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北黄海泥质区多环芳烃与黑碳的沉积记录
引用本文:崔敏,陈颖军,方引,林田,田崇国,潘晓辉,唐建辉.北黄海泥质区多环芳烃与黑碳的沉积记录[J].海洋学报,2015,37(8):39-46.
作者姓名:崔敏  陈颖军  方引  林田  田崇国  潘晓辉  唐建辉
作者单位:1.中国科学院烟台海岸带研究所 海岸带环境过程与生态修复重点实验室 山东省海岸带环境过程重点实验室, 山东 烟台 264003;中国科学院大学, 北京 100049
基金项目:国家自然科学基金(41073064,41273135); 中国科学院知识创新工程重要方向项目(KZCX2-YW-QN210)。
摘    要:在北黄海中部泥质区采集柱状沉积物样品,对多环芳烃(PAHs)和黑碳(BC)的含量和来源进行研究。结果表明:(1)PAHs的含量变化范围为207~611ng/g;BC的含量变化范围为0.560~1.32mg/g;(2)对比低分子量(LMW)和高分子量(HMW)PAHs含量的历史变化趋势,发现1980s之前的PAHs主要来自于生物质的低温燃烧,之后主要来自于化石燃料的高温热解;(3)1920s之前,PAHs与BC含量基本保持稳定且处于较低值。1920s-1980s,PAHs含量受工业化和煤炭发展的影响较大,开始出现增长趋势。1980-1990s,由于能源消耗量的大幅度增加,导致PAHs和BC的含量迅速升高并达到最大值(1996年)。1990s初期-2000s初期,由于清洁能源的使用等原因,PAHs与BC含量都开始下降。(4)对PAHs和BC含量进行Spearman相关性分析,得出在1920年之前和1920-1980年之间,BC和PAHs含量无显著性相关(r=-0.25,P0.05,n=34;r=0.06,P0.06,n=11);而1980年之后,BC和PAHs含量呈显著性相关(r=0.90,P=0.04,n=5)。

关 键 词:多环芳烃    黑碳    沉积记录    北黄海
收稿时间:2014/10/8 0:00:00
修稿时间:4/8/2015 12:00:00 AM

Sedimentary records of PAHs and BC from mud area of the central northern Yellow Sea,China
Cui Min,Chen Yingjun,Fang Yin,Lin Tian,Tian Chongguo,Pan Xiaohui and Tang Jianhui.Sedimentary records of PAHs and BC from mud area of the central northern Yellow Sea,China[J].Acta Oceanologica Sinica (in Chinese),2015,37(8):39-46.
Authors:Cui Min  Chen Yingjun  Fang Yin  Lin Tian  Tian Chongguo  Pan Xiaohui and Tang Jianhui
Institution:Shandong Provincial Key Laboratory of Coastal Environmental, Processes Key Laboratory of Coastal Environmental Processes and Ecological Remediation, Yantai Institute of Coastal Zone Research Chinese Academy of Science, Yantai 264003, China;University of Chinese Academy of Sciences, Beijing 100049, China,Shandong Provincial Key Laboratory of Coastal Environmental, Processes Key Laboratory of Coastal Environmental Processes and Ecological Remediation, Yantai Institute of Coastal Zone Research Chinese Academy of Science, Yantai 264003, China,Shandong Provincial Key Laboratory of Coastal Environmental, Processes Key Laboratory of Coastal Environmental Processes and Ecological Remediation, Yantai Institute of Coastal Zone Research Chinese Academy of Science, Yantai 264003, China;University of Chinese Academy of Sciences, Beijing 100049, China,State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry Chinese Academy of Sciences, Guiyang 550002, China,Shandong Provincial Key Laboratory of Coastal Environmental, Processes Key Laboratory of Coastal Environmental Processes and Ecological Remediation, Yantai Institute of Coastal Zone Research Chinese Academy of Science, Yantai 264003, China,Shandong Provincial Key Laboratory of Coastal Environmental, Processes Key Laboratory of Coastal Environmental Processes and Ecological Remediation, Yantai Institute of Coastal Zone Research Chinese Academy of Science, Yantai 264003, China and Shandong Provincial Key Laboratory of Coastal Environmental, Processes Key Laboratory of Coastal Environmental Processes and Ecological Remediation, Yantai Institute of Coastal Zone Research Chinese Academy of Science, Yantai 264003, China
Abstract:Concentrations and sources of polycyclic aromatic hydrocarbons (PAHs) and black carbon (BC) were investigated based on a sediment core collected in the mud area of the central northern Yellow Sea. Results showed that: (1) The concentration of PAHs were in the value of 207 to 611 ng/g, and the values for BC were 0.560 to 1.32 mg/g.(2)The comparison of low-molecular-weighted(LMW) and high-molecular-weighed (HMW) PAHs indicated that biomass burning with relatively low temperature was their main source prior to 1980s, and shifted to fossil fuels with higher combustion temperature after 1980s. (3) Before 1920s, the concentration of PAHs and BC remained in stable and lower levels. In 1920s-1980s, PAHs concentrations began to increase which could be largely contributed to the rapid industrialization and coal usage in adjacent areas. After 1980s, the increase of energy consumption and vehicle population account for the continued increase of PAHs and BC concentrations, which reached to their maximum values about 1996, But the use of clean energy made them decreased since 1990s. (4) Before 1920s and 1920s-1980s, there are no correlation between PAHs and BC (r=-0.25, P>0.05, n=34; r=0.06, P>0.06, n=11). After 1980, there is a strong association of PAHs and BC (r=0.90, P=0.04, n=5).
Keywords:PAHs  BC  sedimentary record  northern Yellow Sea
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