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[近二十年来鄱阳湖流域河漫滩沉积物微量元素含量及污染水平变化]

[Changes in Concentrations and Pollution Levels of Trace Elements of Floodplain Sediments of Poyang Lake Basin in Recent Twenty Years].

作者信息

Li Kuo, Yang Ke, Peng Min, Liu Fei, Yang Zheng, Zhao Chuan-Dong, Cheng Hang-Xin

机构信息

School of Geosciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China.

Institute of Geophysical & Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, China.

出版信息

Huan Jing Ke Xue. 2021 Apr 8;42(4):1724-1738. doi: 10.13227/j.hjkx.202008083.

Abstract

Investigating the pollution conditions of trace elements in the Poyang Lake basin, identifying the pollution sources, evaluating the ecological risks play an important part in formulating the effective strategies for protecting the basin ecosystem. To understand the concentration characteristics, pollution levels, and ecological risks of twelve trace elements (Cd, Hg, Pb, As, Cu, Zn, Cr, Ni, Mn, Sb, W, and Sn) in the floodplain sediments of the five main tributaries in Poyang Lake basin in the past twenty years, we used the enrichment factor (EF) and modified pollution index (MPI) to quantify the pollution levels of the trace elements, and analyzed and discussed the pollution sources in the areas with significant pollution level changes. The results indicated that the concentrations of cadmium, zinc, manganese, tungsten and lead in the floodplain sediments of the Poyang Lake basin during the past twenty years have increased by 134%, 26%, 41%, 25%, and 8%, respectively, and mercury, arsenic, chromium, nickel, antimony, and tin have decreased by 35%, 15%, 22%, 10%, 14%, and 13%, respectively, while copper has not changed significantly. The concentrations of cadmium in the Raohe River, Ganjiang River, and Xinjiang River basins have increased by 331%, 151%, and 107%, while mercury decreased in the Fuhe River, Ganjiang River, and Xiushui River basins by 87%, 41%, and 40%, respectively. The classification results based on the EF indicated that the changes in the pollution levels of trace elements in the Poyang Lake basin were characterized by the aggravation of cadmium pollution and the degradation of mercury pollution, the pollution level of cadmium in the Ganjiang River basin was upgraded to moderate and significant, the pollution level of cadmium in the Le'an River was upgraded to very high, and the pollution level of mercury in the Fuhe River basin was reduced to unpolluted or minimal. The MPI classification results established that the increase in the cadmium pollution had intensified the comprehensive pollution in the Poyang Lake basin, causing the proportion of severely and heavily polluted sites to be raised from 17% to 33%. The MRI classification results also demonstrated that the proportion of very high ecological risk sites have increased from 11% to 22%. The element with the highest MRI contribution rate changed from mercury to cadmium, which was caused by the reduction of the ecological risk level from very high to moderate. The results demonstrated that the significant pollution changes in the trace elements in the floodplain sediments of the Poyang Lake basin were primarily caused by human activities, such as mineral exploitation, smelting, and industrial and agricultural production. Our findings can provide scientific evidence for the prevention and control of river pollution and the optimal management of a watershed ecosystem.

摘要

调查鄱阳湖流域微量元素污染状况、识别污染源、评估生态风险,对制定有效的流域生态系统保护策略具有重要意义。为了解鄱阳湖流域五条主要支流河漫滩沉积物中12种微量元素(镉、汞、铅、砷、铜、锌、铬、镍、锰、锑、钨和锡)在过去二十年中的浓度特征、污染水平及生态风险,我们采用富集因子(EF)和修正污染指数(MPI)来量化微量元素的污染水平,并对污染水平变化显著区域的污染源进行了分析和讨论。结果表明,过去二十年鄱阳湖流域河漫滩沉积物中镉、锌、锰、钨和铅的浓度分别增加了134%、26%、41%、25%和8%,汞、砷、铬、镍、锑和锡的浓度分别下降了35%、15%、22%、10%、14%和13%,而铜的浓度变化不显著。饶河流域、赣江流域和信江流域镉的浓度分别增加了331%、151%和107%,抚河流域、赣江流域和修水河流域汞的浓度分别下降了87%、41%和40%。基于EF的分类结果表明,鄱阳湖流域微量元素污染水平变化的特征是镉污染加剧和汞污染减轻,赣江流域镉的污染水平升级为中度和显著,乐安河镉的污染水平升级为极高,抚河流域汞的污染水平降至未污染或轻微污染。MPI分类结果表明镉污染的增加加剧了鄱阳湖流域的综合污染,使重度和严重污染站点的比例从17%提高到33%。MRI分类结果还表明,生态风险极高的站点比例从11%增加到22%。MRI贡献率最高的元素从汞变为镉,这是由于生态风险水平从极高降至中度所致。结果表明,鄱阳湖流域河漫滩沉积物中微量元素的显著污染变化主要是由矿产开采、冶炼以及工农业生产等人类活动引起的。我们的研究结果可为河流污染防治和流域生态系统的优化管理提供科学依据。

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