长江中下游边滩泥沙运动特性初探

here are many compound channels which have bottomland with deep flume in the plain rivers of middle and downstream in Yangtse River. Side banks are the low one attach to the bank which have compound characteristics. They are support boundary of flow in the river channel. After SanXia Hinge working, the stability of the side banks are threatened by the less sands coming from the upriver. This article based on the renovation engineering of Majiazu and Zhoutian channel. Whereas the simulation technology of side bank construction protection, the shape of side banks sum up to 8 kinds. Based on kind 7and 8, movement experiments were made to summarize the sands movement line and the bottomland circumstances. Characteristics of sand movement around the side bank would be observed by using flume experiment in two conditions of flood and non-flood.