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离子吸附型稀土矿区水、沉积物和农田土壤污染

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

机构信息

School of Environmental Science and Engineering, Sun Yat-sen University, Guangzhou, China; Guangdong Provincial Key Laboratory of Environmental Pollution Control and Remediation Technology, Guangzhou, China; Guangdong Provincial Engineering Research Center for Heavy Metal Contaminated Soil Remediation (Sun Yat-sen University), Guangzhou, China.

School of Environmental Science and Engineering, Sun Yat-sen University, Guangzhou, China; Guangdong Provincial Key Laboratory of Environmental Pollution Control and Remediation Technology, Guangzhou, China; Guangdong Provincial Engineering Research Center for Heavy Metal Contaminated Soil Remediation (Sun Yat-sen University), Guangzhou, China.

出版信息

Chemosphere. 2019 Feb;216:75-83. doi: 10.1016/j.chemosphere.2018.10.109. Epub 2018 Oct 17.

Abstract

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), stream waters (4460 μg L), sediments (462 mg kg) and farmland soils (928 mg kg) 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.

摘要

由于其特殊性质,离子吸附型稀土矿可能对相邻环境构成威胁。本研究旨在评估离子吸附型稀土矿的开采作业是否对周围环境的水体和土壤产生重大影响。从世界上最大的离子吸附型稀土矿之一(中国南方)采集了尾矿土壤材料、溪流水和沉积物以及农田土壤。测量了稀土元素(REEs)、Fe、Al 等的总量浓度和 pH 值。结果表明,与对照点相比,尾矿(392mgkg)、溪流水(4460μg/L)、沉积物(462mgkg)和农田土壤(928mgkg)中的 REEs 浓度较高。在尾矿剖面中,轻REE(LREE)优先于中REE(MREE)和重REE(HREE)浸出。尾矿和溪流水中的异常表明尾矿内发生强烈的土壤风化(Eu)和淋滤活动(Ce)。溪流水中的 MREE 富集模式与 Al 和 Fe 氧化物以及配体等水参数的关系比 REEs 源更为密切。异常还表明,农田土壤中 REEs 的污染主要来源于受尾矿淋滤污染的溪流水。总之,在离子吸附型稀土矿的周围环境中记录了严重的 REEs 污染。REEs 分馏、Ce 和 Eu 异常为了解 REEs 的淋滤和土壤风化过程以及稀土矿区 REEs 的环境归宿提供了线索。

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