不同程度的浸出。最长链和中等链长的 PFAS 分别观察到最小或差异浸出,这表明保留过程显著影响了迁移。岩芯底部较短链 PFAS 的积累,可能是由于钙质层的限制深层渗透和潜在增强保留所致。

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