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Detecting temporal shoreline changes and erosion/accretion rates, using remote sensing, and their associated sediment characteristics along the coast of North Sinai, Egypt

机译:使用遥感方法检测埃及北部西奈海岸沿岸的时间海岸线变化和侵蚀/富集率及其相关的沉积物特征

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The variation during 15 years in the shoreline along the North Sinai coast has been determined by analysing TM and ETM true colour Landsat images from 1986 to 2001. The analyses identified erosion and accretion patterns along the coast. The shoreline has advanced west of El Bardawil inletl, El Bardawil inlet2, and El Arish Harbour, where the wave-induced littoral transport has been halted by jetty construction and beach growth rates are 20,681, 69,855 and 20,160 m~2/year, respectively. On the downdrift side of the constructed jetties to the east, the shoreline is retreating and beaches erode at rates of -71,710, -69,968, and -11,760 m~2/year, respectively. Sedimentological analyses of beach sediment samples have indicated selective transport of heavy minerals according to their densities and grain sizes. A general correspondence has been found between variation in grain size, sorting and heavy-mineral content of beach sand and the patterns of shoreline changes.
机译:通过分析1986年至2001年TM和ETM真彩色Landsat影像,可以确定北西奈海岸沿岸15年间的变化。这些分析确定了沿海岸的侵蚀和增生模式。海岸线向西延伸至El Bardawil入口,El Bardawil入口2和El Arish港口,在这些港口,波浪导致的沿海运输因码头建设而停止,海滩增长率分别为20,681、69,855和20,160 m〜2 /年。在向东的人工跳船的下沉侧,海岸线正在退缩,海滩被侵蚀的速度分别为-71,710,-69,968和-11,760 m〜2 /年。沙滩沉积物样品的沉积学分析表明,根据重矿物质的密度和粒径,它们可以选择性地运输。人们已经发现,在沙粒的粒度,分选和重矿物含量的变化与海岸线变化的模式之间存在一般的对应关系。

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