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湘江下游沉积物中稀土元素的分布、来源和污染。

Distribution, source and contamination of rare earth elements in sediments from lower reaches of the Xiangjiang River, China.

机构信息

School of Geographic Science, Hunan Normal University, Changsha, 410081, PR China; College of Geography and Tourism, Hengyang Normal University, Hengyang, 421002, PR China.

School of Geographic Science, Hunan Normal University, Changsha, 410081, PR China; Key Laboratory of Environmental Heavy-Metal Contamination and Ecological Remediation, Hunan Normal University, Changsha, 410081, PR China.

出版信息

Environ Pollut. 2023 Nov 1;336:122384. doi: 10.1016/j.envpol.2023.122384. Epub 2023 Aug 14.

Abstract

Rare earth elements (REEs) are emerging micropollutants in aquatic environments. In this study, concentrations of REEs and major elements, and mineralogical compositions of sediments from lower reaches of the Xiangjiang River (China) were analyzed using ICP-MS technique. The results suggested that sediments were characterized by terrigenous compositions TiO, SiO, AlO, KO, NaO and PO, and contained high concentrations of REEs with mean total REE concentrations (∑REE) of 318.7 mg/kg. REEs were moderately enriched in upper river sediments, and slightly or less enriched in downriver sediments. The normalized REE distribution pattern for sediments was characterized by flat shalelike and Eu depleted V-shape REE patterns, which indicated REEs in sediments were lithologically contributed from sedimentary rocks and granites distributed in the watershed respectively. REEs in sediments were hosted mainly in Fe-Mn oxides, and sulfide and organic matters that were characterized by middle REEs (MREE) enrichments relative to light REEs (LREE) and heavy REEs (HREE), and the distribution and differentiation of REEs in sediments were controlled by clays, Fe-Mn oxides, organic matters and finer grains; and also by accessory minerals (e.g., zircon) from granite. The distribution features of REEs in sediments and BCR extraction results suggested that the sediment REE enrichment resulted from additional REE input from anthropogenic sources, including those in discharges from sulfide-ore smelting industries at Zhuzhou city and from phosphate fertilizer plants at Xiangtan city along the river. Thus, sediments were contaminated with REEs in moderate degree in upper river area, and REE contamination was then formed by superimposing anthropogenic REEs on lithological residues. Finally, concentrations of Ce > 100 mg/kg, Gd > 8.12 mg/kg, ∑REE >274.9 mg/kg, ∑LREE >252.3 mg/kg and ∑HREE >28.8 mg/kg here were recommended as the REE contamination levels that represented as REE indices for identifying and rating REE contamination in this mining impacted river.

摘要

稀土元素(REEs)是水生环境中新兴的微量污染物。本研究采用 ICP-MS 技术分析了湘江下游沉积物中的 REEs 和主要元素浓度及矿物组成。结果表明,沉积物具有陆源组成 TiO 2 、SiO 2 、Al 2 O 3 、K 2 O、Na 2 O 和 PO 4 3- ,并含有高浓度的 REEs,∑REE 平均浓度为 318.7 mg/kg。上游河流沉积物中 REE 中等富集,下游沉积物中 REE 略有富集或低度富集。沉积物的归一化 REE 分布模式以平缓的似层状和 Eu 亏损的 V 形 REE 模式为特征,这表明沉积物中的 REE 分别来自流域内分布的沉积岩和花岗岩。沉积物中的 REE 主要赋存于 Fe-Mn 氧化物、硫化物和有机物中,相对于轻 REE(LREE)和重 REE(HREE),中 REE(MREE)富集,REE 在沉积物中的分布和分异受粘土、Fe-Mn 氧化物、有机物和细颗粒以及花岗岩中副矿物(如锆石)的控制。沉积物中 REE 的分布特征和 BCR 提取结果表明,沉积物的 REE 富集是由于人为源的额外 REE 输入,包括来自株洲市硫化矿冶炼厂和湘江沿岸湘潭市磷肥厂的排放。因此,上游地区河流沉积物中 REE 受到中度污染,REE 污染是人为 REE 叠加在岩石残留物上形成的。最后,建议将 Ce>100mg/kg、Gd>8.12mg/kg、∑REE>274.9mg/kg、∑LREE>252.3mg/kg 和∑HREE>28.8mg/kg 作为 REE 污染水平,作为识别和评价该矿区河流 REE 污染的 REE 指标。

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