数字农科院2.0

Evaluation Of The Environment Risk, Fractions And Mobilization Of Nickel (Ni) In Sediments Of The Jialing River By Sediment Quality Guidelines, Sequential Extraction And Chelex-Agi Gel Dgt Probe

文献类型: 外文期刊

作者: Zhang, T; Li, LJ; Xu, F; Chen, XY; Du, L; Wang, XJ; Li, YX

作者机构:

关键词: Jialing River; Ni; Sqgs; Bcr; Dgt

期刊名称: APPLIED GEOCHEMISTRY

ISSN: 0883-2927

年卷期: 2020 年 118 卷

页码:

收录情况: JCR(2021版) ; EI(2021版)

摘要: The Jialing River is one of the largest tributaries of the Yangtze River and has the largest drainage area. Nickel (Ni) is a one of the most serious heavy metal contaminants in the downstream section of the Jialing River as a result of the prosperity of nearby chemical, electronic and mining industries. In the present work, sediment quality guidelines (SQGs), a Community Bureau of Reference (BCR) sequential extraction and the diffusive gradients in thin films (DGT) technique were applied to evaluate the environment risk, fractions and remobili- zation of Ni in the downstream Jialing River. The results indicated that the average total concentration of Ni (54.7 mg kg(-1) ) at all sites was higher than the background values of soil in China and Sichuan (26.9 and 35.8 mg kg(-1) , respectively). Environment risk assessment with four types of SQG values found that at three sites, the Ni concentration was over two high guideline values (probable effect concentration, PEC; effect range median, ERM), indicating that Ni may frequently pose a threat to the local aquatic ecosystem. The DGT results showed that C DGT -Ni had an inverse variation trend with C DGT -Fe and presented a significant increasing trend at the bottom of the DGT probes. Flux results revealed that sediments at S1, S2 and S3 were the source for Ni release across the sediment -water interface (SWI), and only S4 was a sink for Ni. Two further studies found that C DGT - Ni presented a significant negative correlation with C DGT -Fe. In addition, the "hotspot" of C DGT -Ni at the bottom correlated well with the ?dark area ? of C DGT -S. These results indicated that Fe and S were factors that mitigated the release of Ni in the sediments.

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