烟台芝罘区北部海域表层沉积物粒度特征及其对沉积动力环境的指示作用

Grain size characteristics of surface sediments in the northern waters of Zhifu District, Yantai and their indications of the sedimentary dynamical environment

  • 摘要: 本文对烟台芝罘区北部海域的80个表层沉积物样品进行了粒度组分、粒度参数、沉积物类型及输运趋势分析。结果表明研究区共有两种沉积物类型,分别是粉砂质砂和砂质粉砂,粒级组成以砂、粉砂和黏土为主,其中粉砂占据了优势地位,沉积物的平均粒径介于3.46Φ~6.10Φ。研究区沉积物东南部粒径较粗,分选较差,正偏,峰态尖锐;西北部粒径较细,分选较差,正偏,峰态更尖锐。通过研究区粒度多元统计以及输运趋势分析,将研究区划分为A区(远岸沉积区)和B区(近岸沉积区):A区主要沉积物类型为粉砂质砂,B区主要沉积物类型为砂质粉砂,A区与B区受山东半岛沿岸流、黄海暖流余流的影响,区域主要物质来源均为黄河入海沉积物。

     

    Abstract: In this paper, the grain size composition, grain size parameters, sediment types and transport trend of 80 surface sediment samples from the northern area of Zhifu District, Yantai were analyzed. The results show that there are two types of sediment in the study area, namely, silty sand and sandy silty sand. The grain size is mainly composed of sand, silt and clay, in which silt occupies the dominant position. The average particle size of the sediment ranges from 3.46Φ to 6.10Φ. In the study area, the sediment in the southeast of the study area has coarser particle size, poor sorting, positive bias, and sharp peak state, and the sediment in the northwest is fine, poor sorting, positive bias, and sharper peak state. Based on multivariate grain size statistics and transport trend analysis, the study area is divided into A region (far shore sediment area) and B region (near shore sediment area) : The main sediment type in A region is silty sand, and the main sediment type in B region is sandy silt. Both areas are affected by coastal current of Shandong Peninsula and residual current of Yellow Sea warm current, and the main material source in the region is the Yellow River sediment.

     

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