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富营养化湖泊沉积物中因溶解有机质络合和氧化锰还原导致的高镉污染。

High cadmium pollution from sediments in a eutrophic lake caused by dissolved organic matter complexation and reduction of manganese oxide.

机构信息

State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China.

State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China.

出版信息

Water Res. 2021 Feb 15;190:116711. doi: 10.1016/j.watres.2020.116711. Epub 2020 Nov 30.

Abstract

Eutrophication and metal pollution are global environmental problems. The risk of metal pollution is high in the eutrophic lakes because of high mobility of metal in sediments. However, the mechanism of cadmium (Cd) mobility in sediments is still unclear. Here we study the mobilization of Cd in sediments from the eutrophic Lake Taihu via monthly field monitoring of mobile Cd using diffusive gradient in thin films (DGT) and high resolution dialysis (HR-Peeper) techniques. We found a high mobility of Cd in sediments in February and March, resulting from reductive dissolution of Mn oxide mediation by high microbial activities, as shown by the similarities in distribution patterns of DGT-labile Cd and Mn. A two orders of magnitude increase in dissolved Cd concentrations (about 28 μg L) was observed in May and June, with dissolved Cd concentrations in overlying water about 110 times higher than the criteria continuous concentration set by Environmental Protection Agency. Hourly changes were found to coincide and correlate between dissolved Cd and dissolved organic matter (DOM) under simulated anaerobic conditions, strongly suggesting that the sudden outbreak of Cd pollution observed in the field resulted from the complexation of DOM with Cd in sediments. This was further supported by the NICA-Donnan model that more than 71% of dissolved Cd in the pore water in May and June was present as Cd-DOM complexes. Three components of DOM including humic-, tryptophan-, and tyrosine-like components in the sediments in June was identified using the fluorescence excitation emission matrix-parallel factor analysis. We found that Cd was stable complexed with tyrosine-like component. The Fourier transform infrared and two-dimensional correlation spectroscopy further revealed that Cd was bound to phenolic OH, alkene CC, alcoholic CO, aromatic CH, and alkene CH groups. Our study effectively promotes the understanding of Cd mobilization in sediments and highlights the risk of sudden Cd pollution events in the eutrophic lakes.

摘要

富营养化和金属污染是全球性的环境问题。由于沉积物中金属的高迁移性,富营养湖泊中的金属污染风险很高。然而,沉积物中镉(Cd)迁移的机制尚不清楚。在这里,我们通过使用扩散梯度薄膜(DGT)和高分辨率透析(HR-Peeper)技术对太湖富营养化湖泊中的沉积物中 Cd 的迁移进行了每月的现场监测,研究了 Cd 在沉积物中的迁移。我们发现,由于高微生物活性介导的 Mn 氧化物的还原溶解,2 月和 3 月沉积物中 Cd 的迁移性很高,这与 DGT-不稳定 Cd 和 Mn 的分布模式相似。5 月和 6 月观察到溶解 Cd 浓度(约 28μg/L)呈两个数量级增加,上覆水中的溶解 Cd 浓度比环境保护局设定的连续浓度标准高出约 110 倍。在模拟厌氧条件下,发现溶解 Cd 和溶解有机物(DOM)之间的小时变化相吻合且相关,这强烈表明野外观察到的 Cd 污染的突然爆发是由于 DOM 与沉积物中的 Cd 络合所致。NICA-Donnan 模型进一步支持了这一观点,该模型表明,5 月和 6 月孔隙水中溶解 Cd 的 71%以上以 Cd-DOM 络合物的形式存在。使用荧光激发发射矩阵-平行因子分析,鉴定了 6 月沉积物中三种 DOM 成分,包括腐殖质、色氨酸和酪氨酸样成分。我们发现 Cd 与酪氨酸样成分稳定络合。傅里叶变换红外和二维相关光谱进一步表明,Cd 与酚 OH、烯键 CC、醇 CO、芳基 CH 和烯键 CH 基团结合。我们的研究有效地促进了对沉积物中 Cd 迁移的理解,并强调了富营养湖泊中突然发生 Cd 污染事件的风险。

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