成海燕,姜胜辉,张 超,等. 渤海海峡表层沉积物地球化学特征[J]. 海洋地质前沿,2020,36(8):19-28. DOI: 10.16028/j.1009-2722.2020.015
    引用本文: 成海燕,姜胜辉,张 超,等. 渤海海峡表层沉积物地球化学特征[J]. 海洋地质前沿,2020,36(8):19-28. DOI: 10.16028/j.1009-2722.2020.015
    CHENG Haiyan, JIANG Shenghui, ZHANG Chao, ZHAO Dongdong. GEOCHEMICAL CHARACTERISTICS OF SURFACE SEDIMENS IN BOHAI STRAIT AND CONTROLLING FACTORS[J]. Marine Geology Frontiers, 2020, 36(8): 19-28. DOI: 10.16028/j.1009-2722.2020.015
    Citation: CHENG Haiyan, JIANG Shenghui, ZHANG Chao, ZHAO Dongdong. GEOCHEMICAL CHARACTERISTICS OF SURFACE SEDIMENS IN BOHAI STRAIT AND CONTROLLING FACTORS[J]. Marine Geology Frontiers, 2020, 36(8): 19-28. DOI: 10.16028/j.1009-2722.2020.015

    渤海海峡表层沉积物地球化学特征

    GEOCHEMICAL CHARACTERISTICS OF SURFACE SEDIMENS IN BOHAI STRAIT AND CONTROLLING FACTORS

    • 摘要: 通过对渤海海峡412个站位的表层沉积物粒度及123个站位的表层沉积物地球化学特征分析,探讨了其空间分布特征、元素相关性、元素组合特征、表层沉积物沉积动力环境及沉积物输运方式,揭示了沉积物地球化学特征的环境意义。结果表明:研究区表层沉积物常量元素以SiO2和Al2O3为主,随着沉积物粒径变粗SiO2含量逐渐增加,Al2O3含量逐渐减小。全区表层沉积物微量元素含量最高为Ba。各类型沉积物中元素的富集因子表明元素含量的变化服从粒度控制规律。采用聚类分析方法,将元素分布划分为5个分区:残留沉积区、老铁山水道区、水道东西两侧区、海峡中部区和海峡南部区。

       

      Abstract: Based on the grain size data of surface sediments collected at 412 stations and the geochemical data from 123 stations in the Bohai Strait, we discussed in this paper the spatial distribution pattern of elements, elements correlation, element assemblages, sedimentary dynamic environment and sediment transportation mechanism of the surface sediments, aiming at revealing the environmental significance of sediment geochemistry. The results indicate that the major elements of the surface sediments in the study area are predominated by SiO2 and Al2O3. The content of SiO2 increase and Al2O3 decrease gradually with the increase in grain size of sediments. The highest trace element in the surface sediments is Ba. The element enrichment factors of the sediments from the study area also indicate that the distribution of element content is controlled by the grain size of sediments. The results of cluster analysis further suggest that the spatial distribution of elements in the study area could be subdivided into 5 areass, namely, the relict deposits area, the Laotieshan area, the east and west sides of the watercourse, the central area of the Straits and the southern part of the Straits.

       

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