首页> 外文会议>Conference on Geospatial Information Technology and Applications; 20070525-27; Nanjing(CN) >Analysis on evolution process of the Meizizhou reach of the Yangtze River from the revetment based on GIS
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Analysis on evolution process of the Meizizhou reach of the Yangtze River from the revetment based on GIS

机译:基于GIS护岸的长江梅子洲河段演变过程分析。

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Based on the data, which are underwater relief maps of the lower reach of Yangtze River in the years of 1959,1970,1983,1992 and 2003 and three profiles investigated with utilizing Arc-GIS software, this paper studied the evolution process and differences in time and space influenced by revetment in Meizizhou reach of the Yangtze River. Comparing the proportion of the width and depth, and the swing velocities of the water-front and channel line, the results show that since the revetment was undertaken, the swinging range of left waterfront and channel line decreased distinctly and the channel plane distortion was controlled effectively. Then the riverbed was eroded continuously, on which the deepest point was moving towards right. The shoal on the head of Meizizhou becomes deeper and narrower. The channel trends to stability. The Third Nanjing Yangtze River Bridge has further effectively controlled the evolution process of the Meizizhou reach of the Yangtze River.
机译:基于这些数据,分别是1959年,1970年,1983年,1992年和2003年的长江下游水下浮雕图,并利用Arc-GIS软件研究了三个剖面,本文研究了长江流域的演变过程和差异。长江梅子洲段护岸对时空的影响。比较宽度和深度的比例,以及水岸线和河道线的摆动速度,结果表明,由于进行护岸,左侧水岸线和河道线的摆动范围明显减小,并且控制了水道面的变形。有效地。然后河床不断被侵蚀,最深的点向右移动。梅子洲头上的浅滩越来越深。渠道趋于稳定。南京长江第三大桥进一步有效地控制了长江梅子洲河段的演变过程。

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