摘要
简述三峡工程变动回水区的青岩子河段概况，分析该河段的自然演变规律及原因，并探讨了川江“走沙水”的形成机理。
General situation of Qingyanzi reach at backwater area of the Three-Gorges is briefly introduced. Regularity and reason of erosion & siltation of the reachunder natural condition are analyzed. Finally, the formation mechanism of the flow erodingsediment after main flood in Chuanjiang River is investigated and discussed.
出处
《水运工程》
北大核心
1999年第7期18-21,5,共5页
Port & Waterway Engineering
