长江科学院院报 ›› 2008, Vol. 25 ›› Issue (2): 26-28.

• 江湖泥沙与治理 • 上一篇    下一篇

基于DEM的河道演变可视化表达和定量分析

 胡红兵, 胡光道   

  1. 中国地质大学(武汉) 资源学院数学地质与遥感地质研究所,武汉430074
  • 出版日期:2008-04-01 发布日期:2012-03-05

DEMbased Visualization and Quantitative Analysis ofRiver Channel Evolution of South Branch in Changjiang Estuary

 HU  Hong-Bing, HU  Guang-Dao   

  • Online:2008-04-01 Published:2012-03-05

摘要: 为了解长江口南支河道近百年来的演变特征,利用该河道1900-2001年的海图资料,建立河道水下数字高程模型(DEM),并对其1900年以来的冲淤演变进行可视化表达和定量分析。结果表明:①DEM是进行河道演变可视化分析和定量分析的有效手段。②1900-2001年间长江口南支河道槽蓄量略微增大,0 m以深槽蓄量年均增大0.027亿m3;整个河道区域表现为微冲,年均冲刷量为0.033亿m3,年均冲刷厚度为0.37cm(包括人工挖泥吹填、疏浚量在内)。③不同时段和不同河段的冲淤状态不同。1958年以前和1979年以后河道演变表现为冲刷和扩大,在1958-1979年间为淤积;位于南支河道入口处和出口处断面的冲淤变化比河道中段断面剧烈。

关键词: 河道演变, DEM, 可视化表达, 长江

Abstract: The purpose of this paper is to analyze the evolution characteristics of the river channel of south branch in the Changjiang River estuary for the recent 100 years visually and quantitatively with the help of DEM technology. In support of GIS, 5 pieces of charts of south branch from 1900 to 2001 are digitized and the digital elevation model(DEM) of south branch in different periods is established with Kringing gridding method. On the basis of the above approach, the evolution of the river channel of south branch is visualized and the characteristics of erosiondeposition sedimentation are analyzed. The results show as follows: (1) DEM is an effective means for visualization and quantitative analyses of environmental evolution. (2) The river channel storage volume below 0 m increased slightly with the annual average rate of 0.027×108 m3,which coincided with the state of slight erosion of entire river channel with the annual average rate of 0.033×108 m3 of volume and 0.37 cm of thickness respectively from 1900 to 2001. (3) The states of erosion and siltation were different in different time domains and different stretches, scouring before 1958 and after 1979, whereas filling from 1958 to 1979; changes of cross sections at the entrance and exit were more intense than those in the middle of south branch.