摘要
为弄清磨刀门水道河床演变及其冲淤成因,利用历年实测地形资料,建立DEM模型,进行河床演变分析,结果表明:磨刀门水道主槽不断冲刷,滩地有淤有冲。从上游来水来沙条件、河床边界条件、人类活动等方面进行冲淤成因分析,确定主要影响因素,预测河床演变趋势,为将来河道治理与开发提供科学依据。
Use of historic terrain data, Digital Elevation Model for the evolution of the reach is established. The results indicate that:1 )Modaomen reach main channel keeps being eroded;2)beaches is general charactered by siltation. In order to clarify the reasons of riverbed deformation, We analyze the reason of the riverbed de- formation from upstream inflow and sediment conditions, riverbed boundary conditions and human activities, etc. we determine the main influence factors and forecast riverbed evolution trend. The research results pro- vide a scientific basis for river management and development in the future.
作者
林凤标
郑国栋
刘壮添
LIN Feng-biao ZHENG Guo-dong LIU Zhuang-tian(Guangzhou Branch of Zhe Jiang Guiren Information Technology Co, Ltd. , Guangzhou 510670, China Pearl River Water Resources Commission, Pearl River Scientific Research htstitute, Guangzhou 510610, China)
出处
《泥沙研究》
CSCD
北大核心
2017年第3期48-53,共6页
Journal of Sediment Research
关键词
磨刀门水道
河床演变
冲淤成因
Modaomen river
riverbed evolution
causes of erosion and siltation