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中国渤海表层和岩芯沉积物中镉的地球化学来源、沉积及环境风险评估

Geochemical source, deposition, and environmental risk assessment of cadmium in surface and core sediments from the Bohai Sea, China.

作者信息

Ningjing Hu, Peng Huang, Hui Zhang, Xiaojing Wang, Aimei Zhu, Jihua Liu, Xuefa Shi

机构信息

First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China.

Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China.

出版信息

Environ Sci Pollut Res Int. 2017 Jan;24(1):827-843. doi: 10.1007/s11356-016-7800-0. Epub 2016 Oct 18.

Abstract

Geochemical sources, spatio-temporal distribution, and associated environmental risk of Cd in the Bohai Sea were investigated using data from 405 surface sediment samples and two sediment cores. Local point Cd sources, TOC content, and currents are the main controlling factors of Cd distribution. The contribution of Cd from river discharge surpasses that from atmospheric deposition. Sediment-quality guidelines, enrichment factors, and chemical fraction analysis were used to assess metal toxicity in the collected sediments. Results show that Bohai Sea sediments have a moderate Cd enrichment level. This enrichment poses a high risk due to the relatively high mobility and bioavailability of Cd despite measured levels below sediment-quality guidelines at most stations. Vertical profiles of Cd concentrations, Al-normalized enrichment factors, and excess burial fluxes combined with Pb dating reveal the history of Cd pollution in the Bohai Sea over the last century. Data show Cd unvaried before the 1800s, a slight increase from the 1800s to the late 1950s, a decrease from the late 1960s to the 1970s, and an increase from the 1980s to 2001, including a relatively high value in 1998. Historic variation in Cd is closely associated with both natural and anthropogenic activities.

摘要

利用405个表层沉积物样本和两个沉积岩芯的数据,对渤海中镉的地球化学来源、时空分布及相关环境风险进行了调查。局部点源镉、总有机碳含量和海流是控制镉分布的主要因素。河流排放的镉贡献超过大气沉降。采用沉积物质量准则、富集因子和化学形态分析来评估所采集沉积物中的金属毒性。结果表明,渤海沉积物镉富集水平中等。尽管大多数站点测得的镉含量低于沉积物质量准则,但由于镉具有较高的迁移性和生物有效性,这种富集仍带来了高风险。镉浓度、铝归一化富集因子和过剩埋藏通量的垂直剖面结合铅测年揭示了渤海过去一个世纪的镉污染历史。数据显示,19世纪以前镉含量没有变化,19世纪到20世纪50年代末略有增加,20世纪60年代末到70年代有所下降,20世纪80年代到2001年有所上升,其中1998年出现了一个相对较高的值。镉的历史变化与自然活动和人为活动都密切相关。

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