The main watercourse of Yangtze was made of some surface river sectors and underground rivers.
地表河与地下河相连接构成长江主河道。
The productive embankments on the watercourse bottomland disturb the water-sediment lateral exchange between bottomland and main flume, which have great influence on the riverbed evolution.
河道主槽两侧修建的生产堤影响滩槽泥沙横向交换,对河床演变带来很大影响。
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