1938—2023年庄河南尖岬角附近淤泥质潮滩地形冲淤演变规律

    Erosion and Accretion Evolution Law of the Muddy Tidal Flat Topography near the Nanjian of Zhuanghe (1938—2023)

    • 摘要: 庄河南尖海岸是我国典型的岬湾型淤泥质海岸之一。近百年来,在流域和沿岸人类活动的影响下,海岸经历了复杂的演变过程,研究其演变特征对认识此类海岸地形演变具有重要意义。基于1938—2023年共85年不同时期的水深和遥感影像数据,利用3S技术分析潮滩及水下地形冲淤变化。结果表明:①自1938年以来南尖潮滩面积不断下降,至2023年面积减少85.74%,共减少49.68 km2,围垦活动是导致潮滩萎缩的主要因素;②水下地形整体处于淤积状态,平均淤积厚度为0.57 m,水下地形在数十年尺度上冲淤演变规律复杂,不同阶段呈现冲淤交替的演变趋势,稳定性较差;等深线变化显著,0 m等深线整体向陆蚀退0.47 km,2、5和8 m等深线分别向海推进0.66、0.99和0.16 km。

       

      Abstract: ZhuangHe NanJian coast is one of the most typical Cape Bay mud coasts in China, over the past century, along with human activities in the watershed and along the coast, the coastal landform has undergone complex evolution laws, it is of great significance to study the evolution of this kind of coastal landform. Used the bathymetric data and remote sensing images from five periods since 1938, studied the tidal flats and offshore slope evolution based on 3S technology. The results showed that: ①The area of tidal flats has been declining since 1938, and by 2023 the area had decreased by 85.74%, a total decrease of 49.68 km2. Reclamation is the key factor causing its shrinkage. ②The whole subaqueous slope is in a siltation state, the average siltation thickness is 0.57 m, the evolution law of subaqueous slope on the scale of decades is complex, and the evolution trend of different stages is alternating, and the stability is poor; the isobath changes significantly, the 0m isobath retreated 0.47 km to the mainland, while the 2m, 5m and 8m isobath advanced 0.66 km, 0.99 km and 0.16 km to the sea.

       

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