长江口外海域岩心沉积物地球化学特征及其对人类活动的响应

董爱国, 翟世奎, Zabel Matthias, 于增慧, 褚忠信. 长江口外海域岩心沉积物地球化学特征及其对人类活动的响应[J]. 海洋地质与第四纪地质, 2009, 29(4): 107-114. doi: 10.3724/SP.J.1140.2009.04107
引用本文: 董爱国, 翟世奎, Zabel Matthias, 于增慧, 褚忠信. 长江口外海域岩心沉积物地球化学特征及其对人类活动的响应[J]. 海洋地质与第四纪地质, 2009, 29(4): 107-114. doi: 10.3724/SP.J.1140.2009.04107
DONG Aiguo, ZHAI Shikui, Zabel Matthias, YU Zenghui, CHU Zhongxin. GEOCHEMISTRY CHARACTERS OF THE CORE SEDIMENTS IN THE YANGTZE ESTUARY AND THE RESPONSE TO HUMAN ACTIVITIES[J]. Marine Geology & Quaternary Geology, 2009, 29(4): 107-114. doi: 10.3724/SP.J.1140.2009.04107
Citation: DONG Aiguo, ZHAI Shikui, Zabel Matthias, YU Zenghui, CHU Zhongxin. GEOCHEMISTRY CHARACTERS OF THE CORE SEDIMENTS IN THE YANGTZE ESTUARY AND THE RESPONSE TO HUMAN ACTIVITIES[J]. Marine Geology & Quaternary Geology, 2009, 29(4): 107-114. doi: 10.3724/SP.J.1140.2009.04107

长江口外海域岩心沉积物地球化学特征及其对人类活动的响应

  • 基金项目:

    国家重点基础研究发展规划项目(2002CB412409)

    教育部新教师基金项目(200804231011)

详细信息
    作者简介: 董爱国(1982-),男,博士生,研究方向为环境地球化学,E-mail:aiguo.dong@gmail.com
  • 中图分类号: P736.41

GEOCHEMISTRY CHARACTERS OF THE CORE SEDIMENTS IN THE YANGTZE ESTUARY AND THE RESPONSE TO HUMAN ACTIVITIES

  • 对长江口外海域Y16站岩心沉积物中元素含量和粒度组成进行了分析,并通过137Cs测定了年龄。结果表明,该岩心沉积物中元素含量在垂向上的变化与沉积物粒度组成的变化密切相关,根据元素含量的变化特征可将其分为3段:1966年之前、1967-1989年和1990-2006年。R型因子分析表明,影响该岩心沉积物中元素含量变化的主要因素为陆源物质供给。另外,生物沉积作用和人为污染对部分元素含量的变化有一定影响。元素含量的变化特征在前两个阶段主要与流域自然过程相联系,在后一阶段(1990-2006年)人为污染对沉积物中Pb和Zn元素含量的变化有所影响,但这种影响在长江大量输沙的背景下被明显减少。目前,由于长江输沙量的大幅下降(2006年长江输沙量仅为0.85亿t)以及人为污染影响程度的增强(煤、石油燃料消耗的持续增加以及工业的持续发展),未来长江口海域重金属元素的污染情况将面临更大的挑战。
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出版历程
收稿日期:  2009-05-30
修回日期:  2009-06-20

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