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中国包头某尾矿库周边土壤中稀土元素的地球化学形态

Geochemical fractions of rare earth elements in soil around a mine tailing in Baotou, China.

作者信息

Wang Lingqing, Liang Tao

机构信息

Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.

出版信息

Sci Rep. 2015 Jul 22;5:12483. doi: 10.1038/srep12483.

Abstract

Rare earth mine tailing dumps are environmental hazards because tailing easily leaches and erodes by water and wind. To assess the influence of mine tailing on the geochemical behavior of rare earth elements (REEs) in soil, sixty-seven surface soil samples and three soil profile samples were collected from different locations near China's largest rare earth mine tailing. The total concentration of REEs in surface soils ranged from 156 to 5.65 × 10(4) mg·kg(-1) with an average value of 4.67 × 10(3) mg·kg(-1), which was significantly higher than the average value in China (181 mg·kg(-1)). We found obvious fractionation of both light and heavy REEs, which was supported by the North American Shale Composite (NASC) and the Post-Archean Average Australian Shale (PAAS) normalized concentration ratios calculated for selected elements (La(N)/Yb(N), La(N)/Sm(N) and Gd(N)/Yb(N)). A slightly positive Ce anomaly and a negative Eu anomaly were also found. For all 14 REEs in soils, enrichment was intensified by the mine tailing sources and influenced by the prevailing wind.

摘要

稀土矿尾矿堆是环境危害源,因为尾矿很容易被水和风淋滤和侵蚀。为了评估尾矿对土壤中稀土元素(REEs)地球化学行为的影响,从中国最大的稀土矿尾矿附近的不同地点采集了67个表层土壤样品和3个土壤剖面样品。表层土壤中稀土元素的总浓度范围为156至5.65×10⁴mg·kg⁻¹,平均值为4.67×10³mg·kg⁻¹,显著高于中国的平均值(181mg·kg⁻¹)。我们发现轻稀土和重稀土均有明显的分馏现象,这通过为选定元素(La(N)/Yb(N)、La(N)/Sm(N)和Gd(N)/Yb(N))计算的北美页岩组合(NASC)和后太古代澳大利亚页岩平均(PAAS)归一化浓度比得到了证实。还发现了轻微的正铈异常和负铕异常。对于土壤中的所有14种稀土元素,尾矿源加剧了其富集,且受盛行风的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dd91/4510494/02985133655d/srep12483-f1.jpg

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