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Spatial Distributions and Deposition Chronology of Short Chain Chlorinated Paraffins in Marine Sediments across the Chinese Bohai and Yellow Seas

机译:渤海和黄海海洋沉积物中短链氯化石蜡的空间分布和沉积年表

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摘要

As the most complex halogenated contaminants, short chain chlorinated paraffins (SCCPs) are scarcely reported in marine environments. In this work, a total of 117 surficial sediment (0-3 cm) samples and two sediment cores were collected from the Chinese Bohai and Yellow Seas to systematically study the spatial and temporal trends of SCCPs at a large scale in the Chinese marine environment. Total SCCP concentrations in the surficial sediments were in the range of 14.5-85.2 ng g~(-1) (dry weight, Aw.) with an average level of 38.4 ng g~(-1) d.w. Spatial distribution showed a decreasing trend with the distance from the coast to the open waters. Compositional pattern analysis suggested that C_10 was the most predominant homologue group, followed by C_(11),C_(12), and C_(13) homologue groups. The concentrations of total SCCPs in sediment cores ranged from 11.6 to 94.7 ng g~(-1) d.w. for YS1 and from 14.7 to 195.6 ng g~(-1) d.w. for YS2, with sharp rise from the early 1950s to present based on ~(210)Pb dating technique. The historical records in cores correspond well to the production and usage changes of CPs in China. Multivariate regression statistics indicate TOC, latitude and longitude are the major factors influencing surficial SCCP levels in the Chinese East Seas by combining analysis with the data from the East China Sea (R~2 = 0.332, p < 0.01). These findings indicated that the sources of SCCPs were mainly from river outflows via ocean current and partly from atmospheric depositions by East Asian monsoon in the sampling areas.
机译:作为最复杂的卤化污染物,在海洋环境中几乎没有报道过短链氯化石蜡(SCCP)。在这项工作中,从中国渤海和黄海总共收集了117个表面沉积物(0-3厘米)样本和两个沉积物核心,以系统地研究中国海洋环境中短链氯化石蜡的时空趋势。表层沉积物中的短链氯化石蜡总浓度在14.5-85.2 ng g〜(-1)(干重,Aw。)范围内,平均水平为38.4 ng g〜(-1)d.w。空间分布随着从海岸到开阔水域的距离而减小。组成模式分析表明,C_10是最主要的同源物组,其次是C_(11),C_(12)和C_(13)同源物组。沉积物芯中总短链氯化石蜡的浓度范围为11.6至94.7 ng g〜(-1)d.w。 YS1的浓度为14.7至195.6 ng g〜(-1)d.w.根据〜(210)Pb测年技术,YS2的数量从1950年代初到现在急剧上升。核心的历史记录与中国CP的生产和使用变化非常吻合。多元回归统计表明,结合分析和来自东海的数据,TOC,纬度和经度是影响中国东海表层短链氯化石蜡水平的主要因素(R〜2 = 0.332,p <0.01)。这些发现表明,短链氯化石蜡的来源主要是来自洋流的河流流出,部分是来自东亚季风在采样区的大气沉积。

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  • 来源
    《Environmental Science & Technology》 |2013年第20期|11449-11456|共8页
  • 作者单位

    State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, People's Republic of China School of Chemistry and Chemical Engineering, University of Chinese Academy of Sciences, Beijing 100049, People's Republic of China;

    State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, People's Republic of China Environment Research Institute, Shandong University, Jinan 250100, People's Republic of China;

    Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100,People's Republic of China;

    State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, People's Republic of China;

    State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, People's Republic of China;

    School of Public Health, University of Illinois at Chicago, Chicago, Illinois 60612, United States;

    State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, People's Republic of China;

    State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, People's Republic of China;

    Institute of Polar Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026,People's Republic of China;

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