张洪运, 栾振东, 李近元. 海南东方岸外风电场海底地形地貌特征[J]. 海洋地质前沿, 2016, 32(9): 1-6. DOI: 10.16028/j.1009-2722.2016.09001
    引用本文: 张洪运, 栾振东, 李近元. 海南东方岸外风电场海底地形地貌特征[J]. 海洋地质前沿, 2016, 32(9): 1-6. DOI: 10.16028/j.1009-2722.2016.09001
    ZHANG Hongyun, LUAN Zhendong, LI Jinyuan. RESEARCH OF SUBMARINE TOPGRAPHY AND GEOMORPHOLOGY IN DONGFANG OFFSHORE WIND FARM, HAINAN[J]. Marine Geology Frontiers, 2016, 32(9): 1-6. DOI: 10.16028/j.1009-2722.2016.09001
    Citation: ZHANG Hongyun, LUAN Zhendong, LI Jinyuan. RESEARCH OF SUBMARINE TOPGRAPHY AND GEOMORPHOLOGY IN DONGFANG OFFSHORE WIND FARM, HAINAN[J]. Marine Geology Frontiers, 2016, 32(9): 1-6. DOI: 10.16028/j.1009-2722.2016.09001

    海南东方岸外风电场海底地形地貌特征

    RESEARCH OF SUBMARINE TOPGRAPHY AND GEOMORPHOLOGY IN DONGFANG OFFSHORE WIND FARM, HAINAN

    • 摘要: 利用Sonic 2024多波束测深系统对海南东方岸外进行高精度的水深测量,根据所测数据绘制海底水深地形地貌图等。研究区水深范围在8~32 m之间,西部深,东部浅,水深向岸线方向变浅,地势东北高,西南低。研究区存在2种典型的海底地形地貌,西部的U型冲刷谷和两片沙波活动区。U型谷内水深较大,地形较为平坦,无大的起伏。沙波活动区的沙波规模较大,以大型和巨型沙波为主,沙波脊线基本沿WE向,但两片沙波并不完全相同,存在空间差异,沙波的形态参数上也存在一定差异。

       

      Abstract: A high resolution bathymetric survey has been carried out using the Sonic 2024 Multi-Beam Sounding System in the Dongfang Wind Farm offshore Hainan Island. A lot of images such as the bathymetric charts, 3D submarine geomorphologic maps etc are made from the survey data. The water depth depth of the study area ranges between 8 to 32 meters and it is deeper in the west rather than in the east. As the results, the terrain is higher in the northeast. There are two submarine geomorphological features in the study area, a U-shaped erosion valley and two sand wave areas. The water depth of the U-shaped valley is deeper than any part of the study area. The topography of the valley bottom is relatively flat, and there are no big relieves. The sand waves are widely distributed and belong to large and giant sand waves. The crests of sand waves are basically in E-W direction. But there are differences in spatial distribution patterns and geometric parameters between the two sand wave areas.

       

    /

    返回文章
    返回