李近元,刘建民,方念乔,等. 山东黑山岛近海风电场海底地形地貌及沉积特征[J]. 海洋地质前沿,2020,36(10):84-92. DOI: 10.16028/j.1009-2722.2020.057
    引用本文: 李近元,刘建民,方念乔,等. 山东黑山岛近海风电场海底地形地貌及沉积特征[J]. 海洋地质前沿,2020,36(10):84-92. DOI: 10.16028/j.1009-2722.2020.057
    LI Jinyuan, LIU Jianmin, FANG Nianqiao, TANG Qichao, CAO Shugang, YAO Xinglong. SUBMARINE TOPOGRAPHY AND SEDIMENTARY CHARACTERISTICS OF OFFSHORE WIND FARM IN HEISHAN ISLAND OF SHANDONG[J]. Marine Geology Frontiers, 2020, 36(10): 84-92. DOI: 10.16028/j.1009-2722.2020.057
    Citation: LI Jinyuan, LIU Jianmin, FANG Nianqiao, TANG Qichao, CAO Shugang, YAO Xinglong. SUBMARINE TOPOGRAPHY AND SEDIMENTARY CHARACTERISTICS OF OFFSHORE WIND FARM IN HEISHAN ISLAND OF SHANDONG[J]. Marine Geology Frontiers, 2020, 36(10): 84-92. DOI: 10.16028/j.1009-2722.2020.057

    山东黑山岛近海风电场海底地形地貌及沉积特征

    SUBMARINE TOPOGRAPHY AND SEDIMENTARY CHARACTERISTICS OF OFFSHORE WIND FARM IN HEISHAN ISLAND OF SHANDONG

    • 摘要: 山东海域海上风资源丰富,风电规模化开发条件好。为了解海底地形地貌及沉积物分布特征,以顺利推进近海风电场的开发,选取黑山岛附近海域作为研究对象,在研究海域进行了综合地质地球物理调查。对调查数据的分析表明,研究区域海底地形平缓,整体水体较浅,最浅10 m,最深25 m,平均17.5 m。研究区内沉积物主要呈青灰色、灰色、浅褐色。沉积物类型主要粉砂,粉砂含量均在75%以上,全区分布。沉积物峰态主要表现为平坦、中等、尖锐3种。研究区西区海底表层沉积物分选系数为1.35~1.8,东区海底表层沉积物分选系数为0.9~1.75。整个研究区海域表层沉积物平均粒径在4.3Φ~5.9Φ之间变化,沉积物颗粒较细,以粉砂为主。分析表明,这种地形地貌及沉积物特点反映出研究海域属于离岸海域,水动力作用较弱,适于进行海上风电开发等工程建设。

       

      Abstract: The sea area off the Shandong Peninsula is rich in wind resources and there are excellent conditions for large-scale development of wind energy. In order to understand the topography and sediment distribution patterns of the seabed, so as to promote the development of offshore wind farms smoothly, the sea area near the Heishan island was selected as a case for geological study. An integrated geological and geophysical survey was then undertaking in the selected area. The survey data suggests that the seafloor topography of the study area is rather gentle and the water depth changes from 10 m to 25 m, 17.5 m on average. The sediment in the study area is cyan gray, gray and light brown in color and dominated by silty sand which covers over 75% of the whole area. The kurtosis of the sediment varies from flat to medium to sharp. In the west part of the study area, the sorting of the seafloor sediment changes from 1.35 up to 1.80. while in the east part the sorting of the sea bottom sediment varies from 0.90 to 1.75. The mean grain size of bottom sediments of the whole study area ranges from 4.3Φ to 5.9 Φ and is silt dominated. The topography and sediment characteristics reflect that the study area is an area with weak hydrodynamic effect and therefore suitable for offshore wind power development and other kinds of sub-bottom constructions.

       

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