首页> 外文OA文献 >Influence on present-day coastal dynamics and evolution of a relict subaqueous delta lobe: Sol de Riu lobe, Ebro Delta. Continental Shelf Research, 74: 94-104. doi:10.1016/j.csr.2013.11.021
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Influence on present-day coastal dynamics and evolution of a relict subaqueous delta lobe: Sol de Riu lobe, Ebro Delta. Continental Shelf Research, 74: 94-104. doi:10.1016/j.csr.2013.11.021

机译:对当今沿海动力学的影响以及遗骸水下亚三角洲的演化:埃布罗三角洲的Sol de Riu三角洲。大陆架研究,74:94-104。 doi:10.1016 / j.csr.2013.11.021

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摘要

We used high-resolution swath-bathymetry data to characterise the morphology of the abandoned subaqueous Sol de Riu delta lobe in the Ebro Delta, Western Mediterranean Sea. This study aims to assess the influence of an abandoned delta lobe on present-day coastal dynamics in a micro-tidal environment. Detailed mapping of the relict Sol de Riu lobe also showed a set of bedforms interpreted as footprints of human activities: seasonal V-shaped depressions on the middle shoreface due to boat anchoring and old trawling marks between 16 and 18 m water depth. Estimations of the mobility of bottom sediment showed that the shallowest shoreface (i.e. less than 7 m depth) is the most dynamic part of the relict lobe, while the middle shoreface experienced significant morphological changes since the lobe was abandoned. The deepest shoreface (i.e. water depth in excess of 15 m), which corresponds to the front of the lobe, is defined by a very small potential for morphological change. Simulations showed that while the relict lobe does not significantly affect the typical short period waves (Tp ≈4 s) in the study area, it does interfere with the most energetic wave conditions (Tp ≥ 7 s) acting as a shoal leading to the concentration of wave energy along the shoreline northwest of the lobe. The consequence of such modification of the high-energy wave propagation pattern by the relict lobe is an alteration of the wave-induced littoral sediment dynamics with respect to a situation without the lobe.
机译:我们使用高分辨率的条带测深仪数据表征了西地中海埃布罗三角洲遗弃的水下Sol de Riu三角洲叶的形态。这项研究旨在评估微潮环境中废弃三角洲对当今沿海动力学的影响。残骸Sol de Riu叶片的详细地图还显示出一组被解释为人类活动足迹的床形:由于船锚和水深在16至18 m之间的旧拖网痕迹,中间岸面上出现季节性V形凹陷。对底部沉积物迁移率的估算表明,最浅的海岸面(即小于7 m的深度)是遗迹波瓣最活跃的部分,而中间的海岸坡由于废弃了该叶而经历了明显的形态变化。对应于波瓣前缘的最深的岸面(即超过15 m的水深)是由很小的形态变化潜力定义的。模拟表明,尽管遗迹波对研究区域的典型短时波(Tp≈4s)没有明显影响,但确实干扰了最活跃的波状条件(Tp≥7 s),从而导致了集中。沿波瓣西北海岸线的波能。遗叶对高能波传播模式的这种改变的结果是,相对于没有叶的情况,波浪引起的沿海沉积物动力学发生了变化。

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