Morphodynamics in a Tropical Shallow Lagoon: Observation and Inferences of Change

Alfred S. Alademomi, A. Manning, V. J. Abbott, R. Whitehouse
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引用次数: 1

Abstract

The Lagos Lagoon system and its adjacent tidal basins exhibit dynamics that are significantly different on both spatial and temporal scales. As urbanisation and human activities around the lagoon have intensified, the volume of sediment deposited into the basin is increasing on a daily basis. Changes on the lagoon bed over a 6-year time scale using repeated bathymetric data (2008, 2014) are presented, and the related data acquisition technique is explained. Data reduction is followed by analysis of the lagoon water bed dynamics using abstracted profile lines from the bathymetric data within a GIS environment. The results of the significant accretion and erosion within the lagoon system were analyzed spatially to quantify the volume of sediment gain or loss on the lagoon bed. The findings partly show that over 6 years, an average height of 0.16 m was gained by the lagoon. This amount translates into an annual accretion rate of 0.026 m. These findings enhance the prospect of verifying in the long term whether the Lagos Lagoon is gradually disappearing. To the best of the author ’ s knowledge, this research reveals for the first time the complex evolutionary changes (channel movement, accretion, erosion, infill and movement of shoal) on the Lagos Lagoon bed.
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热带浅泻湖的形态动力学:变化的观察和推论
拉各斯泻湖系统及其邻近的潮汐盆地在空间和时间尺度上都表现出显著不同的动态。随着城市化和环礁湖周围人类活动的加剧,沉积到盆地的沉积物量每天都在增加。介绍了使用重复水深数据(2008年,2014年)的6年时间尺度上泻湖床的变化,并解释了相关的数据采集技术。数据减少之后,使用GIS环境中水深数据的抽象剖面线分析泻湖水床动态。在空间上分析了泻湖系统内显著的吸积和侵蚀的结果,以量化泻湖床上的泥沙损失量。研究结果部分表明,在6年的时间里,泻湖的平均高度增加了0.16米。这个数字换算成每年0.026米的增长速度。这些发现增强了长期验证拉各斯泻湖是否正在逐渐消失的前景。据作者所知,本研究首次揭示了拉各斯泻湖河床复杂的演化变化(河道运动、淤积、侵蚀、填充物和浅滩运动)。
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