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在藻类到大型水生植物的生境变化下,湖泊沉积物中钨的迁移和转化特征。

Tungsten migration and transformation characteristics in lake sediments under changing habitats from algae to macrophytes.

机构信息

Nanjing Institute of Environmental Sciences, Ministry of Ecology and Environment, Nanjing 210042, China; The National Key Laboratory of Water Disaster Prevention, Hohai University, Nanjing 210098, China.

Nanjing Institute of Environmental Sciences, Ministry of Ecology and Environment, Nanjing 210042, China.

出版信息

J Hazard Mater. 2024 Dec 5;480:136134. doi: 10.1016/j.jhazmat.2024.136134. Epub 2024 Oct 10.

Abstract

Tungsten (W), a toxic and hazardous pollutant, poses substantial risks to both aquatic life and human health. However, the available understanding of the migration properties of W in lake sediments under various habitats is still limited. This study was designed to evaluate variations in the concentrations of soluble W, manganese (Mn), and iron (Fe) in the summer season by applying a high-resolution Peeper sampling device. According to the results, soluble W concentrations and release fluxes were higher in the pore water of sediments in algae-dominated lake areas than in areas dominated by aquatic plants. This result indicates that the competition for adsorption between algae-derived dissolved organic matter and W, as well as the reductive dissolution caused by dissolved organic matter on Fe (III)/Mn (IV) (hydroxyl) oxides, contributes to the release of W from lake sediments. W uptake by aquatic plants and in-situ formation of Fe (III)/Mn (IV) (hydroxyl) oxides might be the primary factor that controls W release from lake sediments. Aquatic plants can effectively control W release from sediments. The findings of this work provide a scientific basis for the effective control of W release from shallow lake sediments.

摘要

钨(W)是一种有毒有害的污染物,对水生生物和人类健康构成重大风险。然而,对于不同生境下湖泊沉积物中 W 的迁移特性的现有认识仍然有限。本研究旨在通过应用高分辨率的 Peeper 采样装置来评估夏季可溶性 W、锰(Mn)和铁(Fe)浓度的变化。结果表明,藻类占优势的湖区沉积物中孔隙水中的可溶性 W 浓度和释放通量高于水生植物占优势的区域。这一结果表明,藻类来源的溶解有机质与 W 之间的吸附竞争,以及溶解有机质对 Fe(III)/Mn(IV)(氢氧)氧化物的还原溶解,导致 W 从湖泊沉积物中释放。水生植物对 W 的吸收和原位形成的 Fe(III)/Mn(IV)(氢氧)氧化物可能是控制 W 从湖泊沉积物中释放的主要因素。水生植物可以有效地控制 W 从沉积物中的释放。这项工作的结果为有效控制浅水湖泊沉积物中 W 的释放提供了科学依据。

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