典型人类活动对砂质海岛岸滩演变的影响以海南马岛为例

Impact of Typical Human Activities on the Coastal Evolution of Sandy Islands: A Case Study of Ma Island, Hainan

  • 摘要: 全球气候变化背景下,海岛砂质岸滩普遍遭受不同程度的侵蚀。人类活动已成为影响海岛岸滩稳定的主要驱动力。有效识别影响海岛岸滩演化规律的主要因素,对海岛岸滩防护具有重要的意义。本文基于1964年数字栅格图、1984年至2022年11期历史遥感影像、2016年和2022年两期实测岸滩及周边海域水深等数据,探讨海南马岛岸线的动态变化、砂质岸滩冲淤演变及其驱动因素,结果表明,近60年来,受航道开挖和临近码头建设等典型人类活动的影响,马岛岸滩稳定性发生明显改变。马岛南、北两侧岸线位置分别向海推进0.10和0.06 km,海岛总岸线长度由5.24 km增长到8.29 km,增长速率为0.053 km/a;海岛面积由55.70 hm2增大到87.72 hm2,增长速率为0.552 hm2/a。马岛北部岸滩整体处于弱冲刷状态,冲刷深度一般小于1 m;相比之下,马岛南部岸滩整体处于动态平衡状态,地形变化幅度在−1~1 m。典型人类活动明显改变了岸滩的自然演化进程,马岛东北部区域的周边海底处于淤积状态,平均淤积深度约为1 m,最大淤积达3 m,位于拟建桥梁区域。由于地形变化,马岛东侧断开处海域水深较未开挖前变深3~6 m。本文研究结果可为海岛保护与开发利用提供科学依据。

     

    Abstract: In the context of global climate change, sandy coastlines of islands are widely subject to different degrees of erosion. Human activities have become a primary driver force affecting the stability of island coastlines. Effectively identifying the key factors influencing the evolutionary pattern of island coastlines holds significant importance for coastline protection. Based on the data including 1964 digital topography map, 11 phases of historical remote sensing images during 1984-2022, and measured coastline and surrounding bathymetric data in 2016 and 2022, discussed the dynamic changes in coastline, erosion-deposition pattern of sandy beaches, and their driving factors on Ma Island, Hainan. The results show that typical human activities such as channel excavation and pier construction have significantly altered the stability of the island’s coastlines over the past 60 years. The southern and northern coastlines advanced seaward by 0.10 km and 0.06 km, respectively, while the total coastline length increased from 5.24 km to 8.29 km, with a growth rate of 0.053 km/a. The area of the island expanded from 55.70 hm2 to 87.72 hm2, at a rate of 0.552 hm2/a. The northern coastline experienced weak erosion, with scouring depths less than 1 m, whereas the southern coastline remained in dynamic equilibrium, with topographic changes ranging between −1 m to 1 m. Typical human activities have notably disruped the natural evolution of the coastlines. The seabed near the northeastern area of the Ma Island has accumulated sediment with an average deposition depth of approximately 1 m, with a maximum of 3 m near the proposed bridge site. Due to these topographic changes, water depths in the eastern disconnected area of the island increased by 3-6 m compared to pre-excavation conditions. The findings of this study provide a scientific basis for the protection and sustainable development of islands coastlines.

     

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