水库下游河流再造床过程中的河岸侵蚀
Lateral erosion in downstream of the reservoir
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摘要: 根据实测河道地形资料,分析了水库下游河床演变中的河岸侵蚀现象,包括不同横向边界约束条件、不同床沙组成和不同河型河段的河岸侵蚀的特征及规律。结果表明:①水库下游均会有河岸侵蚀发生,但初期一般以下切为主,后期以展宽为主。②对于横向边界约束较强的河段,河岸侵蚀相对较弱;相反,则河岸坍塌严重,河岸侵蚀强烈;③对不同的河床组成和边滩组成的河段:河床较粗特别是形成抗冲粗化层,且边滩组成较细的河段,河岸侵蚀现象非常剧烈;河床组成较细的河段,如果边滩抗冲性较强,则河岸侵蚀现象相对较弱,如果滩地组成较细、容易坍塌,河岸侵蚀也会较强;④不同的河型有着不同的河岸侵蚀现象。分汊河段以主汊为主;游荡段的游荡特性在初期受到抑制;弯曲河段的撇弯切滩现象较普遍。Abstract: Based on the field data,the lateral erosion in the downstream of the resemvir is dealt with in the paper.The effect of lateral boundary condition,the river regime and the bed material on lateral erosion are analyzed.Some conclusions could be drawn:①The lateral erosion does exist in the downstream of the resemvir.The lateral erosion is slight at the begining,and then gradually enhanced,sometimes the lateral erosion in the downstream may result in a bigger width than before;②In the reaches where the lateral boundary conditions are strong,the lateral erosion is weak and it is strong in the reaches where the lateral boundary conditions are weak;③In the reaches where the bed material is coarse and the material in the bank is fine,the lateral erosion is strong,while in the reaches where the bed material is fine and the erosive resistance of bank is strong,the lateral erosion i s weak;And④in the bifurcated reaches,the lateral erosion mainly happens in the main channel;In the wandering reaches,the character of wandering is controlled firstly and the effect of lateral erosion is submerged;In the meandering reaches,the phenomena of the cut-bank and thrown-away-elbow are prevalent.