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SEDIMENT TRANSPORT NEAR JINGTANG PORT BASED ON REMOTE SENSING TECHNOLOGY

机译:基于遥感技术的景垄港附近的沉积物运输

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The Jingtang Port is located between two estuaries on the north side of the Bohai Bay, the Daqinghe Estuary and the Luanhe Estuary. The adjacent coastline of the port is NE~SW orientation, with some longshore bars and lagoons. The port is the first Chinese large port built on fine sand coasts where sediment transport is relatively active. Due to the sediment coming from the Luanhe River decreased shapely, longshore transport resulted in erosions along the downdrift coastline. As a remote sensing media, satellite images can record the shore line positions and the nearshore bar shapes. Such images were used to analysis evolution of the coastline near the port, and to further study the sediment transport characteristics and the reason of siltation in the access channel. Comparisons of the images at different time showed that the offshore sides of the bars retreated, while the outlines of the bars shifted southwestward, which indicated that the longshore transport was from northeast to southwest. The sediment was stirred up by large waves and transported by strong tidal currents, which caused the sudden siltation in the access channel.
机译:京塘港位于渤海湾北侧的两个河口之间,大庆海河和滦河河口。港口的相邻海岸线是NE〜SW定位,有一些漫长的酒吧和泻湖。该港口是第一批在细砂海岸上建造的中国大港,其中沉积物传输相对活跃。由于来自滦河的沉积物匀称,龙岸运输导致了沿着颠覆压海岸线的侵蚀。作为遥感介质,卫星图像可以记录岸线位置和近孔条形。这些图像用于分析港口附近的海岸线的演变,进一步研究沉积物传输特性和淤积在接入通道中的原因。在不同时间的图像的比较表明,酒吧的海上侧面撤退,而巴斯的轮廓向西南移动,这表明龙岸运输是从东北到西南部的。沉积物被大波浪搅拌并通过强潮流运输,这导致通道中的突然淤积。

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