Wang Hui, Gong Xueying, Zhang Yankun, Liu Fengping, Zhang Jia, Yuan Ying, Samuel Barnie, Tan Wenbing, Xi Beidou, Chen Honghan
State Key Laboratory of Environmental Criteria and Risk Assessment, and State Environmental Protection Key Laboratory of Simulation and Control of Groundwater Pollution, Chinese Research Academy of Environmental Sciences, Beijing, 100012, PR China; Beijing Key Laboratory of Water Resources & Environmental Engineering, China University of Geosciences, Beijing, 100083, PR China.
Chinese Academy for Environmental Planning, Beijing, 100020, PR China.
Environ Pollut. 2024 Dec 15;363(Pt 1):125057. doi: 10.1016/j.envpol.2024.125057. Epub 2024 Sep 30.
Wetlands exhibit a self-purification effect on Cr(VI) owing to the adsorption and reduction capabilities of their humic substance (HS)-Fe(III) coprecipitates. However, the similarities and differences in the adsorption and reduction of Cr(VI) by different types of HS-Fe(III) coprecipitates remains unknown. In this study, fulvic acid (FA)- and humic acid (HA)-Fe(III) coprecipitates were synthesized with initial C/Fe ratios ranging from 0.25 to 15, and a comparative analysis of their adsorption and reduction effects was conducted. The results showed that FA- and HA-Fe(III) coprecipitates exhibit similar abilities to adsorb Cr(VI) by forming inner-sphere complexes with ferrihydrite (Fh), as well as with FA/HA. The association between FA/HA and Fe(III) not only blocked certain FeOH adsorption sites, but also enhanced the electrostatic repulsion towards Cr(VI), resulting in a proportionate decrease in their adsorption ability. For reduction, inductive and intrinsic reduction were involved in both FA- and HA-Fe(III) coprecipitates. However, the synergism/antagonism differed with the inherent sites (e.g., phenolic hydroxyl, ArOH) and activated sites (e.g., alcoholic hydroxyl, AlOH). Based on the size differences between FA and HA, the AlOH contained in FA was more easily activated by Fe(III) than that in HA, owing to the shorter induction path required. Thus, consistent synergism was observed in FA-Fe(III) coprecipitates regardless of Fe(III) species. In contrast, synergism was only observed in HA-Fe(III) coprecipitates containing Fh, because the inductive ability of Fe(III) cations was too weak to activate AlOH through the longer path. Moreover, with irreversible consumption of AlOH, intrinsic reduction became the dominant pathway at concentrations >1 mM Cr(VI). The preferential elimination of ArOH subsequently led to a transition to antagonism. These outcomes deepen our scientifical understanding of the environmental effects of HS-Fe(III) coprecipitates and offer new perspectives for exploring their potential applications in the remediation of Cr-contaminated sites.
由于湿地腐殖质(HS)-铁(III)共沉淀的吸附和还原能力,湿地对六价铬具有自净作用。然而,不同类型的HS-铁(III)共沉淀对六价铬的吸附和还原的异同仍不清楚。在本研究中,合成了初始C/Fe比为0.25至15的富里酸(FA)-和腐殖酸(HA)-铁(III)共沉淀,并对它们的吸附和还原效果进行了对比分析。结果表明,FA-和HA-铁(III)共沉淀通过与水铁矿(Fh)以及FA/HA形成内球络合物,表现出相似的吸附六价铬的能力。FA/HA与铁(III)之间的缔合不仅阻断了某些FeOH吸附位点,还增强了对六价铬的静电排斥,导致它们的吸附能力成比例下降。对于还原作用,FA-和HA-铁(III)共沉淀均涉及诱导还原和固有还原。然而,协同作用/拮抗作用因固有位点(如酚羟基,ArOH)和活化位点(如醇羟基,AlOH)而异。基于FA和HA之间的尺寸差异,由于所需的诱导路径较短,FA中含有的AlOH比HA中的更容易被铁(III)活化。因此,无论铁(III)种类如何,在FA-铁(III)共沉淀中均观察到一致的协同作用。相比之下,仅在含有Fh的HA-铁(III)共沉淀中观察到协同作用,因为铁(III)阳离子的诱导能力太弱而无法通过较长路径活化AlOH。此外,随着AlOH的不可逆消耗,在六价铬浓度>1 mM时,固有还原成为主要途径。随后ArOH的优先消除导致转变为拮抗作用。这些结果加深了我们对HS-铁(III)共沉淀环境效应的科学理解,并为探索它们在铬污染场地修复中的潜在应用提供了新的视角。