Department of Environmental Engineering, College of Biology and Environment, Nanjing Forestry University, Nanjing, 210037, China.
Department of Environmental Engineering, College of Biology and Environment, Nanjing Forestry University, Nanjing, 210037, China.
Environ Pollut. 2022 Oct 15;311:119820. doi: 10.1016/j.envpol.2022.119820. Epub 2022 Aug 5.
The coexistence of per- and polyfluoroalkyl substances (PFASs) and heavy metals have been found in soils. However, the interaction between the combined pollutants in soils remains unclear. In this study, the adsorption processes of single and combined Cr(VI) and chlorinated polyfluoroalkyl ether potassium sulfonate (F-53 B) in red, yellow and black soils were simulated. When compared with the single F-53 B and Cr(VI), the adsorption amount of the combined F-53 B and Cr(VI) on soils changed with the types of soils. The interactions between F-53 B and Cr(VI) in soils affected their adsorption behavior. The adsorption of the combined F-53 B and Cr(VI) best fit second-order kinetics and the Freundlich equation. Moreover, aluminum and iron oxides are highly correlated with adsorption of F-53 B and Cr(VI). Both F-53 B and Cr(VI) can form complexes with aluminum and iron oxides through electrostatic interactions, but PFOS could be bridged with iron oxides to form an inner sphere complex and with aluminum oxides to form an outer sphere complex. The coexistence of F-53 B and Cr(VI) could change the fluorescent group of dissolved organic matter (DOM) in soils due to the complexation between F-53 B and DOM. In addition, F-53 B increased the acid-soluble portion of Cr and decreased its residual form, which promoted the environmental risk of Cr in soils.
多氟和全氟烷基物质(PFASs)和重金属在土壤中共存。然而,土壤中联合污染物之间的相互作用仍不清楚。本研究模拟了红色、黄色和黑色土壤中单一和复合 Cr(VI)和全氟辛基磺酸氯代醚钾盐(F-53B)的吸附过程。与单一 F-53B 和 Cr(VI)相比,复合 F-53B 和 Cr(VI)在土壤中的吸附量随土壤类型而变化。土壤中 F-53B 和 Cr(VI)之间的相互作用影响了它们的吸附行为。复合 F-53B 和 Cr(VI)的吸附最符合二级动力学和 Freundlich 方程。此外,铝和铁氧化物与 F-53B 和 Cr(VI)的吸附高度相关。F-53B 和 Cr(VI)都可以通过静电相互作用与铝和铁氧化物形成配合物,但 PFOS 可以与铁氧化物形成内球配合物,与氧化铝形成外球配合物。F-53B 和 Cr(VI)的共存可能会由于 F-53B 和 DOM 之间的络合作用而改变土壤中溶解有机质(DOM)的荧光基团。此外,F-53B 增加了 Cr 的酸溶性部分,降低了其残留形式,从而增加了 Cr 在土壤中的环境风险。