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Water, sediment and agricultural soil contamination from an ion-adsorption rare earth mining area

机译:离子吸附稀土矿区的水,沉积物和农业土壤污染

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Due to their specific properties, ion-adsorption rare earth mine sites may be a threat for adjacent environments. This work was undertaken to assess whether former mining operations on ion-adsorption rare earth mine sites have a significant impact on water bodies and soils of the surrounding environments. Tailing soil materials, stream waters and sediments, and farmland soils were collected from one of the largest ion-adsorption rare earth mine sites worldwide (Southern China). Total concentrations of rare earth elements (REEs), Fe, Al, etc., and pH were measured. Results revealed high concentrations of REEs in tailing soils (392 mg kg(-1)), stream waters (4460 mu g L-1), sediments (462 mg kg(-1)) and farmland soils (928 mg kg(-1)) in comparison with control sites. In the tailing profiles, light REEs (LREEs) were preferentially leached compared to middle REEs (MREEs) and heavy REEs (HREEs). Anomalies in tailings and stream water indicated strong soil weathering (Eu) and leaching activities (Ce) within the tailings. The MREE enriched pattern in stream water was more related to water parameters such as Al and Fe oxides, and ligands, than to the source of REEs. Anomalies also indicated that REEs contamination in the farmland soils was mainly originated from the stream water contaminated by the leaching from the tailings. In conclusion, a heavy REEs pollution was recorded in the surrounding environment of ion adsorption rare earth mine. REEs fractionation, Ce and Eu anomalies provided an insight to the understanding of REEs leaching and soil weathering processes, and REEs environmental fate in rare earth mining area. (C) 2018 Elsevier Ltd. All rights reserved.
机译:由于其特殊的特性,离子吸附稀土矿场可能对邻近环境构成威胁。进行这项工作是为了评估以前在离子吸附稀土矿场上进行的采矿作业是否会对周围环境的水体和土壤产生重大影响。尾矿土材料,溪流水和沉积物以及农田土壤是从全球(中国南方)最大的离子吸附稀土矿场之一收集的。测量了稀土元素(REE),Fe,Al等的总浓度和pH。结果显示,尾矿土壤(392 mg kg(-1)),溪流水(4460 mu g L-1),沉积物(462 mg kg(-1))和农田土壤(928 mg kg(-1))中的REE浓度很高。 ))与控制站点相比。在尾矿剖面中,轻质稀土元素(LREEs)优先于中层稀土元素(MREEs)和重质稀土元素(HREEs)浸出。尾矿和溪流水的异常表明尾矿内部土壤风化(Eu)强,浸出活性(Ce)强。溪流水中富含MREE的模式与水参数(如Al和Fe氧化物以及配体)的关系更大,而不是与REE的来源有关。异常现象还表明,农田土壤中的稀土元素污染主要来自尾矿浸出所污染的溪水。总之,在离子吸附稀土矿的周围环境中记录到严重的REEs污染。稀土元素的分馏,铈和Eu的异常为了解稀土矿区的稀土元素浸出和土壤风化过程以及稀土元素的环境命运提供了见识。 (C)2018 Elsevier Ltd.保留所有权利。

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