Brusseau Mark L, Guo Bo
Environmental Science Department; Hydrology and Atmospheric Sciences Department, University of Arizona, Tucson, AZ 85721, United States.
Hydrology and Atmospheric Sciences Department, University of Arizona, Tucson, AZ 85721, United States.
Water Res. 2021 Dec 1;207:117785. doi: 10.1016/j.watres.2021.117785. Epub 2021 Oct 21.
Per and polyfluoroalkyl substances (PFAS) present in the soil pose a long-term threat to groundwater. Robust characterization and modeling of PFAS retention and transport in unsaturated systems requires an accurate determination of the magnitude of air-water interfacial area (AWIA). Multiple methods are available for measuring or estimating air-water interfacial area, including x-ray microtomography (XMT), various aqueous and gas-phase interfacial tracer-test (ITT) methods, and thermodynamic-based estimation methods. AWIAs determined with the different methods can vary significantly. Therefore, it is critical to determine which measurement methods are relevant for application to PFAS retention and transport. This is achieved by employing AWIAs determined with different methods to simulate the results of miscible-displacement experiments reported in the literature for the transport of perfluorooctanoic acid (PFOA) in an unsaturated quartz sand. Measured PFOA breakthrough curves were successfully predicted using AWIA values measured by aqueous ITT methods. Conversely, AWIAs measured with the XMT method and estimated with the thermodynamic method under-predicted the magnitude of retardation and could not successfully simulate the measured transport data. These results indicate that the ITT method appears to provide the most appropriate AWIA values for robust characterization and modeling of PFAS transport in unsaturated systems. The long-term impact of employing different AWIA values on PFOA leaching in the vadose zone was simulated for a representative AFFF application scenario. The predicted timeframes for PFOA migration to groundwater varied from 3 to 6 to 20 years depending on which AWIA was used in the simulation. These relatively large differences would result in significantly different risk-assessment outcomes. These results illustrate that it is critical to employ the AWIA that is most representative of PFAS retention for accurate predictions of PFAS leaching in the vadose zone.
土壤中存在的全氟和多氟烷基物质(PFAS)对地下水构成长期威胁。要对PFAS在非饱和系统中的吸附和运移进行可靠的表征和建模,需要准确测定气水界面面积(AWIA)的大小。有多种方法可用于测量或估算气水界面面积,包括X射线显微断层扫描(XMT)、各种水相和气相界面示踪剂测试(ITT)方法以及基于热力学的估算方法。用不同方法测定的AWIA可能会有显著差异。因此,确定哪种测量方法适用于PFAS的吸附和运移至关重要。这是通过使用不同方法测定的AWIA来模拟文献中报道的全氟辛酸(PFOA)在非饱和石英砂中运移的混溶驱替实验结果来实现的。使用水相ITT方法测量的AWIA值成功预测了测得的PFOA突破曲线。相反,用XMT方法测量并用热力学方法估算的AWIA对阻滞程度的预测偏低,无法成功模拟测得的运移数据。这些结果表明,ITT方法似乎为PFAS在非饱和系统中的运移进行可靠表征和建模提供了最合适的AWIA值。针对一个典型的水成膜泡沫灭火剂(AFFF)应用场景,模拟了采用不同AWIA值对渗流带中PFOA淋溶的长期影响。根据模拟中使用的AWIA不同,预测PFOA迁移到地下水的时间范围从3年到6年到20年不等。这些相对较大的差异将导致显著不同的风险评估结果。这些结果说明,采用最能代表PFAS吸附的AWIA对于准确预测渗流带中PFAS的淋溶至关重要。